- Research article
- Open Access
Arthroaspisn. gen., a common element of the Sirius Passet Lagerstätte (Cambrian, North Greenland), sheds light on trilobite ancestry
BMC Evolutionary Biology volume 13, Article number: 99 (2013)
Exceptionally preserved Palaeozoic faunas have yielded a plethora of trilobite-like arthropods, often referred to as lamellipedians. Among these, Artiopoda is supposed to contain taxa united by a distinctive appendage structure. This includes several well supported groups, Helmetiida, Nektaspida, and Trilobita, as well as a number of problematic taxa. Interrelationships remain unclear, and the position of the lamellipedian arthropods as a whole also remains the subject of debate.
Arthroaspis bergstroemi n. gen. n. sp., a new arthropod from the early Cambrian Sirius Passet Lagerstätte of North Greenland shows a striking combination of both dorsal and ventral characters of Helmetiida, Nektaspida, and Trilobita. Cladistic analysis with a broad taxon sampling of predominantly early Palaeozoic arthropods yields a monophyletic Lamellipedia as sister taxon to the Crustacea or Tetraconata. Artiopoda is resolved as paraphyletic, giving rise to the Marrellomorpha. Within Lamellipedia, a clade of pygidium bearing taxa is resolved that can be shown to have a broadly helmetiid-like tergite morphology in its ground pattern. This morphology is plesiomorphically retained in Helmetiida and in Arthroaspis, which falls basally into a clade containing Trilobita. The trilobite appendages, though similar to those of other lamellipedians in gross morphology, have a unique outward rotation of the anterior trunk appendages, resulting in a ‘hard wired’ lateral splay, different to that observed in other Lamellipedia.
The combination of helmetiid, trilobite, and nektaspid characters in Arthroaspis gives important hints concerning character polarisation within the trilobite-like arthropods. The distinctive tergite morphology of trilobites, with its sophisticated articulating devices, is derived from flanged edge-to-edge articulating tergites forming a shield similar to the helmetiids, previously considered autapomorphic for that group. The stereotypical lateral splay of the appendages of lamellipedians is a homoplastic character shown to be achieved by several groups independently.
Arthropod diversity in the Cambrian is now reasonably well-known through the discovery and description of the faunas from the Chengjiang, Emu Bay Shale, and Sirius Passet Lagerstätten in the early Cambrian, the Burgess Shale and similar deposits in the middle Cambrian, and the Orsten-type deposits, mostly from the late Cambrian. When the true diversity of these taxa became clear in the 1970s, their unfamiliarity prompted the view that they represented the end points of many independent lines of evolution that had convergently undergone arthropodisation . However, this view was relatively short-lived in the advent of rigorous cladistic analysis [2, 3], and the essential similarity between many of these taxa began to be recognised . The first full-blown cladistic analysis of the Burgess Shale taxa was that of D. E. G. Briggs and R. A. Fortey , which suggested that most Cambrian arthropods lay within the stem group of Chelicerata, and that the trilobites were relatively derived. An important exception to this view were the arthropods of the Orsten fauna, some of which have been shown convincingly to lie in the stem- and crown-group of Crustacea or Tetraconata [6–10].
More recently, the view that some Cambrian arthropods lie outside the crown-group of Euarthropoda has gained ground [11–13]. These taxa include, for example, Fuxianhuia protensa Hou, 1987, Chengjiangocaris longiformis Hou & Bergström, 1991, and Shankouia zhenghei Chen, Wang, Maas & Waloszek in Waloszek et al., 2005. Whether taxa such as Canadaspis perfecta (Walcott, 1912) are derivatives of the euarthropod stem-lineage [14–16] or represent the crown-group  is still a matter of debate. Another open debate is whether Megacheira, including taxa such as Leanchoilia superlata Walcott, 1912 and Yohoia tenuis Walcott, 1912 fall outside Euarthropoda [12, 14, 16, 18, 19] or are derivatives of the early chelicerate stem-lineage [20–24].
There is consensus that Trilobita belongs to Euarthropoda, but there are two competing hypotheses for their phylogenetic position within the monophylum. The traditional Arachnomorpha [20, 22, 25–27] is being increasingly questioned, and an increasing number of studies suggest trilobites to be derivatives of the mandibulatan stem-lineage [16, 19, 28–31]. Regardless, there is consensus that trilobites belong to a larger group of early Paleozoic arthropods, containing many of the non-biomineralizing taxa attributed to Arachnomorpha. They share the presence of distinctive lamellar blades on their exopods, and X-g. Hou and J. Bergström proposed Lamellipedia to embrace them . In its original concept, Lamellipedia was a grade comprising the stem-lineage of Chelicerata, including the non-chelicerate arachnomorphs except for Megacheira . Within Lamellipedia, the basal split set off Marrellomorpha from Artiopoda, which comprised the remainder of the chelicerate stem-lineage. Some authors have suggested that Artiopoda could be a monophylum based on the shared presence of a rather similar limb with a bilobate exopod of a proximal lobe bearing the lamellae and a flap-like distal lobe fringed with setae  and indeed they were rendered monophyletic in some analyses [16, 19, 31]. While most analyses yield a number of well supported groups of artiopodans, in particular Helmetiida, Nekatspidida, Trilobita, and Xandarellida, their interrelationships remain unclear [19, 22, 26, 27, 31, 32].
In summary, then, whereas several groups of Cambrian arthropods are clearly related, their overall relationships remain uncertain. Furthermore, the monophyletic or paraphyletic status of several of these groupings remains in question. Whilst this debate will not be resolved quickly – it depends partly on differences in philosophy of systematics – the further description of exceptionally-preserved taxa will aid its resolution. Here, then, we describe a new exceptionally-preserved lamellipedian arthropod from the Sirius Passet Lagerstätte that adds significant new data to the debate, and that also has a bearing on the ecology of these early arthropods.
The Sirius Passet Lagerstätte
The discovery of the Sirius Passet Lagerstätte was announced by S. Conway Morris, J. S. Peel, A. K. Higgins, N. J. Soper, and N. C. Davis  and has been recounted by S. Conway Morris  and J. S. Peel and J. R. Ineson . The fossiliferous strata crop out in north-west Peary Land along the southern slopes of the broad valley which gives its name to the locality and just south of the mountainous northern rim (Nansen Land) of Greenland (lat. 82°47.6´N, long. 42°13.7´W); it is the most remote and least well known of the classic Cambrian Explosion biotas. The lagerstätte is of early Cambrian age, (Cambrian Series 2, Montezuman Stage of Laurentian usage ).
The geological setting was described by J. S. Peel and J. R. Ineson [35, 37]; it is now known that the deposits yielding exceptional preservation are located within a 14 m interval of the Buen Formation at the main locality  and fossils are especially common in the middle part of the section. However, the relationship of other fossiliferous localities in the immediate vicinity to the main locality is uncertain . Since its discovery in 1984, expeditions in 1985, 1989, 1991, 1994 and 2006, partly under the auspices of the Geological Survey of Greenland, have assembled almost 10 000 specimens mainly from talus below the main outcrop . More than 30 species have been described in detail to date [38, 39] and the fauna is dominated by arthropods, lobopods and cycloneuralian and polychaete worms. New collections made during expeditions from the Natural History Museum, University of Copenhagen, in 2009 and 2011 focussed on in situ material from the main exposure of the Transitional Buen Formation at the Sirius Passet locality [40, 41] and have allowed the mapping of faunal associations within the formation.
The Buen Formation crops out across a large part of North Greenland [42, 43]. Its siliciclastic sediments represent the expansion of a northern basin across a subsiding carbonate platform to the south within the trans-arctic Franklinian Basin succession. In southern areas the formation is dominated by sandstones but the proportion of coarse-grained siliciclastics decreases northwards into the deeper-water parts of the basin. In the vicinity of the Sirius Passet locality, a narrow belt (200 – 1400 m wide) of mainly fine-grained siliciclastic sediments forms a transitional zone between the southern shelf succession and the equivalent deep-water basinal deposits of the Polkorridoren Group to the north [35, 42]. This so-called Transitional Buen Formation includes the fossiliferous deposits of the Sirius Passet Lagerstätte .
Bioturbation, indicated by mottling, is pervasive throughout much of the Transitional Buen Formation except for the lagerstätte intervals, where the lamination is strongly developed, showing partings at a 3–10 mm scale. A depositional setting on the outer parts of the shelf to upper slope, possibly dominated by suspension fallout material [35, 42] is envisaged.
The understanding of the preservational processes in the Sirius Passet Lagerstätte is far less advanced than those for the Burgess [44–46] and Chengjiang  lagerstätten. The preservation of the Greenland fossils appears to differ significantly from that of other Cambrian exceptionally-preserved faunas, with early mineralisation appearing to play an important role [48, 49]. However, preservation within the Sirius Passet Lagerstätte is variable. Mineralised forms such as trilobites, hyolithids and articulated halkieriids preserve much of their relief while even un-mineralised organisms retain a measure of 3-dimensional form. At certain horizons relief is lost and organisms are preserved as reflective films. The Sirius Passet fossils are often visually unimpressive when compared to those from Chengjiang or the Burgess Shale. It is characteristic that central regions of many fossils, mainly the body cavity, tend to be best preserved in contrast to the poor definition of body outlines (e.g. Kerygmachela kierkegaardi Budd, 1993 , Pambdelurion whittingtoni Budd, 1997 , and Campanamuta mantonae Budd, 2011 ; preferential preservation of the central regions is possibly associated with high concentrations of carbon . As a result, taphonomic insights gained from other faunas should only be applied with caution to these fossils. This can make comparison of these to more conventionally-preserved taxa difficult. In addition the high metamorphic grade, illustrated by abundant acicular chlorite crystals within the sediments, adds a further dimension to the understanding of a complex set of taphonomic pathways.
The new taxon is large (some specimens exceed 20 cm in length). Specimens, as preserved, appear generally robust with good relief and show few wrinkles, and are largely complete although isolated thoracic tergites, limbs and cephalic and pygidial shields are not uncommon. The majority of the specimens appear to have been preserved in situ, with little or no evidence of transport and the wide range of instars confirms the remains of a census population.
The specimens of the new taxon are generally characterised by a network of complex, interconnected burrow systems constructed by a meiofauna and small macrofauna of invertebrates [36, 37, 39, 54]. Moreover apart from providing an oasis of primary nutrients in an otherwise poorly-resourced landscape, high sulphate concentrations may have encouraged the colonization of the burrows by sulphur bacteria, providing a secondary food source . The slowly decaying carcasses clearly attracted invertebrate communities that both mined and farmed the burrow systems.
Initial impressions of the sediments suggest deposition within dysoxic environments; nevertheless specimens of the new taxon are preserved with a post-mortem, commensal epifauna of small invertebrates. The dark shales within the lagertätte intervals are, however, punctuated by thin partings of coarser sediment, which suggest a periodic freshening of the sediment-water interface and the potential to transport living meiofauna into deeper-water environments where they could profitably engage with the Arthroaspis carcasses. The proposed presence of sulphate and sulphur bacteria  suggests oxygen deprivation that would inhibit destructive, microbial activity  and the coarser-grained sediments, the distal products from shelfal storms, subsequently entombed the large arthropods in obrution deposits. The large Arthroaspis clearly thrived in conditions at the sediment-water interface but its preservation was aided by local dysoxic conditions within the sediment and the cover of coarser sediments derived from upslope.
Where required, specimens were prepared with a pneumatic chisel. All specimens were cleaned with an ultrasonic bath and coated with colloidal graphite that was applied with an air brush. Prior to photography specimens were coated with ammonium chloride. Photographs were taken under low-angle light.
The description in general refers to large specimens that represent holaspids; morphometric change throughout holaspid ontogeny was not studied in detail. The post-antennular limbs are not sufficiently well-known to allow their individual description, although a general understanding of their structure is possible.
Repositories: MGUH, Natural History Museum of Denmark, Copenhagen, Denmark; USNM, National Museum of Natural History, Smithsonian Institution, Washington, DC.
Terminology follows standard trilobite terminology  complemented with descriptive terminology applied to exceptionally preserved arthropods from the Orsten and Burgess Shale Lagerstätten [31, 56]. Deviating from these works, the term trunk in the following refers to the thorax and pygidium combined, and hypostomal complex to the hypostome and prehypostomal sclerite. Abbreviations used in the figures are summarized in Table 1.
The cladistic analysis of 74 characters scored for 54 taxa (section Taxa included in the analysis) was run in TNT  under both equal and implied weights. A heuristic search algorithm was employed with 10000 replicates using the ratchet and drift algorithms. Searches were carried out both unweighted and with implied weights using concavity constants k=1–20, 22, 24, 26, 28, 30, 35, 40, 50, 75, 100, 150, 300, 400, 500, 750, and 1000. A file including the character matrix and trees obtained under unweighted analysis is included in .nex format within the article’s Additional file 1.
The characters are broadly based on those of J. Ortega Hernández, D. A. Legg, and S. J. Braddy , but the taxonomic scope has been altered, and a number of character codings changed. Shankouia zhenghei Chen, Wang, Maas and Waloszek in Waloszek, Chen, Maas & Wang, 2005 has been used as an out-group rather than Fortiforceps foliosa Hou & Bergström, 1997. The latter has been discussed as a possible derivative of the chelicerate stem-lineage [21, 23] and therefore is more suitable as part of the analysed in-group. All aglaspidid taxa except Aglaspis spinifer Raasch, 1939 and Flobertia kochi Hesselbo, 1992 have been removed since internal aglaspidid relationships are not the focus of the present analysis. The problematic “arachnomorphs” Nettapezoura basilika Briggs, Lieberman, Hendricks, Halgedahl & Jarrard, 2008, Dicranocaris guntherorum Briggs, Lieberman, Hendricks, Halgedahl & Jarrard, 2008 from the Cambrian Series 3 of Utah, the putative artiopodans Panlongia Liu & Luo in Liu, Luo, Chen & Hu, 2006, Buenaspis forteyi Budd, 1999, and Pygmaclypeatus daziensis Zhang, Han & Shu, 2000, and the cheloniellids Duslia insignis Jahn, 1893, Neostrabops martini Caster & Macke, 1952, Pseudarthron whittingtoni Selden & White, 1983, and Triopus draboviensis Barrande, 1872 have been removed because of the paucity of information on their morphology. The scope of artiopodan taxa has been extended by Arthroaspis bergstroemi n. gen. n. sp., Australimicola spriggi Paterson, García-Bellido & Edgecombe 2012, Campanamuta mantonae Budd, 2011 and the nektaspids Emucaris fava Paterson, Edgecombe, García-Bellido, Jago & Gehling, 2010 and Kangacaris zhangi Paterson, Edgecombe, García-Bellido, Jago & Gehling, 2010, and the trilobite Triarthrus eatoni (Hall, 1838). Further taxa added are the problematic Agnostus pisiformis (Wahlenberg, 1818), Isoxys volucris Williams, Siveter & Peel, 1996, and Kiisortoqia soperi Stein, 2010, and the stem lineage crustaceans Henningsmoenicaris scutula (Walossek & Müller, 1990), Oelandocaris oelandica Müller, 1983. The taxa included in the analysis are summarized in the section Taxa included in the analysis.
Taxa included in the analysis
*Shankouia zhenghei Chen, Wang, Maas and Waloszek in Waloszek, Chen, Maas & Wang, 2005
Aglaspis spinifer Raasch, 1939
Agnostus pisiformis (Wahlenberg, 1818)
Alalcomenaeus cambricus Simonetta, 1970
Arthroaspis bergstroemi n. gen. n. sp.
Australimicola spriggi Paterson, Garcíía-Bellido & Edgecombe, 2012
Burgessia bella Walcott, 1912
Campanamuta mantonae Budd, 2011
Cheloniellon calmani Broili, 1932
Cindarella eucalla Chen, Ramsköld, Edgecombe & Zhou in Chen, Zhou, Zhu & Yeh, 1996
Emeraldella brocki Walcott, 1912
Emucaris fava Paterson, Edgecombe, García-Bellido, Jago & Gehling, 2010
Eoredlichia intermedia (Lu, 1940)
Flobertia kochi Hesselbo, 1992
Fortiforceps foliosa Hou & Bergström, 1997
Haikoucaris ercaiensis Chen, Waloszek & Maas, 2004
Helmetia expansa Walcott, 1918
Henningsmoenicaris scutula (Walossek & Müüller, 1990)
Isoxys volucris Williams, Siveter & Peel, 1996
Jiangfengia multisegmentalis Hou, 1987a
Kangacaris zhangi Paterson, Edgecombe, García-Bellido, Jago & Gehling, 2010
Kiisortoqia soperi Stein, 2010
Kuamaia lata Hou, 1987b
Kwanyinaspis maotianshanensis Zhang & Shu, 2005
Marrella splendens Walcott, 1912
Martinssonia elongata Müller & Walossek, 1986
Mimetaster hexagonalis Gürich, 1931
Misszhouia longicaudata (Zhang & Hou, 1985)
Molaria spinifera Walcott, 1912
Naraoia compacta Walcott, 1912
Naraoia spinosa Zhang & Hou, 1985
Oelandocaris oelandica Müller, 1983
Olenoides serratus (Rominger, 1887)
Phytophilaspis pergamena Ivantsov, 1999
Retifacies abnormalis Hou, Chen & Lu, 1989
Saperion glumaceum Hou, Ramsköld & Bergström, 1991
Sidneyia inexpectans Walcott, 1911
Sinoburius lunaris Hou, Ramsköld & Bergström, 1991
Siriocaris trollae Lagebro, Stein & Peel, 2009
Skioldia aldna Hou & Bergström, 1997
Soomaspis splendida Fortey & Theron, 1994
Squamacula clypeata Hou & Bergström, 1997
Tariccoia arrusensis Hamman, Laske & Pillola, 1990
Tegopelte gigas Simonetta & Delle Cave, 1975
Triarthrus eatoni (Hall, 1838)
Weinbergina opitzi Richter & Richter, 1929
Xandarella spectaculum Hou, Ramsköld & Bergström, 1991
Yohoia tenuis Walcott, 1912
Leanchoilia superlata Walcott, 1912 and Leanchoilia illecebrosa (Hou, 1987) (combined)
Liwia plana (Lendzion, 1975) and convexa (Lendzion, 1975) (combined)
Most of the characters are derived, with modification, from Ortega Hernández, Legg, and Braddy . Characters pertinent only to the internal relationships of aglaspidids have been removed, whilst other characters have been added from previous studies of Cambrian arthropods [31, 32, 59, 60]. The characters are listed below. Explanations are given where they have been significantly modified or the scoring differs from that of previous authors.
1. Nature of first cephalic appendage: (0) limb-like appendage; (1) antennae. Modified from Ortega Hernández et al. character 1. Limb-like appendage, substituted for raptorial , applies to any appendage that is not a specialised sensorial appendage. This character was coded by Ortega Hernández et al. as state one for Aglaspis, Kwanyinaspis, and Sinoburius, but has been coded as uncertain for all of these taxa here. No antennulae are preserved in Kwanyinaspis and from Aglaspis only the most proximal articles are known  while in Sinoburius there are only impressions that have been interpreted as antennulae [12, 26]. The antennula of Martinssonia is interpreted as a feeding antennula  as is that of Rehbachiella .
2. Composition of first cephalic appendage: (0) 7–15 articles; (1) > 15 articles; (2) ≤ 7 articles. Modified from Stein and Selden character 19 , the autapomorphic state for Oelandocaris has been removed and the character is here coded as unknown for that taxon. Contrary to Stein and Selden, the character is not coded as state 0 for Saperion; the antennula in the specimen on which that coding was based (fig. 3.1, 7.1 of Edgecombe and Ramsköld ) appears to be incomplete, preservation terminates at a scarp.
3. Armature of first cephalic appendage: (0) none; (1) pair of simple, robust spines medioventrally on each article; (2) setae on mediodistal margin of articles; (3) single, large, medodistal spine or finger. Modified from Stein and Selden character 21; the autapomorphic state for Oelandocaris has been removed and the character is coded as unknown for that taxon.
4. Number of articles with fingers in short feeding appendage: (0) four; (1) three; (2) two. Modified from Ortega Hernández et al. character 2. The character is here coded unknown for Aglaspis, Kwanyinaspis, and Sinoburius, rather than inapplicable because the antennular morphology is not known for these taxa. The character was coded as state 2 for Fortiforceps and state 1 for Yohoia by Ortega Hernández et al., but both have four fingers .
5. Long spinose projections on distal part of terminal three podomeres of great appendage bearing a flagellum: (0) absent; (1) present. Substituted for character 4 of Ortega Hernández et al. Modified from character 6 of Edgecombe et al. . Here coded unknown for Aglaspis, Kwanyinaspis, and Sinoburius, rather than inapplicable as coded by Ortega Hernáández et al.
6. Feeding appendage with elbow joint: (0) absent; (1) present. This is a newly added character based on the recognition of an elbow joint in the great appendage of megacheirans .
7. Number of appendage bearing post-ocular segments incorporated into the head/prosoma: (0) one; (1) four; (2) five; (3) six; (4) seven. Modified from character 5 of Ortega Hernández et al. Cheloniellon has been coded as having four post-ocular segments (state 1) rather than five. Figure 11a in the redescription by W. Stürmer and J. Bergström  shows that the fourth appendage posterior to the antennula inserts under the first trunk tergite, the fifth under the second. Then there is a gap due to the appendages posteriorly being flipped backward. Marrella and Mimetaster are coded as unknown. Counts of segments in these taxa seem to rest on the number of specialised appendages, while in other taxa the number of segments carrying unspecialised appendages incorporated into the cephalic shield is counted. In both taxa, the latter count can not be established. The character is coded unknown for Naraoia compacta. The character is coded as state 3 (six segments) for Pycnogonida rather than state 4 (seven segments). It is unknown for Sidneyia and Squamacula; there is no direct evidence for cephalic appendages available in Squamacula, and reexamination of the Sidneyia material revealed the presence of gnathobases in the head, though the number cannot be established (Stein in preparation). The number is unknown for Sinoburius, where only impressions of the appendages are known.
8. Exopod on first post-antennular appendage: (0) present; (1) absent. Modified from character 6 of Ortega Hernández et al. This was coded as state 1 for Emeraldella; the character is coded here as unknown for that taxon since, while evidence for presence of an exopod in that limb is inconclusive, there is no evidence of absence . The character has been coded as unknown for Liwia, as no postantennular appendages are preserved. Likewise in Sinoburius where only impressions of the appendages are preserved with no evidence of exopods and Sidneyia, Squamacula, Skioldia, and Saperion where number and morphology of the cephalic appendages are unknown. In Marrella, the second cephalic appendage is a swimming arm. A similar swimming arm occurs in the marrellomorph Vachonisia rogeri Lehmann, 1955  where it is formed by the exopod, and given the correspondence in morphology, this appendage in Marrella is here interpreted as an exopod. The character is coded as unknown for Mimetaster.
9. Exopod on second post-antennular appendage: (0) present; (1) absent. Character 7 of Ortega Hernández et al. The character has been coded as unknown for Liwia, Saperion, Sidneyia, Sinoburius, Skioldia, and Squamacula (see comment on previous character). The second post-antennular appendage of Marrella carries an exopod independent of whether or not it is incorporated into the head, and it has been coded as state 0. The second postantennular appendage of Mimetaster is uniramous  but by comparison with Vachonisia, where the main rami are the exopods , it is not clear if the rami in Mimetaster are endopods or exopods, and the character has been coded as unknown for that taxon.
10. Insertion of cephalic exopods: (0) as in trunk; (1) shorter joint. Character 31 of Stein and Selden.
11. Cephalic endopods: (0) as in trunk limbs; (1) first postantennular limb with fewer podomeres or reduced; (2) endopod of first postantennular limb heavily reduced or absent, of second postantennular limb considerably more slender than in trunk and fewer podomeres. Modified from character 33 of Stein & Selden. Coded as inapplicable for Pycnogonida where the second cephalic appendage is the oviger, and Eurypterida where all appendages are differentiated.
12. Composition of first and second cephalic exopods: (0) as in trunk limbs; (1) multiarticulate, each article with mediodistal setae or pair of lateral setae. Character 34 of Stein and Selden.
13. Trunk endopods: (0) absent or reduced; (1) present. Character 9 of Ortega Hernández et al. Coded inapplicable for Pycnogonida where there is no trunk. No postantennular appendages are preserved in Liwia, so the character is coded as unknown for that taxon.
14. Exopod structure: (0) simple oval flap; (1) bilobate flap, exopod differentiated into proximal and distal lobes; (2) numerous articles; (3) book gills. Modified from character 10 of Ortega Hernández et al. Specifics on setation have been removed from this character. State 3 of Ortega Hernández et al. (undivided with lamellar setae) which was autapomorphic for Retifacies, has been removed since the exopod structure of that taxon is not well known. It is unclear if the most distal lamella as drawn in figure 51 of Hou and Bergström  is a lamella or the distal article of a bilobate exopod. The character has been coded unknown for Retifacies, and further for Burgessia, for which details of the exopods are also unknown. It is coded as unknown for Liwia, Sinoburius, and Skioldia. For Skioldia only impressions of the lamellae are known (figure 16.54 in ). Nebalia has differentiated exopods in the cephalic appendages, but the exopods of the more serially similar thoracopods and pleopods are best described as simple flaps. Similarly, in Martinssonia and Rehbachiella the exopods of the more posterior appendages are simple flaps [7, 10]. Those of Sidneyia are differentiated into proximal and distal lobes, with the proximal lobe carrying the lamellae (Stein in preparation). In Squamacula only the large flap is visible , but if the appendage structure is similar to that of Sidneyia, the proximal lobe could be inaccessible and the character is coded as unknown for that taxon. The exopods of Tegopelte are differentiated into proximal and distal lobes as best seen in newly published photographs . There is also evidence of the exopods in Cheloniellon being differentiated into proximal and distal lobes; the flap-like lobe clearly inserts into a narrower portion in figures 8a, 11 of Stürmer and Bergström .
15. Proximal lobe of exopod: (0) flattened lobe; (1) slender shaft. Character 11 of Ortega Hernández et al. Coded unknown for Burgessia, Cheloniellon, and Squamacula (see discussions in previous character). Tegopelte is coded as state 0. The proximal lobe of the exopods in Sidneyia is also a flattened lobe (state 0).
16. Distal lobe of exopod: (0) small to moderate sized flap; (1) large, teardrop shaped lobe with long attachment; (2) dominant part of appendage, shielding endopod. Modified from character 12 of Ortega Hernández et al. Unknown for Burgessia and Cheloniellon (see previous two characters). The distal lobes of Kwanyinaspis  and Naraoia spinosa  are relative to the proximal lobe better characterised by state 1, cf. Kuamaia . Tegopelte has a moderate sized flap . State 2 has been introduced to describe the condition in Sidneyia (Stein in preparation). Squamacula is coded for that state because of the characteristic shielding of the endopod.
17. Joints in flap-like exopod (0) absent; (1) one; (2) two. Modified from character 13 of Ortega Hernández et al. The term joint is used rather than septum. The character is coded as unknown for Burgessia and Cheloniellon (see characters 14–16). Character state 2 has been introduced for the state in Emeraldella  and Sidneyia (Stein in preparation). The distal lobe in the exopod of Kwanyinaspis is clearly set off by a joint, extending from the basipod/exopod joint at a slight angle to the lateral margin where the lamellar insertion ends and the distal lobe starts (figure 2D in ). The character is coded unknown for Martinssonia, where there could be a single joint (figure 10A in ), but evidence is inconclusive.
18. Imbricate exopod lamellae: (0) absent; (1) present. Character 14 of Ortega Hernández et al. Coded unknown for Burgessia and Cheloniellon (see characters 14–17). The character is also unknown for Liwia, of which no postantennular appendages are preserved, and Sinoburius, for which exopod preservation is poor (figure 77A in ). If Squamacula had a short proximal lobe like Sidneyia, lamellae could be present but not preserved, so the character has been coded as unknown for that taxon as well. Lamellae are present in Tegopelte  and Marrella . It is unclear if the filamentous setae of Mimetaster are lamellae .
19. Non-overlapping marginal setae: (0) absent; (1) small setae; (2) long spines. Modified from character 16 of Ortega Hernández et al. Coded as unknown for Burgessia (see characters 14–18) and for Kuamaia and Saperion where setae may be absent due to preservation of the few specimens that preserve the distal lobe [12, 26]. The character is coded unknown for Haikoucaris, where preservation of the exopods does not allow assessment of whether the preserved structures are lamellae or setae. Unknown also for Retifacies (see character 14) and Mimetaster (see character 18). Pycnogonida do not have exopods, so the character has been coded as inapplicable rather than absent. The large distal lobe of Sidneyia is fringed by very fine setae (picture) and small setae are also found on the pleopods of Nebalia and posterior exopods of Rehbachiella. Martinssonia has long (relative to the body size) spines. Ortega Hernández et al. coded the character as inapplicable for Martinssonia, Rehbachiella, and Nebalia because of their exopod shape, but in all three taxa, the more posterior appendage have paddle shaped (oval) exopods (see character 14) and are here coded. The ‘teeth’ in Weinbergina  are here interpreted as setae.
20. Insertion of exopod on trunk appendages: (0) along lateral edge of multiple podomeres of limb axis; (1) on basipod and first endopod podomere; (2) on basipod only. Character 30 of Stein and Selden.
21. Setae of anterior exopods facing endopods: (0) absent; (1) present. New character. This is present in Oelandocaris, Henningsmoenicaris, Martinssonia, and Rehbachiella, where exopod setation is mainly on the median side of the anterior cephalic exopods.
22. Body–limb joint: (0) short, sclerotized, pivot-jointed rings; (1) arthrodial membrane with partially sclerotized half-rings; (2) arthrodial membrane. Character 23 of Stein and Selden.
23. Endites on basipod/gnathobase: (0) absent; (1) multiple spinose endites; (2) single spinose endite. Modified from character 24 of Stein and Selden. Here coded as unknown for Saperion, as the proximal portions of the appendages of that taxon are not well known.
24. Composition of endopod: (0) nine or eight podomeres; (1) seven podomeres; (2) fewer than seven podomeres. Modified from character 25 of Stein and Selden. According to  the endopod of Leanchoilia superlata consists of only 7 podomeres, but an isolated limb figured by D. L. Bruton and H. B. Whittington in their figure 105 clearly shows 9 .
25. Median armature of podomeres: (0) none; (1) mediodistal spines or spinules/denticles on all but penultimate and distal podomeres; (2) biserial spines or spinose endites along median edge of podomeres 1–4. Character 27 of Stein and Selden.
26. Proximal endite or coxa as separate sclerotized element proximal to limb base in cephalic appendages (0) absent; (1) present. New character, derived from the analysis of J. T. Haug, A. Maas, and D. Waloszek (there coded individually for appendages and ontogenetic stages, characters 6, 7, 13, 14, 20, 21) . Here, only the appearance of a proximal endite on any limb is coded.
27. Position of lateral eyes: (0) ventral; (1) dorsal. Modified from character 18 of Ortega Hernández et al., coded as state 0 where eyes are not dorsal, even if they are not preserved. An exception is Weinbergina, where eyes are not preserved, but ophthalmic ridges indicate a dorsal position. For Pycnogonida and Martinssonia, where there is positive evidence for the absence of lateral eyes (the eyes of pycnogonids are interpreted as median eyes ), this is coded as inapplicable. The putative dorsal eyes of Cheloniellon  could be the large, dorsoventrally extending gnathobases of the anterior trunk appendages superimposed on the head shield in the radiographs. The character is coded here as unknown for that taxon. It is coded unknown for Liwia, where the dorsal cuticle of the cephalon is not preserved  and Marrella, where position and preservation of the eyes is unclear. By comparison with the position and structure of the eyes in Henningsmoenicaris [60, 75] the eyes of Oelandocaris are interpreted as lateral eyes and are ventral.
28. Visual surface with calcified lenses, bounded with circumocular suture: (0) absent; (1) present. Character 21 of Ortega Hernández et al.
29. Dorsal bulge in exoskeleton accommodating drop-shaped ventral eyes: (0) absent; (1) present. Character 22 of Ortega Hernández et al. The eyes of helmetiids and Kwanyinaspis appear to be in sharply defined bulges (e.g. figure 5 in ), which does not seem to be the case in Sinoburius where the bulges are confluent with the shield (figure 77B–D in ) and could be compactional artefacts. The character is coded as unknown for that taxon.
30. Eye slits: (0) absent; (1) present. Character 23 of Ortega Hernández et al. This is often interpreted as present in Sinoburius , but the evidence is inconclusive and the character is here coded as unknown for that taxon.
31. Dorsal median eyes: (0) absent; (1) present. Character 24 of Ortega Hernández et al.
32. Bilobate lateral eyes where four visual surfaces are arranged in a subtransverse band across head shield: (0) absent; (1) present. Modified from character 9 of Edgecombe et al., taking a recent reinterpretation of the eyes of Leanchoilia superlata into account .
33. Expanded cephalic doublure: (0) absent; (1) concentric; (2) crescentic. Modified from character 27 of Ortega Hernández et al. State 2 occurs in Soomaspis and Tarricoia. Contrary to the coding of Ortega Hernández et al., the cephalic doublure is unknown for Burgessia, Haikoucaris, Retifacies, and Tegopelte. An expanded doublure is absent in Cheloniellon where doublure covers less than 10% of the total width of the head (figure 12C in ), likewise in Cindarella (figure 5g in ), Xandarella (figure 68C, 70 in ), Emeraldella  Misszhouia , Naraoia compacta (pl. 10:9 in ) and N. spinosa , and Sinoburius (figure 1 in ). If the interpretation of the elevated structure anteromedially in the cephalon of Kwanyinaspis as the hypostome (figure 1b in ) is correct, the taxon can not have an expanded doublure, since the structure extends all the way to the very margin. Accordingly, the character is coded as state 0 for this taxon. The character is also coded as unknown for Squamacula where often a doublure covering the whole ventral side of the cephalon is inferred, as in Sidneyia. In Sidneyia, this is an artefact of folding under of the anterior margin of the cephalon (Stein in preparation).
34. Anteromedian margin of cephalon notched, accommodating strongly sclerotised plate: (0) absent; (1) present. Character 28 of Ortega Hernández et al.
35. Hypostomal sclerite: (0) wide attachment with or without suture; (1) natant; (2) with narrow overlap with prehypostomal sclerite; (3) absent. Modified from character 29 of Ortega Hernández et al.; their states 0 and 3 have been merged. The character is coded unknown for Australimicola (contra ) where the mode of attachment can not be confirmed in the available photographs. It is also coded unknown for Burgessia where the presence and state of the hypostome are entirely unclear. The same is true for Fortiforceps, Haikoucaris, Jianfengia, Yohoia, Sinoburius, and Tegopelte. There is sclerotized cuticle covering the backward curved mouth in Alalcomenaeus (e.g. pl. 6:5, 3 and text-figures 10–11 in ) which represents the hypostome, and the attachment has to be natant because of the eyes between the hypostome and the anterior margin of the cephalon. The same is true for Leanchoilia [24, 80]. The hypostome of Martinssonia is incorporated into the ‘forehead’ and its delimitation from the remainder of that and relation with the head shield margin is unclear, and the character is coded as unknown for Martinssonia. In Nebalia and Rehbachiella the hypostome is subsumed by the labrum, but the whole hypostome-labrum complex is natant.
36. Hypostome divided into anterior and posterior parts by transverse suture: (0) absent; (1) present. Character 13 of Paterson et al. [32, 81]. This is coded as unknown for Marrella where the hypostome morphology is unclear.
37. Labrum: (0) absent; (1) present. Character 1 of Haug et al. .
38. Prehypostomal sclerite: (0) as individual sclerite anterior to head tergite or recessed in notch in head shield; (1) incorporated in doublure as rostral plate or reduced. Character 5 of Stein and Selden, substituted for character 30 of Ortega Hernández et al. Coded as unknown for Yohoia .
39. Frontal organs on prehypostomal sclerite: (0) absent; (1) present. Character 11 of [32, 81]. It is questionable whether the spots observed on the prehypostomal sclerite in Helmetia  are homologous to the bulges in nektaspids as they differ in preservation, which is more like that of internal structures preserved more posteriorly in USNM 83952. The character is here coded as absent for Helmetia.
40. Visible ecdysial dorsal sutures: (0) absent; (1) present. Character 31 of Ortega Hernández et al.
41. Position of ecdysial sutures: (0) marginal; (1) dorsal. Character 32 of Ortega Hernández et al.
42. Elevated marginal rim: (0) absent; (1) present. Character 33 Ortega Hernández et al. There is no elevated marginal rim in Kwanyinaspis, contrary to the coding of Ortega Hernández et al.
43. Distinct trilobation of head shield, marked by axial furrows: (0) absent; (1) present. Character 6 of Stein and Selden. This is unclear for Siriocaris and coded unknown for the taxon.
44. Dorsal expression of last segment of head shield: (0) absent; (1) present. Character 7 of Stein and Selden.
45. Head shield outline: (0) genal angles, rounded, acute or with spines; (1) lateral spine-like extensions of the head shield; (2) lateral margin extending into genal spines flanking anterior trunk. Modified from character 36 of Ortega Hernández et al. Their states 0, 1 and 2 have been collapsed into a single state. State 2 is new and occurs in aglaspidids, trilobites, and Sinoburius. The character has been coded as state 0 for Saperion and Skioldia, where the posterolateral corners of the cephalon are visible and their morphology can be described, even if it is debated whether the articulation between cephalon and trunk tergites is functional.
46. Mineralized cuticle: (0) absent; (1) calcitic; (2) phosphatic. Modified from character 40 of Ortega Hernández et al. (see also Paterson et al. ).
47. Trunk tergites with expanded tergopleurae covering appendages dorsally: (0) absent; (1) present. Character 41 of Ortega Hernández et al. (cf pars character 10 of Stein and Selden). Coded inapplicable for Pycnogonida which does not have a trunk.
48. Free thoracic tergites: (0) absent; (1) present. Character 42 of Ortega Hernández et al. Coded inapplicable for Pycnogonida which does not have a trunk.
49. Decoupling of thoracic tergites and segments: (0) absent; (1) present. Character 43 of Ortega Hernández et al. Coded inapplicable for Pycnogonida which does not have a trunk.
50. Tergite articulations: (0) tergites non-overlapping, edges separated by arthrodial membrane; (1) extensive overlap of tergites; (2) edge-to-edge pleural articulations. Character 44 of Ortega Hernández et al. Coded unknown for Burgessia, where little of the tergites is known, and Sinoburius, where preservation of the minute specimens is too coarse to discern tergite articulations. Articulations are equally unknown for Marrella and Mimetaster. Australimicola has been coded as having overlapping tergites rather than edge to edge articulations as coded in the analysis included with the original description . The overlap is shown in figures 10 and 12 of Paterson et al.  and even labeled as such in their interpretative line drawing (figure 9 in ) and overlap is given as up to one half the tergal length in the description . Kangacaris on the other hand seems to have edge to edge articulations (plate 5 of ) while articulations are unclear for Emucaris. Soomaspis, too, has edge to edge articulating tergopleurae (pl. 1:3 in ). The character is coded for Skioldia, where articulations are clearly visible and are edge to edge (figure 16.54 in ). Coded inapplicable for Pycnogonida which does not have a trunk.
51. Cephalic articulation fused: (0) absent; (1) present. Character 46 of Ortega Hernández et al. The authors stated that this was present in Skioldia  but coded it as absent, which is probably correct. Coded inapplicable for Pycnogonida which does not have a trunk.
52. Head shield overlap of thoracic tergites: (0) overlap absent or identical to overlap between thoracic segments; (1) head shield covers first thoracic tergite only; (2) head shield covers multiple anterior trunk tergites. Character 47 of Ortega Hernández et al. This character is coded unknown for Marrella and Mimetaster, where the posterior boundary of the head shield is unclear. Overlap in Martinssonia is clearly identical to the trunk tergites ; there is no overlap of multiple segments as coded by Ortega Hernández et al.. The same is the case in Sinoburius. Despite the possibly non-functional articulations, overlap between the head shield and the first tergite is identical to that between subsequent tergites in Saperion and Skioldia and can be coded. Coded inapplicable for Pycnogonida which does not have a trunk.
53. Trunk narrowed anteriorly relative to head shield, widest posteriorly: (0) absent; (1) present. Character 49 of Ortega Hernández et al. Coded inapplicable for Pycnogonida which does not have a trunk.
54. Raised axial region of trunk defined by axial furrows: (0) absent; (1) present. Modified from character 54 of Ortega Hernández et al. (cf pars character 10 of Stein and Selden). The character has been coded absent for Kuamaia, where the axis in the fossils is defined by compactional folds as in Arthroaspis. The axis of Weinbergina is defined by nodes rather than furrows as is best seen in the non-lateral compressed specimens (figure 6a in ). Coded inapplicable for Pycnogonida which does not have a trunk.
55. Articulating device: (0) articulating half-ring and flanges; (1) articulating ridge/anterior process; (2) no skeletal device. Modified from character 55 of Ortega Hernández et al. (anterior tergal process absent/present). Coded unknown for Alalcomenaeus, Burgessia, Cindarella, Fortiforceps, Haikoucaris, Jianfengia, Marrella, Mimetaster, Sinoburius, Squamacula, Tariccoia, Xandarella, and Yohoia. Articulating ridges are present in Cheloniellon (figure 12a in ), Leanchoilia , Retifacies , Sidneyia (pl. 5:37 in ), Eurypterida, and Weinbergina (figure 4c in ). The articulating half-ring (state 0) is visible in the holotype of Liwia convexa (figure 4D in ) and is also present in Soomaspis (text-figure 1b–c in ). No skeletal articulation devices are present in Martinssonia, Rehbachiella, Nebalia, and the pycnogonids. The character is coded inapplicable for taxa without free tergites (Misszhouia and Naraoia) or where the tergites are fully effaced (Tegopelte). Coded inapplicable for Pycnogonida which does not have a trunk with articulating tergites.
56. Postcephalic tagmosis: (0) uniform trunk with free tergites and telson or pygidium; (1) bipartite trunk with free tergites and telson, segments in abdomen apodous, tergites ring-shaped, without tergopleurae. Modified from character 2 of Stein and Selden. The pygidium is here defined as a uniform shield formed by the ankylosed posterior tergites, and not considered a true tagma . Aglaspidids as Emeraldella are not considered to have an abdomen. Tergopleurae are present, though posterior limbs are never known. This is unclear for Cheloniellon where the tergites of the posterior most segments appear to lack tergopleurae, but seem to be appendage bearing. The posterior end of Flobertia is poorly known and the character is coded as unknown also for that taxon. Coded inapplicable for Pycnogonida which does not have a trunk.
57. Trunk segments form single shield: (0) absent; (1) present. Character 3 of Stein and Selden. Coded inapplicable for Pycnogonida which does not have a trunk.
58. Posterior tergites strongly curved in dorsal aspect compared to anterior tergites: (0) absent; (1) present. Modified from character 61 of Ortega Hernández et al. Here coded inapplicable where posterior segments are incorporated into a large pygidium or no tergopleurae are present. This is further coded absent for all taxa where only the tergopleural extremity curves. Unknown for Burgessia, Marrella, and Mimetaster where little is known of tergite morphology. Coded inapplicable for Pycnogonida which does not have a trunk.
59. Pygidium: (0) absent; (1) present. Character 62 of Ortega Hernández et al. Coded as unknown for Cindarella, Henningsmoenicaris, Squamacula, and Xandarella. Evidence for a pygidium in Squamacula and Australimicola is inconclusive. In Cindarella and Xandarella a number of tergites cover an increasing number of appendiferous segments posteriorly. This seems incompatible with recent interpretations of the pygidium as a frozen growth zone . Further, a recently described xandarellid, Luohuilinella rarus Zhang, Fu & Dai, 2012, appears to be lacking a pygidium or elongate posterior tergites . The absence of a pygidium in a member of Xandarellida casts further doubt on the nature of the other xandarellids’ elongate tergites as a true pygidium. Henningsmoenicaris scutula has been described as having a developmental mode where segments are released from a growth zone, but until release aggregate in that growth zone . This is technically a pygidium, but since the known stages of Henningsmoenicaris are immature and it is unclear if a pygidium is retained in the adult, the character is scored as unknown. Coded inapplicable for Pycnogonida which does not have a trunk.
60. Position of the anus: (0) terminal; (1) ventral. Character 63 of Ortega Hernández et al. Coded unknown for Australimicola, Marrella, and Mimetaster. The position of the anus is not preserved in Aglaspis, but because the styliform telson is closed posteriorly, it is likely to have been at the base of the telson. The same in Kwanyinaspis. The character is coded inapplicable for pycnogonids, where the telson is reduced.
61. Pygidium with median keel: (0) absent; (1) present. Character 64 of Ortega Hernández et al. Coded unknown for all taxa where the presence of a pygidium is unclear.
62. Pygidium with broad-based median spine: (0) absent; (1) present. Character 65 of Ortega Hernández et al. Coded unknown for all taxa where the presence of a pygidium is unclear.
63. Pygidium with lateral spines: (0) absent; (1) present. Character 66 of Ortega Hernández et al. Coded unknown for all taxa where the presence of a pygidium is unclear. This is here coded only where the spines are segmental, i.e. remnants of the teopleural tips of the ankylosed tergites. Defined as such, they are absent in Retifacies, but present in Soomaspis and Tariccoia.
64. Size of caudal end: (0) shorter to slightly longer than cephalon; (1) much longer than cephalon. Modified from character 23 of Paterson et al. [32, 81]. The term caudal end applies to both pygidium and the axial portion of the telson. Coded even for taxa where the presence of a pygidium is unclear. Coded present for the naraoiids, where the whole trunk is considered subsumed by the pygidium which is longer than the cephalon, but absent in Saperion and Skioldia, where the pygidium is visible despite possibly non-functional articulations, and not much longer than the cephalon. Coded present in Liwia, Soomaspis, and Tariccoia.
65. Free telson: (0) present; (1) absent. Modified form character 67 of Ortega Hernández et al. Coded unknown for Australimicola where the nature of the caudal region is unclear.
66. Telson shape: (0) styliform keeled; (1) plate-like; (2) tubular cap-like to tubular styliform. Modified from character 68 of Ortega Hernández et al. The states have been modified. The telson of Weinbergina and Eurypterida is a stylus with a triangilar cross section (keeled), whereas those of Aglaspis and Kwanyinaspis have more of an extended tubular shape, as also seen, albeit shorter, in Oelandocaris and Henningsmoenicaris. The telson is seen in the latter two taxa, even though during ontogeny it may be part of a pygidium. Coded unknown for Australimicola and other taxa for which the nature of the caudal portion is unclear. Also, the telson shape of Jianfengia is unknown, while the character is coded inapplicable for Pycnogonida where the telson is reduced. The megacheirans Fortiforceps, Haikoucaris, Leanchoilia, and Yohoia have all been coded as ‘spinose’ (styliform) by Ortega Hernández et al., but their morphology is better described as plate-like.
67. Telson carrying furca: (0) absent; (1) present. Newly added character. Coded inapplicable for taxa with a pygidium, unknown for taxa where the nature of the caudal end is unclear.
68. Spines on telson: (0) absent; (1) present. Character 71 of Ortega Hernández et al. Coded unknown where the nature of the caudal end is unknown. Furthermore unknown in the megacheirans Fortiforceps and Jianfengia. Inapplicable for Pycnogonida where the telson is reduced. The telson of Yohoia carries spines distally .
70. Postventral plates: (0) absent; (1) present. Character 74 of Ortega Hernández et al.
71. Paired modified appendages attached to a differentiated pre-telsonic segment: (0) absent; (1) present. Character 75 of Ortega Hernández et al. Filiform caudal cerci are present in Olenoides , even though they were coded as absent by Ortega Hernández et al.
72. Nature of pre-terminal appendages: (0) paddle; (1) cerci. Modified from Ortega Hernández et al. character 76; more neutral descriptive terms are adopted here. Olenoides has state 1 .
73. Relative length of thorax: (0) shorter than caudal end; (1) longer than caudal end. Modified from character 79 of Ortega Hernández et al.
74. Differentiation of cephalic gut diverticulae: (0) small, serially regular diverticulae; (1) anterior pair of diverticulae large, expanding across genal region of cephalic shield, with complicated ramification. Character 37 of Paterson et al. [32, 81]. This is coded absent for Burgessia where it is not the anterior pair that is differentiated.
Arthro from arthron―articulation or joint, aspis―shield.
Arthroaspis bergstroemi, by monotypy.
Large ‘artiopodan’ attaining maximum length of up to 215 mm with helmetiid-like tergum of edge-to-edge articulating tergites and pygidium with segmental marginal spines. Distinguished from Helmetiida by semi-elliptical cephalon with integral margin lacking recess accommodating prehypostomal sclerite. Cephalon broadly nektaspid-like with preglabellear sagittal crease and natant complex of hypostome and arcuate prehypostomal sclerite. Differentiated from Nektaspida by raised glabella laterally marked by axial furrows and dorsally demarcated occipital segment with occipital ring; trunk differentiated dorsally into thorax of 14 tergites, and pygidium.
Arthroaspis n.g. matches the revised diagnosis for Artiopoda , but the present analysis does not find support for a monophyletic Artiopoda.
Arthroaspis bergstroemi n.sp.
1987 arthropod―S. Conway Morris, J. S. Peel, A. K. Higgins, N. J. Soper & N. C. Davis, p. 182, figure 2g (MGUH 17516) ; non figure 2a (MGUH 17512), the specimen figured here is Campanamuta, see synonymy list in .
1996 animal reported as a tegopeltid―L. Ramsköld, J-y. Chen, G. D. Edgecombe, and G-q. Zhou, p. 15 .
2007 undescribed arthropod―L. E. Babcock and J. S. Peel, figure 3E (MGUH 28755) .
2009 Outer limb branch of an undescribed Sirius Passet (Lower Cambrian of Greenland) lamellipedian arthropod―G. E. Budd and M. J. Telford, p. 815, figure 3f .
2010 undescribed arthropod―J. S. Peel, p. 386, figure 2 (MGUH 28755) .
2011 Campanamuta―G. E. Budd, p. 222 in synonymy list .
2011 arthropod—J. S. Peel & J. R. Ineson a figure 4I .
2012 “undetermined nonbiomineralized - Tegopelte-like arthropods.”—M. G. Mangano, R. G. Bromley, D. A. T. Harper, A. T. Nielsen, M. P. Smith, and J. Vinther, p. 520, figure 1 and in text .
In memory of the late Jan Bergström in the 40th year since his publication of Organization, life, and systematics of trilobites.
MGUH 30382, part and counterpart.
Type locality and horizon
Arthroaspis bergstroemi is one of the most common elements within the Sirius Passet Lagerstätte occurring in various lithologies both within the main Sirius Passet locality and at localities 2 and 3 described by J. S. Peel and J. R. Ineson . Cambrian, Series 2, Montezuman Stage.
As for genus.
Arthroaspis bergstroemi is one of the largest organisms in the Sirius Passet Lagerstätte; the largest specimens are over 210 mm in length. In outline it is subrectangular, with distinctly delimited cephalic, thoracic and pygidial regions. The cephalon of A. bergstroemi is a large, semi-elliptical shield that lacks genal spines and bears a glabella (Figures 1A, 2A, 3A). The hypostome is rounded and rectangular to oval in outline, longer than wide (Figures 2E, 3A, 4, 5). Its total length is about one third of total cephalic length; the total width is one fifth of the total cephalic width. Its maximum width is in the anterior quarter at the forward-projecting anterior wings (Figure 5A). Its lateral margins curve outward posteriorly to form posterior wings (Figures 2E; 4C); the antennular insertion (see below) is at a notch between the anterior and posterior wings, recessed under the median body (Figure 5B). Anteriorly, the hypostome is bounded at a transverse suture by an arcuate prehypostomal sclerite with an anteriorly diverging, raised central region (Figures 2B; 5A). The prehypostomal sclerite is well-separated from the cephalic margin and doublure (Figures 2A, B; 3A); together, the hypostome/prehypostomal sclerite complex is natant (Figures 2E; 3A; 4; 5A). Some specimens show a preglabellar sagittal crease directly in front of the hypostome in the dorsal cephalic shield (Figures 1B; 2A, E). The final segment of the cephalon is somewhat differentiated (Figures 2A, B, E; 3A), especially in the axial region where the glabella is marked by a furrow bearing a poorly-developed occipital node (Figures 2E; 3A). The occipital furrow continues laterally into the cephalon away from the glabella, but dies out at the margin. The margin of the cephalon is delimited by a very narrow but distinct border, less than 2% of the length of the cephalon (Figure 2B–D). There is a narrow doublure that bears terrace lines (Figure 2C).
The thorax consists of 14 trilobate tergites with clearly defined transverse tergal boundaries (Figures 1; 2A). The narrow axis occupies about one fifth of the total width (Figures 1, 2A, 3A, D), laterally demarcated by a weak axial furrow. The axial rings carry broad based axial nodes in their posterior third (Figure 3A) and a crescentic doublure with reticulate cuticular sculpture ventrally, which covers the posterior third of the total length (Figure 3A). The main articulation device is a short (sag, less than one fourth of the tergal length) crescentic articulating half ring (Figure 3A, D). The half ring is not set off by an articulating furrow, but is, rather, laterally confluent with a very short (sag.) flange along the anterior margin of the tergopleura (Figure 3D). The tergopleurae articulate edge to edge (Figures 1A, B, 2A). The outer tergopleura is more distinctively sloping than the inner (Figure 3D), but is defined by a gradual change in slope at about one third the tergopleural width from the axis, rather than possessing a well-developed fulcral line. The tergites bend around laterally at the shelf-like margin to form a narrow doublure (<2% Figure 3D). The ventral side is covered by an inner lamella (Figure 3B). The lateral extremities of tergites bear minute pleural tips that increase in relative length in posterior segments (Figure 6A).
The pygidium takes up slightly more than one third of the total length of the trunk (Figure 1A). The Anteriormost incorporated segment (trunk segment 15) shows traces of a segment boundary, mostly adaxially: the expression of the boundary is weaker, however, than the fully-expressed boundaries of the free trunk segments (Figure 6A). The margin of the pygidium bears well-developed spines, corresponding in morphology and spacing to the tergopleural tips of the trunk tergites and are interpreted as segmental. The spines indicate the presence of altogether 11 segments in the pygidium (Figures 1A; 6A, B). Three axial rings are developed in the pygidial axis (Figure 6A, B). The postaxial portion of the pygidium is a plate-like inversely teardrop shaped strip, laterally delimited by the 11th marginal spine pair (Figure 1A).
All postantennular segments, including the first cephalic one, carry sternites ventrally (Figure 6A). The sternites are hourglass shaped with a narrow convex rim laterally, bounding a weak central depression with an axial ridge. The anterior and posterior margins are straight, and the posterior margin slightly narrower than the anterior (Figure 7A). The sternites decrease moderately in width, more strongly in length towards the posterior of the animal (Figure 7A). Sternites in the trunk directly underly the tergal boundaries (Figures 5A, 7B).
The antennula is filiform (Figures 5B; 8), consisting of a single branch of well in excess of 20 articles (Figure 8A). The proximal portion is stout, reaching one third of the width of the hypostome (Figure 5B). Articles are short (two times wider than long) proximally, and increase in relative length distal to the cephalic margin (longer than wide; Figures 5B; 8). The articles are tubular, with a slight mediodistal extension carrying biserially arranged spines (Figure 8).
Three appendage-bearing postantennular segments are incorporated into the cephalic region (Figure 9A). The cephalic appendages increase in size posteriorly. The insertions of the anterior cephalic limbs are rotated around the posterior margin of the hypostome (Figure 5B), and the third postantennular limb inserts transversely, as do the trunk appendages (Figure 10A).
The body–limb joint of the trunk appendages consists of extensive arthrodial membrane with three to four weakly sclerotized half-rings (Figure 10B2). The basipod carries the proximal portion of the exopod laterally, and the endopod distally to laterodistally. The median edge of the basipod is drawn out into a single endite (Figures 6C; 7B1; 11B) armed with biserial spines (Figure 10A). The endopod has seven podomeres (Figures 11A, E–F); en7 forms a distal claw (Figures 10A3, 11E). en1 articulates with the proximal portion of the exopod laterally, and is drawn out into a spinose endite medially (Figure 11B). The median edges of en2–4 are drawn out into spinose endites (Figure 11D). The mediodistal extremities of the podomeres carry mediodistal spines (Figure 11D). Laterodistal spines or other armature at the distal margins of podomeres such as denticles are absent (Figure 11D). The length of the endopods roughly corresponds to or slightly exceeds the width of the tergopleurae in the anterior trunk (Figures 1A; 2A; 9A; 11F) and decreases rapidly in the posterior third (Figure 1A).
The lateroproximal extremity of the exopod slightly extends beyond the proximal margin of the basipod (Figure 11B). The exopods are bilobate flaps consisting of two articles (Figure 6C); the proximal is elongate, carries more than 35 lamellae on an arched lateral edge (Figures 3C; 6C; 9C; 11B), and inserts in the lateral edge of the basipod and en1 (Figure 11A–C). The length of the lamellae corresponds to the maximum length of the distal article (Figure 6C). The distal article is teardrop-shaped to oval and fringed with minute marginal setae (Figures 3E; 6C; 10A2; 11D; 12); it articulates with the proximal portion of the exopod, articulation with the endopod is unclear. The marginal setae are roughly the length of the width of the lamellae.
Apart from impressions of appendages (Figure 9A), evidence for the presence of four post-ocular segments in the head is derived from the cephalic midgut diverticula. There are four pairs of diverticula, the most anterior one being differentiated (Figures 1A, 3C, 9B). Differentiation of the most anterior diverticula pair is known from e.g. Nektaspida [69, 91] and Emeraldella brocki. In Arthroaspis bergstroemi n. sp., the most anterior pair of diverticula is reduced, as in Misszhouia longicaudata. The most posterior diverticula pair is in the occipital ring (Figures 1A; 9B), providing evidence that this portion of the glabella and the adjacent strip of tergopleural region set off by a sharp furrow are the dorsal expression of the last segment incorporated into the head, here called the occipital segment. A similar dorsal expression of the last cephalic segment is present in many trilobites that have an occipital ring axially and posterior cephalic border and border furrow abaxially . Alternatively, the posterior border and border furrow might represent the pleural furrow and thereby an intra- rather than intersegment boundary.
The axis of cephalon and trunk tergites must have been differentiated from the tergopleural areas by a change in convexity, as indicated by folds along the axial margin (Figure 2A). These folds often overprint the axial furrow. A similar compactional effect is observed in Sinoburius lunaris, where the specimen figured by L-h. Luo, S-x. Hu, S-s. Zhang, Y-h. Tao in their plate 2 figure 4  displays a clear axial furrow, while it is entirely obscured in specimens figured by X-g. Hou and J. Bergström in their figure 77 .
At about one third of the tergopleural width from the axis, there is a curvature of the tergopleurae, indicating a change in slope. There is, however, no clearly defined fulcral line as observed in Siriocaris trollae or in most trilobites, and the inner tergopleura of Arthroaspis does not appear to have been horizontal as in those taxa.
Thoracic tergite articulations are functional in the sense that they contain arthrodial regions separating individual tergites. Tergites are not ankylosed to a single, sclerotized shield. This is evident in the common occurrence of disarticulated material. Frequently disarticulation happens at the cephalon-trunk boundary (Figure 2E) between the thorax and pygidium (Figure 2A) but even thoracic tergites show partial (Figure 3C) or full disarticulation (Figure 3A, D). Often, adjacent tergopleurae are tilted relative to each other, but remain connected, indicating a membranous connection between the individual tergopleurae (Figure 3B) all the way to the lateral extremities. While the tergites thus were clearly separate, it is questionable if the tergite articulations allowed for much, if any, axial flexing of the trunk. Considering the convexity and division in inner and more sloping outer tergopleurae, ventral flexing would only be possible if the outer tergopleurae were imbricating and overlap could have increased during flexing. But since the outer tergopleural margins abut entirely edge to edge, with no signs of overlap in any of the specimens, ventral flexing, for example enrolment, was unlikely. If the inferred presence of a membraneous connection to the lateral extremities is correct, even dorsal flexing, leading to splay of the outer tergopleurae, would have been impossible. Lateral flexing must have been equally impossible. In conclusion, except when moulting, the whole tergum must have functioned more or less as a single shield, as has been inferred for Skioldia aldna and Saperion glumaceum and the anterior part of the tergum of Kuamaia lata and Helmetia sparsa[26, 88]. In particular for the latter taxa, much weight in the interpretation of non-functional (as in non-rotating) tergite articulations has been laid on the presence of anterolaterally reflexed margins of the anterior tergites. Such anterior flexure does occur in specimens of Arthroaspis where cephalon and the larger part of the trunk are articulated (Figures 1A; 2A), but not where only a few tergites are articulated with the cephalon (Figure 3A). We suggest that the anterior flexure is a compactional artefact, owed to distortion of tergite boundaries upon compaction of the semi-elliptoid geometry of the tergum into an elliptical geometry. This has likely also happened in Kuamaia, Skioldia, and Saperion of which disarticulated material is unknown. The absence of disarticulated specimens in these taxa could be because of a genuine absence of functional articulations or merely the paucity of specimens; in Arthroaspis, the majority of material is articulated, and given the abundance of the species, the absence of disarticulated specimens in the other taxa could be a statistical effect. Even in the articulated specimens of Kuamaia, Skioldia, and Saperion, the anterolateral flexure varies from moderate to absent (e.g. figs 57, 63, 64A, 66 of Hou and Bergström  or figure 5:1, 2 of Edgecombe & Ramsköld ). We would therefore discourage the use anterolateral flexure of the anterior tergites’ margins as a helmetiid autapomorphy as frequently suggested [19, 22, 26, 32, 81].
Laterally, the tergal margins in Arthroaspis can appear effaced (Figures 1A; 2A; 3B) while they appear well-defined adaxially. The presence of disarticulating tergites (Figure 3C, D) demonstrates this effacement to be a preservational artefact. The same kind of effacement is present in Skioldia, and based on evidence from Arthroaspis, it is suggested that the effacement in Skioldia is preservational, too. As in Arthroaspis, even in Skioldia, the lateral extremities of the tergopleurae form minute but free tips (fig. 16:54 of Hou et al. ).
The hypostome is often preserved by its outline where the glabella collapsed into the hypostomal cavity below. It appears in negative relief in dorsal aspect specimens (Figure 5A), positive relief on ventral aspect specimens (Figures 2E; 3A; 4; 5B). Impressions of the hypostome occur in both articulated specimens and disarticulated cephalic shields. The hypostomal complex can occur displaced relative to the anterior margin of the glabella. The anterior wings of the hypostome project forward and often cause box-like wrinkling of the cephalic shield above the anterolateral corners of the hypostome (Figure 4). The hypostome and prehypostomal sclerite, where preserved, are always in immediate juxtaposition. They were likely fused or separated by a non-functional suture.
The preglabellar sagittal crease is not observed in all specimens and could be a compactional artefact as suggested elsewhere for other taxa [49, 94]. It does seem to follow a morphological structure; it is possible that it is caused by a possible median node on the prehypostomal sclerite (Figure 5B, C) as is present in nekatspids . There are also faint elevations on the prehypostomal sclerite lateral to the preglabellar sagittal crease (Figure 5C), which could be homologous to the paired “frontal organs” of nektaspids .
The position of the mouth is unknown; the most posterior position would be at the posterior margin of the hypostome. Since the hypostome is followed by the sternite of the first postantennular appendage immediately (Figure 5A), the position of the mouth is unlikely to have been further posterior than that. The hypostome is relatively short and judging from the antennular insertion (Figure 5B) it seems unlikely that the mouth is recessed far anteriorly under the hypostome.
An exact count of antennular articles is not possible because the antennule is never complete and articles are poorly preserved distally. Some 22 articles have been counted (Figure 8A), but that count does not start at the insertion, so proximal articles could not be counted. Joints become indistinct distally, and cannot be counted either, so it is assumed that the total count of antennular articles is well in excess of the countable number.
The overall preservation does not allow detailed description of the structure of the postantennular cephalic limbs, but there is evidence for lamella-bearing exopods at least in the second and third postantennular appendages (Figures 5A; 9B). The relative proportions of endopods (as seen from impressions) and exopods and the orientation of the exopod lamellae are as in the trunk appendages (Figure 9C). All trunk appendages appear to be inserted transversely (Figure 10A). If the position of the mouth corresponded with the posterior margin of the hypostome, insertion of the first postantennular appendage must have been paraoral but hardly preoral (Figure 5B).
A generalised reconstruction of the trunk appendages is given in Figure 13. The appendages appear to change in stance from laterally splayed in the anterior trunk to pendant in the posterior in some specimens (Figure 1A). An isolated appendage (Figure 11C) shows outward curvature of the basipod, as evidenced by the basipod endite that appears rotated relative to the limb axis. Remnants of the margin of the body limb joint indicate the joint to be dorsal to the endopods, but dorsolateral to the basipod-exopod body. It seems that this change in stance is accomplished through change in basipod morphology rather than outward curvature of the proximal endopod podomeres as in Emeraldella brocki. In other specimens (Figure 10) even the posterior limbs appear splayed, which might indicate postmortem effects. In either case, judging from what is visible from the proximal portions of the appendages (Figure 10) it seems most likely that further rotation could occur around the extensive membrane of the body–limb joint. Cephalic appendages are consistently splayed to anteriorly extended. The pygidial appendages are not preserved except for their body–limb joints (Figure 10A). The terminal appendages are not preserved, so it is not known whether there were specialized caudal appendages as in e.g. Olenoides serratus or Emeraldella brocki.
The distal article of the exopod is often wrinkled, indicating convexity (Figure 12). However, the massive wrinkling towards the lateral edge in one three-dimensionally preserved specimen (Figure 12A) is likely to be the result from those margins being compressed onto the bedding plane. The distal article of the exopod is sometimes disarticulated (Figure 12B–C), and details of the joint with the proximal article are visible in this disarticulated material. The joint is straight on one side, and embayed on the other. The antero-posterior orientation is not known in the disarticulated material, so it is not clear which side is straight and which embayed. The embayment, which goes across the apex of the proximal corner, could be an indication that the distal article also articulated with the endopod. The distal article seems to be homologous to the two distal articles of the tripartite exopods of Emeraldella brocki. The joint with the proximal article in that taxon has the same shape as does its articulation with the endopod, and the median part has setae along its median edge. The character polarity―secondary subdivision of the distal article in Emeraldella vs loss of the second joint in Arthroaspis―is unclear. A generalised mid-trunk appendage is reconstructed in Figure 13.
The inner lamella is preserved in only a few specimens (Figures 3B; 14A), and tends to follow the internal segmental organisation of the tergum. This is even the case where the tergites are fused, as in the pygidium (Figure 14A2–3).
Tendinous bars are present as transverse intersegmental bars between the sternites, and they extend laterally beyond the lateral margins of the sternites (Figures 7; 10; 11A). Potential muscle preservation as observed in other taxa described from the Sirius Passet Lagerstätte [48, 52, 95] is observed in some specimens (e.g. Figure 2A).
The unweighted analysis yielded 2851 MPTs (strict consensus in Figure 15). Weighted analyses yielded 21 MPTs for k=1, 42 for k=2, 20 for k=3, and 21 for k=4. Analysis with k>4 yielded 63 MPTs consistently. Topology remains unchanged for k=5–k=16 (Figure 16A), and broadly mirrors that of the unweighted analysis, except for increased resolution among basal lamellipedians and a different position for Agnostus pisiformis (see below). At k ≥17, Agnostus is in the same position as in the unweighted analysis (Figure 16B). The topology remains stable with increased k values.
Unweighted and weighted analyses retrieve a basal polytomy of Isoxys, Kiisortoqia, the total group Chelicerata, and a clade of Crustacea s.l. + Lamellipedia which probably represents the total group Mandibulata. In the unweighted analysis, and at k≥17, Agnostus pisiformis is the sister taxon to Crustacea s.l., whereas it forms a clade with Phytophilaspis pergamena which is sister group to Trilobita in weighted analysis with k=4–16.
The total group Chelicerata comprises a polytomy of taxa with a short great appendage  and the crown group Chelicerata. Autapomorphies for this clade are: 2, first cephalic appendage composed of ≤7 articles (convergent with Martinssonia + Eucrustacea); 3, single, large, mediodistal finger on articles of first appendage; 6, elbow joint; 68 (optimized) spines on telson (reversal in crown group Chelicerata). A monophyletic Megacheira () is not retrieved, but there is no positive evidence for a grade of ‘megacheirans’ leading to the crown group Chelicerata, either [21, 23]. We are reluctant to follow  and apply the name Megacheira to the whole total group of Chelicerata until relationships are better resolved. Cheliceromorpha  also included Aglaspidida, which in the present analysis and that of Ortega Hernández et al.  is part of the total group Mandibulata. Possible autapomorphies for crown group Chelicerata are: 4, two fingers on short feeding appendage; 7, six postocular segments incorporated into head (prosoma); 8 and 9, exopod on first and second post-antennular appendages absent (convergent in Cheloniellon); 22, body limb-joint of arthrodial membrane only (convergent with Agnostus + Crustacea s.l.; problematic because the proximal rings in Palaeoisopus problematicus could be homologous to the partially sclerotized half-rings ); 31, dorsal median eyes; 35, hypostomal sclerite absent. Further characters that are present in Euchelicerata and have been optimized for Chelicerata: 56, apodous abdomen (possibly with Pycnogonida, see Palaeoisopus; convergent with Yohoia, Martinssonia + Eucrustacea, and Sidneyia); 66, keeled styliform telson (present in Palaeoisopus).
The clade of (Agnostus + Crustacea s.l.) + Lamellipedia, retrieved in the unweighted analysis and in weighted analysis with k≥17, has a number of potential autapomorphies: 3, armature of first cephalic appendage are mediodistal setae; 25, biseral spines or spinose endites along median edge of podomeres 1–4. Characters assumed to be present in the ground pattern but lost in some of the in-group taxa are: 14, exopods differentiated into proximal and distal lobes (Agnostus and Lamellipedia, with a reversal in Crustacea s.l. and modification in Marrellomorpha); 24, endopod of seven podomeres (shortened in Crustacea s.l.); 66, tubular cap-like to tubular styliform telson (with reversals to plate-like in Sidneyia and Siriocaris).
The phylogenetic placement of Agnostus has been a matter of contentious debate [9, 97, 98]. As in some earlier analyses [31, 60], Agnostus is not retrieved as a trilobite but as sister taxon to Crustacea s.l., but the clade has no jackknifing or Bremer support and is not retrieved in weighted analyses with k<17. A problem here is that most characters uniting Agnostus with Crustacea s.l. are only present in the ground pattern of that taxon and lost or modified in Eucrustacea or even earlier in the eucrustacean stem-lineage. Possible synapomorphies of Agnostus with the Crustacea s.l. stem species (represented by the ground pattern) are: 10, cephalic exopods inserting along shorter joint in limbs (character reversal in Eucrustacea is an artefact from character definition, as the exopods insert only in the basipod even in the trunk limbs of the eucrustacean taxa coded here); 11, endopod of first postantennular limb heavily reduced or absent, of second reduced (absent in Martinssonia and Nebalia because in these taxa the trunk endopods are short); 12, first and second cephalic exopods multiarticulate, each article with mediodistal setae or pair of lateral setae (reversal in Nebalia); 19, long spines on exopods (reversal in Eucrustacea); 22, body limb-joint of arthrodial membrane only (convergent with Chelicerata or Euchelicerata). Weighted analysis with k ≥ 5 <17 retrieve Agnostus as sister taxon to Phytophilaspis. The clade has no jackknifing support; a potential synapomorphy is character 73, relative length of thorax longer than caudal end. Agnostus + Phyotphilaspis resolve as sister taxon to Trilobita, with potential synapomorphies: 46, calcitic cuticle; 54, raised axial region of trunk defined by axial furrows; 63, pygidium lacking lateral spines. The clade of (Agnostus + Phytophilaspis) + Trilobita is lacking jackknifing support.
All ‘artiopodan’ taxa and the Marrellomorpha form a clade that corresponds to the original Lamellipedia , though that taxon originally was defined as a grade of stem-chelicerates. Possible autapomorphies would be: 1, first cephalic appendage as antenna (convergent with Nebalia, though the latter has a quite different morphology); 2, first cephalic appendage composed of >15 articles (convergently in Nebalia; absent in Molaria); 18, imbricate exopod lamellae. Further, wide attachment of the hypostomal sclerite (character 35) is the ground pattern state optimized for the lamellipedian node. In the non-lamellipedian taxa included in the analysis, the hypostome is either natant or absent (Chelicerata, following Ortega Hernández et al. ). Within Lamellipedia, there are multiple reversals to natant, while helmetiids have an autapomorphic state. The analysis does not resolve a monophyletic Artiopoda within Lamellipedia.
Both unweighted and weighted analyses retrieve a clade of Kwanyinaspis, Siriocaris, and pygidium-bearing 'artiopodans', in the following referred to as NN1. Possible autapomorphies (both convergent with Agnostus) are: 50, edge to edge tergite articulations; 55, articulating half-rings and flanges. A possible ground pattern character lost or modified in subsequent nodes is: 16, distal lobe of exopod large, teardrop shaped with long attachment (reversals in Trilobita, Tegopelte, and Misszhouia + Naraoia compacta). A possible autapomorphy for the clade of pygidium-bearing taxa apart from the pygidium (character 59, convergent with Agnostus and Retifacies) is the absence of a free telson (character 65, convergent with Agnostus). The clade consists of a polytomy of Conciliterga, Nektaspida and a clade comprising Trilobita, Phytophilaspis, Sinoburius, and Arthroaspis. It is noteworthy, that among Naraoiidae, well supported within Nektaspida, Naraoia is paraphyletic. This mirrors a taxonomic dispute [12, 65, 69, 77] whether or not Misszhouia Chen, Edgecombe & Ramsköld 1997 is a valid genus. Despite our result, we refrain from making a statement on the matter given that neither the character set nor the taxon sampling of our analysis is tailored to resolve naraoiid relationships.
Arthroaspis bergstroemi itself resolves as the most basal member of a clade including the trilobites. Potential autapomorphies are: 43, distinct trilobation of head shield, defined by axial furrows; 44, Dorsal expression of last segment of head shield (convergent with Agnostus in unweighted analysis and with k ≥ 17). Sinoburius lunaris is united with the clade of Phytophilaspis + Trilobita by the head shield extending into genal spines flanking the anterior trunk (character 45; convergent with Aglaspidida, a character reversal has to be postulated for Agnostus in weighted analysis with k=4–16). This placement of Sinoburius is at odds with its conventional placement in Xandarellida or Petalopleura Hou & Bergström, 1997 [12, 19, 22, 26, 32, 81]. Characters proposed as synapomorphies between Sinoburius and Xandarella + Cindarella: eye slits (also Phyotphilaspis) [26, 81], a head shield overlapping multiple anterior trunk tergites, with small median area of attachment  and the presence of an axial spine on a posterior tergite . The last character is problematic, as the spine occurs on the pygidium in Sinoburius, a subterminal tergite in Cindarella, and the terminal in Xandarella. Homology of this spine is therefore questionable, if not the presence and subsequent loss of a true pygidium were postulated for Xandarellida with the spine being originally on the pygidium and then on different parts of the posterior trunk after the pygidium became split up in Xandarellidae. This seems unlikely when Luohuilinella rarus, which seems to lack a pygidium, is taken into account. The presence of eye slits in Sinoburius is tenuous, and they are absent in Cindarella. Overlap of multiple tergites is present in Xandarella and Cindarella, but probably not in Sinoburius. Edgecombe and Ramsköld  cite the holotype as showing the seventh tergite counted from posterior as fully overlain by the head shield, the sixth as partly overlain. The specimen (see also Hou & Bergström figure 77A, B ) shows seven free trunk tergites; the head shield is strongly curved adaxially, leaving effectively no overlap with the first (seventh from the posterior) tergite, let alone the second (sixth from posterior). The same is true in the other specimen figured by Hou and Bergström (figure 77C, D in ) and that figured by Luo et al. (pl. II:4 in ) and we assume that the same is the case in the poorly preserved specimens figured by Edgecombe and Ramsköld (figure 1 in ). The curvature is an effect of the genal spines bracing the thorax, the synapomorphy with the Phytophilaspis + Trilobita clade. The latter clade is defined by charcters 27, the lateral eyes being dorsal (convergent with Euchelicerata and Aglaspidida); 54, raised axial region of the trunk defined by axial furrows (convergent with Cheloniellon and Emucaris) and the absence of lateral spines on the pygidium (convergent with Tegopeltidae, Emucarididae, and Naraoia compacta + Misszhouia longicaudata; reversal in Olenoides).
Weighted analyses with k ≥ 5 resolve a clade herein referred to as NN2. A potential autapomorphy is wide attachment of the hypostomal sclerite (character 35, convergent with Kwanyinaspis, Siriocaris, and Trilobita; reversal in Mimetaster, possibly Marrellomorpha + Burgessia). Two addiditional characters are optimized as ground pattern characters of the group, but are known only for few of the included taxa and seem dubious; 17, two joints in flap-like exopod (present in Emeraldella and Sidneya, while the exopods of Retifacies lack joints; unknown for the other taxa). 72, paddles as pre-terminal appendages (known only for Sidneya and Emeraldella).
Tergite morphology in NN1
Unweighted and weighted analyses resolve a clade of all pygidium bearing taxa except Agnostus and Retifacies. Kwanyinaspis and Siriocaris are united with this clade by tergites that articulate edge to edge with axial articulating half-rings and lateral articulating flanges (characters 50, 55). Previous studies have recognised edge to edge articulations as a potential synapomorphy between Helmetiida and Trilobita , but the present results rather strongly suggest this to be a symplesiomorphy. Indeed, tergite morphology is strikingly similar between Kwanyinaspis, Siriocaris, Arthroaspis, and the helmetiids. This has two interesting functional corollaries; first, the articulating half-rings of the mentioned taxa seem to be narrow axial projections of the tergites, while they are well formed devices set off by articulating furrows in the trilobites. The present topology suggests that the trilobite condition is likely derived from the short sagittal projections of taxa like Arthroaspis, while articulating flanges and edge to edge articulations are potentially functionally coupled and have already been present in the ground pattern of NN1 as evident by Siriocaris. The sophisticated half-rings of trilobites are an adaptation to enrolment [26, 99]. The capability to enrol has also been suggested for the Sirius Passet arthropod Buenaspis forteyi Budd 1999 , where the axis and articulating half-ring take up most of the tergal width and the lateral extremities of the tergopleurae ostensibly have articulating facets , as do many enrolling trilobites, but as seem to be absent in the non-trilobite members of NN1. Encapsulated enrolment, i.e. enrolment effectively shielding the ventral side is considered to be a homoplastic feature of derived trilobite taxa [99–101].Various types of encapsulated enrolment have been described , and many, though not all of these are functionally linked with a large pygidium. Consequently, the large pygidium, or iso- to macropygous condition, is often considered to have evolved homoplasticly in different trilobite taxa from the supposed plesiomorphic micropygous state, i.e. a small pygidium, in the ground pattern of Trilobita . This seems counterintuitive at first glance, when taking the pygidium bearing clade within NN1 into account; all taxa including the trilobite’s immediate sister taxon and stem, are iso- to macropygous. But with the notable exception of Eodiscina, Kobayashi, 1939, the stratigraphically old trilobite taxa are indeed almost universally micropygous. Basal trilobite phylogeny remains a matter of debate , but the basal split, as best supported would be among micropygous Olenellina  and all other trilobites, including a paraphyletic “Redlichiina” at the base . The “redlichiine” trilobites equally are micropygous, while the isopygous Eodiscina are considered to branch off above, although some have suggested them to be derived from olenellines . Either placement would support the hyposthesis of the micropygous condition as the ground pattern state for Trilobita. Thus, the relevant questions are; what drove the evolution of large pygidia basally in NN1?, and why the reversal in the stem species of trilobita? Reduction of number of articulations in order to reduce the risk of intersclerite rupture has been suggested as a reaction to selective pressure in eutrilobites driving caudalization [99, 106], and this would be equally true for animals with limited ability to flex or enrol. Indeed, the disarticulated material of Arthroaspis indicates that the articulation style of basal members of NN1 was more prone to intersclerite rupture, though it is not clear if the preserved cases are postmortem or exuvial. The early trilobites, in contrast to taxa with the plesiomorphic articulation type, could enrol, albeit not encapsulated, and it is possible that the initial loss of the large pygidium in Trilobita is linked to the ability of incipient enrolment, potentially coupled with biomineralization in order to strengthen the tergites for protection. But this remains speculation until more is known about the stem lineage of Trilobita.
One aspect of trilobite tergite morphology that has recently garnered attention is the mismatch of tergite and segment boundaries . There is no direct evidence of the presence or absence of that mismatch in many of the taxa coded in the analysis. There is evidence for Leanchoilia illecebrosa where a specimen documented by Y. Liu, X-g. Hou, and J. Bergström in their figure 2D  shows very clearly how the appendages insert under the tergite boundaries. A specimen of Alalcomenaeus cambricus that shows the relations between tergites and limb insertion best is figured by D.E.G. Briggs and D. Collins in their plate 2, figure 3  and also shows limbs inserting under tergal boundaries. Reinterpretation of the putative tendinous bars in Kiisortoqia soperi as ventral cuticle  is somewhat tenuous. One criterium for that was that the putative bars did not extend past the axis, but the specimen in figure 12C by Stein  shows them to do just that. Kiisortoqia thus does not serve as a model for a fossil arthropod displaying dorsoventral alignment of tergites and segments. According to Ortega Hernández and Brena, Agnostus pisiformis does not show the dorsoventral mismatch , yet the specimen shown in plate 29, figure 4 of K. J. Müller and D. Walossek  clearly shows appendages to insert exactly under the edge-to-edge articulations of the tergites. It is therefore possible that the dorsoventral mismatch is more widely distributed than assumed by Ortega Hernández and Brena and may not necessarily mirror a derived mode of tergite formation in trilobites, helmetiids, and nektaspids.
Appendage morphology and posture
The appendages of trilobites and many of their lower Palaeozoic allies have long been recognized as being similar in morphology [20, 109]. In particular, among Trilobita, Nektaspida, Helmetiida, and Xandarellida, appendage morphology seems to be constant, and their exopod morphology in particular has been suggested a synapomorphy [28, 31]. Our topology suggests, that this bilobate exopod morphology with lamellar setae is potentially a ground pattern character for Lamellipedia and experiences modification in some of the lamellipedian taxa, such as e.g. Marrellomorpha, where lamellae insert on individual articles rather than on the proximal lobe of a bilobate flap . The presence of this trilobite-like limb morphology basally in a large clade of non-biomineralizing arthropods suggests that the trace fossils often attributed to the trilobites from the earliest Cambrian, notably Rusophycus, may be indicative of the behaviour of other members of the clade rather than trilobites themselves, which indeed appear in the geological record somewhat after the trace fossils. However, one aspect that would affect trace fossils is limb stance . Conventionally, the limbs of most lamellipedian taxa have been considered laterally splayed , though whether this is a true morphological feature, postmortem effect, or subject to flexibility of the body–limb joint has been debated [113, 114]. Laterally deflected limbs could be shown to be present in Emeraldella brocki, though the outward curvature is achieved in the proximal endopod podomeres , as is also the case in Sidneyia inexpectans (Stein in preparation). For the Nektaspida, available evidence suggests that the appendages could swing out at the body-limb joint, but there was no outward flexure ‘hard wired’ into the limb axis morphology [69, 77, 113]. For Olenoides serratus, it seems that the limbs indeed were deflected through outward rotation at the basipod, resulting in the endopods inserting distolaterally rather than distally, as reinvestigation of specimens USNM 65515 and 188573 shows (see Whittington’s plates 11 and 16 respectively ). How exactly this is morphologically achieved remains unclear. It is worth noting, that the outward splay is restricted to the anterior trunk region, and that limb stance changes gradually to pending towards the posterior, as is observed in Emeraldella brocki, defying the conventional wisdom of the fully homonomous limb series in trilobites and their allies. The pending posterior limbs of taxa such as Emeraldella and Olenoides, like the rotated anterior ones, insert in an extensive arthrodial membrane, and thus are similar to those of the naraoiids. As an interesting developmental note, these are the appendages of the segments that have been formed the latest during development, and thus are the least differentiated and display an ontogenetically early morphology. A similar outward rotation at the basipod as in Olenoides seems to be present in Arthroaspis, as indicated by the relatively inward turned basipod endite in the isolated limb in Figure 11C. This suggests, that the trilobite-type limb stance was present in the ground pattern of the clade Arthroaspis + (Sinoburius + (Phytophilaspis + Trilobita)).
Arthroaspis bergstroemi is a new arthropod from the early Cambrian Sirius Passet Lagerstätte of North Greenland that displays an interesting combination of characters, with a broadly helmetiid-like tergum, a nektaspid-like configuration of the hypostome and prehypostomal sclerite complex, and trilobite-like features of the head shield and stance of the appendages. Cladistic analysis resolves a monophyletic Lamellipedia as sister taxon to Crustacea s.l. (possibly representing Tetraconata), lending further support to the notion that the trilobite-like arthropods belong with Mandibulata [19, 28, 29, 31] rather than with Chelicerata as postulated under the traditional Arachnomorpha concept [20, 22, 27]. Arthroaspis falls basally within the clade including the trilobites, Phytophyilaspis, and Sinoburius, indicating that its helmetiid-like tergum morphology represents the plesiomorphic tergite morphology of a large clade including the pygidium bearing Helmetiida, Nektaspida, and Trilobita. The sophisticated articulating devices of the trilobites are derived from the helmetiid-like tergite articulations, already established in the sister taxa to the pygidium bearing clade. Causes for their evolution remain a matter of speculation, but a functional coupling to the evolution of the ability to enrol is one possible factor. The trilobites' stereotypical lateral splay of appendages, where the endopods insert almost laterally rather than distally on the basipods of the anterior trunk limbs was present in the trilobites closest relatives, including Arthroaspis, but not at deeper nodes in the Lamellipdia. This has consequences for the attribution of trace fossils to trilobite-like arthropods.
Whittington HB: Early arthropods, their appendages and relationships. Systematic Association special Volume. 1979, 12: 253-268.
Briggs DEG, Whittington HB: Relationships of arthropods from the Burgess Shale and other Cambrian sequences. Short Papers for the Second International Symposium on the Cambrian System. Edited by: Taylor ME. 1981, Unites States Depatment of the Interior, Geological Survey Open-File Report, 81-743:38–41
Briggs DEG: Affinities and early evolution of the Crustacea: The evidence of the Cambrian fossils. Crustacean Phylogeny. Edited by: Schram FR. 1983, Rotterdam: Balkema, 1-22.
Bergström J: Morphology of fossil arthropods as a guide to phylogenetic relationships. Arthropod phylogeny. Edited by: Gupta AP. 1979, New York: Van Nostrand Reinhold, 3-56.
Briggs DEG, Fortey RA: The early radiation and relationships of the major arthropod groups. Science. 1989, 246: 241-243. 10.1126/science.246.4927.241.
Müller KJ, Walossek D: Skaracarida, a new order of Crustacea from the Upper Cambrian of Västergötland, Sweden. Fossils Strata. 1985, 17: 1-65.
Müller KJ, Walossek D: Martinssonia elongata gen. et sp.n., a crustacean-like euarthropod from the Upper Cambrian 'Orsten' of Sweden. Zool Scr. 1986, 15: 73-92. 10.1111/j.1463-6409.1986.tb00211.x.
Müller KJ, Walossek D: External morphology and larval development of the Upper Cambrian maxillopod Bredocaris admirabilis. Fossils Strata. 1988, 23: 1-70.
Walossek D, Müller KJ: Upper Cambrian stem-lineage crustaceans and their bearing upon the monophyletic origin of Crustacea and the position of Agnostus. Lethaia. 1990, 23: 409-427. 10.1111/j.1502-3931.1990.tb01373.x.
Walossek D: The Upper Cambrian Rehbachiella and the phylogeny of Branchiopoda and Crustacea. Fossils Strata. 1993, 32: 1-202.
Chen J, Edgecombe GD, Ramsköld L, Zhou G: Head segmentation in Early Cambrian Fuxianhuia: implications for arthropod evolution. Science. 1995, 268: 1339-1343. 10.1126/science.268.5215.1339.
Hou X, Bergström J: Arthropods of the Lower Cambrian Chengjiang Fauna, southwest China. Fossils Strata. 1997, 45: 1-116.
Waloszek D, Chen J, Maas A, Wang X: Early Cambrian arthropods—new insights into arthropod head and structural evolution. Arthropod Struct Dev. 2005, 34: 189-205. 10.1016/j.asd.2005.01.005.
Budd GE: A palaeontological solution of the arthropod head problem. Nature. 2002, 417: 271-275. 10.1038/417271a.
Budd GE: Head structure in upper stem-group euarthropods. Palaeontology. 2008, 51: 561-573. 10.1111/j.1475-4983.2008.00752.x.
Legg DA, Sutton MD, Edgecombe GD, Caron J-B: Cambrian bivalved arthropod reveals origin of arthrodization. P Roy Soc Lond B Bio. 2012, 279: 4699-4704. 10.1098/rspb.2012.1958.
Briggs DEG, Lieberman BS, Hendricks JR, Halgedahl SL, Jarrard RD: Middle Cambrian arthropods from Utah. J Pal. 2008, 82: 238-254. 10.1666/06-086.1.
Daley AC, Budd GE, Caron J-B, Edgecombe GD, Collins D: The Burgess Shale anomalocaridid Hurdia and its significance for early euarthropod evolution. Science. 2009, 323: 1597-1600. 10.1126/science.1169514.
Ortega-Hernández J, Legg DA, Braddy SJ: The phylogeny of aglaspidid arthropods and the internal relationships within Arthropoda. Cladistics. 2013, 29: 15-45. 10.1111/j.1096-0031.2012.00413.x.
Størmer L: On the relationships and phylogeny of fossil and recent Arachnomorpha. Skrifter Utgitt av Det Norske Videnskaps-Akademi i Oslo. I. Matematisk-Naturvetenskapelig Klasse. 1944, 5: 1-158.
Chen J, Waloszek D, Maas A: A new ‘great-appendage’ arthropod from the Lower Cambrian of China and homology of chelicerate chelicerae and raptorial antero-ventral appendages. Lethaia. 2004, 37: 3-20.
Cotton TJ, Braddy SJ: The phylogeny of arachnomorph arthropods and the origin of the Chelicerata. Trans R Soc Edinb Earth Sci. 2004, 94: 169-193.
Haug JT, Waloszek D, Maas A, Liu Y, Haug C: Functional morphology, ontogeny and evolution of mantis shrimp-like predators in the Cambrian. Palaeontology. 2012, 55: 369-399. 10.1111/j.1475-4983.2011.01124.x.
Haug JT, Briggs DEG, Haug C: Morphology and function in the Cambrian Burgess Shale megacheiran arthropod Leanchoilia superlata and the application of a descriptive matrix. BMC Evol Bio. 2012, 12: 1-20. 10.1186/1471-2148-12-1.
Heider K: Entwicklungsgeschichte und Morphologie der Wirbellosen. Die Kultur der Gegenwart, Theil 3, Abt. 4. 1913, Leipzig: BG Teubner
Edgecombe GD, Ramsköld L: Relationships of Cambrian Arachnata and the systematic position of Trilobita. J Pal. 1999, 73: 263-287.
Hendricks JR, Lieberman BS: New phylogenetic insights into the Cambrian radiation of arachnomorph arthropods. J Pal. 2008, 82: 585-594. 10.1666/07-017.1.
Scholtz G, Edgecombe GD: Heads, Hox and the phylogenetic position of trilobites. Crustacean Issues 16. Crustacea and Arthropod Relationships. Edited by: Koenemann S, Jenner RA. 2005, Boca Raton, Fl: Taylor & Francis, 139-165.
Scholtz G, Edgecombe GD: The evolution of arthropod heads: reconciling morphological, developmental and palaeontological evidence. Dev Genes Evol. 2006, 216: 395-415. 10.1007/s00427-006-0085-4.
Hughes NC, Haug JT, Waloszek D: Basal euarthropod development: a fossil based perspective. Evolving Pathways: Key Themes in Evolutionary Developmental Biology. Edited by: Minelli A, Fusco G. 2008, Cambridge, UK: Cambridge University Press, 281-298.
Stein M, Selden PA: A restudy of the Burgess Shale (Cambrian) arthropod Emeraldella brocki and reassessment of its affinities. J Syst Pal. 2012, 10: 361-383. 10.1080/14772019.2011.566634.
Paterson JR, García-Bellido DC, Edgecombe GD: New Artiopodan Arthropods from the Early Cambrian Emu Bay Shale Konservat-Lagerstätte of South Australia. J Pal. 2012, 86: 340-357. 10.1666/11-077.1.
Conway Morris S, Peel JS, Higgins AK, Soper NJ, Davis NC: A Burgess Shale-like fauna from the Lower Cambrian of North Greenland. Nature. 1987, 326: 181-183. 10.1038/326181a0.
Conway Morris S: The crucible of creation. The Burgess Shale and the rise of animals. 1998, Oxford, UK: Oxford University Press
Ineson JS, Peel JR: Geological and depositional setting of the Sirius Passet Lagerstätte (Early Cambrian), North Greenland. Can J Earth Sci. 2011, 48: 1259-1281. 10.1139/e11-018.
Babcock LE, Peel JS: Palaeobiology, taphonomy, and stratigraphic significance of the trilobite Buenellus from the Sirius Passet Biota, Cambrian of North Greenland. MAAP. 2007, 34: 401-418.
Peel JS, Ineson JR: The extent of the Sirius Passet Lagerstätte (early Cambrian) of North Greenland. Bull Geosci. 2011, 86: 535-543.
Peel JS, Ineson JR: The Sirius Passet Lagerstätte (early Cambrian) of North Greenland. Palaeontographica Canadiana. 2011, 31: 109-118.
Peel JS: Articulated hyoliths and other fossils from the Sirius Passet Lagerstätte (early Cambrian) of North Greenland. Bull Geosci. 2010, 85: 385-394.
Vinther J, Eibye-Jacobsen D, Harper DAT: An Early Cambrian stem polychaete with pygidial cirri. Biol Letters. 2011, 7: 929-932. 10.1098/rsbl.2011.0592.
Vinther J, Smith MP, Harper DAT: Vetulicolians from the Lower Cambrian Sirius Passet Lagerstätte, North Greenland, and the polarity of morphological characters in basal deuterostomes. Palaeontology. 2011, 54: 711-719. 10.1111/j.1475-4983.2011.01034.x.
Higgins AK, Ineson JR, Peel JS, Surlyk F, Sønder-Holm M: Lower Palaeozoic Franklinian Basin of North Greenland. Grønlands Geologiske Undersøgelse Bulletin. 1991, 160: 71-139.
Ineson JR, Peel JS: Cambrian shelf stratigraphy of North Greenland. Geology of Greenland Survey Bulletin. 1997, 172: 1-120.
Butterfield NJ: Organic preservation of non−mineralizing organisms and the taphonomy of the Burgess Shale. Paleobiology. 1990, 16: 272-286.
Orr PJ, Briggs DEG, Kearns SL: Cambrian Burgess Shale Animals replicated in clay minerals. Science. 1998, 281: 1173-1175.
Caron J-B, Jackson DA: Taphonomy of the Greater Phyllopod Bed Community, Burgess Shale. PALAIOS. 2006, 21: 451-465. 10.2110/palo.2003.P05-070R.
Gaines RR, Hammarlund EU, Hou X, Qi C, Gabbott SE, Zhao Y, Peng J, Canfield DE: Mechanism for Burgess Shale-type preservation. PNAS. in press
Budd GE: Arthropod body-plan evolution in the Cambrian with an example from anomalocaridid muscle. Lethaia. 1998, 31: 197-210.
Budd GE: A nektaspid arthropod from the Early Cambrian Sirius Passet fauna, with a description of retrodeformation based on functional morphology. Palaeontology. 1999, 42: 99-122. 10.1111/1475-4983.00064.
Budd GE: A Cambrian gilled lobopod. Nature. 1993, 364: 709-711. 10.1038/364709a0.
Budd GE: Stem group arthropods from the Lower Cambrian Sirius Passet fauna of North Greenland. Arthropod Relationships, Systematics Association Special Volume Series. Edited by: Fortey RA, Thomas RH. 1997, London: Chapman and Hall, 125-138.
Budd GE: Campanamuta mantonae gen. et sp. nov., an exceptionally preserved arthropod from the Sirius Passet Fauna (Buen Formation, lower Cambrian, North Greenland). J Syst Pal. 2011, 9: 217-260. 10.1080/14772019.2010.492644.
Butterfield NJ: Secular distribution of Burgess-Shale-type preservation. Lethaia. 1995, 28: 1-13. 10.1111/j.1502-3931.1995.tb01587.x.
Mángano MG, Bromley RG, Harper DAT, Nielsen AT, Smith MP, Vinther J: Nonbiomineralized carapaces in seafloor landscapes (Sirius Passet, Greenland): Opening a new window into early Phanerozoic benthic ecology. Geology. 2012, 40: 519-522. 10.1130/G32853.1.
Whittington HB: Morphology of the exoskeleton. Treatise on Invertebrate Paleontology, Pt. O, Arthropoda 1, Trilobita, Revised. Edited by: Kaesler RL. 1997, Lawrence: Geological Society of America and University of Kansas Press, 1-85.
Stein M, Waloszek D, Maas A, Haug JT, Müller KJ: The stem crustacean Oelandocaris oelandica Müller re-visited. Acta Pal Pol. 2008, 53: 461-484. 10.4202/app.2008.0308.
Goloboff PA, Farris JS, Nixon KC: TNT, a free program for phylogenetic analysis. Cladistics. 2008, 24: 774-786. 10.1111/j.1096-0031.2008.00217.x.
Goloboff PA: Estimating character weights during tree search. Cladistics. 1993, 9: 83-91. 10.1111/j.1096-0031.1993.tb00209.x.
Edgecombe GD, García-Bellido DC, Paterson JR: A New Leanchoiliid Megacheiran Arthropod from the Lower Cambrian Emu Bay Shale, South Australia. Acta Pal Pol. 2011, 56: 385-400. 10.4202/app.2010.0080.
Haug JT, Maas A, Waloszek D: †Henningsmoenicaris scutula, †Sandtorpia vestrogothiensis gen. et sp. nov. and heterochronic events in early crustacean evolution. Earth Env Sci Trans R Soc Edinb. 2010, 100: 311-350.
Briggs DEG, Bruton DL, Whittington HB: Appendages of the arthropod Aglaspis spinifer (Upper Cambrian, Wisconsin) and their significance. Palaeontology. 1979, 22: 167-180.
Stürmer W, Bergström J: The arthropod Cheloniellon from the Devonian Hunsrück Slate. Pal Z. 1978, 52: 57-81.
Kühl G, Bergström J, Rust J: Morphology, Palaeobiology, and Phylogenetic Position of Vachonisia rogeri (Arthropoda) from the Lower Devonian Hunsrück Slate (Germany). Palaeontographica Abteilung A. 2008, 286: 123-157.
Kühl G, Rust J: Re-investigation of Mimetaster hexagonalis: a marrellomorph arthropod from the Lower Devonian Hunsrück Slate (Germany). Pal Z. 2010, 84: 397-411. 10.1007/s12542-009-0049-x.
Hou X, Aldridge RJ, Bergström J, Siveter DJ, Siveter DJ, Fen X: The Cambrian Fossils of Chengjiang, China. The Flowering of Early Animal Life. 2004, Oxford: Blackwell
Zhang X, Han J, Zhang Z, Liu H, Shu D: Redescription of the Chengjiang arthropod Squamacula clypeata Hou and Bergström, from the Lower Cambrian, South-West China. Palaeontology. 2004, 47: 605-617. 10.1111/j.0031-0239.2004.00363.x.
Minter NJ, Mángano MG, Caron J-B: Skimming the surface with Burgess Shale arthropod locomotion. P Roy Soc Lond B Bio. 2012, 279: 1613-1620. 10.1098/rspb.2011.1986.
Zhang X, Shu D: A new arthropod from the Chengjiang Lagerstätte, Early Cambrian, southern China. Alcheringa. 2005, 29: 185-194. 10.1080/03115510508619300.
Zhang X, Shu D, Erwin DH: Cambrian naraoiids (Arthropoda): morphology, ontogeny, systematics, and evolutionary relationships. J Pal. 2007, 81: 1-52.
Haug JT, Castellani C, Haug C, Waloszek D, Maas A: A Marrella-like arthropod from the Cambrian of Australia: A new link between “Orsten”-type assemblages and the Burgess Shale. Acta Pal Pol.
Moore RA, Briggs DEG, Bartels C: A new specimen of Weinbergina opitzi (Chelicerata: Xiphosura) from the Lower Devonian Hunsrück Slate, Germany. Pal Z. 2005, 79: 399-408.
Bruton DL, Whittington HB: Emeraldella and Leanchoilia, two arthropods from the Burgess Shale, Middle Cambrian, British Columbia. Philos Trans R Soc Lond. 1983, 300: 553-582. 10.1098/rstb.1983.0020.
Dunlop JA, Arango CP: Pycnogonid affinities: a review. J Zool Syst Evol Res. 2005, 43: 8-21. 10.1111/j.1439-0469.2004.00284.x.
Dzik J, Lendzion K: The oldest arthropods of the East European Platform. Lethaia. 1988, 21: 29-38. 10.1111/j.1502-3931.1988.tb01749.x.
Castellani C, Haug JT, Haug C, Maas A, Schoenemann B, Waloszek D: Exceptionally well-preserved isolated eyes from Cambrian ‘Orsten’ fossil assemblages of Sweden. Palaeontology. 2012, 55: 553-566. 10.1111/j.1475-4983.2012.01153.x.
Ramsköld L, Chen J, Edgecombe GD, Zhou G: Cindarella and the arachnate clade Xandarellida (Arthropoda, Early Cambrian) from China. Trans R Soc Edinb Earth Sci. 1997, 88: 19-38. 10.1017/S0263593300002297.
Chen J, Edgecombe GD, Ramsköld L: Morphological and ecological disparity in naraoiids (Arthropoda) from the Early Cambrian Chengjiang Fauna, China. Rec Aust Mus. 1997, 49: 1-24. 10.3853/j.0067-1975.49.1997.249.
Whittington HB: The Middle Cambrian trilobite Naraoia, Burgess Shale, British Columbia. Philos Trans R Soc Lond. 1977, 280: 409-443. 10.1098/rstb.1977.0117.
Briggs DEG, Collins D: The arthropod Alalcomenaeus cambricus Simonetta, from the Middle Cambrian Burgess Shale of British Columbia. Palaeontology. 1999, 42: 953-977. 10.1111/1475-4983.00104.
Liu Y, Hou X, Bergström J: Chengjiang arthropod Leanchoilia illecebrosa (Hou, 1987) reconsidered. GFF. 2007, 129: 263-272. 10.1080/11035890701293263.
Paterson JR, Edgecombe GD, García-Bellido DC, Jago JB, Gehling JG: Nektaspid arthropods from the lower Cambrian Emu Bay Shale lagerstätte, South Australia, with a reassessment of lamellipedian relationships. Palaeontology. 2010, 53: 377-402. 10.1111/j.1475-4983.2010.00932.x.
Fortey RA, Theron JN: A new Ordovician arthropod, Soomaspis, and the agnostid problem. Palaeontology. 1994, 37: 841-861.
Stürmer W, Bergström J: Weinbergina, a xiphosuran arthropod from the Devonian Hunsrück Slate. Pal Z. 1981, 55: 237-255.
Bruton DL: The arthropod Sidneyia inexpectans, Middle Cambrian, Burgess Shale, British Columbia. Philos Trans R Soc Lond. 1981, 295: 619-656. 10.1098/rstb.1981.0164.
Minelli A, Fusco G, Hughes NC: Tagmata and segment specification in trilobites. Spec Pap Palaeontol. 2003, 70: 31-43.
Zhang X, Fu D, Dai T: A new xandarellid arthropod from the Chengjiang Lagerstätte, Lower Cambrian of Southwest China. Geobios. 2012, 45: 335-338. 10.1016/j.geobios.2011.09.001.
Whittington HB: Trilobites with appendages from the Middle Cambrian, Burgess Shale, British Columbia. Fossils Strata. 1975, 4: 97-136.
Ramsköld L, Chen J, Edgecombe GD, Zhou G: Preservational folds simulating tergite junctions in tegopeltid and naraoiid arthropods. Lethaia. 1996, 29: 15-20. 10.1111/j.1502-3931.1996.tb01832.x.
Budd GE, Telford MJ: The origin and evolution of arthropods. Nature. 2009, 457: 812-817. 10.1038/nature07890.
Bergström J: Organization, life and systematics of trilobites. Fossils Strata. 1973, 2: 1-69.
Vannier J, Chen J: Digestive system and feeding mode in Cambrian naraoiid arthropods. Lethaia. 2002, 35: 107-120. 10.1080/002411602320183971.
Luo H, Hu S, Zhang S, Tao Y: New occurrence of the Early Cambrian Chengjiang Fauna in Haiku, Kunming, Yunnan Province, and study on Trilobitoidea. Acta Geol Sin. 1997, 71: 122-132.
Lagebro L, Stein M, Peel JS: A new ?lamellipedian arthropod from the early Cambrian Sirius Passet Fauna of North Greenland. J Pal. 2009, 83: 820-825. 10.1666/09-011.1.
Jell PA, Hughes NC: Himalayan Cambrian trilobites. Spec Pap Palaeontol. 1997, 58: 1-113.
Stein M: A new arthropod from the Early Cambrian of North Greenland with a ‘great appendage’ like antennula. Zool J Linn Soc-Lond. 2010, 158: 477-500. 10.1111/j.1096-3642.2009.00562.x.
Bergström J, Stürmer W, Winter G: Palaeoisopus, Palaeopantopus and Palaeothea, pycnogonid arthropods from the Lower Devonian Hunsrück Slate, West Germany. Pal Z. 1980, 54: 7-54.
Stein M, Waloszek D, Maas A: Oelandocaris oelandica and the stem lineage of Crustacea. Crustacean Isues 16. Crustacea and Arthropod Relationships. Edited by: Koenemann S, Jenner RA. 2005, Boca Raton, FL: Taylor & Francis, 55-71.
Cotton TJ, Fortey RA: Comparative morphology and relationships of the Agnostida. Crustacean Isues 16. Crustacea and Arthropod Relationships. Edited by: Koenemann S, Jenner RA. 2005, 95-136.
Esteve J, Hughes NC, Zamora S: Thoracic structure and enrolment style in Middle Cambrian Eccaparadoxides pradoanus presages caudalization of the derived trilobite trunk. Palaeontology. in press
Whittington HB: Articulation and exuviation in Cambrian trilobites. Philos Trans R Soc Lond. 1990, 329: 27-46. 10.1098/rstb.1990.0147.
Hughes NC: Trilobite tagmosis and body patterning from morphological and developmental perspectives. Integr Comp Biol. 2003, 43: 185-206. 10.1093/icb/43.1.185.
Lieberman BS, Karim TS: Tracing the trilobite tree from the root to the tips: a model marriage of fossils and phylogeny. Arthropod Struct Dev. 2010, 39: 111-123. 10.1016/j.asd.2009.10.004.
Lieberman BS: Phylogenetic analysis of the Olenellina Walcott, 1890 (Trilobita, Cambrian). J Pal. 2001, 75: 96-115. 10.1666/0022-3360(2001)075<0096:PAOTOW>2.0.CO;2.
Lieberman BS: Phylogenetic analysis of some basal Early Cambrian trilobites, the biogeographic origins of Eutrilobita, and the timing of the Cambrian radiation. J Pal. 2002, 76: 692-708. 10.1666/0022-3360(2002)076<0692:PAOSBE>2.0.CO;2.
Jell PA: Phylogeny of early Cambrian trilobites. Spec pap Palaeontol. 2003, 70: 45-57.
Hughes NC: The evolution of trilobite body patterning. Ann Rev Earth Plan Sci. 2007, 2007 (35): 401-434.
Ortega-Hernández J, Brena C: Ancestral Patterning of Tergite Formation in a Centipede Suggests Derived Mode of Trunk Segmentation in Trilobites. PLoS One. 2012, 7: e52623-10.1371/journal.pone.0052623.
Müller KJ, Walossek D: Morphology, ontogeny, and life habit of Agnostus pisiformis from the Upper Cambrian of Sweden. Fossils & Strata. 1987, 19: 1-124.
Bergström J, Hou X: Chengjiang arthropods and their bearing on early arthropod evolution. Arthropod Fossils and Phylogeny. Edited by: Edgecombe GD. 1998, New York: Columbia University Press, 151-184.
Narbonne GM, Myrow PM, Landing E, Anderson MM: A candidate stratotype for the Precambrian-Cambrian boundary, Fortune Head, Burin Peninsula, southeastern Newfoundland. Can J Earth Sci. 1987, 24: 1277-1293. 10.1139/e87-124.
Lane AA, Braddy SJ, Briggs DEG, Elliott DK: A new trace fossil from the Middle Cambrian of the Grand Canyon, Arizona, USA. Palaeontology. 2003, 46: 987-997. 10.1111/1475-4983.00329.
Bergström J: The oldest arthropods and the origin of the Crustacea. Acta Zool. 1992, 73: 287-291. 10.1111/j.1463-6395.1992.tb01093.x.
Ramsköld L, Edgecombe GD: Trilobite appendage structure—Eoredlichia reconsidered. Alcheringa. 1996, 20: 269-276. 10.1080/03115519608619471.
Stein M: A new look at old data: an example from the arthropods. PALAIOS. 2011, 26: 391-393. 10.2110/palo.2011.S04.
MS is funded by the Carlsberg Foundation, Copenhagen. Field work by DATH was supported by the Agouron institute and the Carlsberg Foundation. Field work by JSP and Simon Conway Morris was supported by the Carlsberg Foundation and National Geographic Society, Washington. We thank all members of the various expeditions to the Sirius Passet locality for help with collection of the material. Fernando Pardos helped with advice on the etymology for the genus. TNT is provided by the Willi Hennig Society. Nigel Hughes and an anonymous referee helped to improve the consistency and overall quality of the manuscript.
The authors declare that they have no competing interests.
MS prepared, studied, and photographed the material, wrote the initial description, carried out the phylogenetic analysis and wrote the discussion. GEB participated in preparation and study of some of the material and supplemented the description and discussion. JSP and DATH collected the material through several field seasons, organised the material and wrote the sections on the geological setting. All authors have revised and edited the manuscript. All authors have read and approved the final manuscript.
Authors’ original submitted files for images
Below are the links to the authors’ original submitted files for images.
About this article
Cite this article
Stein, M., Budd, G.E., Peel, J.S. et al. Arthroaspisn. gen., a common element of the Sirius Passet Lagerstätte (Cambrian, North Greenland), sheds light on trilobite ancestry. BMC Evol Biol 13, 99 (2013). https://doi.org/10.1186/1471-2148-13-99
- Sirius Passet Lagerstätte
- Functional morphology