Morphology and function in the Cambrian Burgess Shale megacheiran arthropod Leanchoilia superlata and the application of a descriptive matrix
© Haug et al.; licensee BioMed Central Ltd. 2012
Received: 26 May 2012
Accepted: 17 August 2012
Published: 30 August 2012
Leanchoilia superlata is one of the best known arthropods from the middle Cambrian Burgess Shale of British Columbia. Here we re-describe the morphology of L. superlata and discuss its possible autecology. The re-description follows a standardized scheme, the descriptive matrix approach, designed to provide a template for descriptions of other megacheiran species.
Our findings differ in several respects from previous interpretations. Examples include a more slender body; a possible hypostome; a small specialised second appendage, bringing the number of pairs of head appendages to four; a further sub-division of the great appendage, making it more similar to that of other megacheirans; and a complex joint of the exopod reflecting the arthropod’s swimming capabilities.
Different aspects of the morphology, for example, the morphology of the great appendage and the presence of a basipod with strong median armature on the biramous appendages indicate that L. superlata was an active and agile necto-benthic predator (not a scavenger or deposit feeder as previously interpreted).
KeywordsMegacheira Great-appendage arthropods Chelicerata sensu lato Descriptive matrix Active predator
The description of species is fundamental to the science of zoology, including taxonomy, phylogenetic systematics, functional morphology and ultimately evolutionary biology and ecology. But living organisms can never be completely described at every level of detail down to cellular morphology. It is easier to describe fossil species entirely, but only because much less detail is available. However, many descriptions of fossils are inadequate to allow them to be used directly to prepare cladistic matrices for phylogenetic analyses. This is usually because authors concentrate on morphological features that differentiate new species from those previously described. Thus, the focus is on structures that are unique even though cladistic matrices require structures that are shared with other species. As a consequence, morphological details in many phylogenetic matrices have to be (re-)interpreted, often without the benefit of a comprehensive description. While every character and character state should be carefully reviewed prior to analysis [1–4], it is also essential to provide explicit explanations of the basis for coding.
The so-called short great-appendage arthropods have been incorporated into many recent arthropod phylogenies. Short great-appendage arthropods, which, together with Chelicerata sensu stricto, form Megacheira , have only been reported from Cambrian strata. The characteristic short great appendage is the first appendage on the head. In their redescription of Yohoia tenuis Walcott, 1912, one of these arthropods from the middle Cambrian Burgess Shale biota of British Columbia, Haug JT et al.  noted that previous phylogenetic analyses of the short great-appendage arthropods included incomplete and/or controversial codings. The present paper represents a further step in addressing this problem: a redescription of Leanchoilia superlata Walcott, 1912, one of the most abundant short great-appendage arthropods.
Leanchoilia superlata is a relatively common megacheiran arthropod (more than a thousand specimens) from the Burgess Shale. García-Bellido and Collins  redescribed it and resurrected the species L. persephone Simonetta, 1970, which had been synonymized with L. superlata by Bruton and Whittington , a view supported by Briggs and Robison . García-Bellido and Collins  also indicated that the material synonymized with L. superlata by Bruton and Whittington  might include other valid species. One of these, L. protogonia Simonetta, 1970, was subsequently resurrected by Briggs et al. .
Our reconsideration of L. superlata here is prompted by a number of factors. García-Bellido and Collins  focused on characters useful for distinguishing L. superlata from other species of Leanchoilia present in the Burgess Shale. Here we pay equal attention to other morphological details that might be important in determining the phylogenetic position or autecology of Leanchoilia. New information on Leanchoilia illecebrosa (Hou, 1987) from the lower Cambrian Chengjiang lagerstätte of China, published by Liu et al. , was not available to García-Bellido and Collins . A direct comparison of these two species is desirable as L. illecebrosa has been identified as the sister species of L. superlata and the morphology of one might illuminate that of the other. García-Bellido and Collins  discussed the relationships of Leanchoilia superlata in the context of the arachnomorph concept [11, 12]. We reconsider its affinities in the light of increasing evidence that megacheirans are derivatives of the evolutionary lineage leading to modern chelicerates, representing a monophyletic group together with Chelicerata sensu stricto[5, 13, 14].
The redescription of Leanchoilia superlata here provides a template for future investigations of other megacheirans; comparable details of other taxa would allow more robust phylogenetic and evolutionary interpretations.
Specimens in the collections of the Royal Ontario Museum, Toronto (ROM), previously identified as representatives of Leanchoilia, were inspected: a total of 1,253 slabs, very few with more than one specimen. These specimens were the basis for the study by García-Bellido and Collins , who provided details of the material and geological setting. 170 specimens preserved sufficient detail to merit being photographed (see below). Only specimens attributed to L. superlata are discussed here. A comparison with other species of Leanchoilia will be the topic of a separate paper.
Documentation and image processing
All specimens were inspected dry with a Nikon SMZ 1500 stereomicroscope under cross-polarized light. Specimens were photographed dry under cross-polarized light. Only in very rare cases did wetting specimens and photographing them under reflected light (high angle) without polarizers provide better contrast. Images were taken with a Canon Rebel T3i camera, equipped with either an EF-S 18-55 mm lens or a MP-E 65 mm macro lens. Lighting was provided by a MeiKe FC 100 LED macro ring flash and additional fiber light sources. Images were often recorded as a stack at different focal planes, especially for close-ups. Stacks were fused with CombineZM or CombineZP. Overview images, in particular, were taken as several photographs in different x- and y-positions and then stitched together with Adobe Photoshop CS3 or Microsoft Image Composite Editor (for details on composite imaging see ). Images were color- and contrast-optimized in Adobe Photoshop CS3 or GIMP 3.0. Unsharp mask filters were applied in Adobe Photoshop CS3. The 3D computer model was reconstructed using Blender.
The movable finger in the great appendage is usually a single element, i.e., a spine arising from the next distal element, but it may include more than one. Such an arrangement occurs not only in Leanchoilia, but also, e.g., in different (sub-)chelate appendages in various crustaceans and insects (Figure 1C) and in the first appendage in Amplectobelua. The different functional chelae of a multi-chela can be described independently: that in Leanchoilia superlata, for example, is composed of a proximal chela with a movable finger including a single element (the movable finger is the spine arising from the next distal element) and a distal chela where the movable finger includes two elements (Figure 1D).
In order to allow direct comparison of structures in different megacheirans, we propose a standardized description. Clearly if an interesting structure is discovered in one species, it is necessary to check for its occurrence in others (Hennig’s principal of reciprocal illumination). Even if a structure were present in closely related species, it may not have been considered sufficiently important to warrant a mention. A morphological re-interpretation is usually triggered in this way - with the discovery of a new detail in a related species.
New discoveries and new interpretations often make it necessary to re-work species descriptions . However, this process should not be restricted to supplementing or modifying data matrices, new interpretations of morphological characters should be properly explained and justified. This could be achieved by handling descriptions in a similar way to matrices, with a systematic treatment of character states and presence/absence information. Comparable approaches have been used in database projects like DELTA (DEscription Language for TAxonomy; ) although this program is neither readily accessible nor appropriate in its recent form.
Here we follow a simple 'descriptive matrix' approach, compiling the description in an xls.-file in OpenOffice with appropriate rows and columns (see Additional file 1). Following this approach will ensure that subsequently described species will be checked for all characters. When new characters come to light they can be added, but need to be checked on all species. The application of such an approach will result in a comparable set of descriptions that can be converted easily into a cladistic matrix (some characters may be dependent or reciprocal, and therefore omitted). Yet, the whole process must remain an iterative one: with the addition of each new species, new characters will be introduced, which then will have to be described in already named species. The descriptive matrix approach is established here for the short great-appendage arthropods, a small group of morphologically similar species. Expanding this approach to a larger group such as Megacheira will require a clear discussion of assumed character homologies. Even though such a process will be labor-intensive, the descriptive matrix provides a tool to make the enterprise transparent and comprehensible.
The descriptive matrix approach generates a data set that can be readily converted to a “plain language” description of the species (term from DELTA) which is easily compared to other descriptions using the same matrix. We will use the re-description of Leanchoilia superlata generated in this way here as a basis for preparing descriptions of other leanchoiliid species. Although it is straightforward to generate text directly from the matrix, we provide such a description here, but shortened to avoid repetitions.
The studied specimens of Leanchoilia superlata range in size from ca 24 mm to 70 mm. It was not possible to distinguish ontogenetic stages on the basis of measurements, nor did changes in morphology occur within this size range. Where structures vary in morphology, e.g., the number of setae on the exopods, such changes do not correlate with size and may reflect differences in preservation. Where the limitations of preservation resulted in uncertainties (e.g., in the posterior appendages) these are indicated with queries in the description (see below). For the purposes of reconstruction such missing information was inferred from the adjacent appendage(s) assuming serial similarity.
Post-ocular segment 5: trunk segment 1
Length about one fifth that of the head shield. Total width slightly greater than that of the head shield. Width of axial region similar to that of the head shield. Tergo-pleural region on each side about one quarter entire width, almost straight, curving slightly posteriorly. Lateral rim with 7 to 8 serrations (Figures 2A-C, 4).
Post-ocular segment 6
Length as in preceding segment. Total width and width of axial region slightly greater than those of preceding segment. Tergo-pleural region as in previous segment. Lateral rim with about 7 serrations (Figures 2A-C, 4).
Post-ocular segment 7
Length as in preceding segment. Total width and width of axial region slightly greater than those of preceding segment. Tergo-pleural region on each side slightly more than one quarter entire width, curving slightly posteriorly at roughly 20°. Lateral rim with about 7 serrations (Figures 2A-C, 4).
Post-ocular segment 8
Length as in preceding segment. Total width and width of axial region slightly greater than those of preceding segment. Tergo-pleural region on each side slightly more than one quarter of entire width, curving posteriorly at roughly 30°. Lateral rim with 7 to 8 serrations (Figures 2A-C, 4).
Post-ocular segment 9
Length as in preceding segment. Total width slightly greater than that of preceding segment. Axial region slightly narrower than that of preceding segment. Tergo-pleural region on each side more than one quarter of entire width, curving posteriorly at roughly 40°. Lateral rim with 7 to 8 serrations (Figures 2A-C, 4).
Post-ocular segment 10
Length as in preceding segment. Total width slightly greater than that of preceding segment, largest of series. Axial region slightly narrower than that of preceding segment. Tergo-pleural region on each side slightly less than one third of entire width, curving posteriorly at roughly 40°. Lateral rim with 7 to 8 serrations (Figures 2A-C, 4).
Post-ocular segment 11
Length as in preceding segment. Total width slightly less than that of the preceding segment. Axial region slightly narrower than that of preceding segment. Tergo-pleural region on each side about one third of entire width, curving posteriorly at roughly 45°. Lateral rim with 7 to 8 serrations (Figures 2A-C, 4).
Post-ocular segment 12
Length as in preceding segment. Total width less than that of the preceding segment. Axial region slightly narrower than that of preceding segment. Tergo-pleural region on each side about one third of entire width, curving posteriorly at roughly 50°. Lateral rim with about 7 serrations (Figures 2A-C, 4).
Post-ocular segment 13
Length as in preceding segment. Total width less than that of the preceding segment. Axial region narrower than that of preceding segment. Tergo-pleural region on each side slightly less than one third of entire width, curving posteriorly at roughly 60°. Lateral rim with probably 7 serrations (Figures 2A-C, 4).
Post-ocular segment 14
Length about one sixth of the head shield. Total width about three-quarters of preceding segment. Axial region narrower than that of preceding segment. Tergo-pleural region on each side slightly less than one third of entire width, curving posteriorly at roughly 70°. Lateral rim with probably 7 serrations (Figures 2A-C, 4).
Post-ocular segment 15: trunk segment 11
Length as in preceding segment. Total width less than two thirds of the preceding segment. Axial region narrower than that of preceding segment. Tergo-pleural region on each side slightly less than one third of entire width, curving posteriorly at roughly 85°. Lateral rim with 6 to 7 serrations (Figures 2A-C, 4).
Lateral eyes with short stalks arising from the antero-ventral region of the head (Figure 3D, F-H). Each eye consisting of two lobes.
Hypostome elongate drop-shaped, situated ventrally between the insertions of the eyes (anteriorly), appendage 1 (antero-laterally) and appendage 2 (postero-laterally) (Figure 3C). Presumably carrying the mouth opening posteriorly.
Similar in morphology (Figure 9A) but larger than appendage 3, length similar to that of head shield. Basipod with 4 groups of robust spines arranged from proximal to distal along the median edge (Figure 9B). Spine groups apparently triplets, probably with one central and two adjacent spines. Basipod-body joint the same as that in appendage 3. Endopod consists of 7 elements, their length similar to or slightly longer than width (Figure 9A), tapering progressively distally. One seta arises medio-distally from each element (Figure 9C) and an additional latero-distal seta is present on element 6. Element 7 about twice as long as element 6, length 5x width (diameter), curving slightly inwards. Exopod slightly shorter than endopod, length about 2x width, bipartite, with a triangular proximal part and a paddle-shaped distal part (Figure 9D). Proximal part articulates with basipod and bears 4 spine-like setae laterally. Distal part articulates with endopod element 1 and preserves 16 spine-like setae of an estimated 19 (3 median, 1 distal, 12 (estimated 15) laterally).
Similar in morphology (Figure 9D) and size to appendage 5. Neither basipod armature nor body joint preserved, but presumably as in appendage 4. Endopod consists of 7 elements, their length similar to or slightly longer than width (Figure 10B). Elements 1–6 tapering progressively distally. One seta arises medio-distally from each element and an additional latero-distal seta may be present on element 6. Element 7 about twice as long as element 6, length 5x width, curving slightly inwards. Exopod slightly shorter than endopod, length about 2x width, bipartite, with a triangular proximal part and a paddle-shaped distal part. Proximal part articulates with basipod and bears 4 (?) spine-like setae laterally. Distal part articulates with endopod element 1 (?) and bears 19 spine-like setae (estimated).
Similar in general aspect and size to appendage 6 (Figure 9D). Basipod with 3 or 4 groups of robust spines arranged from proximal to distal along the median edge. Spines grouped apparently as triplets, with one central and two adjacent spines (Figure 10C). Arthrodial membrane, possibly with three large folds, occupies a medial notch in the basipod where it articulates with the body (Figure 10C). Endopod consists of 7 elements (Figure 10C, D), 1–6 tapering progressively distally. All elements as long or slightly longer than wide. One seta arises medio-distally from each element and an additional latero-distal seta may be present on element 6. Element 7 about twice as long as endopod element 6, length 5x width, curving slightly inwards. Exopod slightly shorter than endopod, length about 2x width, bipartite with a triangular proximal part and a paddle-shaped distal part. Proximal part articulates with basipod and bears 4 (?) spine-like setae laterally. Distal part articulates with endopod element 1 and bears 16 spine-like setae (estimated 19).
Similar in general aspect and size to appendage 7 (Figure 9D). Neither basipod armature nor body joint preserved, but presumably as in appendage 7. Endopod and exopod as in appendage 7 (Figure 10F). Distal part bears 19 spine-like setae.
Similar in general aspect but slightly smaller than appendage 8; slightly shorter than the head shield. Basipod armature not preserved, presumably as in appendage 7. Basipod-body joint as in appendage 7 (Figure 10E). Endopod as in appendage 8. Exopod as in appendage 8 (Figure 9D), but proximal part bears only 3 (estimated) spine-like setae laterally. Distal part bears 17 spine-like setae (estimated 18).
Similar in general aspect but slightly smaller than appendage 9. Neither basipod armature nor body joint preserved, but presumably as in appendages 7 and 9, respectively. Endopod details not preserved, presumably as in appendage 9. Exopod presumably as in appendage 9, but with 16 (estimated) spine-like setae (Figure 9D).
Similar in general aspect but slightly smaller than appendage 10; length about four fifths of the head shield (Figures 9D, 10E). Neither basipod armature nor body joint preserved, but presumably as in appendages 7 and 9, respectively. Endopod as in appendage 8. Exopod presumably as in appendage 10.
Similar in general aspect but slightly smaller than appendage 11; length about three quarters of the head shield. Neither basipod armature nor body joint preserved, but presumably as in appendages 7 and 9, respectively. Endopod as in appendage 8, but elements 1 and 3 have one adjacent seta each (Figure 10G). Exopod presumably as in appendage 10.
Appendage 13–15 not preserved with details. Presumably similar in general aspect but slightly smaller than preceding appendages (Figure 2D).
Our description of Leanchoilia superlata differs significantly from earlier interpretations.
The dorsal morphology of both the head shield and tergites of Leanchoilia superlata was strongly trilobate. The body axis was slender and spindle-shaped (Figures 2B, E4A). The broad appearance of L. superlata in dorso-ventral view reflects the very wide tergo-pleurae relative to the axis (Figure 2B). García-Bellido and Collins , in contrast, interpreted the body of L. superlata as relatively broad and massive, extending across much of the width of the tergo-pleurae, which they depicted oriented ventrally (, their text-Figures nine and eleven A). Our observations show that the tergo-pleurae projected more or less horizontally (Figure 2D; , their Plate two, Figure one; , e.g., their Figures eighty-two, eighty-eight). This attitude allows the high lateral flexibility exhibited by various specimens of L. superlata (Figure 4A, C, D, H). Although dorsal flexure between tergites was limited by the backward projecting keels, specimens show that the animal could also curve to a large degree in this direction (either actively or passively) without disarticulating. L. illecebrosa from the lower Cambrian Chengjiang fauna, interpreted as sister species to L. superlata, has only been reconstructed in lateral aspect (, their Figure one). A pronounced trilobation with a slender axial region is evident, however, in well preserved specimens in dorsal view (, their Figure two F).
Leanchoilia superlata was originally described as possessing eyes [19, 20]. Subsequent studies cast doubt on this interpretation and Bruton and Whittington  considered L. superlata to be blind. García-Bellido and Collins  provided clear evidence for the presence of eye structures in this species (for a more detailed history see , p. 698). They identified four eyes in total, interpreting them as “simple” due to the absence of evidence for ommatidia. Here we demonstrate that the structures on the left and right side of the head are connected and represent just two eyes, each with two lobes (Figure 3D, F). Similar structures in L. illecebrosa were interpreted in the same way. The presence of a short stalk (Figure 3F) in L. superlata indicates that these are compound lateral eyes. The absence of evidence for ommatidia is presumably taphonomic; such evidence is unknown in Burgess Shale arthropods. The general organisation of the eye, e.g., bilobation, presence of a stalk, remains to be reinvestigated in the other leanchoiliid species.
We found no evidence to support the interpretation of the eye structures of Leanchoilia superlata and L. illecebrosa offered by Schoenemann . She reported the presence of two sets of eyes, lateral (compound) eyes and median ocelli. The structures interpreted by Schoenemann  as ocelli in L. superlata are the compound eyes below the shield (Figure 3G, H). The structure that she interpreted as a stalked eye in lateral view in L. illecebrosa is part of the great appendage, as already shown by Hou and Bergström (, their Figure twenty-four). The phylogenetic position of Leanchoilia indicates that it possessed median eyes, but we could find no evidence of them on the fossils.
A hypostome is a sclerotised plate covering the mouth opening. It is known especially in trilobites [23, 24], other Burgess Shale arthropods , and also in early crustaceans [26, 27]. While the hypostome appears among early sclerotised arthropods [28, 29] it has not been reported previously in any short great-appendage arthropod . The structure interpreted here as the hypostome in Leanchoilia superlata has the shape and position of that in other arthropods. Yet, compared to other known hypostomes of arthropods from the Burgess Shale it appears to have been less well-sclerotised . The structure has been found in only a few specimens of L. superlata, but this is also true for other important details such as the short eye stalks (see above) and the tiny second appendage (see below).
The great appendages can be preserved in different ways. In some specimens the fingers are broken off (Figure 6G), and the great appendage appears similar to that in Yohoia tenuis. In others only the distal flagellum is missing (Figure 6E). The curvature of the two more proximal fingers varies from almost straight (Figure 6D) to more strongly curved (Figure 6E), but this variation may be preservational.
Another feature of the great appendage may also be an effect of preservation: its posteriorly directed position in some specimens. Bruton and Whittington (, p. 571) discussed whether this attitude (their Figures eighty-three, one hundred and seven) could represent a position in life and interpreted this as possible but not certain. They (, their Figure one hundred and twelve b) reconstructed the posteriorly directed position of the great appendage as an attitude during swimming, and this interpretation was accepted by later authors . The difficulty with this interpretation is the movement required at the articulations (Figure 12C-G). The transition from projecting anteriorly to posteriorly demands either 1) a large membranous area, which would weaken the junction between the appendage and the body, or 2) a large notch in the most basal element of the great appendage. Evidence of such features has not been observed in any of the specimens investigated here. The two specimens used by Bruton and Whittington (, their Figures eighty-three, one hundred and seven) as a basis for their reconstruction appear to show a rotation of the appendages through 180°, based on the position of the spines. In order to achieve such a rotation without disarticulating the elements of the appendage, very extensive arthrodial membranes are required in the joints (Figure 12H-L) but there is no evidence for notches to accommodate them. The great appendages of Leanchoilia superlata that project posteriorly may have been subjected to some disarticulation (Figure 6F; ).
The second appendage and the number of head appendages
García-Bellido and Collins  followed Bruton and Whittington  in reconstructing the head of Leanchoilia superlata as comprising three appendage-bearing segments, while L. illecebrosa (a supposed sister species) was reconstructed with four . Edgecombe et al.  accepted this discrepancy as variation within the genus. We discovered that L. superlata possessed a very small second appendage, which has not been recognized before (Figures 3B8A-D). This appendage can be interpreted as a specialized mouth part. In addition to its significantly different size, it has much longer setae on the endopod than the succeeding appendages. Accordingly, L. superlata, like its sister species, has four appendage-bearing segments in the head. This feature requires reinvestigation in other leanchoiliids.
Third and succeeding appendages
A rigid basipod with median spination was described in Leanchoilia illecebrosa and L. persephone[6, 10], yet had not been reported previously in L. superlata (e.g., , their text-Figure eleven A). The apparently four spine groups observed here, at least on appendages 3–5 (Figure 9B; unclear on others), is an arrangement similar to the enditic structures on the basipod in L. illecebrosa. But the armature in L. illecebrosa consists of single spines whereas there are spine triplets in L. superlata (Figure 10C). This feature requires reinvestigation in other leanchoiliids.
The endopod in Leanchoilia superlata never comprises more than seven elements. In L. illecebrosa it was reconstructed with nine elements . García-Bellido and Collins (, their text-Figure six) interpreted the number of elements in L. persephone as nine, but they numbered their supposed most proximal element (the basipod) as endopod element 1 (“bearing gnathobases”), and did not number the distal claw. A comparison of the specimen they refer to in this context (, their text-Figure six) with similar specimens of L. superlata (Figure 10C) suggests that their “podomere 3” corresponds to the basipod. If this interpretation is correct, the structure of the endopod in L. persephone is similar to that in L. superlata. It is clear that an endopod with nine elements is not necessarily a ground pattern feature of leanchoiliids, and may not be a reliable basis for excluding the group from Euarthropoda (cf. , character 30 of their phylogenetic analysis).
While the endopods of most appendages of Leanchoilia superlata bear one seta per element, we discovered one specimen that preserves the endopod of appendage 12 and it shows two setae on elements 1 and 3 (Figure 10G). The setae on the endopods of the preceding and succeeding appendages of this specimen are not preserved so it is not known whether this pattern is unique to appendage 12 or to this specimen. With this uncertainty, we did not include this setation pattern in the reconstruction. The setation pattern requires reinvestigation in other leanchoiliids.
The general appearance of the exopods of Leanchoilia superlata has often been reconstructed as feather-like (, their text-Figure nine; , their Figure one hundred and eleven b), as if the outer rim was deeply divided. Additionally, the supposed filaments resulting from this division were reconstructed with a rounded tip. We could not confirm this interpretation. The exopod paddle has a well defined rim (Figures 9A, C, D; also , their Plate two, Figure two), from which elongate pointed structures arise. There is no evidence that these structures are filamentous and we interpret them as setae.
Functional morphology of the biramous appendages
The exopod of the third and succeeding appendages has been described as comprising two elements in Leanchoilia superlata L. persephone and L. illecebrosa[6, 10]. Yet, the nature of the articulation has been reconstructed only in L. illecebrosa and its functional morphology discussed only briefly . The main function and the evolutionary novelty represented by this articulation have not been recognized, although it represents a specialized bio-mechanical system. This system, with the proximal part of the exopod articulating with the basipod and the distal part of the exopod articulating with endopod element 1, occurs in appendage three and those following, and probably also in appendage two, although details of the last are not available due to its small size.
The extensive arthrodial membrane at the limb–body junction shows four distinct folds on the inner margin. The limb appears to articulate with the body (pivot joint) on the outer margin; thus the arthrodial membrane allowed it to swing outwards during the power stroke. Liu et al.  also suggested a degree of rotation (their Figure six D). Inward and outward movement of the appendages probably also functioned in feeding, providing the possibility of crushing food between the basipod spines. Such a movement is reminiscent of that used by different types of mandibles (, their Figure two.four.six).
The new understanding of the morphology of Leanchoilia superlata prompts a re-evaluation of its autecology. The slender body and relatively large limbs, together with the presence of stalked compound eyes, point to a more active mode of life than previously inferred. The endopods do not have a tip suitable for walking, and the long exopod setae extend distally beyond the tip of the endopods. These observations, together with the sophisticated exopod articulation and the flexibility of the limb–body junction, indicate that L. superlata was a swimmer.
There is no evidence that the exopods functioned as gills (e.g., ; see  for an extensive discussion). Gills are specialized organs with a particular ultrastructure that facilitates gas exchange. This cannot be inferred for the fossils. The large number of setae on the exopods enlarged the body surface and presumably enhanced gas exchange. Yet, their primary function appears to be for swimming. Similar considerations apply to all Burgess Shale arthropods; no exopod in any extant taxon is just a gill, but exopods may carry gill structures (e.g., in Xiphosura, Stomatopoda).
The armature of the appendages of Leanchoilia superlata indicates a predatory lifestyle. Both the basipods and endopods are equipped with spines and are unlikely to have been used for walking (supporting , p. 576). The specialized basal articulation that facilitates swimming is also advantageous for processing food. Such articulations, with a far laterally positioned pivot joint close to the body proper and a larger membrane on the median side, are often associated with mandibles, indicating that L. superlata could crush food items between its basipods. Most obviously the multi-chela of the great appendage, with its distal feelers, is a raptorial structure. Butterfield  argued that the phosphatic gut fill indicates a predatory (or scavenging) mode of life. L. superlata appears to have been an agile necto-benthic predator, actively pursuing prey.
Accordingly, Leanchoilia superlata is not interpreted as a scavenger or mud eater (contra [7, 36]). Possible prey items are more difficult to identify. The prey of Yohoia tenuis has been supposed to include the smallest arthropods such as agnostines and bradoriids . Based on its size, L. superlata probably fed on larger prey items. However, there is no evidence that it fed on scalidophoran worms like Ottoia as suggested for L. illecebrosa (, their Figure twelve). Specimens of Ottoia prolifica Walcott, 1911 often occur on the same slab as specimens of L. superlata. These specimens of O. prolifica are about the same size as the specimens of L. superlata and it is more likely that both predatory species fed on the same type of prey rather than on each other.
Our interpretation of the morphology and autecology of Leanchoilia superlata differs in important respects from earlier versions. Our study, like some other recent reinvestigations [5, 25, 37] took advantage of new investigation techniques (polarized light, composite imaging) and the availability of more taxa for comparison. Paleoecological reconstructions of the Burgess Shale biota depend on autecological interpretations of individual organisms and will be refined by future reinvestigations of other organisms.
Similarly, current phylogenetic analyses of the Burgess Shale arthropods will be improved by new morphological investigations (for a more extensive discussion, see [5, 25]). Future application of a descriptive matrix approach such as that used here will facilitate comparisons between taxa and the construction of new data matrices.
We are very grateful to Jean-Bernard Caron and Peter Fenton (Royal Ontario Museum: ROM, Toronto) who supplied us with specimens over several weeks. Brian Iwama (ROM) helped us with technical equipment. We acknowledge those who programmed the freely available software used in this study, such as OpenOffice, CombineZM/ZP, Microsoft Image Composite Editor, GIMP 3.0, and Blender. The research was carried out while JTH and CH were based at Yale. JTH was supported by a Feodor Lynen postdoctoral research fellowship from the Alexander von Humboldt-Foundation (AvH) and by Yale University. He is currently funded by AvH with a Feodor Lynen return fellowship. CH is supported by the German Academic Exchange Service (DAAD) with a return fellowship. JTH and CH are grateful to their current host Steffen Harzsch, University of Greifswald, for his support. Greg Edgecombe, Natural History Museum London, and Matthew Wills, University of Bath, made helpful suggestions on the manuscript.
- Richter S, Scholtz G: Phylogenetic analysis of the Malacostraca (Crustacea). J Zool Syst Evol Res. 2001, 39: 113-136. 10.1046/j.1439-0469.2001.00164.x.View Article
- Haug JT, Haug C, Maas A, Kutschera V, Waloszek D: Evolution of mantis shrimps (Stomatopoda, Malacostraca) in the light of new Mesozoic fossils. BMC Evol Biol. 2010, 10: 290-10.1186/1471-2148-10-290.PubMedPubMed CentralView Article
- Wirkner CS, Richter S: Evolutionary morphology of the circulatory system in Peracarida (Malacostraca; Crustacea). Cladistics. 2010, 26: 143-167. 10.1111/j.1096-0031.2009.00278.x.View Article
- Edgecombe GD, García-Bellido DC, Paterson JR: A new leanchoiliid megacheiran arthropod from the lower Cambrian Emu Bay Shale, South Australia. Acta Palaeontol Pol. 2011, 56: 385-400. 10.4202/app.2010.0080.View Article
- 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.View Article
- García-Bellido DC, Collins D: Reassessment of the genus Leanchoilia (Arthropoda, Arachnomorpha) from the Middle Cambrian Burgess Shale, British Columbia, Canada. Palaeontology. 2007, 50: 693-709. 10.1111/j.1475-4983.2007.00649.x.View Article
- Bruton DL, Whittington HB: Emeraldella and Leanchoilia, two arthropods from the Burgess Shale, Middle Cambrian, British Columbia. Philos Trans R Soc Lond. 1983, 300: 553-585. 10.1098/rstb.1983.0020.View Article
- Briggs DEG, Robison RA: Exceptionally preserved nontrilobite arthropods and Anomalocaris from the Middle Cambrian of Utah. Univ Kans Paleontol Contrib. 1984, 111: 1-24.
- Briggs DEG, Lieberman BS, Hendricks JR, Halgedahl SL, Jarrard RD: Middle Cambrian arthropods from Utah. J Paleontol. 2008, 82: 238-254. 10.1666/06-086.1.View Article
- Liu Y, Hou X, Bergström J: Chengjiang arthropod Leanchoilia illecebrosa (Hou, 1987) reconsidered. Geol Fören Stockh Förh. 2007, 129: 263-272.
- Briggs DEG, Fortey RA, Wills MA: Morphological disparity in the Cambrian. Science. 1992, 256: 1670-1673. 10.1126/science.256.5064.1670.PubMedView Article
- Wills MA, Briggs DEG, Fortey RA: Disparity as an evolutionary metric: a comparison of Cambrian and Recent arthropods. Paleobiology. 1994, 20: 93-130.
- Cotton TJ, Braddy SJ: The phylogeny of arachnomorph arthropods and the origin of Chelicerata. Trans R Soc Edinb Earth Sci. 2004, 94: 169-193.
- 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, 15: 3-20.
- Haug C, Haug JT, Waloszek D, Maas A, Frattigiani R, Liebau S: New methods to document fossils from lithographic limestones of southern Germany and Lebanon. Palaeontol Electron. 2009, 12: 6T-
- 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.PubMedView Article
- Hou X-G, Bergström J, Ahlberg P: Anomalocaris and other large animals in the Lower Cambrian Chengjiang fauna of southwest China. GFF. 1995, 117: 163-183. 10.1080/11035899509546213.View Article
- Dallwitz MJ: A general system for coding taxonomic descriptions. Taxon. 1980, 29: 41-46. 10.2307/1219595.View Article
- Walcott CD: Cambrian geology and paleontology 2, 6. Middle Cambrian Branchiopoda, Malacostraca, Trilobita and Merostomata. Smithson Misc Coll. 1912, 57: 145-229.
- Raymond PE: Leanchoilia and other Mid-Cambrian Arthropoda. Bull Mus Comp Zool Harvard Univ. 1935, 76: 205-230.
- Schoenemann B: Cambrian view. Palaeoworld. 2006, 15: 307-314. 10.1016/j.palwor.2006.10.012.View Article
- Hou X-G, Bergström J: Arthropods of the Lower Cambrian Chengjiang fauna, southwest China. Fossils Strata. 1997, 45: 1-116.
- Müller KJ, Walossek D: Morphology, ontogeny, and life habit of Agnostus pisiformis from the Upper Cambrian of Sweden. Fossils Strata. 1987, 19: 1-124.
- Hegna TA: The function of forks: Isotelus-type hypostomes and trilobite feeding. Lethaia. 2010, 43: 411-419.
- Haug JT, Maas A, Haug C, Waloszek D: Sarotrocercus oblitus - small arthropod with great impact on the understanding of arthropod evolution?. Bull Geosci. 2011, 86: 725-736.View Article
- Haug JT, Maas A, Waloszek D: Ontogeny of two Cambrian stem crustaceans, †Goticaris longispinosa and †Cambropachycope clarksoni. Palaeontographica A. 2009, 289: 1-43.
- 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.
- 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.View Article
- Budd GE: Head structure in upper stem-group euarthropods. Palaeontology. 2008, 51: 561-573. 10.1111/j.1475-4983.2008.00752.x.View Article
- Maas A, Waloszek D, Chen J-y, Braun A, Wang X-g, Huang D-y: Phylogeny and life habits of early arthropods - predation in the Early Cambrian sea. Progress Nat Sci. 2004, 14: 158-166. 10.1080/10020070412331343301.View Article
- Chen J, Waloszek D, Maas A, Braun A, Huang D, Wang X, Stein M: Early Cambrian Yangtze Plate Maotianshan Shale macrofauna biodiversity and the evolution of predation. Palaeogeogr Palaeoclim Palaeoecol. 2007, 254: 250-272. 10.1016/j.palaeo.2007.03.018.View Article
- Haug JT, Maas A, Haug C, Waloszek D: Chapter 2: Evolution of crustacean appendages. The Natural History of the Crustacea. Volume 1: Functional Morphology and Diversity. Edited by: Watling L, Thiel M. Oxford University, Oxford, in press
- Suzuki Y, Bergström J: Respiration in trilobites: a reevaluation. GFF. 2008, 130: 211-229.View Article
- Maas A, Haug C, Haug JT, Olesen J, Zhang X, Waloszek D: Early crustacean evolution and the appearance of epipodites and gills. Arthropod Syst Phylogeny. 2009, 67: 255-273.
- Butterfield NJ: Leanchoilia guts and the interpretation of three-dimensional structures in Burgess Shale-type fossils. Paleobiology. 2002, 28: 155-171. 10.1666/0094-8373(2002)028<0155:LGATIO>2.0.CO;2.View Article
- Briggs DEG, Whittington HB: Modes of life of arthropods from the Burgess Shale, British Columbia. Trans R Soc Edinb Earth Sci. 1985, 76: 149-160. 10.1017/S0263593300010415.View Article
- Stein M, Selden PA: A restudy of the Burgess Shale (Cambrian) arthropod Emeraldella brocki and reassessment of its affinities. J Syst Palaeontol. 2012, 10: 361-383. 10.1080/14772019.2011.566634.View Article
- Weirauch C: Hairy attachment structures in Reduviidae (Cimicomorpha, Heteroptera), with observations on the fossula spongiosa in some other Cimicomorpha. Zool Anz. 2007, 246: 155-175. 10.1016/j.jcz.2007.03.003.View Article
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