The biodiversity hotspot as evolutionary hot-bed: spectacular radiation of Erica in the Cape Floristic Region
© The Author(s). 2016
Received: 7 May 2016
Accepted: 8 September 2016
Published: 17 September 2016
The disproportionate species richness of the world’s biodiversity hotspots could be explained by low extinction (the evolutionary “museum”) and/or high speciation (the “hot-bed”) models. We test these models using the largest of the species rich plant groups that characterise the botanically diverse Cape Floristic Region (CFR): the genus Erica L. We generate a novel phylogenetic hypothesis informed by nuclear and plastid DNA sequences of c. 60 % of the c. 800 Erica species (of which 690 are endemic to the CFR), and use this to estimate clade ages (using RELTIME; BEAST), net diversification rates (GEIGER), and shifts in rates of diversification in different areas (BAMM; MuSSE).
The diversity of Erica species in the CFR is the result of a single radiation within the last c. 15 million years. Compared to ancestral lineages in the Palearctic, the rate of speciation accelerated across Africa and Madagascar, with a further burst of speciation within the CFR that also exceeds the net diversification rates of other Cape clades.
Erica exemplifies the “hotbed” model of assemblage through recent speciation, implying that with the advent of the modern Cape a multitude of new niches opened and were successively occupied through local species diversification.
KeywordsBiodiversity Cape Floristic Region Diversification Erica Evolution
Biological diversity is spread unevenly across the globe and across the tree of life, clustered in geographic hotspots  and species-rich clades [2–4]. Diverse organisms with a range of life history and other traits have radiated in environments with different topographies, climates, and histories. The hyper-diverse tropical Andes set the stage for a spectacular radiation of lupins (Lupinus; Fabaceae) , the Amazon rainforest for that of Inga (Fabaceae) , the Mediterranean hotspot for that of carnations (Dianthus; Caryophyllaceae)  and Southern Africa’s succulent karoo for that of ice plants (Ruschioideae; Aizoaceae) . These species-rich groups present us with a rich and powerful source of data for bettering our understanding of the origins of biological diversity: we can analyse numerous speciation events in comparable biological systems within evolutionarily recent, and hence more tractable, timescales.
The mountainous landscape of South Africa’s Cape Floristic Region (CFR) hotspot  hosts 9000 plant species, 70 % endemic [6, 7], within only c. 90,000 km2. Thirty-three species rich “Cape clades” collectively account for around half of this remarkable richness , of which the genus Erica L. would be the largest, if the around 690 species  represent a single clade. Erica species are woody shrubs that dominate the CFR’s heathland “fynbos” vegetation as well as heathland ecosystems in the western Palearctic (including the Mediterranean) and mountain “sky islands” of Tropical Africa  and Madagascar. However, the numbers of species in regions outside the CFR are lower by an order of magnitude. Such striking regional asymmetries in species richness within a group of notably consistent habit pose a fascinating evolutionary conundrum, the solutions for which can inform our general understanding of the assemblage of regional biotas.
Here we ask: a) Does the extraordinary diversity of Erica in the CFR stem from a single common ancestor in the Cape? b) Are regional asymmetries in species richness the result of shifts in rates of diversification within the Erica clade and in different areas? c) Does the radiation of Cape Erica reflect a ‘museum’ (low extinction) and/or ‘hot-bed’ (high speciation) model for the biotic assemblage of the CFR? Such an analysis demands a credible, detailed and dated phylogenetic tree of the group: we present a phylogenetic hypothesis for Erica based on greatly increased sampling of species and molecular markers.
Taxon and character sampling: Our phylogenetic hypothesis is informed by nuclear and plastid DNA sequences of c. 60 % of all Erica species, represented by 606 accessions of 488 species and 28 sub-specific taxa from across the geographic range of the clade (17 of 19 Palearctic species [89 %], 414 of 690 CFR [60 %]; 13 of 23 Tropical Africa [57 %]; 27 of 51 Drakensberg [53 %]; and 17 of c. 41 Madagascar/Mascarenes [42 %]), plus six outgroups (Additional file 1: Table S1). Specimens were collected in the field and determined by EGHO. Vouchers were lodged in herbaria (Additional file 1: Table S1), and leaf samples dried in silica gel and archived at -20 °C to preserve the DNA. Most sequences were obtained newly for this study, with some from previous work [10–12]. We obtained DNA sequences mostly using a direct PCR amplification protocol  with universal angiosperm primers [14, 15] as described in . We employed a targeted supermatrix sampling strategy : ITS and chloroplast trnT-trnL and trnL-trnF-ndhJ spacer sequences were obtained for all samples, and other plastid markers (trnL intron, atpI-atpH spacer, trnK-matK intron and matK gene, psbM-trnH spacer, rbcL gene, rpl16 intron, trnL-rpl32 spacer) were added for taxa selected, on the basis of preliminary analyses, as representative of early diverging lineages within each of the major subclades, in order to improve resolution of deeper nodes in the plastid tree. Sequences in general, and particularly ITS, were inspected to confirm the absence of polymorphism and (other) evidence of paralogy (e.g. indels in coding regions). An accessions table including Genbank accessions numbers is presented in Additional file 1: Table S1.
Phylogenetic inference: Individual matrices including all sequences for each marker were aligned in Mesquite  and imported into SequenceMatrix  to export concatenated matrices (excluding taxa causing topological conflict between gene trees; see below) for further analyses. A matrix of 63 phylogenetically representative taxa for which a minimum of 14 of the 20 data partitions were available was analysed using PartitionFinder  to infer best fitting data partitioning strategies and substitution models (heuristic search strategy ‘greedy’; comparison of fit using the Bayesian information criterion). Individual markers, coding and non-coding regions within those markers, and codon positions within protein coding genes were all specified as potential data partitions. Maximum likelihood (ML) analyses were performed using RAxML on CIPRES [20, 21] incorporating the data partitions inferred using PartitionFinder. Clade support was estimated using bootstrapping halted automatically by RAxML following the majority-rule ‘autoMRE’ criterion. To test for experimental error, confirm congruence of individual plastid markers, and to infer and compare gene trees we performed preliminary phylogenetic analyses of individual markers separately. These were followed by final analyses of ITS, combined plastid data and combined ITS and plastid data. Fifteen taxa causing topological conflict subject to ≥70 % bootstrap support (BS) between ITS and combined plastid gene trees were excluded from analyses of the concatenated data (leaving 597) under the assumption that such conflicts reflect (apparently uncommon) incidences of reticulation or incomplete lineage sorting that violate the assumption of a bifurcating tree . Further phylogenetic analyses were performed using BEAST 1.8  (as below).
Molecular dating: Two dating methods were employed on the Ericeae matrix: BEAST , using the 63 taxa matrix but excluding the most distant outgroup, Empetrum; and RELTIME , using the 597 taxa ML tree from the RAxML concatenated data analysis, removing Empetrum and Corema album. We used the 63 taxa matrix with BEAST because of the failure of multiple runs to converge with the full supermatrix, a not unexpected phenomenon in the presence of large proportions of missing data . The targeted sampling strategy meant that the same internal focal nodes are represented in both trees. For BEAST, the root age (most recent common ancestor of Erica and Daboecia) was constrained based on the results of  in Ericaceae-wide analyses employing multiple fossil calibrations (producing results consistent with those presented in ). We used a normal distribution with mean 62 Mya and SD 10, giving a 95 % prior probability distribution of 42-82 Mya reflecting uncertainty in the original analyses . In a further analysis an additional prior was implemented to reflect the age of Ericaceae pollen in sediments offshore of Southern Africa  and thereby test the impact on age estimates assuming that this pollen record represents Erica. For this, we used an exponential distribution with offset of 10 Mya (a hard minimum) and mean of 2.0, giving a 95 % prior probability distribution of 10-16 Mya (i.e. a soft maximum) for the stem node of Cape Erica. This is to assume that the Cape Erica clade is at least as old as the age of the pollen record and may be older to a limited degree. Following preliminary partitioned analyses that failed to converge, the data were not partitioned; we applied a GTR + G substitution model, lognormal relaxed clock, Yule process speciation model, and otherwise default priors, and performed two runs of 10 million generations sampling every 1000 in each case. Convergence was assessed using TRACER 1.6  and Are We There Yet , and the results summarised using programs of the BEAST package. For RELTIME we assumed local clocks and imposed age constraints by means of a point estimate for the root node (the minimum, mean and maximum ages as above).
Diversification rates analyses: To infer the net diversification rate of the Erica Cape clade and compare it to those of other Cape and rapidly radiating clades, we used the method of Magallón & Sanderson (, as implemented in GEIGER; ). For Cape Erica, we used species richness and full range of crown node ages (minimum and maximum under RELTIME and highest posterior density intervals under BEAST) as inferred here. For comparison, we performed the same calculations based on data from the literature for the recent rapid radiations of lupins , Inga , carnations , and ice plants ; as well as the Cape clades Muraltia , Pentameris  Protea  and Restionoideae (“African Restionaceae”) . The latter are examples for which detailed time-calibrated phylogenies of ancestrally CFR species – not those that also diversified in other areas – are available. We did not account for the impact on crown node age estimates of unsampled species during the calculation, and used relative extinction rates of 0.9 and zero across the board.
To further determine whether there is diversification rate heterogeneity in the Erica dataset, we used BAMM 2.5 and Bammtools 2.1 [36, 37]. The method compares the fit of different models (a series of diversification processes) assuming different numbers of shifts based on a reversible jump MCMC to explore parameter space. We used the pruned, rate-smoothed RAxML tree, as above, and corrected for non-random species sampling by assigning regional specific proportions to the few, largely endemic, clades. We used “setBAMMpriors” to adjust the priors according to the scaling of the tree. The initial speciation rate was set to 0.18 and extinction rate to 0.111 according to inferred rates for Ericaceae . Preliminary results showed that different initial speciation and extinction rate did not have a large effect on our results. The MCMC was run for 10,000,000 generations, with every 1000 generation saved. To assess convergence, the likelihood of all sampled generations was plotted in R (burnin = 10 %) and ESS values for the likelihood and the inferred numbers of shifts were calculated using the coda package . It was not possible to compare Bayes Factors for zero rate shifts with those for given numbers of shifts (see BAMM Documentation part 7.6), but we compared the prior probability of a given number of shifts to the posterior probability to confirm that these differed. We then computed the set of credible shifts and reconstructed the mean of the marginal posterior density of speciation, extinction and net diversification rates across the tree. We sought to assess whether the BAMM results are dependent on the particular topology and branch lengths of the phylogenetic tree used above by repeating the analyses with 25 randomly selected, rate smoothed and pruned RAxML bootstrap trees.
Results of preliminary analyses of individual plastid markers (TreeBase study accession URL: http://purl.org/phylo/treebase/phylows/study/TB2:S18291) showed no conflicting nodes supported at ≥70 % bootstrap support (BS). The better resolved combined plastid gene tree (Additional file 2: Figure S1a) was largely consistent with that of ITS (Additional file 2: Figure S1b). Fifteen taxa causing topological conflict subject to ≥70 % BS between ITS and combined plastid gene trees (indicated in Additional file 2: Figures S1a and b) were excluded from analyses of the concatenated data (leaving 597; Additional file 2: Figure S1c). Further exclusion of one Cape species, E. pauciovulata, resulted in an increase in support for a single Cape clade (see below) from 70 % BS (Additional file 2: Figure S1c) to 89 % (Additional file 2: Figure S1d).
The Erica phylogeny roots in a northern Palearctic grade subtending a southern African/Madagascan clade. The latter comprises a deep polytomy including a) the Cape clade, including all but one Cape species plus four found in the Drakensberg (two of which also distributed in the Cape), b) a single further Cape species, E. pauciovulata, c) E. trimera (Tropical Africa), d) the ‘Extra-CFR African clade’ that includes all other Drakensberg and Tropical African species (except for E. arborea) and a clade of all Madagascan/Mascarene species, and e) E. arborea (Palearctic and TA) (Fig. 1, Additional file 2: Figure S1). Our age estimates for clades within Erica (Fig. 1, Additional file 3: Figure S2a-c) are based on the similar results of both the two relaxed clock molecular dating methods (RELTIME, Additional file 3: Figure S2a; and BEAST, Additional file 3: Figure S2b) with secondary calibration, and additional BEAST results (Additional file 3: Figure S2c) further constrained using the Southern Africa offshore microfossil record. The crown node of Erica was estimated at 18 (24-12) Mya (RELTIME on the matrix of 597 taxa; Additional file 3: Figure S2a) and 27-19/31-12 Mya (95 % posterior probability ranges from BEAST, using the reduced matrix of 62 taxa, with/without microfossil evidence; Additional file 3: Figure S2b/c). The radiation of lineages within the African/Madagascan clade was estimated at 9 (12-6) Mya (RELTIME) and 14-11/17-7 Mya (BEAST). The stem node of the Cape clade was estimated at 8 (11-6) Mya (RELTIME) and 12-10/15-6 Mya (BEAST); the crown node at 7 (9-5) Mya (RELTIME) and 11-9/15-6 Mya (BEAST).
Plant diversification rates in the CFR and beyond. Net diversification rates of Cape clades and other recent radiations worldwide in species per million years, estimated using species numbers and clades ages with the method of S Magallón and MJ Sanderson 
Crown age (Mya)
Rate (Species/Mya) relative extinction = 0.9
Rate (Species/Mya) relative extinction = 0.0
Range of estimates from RELTIME and BEAST analyses
Presented range (molecular dating)
Presented range (molecular dating)
Presented range (molecular dating)
Presented range (molecular dating)
Lupinus stem calibrated at 21.16 Ma
Lupinus stem calibrated at 16.01 Ma
Ice plants (Aizoaceae: Ruschioideae)
Calibrated with ITS substitution rates
Calibrated with plastid substitution rates
Min. and max. ages reported
Calibrated with trnL-F/ITS substitution rates
Comparison of different MuSSE models estimated for 478 species of Erica
No. of λ parameters
No. of μ parameters
No. of q parameters
Palearctic, Cape, Drakensberg, Madagascar, Tropical Africa
λ, μ, q
Palearctic, Cape, rest of Africa
λ, μ, q
Additional file 4: Table S2, Model 1
λ, μ, q
Additional file 4: Table S2, Model 2
Additional file 4: Table S2, Model 3
λ, μ, q
Parameter estimates given the best scoring MuSSE model
Whilst the richness of Erica species in the CFR is renowned, our results can finally confirm Erica as the most species rich Cape clade. With the possible exception of a single anomalous species (E. pauciovulata), all Erica in the CFR that we analysed can be traced back to a single common ancestor that colonised the region no earlier than c. 15 Mya, and all but a handful are endemic (Fig. 1). A Late Miocene initiation of the Erica radiation in the CFR is consistent with the first appearance of pollen of Ericaceae (and various other typical fynbos groups) in the fossil record in Southern Africa after 10 Mya . Cape clades differ widely in age , and Cape Erica is neither conspicuously old nor young in this context. Its net diversification rate is modest compared to the most spectacular examples in flowering plants, documented from the much greater areas of the Andean Páramo  and the Mediterranean . The Erica diversification rate is more similar to those of other rapidly evolving Cape clades, although notably faster than any that we compared (Table 1).
This remarkable radiation of Erica in the CFR is in stark contrast to the comparatively impoverished older Palearctic lineages. The heathers originated in the Northern Hemisphere [10, 12] and northern lineages (including monotypic Calluna and two species of Daboecia) are older than the single southern Erica clade (‘African/Malagasy Erica’; ). Higher diversity in Cape compared to Mediterranean clades has been attributed to lower rates of extinction . Our results instead imply slower speciation in the wider western Palearctic (Fig. 1; Table 3 and Additional file 4: Table S2), although this conclusion must be qualified by the known difficulty of inferring extinction rates from molecular phylogenies . Although the ranges of speciation (and hence net diversification) rates in different regions outside the Palearctic overlapped (perhaps a methodological artefact caused by the much lower species numbers outside the Cape ), we discovered evidence for a rate increase within the Cape clade (Figs. 1 and 2). Phylogenetic uncertainty within the Cape clade is considerable (reflecting the short internal branches typical of bursts of lineage diversification ), but geographically, this diversification centres on lineages of the large SW-clade  mostly restricted within the South-Western CFR. Irrespective of inferred shifts in diversification rates, the greater areas of equivalent habitat in Tropical Africa and the Drakensberg (for similarly distributed Protea, estimated at roughly 17-fold; ) and in Madagascar compared to the CFR represent far lower densities of species and of speciation events through time given the phylogeny and clade ages inferred here.
The CFR is one of a number of mountainous and Mediterranean climate regions with unique and hyper-diverse biotas that both coincidentally, and as the result of worldwide climatic changes, originated within similar, relatively recent timeframes [2, 25, 40, 43]. The modern CFR was shaped by globally influenced palaeoclimatic dynamics that established during the Miocene, particularly world-wide cooling that led to aridification , and the establishment of the cold Benguela current off the south-west African coast, that led to the development of a winter rainfall regime and frequent fires [45, 46]. The disappearance of more mesic tropical forest elements from fossil deposits [27, 47] was followed by the appearance of more arid and/or fire adapted elements such as Aizoaceae, including Ruschioideae (in the succulent karoo), and Erica (in the CFR) ; the latter with its reduced leaf area and resistant yet inflammable wax-rich cuticles  combined with post-fire re-sprouting and smoke-stimulated re-seeding recruitment strategies [49, 50].
As with other mountainous hotspots , the CFR was also influenced by local uplift, that occurred during the Miocene [51, 52]. The high species richness and local endemism of the present day Cape is plausibly a direct result of this uplift: new niches opened, with physical barriers to gene flow between them, creating a stimulus for allopatric speciation . Topographical complexity also creates local temperature and moisture gradients , and the patchwork of soils derived from the different lithologies of the Cape [54, 55] adds a further dimension to the resulting fine-scaled mosaic of habitats. By contrast to regions of the Northern Hemisphere, the Cape was buffered from the extremes of Pleistocene glacial cycles, and by implication from resulting extinction ; instead (less extreme) shifts in multiple local-scale ecological gradients, acting in concert, might actually drive speciation . Key innovations in particular groups are also often mooted, such as adaptations to specialised pollinator interactions  that might reinforce speciation . The numerous apparent shifts in pollination syndrome in Erica and the higher diversity of different syndromes in Erica in the Cape than elsewhere  make the latter a tempting explanation for the acceleration of the Cape Erica radiation.
However, meta-analyses of Cape phylogenies have provided support for multiple such hypotheses, with evidence for both ecological and/or pollinator shifts  and distributional and phenological shifts  in e.g. Muraltia, Cape Restionaceae and Pentameris; each of these and others too (such as edaphic shifts apparent in Babiana (Iridaceae) ) may have played a role. Given the results presented here, it is also plausible that (combinations of) factors specific to the most species-rich SW region may be responsible for the highest rates of diversification within the CFR. The relative contribution of these different factors overall is still hotly debated, and with a phylogenetic hypothesis for the clade now available, Cape Erica offers the greatest single source of data for further testing their importance in the assemblage of the flora.
In two contrasting perspectives, the CFR is interpreted as a ‘museum’ of diversity , with persistence of pre-Miocene lineages  and lower extinction e.g. compared to the Mediterranean ; or the evolutionary ‘hot-bed’ of (recent) radiations [32, 39, 65, 66]. These models are not mutually exclusive [39, 67]. However, our results further weigh the balance in favour of the latter. The largest Cape clade, Erica, represents more species than included in most meta-analyses of Cape clades performed to date. Much of this remarkable diversity originated within the last few million years.
We thank F.P.D. Cotterill, T. van der Niet and J.W. Kadereit for comments on drafts of the paper; D. Franke for assistance with graphics; J. Fagúndez, A. Hitchcock, R. Turner, M. Muasya, C. Stirton, R. Clark, B. Bytebier, M. Pimentel, F. Ojeda, C. Merry, and many others for providing samples; and Cape Nature and South Africa National Parks for assistance with permits. The authors gratefully acknowledge the computing time granted on the supercomputer Mogon at Johannes Gutenberg University Mainz (https://hpc.uni-mainz.de/).
South African National Research Foundation (NRF; DUB and MDP); a postdoctoral fellowship from the Claude Leon Foundation (MDP); DFG (PI1169/1-1 to MDP); and the Ministerium für Klimaschutz, Umwelt, Landwirtschaft, Natur- und Verbraucherschutz des Landes Nordrhein-Westfalen, the Faculty of Agriculture Lehr- und Forschungsschwerpunkt „Umweltverträgliche und Standortgerechte Landwirtschaft“, Bonn University; and the Landgard foundation (AMK). Any opinion, finding and conclusion or recommendation expressed in this material is that of the authors and the NRF does not accept liability in this regard.
Availability of data and material
DNA sequence data presented here will be available on publication from Genbank (accession numbers KU831550-KU833209 and KU863006-KU863021) and matrices and phylogenetic trees from TreeBase (study accession URL: http://purl.org/phylo/treebase/phylows/study/TB2:S18291).
DUB, MDP & EGHO planned and designed the research; EGHO, MDP, BG and DUB conducted fieldwork; EGHO identified specimens; NLM, AMK, & MDP: performed lab work; MDP & MK: analysed data; and MDP led the writing (to which all authors contributed). All authors read and approved the final manuscript.
MDP & BG are research associates/lecturers, and MK received her PhD (2015), at the Johannes Gutenberg-Universität, Mainz, Germany; MDP and EGHO are honorary research Associates, NLM PhD student, and DUB full professor, at the University of Stellenbosch, South Africa; and AMK received her PhD (2013) at the University of Bonn, Germany.
The authors declare that they have no competing interests.
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