Traditionally, the origin and evolution of modern arthropod body plans has been revealed through increasing levels of appendage specialisation exhibited by Cambrian euarthropods. Here we show significant variation in limb morphologies and patterns of limb-tagmosis among three early Cambrian arthropod species conventionally assigned to the Bradoriida. These arthropods are recovered as a monophyletic stem-euarthropod group (and sister taxon to crown-group euarthropods, i.e. Chelicerata, Mandibulata and their extinct relatives), thus implying a radiation of stem-euarthropods where trends towards increasing appendage specialisation were explored convergently with other euarthropod groups. The alternative solution, where bradoriids are polyphyletic, representing several independent origins of a small, bivalved body plan in lineages from diverse regions of the euarthropod and mandibulate stems, is only marginally less parsimonious. The new data reveal a previously unknown disparity of body plans in stem-euarthropods and both solutions support remarkable evolutionary convergence, either of fundamental body plans or appendage specialization patterns.
The bivalved bradoriid euarthropods are a prolific and geographically widespread group in Cambrian to Lower Ordovician strata worldwide1. They are reported as the most abundant euarthropods in the Burgess Shale and Chengjiang Lagerstätten1,2 and clearly formed an important component of Cambrian marine benthic and nektobenthic communities. Most bradoriid species are known only from their carapace. Based solely on the observation that bradoriids are small and have a bivalved carapace (adults typically range up to about 5 mm long), more or less all such fossils in the Cambrian and Lower Ordovician have traditionally been assigned to the Bradoriida, and formerly they were, ipso facto, regarded as the earliest evidence of ostracod crustaceans (Archaeocopida3). Previous analyses of incomplete soft anatomies from two bradoriid species from the exceptionally preserved Chengjiang biota of Yunnan Province, China, namely Kunmingella douvillei (Mansuy, 1912)4 and Kunyangella cheni (Huo, 1965)5, recovered a monophyletic Bradoriida as stem-crustaceans6 or as the sister group to total group Mandibulata7. Here we describe new material of three bradoriid taxa, K. douvillei, K. cheni and Indiana sp., from the Chengjiang biota. As revealed by micro-computed tomographic (micro-CT) scanning, these bradoriids preserve unprecedented three-dimensional (3-D) detail of their soft anatomy revealing hitherto unknown and marked morphological differences in limb anatomy between the species. This fundamentally poses the question of whether the Bradoriida is a non-monophyletic group. Alternatively, they may be a monophyletic group but one that represents an independent radiation of stem-euarthropods where trends towards increasing appendage specialisation were developed convergently with other groups.
Micro-CT analysis of soft anatomy
Using micro-CT scanning, we herein reveal remarkable details of soft anatomy that demonstrate that bradoriids constitute an assemblage of highly disparate euarthropods with substantially more diverse limb morphologies than previously known (Figs. 1–3, Supplementary notes). Thus K. douvillei exhibits 12 appendages with a distinction between an anterior set of 4 post-antennular appendages with double rows of endites and a posterior set of five appendages with single rows of endites, as well as distinct anterior-most and posterior-most uniramous appendages (Figs. 1 and 3). K. cheni has a succession of four head appendages that are each distinct from one another, followed by nine trunk appendages, the posterior-most appendage being uniramous (Figs. 2, 3). Indiana sp., however, possesses a morphologically distinct antenna followed by a homonomous series of 11 uniramous appendages (Figs. 2 and 3). Our interpretations of the anatomy of the bradoriid appendages are taphonomically informed, with effects of decay distinguishable from primary absence of features (see Supplementary Fig. 1).
To test whether bradoriids represent a polyphyletic or monophyletic group, we conducted a cladistic analysis of K. douvillei, K. cheni and Indiana sp. using the phylogenetic database of Siveter et al.8 (Fig. 4), which has the taxonomic coverage necessary. In the most parsimonious solution, the three bradoriid taxa consistently formed a monophyletic clade as sister taxon to crown-group euarthropods (Chelicerata, Mandibulata and their extinct relatives). This contrasts with previous analysis of this data set, which found Bradoriida to be stem-mandibulates7 or stem-crustaceans6. A monophyletic Bradoriida as recovered in our analysis implies extensive character evolution within the group that is convergent on trends seen elsewhere in the euarthropod tree. To explore the full implications of this result, we conducted a survey of limb differentiation along the body (sensu9), which provides a comparative measure of specialisation along the appendage series, without requiring knowledge of appendage homologies10,11. Indiana sp. exhibits an extremely low degree of limb specialisation with a limb formula of (1,11), i.e. a morphologically distinct antenna followed by a homonomous series of 11 appendages. This degree of limb differentiation is otherwise restricted to certain lobopodians, anomalocaridids and ‘short-great appendage’ arthropods (see ref. 11). In contrast, K. douvillei exhibits a distinction between an anterior set of appendages with double rows of endites and a posterior set with single rows, as well as distinct anterior-most and posterior-most uniramous appendages, i.e. a limb formula of (1,4,5,1,1), with no obvious correspondence in other euarthropods. K. cheni is different again, with a succession of four head appendages that are distinct from one another, giving a limb formula of (1,1,1,1,8,1), more similar to mandibulates (i.e. modern pancrustaceans plus various Cambrian ‘Orsten’ taxa).
Traditionally, increasing levels of appendage specialisation have been associated with the establishment of crown-group euarthropod body plans, particularly in Pancrustacea/Mandibulata12,13. Recently, fossil evidence has demonstrated unanticipated levels of appendage specialisation and body tagmosis in the euarthropod stem, including among lobopodians11. In this sense, bradoriids could add to a picture of complex transitions (experimentation) in stem-group euarthropod body plans. To test the alternative hypothesis, that bradoriids are not monophyletic and limb transitions were fewer, we ran a constrained parsimony phylogenetic analysis to minimise the multiple appendage specialisations required by the bradoriids (i.e. Indiana sp. constrained to a position on the euarthropod stem closer to the root than Fuxianhuia; K. cheni constrained to have a position within the mandibulates closer to crustaceans than Marrella; and K. douvillei left unconstrained). Bayesian analyses to evaluate alternative topologies were not possible given the lack of convergence in this data set. In our constrained parsimony analysis (unfigured), Indiana sp. resolved with other bivalved stem-euarthropods (such as Nereocaris and Odaraia) and K. cheni resolved within crustaceans, while K. douvillei variously resolved with either of the other bradoriid taxa or between them. The most parsimonious constrained trees were only marginally less parsimonious than the unconstrained trees (lengths of 141.99 and 141.16, respectively), meaning it is not possible to rule out this alternative on the basis of the available data. In this polyphyletic scenario, bradoriids would represent several independent origins of a small, bivalved body plan in lineages from diverse regions of the euarthropod and mandibulate stems and an astounding case of convergence from disparate origins.
Whichever of our two hypotheses is correct, it is now clear that a miniaturised, bivalved body form arose early on in arthropod evolution, among stem-euarthropods with comparatively unspecialised limbs (particularly so in Indiana sp.). At the same time, other stem-euarthropods (notably Isoxys) were exploring macroscopic bivalved body forms. Both required extreme modification from the plesiomorphic arthropod body plan, and both were rediscovered by comparatively derived mandibulates (phosphatocopines, phyllocarids, some branchiopods and ostracods). Bradoriids therefore add to a picture of early innovation combined with complex transitions in stem-euarthropod body plans.
The bradoriids were collected from the Yu’anshan Member, Chiungchussu Formation, Eoredlichia-Wutingaspis trilobite biozone, Cambrian Series 2, Stage 3, Yunnan Province, China. Two specimens of K. douvillei (YKLP 16233, YKLP 16235) were collected from Mafang, Haikou, Kunming; one specimen of K. cheni (YKLP 16232) is preserved on the same rock slab with K. douvillei YKLP 16233. A second K. cheni (YKLP 16236) was collected from Erjie, Jinning, Kunming. The specimen of Indiana sp. (YKLP 16231) was collected from Mt. Jianshan, Haikou. All specimens are from event beds14. The bradoriids are laterally compressed but with a degree of 3-dimensionality (valve thickness up to about 90 μm, overall compacted thickness of the animals up to about 410 μm) which has been emphasised in our figures by using stereo-photography with a tilt angle of 20° (Figs. 1 and 2). The appendages of any one specimen show different degrees of compression (e.g. K. cheni YKLP 16232, Supplementary Fig. 1), although none of the appendages are as systematically compressed as those fossils preserved as black carbon films in the so-called background beds of the Chengjiang Lagerstätte14. The mineralogical composition of the fossils is similar to that previously reported for Chengjiang specimens15,16,17. Iron oxides pseudomorphing framboidal or microcrystalline pyrite coat the fossil surface, resulting in a high-density contrast between fossil and matrix and facilitating micro-CT imaging. The preservation of an organic film, also known from Chengjiang fossils, cannot be resolved through micro-CT imaging owing to a lack of density contrast between organic film and matrix and/or that the organic film is too thin to be distinguished. However, scanning electron microscopy energy-dispersive X-ray analysis (K. cheni YKLP 16232) has revealed a very weak carbon signal in some areas.
Fossil structures that are exposed on the surface of the rock slabs were imaged with a Leica M205C stereo-microscope.
Fossil structures unexposed, within the slabs, were scanned using a Zeiss Xradia 520 Versa X-ray Microscope (used for YKLP 16231, YKLP 16235 and YKLP 16236) and a GE Phoenix Nanotom M X-ray scanner (used for YKLP 16232 and YKLP 16233). The two instruments produced comparable results. Scanning resolution ranged from 3.0 to 6.1 μm, depending on the size of the scanned region and the slab. The data from each specimen, in the form of a series of TIFF images (one to a few thousand in number), representing cross-sections through different parts of the slab, were processed with the Drishti (Versions 2.4 and 2.6.4) software to generate 3-D models of the fossils figured herein (Figs. 1 and 2, Supplementary Fig. 1).
Phylogenetic analysis utilised the database of Siveter et al.8. We have revised the character codings for K. cheni and K. douvillei in light of our new data and have added Indiana sp. Furthermore, character 23 (bivalved carapace) was revised so as to be contingent on the presence of a free head shield (character 22; for an explanation of this character, see also ref. 18, characters 25 and 26). The data set was analysed using parsimony analysis with implied weighting (k = 3, following ref. 7).
Further information on research design is available in the Nature Research Reporting Summary linked to this article.
Data are available from the authors on request. Fossil specimens are deposited at the Yunnan Key Laboratory for Palaeobiology (YKLP), Yunnan University, China, with the accession numbers: YKLP 16231, 16232, 16233, 16235, 16236. For the phylogenetic analysis depicted in Fig. 4, the data matrix and associated search commands are available via MorphoBank, project 3499 (http://morphobank.org/permalink/?P3499).
Williams, M., Siveter, D. J., Popov, L. E. & Vannier, J. M. C. Biogeography and affinities of the bradoriid arthropods: cosmopolitan microbenthos of the Cambrian seas. Palaeogeography Palaeoclimatol. Palaeoecol. 248, 202–232 (2007).
Hou, X., Siveter, D. J., Williams, M. & Feng, X. A monograph of bradoriid arthropods from the Lower Cambrian of SW China. Trans. R. Soc. Edinb. Earth Sci. 92, 347–409 (2002). (for 2001).
Sylvester-Bradley, P. C. in Treatise on Invertebrate Paleontology Part Q, Arthropoda 3, Crustacea, Ostracoda (eds Moore, R. C. & Pitrat, C. W.) Q100–Q103 (Geological Society of America and University of Kansas Press, Boulder, CO, 1961).
Mansuy, H. in Etude Géologique du Yun-Nan Oriental. Mémoires du Service Géologquie de l’Indochine (eds Deprat, J. & Mansuy, H.) 146 pp, 7 pls (Imprimerie d'Extreme-Orient, 1912).
Huo, S. Additional notes on Lower Cambrian Archaeostraca from Shensi and Yunnan. Acta Palaeontol. Sin. 13, 291–307 (1965).
Hou, X., Williams, M., Siveter, D. J., Aldridge, R. J. & Sansom, R. S. Soft-part anatomy of the Early Cambrian bivalved arthropods Kunyangella and Kunmingella: significance for the phylogenetic relationships of Bradoriida. Proc. R. Soc. B 277, 1835–1841 (2010).
Legg, D., Sutton, M. D. & Edgecombe, G. Arthropod fossil data increase congruence of morphological and molecular phylogenies. Nat. Commun. 4, 2485 (2013).
Siveter, D. J., Briggs, D. E. G., Siveter, D. J., Sutton, M. D. & Legg, D. A new crustacean from the Herefordshire (Silurian) Lagerstätte, UK, and its significance in malacostracan evolution. Proc. R. Soc. B 284, 2017029 (2017).
Cisne, J. L. Evolution of world fauna of aquatic free-living arthropods. Evolution 28, 337–366 (1974).
Adamowicz, S. J., Purvis, A. & Wills, M. A. Increasing morphological complexity in multiple parallel lineages of the Crustacea. Proc. Natl Acad. Sci. USA 105, 4786–4791 (2008).
Yang., J. et al. A superarmored lobopodian from the Cambrian of China and early disparity in the evolution of Onychophora. Proc. Natl Acad. Sci. USA 112, 8678–8683 (2015).
Lankester, E. R. The structure and classification of Arthropoda. Q. J. Microsc. Sci. 47, 523–582 (1904).
Waloszek, D. Cambrian ‘Orsten’-type preserved arthropods and the phylogeny of Crustacea. The new Panorama of animal evolution. In Proc. 18th International Congress on Zoology (eds Legakis, A. et al.) 69–87 (Pensoft Publishers, Sofia, Moscow, 2003).
Hou, X. et al. The Cambrian Fossils of Chengjiang, China: The Flowering of Early Animal Life 2nd edn (Wiley Blackwell, Oxford, 2017).
Gabbott, S. E., Hou, X., Norry, M. J. & Siveter, D. J. Preservation of early Cambrian animals of the Chengjiang biota. Geology 32, 901–904 (2004).
Zhu, M., Babcock, L. E. & Steiner, M. Fossilization modes in the Chengjiang Lagerstätte (Cambrian of China); testing the roles of organic preservation and diagenetic alteration in exceptional preservation. Palaeogeography Palaeoclimatol. Palaeoecol. 220, 31–46 (2005).
Forchielli, A., Steiner, M., Kasbohm, J., Hu, S. & Keupp, H. Taphonomic traits of clay-hosted early Cambrian Burgess Shale-type fossil Lagerstätten in South China. Palaeogeography Palaeoclimatol. Palaeoecol. 398, 59–85 (2014).
Ortega-Hernández, J., Legg, D. A. & Braddy, S. J. The phylogeny of aglaspidid arthropods and the internal relationships within Arthropoda. Cladistics 29, 15–45 (2013).
This study is supported by NSFC grants 41861134032 and 2015HC029 and Yunnan Provincial Research Grants 2018FA025 and 2018IA073. Shaogang Zang, Shuyan Hou, Xiaoyu Yang and Chunjie Cao assisted with micro-CT and SEM analyses. Ajay Limaye (Australian National University), Jing Lu and Yuzhi Hu (Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences) provided guidance with Drishti software. M.W. thanks the Leverhulme Trust for a Research Fellowship (RF-2018-275/4). We are grateful for the constructive comments of the three reviewers. This is publication number 2019002 from the University of Leicester Centre for Palaeobiology Research.
The authors declare no competing interests.
Publisher’s note: Springer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.
About this article
Cite this article
Zhai, D., Williams, M., Siveter, D.J. et al. Variation in appendages in early Cambrian bradoriids reveals a wide range of body plans in stem-euarthropods. Commun Biol 2, 329 (2019). https://doi.org/10.1038/s42003-019-0573-5
Current Biology (2020)
Annual Review of Ecology, Evolution, and Systematics (2020)
Moving legs: A workflow on how to generate a flexible endopod of the 518 million‐year‐old Chengjiang arthropod Ercaicunia multinodosa using 3D ‐kinematics (Cambrian, China)
Microscopy Research and Technique (2020)
Computed tomography sheds new light on the affinities of the enigmatic euarthropod Jianshania furcatus from the early Cambrian Chengjiang biota
BMC Evolutionary Biology (2020)