Molecular studies suggest that the origin of jawed vertebrates was no later than the Late Ordovician period (around 450 million years ago (Ma))1,2. Together with disarticulated micro-remains of putative chondrichthyans from the Ordovician and early Silurian period3,4,5,6,7,8, these analyses suggest an evolutionary proliferation of jawed vertebrates before, and immediately after, the end-Ordovician mass extinction. However, until now, the earliest complete fossils of jawed fishes for which a detailed reconstruction of their morphology was possible came from late Silurian assemblages (about 425 Ma)9,10,11,12,13. The dearth of articulated, whole-body fossils from before the late Silurian has long rendered the earliest history of jawed vertebrates obscure. Here we report a newly discovered Konservat-Lagerstätte, which is marked by the presence of diverse, well-preserved jawed fishes with complete bodies, from the early Silurian (Telychian age, around 436 Ma) of Chongqing, South China. The dominant species, a ‘placoderm’ or jawed stem gnathostome, which we name Xiushanosteus mirabilis gen. et sp. nov., combines characters from major placoderm subgroups14,15,16,17 and foreshadows the transformation of the skull roof pattern from the placoderm to the osteichthyan condition10. The chondrichthyan Shenacanthus vermiformis gen. et sp. nov. exhibits extensive thoracic armour plates that were previously unknown in this lineage, and include a large median dorsal plate as in placoderms14,15,16, combined with a conventional chondrichthyan bauplan18,19. Together, these species reveal a previously unseen diversification of jawed vertebrates in the early Silurian, and provide detailed insights into the whole-body morphology of the jawed vertebrates of this period.
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All data analysed in this paper, including the phylogenetic datasets, are available as part of the Article, Extended Data Figs. 1–10 or the Supplementary Information. Supplementary Data 1 and 5 are available at Figshare (https://doi.org/10.6084/m9.figshare.20317233.v1). The nomenclature described in this publication has been registered at ZooBank (LSID: urn:lsid:zoobank.org:pub: A85E3402-5F4D-4694-8BB9-90D2D87BB1D7).
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We thank L. Jia, Q. Wang, Q. Wen, Q. Rao, Y. Zhao, R. Zhao, Q. Xue, Z. Xian, Y. Luo, Y. Yan, H. Wang, Q. Deng, J. Xiong, C. H. Xiong, C. Y. Xiong, J. Zhang, Z. Zhou and L. Nie for fieldwork assistance; J. Rong and Y. Wang for discussion on stratrigraphy; J. Xiong, C. H. Xiong and C. Y. Xiong for fossil preparation; X. Liu and L. Jia for assistance with photography and RTI imaging; Y. Hou and P. Yin for computed microtomography scanning; R. Guo for assistance with drawing and producing the figures; and Q. Zheng for the artistic life reconstruction. This work was supported by the Strategic Priority Research Program of Chinese Academy of Sciences (XDA19050102 and XDB26000000), the National Natural Science Foundation of China (42130209, 42022011, 42072026), the One Hundred Talents Projects of CAS (E0CQ010103) and the Mineral Resources Protection and Supervision Projects of Chongqing (YGZ2020-416). P.E.A. acknowledges the support of a Wallenberg Scholarship from the Knut and Alice Wallenberg Foundation.
The authors declare no competing interests.
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Extended data figures and tables
a, Map showing the location of Chongqing Municipality. b, Map of Chongqing Municipality showing the general location of the fossil locality. c, Geological map of the studied region, showing the locations of the three sections. d, Life restoration of fishes and associated biota in the Chongqing Lagerstätte. Art credit: Qiuyang Zheng.
Extended Data Fig. 2 Silurian stratigraphic columns of the three sections in the studied area yielding fish fossils.
a, Yongdong; b, Tianlu; and c, Kapeng.
a, Slab bearing the holotypes of Xiushanosteus mirabilis and Shenacanthus vermiformis. b, Interpretative drawing of a. c, Slab bearing a concentration of galeaspids, Xiushanosteus and undescribed jawed vertebrate fossils. d, Interpretative drawing of b. e, Possible vertebrae preserved alongside a placoderm. f, RTI photograph of a complete phyllocarid crustacean. Numbers on the interpretative drawings: 1, galeaspid fossil; 2, Xiushanosteus fossil; unlabeled, undescribed or unidentifiable jawed vertebrate fossils. Scale bars, a-d, 10 mm; e-f, 5 mm.
a, Ammonium chloride coated photograph of the negative half of the holotype, V300001b. b, Ammonium chloride coated photograph of a partly flattened specimen showing more sutures, V300010b. c, d, Interpretative drawing of a, b. e, Ammonium chloride coated photograph of V300008b, showing the suture between the preorbital and central plates. f, a specimen showing the cheek and operculum plates, V300002b. g, Interpretative drawing of f. For the abbreviations, see Fig. 2. Scale bars, 5 mm.
a, Ammonium chloride coated photograph of V300009a. b, Ammonium chloride coated photograph of V300002a, showing the paired fins, the midline scutes and the squamation. c, Ammonium chloride coated photograph of a complete specimen, V300004, showing the two dorsal and caudal fins. d-f, Interpretative drawings of a-c. g, Ammonium chloride coated photograph of a partly articulated specimen missing the anterior part of the head, V300003. h, Interpretative drawing of g. i, V300011, a specimen showing the posterior dorsal and the caudal fins. For the abbreviations, see Fig. 2. Scale bars, 5 mm.
a-c, Rendering of the holotype V300001a (a), V300007a (b) and V300008a (c) specimens. d-f, Tomographs through the coronal section of the anterior part of above specimens. Not to scale.
a, Xiushanosteus. b, Acanthothoracid Romundina. c, Arthrodire Dicksonosteus. d, Maxillate placoderm Bianchengichthys. e, Sarcopterygian osteichthyan Eusthenopteron. f, Actinopterygian osteichthyan Moythomasia. Not to scale.
Extended Data Fig. 8 Additional photographs and energy dispersive spectroscopy of the S. vermiformis holotype (IVPP V300000).
a, The positive half of the holotype, V300000a. b, the head and pectoral region of a. c, Mapping of the concentration of manganese. d, the negative half of the holotype, V300000b. e, Ammonium chloride coated photograph of V300000a. i-j, enlarged ammonium chloride coated photograph of V300000a, showing details of ornament. Scale bar, 5 mm.
Extended Data Fig. 9 Full cladograms of the phylogenetic analyses showing the phylogenetic positions of Xiushanosteus and Shenacanthus.
a, strict consensus tree of the parsimony result, Numbers above branches denote Bremer decay indices larger than zero. b, majority-rule consensus tree of the Bayesian inference analysis.
a, morphospace based on the two major axes of variation (NMDS1 and NMDS2), with the colours denotes the five gnathostome groups. b, stress plot denoting the fit of the reduced dimensional space (NMDS1 and NMDS2) to the actual multivariate distance.
The Supplementary Information contains seven sections. (1) Geological context of the Chongqing Lagerstätte. (2) Additional descriptions of Xiushanosteus mirabilis. (3) Additional descriptions of Shenacanthus vermiformis. (4) List of taxa, geological time and references. (5) List of characters. (6) Description of Supplementary Data 1–5 and Supplementary Video 1. (7) Supplementary References.
Volume renderings of three Xiushanosteus specimens (the holotype IVPP V300001a, IVPP V300007a and IVPP V300008a) based on computed microtomography data. Accessible at Figshare (https://doi.org/10.6084/m9.figshare.20317233.v1).
Nexus file of the data matrix used in the parsimony and Bayesian phylogenetic analyses.
The strict consensus tree of the 46 most parsimonious trees resulting from the data matrix of Supplementary Data 1 excluding Xiushanosteus and Shenacanthus.
Nexus file of the data matrix used in the morphospace analysis. This data matrix is essentially the same as the one used for the phylogenetic analyses, except that the agnathan taxa were expanded.
Original photographs of the slabs and individual specimens. Accessible at Figshare (https://doi.org/10.6084/m9.figshare.20317233.v1).
The dawn of fishes. A video reconstructing the fauna, environment and possible taphonomy of the early Silurian Chongqing Lagerstätte.
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Zhu, Ya., Li, Q., Lu, J. et al. The oldest complete jawed vertebrates from the early Silurian of China. Nature 609, 954–958 (2022). https://doi.org/10.1038/s41586-022-05136-8