Skip to main content
Log in

Chief sources of brachiopod recovery from the end Ordovician mass extinction with special references to progenitors

  • Published:
Science in China Series D: Earth Sciences Aims and scope Submit manuscript

Abstract

Survivor, Lazarus and progenitor taxa are sources of biotic recovery following mass extinction. Investigations of the benthic brachiopods through the latest Ordovician mass extinction shows that progenitors developed many evolutionary novelties and successful surviving mechanisms. They are superior to survivors and Lazarus taxa in their ability to adapt to environmental changes. They are the primary source of macroevolution and the ancestors of a number of new taxa. Three kinds of progenitors are recognized based on the Ordovician-Silurian brachiopods from South China: survivor-progenitors, crisis-progenitors and Lazarus-progenitors; the last has the strongest ability to resist adverse environments, and is the most diverse and abundant.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Similar content being viewed by others

References

  1. Boutcot, A. J., Does evolution take place in an ecological vacuum? II,Journal of Paleontology, 1983, 57(1): 1.

    Google Scholar 

  2. Rong Jiayu, Fang Zongjie, Chen Xu et al., Biotic recovery—first episode of evolution after mass extinction,Acta Palaeonto-logica Sinica (in Chinese with English abstract), 1996, 35(3): 259.

    Google Scholar 

  3. Bretsky, P. W., Evolutionary patterns in the Paleozoic bivalvia: documentation and some theoretical considerations,Bulletin Geological Society of America, 1973, 83: 1.

    Google Scholar 

  4. Jablonski, D., Causes and consequences of mass extinctions: a comparative approach, inDynamics of Extinction ((ed. Elliott, D. K.), New York: Wiley, 1986, 183–229.

    Google Scholar 

  5. Kauffman, E. G., Harries, P. J., The importance for crisis progenitors in recovery from mass extinction,Biotic Recovery from Mass Extinction Events (ed. Hart, M. B.), London: Geological Society Special Publication, 1996, 102: 1–392.

    Google Scholar 

  6. Kauffman, E. G., Erwin, D. H., Surviving mass extinction,Geotimes, 1995, 40(3): 14.

    Google Scholar 

  7. Roman, K. S., Early Ashgill Stropheodontacea (brachiopods) from Central Asia,Paleontologcheskii Zhurnal, 1983, 61.

  8. Hiller, H.. Ashgill Brachiopoda from the Glyn Ceiriog District, North Wales,Bulletin of the British Museum (Nutural History), 1980, 34(3): 109.

    Google Scholar 

  9. Rong Jiayu, Distribution of theHirnantia fauna and its meaning,Aspects of the Ordovician System ((ed. Bruton, D. L.), Oslo: Universitetsforlaget, 1984, 101–112.

    Google Scholar 

  10. Rong Jiayu, Harper, D. A. T., A global synthesis of the latest Ordovician Hirnantian brachiopod faunas,Transactions of the Royal Society of Edinburgh:Earth Sciences, 1988, 79: 383.

    Google Scholar 

  11. Rong Jiayu. TheHirnantia fauan of China with comments on the Ordovician-Silurian boundary,Journal of Stratigraphy, 1984, 3(1): 1.

    Google Scholar 

  12. Rong Jiayu, Ecostratigraphy and community analysis of the Late Ordovician and Silurian in Southern China,Selected Papers from the 13 th and 14th Annual Conventions of Palaeontological Society of China (in Chinese with English summary) ((ed. Phnto- logical Socitey of China), Hefei: Anhui Science and Technology Publishing House, 1986, 1–22.

    Google Scholar 

  13. Kauffman, E. G., Harries, P. J., Amodel for survival and recovery after mass extinction,Global Boundary Events, Conference Abstracts, Warsaw: Polish Geological Institute, 1993, 27.

    Google Scholar 

  14. Jin Chuntai, Ye Shaohua, Jiang Xinsheng et al., The Silurian stratigraphy and paleontology in Erlangshan District, Sichuan,Bulletin of Chengdu Institute of Geology and Mineral Resources, Chinese Academy of Geological Sciences (in Chinese with English summary), 1989, 11: 1.

    Google Scholar 

  15. Rong Jiayu, Zhan Renbin, Han Nairen, The oldest knownEospirifer (Brachiopoda) in the Changwu Formation (Late Ordovician) of western Zhejiang, East China, with a review of the earliest spiriferoids,Journal of Paleontology, 1994, 68(4): 763.

    Google Scholar 

  16. Zhan Renbin, Rong Jiayu, Synecology and their distribution pattern of Late Ordovician brachiopods from the Zhejiang-Jiangxi border region, E. China,Chinese Bulletin of Sciences, 1995, 40(5): 932.

    Google Scholar 

  17. Rong Jiayu, Zhan Renbin, Brachidia of late Ordovician and Silurian eospiriferines (Brachiopoda),Palaeontology, 1996, 39(4): 941.

    Google Scholar 

  18. Rong Jiayu, Yang Xuechang, Silurian spiriferoids from Southwest China with special reference to their stratigraphic signiticance,Acta Palaeontologica Sinica (in Chinese with English summary), 1978, 17(4): 357.

    Google Scholar 

  19. Copper, P.,Zygospira and some related Ordovician and Silurian atrypoid brachiopods,Palaeontology, 1977, 20(2): 295.

    Google Scholar 

  20. Rong Jiayu, Yang Xuechang, Middle and late Early Silurian brachiopod faunas in Southwest China,Memoir of Nanjing Institute of Geology and Palaeontology, Academia Sinica (in Chinese with English summary), 1981, 13: 163.

    Google Scholar 

  21. Zeng Qingluan, Liu Yinhuan, Wan Jianping et al., Succession and ecology of brachiopod faunas across Ordovican-Silurian boundary south of eastern Qinling Mountains,Acta Palaeontologica Sinica (in Chinese with English summary), 1993, 32(3): 372.

    Google Scholar 

  22. Xu Hankui, Late Ordovician brachiopods from central part of eastern Qinling region,Acta Palaeontologica Sinka, 1996, 35(5): 544.

    Google Scholar 

  23. Mei Shilong, Biostratigraphy and tectonic implications of late Ordovician conodonts from Shiyanhe Formation, Neixiang, Henan,Acta Palaeontologica Sinica, 1995, 34(6): 674.

    Google Scholar 

  24. Chen Xu, Rong Jiayu, Qiu Jinyu et al., Preliminary investigation of the late Ordovician strata of Zhuzhai in Yushan of Jiangxi, their depositional features and environment,Journal of Stratigraphy, 1987, 11(1): 23.

    Google Scholar 

  25. Zhan Renbin, Cocks, L. R. M., Late Ordovician brachiopods from the South China Plate and their palaeogeographical significance,Special Papers in Palaeontology, 1998, 59: 1.

    Google Scholar 

  26. Zhang Ning, Boucot, A. J., Epitomyonia (Brachiopoda): ecology and functional morphology,Journal of Paleontology, 1988. 62: 753.

    Google Scholar 

  27. Boucot, A. J.,Evolution and Extinction Rate Controls, Amsterdam: Elsevier, 1975.

    Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Additional information

Project supported by the National Natural Science Foundation of China (Grant No. 49672083) and Major Project of the Chinese Academy of Sciences (CAS) (Grant KZ952-51-023).

Rights and permissions

Reprints and permissions

About this article

Cite this article

Rong, J., Zhan, R. Chief sources of brachiopod recovery from the end Ordovician mass extinction with special references to progenitors. Sci. China Ser. D-Earth Sci. 42, 553–560 (1999). https://doi.org/10.1007/BF02875250

Download citation

  • Received:

  • Issue Date:

  • DOI: https://doi.org/10.1007/BF02875250

Keywords

Navigation