Keywords
palaeobiodiversity
mass extinctions
Middle Devonian
Late Devonian
Mississippian
central Asia
How to Cite
Abstract
Interregional tracing of trends and events in the biotic evolution is an important task of modern palaeobiology. In Soviet times (1917-1991), numerous palaeontological data have collected for the territory of Russia and neighbouring U. S. S. R. countries. Later, these data were compiled and published in a series of reference volumes. Although this information cannot be updated in a conventional way, it remains valuable for quantitative analyses, particularly because of its comprehensive and unique character. Assessment of the previously collected data on the stratigraphic distribution of Middle Devonian-Mississippian marine invertebrates in three regions of central Asia (central Kazakhstan, Uzbekistan and Tajikistan) reveals some general patterns of biodiversity dynamics. The total number of genera generally declined during the Givetian-Famennian, whereas a remarkable diversity peak occurred in the Visean. This is consistent with the global pattern and, thus, permits to hypothesize a regional signature of the global trends. Changes in the extinction rate differ, however, between central Asia and the Earth in its entirety, which may be explained particularly by biases in either the regional or the global records. Evidence of the Givetian and Frasnian/Famennian mass extinctions is found in the three regions under study. Results of this tentative study indicate important directions for further research and suggest that central Asia is a highly important domain for studies of mid-Palaeozoic biodiversity dynamics.
References
Abrajevitch, A., Van der Voo, R., Bazhenov, M. L., Levashova, N. M. & McCausland, P. J. A., 2008. The role of the Kazakhstan orocline in the late Paleozoic amalgamation of Eurasia. Tectonophysics 455, 61-76.
Alroy, J., Aberhan, M., Bottjer, D. J., Foote, M., Fürsich, F. T., Harries, P. J., Hendy, A. J. W., Holland, S. M., Ivany, L. C., Kiessling, W., Kosnik, M. A., Marshall, C. R., McGowan, A. J., Miller, A. I., Olszewski, T. D., Patzkowsky, M. E., Peters, S. E., Viller, L., Wagner, P. J., Bonuso, N., Borkow, P. S., Brenneis, B., Clapham, M. E., Fall, L. M., Ferguson, C. A., Hanson, V. L., Krug, A. Z., Layou, K. M., Leckey, E. H., Nürnberg, S., Powers, C. M., Sessa, J. A., Simpson, C., Tomašových, A. & Visaggi, C. C., 2008. Phanerozoic trends in the global diversity of marine invertebrates. Science 321, 97-100.
Bambach, R. K., 2006. Phanerozoic biodiversity and mass extinctions. Annual Review of Earth and Planetary Sciences 34, 127-155.
Baratov, R. B. (Ed), 1976. Rastchlenenije stratifitsirovannykh i intruzivnykh obrazovanij Tadzhikistana [Subdivision of stratified and intrusive bodies of Tajikistan]. Donish, Dushanbe, 268 pp. (in Russian)
Bazhenov, M. L., Collins, A. Q., Degtyarev, K. E., Levashova, N. M., Mikolaichuk, A. V., Pavlov, V. E. & Van der Voo, R., 2003. Paleozoic northward drift of the North Tien Shan (central Asia) as revealed by Ordovician and Carboniferous palaeomagnetism. Tectonophysics 366, 113-141.
Becker, R. T. & House, M. R., 1994. Kellwasser events and goniatite successions in the Devonian of the Montagne Noire with comments on possible causations. Courier Forschungsinstitut Senckenberg 16, 45-77.
Becker, R. T., House, M. R., Kirchgasser, W. T. & Playford, P. E., 1991. Sedimentary and faunal changes across the Frasnian/Famennian boundary at the Canning Basin of Western Australia. Historical Biology 5, 183-196.
Benton, M. J., 2001. Biodiversity on land and in the sea. Geological Journal 36, 211-230.
Bespalov, V. F. & Kostenko, N. N. (Eds), 1981a. Geologitcheskaja karta Kazakhskoj SSR. Serija turgajsko-mugodzharskaja. Ob'jasnitel'naja zapiska [Geological map of the Kazakh SSR. Turgaj-Mugodzhary Series. Descriptive note]. VSEGEI, Alma-Ata, 228 pp. (in Russian)
Bespalov, V. F. & Kostenko, N. N. (Eds), 1981b. Geologitcheskaja karta Kazakhskoj SSR. Serija juzhnokazakhstanskaja. Ob'jasnitel'naja zapiska [Geological map of the Kazakh SSR. South Kazakhstan Series. Descriptive note]. VSEGEI, Alma-Ata, 324 pp. (in Russian)
Biske, Yu.S. & Seltmann, R. 2010. Paleozoic Tian-Shan as a transitional region between the Rheic and Urals-Turkestan oceans. Gondwana Research 17, 602-613.
Bonelli, R. & Patzkowsky, M. E., 2008. How are global patterns of faunal turnover expressed at regional scales? Evidence from the Upper Mississippian (Chesterian Series), Illinois Basin, USA. Palaios 23, 760-772.
Boucot, A. J., 2006. So-called background extinction rate is a sampling artifact. Palaeoworld 15, 127-134.
Buggisch, W., 1991. The global Frasnian-Famennian Kellwasser event. Geologische Rundschau 80, 49-72.
Buslov, M. M., Watanabe, T., Fujiwara, Y., Iwata, K., Smirnova, L. V., Safonova, I. Yu., Semakov, N. N. & Kiryanova, A. P., 2004. Late Paleozoic faults of the Altai region, central Asia: tectonic pattern and model of formation. Journal of Asian Earth Sciences 23, 655-671.
Caplan, M. L. & Bustin, R. M., 1999. Devonian-Carboniferous Hangenberg mass extinction event, widespread organic-rich mudrock, and anoxia: causes and consequences. Palaeogeography, Palaeoclimatology, Palaeoecology 148, 187-208.
Copper, P., 1977. Paleolatitudes in the Devonian of Brazil and the Frasnian-Famennian extinction event. Palaeogeography, Palaeoclimatology, Palaeoecology 21, 165-207.
Copper, P., 1986. Frasnian-Famennian mass extinction and cold water oceans. Geology 14, 835-839.
Copper, P., 2002. Reef development at the Frasnian/Famennian mass extinction boundary. Palaeogeography, Palaeoclimatology, Palaeoecology 181, 27-65.
Filippova, L. B., Bush, V. A. & Didenko, A. N., 2001. Middle Paleozoic subduction belts: the leading factor in the formation of the central Asian fold-and-thrust belt. Russian Journal of Earth Sciences 3, 405-426.
Grunt, T. A. & Dmitriev, V. Yu., 1973. Permskie brakhiopody Pamira [Permian brachiopods of the Pamirs]. Nauka, Moskva, 212 pp. (in Russian).
Hallam, A. & Wignall, P. B., 1997. Mass extinctions and their aftermath. Oxford University Press, Oxford, 320 pp.
House, M. R., 2002. Strength, timing, setting and cause of mid-Paleozoic extinction. Palaeogeography, Palaeoclimatology, Palaeoecology 181, 5-25.
Jablonski, D., 2008. Extinction and the spatial dynamics of biodiversity. Proceedings of the National Academy of Sciences 105 (Suppl. 1), 11528-11535.
Kalvoda, J., 2002. Late Devonian-Early Carboniferous foraminiferal fauna: zonations, evolutionary events, paleobiogeography and tectonic implications. Folia Facultatis Scientiarum Universitatis Masarykianae Brunensis, Geologia 39, 1-214.
Krug, A. & Patzkowski, M., 2005. Sampling standardized regional diversity and turnover patterns during the Late Ordovician mass extinction. Geological Society of America, Abstracts with Programs 37 (7), 384.
Krug, A. Z. & Patzkowsky, M. E., 2007. Geographic variation in turnover and recovery from the Late Ordovician mass extinction. Paleobiology 33, 435-454.
McGhee, G. R., 1996. The Late Devonian mass extinction - the Frasnian-Famennian crisis. Columbia University Press, New York, 303 pp.
Morozova, I. P., 1970. Mshanki pozdnej permi [Late Permian bryozoans]. Trudy Paleontologitcheskogo instituta AN SSSR 122, 3-332.
Nalivkin, D. V., Rzhonsnitskaja, M. A. & Markovskij, B. P. (Eds), 1973. Stratigrafija SSSR. Devonskaja sistema. Kniga 1 [Stratigraphy of the USSR. Devonian System. Volume 1]. Nedra, Moskva, 520 pp. (in Russian).
Ogg, J. G., Ogg, G. & Gradstein, F. M., 2008. The concise geologic time scale. Cambridge University Press, Cambridge, 177 pp.
Orlov, I. V. & Bespalov, V. F. (Eds), 1981. Geologitcheskaja karta Kazakhskoj SSR. Serija Tsentral'no-Kazakhstanskaja. Ob'jasnitel'naja zapiska [Geological map of the Kazakh SSR. Central Kazakhstan Series. Descriptive note]. VSEGEI, Alma-Ata, 247 pp. (in Russian)
Peters, S. E. & Foote, M., 2001. Biodiversity in the Phanerozoic: a reinterpretation. Paleobiology 27, 583-601.
Purdy, E. G., 2008. Comparison of taxonomic diversity, strontium isotope and sea-level patterns. International Journal of Earth Sciences 97, 651-664.
Racki, G., 2005. Towards understanding Late Devonian global events: few answers, many questions. [In:] D. J. Over, J. R. Morrow & P. B. Wignall (Eds): Understanding Late Devonian and Permian-Triassic biotic and climatic events: towards an integrated approach. Elsevier, Amsterdam, pp. 5-36.
Racki, G., 2009. Wielkie wymierania i ich przyczyny [Great extinctions and their origin]. Kosmos 58, 529-545.
Racki, G., Racka, M., Matyja, H. & Devleeschouwer, X., 2002. The Frasnian/Famennian boundary interval in the South Polish-Moravian shelf basins: integrated event-stratigraphical approach. Palaeogeography, Palaeoclimatology, Palaeoecology 181, 251-297.
Raup, D. W. & Sepkoski, J. J., 1982. Mass extinctions in the marine fossil record. Science 215, 1501-1503.
Ruban, D. A., 2005. Mesozoic marine fossil diversity and mass extinctions: an experience with the middle XIX century paleontological data. Revue de Paléobiologie 24, 287-290.
Ruban, D. A. & Van Loon, A. J., 2008. Possible pitfalls in the procedure for paleobiodiversity-dynamics analysis. Geologos 14, 37-50.
Ruban, D. A., Al-Husseini, M. I. & Iwasaki, Y., 2007. Review of Middle East Paleozoic plate tectonics. GeoArabia 12, 35-56.
Scotese, C. R., 2004. A continental drift flipbook. Journal of Geology 112, 729-741.
Sengör, A. M. C. & Natal'in, B. A., 1996. Paleotectonics of Asia: fragments of a synthesis. [In:] A. Yin & M. Harris (Eds): The tectonic evolution of Asia. Cambridge, University Press, pp. 486-640.
Sepkoski, J. J., 1993. Ten years in the library: new data confirm paleontological patterns. Paleobiology 19, 43-51.
Sepkoski, J. J., 2002. A compendium of fossil marine animal genera. Bulletins of American Paleontology 363, 1-560.
Sepkoski, J. J., Bambach, R. K., Raup, D. M. & Valentine, J. W., 1981. Phanerozoic marine diversity and fossil record. Nature 293, 435-437.
Stampfli, G. M. & Borel, G. D., 2002. A plate tectonic model for the Paleozoic and Mesozoic constrained by dynamic plate boundaries and restored synthetic oceanic isochrons. Earth and Planetary Science Letters 196, 17-33.
Torsvik, T. H. & Cocks, L. R. M., 2004. Earth geography from 400 to 250 Ma: a palaeomagnetic, faunal and facies review. Journal of the Geological Society, London 161, 555-572.
Tuljaganov, Kh.T. & Jaskovitch, B. V., 1980. Geologitcheskaja karta Uzberkskoj SSR [Geological map of Uzbek SSR]. Fan, Tashkent, 200 pp. (in Russian).
Veimarn, A. B., Kuzmin, A. V. & Vorontsova, T. N., 1997. Geologitcheskie sobytija v Kazakhstane na rubezhe franskogo i famenskogo vekov i ikh znatchenie v rjadu global'nykh sobytij etogo vremenii [Geological events in Kazakhstan at the boundary of the Frasnian and the Famennian and their significance within the row of events of the pertinent time]. Bulletin of Moscow Society of Naturalists, Geological Series 72 (4), 35-46. (in Russian).
Wall, P. D., Ivany, L. C. & Wilkinson, B. H., 2009. Revisiting Raup: exploring the influence of outcrop area on diversity in light of modern sample standardization techniques. Paleobiology 35, 146-167.
Walliser, O. H., 1996. Global events in the Devonian and Carboniferous. [In:] O. H. Walliser (Ed): Global events and event stratigraphy in the Phanerozoic. Berlin, Springer, pp. 225-250.
Wang, K., Orth, K. J., Attrep Jr., M., Chatterton, B. D. E., Hou, H. & Geldsetzer, H. H. J., 1991. Geochemical evidence for a catastrophic biotic event at the Frasnian/ Famennian boundary in south China. Geology 19, 776-779.
Zhamojda, A. I. (Ed), 1968. Geologitcheskoje strojenije SSSR. Vol. 1. Stratigrafija [Geological structure of the USSR. Vol. 1. Stratigraphy]. Nedra, Moskva, 709 pp. (in Russian).
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