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Quantitative analysis of the ecological dominance of benthic disaster taxa in the aftermath of the end-Permian mass extinction

Published online by Cambridge University Press:  28 April 2016

Elizabeth Petsios  and
David J. Bottjer
Elizabeth Petsios
Affiliation:
Department of Earth Sciences, University of Southern California, 3651Trousdale Parkway, Los Angeles, California 90089-0740, U.S.A. E-mail: [email protected], [email protected]
David J. Bottjer
Affiliation:
Department of Earth Sciences, University of Southern California, 3651Trousdale Parkway, Los Angeles, California 90089-0740, U.S.A. E-mail: [email protected], [email protected]
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Abstract

The end-Permian mass extinction, the largest extinction of the Phanerozoic, led to a severe reduction in both taxonomic richness and ecological complexity of marine communities, eventually culminating in a dramatic ecological restructuring of communities. During the Early Triassic recovery interval, disaster taxa proliferated and numerically dominated many marine benthic invertebrate assemblages. These disaster taxa include the bivalve genera Claraia, Unionites, Eumorphotis, and Promyalina, and the inarticulate brachiopod Lingularia. The exact nature and extent of their dominance remains uncertain. Here, a quantitative analysis of the dominance of these taxa within the fossil communities of Panthalassa and Tethys benthic realms is undertaken for the stages of the Early Triassic to examine temporal and regional changes in disaster-taxon dominance as recovery progresses. Community dominance and disaster-taxon abundance is markedly different between Panthalassic and Tethyan communities. In Panthalassa, community evenness is low in the Induan stage but increases significantly in the Smithian and Spathian. This is coincident with a significant decrease in the relative abundance and occurrence frequency of the disaster taxa, most notably of the low-oxygen-affinity taxa Claraia and Lingularia. While the disaster taxa are present in post-Induan assemblages, other taxa, including two articulate brachiopod genera, outrank the disaster taxa in relative abundance. In the Tethys, assemblages are generally more even than contemporaneous Panthalassic assemblages. We observe an averaged trend toward more even communities with fewer disaster taxa in both Panthalassic and Tethyan assemblages over time.

Type
Articles
Information
Paleobiology , Volume 42 , Issue 3 , August 2016 , pp. 380 - 393
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Copyright © 2016 The Paleontological Society. All rights reserved 

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References

Literature Cited

Aberhan, M., and Baumiller, T. K.. 2003. Selective extinction among Early Jurassic bivalves: a consequence of anoxia. Geology 31:1077–1080.Google Scholar
Algeo, T. J., Chen, Z. Q., Fraiser, M. L., and Twitchett, R. J.. 2011. Terrestrial–marine teleconnections in the collapse and rebuilding of Early Triassic marine ecosystems. Palaeogeography, Palaeoclimatology, Palaeoecology 308:1–11.Google Scholar
Allison, P. A., Wignall, P. B., and Brett, C. E.. 1995. Palaeo-oxygenation: effects and recognition. Geological Society of London Special Publication 83:97–112.Google Scholar
Alroy, J., Aberhan, M., Bottjer, D. J., Foote, M., Fürsich, F. T., Harries, P. J., Hendy, A. J., Holland, S. M., Ivany, L. C., and Kiessling, W.. 2008. Phanerozoic trends in the global diversity of marine invertebrates. Science 321:97–100.Google Scholar
Bailey, J. V., Corsetti, F. A., Bottjer, D. J., and Marenco, K. N.. 2006. Microbially-mediated environmental influences on metazoan colonization of matground ecosystems: evidence from the Lower Cambrian Harkless Formation. Palaios 21:215–226.Google Scholar
Benton, M. J. 2003. When life nearly died: the greatest mass extinction of all time. Thames and Hudson, London.Google Scholar
Boyer, D. L., Bottjer, D. J., and Droser, M. L.. 2004. Ecological signature of Lower Triassic shell beds of the western United States. Palaios 19:372–380.Google Scholar
Brayard, A., Bucher, H., Escarguel, G., Fluteau, F., Bourquin, S., and Galfetti, T.. 2006. The Early Triassic ammonoid recovery: paleoclimatic significance of diversity gradients. Palaeogeography, Palaeoclimatology, Palaeoecology 239:374–395.Google Scholar
Caswell, B. A., and Coe, A. L.. 2013. Primary productivity controls on opportunistic bivalves during Early Jurassic oceanic deoxygenation. Geology 41:1163–1166.Google Scholar
Caswell, B. A., Coe, A. L., and Cohen, A. S.. 2009. New range data for marine invertebrate species across the early Toarcian (Early Jurassic) mass extinction. Journal of the Geological Society 166:859–872.CrossRefGoogle Scholar
Chen, Z.-Q., and Benton, M. J.. 2012. The timing and pattern of biotic recovery following the end-Permian mass extinction. Nature Geoscience 5:375–383.CrossRefGoogle Scholar
Clapham, M. E., Bottjer, D. J., Powers, C. M., Bonuso, N., Fraiser, M. L., Marenco, P. J., Dornbos, S. Q., and Pruss, S. B.. 2006. Assessing the ecological dominance of Phanerozoic marine invertebrates. Palaios 21:431–441.Google Scholar
Craig, G. Y. 1952. A comparative study of the ecology and palaeoecology of Lingula. Transactions of the Edinburgh Geological Society 15:110–120.Google Scholar
Dineen, A. A., Fraiser, M. L., and Sheehan, P. M.. 2014. Quantifying functional diversity in pre-and post-extinction paleocommunities: a test of ecological restructuring after the end-Permian mass extinction. Earth-Science Reviews 136:339–349.Google Scholar
Emig, C. C. 2003. Proof that Lingula (Brachiopoda) is not a living-fossil, and emended diagnoses of the Family Lingulidae. Carnets de Géologie/Notebooks on Geology, Maintenon, France, Letter 1.Google Scholar
Ferguson, L. 1963. The paleoecology of Lingula squamiformis Phillips during a Scottish Mississippian marine transgression. Journal of Paleontology 37:669–681.Google Scholar
Fischer, A. G., and Arthur, M. A.. 1977. Secular variations in the pelagic realm. SEPM Special Publications 25:19–50.Google Scholar
Foster, W. J., and Twitchett, R. J.. 2014. Functional diversity of marine ecosystems after the Late Permian mass extinction event. Nature Geoscience 7:233–238.Google Scholar
Fraiser, M. L., and Bottjer, D. J.. 2007. When bivalves took over the world. Paleobiology 33:397–413.Google Scholar
Grasby, S., Beauchamp, B., Embry, A., and Sanei, H.. 2013. Recurrent Early Triassic ocean anoxia. Geology 41:175–178.Google Scholar
Greene, S. E., Bottjer, D. J., Hagdorn, H., and Zonneveld, J.-P.. 2011. The Mesozoic return of Paleozoic faunal constituents: a decoupling of taxonomic and ecological dominance during the recovery from the end-Permian mass extinction. Palaeogeography, Palaeoclimatology, Palaeoecology 308:224–232.Google Scholar
Hallam, A., and Wignall, P. B.. 1997. Mass extinctions and their aftermath. Oxford University Press, Oxford, U.K.Google Scholar
Hammen, C. S., Hanlon, D. P., and Lum, S. C.. 1962. Oxidative metabolism of Lingula. Comparative Biochemistry and Physiology 5:185–191.Google Scholar
Hammer, Ø., and Harper, D. A.. 2008. Paleontological data analysis. Blackwell, Malden, Mass.Google Scholar
Hammer, Ø., Harper, D., and Ryan, P.. 2009. PAST (PAlaeontological STatistics), Version 1.89. University of Oslo, Oslo, Norway.Google Scholar
Harries, P. J., Kauffman, E. G., and Hansen, T. A.. 1996. Models for biotic survival following mass extinction. Geological Society of London Special Publication 102:41–60.Google Scholar
Hautmann, M., Smith, A. B., McGowan, A. J., and Bucher, H.. 2013. Bivalves from the Olenekian (Early Triassic) of southwestern Utah: systematics and evolutionary significance. Journal of Systematic Palaeontology 11:263–293.Google Scholar
Hillebrand, H., Bennett, D. M., and Cadotte, M. W.. 2008. Consequences of dominance: a review of evenness effects on local and regional ecosystem processes. Ecology 89:1510–1520.Google Scholar
Hofmann, R., Goudemand, N., Wasmer, M., Bucher, H., and Hautmann, M.. 2011. New trace fossil evidence for an early recovery signal in the aftermath of the end-Permian mass extinction. Palaeogeography, Palaeoclimatology, Palaeoecology 310:216–226.Google Scholar
Hofmann, R., Hautmann, M., and Bucher, H.. 2013a. A new paleoecological look at the Dinwoody Formation (Lower Triassic, Western USA): intrinsic versus extrinsic controls on ecosystem recovery after the end-Permian mass extinction. Journal of Paleontology 87:854–880.Google Scholar
Hofmann, R., Hautmann, M., Wasmer, M., and Bucher, H.. 2013b. Palaeoecology of the Spathian Virgin Formation (Utah, USA) and its implications for the Early Triassic recovery. Acta Palaeontologica Polonica 58:149–173.Google Scholar
Hofmann, R., Hautmann, M., Brayard, A., Nützel, A., Bylund, K. G., Jenks, J. F., Vennin, E., Olivier, N., and Bucher, H.. 2014. Recovery of benthic marine communities from the end-Permian mass extinction at the low latitudes of eastern Panthalassa. Palaeontology 57:547–589.Google Scholar
Joachimski, M. M., Lai, X., Shen, S., Jiang, H., Luo, G., Chen, B., Chen, J., and Sun, Y.. 2012. Climate warming in the latest Permian and the Permian–Triassic mass extinction. Geology 40:195–198.Google Scholar
Kashiyama, Y., and Oji, T.. 2004. Low-diversity shallow marine benthic fauna from the Smithian of northeast Japan: paleoecologic and paleobiogeographic implications. Paleontological Research 8:199–218.Google Scholar
Kauffman, E. G., and Harries, P. J.. 1996. The importance of crisis progenitors in recovery from mass extinction. Geological Society of London, Special Publication 102:15–39.Google Scholar
Kidwell, S. M. 2002. Time-averaged molluscan death assemblages: palimpsests of richness, snapshots of abundance. Geology 30:803–806.Google Scholar
Kidwell, S. M., and Flessa, K. W.. 1995. The quality of the fossil record: populations, species, and communities. Annual Review of Ecology and Systematics 26:269–299.Google Scholar
Komatsu, T., Huyen, D. T., and Jin-Hua, C.. 2008. Lower Triassic bivalve assemblages after the end-Permian mass extinction in South China and North Vietnam. Paleontological Research 12:119–128.Google Scholar
Magurran, A. E. 2004. Measuring biological diversity. African Journal of Aquatic Science 29:285–286.Google Scholar
McGowan, A., Smith, A., and Taylor, P.. 2009. Faunal diversity, heterogeneity and body size in the Early Triassic: testing post-extinction paradigms in the Virgin Limestone of Utah, USA. Australian Journal of Earth Sciences 56:859–872.Google Scholar
McRoberts, C. A. 2000. Paleobiology of the Triassic “flat clam” Halobia in oxygen-deficient marine facies. Geological Society of America, Abstracts with Programs (Northeastern Section) 33:8.Google Scholar
McRoberts, C. A., and Newell, N. D.. 2005. Marine Myalinidae (Bivalvia: Pterioida) from the Permian of West Texas. American Museum Novitates 469:1–15.Google Scholar
Orchard, M. J. 2007. Conodont diversity and evolution through the latest Permian and Early Triassic upheavals. Palaeogeography, Palaeoclimatology, Palaeoecology 252:93–117.Google Scholar
Paleobiology Database 2014. www.paleobiodb.org, accessed 29 October 2014.Google Scholar
Payne, J. L., Lehrmann, D. J., Wei, J., and Knoll, A. H.. 2006. The pattern and timing of biotic recovery from the end-Permian extinction on the Great Bank of Guizhou, Guizhou Province, China. Palaios 21:63–85.Google Scholar
Peng, Y., Shi, G. R., Gao, Y., He, W., and Shen, S.. 2007. How and why did the Lingulidae (Brachiopoda) not only survive the end-Permian mass extinction but also thrive in its aftermath? Palaeogeography, Palaeoclimatology, Palaeoecology 252:118–131.Google Scholar
Pietsch, C. 2015. Ecological recovery dynamics of the benthic and pelagic fauna in response to extreme temperature events and low oxygen environments developed during the Early Triassic. Ph.D. Dissertation. University of Southern California, Los Angeles.Google Scholar
Pietsch, C., and Bottjer, D. J.. 2014. The importance of oxygen for the disparate recovery patterns of the benthic macrofauna in the Early Triassic. Earth-Science Reviews 137:65–84.Google Scholar
Pietsch, C., Mata, S. A., and Bottjer, D. J.. 2014. High temperature and low oxygen perturbations drive contrasting benthic recovery dynamics following the end-Permian mass extinction. Palaeogeography, Palaeoclimatology, Palaeoecology 399:98–113.Google Scholar
Posenato, R. 2008. Patterns of bivalve biodiversity from Early to Middle Triassic in the Southern Alps (Italy): regional vs. global events. Palaeogeography, Palaeoclimatology, Palaeoecology 261:145–159.Google Scholar
Posenato, R., Holmer, L. E., and Prinoth, H.. 2014. Adaptive strategies and environmental significance of lingulid brachiopods across the late Permian extinction. Palaeogeography, Palaeoclimatology, Palaeoecology 399:373–384.Google Scholar
Pruss, S. B., and Bottjer, D. J.. 2004. Early Triassic trace fossils of the western United States and their implications for prolonged environmental stress from the end-Permian mass extinction. Palaios 19:551–564.Google Scholar
Raup, D. M. 1979. Size of the Permo-Triassic bottleneck and its evolutionary implications. Science 206:217–218.CrossRefGoogle ScholarPubMed
Rodland, D. L., and Bottjer, D. J.. 2001. Biotic recovery from the end-Permian mass extinction: behavior of the inarticulate brachiopod Lingula as a disaster taxon. Palaios 16:95–101.Google Scholar
Romano, C., Goudemand, N., Vennemann, T. W., Ware, D., Schneebeli-Hermann, E., Hochuli, P. A., Brühwiler, T., Brinkmann, W., and Bucher, H.. 2013. Climatic and biotic upheavals following the end-Permian mass extinction. Nature Geoscience 6:57–60.Google Scholar
Schubert, J. K., and Bottjer, D. J.. 1995. Aftermath of the Permian–Triassic mass extinction event: paleoecology of Lower Triassic carbonates in the western USA. Palaeogeography, Palaeoclimatology, Palaeoecology 116:1–39.Google Scholar
Scotese, C. R. 2001. Atlas of Earth History. PALEOMAP Project, Arlington, Tex.Google Scholar
Shumway, S. E. 1982. Oxygen consumption in brachiopods and the possible role of punctae. Journal of Experimental Marine Biology and Ecology 58:207–220.Google Scholar
Song, H., Wignall, P. B., Chen, Z.Q., Tong, J., Bond, D. P., Lai, X., Zhao, X., Jiang, H., Yan, C., and Niu, Z.. 2011. Recovery tempo and pattern of marine ecosystems after the end-Permian mass extinction. Geology 39:739–742.Google Scholar
Song, H., Wignall, P. B., Chu, D., Tong, J., Sun, Y., Song, H., He, W., and Tian, L.. 2014. Anoxia/high temperature double whammy during the Permian–Triassic marine crisis and its aftermath. Scientific Reports 4:4132. doi:10.1038/srep04132Google Scholar
Stanley, S. M. 2009. Evidence from ammonoids and conodonts for multiple Early Triassic mass extinctions. Proceedings of the National Academy of Sciences 106:15264–15267.Google Scholar
Sun, Y., Joachimski, M. M., Wignall, P. B., Yan, C., Chen, Y., Jiang, H., Wang, L., and Lai, X.. 2012. Lethally hot temperatures during the Early Triassic greenhouse. Science 338:366–370.Google Scholar
Tozer, E. T. 1961. The sequence of marine Triassic faunas in western Canada. Department of Mines and Technical Surveys, Canada.Google Scholar
Twitchett, R., Krystyn, L., Baud, A., Wheeley, J., and Richoz, S.. 2004. Rapid marine recovery after the end-Permian mass extinction event in the absence of marine anoxia. Geology 32:805–808.Google Scholar
Van Iten, H., Tollerton, V. P., Ver Straeten, C. A., De Moraes Leme, J., Simoes, M. G., and Rodrigues, S. C.. 2013. Life mode of in situ Conularia in a Middle Devonian epibole. Palaeontology 56:29–48.Google Scholar
Wei, H., Shen, J., Schoepfer, S. D., Krystyn, L., Richoz, S., and Algeo, T. J.. 2014. Environmental controls on marine ecosystem recovery following mass extinctions, with an example from the Early Triassic. Earth-Science Reviews 149:108–135.Google Scholar
Wignall, P.. 1993. Distinguishing between oxygen and substrate control in fossil benthic assemblages. Journal of the Geological Society 150:193–196.Google Scholar
Wignall, P., and Hallam, A.. 1993. Griesbachian (Earliest Triassic) palaeoenvironmental changes in the Salt Range, Pakistan and southeast China and their bearing on the Permo-Triassic mass extinction. Palaeogeography, Palaeoclimatology, Palaeoecology 102:215–237.Google Scholar
Worcester, W. S. 1969. Some aspects of the ecology of Lingula (Brachiopoda) in Kaneohe Bay, Hawaii. University of Hawai’i, Honolulu, Hawaii.Google Scholar
Yin, H. 1981. Palaeogeographical and stratigraphical distribution of the Lower Triassic Claraia and Eumorphotis (Bivalvia). Acta Geologica Sinica 3:161–169.Google Scholar
Zonneveld, J.-P., Beatty, T. W., and Pemberton, S. G.. 2007. Lingulide brachiopods and the trace fossil Lingulichnus from the Triassic of western Canada: implications for faunal recovery after the end-Permian mass extinction. Palaios 22:74–97.Google Scholar