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The Luoping Biota: Exceptional Preservation, and New Evidence on the Triassic Recovery from End-Permian Mass Extinction

Overview
Journal Proc Biol Sci
Specialty Biology
Date 2010 Dec 25
PMID 21183583
Citations 25
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Abstract

The timing and nature of biotic recovery from the devastating end-Permian mass extinction (252 Ma) are much debated. New studies in South China suggest that complex marine ecosystems did not become re-established until the middle-late Anisian (Middle Triassic), much later than had been proposed by some. The recently discovered exceptionally preserved Luoping biota from the Anisian Stage of the Middle Triassic, Yunnan Province and southwest China shows this final stage of community assembly on the continental shelf. The fossil assemblage is a mixture of marine animals, including abundant lightly sclerotized arthropods, associated with fishes, marine reptiles, bivalves, gastropods, belemnoids, ammonoids, echinoderms, brachiopods, conodonts and foraminifers, as well as plants and rare arthropods from nearby land. In some ways, the Luoping biota rebuilt the framework of the pre-extinction latest Permian marine ecosystem, but it differed too in profound ways. New trophic levels were introduced, most notably among top predators in the form of the diverse marine reptiles that had no evident analogues in the Late Permian. The Luoping biota is one of the most diverse Triassic marine fossil Lagerstätten in the world, providing a new and early window on recovery and radiation of Triassic marine ecosystems some 10 Myr after the end-Permian mass extinction.

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References
1.
Baumiller T, Salamon M, Gorzelak P, Mooi R, Messing C, Gahn F . Post-Paleozoic crinoid radiation in response to benthic predation preceded the Mesozoic marine revolution. Proc Natl Acad Sci U S A. 2010; 107(13):5893-6. PMC: 2851891. DOI: 10.1073/pnas.0914199107. View

2.
Payne J, Lehrmann D, Wei J, Orchard M, Schrag D, Knoll A . Large perturbations of the carbon cycle during recovery from the end-permian extinction. Science. 2004; 305(5683):506-9. DOI: 10.1126/science.1097023. View

3.
Jablonski D . Lessons from the past: evolutionary impacts of mass extinctions. Proc Natl Acad Sci U S A. 2001; 98(10):5393-8. PMC: 33224. DOI: 10.1073/pnas.101092598. View

4.
Jin Y, Wang Y, Wang W, Shang Q, Cao C, Erwin D . Pattern of marine mass extinction near the Permian-Triassic boundary in South China. Science. 2000; 289(5478):432-6. DOI: 10.1126/science.289.5478.432. View

5.
Benton M, Tverdokhlebov V, Surkov M . Ecosystem remodelling among vertebrates at the Permian-Triassic boundary in Russia. Nature. 2004; 432(7013):97-100. DOI: 10.1038/nature02950. View