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• W2079851915 abstract "Abstract Analyses of global biodiversity curves have been important for the interpretation of co‐evolution between organisms and environments through geological time. Global curves can be better understood if all the data collected from a multitude of palaeocontinents are analysed and explained separately. South China is a major block possessing more advantages for regional research than any of the other blocks in China. There exists a well‐developed succession of marine strata from the Ediacaran through to the Triassic with a relatively high resolution of bio‐ and chrono‐stratigraphy and an extensive marine fossil record. Stratigraphic occurrences of 5685 genera and 1386 families within 32 phyla or subphyla plus groups with uncertain affinities from this interval have been compiled by a large team of palaeontologists. With the exception of the Ediacaran, 50 time intervals with an average duration of 6.8 Ma are investigated. Diversity curves constructed at the levels of genus, family and order indicate that marine biodiversity peaked six times within the intervals: (1) Early Cambrian explosive radiation, (2) Early‐Mid Ordovician radiation mainly of the Paleozoic Evolutionary Fauna, (3) Early Silurian radiation, (4) late Early‐Mid Devonian radiation, (5) Mid‐Late Permian radiation and (6) Mid Triassic radiation chiefly of the Modern Evolutionary Fauna. Drops in biodiversity are controlled by various factors: (1) global catastrophes, which produced rapid losses of biodiversity during short time intervals; (2) global environmental perturbations with long term effects, as in the Carboniferous; (3) regional tectonics and palaeogeographical constraints, resulting in a lack of marine sedimentary rocks in many areas with biodiversity declining, as in the Wenlock; (4) unique sedimentary facies in large areas resulting in biodiversity losses, as in the Late Cambrian and (5) artifactual constraints associated with a lack of fossil record or low research intensity for some intervals, as in the period of about 30 Ma following the Early Cambrian explosive radiation. Copyright © 2007 John Wiley & Sons, Ltd." @default.
• W2079851915 created "2016-06-24" @default.
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• W2079851915 date "2007-04-30" @default.
• W2079851915 modified "2023-09-26" @default.
• W2079851915 title "Dynamic patterns of latest Proterozoic-Palaeozoic-early Mesozoic marine biodiversity in South China" @default.
• W2079851915 cites W1516852019 @default.
• W2079851915 cites W1698289800 @default.
• W2079851915 cites W1777186793 @default.
• W2079851915 cites W1891849076 @default.
• W2079851915 cites W1960006776 @default.
• W2079851915 cites W1968883957 @default.
• W2079851915 cites W1970056895 @default.
• W2079851915 cites W1972083608 @default.
• W2079851915 cites W1975795882 @default.
• W2079851915 cites W1976721572 @default.
• W2079851915 cites W1977548373 @default.
• W2079851915 cites W1982530104 @default.
• W2079851915 cites W1983335280 @default.
• W2079851915 cites W1983865702 @default.
• W2079851915 cites W1985323878 @default.
• W2079851915 cites W1988966899 @default.
• W2079851915 cites W1991491867 @default.
• W2079851915 cites W1995355123 @default.
• W2079851915 cites W1997713847 @default.
• W2079851915 cites W1999173650 @default.
• W2079851915 cites W1999265896 @default.
• W2079851915 cites W2002352667 @default.
• W2079851915 cites W2004614425 @default.
• W2079851915 cites W2005298615 @default.
• W2079851915 cites W2007558494 @default.
• W2079851915 cites W2010154591 @default.
• W2079851915 cites W2020700198 @default.
• W2079851915 cites W2022032772 @default.
• W2079851915 cites W2050397909 @default.
• W2079851915 cites W2052959767 @default.
• W2079851915 cites W2058208766 @default.
• W2079851915 cites W2069792062 @default.
• W2079851915 cites W2073301242 @default.
• W2079851915 cites W2075137781 @default.
• W2079851915 cites W2076487447 @default.
• W2079851915 cites W2080851551 @default.
• W2079851915 cites W2081171541 @default.
• W2079851915 cites W2086356387 @default.
• W2079851915 cites W2090254843 @default.
• W2079851915 cites W2090340649 @default.
• W2079851915 cites W2097855688 @default.
• W2079851915 cites W2107407744 @default.
• W2079851915 cites W2114435986 @default.
• W2079851915 cites W2118715042 @default.
• W2079851915 cites W2119179804 @default.
• W2079851915 cites W2126367420 @default.
• W2079851915 cites W2128652714 @default.
• W2079851915 cites W2143380472 @default.
• W2079851915 cites W2143576457 @default.
• W2079851915 cites W2146368901 @default.
• W2079851915 cites W2155850496 @default.
• W2079851915 cites W2160525739 @default.
• W2079851915 cites W2163862544 @default.
• W2079851915 cites W2165010994 @default.
• W2079851915 cites W2168463034 @default.
• W2079851915 cites W2176659351 @default.
• W2079851915 cites W2178803965 @default.
• W2079851915 cites W2180612163 @default.
• W2079851915 cites W2209143904 @default.
• W2079851915 cites W2259603924 @default.
• W2079851915 cites W2302143698 @default.
• W2079851915 cites W2315238870 @default.
• W2079851915 cites W2501786537 @default.
• W2079851915 cites W2504649407 @default.
• W2079851915 cites W2522762552 @default.
• W2079851915 cites W2523150076 @default.
• W2079851915 cites W2601667623 @default.
• W2079851915 cites W4232328127 @default.
• W2079851915 cites W4235889006 @default.
• W2079851915 cites W4240131085 @default.
• W2079851915 cites W4241733999 @default.
• W2079851915 cites W4245823893 @default.
• W2079851915 cites W951116398 @default.
• W2079851915 doi "https://doi.org/10.1002/gj.1073" @default.
• W2079851915 hasPublicationYear "2007" @default.
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