Cretaceous tetrapod fossil record sampling and faunal turnover: Implications for biogeography and the rise of modern clades

被引:79
作者
Benson, Roger B. J. [1 ,2 ]
Mannion, Philip D. [3 ,4 ]
Butler, Richard J. [5 ]
Upchurch, Paul [2 ]
Goswami, Anjali [2 ,7 ]
Evans, Susan E. [6 ]
机构
[1] Univ Oxford, Dept Earth Sci, Oxford OX1 3AN, England
[2] UCL, Dept Earth Sci, London WC1E 6BT, England
[3] Univ London Imperial Coll Sci Technol & Med, Dept Earth Sci & Engn, London SW7 2AZ, England
[4] Museum Nat Kunde, D-10115 Berlin, Germany
[5] Univ Munich, GeoBioctr, D-80333 Munich, Germany
[6] UCL, Dept Cell & Dev Biol, London WC1E 6BT, England
[7] UCL, Dept Genet Evolut & Environm, London WC1E 6BT, England
关键词
Cretaceous; Fossil record sampling; Rock record; Faunal turnover; Biogeography; CENOMANIAN-TURONIAN BOUNDARY; JURASSIC MORRISON FORMATION; SAO-PAULO STATE; ROCK-RECORD; MULTITUBERCULATE MAMMALS; ADAMANTINA FORMATION; SEA-LEVEL; PHYLOGENETIC-RELATIONSHIPS; THERIZINOSAUROID DINOSAUR; HISTORICAL BIOGEOGRAPHY;
D O I
10.1016/j.palaeo.2012.10.028
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
We use newly compiled data on global occurrences of Cretaceous lepidosaurs, mammals and crocodylomorphs, and existing data on dinosaurs, to investigate faunal turnover and fossil record heterogeneity. Statistically significant relationships between many clade-specific fossil record sampling proxies within major continental areas (e.g. European mammal-bearing formations) suggest that temporal patterns of fossil record sampling intensity of the most abundant tetrapod clades are similar to each other, with a few exceptions that might reflect clade-specific facies preferences or differences in worker effort (especially in poorly-sampled regions such as Gondwana). However, the absence of strong statistical relationships between tetrapod sampling proxies from different continental areas suggests that there is no unified 'global' sampling signal for terrestrial tetrapods. The Cretaceous witnessed substantial faunal turnover and the rise of many 'advanced' clades that today dominate terrestrial faunas. Despite strong spatiotemporal heterogeneity in sampling of the Cretaceous tetrapod record, it is clear that this transition occurred in a spatiotemporally staggered fashion. Thus, it cannot be attributed to a temporally localised early Late Cretaceous (Cenomanian-Turonian) extinction event. Many advanced clades, including eutherian mammals, iguanian and gekkotan squamates, and the main cryptodiran turtle crown clades first appeared, or first attained high fossil diversities, in Asia. However, relatively poor sampling and dating of 'middle' Cretaceous terrestrial deposits means that hypotheses of Asian, rather than Laurasian, diversifications remain tentative. Differences between Gondwanan and Laurasian faunas became progressively greater during the Cretaceous, and although many Gondwanan clades survived the end-Cretaceous extinction event, these only survive to the present as relictual populations with narrow geographic ranges (e.g. monotremes and rhynchocephalians). (C) 2012 Elsevier B.V. All rights reserved.
引用
收藏
页码:88 / 107
页数:20
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