Changes to the Fossil Record of Insects through Fifteen Years of Discovery

被引:55
作者
Nicholson, David B. [1 ,2 ]
Mayhew, Peter J. [1 ]
Ross, Andrew J. [2 ]
机构
[1] Univ York, Dept Biol, York YO10 5DD, N Yorkshire, England
[2] Natl Museum Scotland, Dept Nat Sci, Edinburgh, Midlothian, Scotland
基金
英国自然环境研究理事会;
关键词
PERMIAN WELLINGTON FORMATION; EOCENE BALTIC AMBER; CZECH-REPUBLIC INSECTA; HEMIPTERA FULGOROMORPHA FULGOROIDEA; CRETACEOUS BEETLES COLEOPTERA; 1ST GLOSSELYTRODEA INSECTA; FORMATION BERMEJO BASIN; MUSEUM-FUR-NATURKUNDE; FAM. NOV INSECTA; NEW-SOUTH-WALES;
D O I
10.1371/journal.pone.0128554
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
The first and last occurrences of hexapod families in the fossil record are compiled from publications up to end-2009. The major features of these data are compared with those of previous datasets (1993 and 1994). About a third of families (>400) are new to the fossil record since 1994, over half of the earlier, existing families have experienced changes in their known stratigraphic range and only about ten percent have unchanged ranges. Despite these significant additions to knowledge, the broad pattern of described richness through time remains similar, with described richness increasing steadily through geological history and a shift in dominant taxa, from Palaeoptera and Polyneoptera to Paraneoptera and Holometabola, after the Palaeozoic. However, after detrending, described richness is not well correlated with the earlier datasets, indicating significant changes in shorter-term patterns. There is reduced Palaeozoic richness, peaking at a different time, and a less pronounced Permian decline. A pronounced Triassic peak and decline is shown, and the plateau from the mid Early Cretaceous to the end of the period remains, albeit at substantially higher richness compared to earlier datasets. Origination and extinction rates are broadly similar to before, with a broad decline in both through time but episodic peaks, including end-Permian turnover. Origination more consistently exceeds extinction compared to previous datasets and exceptions are mainly in the Palaeozoic. These changes suggest that some inferences about causal mechanisms in insect macroevolution are likely to differ as well.
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页数:61
相关论文
共 1143 条
[1]   An empirical assessment of taxic paleobiology [J].
Adrain, JM ;
Westrop, SR .
SCIENCE, 2000, 289 (5476) :110-112
[2]  
Alonso J, 2000, J PALEONTOL, V74, P158, DOI 10.1666/0022-3360(2000)074<0158:ANFRWB>2.0.CO
[3]  
2
[4]  
Alroy J, 2000, GEOLOGY, V28, P1023, DOI 10.1130/0091-7613(2000)28<1023:SAODCT>2.0.CO
[5]  
2
[6]  
Alroy J, 2004, EVOL ECOL RES, V6, P1
[7]   The Shifting Balance of Diversity Among Major Marine Animal Groups [J].
Alroy, J. .
SCIENCE, 2010, 329 (5996) :1191-1194
[8]  
Alroy J, 2000, PALEOBIOLOGY, V26, P707, DOI 10.1666/0094-8373(2000)026<0707:NMFQMP>2.0.CO
[9]  
2
[10]   Effects of sampling standardization on estimates of Phanerozoic marine diversification [J].
Alroy, J ;
Marshall, CR ;
Bambach, RK ;
Bezusko, K ;
Foote, M ;
Fürsich, FT ;
Hansen, TA ;
Holland, SM ;
Ivany, LC ;
Jablonski, D ;
Jacobs, DK ;
Jones, DC ;
Kosnik, MA ;
Lidgard, S ;
Low, S ;
Miller, AI ;
Novack-Gottshall, PM ;
Olszewski, TD ;
Patzkowsky, ME ;
Raup, DM ;
Roy, K ;
Sepkoski, JJ ;
Sommers, MG ;
Wagner, PJ ;
Webber, A .
PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA, 2001, 98 (11) :6261-6266