Phanerozoic Trends in the Global Diversity of Marine Invertebrates-Reference-Cited by-同舟云学术

Phanerozoic Trends in the Global Diversity of Marine Invertebrates

Published:2008-07-04 Issue:5885 Volume:321 Page:97-100
ISSN:0036-8075
Container-title:Science
language:en
Short-container-title:Science

Author:

Alroy John¹²³⁴⁵,Aberhan Martin¹²³⁴⁵,Bottjer David J.¹²³⁴⁵,Foote Michael¹²³⁴⁵,Fürsich Franz T.¹²³⁴⁵,Harries Peter J.¹²³⁴⁵,Hendy Austin J. W.¹²³⁴⁵,Holland Steven M.¹²³⁴⁵,Ivany Linda C.¹²³⁴⁵,Kiessling Wolfgang¹²³⁴⁵,Kosnik Matthew A.¹²³⁴⁵,Marshall Charles R.¹²³⁴⁵,McGowan Alistair J.¹²³⁴⁵,Miller Arnold I.¹²³⁴⁵,Olszewski Thomas D.¹²³⁴⁵,Patzkowsky Mark E.¹²³⁴⁵,Peters Shanan E.¹²³⁴⁵,Villier Loïc¹²³⁴⁵,Wagner Peter J.¹²³⁴⁵,Bonuso Nicole¹²³⁴⁵,Borkow Philip S.¹²³⁴⁵,Brenneis Benjamin¹²³⁴⁵,Clapham Matthew E.¹²³⁴⁵,Fall Leigh M.¹²³⁴⁵,Ferguson Chad A.¹²³⁴⁵,Hanson Victoria L.¹²³⁴⁵,Krug Andrew Z.¹²³⁴⁵,Layou Karen M.¹²³⁴⁵,Leckey Erin H.¹²³⁴⁵,Nürnberg Sabine¹²³⁴⁵,Powers Catherine M.¹²³⁴⁵,Sessa Jocelyn A.¹²³⁴⁵,Simpson Carl¹²³⁴⁵,Tomašových Adam¹²³⁴⁵,Visaggi Christy C.¹²³⁴⁵

Affiliation:

1. National Center for Ecological Analysis and Synthesis, University of California–Santa Barbara, 735 State Street, Santa Barbara, CA 93101, USA.

2. Museum für Naturkunde der Humboldt-Universität zu Berlin, Invalidenstrasse 43, D-10115 Berlin, Germany.

3. Department of Earth Sciences, University of Southern California, Los Angeles, CA 90089–0740, USA.

4. Department of the Geophysical Sciences, University of Chicago, Chicago, IL 60637, USA.

5. Geozentrum Nordbayern, Friedrich-Alexander Universität Erlangen, Loewenichstrasse 28, D-91054, Germany.

Abstract

It has previously been thought that there was a steep Cretaceous and Cenozoic radiation of marine invertebrates. This pattern can be replicated with a new data set of fossil occurrences representing 3.5 million specimens, but only when older analytical protocols are used. Moreover, analyses that employ sampling standardization and more robust counting methods show a modest rise in diversity with no clear trend after the mid-Cretaceous. Globally, locally, and at both high and low latitudes, diversity was less than twice as high in the Neogene as in the mid-Paleozoic. The ratio of global to local richness has changed little, and a latitudinal diversity gradient was present in the early Paleozoic.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

Reference37 articles.

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5. J. J. Sepkoski Jr., in Global Events and Event Stratigraphy, O. H. Walliser, Ed. (Springer, Berlin, 1996), pp. 35–52.

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