Appearance and disappearance rates of Phanerozoic marine animal paleocommunities

Author:

Muscente A.D.12,Martindale Rowan C.2,Prabhu Anirudh3,Ma Xiaogang4,Fox Peter3,Hazen Robert M.5,Knoll Andrew H.6

Affiliation:

1. Department of Geology, Cornell College, 600 First Street SW, Mount Vernon, Iowa 52314, USA

2. Department of Geological Sciences, The University of Texas at Austin, 1 University Station C1100, Austin, Texas 78712, USA

3. Department of Earth and Environmental Sciences, Rensselaer Polytechnic Institute, Jonsson-Rowland Science Center, 1W19, 110 8th Street, Troy, New York 12180, USA

4. Department of Computer Science, University of Idaho, 875 Perimeter Drive, MS 1010, Moscow, Idaho 83844, USA

5. Geophysical Laboratory, Carnegie Institution for Science, 5251 Broad Branch Road, Washington, D.C. 20015, USA

6. Department of Organismic and Evolutionary Biology, Harvard University, 26 Oxford Street, Cambridge, Massachusetts 02138, USA

Abstract

Ecological observations and paleontological data show that communities of organisms recur in space and time. Various observations suggest that communities largely disappear in extinction events and appear during radiations. This hypothesis, however, has not been tested on a large scale due to a lack of methods for analyzing fossil data, identifying communities, and quantifying their turnover. We demonstrate an approach for quantifying turnover of communities over the Phanerozoic Eon. Using network analysis of fossil occurrence data, we provide the first estimates of appearance and disappearance rates for marine animal paleocommunities in the 100 stages of the Phanerozoic record. Our analysis of 124,605 fossil collections (representing 25,749 living and extinct marine animal genera) shows that paleocommunity disappearance and appearance rates are generally highest in mass extinctions and recovery intervals, respectively, with rates three times greater than background levels. Although taxonomic change is, in general, a fair predictor of ecologic reorganization, the variance is high, and ecologic and taxonomic changes were episodically decoupled at times in the past. Extinction rate, therefore, is an imperfect proxy for ecologic change. The paleocommunity turnover rates suggest that efforts to assess the ecological consequences of the present-day biodiversity crisis should focus on the selectivity of extinctions and changes in the prevalence of biological interactions.

Publisher

Geological Society of America

Subject

Geology

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