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Taxonomy and temporal diversity patterns

Published online by Cambridge University Press:  08 February 2016

Heidi E. Robeck
Affiliation:
Museum of Comparative Zoology, 26 Oxford Street, Cambridge, Massachusetts 02138. E-mail: hrobeck@oeb.harvard.edu
Carlo C. Maley
Affiliation:
MIT NE43-937, 545 Technology Square, Cambridge, Massachusetts 02139. E-mail: cmaley@cs.unm.edu
Michael J. Donoghue
Affiliation:
Harvard University Herbaria, 22 Divinity Avenue, Cambridge, Massachusetts 02138. E-mail: mdonoghue@oeb.harvard.edu

Abstract

Temporal diversity patterns have traditionally been analyzed by counting the number of families or genera present over a series of time periods. This approach has been criticized on the grounds that paraphyletic taxa might introduce artifacts. Sepkoski and Kendrick (1993) simulated phylogenetic trees and different classifications of those trees and concluded that paraphyletic taxa need not be rejected. We have reimplemented their model, extended it, and carried out statistical analyses under a variety of experimental conditions. Our results show that the focus on monophyly vs. paraphyly is misplaced. Instead, it appears that the number of groups in the classification and the distribution of the sizes of those groups have dramatic effects on the recovery of diversity information. Furthermore, the influence of these factors depends on whether the fossil record represents a low- or high-frequency sampling of lineages. When sampling is good, the best results are achieved by classifications with large numbers of small taxa. When sampling is poor, however, the best results are achieved by classifications that include some large and medium-sized groups as well as many smaller groups. This suggests that the best estimates of underlying diversity will be achieved by counting (in the same study) taxa assigned to different ranks, so as to best match the inferred quality of the paleontological sample. In practice this will mean abandoning the commitment to counting taxa at a single rank.

Type
Articles
Copyright
Copyright © The Paleontological Society 

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