Quick
Search: 
 
advanced search
 GSW Home    GeoRef Home    My GSW Alerts    Contact GSW    About GSW    Journals List    Help 
Paleobiology Signup for GSW Email News
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS

Paleobiology; March 2006; v. 32; no. 2; p. 173-178; DOI: 10.1666/0094-8373(2006)32[173:MRAATL]2.0.CO;2
© 2006 Paleontological Society
This Article
Right arrow Full Text
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Right arrow Citation Map
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Similar articles in ISI Web of Science
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Vermeij, G. J.
Right arrow Articles by Dietl, G. P.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Majority rule: adaptation and the long-term dynamics of species

Geerat J. Vermeij1 and Gregory P. Dietl2

1 Department of Geology, University of California at Davis, One Shields Avenue, Davis, California 95616. vermeij@geology.ucdavis.edu
2 Department of Geology and Geophysics, Yale University, Post Office Box 208109, New Haven, Connecticut 06520. gregory.dietl@yale.edu

Accepted 19 September 2005

The first 20% of the full text of this article appears below.


    Introduction
 
Where do species that become important players in ecosystems evolve? This simple yet crucial question must be answered if we want to understand how the biosphere is rejuvenated following a crisis. We cannot simply assume that the environments in which we find fossil remains of a given species, or living populations of a species, are the environments in which that species evolved. Take the most obvious example: Fossil human skeletons have been unearthed by the hundreds in North America, but all available evidence points to a human origin in Africa. We can often identify the general geographic origins of species and clades thanks to fossil occurrences and the application of phylogenetic techniques; but can we do likewise for more ecological aspects of the environment? Advances in population biology and in paleobiology now permit us to outline a hypothesis of the circumstances most favorable to the evolution of abundant, widespread, or ecologically powerful species, those with adaptations that are selectively advantageous across many environments, and large short-term and long-term effects in ecosystems.

We can rephrase the problem and the question. Of the very large number of populations of a species inhabiting Earth at any given time, not all will contribute to the population composition of the species in the future. How does the environment in which a population is embedded affect the contribution that it will make over evolutionary time?

The importance of this issue is underscored by the finding that the type and expression of selective regime varies greatly from place to place and over time within most species (Thompson 1994, 1998, 1999a,b; Benkman et al. 2001, 2003; Thompson and Cunningham 2002; Forde et al. 2004). Some populations of pollinating moths and figwasps, for instance, may have a mutualistic relationship . . . [Full Text of this Article]







JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2008 by Paleontological Society