TOWARDS AN ASSESSMENT OF PHANEROZOIC TRENDS IN BETA DIVERSITY: THE IMPORTANCE OF ENVIRONMENTAL AND GEOGRAPHIC SCALE
In our presentation, we will discuss our initial efforts to assess the Phanerozoic history of beta diversity, starting with a comparison of two exemplars: the Caradocian stage of the Ordovician and the Eocene epoch of the Paleogene. In this context, it is important to consider the geographic or environmental scale at which the compositions of collections are compared to one another (the heart of any assessment of beta diversity). While it might be argued that beta diversity during any interval should be analyzed with samples collected from paleocommunities arrayed along local environmental gradients, there are clearly much broader spatial scales at which biotic turnover is also meaningful, including the degree of differentiation among major, paleocontinent-scale regions of the world. With this in mind, we are investigating the nature of biotic differentiation at multiple geographic and environmental scales, to determine: a) whether, during a given interval, the degree of biotic differentiation did, indeed, vary as a predictable function of geographic or environmental scale; and b) whether, for a given scale, the degree of biotic differentiation varies significantly between the intervals under investigation. This will permit a more sophisticated assessment of beta diversity trends than would be possible by focusing on just a single scale, or by attempting to summarize beta diversity for a given interval with a single approximation.