Paper No. 10-0
EXPLORING THE EVOLUTIONARY MORPHOLOGY OF DASYCLADALEAN ALGAE: ADAPTIVE WALKS IN THE R LANDSCAPE
LODUCA, Steven T., Dept Geography & Geology, Eastern Michigan Univ, Ypsilanti, MI 48197, geo_loduca@online.emich.edu and BEHRINGER, Ernest R., Dept Physics & Astronomy, Eastern Michigan Univ, Ypsilanti, MI 48197

Dasycladalean algae, a long-ranging clade of unicellular-, uninucleate-grade shallow marine chlorophytes, have a tightly constrained and readily quantifiable relationship between form and fecundity, and a body plan that is highly amenable to mathematical modeling. Because of this combination of features, it is possible to construct an "R landscape" for dasycladaleans, that is, a theoretical morphospace wherein each morphotype is characterized by R, the number of offspring per unit time. The resulting dasycladalean R landscape possesses a varied and rugged topology, with steep-sided peaks, ridges, and plateaus (regions of high R values) separated by deep chasms (regions of low R values). If extra-clade selection pressure is uniform between dasycladalean morphotypes, then R describes relative fitness, and the R landscape approximates the dasycladalean fitness landscape. Optimal and non-optimal adaptive walks, the latter either maintaining or increasing fitness at each step, provide means to explore this landscape and develop a range of evolutionary insights. We will present examples of both optimal and non-optimal walks generated in the R landscape, and discuss the use of such walks as tools to (1) illuminate the topology of biophysically available "evolutionary pathways" through the dasycladalean theoretical morphospace, (2) examine the sensitivity of the R landscape to differential selection pressure, (3) test the R landscape as being consistent with a fitness landscape for a given interval of dasycladalean evolutionary history, (4) evaluate dasycladalean phylogenetic hypotheses derived by other means (e.g., cladistic analysis), and (5) explore possible causes of particular dasycladalean extinction events.

North-Central Section (36th) and Southeastern Section (51st), GSA Joint Annual Meeting (April 3–5, 2002)
Session No. 10
Evolutionary Morphology
Hyatt Regency Hotel: Regency Ballroom West
1:20 PM-5:00 PM, Wednesday, April 3, 2002
 

© Copyright 2002 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.