Author:
Lieberman Bruce S.,Brett Carlton E.,Eldredge Niles
Abstract
More than 5000 measurements were taken on over 1000 specimens of two species of brachiopods, Mediospirifer audaculus and Athyris spiriferoides, from the Middle Devonian Hamilton Group of New York state. Statistical analyses were performed on these data, with specimens partitioned by their occurrence in one of many paleoenvironments and stratigraphic horizons. Neither species showed substantial morphological departures between first appearance and extinction (the range of the Hamilton Group, roughly 5 m.y.). However, oscillations in morphology were discovered in both taxa.For the two species we studied, groups of organisms occurring in a single paleoenvironment undergo moderate morphological change through time; however, the net sum of changes through time in all paleoenvironments in which these species occur is essentially zero. Therefore, stasis may be partly a property of the organization of species into different environmental populations. Different “environmental populations” may evolve, but they will typically do so in several different “directions,” generally producing no net change. The difference between the morphology of species in different environments over the whole interval of the Hamilton Group is also nil, thereby ruling out any major role that ecophenotypic effects could play in the patterns recognized herein.
Publisher
Cambridge University Press (CUP)
Subject
Paleontology,General Agricultural and Biological Sciences,Ecology,Ecology, Evolution, Behavior and Systematics
Reference28 articles.
1. Brett C. E. , Dick V. B. , and Baird G. C. 1991. Comparative taphonomy and paleoecology of Middle Devonian dark grey and black shale facies from western New York. Pp. 5–36 in Landing E. and Brett C. E. , eds. Dynamic stratigraphy and depositional environments of the Hamilton Group (Middle Devonian) in New York State. New York State Museum Bulletin 469.
2. Symmetrical and upward shallowing cycles in the Middle Devonian of New York State and their implications for the punctuated Aggradational Cycle Hypothesis
3. Endolith associations and their relation to facies distribution in the Middle Devonian of New York State, U.S.A.
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