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Taphonomy and Paleoecology of the Dinosaur Beds of the Jurassic Morrison Formation

Published online by Cambridge University Press:  08 February 2016

Peter Dodson ,
A. K. Behrensmeyer ,
Robert T. Bakker  and
John S. McIntosh
Peter Dodson
Affiliation:
Laboratories of Anatomy, School of Veterinary Medicine, University of Pennsylvania, Philadelphia, Pa. 19104
A. K. Behrensmeyer
Affiliation:
Peabody Museum of Natural History, Yale University, New Haven, Conn. 06520
Robert T. Bakker
Affiliation:
Department of Earth and Planetary Science, Johns Hopkins University, Baltimore, Md. 21218
John S. McIntosh
Affiliation:
Department of Physics, Wesleyan University, Middletown, Conn. 06457
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Abstract

The Upper Jurassic Morrison Formation has yielded one of the richest dinosaur faunas of the world. Morrison sediments are distributed over more than a million square kilometers in the western United States and represent a mosaic of riverine, lacustrine and floodplain environments developed on a vast alluvial plain nourished by debris from the ancestral Rocky Mountains. Plant productivity must have been reasonably high to support abundant large-bodied herbivores, but the absence of coals, scarcity of small aquatic vertebrates, the abundance of oxidized sediments, and presence of calcretes lead us to believe that water was periodically in short supply. A strongly seasonal climate may have necessitated annual large-scale movements of large herbivores, accounting in part for their remarkably broad and uniform geographic distribution. Dinosaur diversity is lower in the Morrison than in the Late Cretaceous, and taphonomic alteration is higher. Massed accumulations of thousands of bones are characteristic of the Morrison. Morrison dinosaurs were not confined to specific depositional environments but were distributed across the complete spectrum of available habitats, from lakes to dry floodplains; this type of distribution is similar to that of large terrestrial mammals such as elephants and rhinos and is different from that of hippos and crocodiles. Common Morrison taxa were Camarasaurus, Apatosaurus, Diplodocus, Allosaurus and Stegosaurus; these genera probably constituted a true dinosaur community. Stegosaurus may have been partially segregated from the other genera, and Camptosaurus more strongly so. Camarasaurus and Diplodocus were gregarious, with juveniles and subadults of the former particularly common; Apatosaurus was less abundant and more solitary in its habits. Juveniles and subadults are known for a number of dinosaurs.

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Articles
Information
Paleobiology , Volume 6 , Issue 2 , Spring 1980 , pp. 208 - 232
Copyright
Copyright © The Paleontological Society 

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