Please use this identifier to cite or link to this item: http://hdl.handle.net/2440/72772
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Type: Journal article
Title: Early Cambrian metazoans in fluvial environments, evidence of the non-marine Cambrian radiation
Author: Kennedy, M.
Droser, M.
Citation: Geology, 2011; 39(6):583-586
Publisher: Geological Soc America Inc
Issue Date: 2011
ISSN: 0091-7613
0091-7613
Statement of
Responsibility: 
Martin J. Kennedy and Mary L. Droser
Abstract: Here we describe the oldest evidence of non-marine animals from the early Cambrian Wood Canyon Formation, California, evidence created by metazoans of a variety of sizes and behaviors. Millimeter-sized vertical trace fossils, including the U-shaped burrow Arenicolites and the vertical burrow Skolithos, as well as a centimeter-scale horizontal trace fossil, occur in conglomerate and gritty arkosic sandstone bed tops within fluvial channels. These fossils demonstrate that animals were dwelling in this habitat coincident with, or possibly predating, the first trilobites, and extend the freshwater record of animals back at least 80 m.y. The development of a functioning terrestrial ecosystem was concurrent with the early Cambrian marine radiation and suggests that freshwater environments were populated early by metazoans and that ecological opportunity likely played a determining role in metazoan exploitation of non-marine habitats versus commonly assumed influences from physiological or nonbiological barriers.
Rights: © Geological Society of America
RMID: 0020106109
DOI: 10.1130/G32002.1
Appears in Collections:Earth and Environmental Sciences publications
Environment Institute Leaders publications

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