The Burgess Shale (Middle Cambrian) Fauna Author(s): Simon Conway Morris Reviewed work(s): Source: Annual Review of Ecology and Systematics, Vol. 10 (1979), pp. 327-349 Published by: Annual Reviews Stable URL: http://www.jstor.org/stable/2096795 . Accessed: 18/10/2012 13:58 Your use of the JSTOR archive indicates your acceptance of the Terms & Conditions of Use, available at . http://www.jstor.org/page/info/about/policies/terms.jsp . JSTOR is a not-for-profit service that helps scholars, researchers, and students discover, use, and build upon a wide range of content in a trusted digital archive. We use information technology and tools to increase productivity and facilitate new forms of scholarship. For more information about JSTOR, please contact
[email protected]. Annual Reviews is collaborating with JSTOR to digitize, preserve and extend access to Annual Review of Ecology and Systematics. http://www.jstor.org Ann. Rev. Ecol Syst. 1979. 10.327-49 Copyright ? 1979 by Annual Reviews Inc. All rights reserved THE BURGESS SHALE *4165 (MIDDLE CAMBRIAN) FAUNA Simon Conway Morris Department of Earth Sciences, The Open University, Milton Keynes MK7 6AA, England INTRODUCTION The preservation of soft parts in fossils is rare because fossilization usually occurs long after decay has destroyed soft tissues. A notable exception is the soft-bodied fauna from the Middle Cambrian Burgess Shale (about 530 million years old) located near Field in southern British Columbia, where both completely soft-bodied groups (e.g. polychaetes) and the soft parts of creatures with resistant skeletons (e.g. trilobites) are beautifully preserved. In addition, this fauna includes animals with fragile skeletons of thin cuticle that normally do not fossilize.