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September Gsat 03 Groundwork: Accreditation: Wrong Path for the Geosciences, p. 52–53 VOL. 18, No. 10 A PUBLICATION OF THE GEOLOGICAL SOCIETY OF AMERICA OCTOBER 2008 Turbulent lifestyle: Microbial mats on Earth’s sandy beaches—Today and 3 billion years ago Inside: Section Meetings: Southeastern Section, p. 21 South-Central Section, p. 23 Northeastern Section, p. 24 Call for 2009 GSA Award and Medal Nominations, p. 10 It’s Not Just Software. It’s RockWare. For Over 24 Years. 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GWB Professional $7,999 1D/2D Reactive Transport Modeling $349 Workbench The Geochemist’s Since 1983 303.278.3534 • 800.775.6745 RockWare.com GSATodayOctober08.indd 1 8/25/2008 9:34:04 AM VOLUME 18, NUMBER 10 ▲ OCTOBER 2008 SCIENCE ARTICLE GSA TODAY publishes news and information for more than 4 Turbulent lifestyle: Microbial mats 21,500 GSA members and subscribing libraries. GSA TODAY (ISSN 1052-5173 USPS 0456-530) is published 11 times per on Earth’s sandy beaches—Today and year, monthly, with a combined April/May issue, by The 3 billion years ago Geological Society of America®, Inc., with offices at 3300 Nora Noffke Penrose Place, Boulder, Colorado. Mailing address: P.O. Box Cover: Multidirected ripple marks preserved in an 9140, Boulder, CO 80301-9140, USA. Periodicals postage paid at Boulder, Colorado, and at additional mailing offices. ancient siliciclastic tidal flat of the 2.9 Ga Pongola Postmaster: Send address changes to GSA Today, GSA Sales Supergroup, South Africa. Studies in modern settings and Service, P.O. Box 9140, Boulder, CO 80301-9140. GSA show that such a chaotic ripple mark pattern is caused provides this and other forums for the presentation of diverse by the interaction of sediment-stabilizing microbial opinions and positions by scientists worldwide, regardless of mats with episodic storm events. In concert with a their race, citizenship, gender, religion, or political viewpoint. Opinions presented in this publication do not reflect official multitude of other “microbially induced sedimentary positions of the Society. structures” (MISS), these ripple marks potentially record the oldest and most diverse cyanobacterial Copyright © 2008, The Geological Society of America (GSA). population in Earth’s history. Photo courtesy N. Noffke. All rights reserved. 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Turbulent lifestyle: Microbial mats on Earth’s sandy beaches—Today and 3 billion years ago Nora Noffke, Old Dominion University, Department of Ocean, In the 1980s–1990s, it was suggested that crinkled upper Earth & Atmospheric Sciences, Norfolk, Virginia 23529, USA bedding planes (“elephant skin textures”) might record ancient microbial mats (e.g., Runnegar and Fedonkin, 1992; Gehling, 1999). Similar conclusions were reached by Seilacher et al. ABSTRACT (1985) in lagoonal sediments of Solnhofen, Germany, and by Archean Earth history is very difficult to reconstruct. Until Schieber (1998) in Mesoproterozoic shales of Montana, USA. recently, only bacterial cells preserved in chert, microborings, Those early observations on microbial mat–related structures and stromatolites provided the few clues to ancient life. Now, were summarized in Hagadorn et al. (1999), followed by a siliciclastic “microbially induced sedimentary structures” (MISS) photo atlas (Schieber et al., 2007). At about the same time, the are adding to our knowledge of both past life and paleo­ genesis of modern microbial mat–associated sedimentary struc­ environments. MISS rise from the interaction of photoauto­ tures was being elucidated (e.g., Cameron et al., 1985; Gerdes trophic microbial mats with physical sediment dynamics in and Krumbein, 1987; Gerdes et al., 1991, 1994). The term siliciclastic, shallow­marine settings. Archean MISS can be “microbially induced sedimentary structures” (MISS) was coined understood through observations of living microbial mats in 1996, based on quantitative analyses of mat­related struc­ and modern biotic­physical sedimentary processes. Such tures in sandy tidal flats (Noffke et al., 1996). The sixteen main geobiological studies are key to the interpretation of the early types of MISS arise exclusively from the interaction of biofilms evolution of prokaryotes. For example, the 2.9 Ga Pongola and microbial mats with the physical sediment dynamics Supergroup, South Africa, includes MISS that possibly point (Noffke, 2009). This contrasts with the formation of stromato­ to the oldest known cyanobacterial community preserved in lites, in which chemical precipitation plays a major role. Earth’s history. Because of their unique biotic­physical genesis, MISS differ sig­ nificantly in morphology from stromatolites (Fig. 1). INTRODUCTION Systematic studies, leading from modern to increasingly The question of where and when the earliest
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