Abstract

Research Article| January 01, 2011 Stratigraphic revision of the Green River Formation in Fossil Basin, Wyoming H. Paul Buchheim; H. Paul Buchheim ∗ 1Department of Earth and Biological Sciences, Loma Linda University, Loma Linda, California 92350, U.S.A. ∗Correspondence should be addressed to: pbuchheim@llu.edu Search for other works by this author on: GSW Google Scholar Robert A. Cushman, Jr.; Robert A. Cushman, Jr. 2Department of Biological Sciences, Walla Walla University, College Place, Washington 99324, U.S.A. Search for other works by this author on: GSW Google Scholar Roberto E. Biaggi Roberto E. Biaggi 3Ciencias Naturales, Universidad Adventista del Plata, Libertador San Martin, Entre Rios 03103, Argentina Search for other works by this author on: GSW Google Scholar Rocky Mountain Geology (2011) 46 (2): 165–181. https://doi.org/10.2113/gsrocky.46.2.165 Article history received: 04 Mar 2011 rev-recd: 13 Sep 2011 accepted: 11 Nov 2011 first online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Twitter LinkedIn Tools Icon Tools Get Permissions Search Site Citation H. Paul Buchheim, Robert A. Cushman, Roberto E. Biaggi; Stratigraphic revision of the Green River Formation in Fossil Basin, Wyoming. Rocky Mountain Geology 2011;; 46 (2): 165–181. doi: https://doi.org/10.2113/gsrocky.46.2.165 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu nav search search input Search input auto suggest search filter All ContentBy SocietyRocky Mountain Geology Search Advanced Search Abstract The Eocene Green River Formation in Fossil Basin, Wyoming provides a detailed record of the paleoecology and depositional history of ancient Fossil Lake. Fossil Lake was one of three Eocene lakes that formed an extensive lake system in Wyoming, Utah, and Colorado. It began as a flood-plain lake in the southern part of Fossil Basin and expanded northward as the lake evolved. Fossil Lake went through the major stages of lake evolution, including the overfilled (Road Hollow Member), balanced-fill (Fossil Butte Member), and underfilled (Angelo Member) stages. These stages are represented in the sedimentary record by a complete suite of lake-margin to lake-center facies.This study establishes the Road Hollow Member of the Green River Formation as representing the earliest stage of lake evolution in Fossil Lake. We also revise the boundaries for the Fossil Butte and Angelo Members of the Green River Formation, which clearly delineate the latest two stages of lake evolution. These revisions not only describe and add a previously unrecognized and thick sequence of lacustrine rocks in Fossil Basin, but help us to better understand the depositional systems that existed during each stage of lake evolution. You do not currently have access to this article.

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