Pre-Cambrian fossiliferous formations

Research Article| January 01, 1899 Pre-Cambrian fossiliferous formations Charles D. Walcott Charles D. Walcott Search for other works by this author on: GSW Google Scholar GSA Bulletin (1899) 10 (1): 199–244. https://doi.org/10.1130/GSAB-10-199 Article history first online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Twitter LinkedIn Tools Icon Tools Get Permissions Search Site Citation Charles D. Walcott; Pre-Cambrian fossiliferous formations. GSA Bulletin 1899;; 10 (1): 199–244. doi: https://doi.org/10.1130/GSAB-10-199 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 SocietyGSA Bulletin Search Advanced Search Abstract IntroductionThe base of the Paleozoic and of the Cambrian has been placed at the lowest known limit of the Olenellus fauna, all clastic rocks beneath being referred to the Algonkian,* a name given to the period embracing the time of the deposition of those clastic rocks which are older than the Cambrian.† The base of the Algonkian is the lowest of the recognizable clastic rocks. This base is easily recognized beneath the Belt series of rocks in Montana, in the Grand Canyon region of Arizona, in portions of the Lake Superior region, and in eastern Newfoundland, as there are great unconformities between the Algonkian and the Archean, above which the clastic rocks are clearly defined. In other regions, however, the delimitation of the Algonkian and the Archean is very difficult. The basal plain of the Algonkian is obscured by volcanic rocks which, with the clastics, have been so altered . . . This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not currently have access to this article.