1938Geological Society of America BulletinRequires access

Lower Cambrian Olenellus zone of the Appalachians

Charles Elmer Resser, B. F. HOWELL

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Research Article| February 01, 1938 Lower Cambrian Olenellus zone of the Appalachians CHARLES ELMER RESSER; CHARLES ELMER RESSER Search for other works by this author on: GSW Google Scholar BENJAMIN FRANKLIN HOWELL BENJAMIN FRANKLIN HOWELL Search for other works by this author on: GSW Google Scholar GSA Bulletin (1938) 49 (2): 195–248. https://doi.org/10.1130/GSAB-49-195 Article history received: 04 Jun 1936 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 ELMER RESSER, BENJAMIN FRANKLIN HOWELL; Lower Cambrian Olenellus zone of the Appalachians. GSA Bulletin 1938;; 49 (2): 195–248. doi: https://doi.org/10.1130/GSAB-49-195 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGSA Bulletin Search Advanced Search Abstract INTRODUCTIONLower Cambrian fossils were first discovered by Emmons in eastern New York almost a century ago. Since then, many specimens have been obtained from the Appalachian region, but the stratigraphy received little attention. Recently, interest in the study of the early Paleozoic rocks of the Appalachians has revived.A. F. Foerste described the cystids. Consequently, the new genus Lepidocystis and the species L. wanneri are to be attributed to him.THE APPALACHIANSIn this paper the name Appalachians applies to a region characterized by a particular stratigraphic history and geologic structure and, therefore, is not used in a physiographic sense. The region embraces the Appalachian Mountains from Alabama to eastern Pennsylvania, or the area to which the physiographic term usually applies. Inasmuch as similar stratigraphic conditions and geologic structure continue beyond Pennsylvania, the term Appalachians must also embrace the Hudson and Champlain valleys, and the St. Lawrence Valley to . . . This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not have access to this content, please speak to your institutional administrator if you feel you should have access.

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Research Article| February 01, 1938 Lower Cambrian Olenellus zone of the Appalachians CHARLES ELMER RESSER; CHARLES ELMER RESSER Search for other works by this author on: GSW Google Scholar BENJAMIN FRANKLIN HOWELL BENJAMIN FRANKLIN HOWELL Search for other works by this author on: GSW Google Scholar GSA Bulletin (1938) 49 (2): 195–248. https://doi.org/10.1130/GSAB-49-195 Article history received: 04 Jun 1936 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 ELMER RESSER, BENJAMIN FRANKLIN HOWELL; Lower Cambrian Olenellus zone of the Appalachians. GSA Bulletin 1938;; 49 (2): 195–248. doi: https://doi.org/10.1130/GSAB-49-195 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGSA Bulletin Search Advanced Search Abstract INTRODUCTIONLower Cambrian fossils were first discovered by Emmons in eastern New York almost a century ago. Since then, many specimens have been obtained from the Appalachian region, but the stratigraphy received little attention. Recently, interest in the study of the early Paleozoic rocks of the Appalachians has revived.A. F. Foerste described the cystids. Consequently, the new genus Lepidocystis and the species L. wanneri are to be attributed to him.THE APPALACHIANSIn this paper the name Appalachians applies to a region characterized by a particular stratigraphic history and geologic structure and, therefore, is not used in a physiographic sense. The region embraces the Appalachian Mountains from Alabama to eastern Pennsylvania, or the area to which the physiographic term usually applies. Inasmuch as similar stratigraphic conditions and geologic structure continue beyond Pennsylvania, the term Appalachians must also embrace the Hudson and Champlain valleys, and the St. Lawrence Valley to . . . This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not have access to this content, please speak to your institutional administrator if you feel you should have access.

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Research Article| February 01, 1938 Lower Cambrian Olenellus zone of the Appalachians CHARLES ELMER RESSER; CHARLES ELMER RESSER Search for other works by this author on: GSW Google Scholar BENJAMIN FRANKLIN HOWELL BENJAMIN FRANKLIN HOWELL Search for other works by this author on: GSW Google Scholar GSA Bulletin (1938) 49 (2): 195–248. https://doi.org/10.1130/GSAB-49-195 Article history received: 04 Jun 1936 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 ELMER RESSER, BENJAMIN FRANKLIN HOWELL; Lower Cambrian Olenellus zone of the Appalachians. GSA Bulletin 1938;; 49 (2): 195–248. doi: https://doi.org/10.1130/GSAB-49-195 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGSA Bulletin Search Advanced Search Abstract INTRODUCTIONLower Cambrian fossils were first discovered by Emmons in eastern New York almost a century ago. Since then, many specimens have been obtained from the Appalachian region, but the stratigraphy received little attention. Recently, interest in the study of the early Paleozoic rocks of the Appalachians has revived.A. F. Foerste described the cystids. Consequently, the new genus Lepidocystis and the species L. wanneri are to be attributed to him.THE APPALACHIANSIn this paper the name Appalachians applies to a region characterized by a particular stratigraphic history and geologic structure and, therefore, is not used in a physiographic sense. The region embraces the Appalachian Mountains from Alabama to eastern Pennsylvania, or the area to which the physiographic term usually applies. Inasmuch as similar stratigraphic conditions and geologic structure continue beyond Pennsylvania, the term Appalachians must also embrace the Hudson and Champlain valleys, and the St. Lawrence Valley to . . . This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not have access to this content, please speak to your institutional administrator if you feel you should have access.

Key concepts: Icon, Citation, Geology, Paleontology, Paleozoic, Download, Library science, Archaeology

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