Abstract

In the paper Conodonts as Paleozoic Guide Fossils in the January, 1946, Bulletin, Vol. 30, No. 1, p. 99, Barnes et al.(FOOTNOTE 2) were cited as having found a Simpson (middle Ordovician) conodont fauna well down in the Ellenburger group (lower Ordovician). This fauna was included as an example of a stratigraphic leak. Barnes et al.(FOOTNOTE 3) have pointed out that this was an erroneous citation. Simpson conodont fauna, mixed with and Mississippian forms, was in a basal Mississippian detrital zone and should be properly classified as a stratigraphic admixture. Therefore, the Simpson fauna is all excellent example of a ghost or phantom fauna exactly as the term phantom was applied by Branson and Mehl.(FOOTNOTE 4) Appreciation is expressed to H. A. Ire and for calling the writer's attention to the error. FOOTNOTE 2. V. E. Barnes, P. E. Cloud, Jr., and L. E. Warren, The of Central Texas, Univ. Texas Bull. 4301 (1945), p. 176. FOOTNOTE 3. V. E. Barnes, P. E. Cloud, Jr., and L. E. Warren, Devonian Rocks of Central Texas, Bull. Geol. Soc. America, Vol. 58 (1947), p. 126. FOOTNOTE 4. E. B. Branson and M. G. Mehl, The Recognition and Interpretation of Mixed Conodont Faunas, Bull. Denison Univ., Vol. 35 (1940), pp. 208; 209. End_of_Article - Last_Page 778------------

Full Text
Paper version not known

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call

Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.