Magnesium in Calcite of Marine Ostracoda

Abstract

Research Article| November 01, 1972 Magnesium in Calcite of Marine Ostracoda H. MEADE CADOT; H. MEADE CADOT Department of Geology, University of Kansas, Lawrence, Kansas 66044 Search for other works by this author on: GSW Google Scholar W. R VAN SCHMUS; W. R VAN SCHMUS Department of Geology, University of Kansas, Lawrence, Kansas 66044 Search for other works by this author on: GSW Google Scholar R. L KAESLER R. L KAESLER Department of Geology, University of Kansas, Lawrence, Kansas 66044 Search for other works by this author on: GSW Google Scholar GSA Bulletin (1972) 83 (11): 3519–3522. https://doi.org/10.1130/0016-7606(1972)83[3519:MICOMO]2.0.CO;2 Article history received: 14 Apr 1972 rev-recd: 05 Jun 1972 first online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share MailTo Twitter LinkedIn Tools Icon Tools Get Permissions Search Site Citation H. MEADE CADOT, W. R VAN SCHMUS, R. L KAESLER; Magnesium in Calcite of Marine Ostracoda. GSA Bulletin 1972;; 83 (11): 3519–3522. doi: https://doi.org/10.1130/0016-7606(1972)83[3519:MICOMO]2.0.CO;2 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 Results of 255 microprobe analyses of Holocene marine Ostracoda show that, for the 21 specimens analyzed, the greatest variation in mole percent MgCO 3 occurs within calcite of individual carapaces rather than between carapaces collected from warm and cold water. Within a single genus, however, differences between specimens from different environments may reflect differences in water temperature. 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.