Stratigraphic Variation in Marine Carbonate Carbon Isotope Ratios

Research Article| January 01, 2001 Stratigraphic Variation in Marine Carbonate Carbon Isotope Ratios Robert L. Ripperdan Robert L. Ripperdan Department of Geology, University of Puerto Rico- Mayagüez, Mayagüez, Puerto Rico 00681 Search for other works by this author on: GSW Google Scholar Reviews in Mineralogy and Geochemistry (2001) 43 (1): 637–662. https://doi.org/10.2138/gsrmg.43.1.637 Article history first online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share MailTo Twitter LinkedIn Tools Icon Tools Get Permissions Search Site Citation Robert L. Ripperdan; Stratigraphic Variation in Marine Carbonate Carbon Isotope Ratios. Reviews in Mineralogy and Geochemistry 2001;; 43 (1): 637–662. doi: https://doi.org/10.2138/gsrmg.43.1.637 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 SocietyReviews in Mineralogy and Geochemistry Search Advanced Search Stratigraphic variation in the carbon isotopic (δ13C) value of marine carbonate and organic matter preserved within it has become a popular tool for supporting paleoclimatic hypotheses and refining stratigraphic correlation. Virtually every important biostratigraphic and sequence stratigraphic event of the last 800 million years has had a δ13C dataset collected to aid in interpreting the causal environmental factors that contributed to the event. The stratigraphic resolution obtainable using δ13C has yielded critical temporal constraints on the interplay between carbon cycle variation and environmental events such as mass extinction and eustasy. Although the non-uniqueness of... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.