Triple Oxygen Isotope Trend Recorded by Precambrian Cherts: A Perspective from Combined Bulk and in situ Secondary Ion Probe Measurements
David Zakharov, Johanna Marin‐Carbonne, Julien Alléon, Ilya N. Bindeman
Abstract
Research Article| January 01, 2021 Triple Oxygen Isotope Trend Recorded by Precambrian Cherts: A Perspective from Combined Bulk and in situ Secondary Ion Probe Measurements D. O. Zakharov; D. O. Zakharov Institute of Earth Sciences, University of Lausanne, Lausanne, 1015 Switzerland * E-mail: [email protected] Search for other works by this author on: GSW Google Scholar J. Marin-Carbonne; J. Marin-Carbonne Institute of Earth Sciences, University of Lausanne, Lausanne, 1015 Switzerland * E-mail: [email protected] Search for other works by this author on: GSW Google Scholar J. Alleon; J. Alleon Institute of Earth Sciences, University of Lausanne, Lausanne, 1015 Switzerland * E-mail: [email protected] Search for other works by this author on: GSW Google Scholar I. N. Bindeman I. N. Bindeman Department of Earth Sciences, University of Oregon, Eugene, OR 97403, USA * E-mail: [email protected] Search for other works by this author on: GSW Google Scholar Reviews in Mineralogy and Geochemistry (2021) 86 (1): 323–365. https://doi.org/10.2138/rmg.2021.86.10 Article history first online: 04 Jan 2021 Cite View This Citation Add to Citation Manager Share Icon Share Twitter LinkedIn Tools Icon Tools Get Permissions Search Site Citation D. O. Zakharov, J. Marin-Carbonne, J. Alleon, I. N. Bindeman; Triple Oxygen Isotope Trend Recorded by Precambrian Cherts: A Perspective from Combined Bulk and in situ Secondary Ion Probe Measurements. Reviews in Mineralogy and Geochemistry 2021;; 86 (1): 323–365. doi: https://doi.org/10.2138/rmg.2021.86.10 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 The surface temperature of a planet is one of the key parameters that define its potential habitablity. On Earth, the temperature regime sustained by the seawater column provided one of the necessary conditions for the evolution and prosperity of life. Ancient marine chemical sediments such as cherts and carbonates offer an opportunity to reconstruct the seawater temperature throughout geologic history, due to temperature-dependent fractionation of oxygen isotope ratios between the aqueous and mineral species. Pioneered by early work on the fractionation of 18O/16O ratio between calcite and seawater (McCrea 1950; Epstein et al. 1951;... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.