Triple Oxygen Isotope Systematics in the Hydrologic Cycle

Abstract

Research Article| January 01, 2021 Triple Oxygen Isotope Systematics in the Hydrologic Cycle Jakub Surma; Jakub Surma Institute of Geology and Mineralogy, University of Cologne, Zülpicher Straße 49b, Cologne, 50674, GermanyPresently at: Geoscience Center, Georg August University, Goldschmidtstraße 1 Göttingen, 37077, Germany * E-mail: jakub.surma@uni-goettingen.de Search for other works by this author on: GSW Google Scholar Sergey Assonov; Sergey Assonov Formerly at: Institute of Geology and Mineralogy, University of Cologne, Zülpicher Straße 49b Cologne, 50674, Germany Search for other works by this author on: GSW Google Scholar Michael Staubwasser Michael Staubwasser Institute of Geology and Mineralogy, University of Cologne, Zülpicher Straße 49b Cologne, 50674, Germany Search for other works by this author on: GSW Google Scholar Reviews in Mineralogy and Geochemistry (2021) 86 (1): 401–428. https://doi.org/10.2138/rmg.2021.86.12 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 Jakub Surma, Sergey Assonov, Michael Staubwasser; Triple Oxygen Isotope Systematics in the Hydrologic Cycle. Reviews in Mineralogy and Geochemistry 2021;; 86 (1): 401–428. doi: https://doi.org/10.2138/rmg.2021.86.12 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 analysis of hydrogen (δD) and oxygen (δ18O) isotope ratios of H2O are widely used tools for studies of the hydrological cycle (Friedman 1953; Dansgaard 1954; Gonfiantini 1986; Gat 1996; Araguás-Araguás et al. 2000; Gat et al. 2000) and climate reconstruction (Dansgaard 1964; Johnsen et al. 1989; Petit et al. 1999). Natural variations of δD and δ18O in precipitation are well correlated and fall on a common global trend, the Global Meteoric Water Line (GMWL, Craig 1961): δD=8·... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.