δ13C and δ18O values of Triassic brachiopods and carbonate rocks as proxies for coeval seawater and palaeotemperature
Top Cited Papers
- 25 August 2005
- journal article
- Published by Elsevier in Palaeogeography, Palaeoclimatology, Palaeoecology
- Vol. 226 (3-4) , 287-306
- https://doi.org/10.1016/j.palaeo.2005.05.018
Abstract
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This publication has 81 references indexed in Scilit:
- Deciphering kinetic, metabolic and environmental controls on stable isotope fractionations between seawater and the shell of Terebratalia transversa (Brachiopoda)Chemical Geology, 2003
- Timing the end-Triassic mass extinction: First on land, then in the sea?Geology, 2000
- Isotope stratigraphy of the European Carboniferous: proxy signals for ocean chemistry, climate and tectonicsPublished by Elsevier ,1999
- 87Sr/86Sr, δ13C and δ18O evolution of Phanerozoic seawaterPublished by Elsevier ,1999
- The abundance of 13C in marine organic matter and isotopic fractionation in the global biogeochemical cycle of carbon during the past 800 MaPublished by Elsevier ,1999
- Interpreting carbon-isotope excursions: carbonates and organic matterChemical Geology, 1999
- U/Pb zircon and baddeleyite ages for the Palisades and Gettysburg sills of the northeastern United States: Implications for the age of the Triassic/Jurassic boundaryGeology, 1990
- Determination of both chemical and stable isotope composition in milligramme-size carbonate samplesSedimentary Geology, 1989
- Permian-Triassic of the Tethys: Carbon isotope studiesInternational Journal of Earth Sciences, 1989
- Isotopic Composition and Origin of the Red Sea and Salton Sea Geothermal BrinesScience, 1966