Advances in Carbon and Oxygen Isotopes and Clumped Isotope of Lacustrine Carbonates

被引：0
|
作者：
Li S. [1 ]
Guan P. [1 ]
机构：
[1] Key Laboratory of Orogenic Belts and Crustal Evolution (MOE), School of Earth and Space Sciences, Peking University, Beijing
来源：
Beijing Daxue Xuebao (Ziran Kexue Ban)/Acta Scientiarum Naturalium Universitatis Pekinensis | 2023年 / 59卷 / 06期
关键词：
carbon and oxygen isotopes; clumped isotope; lacustrine carbonate;
D O I：
10.13209/j.0479-8023.2023.067
中图分类号：
学科分类号：
摘要：
This paper reviews the progress of traditional carbon and oxygen isotope research of lacustrine carbonate and emerging clumped isotope research in recent years, summarizes their influencing mechanisms and applications in geological research, and discusses the problems in existing research. The oxygen isotope composition of lacustrine carbonates is less affected by temperature, which is mainly related to the evaporation and precipitation of lake water. The carbon isotope composition is jointly controlled by the evaporation and salinization of lake water and the interaction between organic matter and inorganic matter. The clumped isotope is only affected by the single factor of temperature and is a good carbonate thermometer. The paper points out two major directions for the study of carbon and oxygen isotopes of lacustrine carbonate: one is to solve the problems existing in the theoretical study of clumped isotopes, especially the resetting mechanism of clumped isotope temperature during burial; and the other is to combine traditional carbon and oxygen isotopes with emerging clumped isotope for comprehensive analysis of multi-index geochemistry, which can effectively resolve their limitation in geology research. © 2023 Peking University. All rights reserved.
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页码：1052 / 1068
页数：16
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  • [1] Urey H C., The thermodynamic properties of isotopic substances, Journal of the Chemical Society (Resumed), pp. 562-581, (1947)
  • [2] McCrea J M., On the isotopic chemistry of carbonates and a paleotemperature scale, The Journal of Chemical Physics, 18, 6, pp. 849-857, (1950)
  • [3] Westerhold T, Marwan N, Drury A J, Et al., An astronomically dated record of Earth’s climate and its predictability over the last 66 million years, Science, 369, pp. 1383-1388, (2020)
  • [4] Zachos J C, Dickens G R, Zeebe R E., An early cenozoic perspective on greenhouse warming and carbon-cycle dynamics, Nature, 451, pp. 279-283, (2008)
  • [5] Zachos J, Pagani M, Sloan L, Et al., Trends, rhythms, and aberrations in global climate 65 Ma to present, Science, 292, pp. 686-693, (2001)
  • [6] Hays J D, Imbrie J, Shackleton N J., Variations in the earth’s orbit: pacemaker of the ice ages, Science, 194, pp. 1121-1132, (1976)
  • [7] Shackleton N J, Matthews R K., Oxygen isotope stratigraphy of Late Pleistocene coral terraces in Barbados, Nature, 268, pp. 618-620, (1977)
  • [8] Kaufman A J, Knoll A H., Neoproterozoic variations in the C-isotopic composition of seawater: stratigraphic and biogeochemical implications, Precambrian Research, 73, 1, pp. 27-49, (1995)
  • [9] McInerney F A, Wing S L, Jeanloz R, Et al., The paleocene-eocene thermal maximum: a perturbation of carbon cycle, climate, and biosphere with implications for the future, Annual Review of Earth and Planetary Sciences, 39, 1, pp. 489-516, (2011)
  • [10] Payne J L, Kump L R., Evidence for recurrent early triassic massive volcanism from quantitative interpretation of carbon isotope fluctuations, Earth and Planetary Science Letters, 256, pp. 264-277, (2007)
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