气候变化领域集成服务门户(CCPortal): Stable carbon isotopes in paleoceanography: atmosphere, oceans, and sediments

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DOI	10.1016/j.earscirev.2019.102893
	Stable carbon isotopes in paleoceanography: atmosphere, oceans, and sediments
	Mackensen A.; Schmiedl G.
发表日期	2019
ISSN	0012-8910
卷号	197
英文摘要	Carbon is one of the key elements in organisms and non-living compounds on Earth. Carbon dioxide and methane are important greenhouse gases in the atmosphere, dissolved inorganic (DIC) and organic carbon (DOC) determine water biogeochemistry, and carbonates are major constituents of marine sediments. Stable carbon isotope ratios (13C/12C), expressed as δ13C values, are widely used in modern Earth sciences. δ13CCO2 values of atmospheric carbon dioxide reflect global climate evolution and change. Marine δ13CDIC is used as water-mass tracer and helps quantifying the anthropogenic CO2 uptake of the ocean. The δ13C values of fossil planktic and benthic carbonates indicate changes in circulation pattern and deep-water ventilation of ancient oceans, as well as paleoproductivity at the sea surface and methane release at the sea floor. The δ13COM values of sedimentary organic matter (OM) and compound-specific δ13C values of molecular organic biomarkers indicate whether the organic carbon is of marine or terrestrial provenience. Secular δ13C variations and excursions in carbonates are important stratigraphic marker and tie points. Here we review the application of stable carbon isotope ratios in ocean water and biogenic carbonates as proxies in paleoceanography, including the atmospheric and sedimentary reservoirs oceanic carbon is in exchange with. Due to the wide use of δ13C values in Earth sciences, this overview necessarily does not claim to be complete; rather we focus on field-based stable carbon isotope research and its significance in paleoceanography. This may assist in evaluating general circulation model results and foster development of new innovative proxies. © 2019 Elsevier B.V.
语种	英语
scopus关键词	atmosphere; carbon isotope; carbon isotope ratio; carbonate rock; marine sediment; paleoceanography; stable isotope
来源期刊	EARTH-SCIENCE REVIEWS
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/209839
作者单位	Alfred Wegener Institute for Polar and Marine Research, Am Alten Hafen 26, Bremerhaven, 27568, Germany; Center for Earth System Research and Sustainability, Institute for Geology, University of Hamburg, Bundesstrasse 55, Hamburg, 20146, Germany
推荐引用方式 GB/T 7714	Mackensen A.,Schmiedl G.. Stable carbon isotopes in paleoceanography: atmosphere, oceans, and sediments[J],2019,197.
APA	Mackensen A.,&Schmiedl G..(2019).Stable carbon isotopes in paleoceanography: atmosphere, oceans, and sediments.EARTH-SCIENCE REVIEWS,197.
MLA	Mackensen A.,et al."Stable carbon isotopes in paleoceanography: atmosphere, oceans, and sediments".EARTH-SCIENCE REVIEWS 197(2019).