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Lein, Alla Yu (2004): Chemical and isotopic compositions of ocean authigenic carbonates [dataset publication series]. P.P. Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow, PANGAEA, https://doi.org/10.1594/PANGAEA.785878, Supplement to: Lein, AY (2004): Authigenic Carbonate Formation in the Ocean. Lithology and Mineral Resources, 39(1), 1-30, https://doi.org/10.1023/B:LIMI.0000010767.52720.8f

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Published: 2004 (exact date unknown) • DOI registered: 2012-08-08

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Abstract:
Oceanic authigenic carbonates are classified according to origin of the carbonate carbon source using a complex methodology that includes methods of sedimentary petrography, mineralogy, isotope geochemistry, and microbiology. Mg-calcite (protodolomite) and aragonite predominate among the authigenic carbonates. All authigenic carbonates are depleted in 13C and enriched in 18O (in PDB system) that indicates biological fractionation of isotopes during carbonate formation. Obtained results show that authigenic carbonate formation is a biogeochemical (microbial) process, which involves carbon from ancient sedimentary rocks, abiogenic methane, and bicarbonate-ion of hydrothermal fluids into the modern carbon cycle.
Project(s):
Archive of Ocean Data (ARCOD)
Coverage:
Median Latitude: 33.782900 * Median Longitude: -141.211583 * South-bound Latitude: 24.895000 * West-bound Longitude: 155.302000 * North-bound Latitude: 50.515000 * East-bound Longitude: -108.700000
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
3 datasets

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Datasets listed in this publication series

  1. Lein, AY (2004): (Table 3) Isotopic composition of pyrite sulfur and carbonate carbon in carbonate nodules and host sediments from Core DM9-666, Gulf of California. https://doi.org/10.1594/PANGAEA.785873
  2. Lein, AY (2004): (Table 4) Changes in chemical composition of pore waters and δ¹³C-CaCO3 of dispersed authigenic carbonates from reduced bottom sediments of the Gulf of California. https://doi.org/10.1594/PANGAEA.785876
  3. Lein, AY (2004): (Table 6) Intensity of methane generation and methane oxidation in bottom sediments (thickness 200 cm) and water column in the methane seepage area of the Sea of Okhotsk. https://doi.org/10.1594/PANGAEA.785877