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Holocene methane emissions in the South-Western part of the Okhotsk Sea (on the basic of carbon isotopes in the tests of benthic foraminifera)
Author(s) -
С. П. Плетнев,
Alexandra Romanova,
Yonghua Wu,
В. К. Аннин,
I. V. Utkin,
О. Ф. Верещагина
Publication year - 2019
Publication title -
doklady akademii nauk. rossijskaâ akademiâ nauk
Language(s) - English
Resource type - Journals
ISSN - 0869-5652
DOI - 10.31857/s0869-5652488191-93
Subject(s) - foraminifera , benthic zone , holocene , methane , oceanography , geology , isotopes of carbon , methane emissions , total organic carbon , greenhouse gas , environmental chemistry , ecology , chemistry , biology
We report several negative carbon stable isotope excursions in benthic foraminifera in a gas-bearing core LV50-05, collected from an area of active methane venting on the Eastern Slope of Sakhalin Island, the Okhotsk Sea. Within the study area, four methane events (ME) are established in Holocene: short-term ME-1 (700-900 yr BP) and ME-2 (from 1200 to 1400 yr BP), long-term ME-3 (2500-4700 yr BP) and ME-4 (7400-10000 yr BP).

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