Article ID Journal Published Year Pages File Type
8884143 Continental Shelf Research 2017 24 Pages PDF
Abstract
The data suggest that organic carbon is mostly produced in situ, with glaciers serving as only a minor source. Calculated dependences indicated that carbonates close to the GF are of terrigenous origin and those at the FM almost exclusively biogenic. Carbonates originating from these two sources differ in their composition.
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Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Geology
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Distribution and origin of inorganic and organic carbon in the sediments of Kongsfjorden, Northwest Spitsbergen, European Arctic
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