Organic carbon isotope ratios of sea surface sediments and sea-ice from the Amerasian Continental shelf
Organic matter origins are inferred from carbon isotope ratios (delta13C) in recent continental shelf sediments and major rivers from 465 locations from the north Bering-Chukchi-East Siberian-Beaufort Sea, Arctic Amerasia. Generally, there is a cross-shelf increase in delta13C, which is due to progr...
Main Authors: | , , , , , |
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Format: | Other/Unknown Material |
Language: | English |
Published: |
PANGAEA
2000
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.712053 https://doi.org/10.1594/PANGAEA.712053 |