Stable organic carbon isotopes in sediments of the north Bering-south Chukchi seas, Alaskan-Soviet Arctic Shelf

Stable organic carbon isotopes in sediments of the north Bering-south Chukchi seas, Alaskan-Soviet Arctic Shelf

The δ 13C and OC/N in carbonate-free sediments show an east to west cross-shelf trend within the north Bering-south Chukchi seas. Generally, the δ 13C increases from the river deltas (10) through the adjacent sound (8–10) to the open shelf (

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Veröffentlicht in:Continental shelf research 1993, Vol.13 (5), p.669-691
Hauptverfasser: Naidu, A.S., Scalan, R.S., Feder, H.M., Goering, J.J., Hameedi, M.J., Parker, P.L., Behrens, E.W., Caughey, M.E., Jewett, S.C.
Format: Artikel
Sprache:eng
Schlagworte:
Marine
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Zusammenfassung:The δ 13C and OC/N in carbonate-free sediments show an east to west cross-shelf trend within the north Bering-south Chukchi seas. Generally, the δ 13C increases from the river deltas (10) through the adjacent sound (8–10) to the open shelf (
ISSN:0278-4343
1873-6955
DOI:10.1016/0278-4343(93)90099-J