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Oxygen isotopic composition of bottom seawater and tunicate cellulose used as indicators of water masses in the northern Bering and Chukchi Seas

Journal Article · · Limnology and Oceanography; (United States)
 [1]; ;  [2]
  1. Univ. of Southern California, Los Angeles (United States)
  2. Univ. of California, Santa Barbara (United States)
Oxygen isotopic composition of bottom seawater and tunicate cellulose were used as short-term and long-term indicators, respectively, of water-mass characteristics in the northern Bering and Chukchi Seas. Oxygen isotopic composition of northeastern Bering Sea waters is influenced by Yukon River inflows of {sup 18}O-depleted continental water mixing with relatively {sup 18}O-enriched waters contributed by the Anadyr Current. Tunicate cellulose sampled under Alaska coastal water is more depleted in {sup 18}O than that collected under Bering shelf and Anadyr waters, which reflects the oxygen isotopic composition of these waters. Tunicate cellulose collected under the mixed Bering shelf water displays intermediate {delta} {sup 18}O values. Oxygen isotopic analyses of bottom seawater were used to determine the spatial location and influence of continental and coastal-derived precipitation and of sea-ice formation on water-mass structure on the continental shelf of the northern Bering and Chukchi Seas. Results indicate that the oxygen isotopic composition of tunicate cellulose, averaged over multiple seasons, may serve as a long-term biochemical indicator of water-mass patterns in ice-covered polar regions where continuous sampling is impractical.
OSTI ID:
5967710
Journal Information:
Limnology and Oceanography; (United States), Journal Name: Limnology and Oceanography; (United States) Vol. 35:5; ISSN LIOCA; ISSN 0024-3590
Country of Publication:
United States
Language:
English