On the 14C and 39Ar Distribution in the Central Arctic Ocean: Implications for Deep Water Formation

• Published in: Radiocarbon
• Main Authors: Schlosser, Peter, Kromer, Bernd, Östlund, Gote, Ekwurzel, Brenda, Bönisch, Gerhard, Loosli, H. H., Purtschert, Roland
• Format: Article in Journal/Newspaper
• Language: English
• Published: Department of Geosciences, The University of Arizona 1994
• Subjects: isolation age; Ar 39; argon; Amundsen Basin; Makarov Basin; Nansen Basin; Arctic Ocean; depth; noble gases; ocean circulation; residence time; sea water; C 14; carbon; isotopes; radioactive isotopes; geochemistry; Arctic; Canada; amundsen basin; Central Arctic; makarov basin
• Online Access: http://hdl.handle.net/10150/653354; https://doi.org/10.1017/S003382220001451X

We present Delta-14C and 39Ar data collected in the Nansen, Amundsen and Makarov basins during two expeditions to the central Arctic Ocean (RV Polarstern cruises ARK IV/3, 1987 and ARK VIII/3,1991). The data are used, together with published Delta-14C values, to describe the distribution of Delta-14C in all major basins of the Arctic Ocean (Nansen, Amundsen, Makarov and Canada Basins), as well as the 39Ar distribution in the Nansen Basin and the deep waters of the Amundsen and Makarov Basins. From the combined Delta-14C and 39Ar distributions, we derive information on the mean "isolation ages" of the deep and bottom waters of the Arctic Ocean. The data point toward mean ages of the bottom waters in the Eurasian Basin (Nansen and Amundsen Basins) of ca. 250-300 yr. The deep waters of the Amundsen Basin show slightly higher 3H concentrations than those in the Nansen Basin, indicating the addition of a higher fraction of water that has been at the sea surface during the past few decades. Correction for the bomb 14C added to the deep waters along with bomb 3H yields isolation ages for the bulk of the deep and bottom waters of the Amundsen Basin similar to those estimated for the Nansen Basin. This finding agrees well with the 39Ar data. Deep and bottom waters in the Canadian Basin (Makarov and Canada Basins) are very homogeneous, with an isolation age of ca. 450 yr. Delta-14C and 39Ar data and a simple inverse model treating the Canadian Basin Deep Water (CBDW) as one well-mixed reservoir renewed by a mixture of Atlantic Water (29%), Eurasian Basin Deep Water (69%) and brine-enriched shelf water (2%) yield a mean residence time of CBDW of ca. 300 yr. This material was digitized as part of a cooperative project between Radiocarbon and the University of Arizona Libraries. The Radiocarbon archives are made available by Radiocarbon and the University of Arizona Libraries. Contact [e-mail] for further information. Migrated from OJS platform February 2021