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Spatial Distribution of Radiocarbon in the Southwestern Japan/East Sea Immediately After Bottom Water Renewal

Bibliographic Data

ID9243590
AuthorsTakafumi Aramaki, Shinichi S Tanaka, Seiko Kushibashi, Young-Il Kim (0000-0001-6806-4551), Chang-Jun Kim, Gi-Hoon Hong (0000-0003-4437-7232), Tomoharu Senjyu
Year2013
Volume55
Issue3
Pages1675-1682
Publication date2013-01-01
Open AccessYes
TypeARTICLE
VenueRadiocarbon (JOURNAL)
Journal identifiersISSN: 0033-8222 • E-ISSN: 1945-5755
PublisherCambridge University Press (CUP) (PUBLISHER)
DOI10.1017/s0033822200048591
OpenAlexW4237812195
LanguageEN
References cited21

In April 2001, immediately after bottom water renewal in the Japan/East Sea, 7 vertical profiles of radiocarbon were obtained from the area, including the Japan Basin and the Tsushima/Ulleung Basin. The bottom water Δ 14 C of the Tsushima/Ulleung Basin increased by 24% during 1979–2001 and was 10–15% higher than the values reported for the Japan Basin and Yamato Basin during 1995–2002. Within the depth interval 800–2000 m, Δ 14 C values at the southernmost station in the Japan Basin were much higher than at other stations, with the maximum difference in Δ 14 C values being more than 50%. Based on a combination of physical observations with analysis of the Δ 14 C data, we concluded that the bottom water, which was formed by the sinking of surface water off Vladivostok, Russia, in late January-early February of 2001, had been widely distributed to depths below 2000 m within the southernmost Japan Basin in a timespan shorter than 2 months. However, there was no evidence that the water had been transported into the Tsushima/Ulleung Basin during the same time interval

Bottom water · Geography · Geomorphology · Physical geography · Radiocarbon dating · Remote sensing · Spatial distribution · Structural basin · Surface water · Archaeology and ancient environmental studies · Environmental Science · Geology and Paleoclimatology Research · Isotope Analysis in Ecology · Geology · Oceanography · Paleontology

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    Open Access•T Aramaki, T Senjyu et al.•Radiocarbon•2007

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Highly citedNo

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