2015
DOI: 10.1186/s40645-015-0045-6
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The Pliocene to recent history of the Kuroshio and Tsushima Currents: a multi-proxy approach

Abstract: The Kuroshio Current is a major western boundary current controlled by the North Pacific Gyre. It brings warm subtropical waters from the Indo-Pacific Warm Pool to Japan exerting a major control on Asian climate. The Tsushima Current is a Kuroshio offshoot transporting warm water into the Japan Sea. Various proxies are used to determine the paleohistory of these currents. Sedimentological proxies such as reefs, bedforms, sediment source and sorting reveal paleocurrent strength and latitude. Proxies such as cor… Show more

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Cited by 160 publications
(130 citation statements)
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“…However, this conclusion does not contradict the possible presence of this rhodaliid near the Philippines, where it could have arrived in the Kuroshio Current. The northward flow of this current may also justify the East China Sea record of A. typica (Qiu 2001), which is located fairly near the northern limit of coral growth in tropical waters in this region (see Gallagher et al 2015).…”
Section: Resultsmentioning
confidence: 99%
“…However, this conclusion does not contradict the possible presence of this rhodaliid near the Philippines, where it could have arrived in the Kuroshio Current. The northward flow of this current may also justify the East China Sea record of A. typica (Qiu 2001), which is located fairly near the northern limit of coral growth in tropical waters in this region (see Gallagher et al 2015).…”
Section: Resultsmentioning
confidence: 99%
“…Because the Kuroshio Current is a source of warm oligotrophic water, its influx into the Okinawa Trough was important for the evolution of modern oceanographic conditions in the northwest Pacific and climate conditions in Far East Asia Gallagher et al, 2015).…”
Section: Introductionmentioning
confidence: 99%
“…In SPEPS "Land-Ocean Linkages under the Influence of the Asian Monsoon," Gallagher et al (2015) reviewed the history of changes in intensities and courses of the Kuroshio and Tsushima Currents since the Pliocene. The Kuroshio Current is a major western boundary current in the North Pacific and the Tsushima Current branches from the Kuroshio and flows into the Japan Sea.…”
Section: Interdisciplinary Researchmentioning
confidence: 99%