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Western Indian Ocean results show a strong<jats:sup>14</jats:sup>C depletion due to upwelling in the Arabian Sea, and indicate that this signal is advected over a wide area to the east and south. In contrast, the surface waters of the South China Sea contain relatively high levels of<jats:sup>14</jats:sup>C, due in part to the input of well-equilibrated water masses from the western Pacific. The easternmost regions of the Indian Ocean are also strongly influenced by the flowthrough of Pacific waters north of Australia.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1382825896060632580","@type":"Researcher","foaf:name":[{"@value":"John Southon"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825896060632579","@type":"Researcher","foaf:name":[{"@value":"Michaele Kashgarian"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825896060632578","@type":"Researcher","foaf:name":[{"@value":"Michel Fontugne"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825896060632577","@type":"Researcher","foaf:name":[{"@value":"Bernard Metivier"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825896060632576","@type":"Researcher","foaf:name":[{"@value":"Wyss W-S Yim"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00338222"},{"@type":"EISSN","@value":"19455755"}],"prism:publicationName":[{"@value":"Radiocarbon"}],"dc:publisher":[{"@value":"Cambridge University Press 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