Please use this identifier to cite or link to this item: http://hdl.handle.net/2440/59155
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dc.contributor.authorZhao, Q.en
dc.contributor.authorLi, Q.en
dc.contributor.authorJian, Z.en
dc.date.issued2009en
dc.identifier.citationThe South China Sea: Paleoceanography and Sedimentology, 2009 / Wang, P., Li, Q. (ed./s), pp.395-438en
dc.identifier.isbn9781402097454en
dc.identifier.urihttp://hdl.handle.net/2440/59155-
dc.description.abstractAmong the low to mid latitude western Pacific marginal seas are the South China Sea (SCS), Sulu Sea and Sea of Japan, the three major enclosed seas in the region with passages connecting to the open ocean. The passage sill depths are ∼130m for the Sea of Japan, ∼420m for the Sulu Sea, and ∼2,400m for the SCS. Therefore, water exchanges with the deeper ocean are more effective in the SCS than in other sea basins. The last 30 Ma deep water history since seafloor spreading in the SCS is a history of basin evolution relating especially to subsidence and sediment preservation, as well as changes in deep water properties. The long sequence recovered at ODP Site 1148 provides a unique opportunity to trace this history. In this chapter, we overview recent progresses of deep water research in the region by focusing on benthic foraminiferal, ostracod and isotopic geochemistry records from Site 1148.en
dc.description.statementofresponsibilityQuanhong Zhao, Qianyu Li and Zhimin Jianen
dc.language.isoenen
dc.publisherSpringeren
dc.relation.ispartofseriesDevelopments in paleoenvironmental research ; v. 13en
dc.rightsCopyright Springer Science + Business Media B.V. 2009en
dc.titleDeep waters and oceanic connectionen
dc.typeBook chapteren
dc.identifier.rmid0020097946en
dc.identifier.doi10.1007/978-1-4020-9745-4_6en
dc.publisher.placeDordrecht, Netherlandsen
dc.identifier.pubid34069-
pubs.library.collectionEarth and Environmental Sciences publicationsen
pubs.verification-statusVerifieden
pubs.publication-statusPublisheden
Appears in Collections:Earth and Environmental Sciences publications

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