https://scholars.lib.ntu.edu.tw/handle/123456789/440452
DC 欄位 | 值 | 語言 |
---|---|---|
dc.contributor.author | Lo, L. | en_US |
dc.contributor.author | Lai, Y.-H. | en_US |
dc.contributor.author | Wei, K.-Y. | en_US |
dc.contributor.author | Lin, Y.-S. | en_US |
dc.contributor.author | Mii, H.-S. | en_US |
dc.contributor.author | LI LO | en_US |
dc.contributor.author | CHUAN-CHOU SHEN | en_US |
dc.contributor.author | KUO-YEN WEI | en_US |
dc.creator | Lo, L. | - |
dc.creator | Lai, Y.-H. | - |
dc.creator | Wei, K.-Y. | - |
dc.creator | Lin, Y.-S. | - |
dc.creator | Mii, H.-S. | - |
dc.creator | Shen, C.-C. | - |
dc.date.accessioned | 2019-12-25T07:13:45Z | - |
dc.date.available | 2019-12-25T07:13:45Z | - |
dc.date.issued | 2013 | - |
dc.identifier.uri | https://www.scopus.com/inward/record.uri?eid=2-s2.0-84875364824&doi=10.1016%2fj.jseaes.2013.01.014&partnerID=40&md5=e6f1632a9a88676fa055ed0ded875183 | - |
dc.identifier.uri | https://scholars.lib.ntu.edu.tw/handle/123456789/440452 | - |
dc.description.abstract | To understand Holocene climate evolutions in low-latitude region of the western Pacific, paired δ18O and Mg/Ca records of planktonic foraminifer Globigerinoides ruber (250-300μm, sensu stricto, s.s.) from a marine core ORI715-21 (121.5°E, 22.7°N, water depth 760m) underneath the Kuroshio Current (KC) off eastern Taiwan were analyzed. Over the past 7500years, the geochemical proxy-inferred sea surface temperature (SST) hovered around 27-28°C and seawater δ18O (δ18OW) slowly decreased 0.2-0.4‰ for two KC sites at 22.7° and 25.3°N. Comparison with a published high-SST and high-salinity equatorial tropical Pacific record, MD98-2181 located at the Mindanao Current (MC) at 6.3°N, reveals an anomalous time interval at 3.5-1.5kyr ago (before 1950 AD). SST gradient between the MC site and two KC site decrease from 1.5-2.0°C to only 0-1°C, and δ18OW from 0.1-0.3‰ to 0‰ for this 2-kyr time window. The high SST and low gradient could result from a northward shift of the North Equatorial Current, which implies a weakened KC. The long-term descending δ18OW and increasing precipitation in the entire low-latitude western Pacific and the gradually decreasing East Asian summer monsoonal rainfall during middle-to-late Holocene is likely caused by different land and ocean responses to solar insolation and/or enhanced moisture transportation from the Atlantic to Pacific associated with the southward movement of ITCZ. © 2013 Elsevier Ltd. | - |
dc.relation.ispartof | Journal of Asian Earth Sciences | - |
dc.subject.classification | [SDGs]SDG13 | - |
dc.subject.other | climate variation; Holocene; monsoon; paleoceanography; precipitation (climatology); rainfall; sea surface salinity; sea surface temperature; seawater; temperature gradient; Atlantic Ocean; Kuroshio Current; Mindanao Current; North Equatorial Current; Pacific Ocean; Pacific Ocean (Northwest); Pacific Ocean (Tropical); Taiwan; Foraminifera; Globigerinoides ruber | - |
dc.title | Persistent sea surface temperature and declined sea surface salinity in the northwestern tropical Pacific over the past 7500years | en_US |
dc.type | journal article | en |
dc.identifier.doi | 10.1016/j.jseaes.2013.01.014 | - |
dc.relation.pages | 234-239 | - |
dc.relation.journalvolume | 66 | - |
item.openairetype | journal article | - |
item.fulltext | no fulltext | - |
item.openairecristype | http://purl.org/coar/resource_type/c_6501 | - |
item.grantfulltext | none | - |
item.cerifentitytype | Publications | - |
crisitem.author.dept | Geosciences | - |
crisitem.author.dept | Geosciences | - |
crisitem.author.orcid | 0000-0003-2833-2771 | - |
crisitem.author.orcid | 0000-0002-2725-5762 | - |
crisitem.author.parentorg | College of Science | - |
crisitem.author.parentorg | College of Science | - |
顯示於: | 地質科學系 |
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