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The appearance of external links associated with a dataset does not constitute endorsement by the Department of Commerce/National Oceanic and Atmospheric Administration of external Web sites or the information, products or services contained therein. For other than authorized activities, the Department of Commerce/NOAA does not exercise any editorial control over the information you may find at these locations. These links are provided consistent with the stated purpose of this Department of Commerce/NOAA Web site."},"dataType":"PALEOCEANOGRAPHY","investigators":"Fan, W.; Jian, Z.; Chu, Z.; Dang, H.; Wang, Y.; Bassinot, F.C.; Han, X.; Bian, Y.","investigatorDetails":[{"firstName":"Weijia","lastName":"Fan","initials":"W.","orcId":null},{"firstName":"Zhimin","lastName":"Jian","initials":"Z.","orcId":"0000-0002-2037-3539"},{"firstName":"Zhihui","lastName":"Chu","initials":"Z.","orcId":null},{"firstName":"Haowen","lastName":"Dang","initials":"H.","orcId":"0000-0002-1320-4761"},{"firstName":"Yue","lastName":"Wang","initials":"Y.","orcId":"0000-0002-2733-6220"},{"firstName":"Franck","lastName":"Bassinot","initials":"F.C.","orcId":"0000-0003-2107-743X"},{"firstName":"Xiqiu","lastName":"Han","initials":"X.","orcId":null},{"firstName":"Yeping","lastName":"Bian","initials":"Y.","orcId":null}],"version":"1.0","funding":[],"studyNotes":"This dataset was contributed as part of the Temperature-12k project (https://doi.org/10.25921/4RY2-G808). Additional notes regarding the use of these data in the Temperature-12k project can be found in the LiPD file listed as an Online_Resource of this template file.","onlineResourceLink":"https://www.ncei.noaa.gov/access/paleo-search/study/30132","difMetadataLink":"https://www.ncei.noaa.gov/pub/data/metadata/published/paleo/dif/xml/noaa-ocean-30132.xml","isoMetadataLink":"https://www.ncei.noaa.gov/pub/data/metadata/published/paleo/iso/xml/noaa-ocean-30132.xml","originalSource":null,"dataTypeInformation":"https://www.ncei.noaa.gov/products/paleoclimatology/paleoceanography","studyCode":null,"scienceKeywords":null,"reconstruction":"Y","contributionDate":"2020-04-15","entryId":"noaa-ocean-30132","earliestYearBP":25045,"mostRecentYearBP":-6,"earliestYearCE":-23095,"mostRecentYearCE":1956,"publication":[{"author":{"name":"Fan, Weijia; Jian, Zhimin; Bassinot, Franck; Chu, Zhihui"},"pubYear":2013,"title":"Holocene centennial-scale changes of the Indonesian and South China Sea throughflows: Evidences from the Makassar Strait","journal":"Global and Planetary Change","volume":"111","edition":null,"issue":null,"pages":"111-117","reportNumber":null,"citation":"Fan, Weijia; Jian, Zhimin; Bassinot, Franck; Chu, Zhihui. 2013. Holocene centennial-scale changes of the Indonesian and South China Sea throughflows: Evidences from the Makassar Strait. Global and Planetary Change, 111, 111-117. doi: 10.1016/j.gloplacha.2013.08.017","type":"publication","identifier":{"type":"doi","id":"10.1016/j.gloplacha.2013.08.017","url":"http://dx.doi.org/10.1016/j.gloplacha.2013.08.017"},"abstract":null,"pubRank":"2"},{"author":{"name":"Fan, Weijia; Jian, Zhimin; Chu, Zhihui; Dang, Haowen; Wang, Yue; Bassinot, Franck; Han, Xiqiu; Bian, Yeping"},"pubYear":2018,"title":"Variability of the Indonesian throughflow in the Makassar Strait over the last 30 ka","journal":"Scientific Reports","volume":"8","edition":null,"issue":null,"pages":"5678","reportNumber":null,"citation":"Fan, Weijia; Jian, Zhimin; Chu, Zhihui; Dang, Haowen; Wang, Yue; Bassinot, Franck; Han, Xiqiu; Bian, Yeping. 2018. Variability of the Indonesian throughflow in the Makassar Strait over the last 30 ka. Scientific Reports, 8, 5678. doi: 10.1038/s41598-018-24055-1","type":"publication","identifier":{"type":"doi","id":"10.1038/s41598-018-24055-1","url":"http://dx.doi.org/10.1038/s41598-018-24055-1"},"abstract":"The hydrological characteristics, including temperatures and salinities, of the upper water over the last 30 ka from two sites connected by the Indonesian Throughflow (ITF) across the Makassar Strait are reconstructed and compared. The thermocline hydrological gradient in the strait was larger during 13.4~19 ka BP and 24.2~27 ka BP than that in the Holocene. The weakened ITF during those periods in the last glacial period, corresponding to the decreased trade wind stress under an El Niņo-like climate mean state, likely accounts for the increased thermocline gradient. The thermocline water temperature variabilities of the two sites, in particular the highest peaks at ~7 ka BP, are different from the records of the open western Pacific. Reoccurrence of the South China Sea Throughflow and thus a decreased surface throughflow along the Makassar Strait perhaps led to a warmer peak of thermocline temperature at ~7 ka BP than at ~11 ka BP.","pubRank":"1"},{"author":{"name":"Kaufman, D., McKay, N., Routson, C., et al."},"pubYear":2020,"title":"A global database of Holocene paleotemperature records","journal":"Scientific Data","volume":"7","edition":null,"issue":null,"pages":null,"reportNumber":"115","citation":"Kaufman, D., McKay, N., Routson, C., et al. 2020. A global database of Holocene paleotemperature records. 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