NOAA/WDS Paleoclimatology - Coral Sea foram counts and sea surface temperature at the Last Glacial Maximum
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organisationName: NOAA World Data Service for Paleoclimatology
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title: NOAA/WDS Paleoclimatology - Coral Sea foram counts and sea surface temperature at the Last Glacial Maximum
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date: 2005-01-18
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Anchor: DOI doi:10.25921/f6q4-ak45
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abstract: This archived Paleoclimatology Study is available from the NOAA National Centers for Environmental Information (NCEI), under the World Data Service (WDS) for Paleoclimatology. The associated NCEI study type is Paleoceanography. The data include parameters of paleoceanography with a geographic location of South Pacific Ocean. The time period coverage is from Unavailable begin date to Unavailable end date in calendar years before present (BP). See metadata information for parameter and study location details. Please cite this study when using the data.
purpose: Records of past climate and ocean circulation derived from marine sediments. Parameter keywords describe what was measured in this dataset. Additional summary information can be found in the abstracts of papers listed in the dataset citations.
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keyword: Earth Science > Paleoclimate > Ocean/Lake Records
keyword: Earth Science > Climate Indicators > Paleoclimate Indicators > Ocean/Lake Records
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keyword: earth science > paleoclimate > paleoceanography
keyword: earth science > paleoclimate > paleoceanography
keyword: earth science > paleoclimate > paleoceanography
keyword: earth science > paleoclimate > paleoceanography
keyword: earth science > paleoclimate > paleoceanography
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keyword: earth science > paleoclimate > climate reconstructions|paleoceanography
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keyword: earth science > paleoclimate > paleoceanography
keyword: earth science > paleoclimate > paleoceanography
keyword: earth science > paleoclimate > paleocean > population abundance
keyword: earth science > paleoclimate > paleocean > lithology
keyword: earth science > paleoclimate > paleocean > reconstruction
keyword: earth science > paleoclimate > paleocean > oxygen isotopes
keyword: earth science > paleoclimate > paleocean > other
keyword: earth science > paleoclimate > paleocean > carbon isotopes
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keyword: What: Neogloboquadrina dutertrei; Material: null
keyword: What: identified foraminifer; Material: null
keyword: What: delta 18O; Material: Trilobatus sacculifer
keyword: What: Globigerinella siphonifera; Material: null
keyword: What: Orbulina universa; Material: null
keyword: What: Neogloboquadrina pachyderma sinistral; Material: null
keyword: What: identified foraminifer; Material: null
keyword: What: identified foraminifer; Material: null
keyword: What: Trilobatus sacculifer with sac; Material: null
keyword: What: Pulleniatina obliquiloculata; Material: null
keyword: What: Globorotalia hirsuta; Material: null
keyword: What: Neogloboquadrina pachyderma dextral; Material: null
keyword: What: delta 13C; Material: Trilobatus sacculifer
keyword: What: identified foraminifer; Material: null
keyword: What: sea surface temperature; Material: null
keyword: What: Globorotalia truncatulinoides; Material: null
keyword: What: identified foraminifer; Material: null
keyword: What: Globorotalia truncatulinoides; Material: null
keyword: What: identified foraminifer; Material: null
keyword: What: identified foraminifer; Material: null
keyword: What: identified foraminifer; Material: null
keyword: What: Globigerina bulloides; Material: null
keyword: What: Globigerinoides ruber white; Material: null
keyword: What: Trilobatus sacculifer without sac; Material: null
keyword: What: sea surface temperature; Material: null
keyword: What: Globorotalia crassaformis; Material: null
keyword: What: Globigerinoides ruber pink; Material: null
keyword: What: identified foraminifer; Material: null
keyword: What: calcium carbonate; Material: sediment
keyword: What: calcium carbonate; Material: null
keyword: What: Globorotalia tumida; Material: null
keyword: What: identified foraminifer; Material: null
keyword: What: identified foraminifer; Material: null
keyword: What: Globorotalia inflata; Material: null
keyword: What: Globorotalia menardii; Material: null
keyword: What: identified foraminifer; Material: null
keyword: What: identified foraminifer; Material: null
keyword: What: identified foraminifer; Material: null
keyword: What: depth; Material: null
keyword: What: identified foraminifer; Material: null
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keyword: Ocean > Pacific Ocean > South Pacific Ocean > V24-170 > LATITUDE -13.52 > LONGITUDE 146.88
keyword: Ocean > Pacific Ocean > South Pacific Ocean > V24-157 > LATITUDE -14.95 > LONGITUDE 147.92
keyword: Ocean > Pacific Ocean > South Pacific Ocean > RC12-113 > LATITUDE -24.88 > LONGITUDE 163.52
keyword: Ocean > Pacific Ocean > South Pacific Ocean > V24-161 > LATITUDE -18.2 > LONGITUDE 151.45
keyword: Ocean > Pacific Ocean > South Pacific Ocean > V24-167 > LATITUDE -15.28 > LONGITUDE 148.05
keyword: Ocean > Pacific Ocean > South Pacific Ocean > V24-184 > LATITUDE -12.87 > LONGITUDE 146.2
keyword: Ocean > Pacific Ocean > South Pacific Ocean > RC10-131 > LATITUDE -14.53 > LONGITUDE 157.97
keyword: Ocean > Pacific Ocean > South Pacific Ocean > RC12-109 > LATITUDE -25.88 > LONGITUDE 157.87
keyword: Ocean > Pacific Ocean > South Pacific Ocean > V24-166 > LATITUDE -16.52 > LONGITUDE 148.05
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otherConstraints: Distribution liability: NOAA and NCEI make no warranty, expressed or implied, regarding these data, nor does the fact of distribution constitute such a warranty. NOAA and NCEI cannot assume liability for any damages caused by any errors or omissions in these data. If appropriate, NCEI can only certify that the data it distributes are an authentic copy of the records that were accepted for inclusion in the NCEI archives.
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otherConstraints: Use liability: NOAA and NCEI cannot provide any warranty as to the accuracy, reliability, or completeness of furnished data. Users assume responsibility to determine the usability of these data. The user is responsible for the results of any application of this data for other than its intended purpose.
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otherConstraints: Please cite original publication, online resource, dataset and publication DOIs (where available), and date accessed when using downloaded data. If there is no publication information, please cite investigator, title, online resource, and date accessed. 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.
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title: Estimates of sea surface temperature in the Coral Sea at the last glacial maximum
date: (CI_Date)
date: 1989
dateType: (CI_DateTypeCode) publication
citedResponsibleParty: (CI_ResponsibleParty)
individualName: Anderson, D.M., W.L. Prell, and N.J. Barratt
role: (CI_RoleCode) author
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organisationName: Paleoceanography
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linkage: https://doi.org/10.1029/PA004i006p00615
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name: Associated Reference published 1989
description: Anderson, D.M., W.L. Prell, and N.J. Barratt, 1989: Estimates of sea surface temperature in the Coral Sea at the last glacial maximum. Paleoceanography, 4, 615-627, 10.1029/PA004i006p00615
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language: eng; USA
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description: Paleo date information not available.
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westBoundLongitude: 146.2
eastBoundLongitude: 163.52
southBoundLatitude: -25.88
northBoundLatitude: -12.87
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TimePeriod:
beginPosition: 1950
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supplementalInformation: ABSTRACT SUPPLIED BY ORIGINATOR: The CLIMAP [1981] reconstruction of the Coral Sea found relatively little cooling (2°C) in the low latitudes (10°S) but a warming off Australia at about 25°S. The small low-latitude changes are of interest because terrestrial pollen and snowline data from the New Guinea highlands imply that surface temperatures may have been 6° to 9°C colder at the last glacial maximum (LGM). The purpose of this paper is to evaluate these conclusions on the basis of additional core sites, new oxygen isotope stratigraphy, and new sea surface temperature (SST) estimates using the modern analog technique (MAT). In the northern Coral Sea, planktonic foraminifer assemblages consist of tropical-subtropical species that show little change over the past 20 kyr. Quantitative estimates of SST using the modern analog technique (MAT) confirm the CLIMAP [1981] conclusion that little or no temperature change occurred in this tropical region at the LGM, thus reinforcing the conflict with terrestrial evidence. In the southern region (25°S), two cores indicate that foraminifer faunas became more subtropical at the LGM. The MAT estimates for the LGM are 3° to 4°C colder than modern, producing a steeper thermal gradient in the southern Coral Sea. These data remove the warm SST anomaly along the eastern coast of Australia and indicate that during the LGM, cool high- latitude waters were displaced northward along the coast of Australia into the southern Coral Sea.
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