NOAA/WDS Paleoclimatology - Northwest Pacific ODP1208 Plio-Pleistocene Stable Isotope Data
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title: NOAA/WDS Paleoclimatology - Northwest Pacific ODP1208 Plio-Pleistocene Stable Isotope Data
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date: 2012-02-21
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Anchor: DOI doi:10.25921/hamy-bb98
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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 North Pacific Ocean. The time period coverage is from 3700000 to 1760000 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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fileDescription: Paleoclimatology - Paleoceanography
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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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date: 2020-01-09
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organisationName: NASA Goddard Space Flight Center, Earth Science Data and Information System
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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 > paleocean > oxygen isotopes
keyword: earth science > paleoclimate > paleocean > carbon isotopes
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keyword: What: depth; Material: null
keyword: What: age; Material: null
keyword: What: delta 18O; Material: Cibicidoides wuellerstorfi
keyword: What: delta 13C; Material: Cibicidoides wuellerstorfi
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keyword: Ocean > Pacific Ocean > North Pacific Ocean > ODP 1208 > LATITUDE 36.127 > LONGITUDE 158.2016
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keyword: DOC/NOAA/NESDIS/NCEI > National Centers for Environmental Information, NESDIS, NOAA, U.S. Department of Commerce
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name: Global Change Master Directory (GCMD) Keywords
description: The information provided on this page seeks to define how the GCMD Keywords are structured, used and accessed. It also provides information on how users can participate in the further development of the keywords.
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otherConstraints: Cite as: Venti, N.L.; Billups, K. (2012-02-21): NOAA/WDS Paleoclimatology - Northwest Pacific ODP1208 Plio-Pleistocene Stable Isotope Data. [indicate subset used]. NOAA National Centers for Environmental Information. https://doi.org/10.25921/hamy-bb98. Accessed [date].
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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: Stable-isotope stratigraphy of the Pliocene-Pleistocene climate transition in the northwestern subtropical Pacific
date: (CI_Date)
date: 2012
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individualName: Venti, N.L. and K. Billups
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organisationName: Palaeogeography, Palaeoclimatology, Palaeoecology
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description: Venti, N.L. and K. Billups, 2012: Stable-isotope stratigraphy of the Pliocene-Pleistocene climate transition in the northwestern subtropical Pacific. Palaeogeography, Palaeoclimatology, Palaeoecology, 326–328, 54-65, 10.1016/j.palaeo.2012.02.001
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description: Date Range: 3700000 cal yr BP to 1760000 cal yr BP;
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westBoundLongitude: 158.2016
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southBoundLatitude: 36.127
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supplementalInformation: STUDY NOTES: Foraminiferal stable isotope (d18O and d13C) were measured via mass spectrometry at orbital-scale resolution (10-cm spacing, or ~2.5 kyr timestep) for the Pliocene-Pleistocene (1.760-3.700 Ma) section in tests of the epifaunal benthic foraminifer Planulina wuellerstorfi. Sample averages only are presented here. The age model is derived by tuning the d18O record to the global stack of Lisiecki and Raymo (2005). ABSTRACT SUPPLIED BY ORIGINATOR: From Ocean Drilling Program (ODP) Site 1208 on Shatsky Rise below the Kuroshio Current Extension, we present the North Pacific's first orbital-scale benthic foraminiferal d18O and d13C time series to span the Pliocene-Pleistocene climate transition. Excellent agreement between the Site 1208 d18O record and the global d18O stack of Lisiecki and Raymo (2005) provides orbital-scale age control and confirms continuous stratigraphy from 3.7 to 1.8 Ma at the single-hole site. Cross-spectral analysis of the d18O and d13C time series reveals that these are coherent to 80% confidence at the 41-kyr obliquity band prior to 3.3 Ma (glacial isotope stage M2) and increase to the 95% level thereafter. Throughout, d18O cycles consistently lead d13 C cycles by ~ 3 kyr. This suggests that global-ocean d13C variations, as produced by terrestrial-marine 12C transfers, were responsive to obliquity-induced climate changes before the Northern Hemisphere glaciations (NHG) reached mid latitudes at 2.7 Ma. In contrast, 41-kyr carbonate sedimentation (as derived from sediment reflectance) cycles, maxima tightly coupled to (>95% confidence) and in phase with minima in the d18O record, do not emerge until 2.7 Ma. Foraminiferal fragmentation counts indicate that carbonate preservation is not the primary process behind enhanced carbonate deposition during interglacials. Thus, we surmise that hydrography-related changes in biogenic opal and carbonate production in surface water best explain glacial-interglacial carbonate cycles beginning with significant NHG. Firm establishment of orbital-scale age control on the stratigraphically complete Site 1208 section now provides a platform for high-resolution paleoceanographic reconstruction of the relatively understudied North Pacific.
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fees: In most cases, electronic downloads of the data are free. However, fees may apply for custom orders, data certifications, copies of analog materials, and data distribution on physical media.
orderingInstructions: Contact NCEI for other distribution options and instructions.
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maintenanceNote: This ISO metadata record was translated from DIF metadata using dif-9x-to-iso-19115-2.xsl Version: 2022-06-21