NOAA/WDS Paleoclimatology - West Greenland 9,500 Year Multiproxy Lake Sediment Data
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fileIdentifier: noaa-lake-13116
language: eng; USA
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electronicMailAddress: ncei.info@noaa.gov
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description: Information for contacts at NCEI.
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organisationName: NOAA World Data Service for Paleoclimatology
positionName: Data Center Contact
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voice: 828-271-4800
facsimile: 303-497-6513
address: (CI_Address)
deliveryPoint: 325 Broadway, E/NE31
city: Boulder
administrativeArea: CO
postalCode: 80305-3328
country: USA
electronicMailAddress: paleo@noaa.gov
role: (CI_RoleCode) pointOfContact
dateStamp: 2024-02-22
metadataStandardName: ISO 19115-2 Geographic Information - Metadata - Part 2: Extensions for Imagery and Gridded Data
metadataStandardVersion: ISO 19115-2:2009(E)
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identificationInfo: (MD_DataIdentification)
citation: (CI_Citation)
title: NOAA/WDS Paleoclimatology - West Greenland 9,500 Year Multiproxy Lake Sediment Data
date: (CI_Date)
date: 2012-06-30
dateType: (CI_DateTypeCode) publication
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identifier: (MD_Identifier)
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Anchor: DOI doi:10.25921/v15d-7q90
identifier: (MD_Identifier)
code: noaa-lake-13116
identifier: (MD_Identifier)
code: NCEI DSI 1200_02
identifier: (MD_Identifier)
code: NCEI DSI 1200_01
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individualName: Perren, B.
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individualName: Perren, B.
role: (CI_RoleCode) author
citedResponsibleParty: (CI_ResponsibleParty)
individualName: Anderson, N.J.
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individualName: Anderson, N.J.
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individualName: Douglas, M.S.V.
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individualName: Douglas, M.S.V.
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individualName: Fritz, S.C.
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individualName: Fritz, S.C.
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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 Lake. The data include parameters of paleolimnology with a geographic location of Greenland. The time period coverage is from 9534 to -50 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 environment derived from lake sediment records. 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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organisationName: NOAA World Data Service for Paleoclimatology
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country: USA
electronicMailAddress: paleo@noaa.gov
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graphicOverview: (MD_BrowseGraphic)
fileName: https://www.ncei.noaa.gov/pub/data/paleo/webimages/pc-default-lake.png
fileDescription: Paleoclimatology - Lake
fileType: PNG
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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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keyword: What: identified diatom; Material: null
keyword: What: identified diatom; Material: null
keyword: What: identified diatom; Material: null
keyword: What: identified diatom; Material: null
keyword: What: identified diatom; Material: null
keyword: What: identified diatom; Material: null
keyword: What: identified diatom; Material: null
keyword: What: identified diatom; Material: null
keyword: What: identified diatom; Material: null
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keyword: What: identified diatom; Material: null
keyword: What: identified diatom; Material: null
keyword: What: identified diatom; Material: null
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keyword: What: identified diatom; Material: null
keyword: What: identified diatom; Material: null
keyword: What: identified diatom; Material: null
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keyword: What: organic matter; Material: sediment
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keyword: What: identified diatom; Material: null
keyword: What: identified diatom; Material: null
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keyword: What: identified diatom; Material: null
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keyword: What: identified diatom; Material: null
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keyword: What: identified diatom; Material: null
keyword: What: identified diatom; Material: null
keyword: What: identified diatom; Material: null
keyword: What: identified diatom; Material: null
keyword: What: identified diatom; Material: null
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keyword: What: identified diatom; Material: null
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keyword: What: identified diatom; Material: null
keyword: What: identified diatom; Material: null
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keyword: What: identified diatom; Material: null
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keyword: Continent > North America > Greenland > SS16 > LATITUDE 66.91 > LONGITUDE -50.46
keyword: Continent > North America > Greenland > SS32 > LATITUDE 66.97 > LONGITUDE -49.8
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otherConstraints: Cite as: Perren, B.; Anderson, N.J.; Douglas, M.S.V.; Fritz, S.C. (2012-06-30): NOAA/WDS Paleoclimatology - West Greenland 9,500 Year Multiproxy Lake Sediment Data. [indicate subset used]. NOAA National Centers for Environmental Information. https://doi.org/10.25921/v15d-7q90. Accessed [date].
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title: The influence of temperature, moisture, and eolian activity on Holocene lake development in West Greenland
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date: 2012
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description: Perren, B.B., N.J. Anderson, M.S.V. Douglas, and S.C. Fritz, 2012: The influence of temperature, moisture, and eolian activity on Holocene lake development in West Greenland. Journal of Paleolimnology, 48, 223-239, 10.1007/s10933-012-9613-6
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language: eng; USA
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description: Date Range: 9534 cal yr BP to -50 cal yr BP;
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westBoundLongitude: -52.64
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supplementalInformation: STUDY NOTES: Multiproxy Holocene sediment data from 3 lakes in west Greenland. Paleoenvironmental proxies measured include diatoms, organic content, and spectrally inferred sediment chlorophyll-a. West Greenland lake locations: SS32(Nunatak): 66.97°N, 49.80°W, 470m elevation, 21m water depth. SS16: 66.91°N, 50.46°W, 477m elevation, 12m water depth. SS49: 66.86°N, 52.64°W, 330m elevation, 10m water depth. ABSTRACT SUPPLIED BY ORIGINATOR: Holocene paleolimnological records (diatoms, organic content, spectrally inferred sediment chlorophyll-a) from three West Greenland lakes (~67°N) situated along a transect from the outer coast to a nunatak at the periphery of the Greenland Ice Sheet are used to explore the nature of regional postglacial lake development and its relationship to Holocene climate evolution. The lakes were deglaciated asynchronously by approximately 4 ka (earliest on the coast) and thus their sediment records document different starting points of Holocene ontogeny, both temporally and paleoclimatically. Despite similar time-transgressive characteristics of the diatom stratigraphies, overarching climatic factors, principally effective moisture, and eolian inputs, govern individual lake development. The transition to Neoglaciation between 5.6 and 4 ka BP marks a shift toward a cooler, moister, windier climate from the aridity and higher temperatures of the mid-Holocene (8–6 ka BP). A shift toward increased aridity, windiness, and eolian activity is documented in the interior lakes over the last 500 years. These lake records demonstrate the sensitivity of freshwater lakes in arid regions to changes in effective moisture and highlight the role of wind and eolian activity in Arctic lake environments.
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