NOAA/WDS Paleoclimatology - Elk Lake, Minnesota 12,000 Year Ostracod Abundance and Geochemical Data
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organisationName: NOAA World Data Service for Paleoclimatology
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title: NOAA/WDS Paleoclimatology - Elk Lake, Minnesota 12,000 Year Ostracod Abundance and Geochemical Data
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date: 2000-01-01
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Anchor: DOI doi:10.25921/ecrb-ev92
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code: noaa-lake-6064
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code: NCEI DSI 1200_02
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individualName: Smith, A.J.
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individualName: Donovan, J.J.
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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 Minnesota, United States Of America. 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 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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fileDescription: Paleoclimatology - Lake
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keyword: Earth Science > Climate Indicators > Paleoclimate Indicators > Ocean/Lake Records
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keyword: earth science > paleoclimate > paleolimnology
keyword: earth science > paleoclimate > paleolimnology
keyword: earth science > paleoclimate > paleolimnology
keyword: earth science > paleoclimate > paleolimnology
keyword: earth science > paleoclimate > paleolimnology
keyword: earth science > paleoclimate > paleolimnology
keyword: earth science > paleoclimate > paleolimnology
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keyword: earth science > paleoclimate > paleolimnology
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keyword: earth science > paleoclimate > paleolimnology > population abundance
keyword: earth science > paleoclimate > paleolimnology > geochemistry
keyword: earth science > paleoclimate > paleolimnology > oxygen isotopes
keyword: earth science > paleoclimate > paleolimnology > lake level
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keyword: What: identified ostracod; Material: sediment
keyword: What: sample identification; Material: null
keyword: What: identified ostracod; Material: sediment
keyword: What: delta 13C; Material: ostracod
keyword: What: delta 18O; Material: ostracod
keyword: What: strontium/calcium; Material: ostracod
keyword: What: identified ostracod; Material: sediment
keyword: What: organic matter; Material: sediment
keyword: What: calcium carbonate; Material: sediment
keyword: What: depth; Material: null
keyword: What: magnesium/calcium; Material: ostracod
keyword: What: mineral matter; Material: sediment
keyword: What: identified ostracod; Material: sediment
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keyword: Continent > North America > United States Of America > Minnesota > Elk Lake > LATITUDE 45.86694 > LONGITUDE -95.80361
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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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otherConstraints: Cite as: Smith, A.J.; Donovan, J.J.; Ito, E.; Engstrom, D.R. (2000-01-01): NOAA/WDS Paleoclimatology - Elk Lake, Minnesota 12,000 Year Ostracod Abundance and Geochemical Data. [indicate subset used]. NOAA National Centers for Environmental Information. https://doi.org/10.25921/ecrb-ev92. 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: Ground-water processes controlling a prairie lake's response to middle Holocene drought
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date: 1997
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individualName: A.J. Smith, J.J. Donovan, E. Ito, and D.R. Engstrom
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organisationName: Geology
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description: A.J. Smith, J.J. Donovan, E. Ito, and D.R. Engstrom, 1997: Ground-water processes controlling a prairie lake's response to middle Holocene drought. Geology, 25, 391-394, 10.1130/0091-7613(1997)025<0391:GWPCAP>2.3.CO;2
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description: Date Range: cal yr BP to cal yr BP;
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beginPosition: 1950
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supplementalInformation: STUDY NOTES: Elk Lake ostracod abundance and geochemical data for mid-Holocene groundwater modeling and drought reconstruction. ABSTRACT SUPPLIED BY ORIGINATOR: Lake response to climate forcing is commonly regarded as being controlled by within-lake processes. We present a case from the northern Great Plains in which Holocene drought response recorded in lake sediments was determined by changes in chemical characteristics of source ground water. Middle Holocene ostracode assemblages were dominated by halophylic Limnocythere staplini, indicating increased lake-water salinity, yet the oxygen isotope values in this period decreased by 2‰ to 3‰, contrary to expectations of evaporative dominance. We infer from these proxy records and ground-water flow-model results that the paleoclimatic record in the lake was mediated by changes in ground-water catchment area and by reduction in evapotranspiration accompanying desiccation of peripheral lake basins.
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