NOAA/WDS Paleoclimatology - Arctic Holocene Proxy Climate Database
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dateStamp: 2024-04-18
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 - Arctic Holocene Proxy Climate Database
date: (CI_Date)
date: 2014-01-03
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Anchor: DOI doi:10.25921/pak9-az20
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code: noaa-lake-15444
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code: NCEI DSI 1200_02
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code: NCEI DSI 1200_01
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individualName: McKay, N.P.
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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 climate reconstructions|insect|paleolimnology with a geographic location of Arctic Ocean. The time period coverage is from 11000 to 0 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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fileName: https://www.ncei.noaa.gov/pub/data/paleo/webimages/pc-default-lake.png
fileDescription: Paleoclimatology - Lake
fileType: PNG
descriptiveKeywords: (MD_Keywords)
keyword: Earth Science > Climate Indicators > Paleoclimate Indicators > Ocean/Lake Records
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title: Global Change Master Directory (GCMD) Science Keywords
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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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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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keyword: earth science > paleoclimate > climate reconstructions|insect|paleolimnology
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keyword: earth science > paleoclimate > paleolimnology
keyword: earth science > paleoclimate > paleolimnology
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keyword: What: sea surface temperature; Material: null
keyword: What: sea surface temperature; Material: null
keyword: What: salinity; Material: sea surface
keyword: What: temperature; Material: null
keyword: What: sea ice cover; Material: null
keyword: What: temperature; Material: null
keyword: What: temperature; Material: null
keyword: What: salinity; Material: sea surface
keyword: What: sea ice cover; Material: null
keyword: What: sea ice cover; Material: null
keyword: What: salinity; Material: sea surface
keyword: What: salinity; Material: sea surface
keyword: What: temperature; Material: null
keyword: What: temperature; Material: null
keyword: What: surface downwelling shortwave radiation; Material: null
keyword: What: precipitation; Material: null
keyword: What: temperature; Material: null
keyword: What: equilibrium line altitude; Material: null
keyword: What: temperature; Material: null
keyword: What: temperature; Material: null
keyword: What: temperature; Material: null
keyword: What: temperature; Material: null
keyword: What: depth; Material: null
keyword: What: age; Material: null
keyword: What: biogenic silica; Material: sediment
keyword: What: accumulation rate; Material: sediment
keyword: What: volume magnetic susceptibility; Material: sediment
keyword: What: humification index; Material: peat
keyword: What: total diatoms; Material: null
keyword: What: temperature; Material: null
keyword: What: temperature; Material: null
keyword: What: temperature; Material: null
keyword: What: temperature; Material: null
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keyword: What: temperature; Material: null
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keyword: What: temperature; Material: null
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keyword: What: temperature; Material: null
keyword: What: temperature; Material: null
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keyword: What: temperature; Material: null
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keyword: What: temperature; Material: null
keyword: What: precipitation; Material: null
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keyword: What: temperature; Material: null
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keyword: What: temperature; Material: null
keyword: What: temperature; Material: null
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keyword: What: temperature; Material: null
keyword: What: temperature; Material: null
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keyword: What: temperature; Material: null
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keyword: What: temperature; Material: null
keyword: What: temperature; Material: null
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keyword: What: melt; Material: bulk ice
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keyword: What: delta 13C; Material: organic matter
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keyword: What: density; Material: dry sediment
keyword: What: organic matter; Material: sediment
keyword: What: delta 2H; Material: null
keyword: What: mineral matter; Material: sediment
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keyword: What: delta 18O; Material: null
keyword: What: temperature; Material: null
keyword: What: temperature; Material: null
keyword: What: temperature; Material: null
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keyword: What: temperature; Material: null
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keyword: What: temperature; Material: null
keyword: What: growing degree days; Material: null
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keyword: What: manganese/calcium; Material: ostracod
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keyword: What: humification index; Material: peat
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keyword: What: delta 18O; Material: cellulose
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keyword: What: ice proxy with 25 carbon atoms; Material: sediment
keyword: What: alkenone unsaturation index Uk37 prime; Material: null
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keyword: What: temperature; Material: null
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keyword: What: anhysteretic remanent magnetization/isothermal remanent magnetization; Material: sediment
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keyword: What: temperature; Material: null
keyword: What: precipitation; Material: null
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keyword: What: temperature; Material: null
keyword: What: temperature; Material: null
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keyword: What: sea ice cover; Material: null
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keyword: What: sea ice cover; Material: null
keyword: What: temperature; Material: null
keyword: What: temperature; Material: null
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keyword: What: temperature; Material: null
keyword: What: temperature; Material: null
keyword: What: temperature; Material: null
keyword: What: temperature; Material: null
keyword: What: temperature; Material: null
keyword: What: temperature; Material: null
keyword: What: temperature; Material: null
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keyword: What: canonical correspondence analysis axis; Material: null
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keyword: What: principal component; Material: null
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keyword: What: temperature; Material: null
keyword: What: temperature; Material: null
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keyword: What: temperature; Material: null
keyword: What: temperature; Material: null
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keyword: What: precipitation; Material: null
keyword: What: temperature; Material: null
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otherConstraints: Cite as: Sundqvist, H.; Kaufman, D.S.; McKay, N.P.; Balascio, N.L.; Briner, J.P.; Cwynar, L.C.; Sejrup, H.P.; Seppä, H.T.; Subetto, D.A.; Andrews, J.T.; Axford, Y.; Bakke, J.; Birks, H.J.B.; Brooks, S.J.; de Vernal, A.; Jennings, A.E.; Ljungqvist, F.C.; Rühland, K.M.; Saenger, C.P.; Smol, J.P.; Viau, A.E. (2014-01-03): NOAA/WDS Paleoclimatology - Arctic Holocene Proxy Climate Database. [indicate subset used]. NOAA National Centers for Environmental Information. https://doi.org/10.25921/pak9-az20. Accessed [date].
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title: Arctic Holocene proxy climate database - new approaches to assessing geochronological accuracy and encoding climate variables
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individualName: H.S. Sundqvist, D.S. Kaufman, N.P. McKay, N.L. Balascio, J.P. Briner, L.C. Cwynar, H.P. Sejrup, H. Seppä, D.A. Subetto, J.T. Andrews, Y. Axford, J. Bakke, H.J.B. Birks, S.J. Brooks, A. de Vernal, A.E. Jennings, F.C. Ljungqvist, K.M. Rühland, C. Saenger, J.P. Smol, and A.E. Viau
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description: H.S. Sundqvist, D.S. Kaufman, N.P. McKay, N.L. Balascio, J.P. Briner, L.C. Cwynar, H.P. Sejrup, H. Seppä, D.A. Subetto, J.T. Andrews, Y. Axford, J. Bakke, H.J.B. Birks, S.J. Brooks, A. de Vernal, A.E. Jennings, F.C. Ljungqvist, K.M. Rühland, C. Saenger, J.P. Smol, and A.E. Viau, 2014: Arctic Holocene proxy climate database - new approaches to assessing geochronological accuracy and encoding climate variables. Climate of the Past, 10, 1605-1631, 10.5194/cp-10-1605-2014
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supplementalInformation: STUDY NOTES: Holocene proxy climate records from the Arctic. Database consisting of 168 sites from north of 58°N, proxy data from lake sediments (60%), marine sediments (32%), glacier ice (5%), and other sources. Data are presented in 6 Excel files organized by region. Measured parameters include: alkenones, ARM/IRM, biogenic silica, bulk density, C & N, carbonate, chironomids, d13C.bulk_organics, d18O.calcite, d18O.cellulose, d18O.diatom, d18O.foram, d18O.ice, dD, diatoms, dinocysts, forams.pl, humification_index, ice_rafted_debris, ice.melt, IP25, magnetic_susceptibility, Mg/Ca.foram, MgCa.ostracodes, mineral.content, mineral.flux, OM.flux, pollen, sedimentation_rate, total_organic_carbon, varve.width. ABSTRACT SUPPLIED BY ORIGINATOR: We present a systematic compilation of previously published Holocene proxy climate records from the Arctic. We identified 170 sites from north of 58N latitude where proxy time series extend back at least to 6 cal ka (all ages in this article are in calendar years before present – BP), are resolved at submillennial scale (at least one value every 400 ± 200 years) and have age models constrained by at least one age every 3000 years. In addition to conventional metadata for each proxy record (location, proxy type, reference), we include two novel parameters that add functionality to the database. First, "climate interpretation" is a series of fields that logically describe the specific climate variable(s) represented by the proxy record. It encodes the proxy-climate relation reported by authors of the original studies into a structured format to facilitate comparison with climate model outputs. Second, "geochronology accuracy score" (chron score) is a numerical rating that reflects the overall accuracy of 14C-based age models from lake and marine sediments. Chron scores were calculated using the original author-reported 14C ages, which are included in this database. The database contains 320 records (some sites include multiple records) from six regions covering the circumpolar Arctic: Fennoscandia is the most densely sampled region (31% of the records), whereas only five records from the Russian Arctic met the criteria for inclusion. The database contains proxy records from lake sediment (60%), marine sediment (32%), glacier ice (5%), and other sources. Most (61%) reflect temperature (mainly summer warmth) and are primarily based on pollen, chironomid, or diatom assemblages. Many (15%) reflect some aspect of hydroclimate as inferred from changes in stable isotopes, pollen and diatom assemblages, humification index in peat, and changes in equilibrium-line altitude of glaciers. This comprehensive database can be used in future studies to investigate the spatio-temporal pattern of Arctic Holocene climate changes and their causes. The Arctic Holocene data set is available from NOAA Paleoclimatology.
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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
