{"NOAAStudyId":"9704","contactInfo":{"address":"325 Broadway, E/NE31","city":"Boulder","constraints":"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.","country":"USA","dataCenterUrl":"https://www.ncdc.noaa.gov/data-access/paleoclimatology-data","email":"paleo@noaa.gov","fax":"303-497-6513","longName":"National Centers for Environmental Information, NESDIS, NOAA, U.S. Department of Commerce ","phone":"303-497-6280","postalCode":"80305-3328","shortName":"DOC/NOAA/NESDIS/NCEI","state":"CO","type":"CONTACT INFORMATION"},"contributionDate":"2010-10-20","dataPublisher":"NOAA","dataType":"CLIMATE RECONSTRUCTIONS","dataTypeInformation":"https://www.ncdc.noaa.gov/data-access/paleoclimatology-data/datasets/climate-reconstruction","difMetadataLink":"http://www1.ncdc.noaa.gov/pub/data/metadata/published/paleo/dif/xml/noaa-recon-9704.xml","doi":null,"earliestYearBP":950,"earliestYearCE":1000,"entryId":"noaa-recon-9704","funding":[{"fundingAgency":"Polish Ministry of Scientific Research and Information Technology","fundingGrant":"2P04G03228"},{"fundingAgency":"Project Millennium ","fundingGrant":"017008-GOCE"}],"investigators":"Lamentowicz, M.; Milecka, K.; Gazka, M.; Cedro, A.; Pawlyta, J.; Piotrowska, N.; Lamentowicz, L.","mostRecentYearBP":-52,"mostRecentYearCE":2002,"onlineResourceLink":"https://www.ncdc.noaa.gov/paleo/study/9704","originalSource":null,"publication":[{"abstract":"This high-resolution, multiproxy, palaeoenvironmental study of \nthe Slowinskie Blota raised bog in N Poland, 10km from the Baltic Sea, \ncovering the last 1200 years reveals different aspects of environmental \nchange in a range of spatial scales from local to regional. Testate \namoebae allowed quantitative reconstruction of the local water table \nusing a transfer function based on a training set from N and W Poland. \nSpecial attention is paid to the testate amoeba Arcella discoides, \nwhich responds to rapid water-table fluctuations more than to average \nsurface wetness. Macrofossils supported by local pollen tracked the \nlocal vegetation dynamics caused by local human impact and disturbance, \nincluding nutrients. Regional pollen showed human-induced landscape \nchange outside the bog. Tree rings of Pinus sylvestris reflected the \nhistory of tree establishment and desiccation of the bog. Strong \ncorrelations between DCA axes 1 of regional pollen, of macrofossils \nand of testate amoebae, and a testate-amoebae-based water-table \nreconstruction that excludes A. discoides, indicate that changes \non all spatial scales are linked, which is explained by a strong \nhydrologic connection between bog and surroundings. The combination \nof proxies shows that groundwater levels were modified by both human \nimpact and climate change.\n","author":null,"citation":"Lamentowicz, M., K. Milecka, M. Gazka, A. Cedro, J. Pawlyta, \nN. Piotrowska, L. Lamentowicz, and W.O. van der Knaap. 2008. \nClimate and human induced hydrological change since AD 800 \nin an ombrotrophic mire in Pomerania (N Poland) tracked by \ntestate amoebae, macro-fossils, pollen and tree rings of pine. \nBoreas, Vol. 38, pp. 214-229. \nDOI: 10.1111/j.1502-3885.2007.00004.x. \nISSN 0300-9843.\n","edition":null,"identifier":{"id":"10.1111/j.1502-3885.2007.00004.x. ","type":"doi","url":"http://dx.doi.org/10.1111/j.1502-3885.2007.00004.x. "},"issue":null,"journal":"Boreas","pages":null,"pubRank":"1","pubYear":2008,"reportNumber":null,"title":"Climate and human induced hydrological change since AD 800  in an ombrotrophic mire in Pomerania (N Poland) tracked by  testate amoebae, macro-fossils, pollen and tree rings of pine","type":"publication","volume":null}],"reconstruction":"Y","scienceKeywords":["hydrology","Other Hydroclimate Reconstruction"],"site":[{"NOAASiteId":"31428","geo":{"geoType":"Feature","geometry":{"coordinates":["54.3645","16.4902"],"type":"POINT"},"properties":{"easternmostLongitude":"16.4902","maxElevationMeters":"30","minElevationMeters":"30","northernmostLatitude":"54.3645","southernmostLatitude":"54.3645","westernmostLongitude":"16.4902"}},"locationName":"Continent>Europe>Eastern Europe>Poland","mappable":"Y","paleoData":[{"NOAADataTableId":"18628","coreLengthMeters":null,"dataFile":[{"NOAAKeywords":["earth science>paleoclimate>reconstructions>ground water"],"fileUrl":"https://www1.ncdc.noaa.gov/pub/data/paleo/paleolimnology/europe/poland/slowinskie2009dwt.txt","linkText":"slowinskie2009dwt.txt","urlDescription":"Data","variables":[{"cvAdditionalInfo":null,"cvDataType":"CLIMATE RECONSTRUCTIONS|PALEOLIMNOLOGY","cvDetail":null,"cvError":null,"cvFormat":"Numeric","cvMaterial":null,"cvMethod":null,"cvSeasonality":null,"cvShortName":null,"cvUnit":"year Common Era","cvWhat":"age variable>age"},{"cvAdditionalInfo":null,"cvDataType":"CLIMATE RECONSTRUCTIONS|PALEOLIMNOLOGY","cvDetail":null,"cvError":null,"cvFormat":"Numeric","cvMaterial":"reconstruction material>biological assemblage>testate amoebae assemblage","cvMethod":null,"cvSeasonality":null,"cvShortName":null,"cvUnit":"centimeter","cvWhat":"earth system variable>hydrographic variable>water table depth"},{"cvAdditionalInfo":"bootstrapped error","cvDataType":"CLIMATE RECONSTRUCTIONS|PALEOLIMNOLOGY","cvDetail":null,"cvError":"unspecified margin of error","cvFormat":"Numeric","cvMaterial":"reconstruction material>biological assemblage>testate amoebae assemblage","cvMethod":null,"cvSeasonality":null,"cvShortName":null,"cvUnit":"centimeter","cvWhat":"earth system variable>hydrographic variable>water table depth"}]},{"NOAAKeywords":["earth science>paleoclimate>reconstructions>ground water"],"fileUrl":"https://www1.ncdc.noaa.gov/pub/data/paleo/paleolimnology/europe/poland/slowinskie2009dwt.xls","linkText":"slowinskie2009dwt.xls","urlDescription":"Data","variables":[]}],"dataTableName":"SL001","dataTableNotes":null,"earliestYear":1000,"earliestYearBP":950,"earliestYearCE":1000,"mostRecentYear":2002,"mostRecentYearBP":-52,"mostRecentYearCE":2002,"species":[],"timeUnit":"AD"}],"siteName":"Slowinskie Bog"}],"studyCode":null,"studyName":"Slowinskie Bog, Poland 1000 Year Testate Amoeba DWT Reconstruction ","studyNotes":"Depth to Water Table (DWT) reconstruction for Slowinskie Bog, \nPoland, based on Testate Amoeba. Slowinskie Bog is located \nin northern Poland, ~10km from the Baltic shoreline. \n\nAll calculations are based on percentage of each species \nof Testate Amoeba in a sample (See Booth et al., 2010). \nAge model is from (Lamentowicz et al., 2009). \n\nDepth to Water Table (DWT) is dependent on vegetation season \ntemperature and summer water deficit, providing a mixed \ntemperature and precipitation signal. \n\nWater table reconstruction based on the transfer function \nof Lamentowicz et al., 2008. \n\n","version":"1.0","xmlId":"8663"}