noaa-recon-9718 eng; USA utf8 dataset Bauer, Bruce DOC/NOAA/NESDIS/NCEI > National Centers for Environmental Information, NESDIS, NOAA, U.S. Department of Commerce +1 303-497-6280 +1 303-497-6513 325 Broadway, E/CC23 Boulder CO 80305-3328 USA paleo@noaa.gov pointOfContact 2018-12-11 ISO 19115-2 Geographic Information - Metadata - Part 2: Extensions for Imagery and Gridded Data ISO 19115-2:2009(E) NOAA/WDS Paleoclimatology - Stazki Bog, Poland 1000 Year Testate Amoeba DWT Reconstruction 2010-10-20 publication noaa-recon-9718 NCEI DSI 1200_01 Lamentowicz, M. originator Lamentowicz, M. author Cedro, A. originator Cedro, A. author Galka, M. originator Galka, M. author Goslar, T. originator Goslar, T. author Miotk-Szpiganowicz, G. originator Miotk-Szpiganowicz, G. author Mitchell, E.A.D. originator Mitchell, E.A.D. author Pawlyta, J. originator Pawlyta, J. author NOAA National Centers for Environmental Information publisher tableDigital 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 Climate Reconstruction. The data include parameters of climate reconstructions|paleolimnology with a geographic location of Poland, Eastern Europe. The time period coverage is from 950 to -52 in calendar years before present (BP). See metadata information for parameter and study location details. Please cite this study when using the data. Records of past temperature, precipitation, and other climate variables derived from paleoclimate proxies. Parameter keywords describe what was measured in this data set. Additional summary information can be found in the abstracts of papers listed in the data set citations. completed Bauer, Bruce DOC/NOAA/NESDIS/NCEI > National Centers for Environmental Information, NESDIS, NOAA, U.S. Department of Commerce +1 303-497-6280 +1 303-497-6513 325 Broadway, E/CC23 Boulder CO 80305-3328 USA paleo@noaa.gov pointOfContact https://www.ncdc.noaa.gov/c/images/pc-default-recon.png Paleoclimatology - Climate Reconstruction PNG Earth Science > Climate Indicators > Paleoclimate Indicators > Paleoclimate Reconstructions theme Global Change Master Directory (GCMD) Science Keywords 2018 revision Version 8.6 Global Change Data Center, Science and Exploration Directorate, Goddard Space Flight Center (GSFC) National Aeronautics and Space Administration (NASA) https://earthdata.nasa.gov/about/gcmd/global-change-master-directory-gcmd-keywords HTTPS Web Browser Global Change Master Directory (GCMD) Keywords 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. information publisher earth science > paleoclimate > climate reconstructions|paleolimnology earth science > paleoclimate > climate reconstructions|paleolimnology earth science > paleoclimate > climate reconstructions|paleolimnology earth science > paleoclimate > reconstructions > ground water theme Global Change Master Directory (GCMD) Science Keywords 2018 revision Version 8.6 Global Change Data Center, Science and Exploration Directorate, Goddard Space Flight Center (GSFC) National Aeronautics and Space Administration (NASA) https://earthdata.nasa.gov/about/gcmd/global-change-master-directory-gcmd-keywords HTTPS Web Browser Global Change Master Directory (GCMD) Keywords 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. information publisher Other Hydroclimate Reconstruction hydrology theme Continent > Europe > Eastern Europe > Poland> Stazki Bog > LATITUDE 54.4243 > LONGITUDE 18.083 place otherRestrictions Cite as: Lamentowicz, M.; Cedro, A.; Galka, M.; Goslar, T.; Miotk-Szpiganowicz, G.; Mitchell, E.A.D.; Pawlyta, J. (2010-10-20): NOAA/WDS Paleoclimatology - Stazki Bog, Poland 1000 Year Testate Amoeba DWT Reconstruction . [indicate subset used]. NOAA National Centers for Environmental Information. https://www.ncdc.noaa.gov/paleo/study/9718. Accessed [date]. otherRestrictions 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. otherRestrictions 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. otherRestrictions None otherRestrictions 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. eng; USA geoscientificInformation Date Range: 1000 AD to 2002 AD; Date Range: 950 cal yr BP to -52 cal yr BP; 18.083 18.083 54.4243 54.4243 Study Coordinates 54.4243 18.083 1000 2002 STUDY NOTES: Depth to Water Table (DWT) reconstruction for Stazki Bog, Poland based on Testate Amoeba. Two time series are included. SL1 is the published data (Lamentowicz et al., 2008a). This peat core has a 400 years hiatus. Also provided is data from peat core SL2, which is continuous and not disturbed, but unpublished. It was analysed with the same methods as peat core SL1. The study site is a Baltic bog located in northern Poland, ca 35 km from the Baltic sea coast, in the Kaszuby Lakeland, near the highest point (214.6 m a.s.l.) of a moraine plateau. All calculations are based on percentage of each species of Testate Amoeba in a sample (See Booth et al., 2010). Age model is from (Lamentowicz et al., 2008a). Depth to Water Table (DWT) is dependent on vegetation season temperature and summer water deficit, providing a mixed temperature and precipitation signal. Water table reconstruction based on the transfer function of Lamentowicz et al., 2008b. ABSTRACT SUPPLIED BY ORIGINATOR: The Baltic coast of Northern Poland is an interesting region for palaeoclimatic studies because of the mixed oceanic and continental climatic influences and the fact that the dominance of one or the other of these two influences might have changed over time. Also, unlike many more intensively studied regions of Europe, human impact in the region was rather limited until the 19th century. We present a 1200-year high-resolution record from Stazki mire, an ombrotrophic bog located 35 km from the Baltic Sea coast. Using testate amoebae, stable isotopes (d13C) of Sphagnum stems, pollen, plant macrofossils and dendroecological analyses, our aims were to: 1) reconstruct the last millennium palaeoenvironment in the study site and its surroundings, 2) identify the major wet-dry shifts, 3) determine if those events correlate with climate change and human impact, 4) assess the resilience of the Baltic bog ecosystem following human impact, and 5) compare the palaeo-moisture signal from the Baltic coast with records from more oceanic regions. Two dry periods are inferred at AD 1100-1500 and 1650-1900 (-2005). The first dry shift is probably climate-driven as pollen record shows little evidence of human indicators. The second dry shift can be related to local peat exploitation of the mire. In the 20th century additional limited drainage took place and since ca. AD 1950 the mire has been recovering. From 1500 AD onwards all proxies indicate wetter condition. The beginning of this wet shift occurred during the Little Ice Age and may therefore be a climatic signal. The macrofossil data show that Sphagnum fuscum dominated the pristine mire vegetation but then declined and finally disappeared at ca. AD 1900. This pattern is comparable with the timing of extinction of Sphagnum austinii (= Sphagnum imbricatum) in the UK. This study illustrates the value of high-resolution multi-proxy studies of peat archives to assess the magnitude of anthropogenic land-use changes. This study presents the first direct comparison of testate amoebae and stable isotope data from the same core. The two proxies correlate significantly throughout the record and most strongly for the latter part of the record when most of the variability was recorded. 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Native Format(s) https://data.nodc.noaa.gov/cgi-bin/iso?id=noaa-recon-9718 HTTPS Landing Page NCEI landing page for this dataset Dataset landing page with general information and links to access the data. information https://www.ncdc.noaa.gov/paleo/study/9718 HTTPS Web Browser NCEI Study Page Study page with dataset access information. search https://www.ncdc.noaa.gov/data-access/paleoclimatology-data/datasets/climate-reconstruction HTTPS Information NCEI Climate Reconstruction Page General information for this data type. information https://www1.ncdc.noaa.gov/pub/data/paleo/paleolimnology/europe/poland/stazki2008dwt.xls HTTP Download NCEI Direct Download Direct download links for dataset files. download https://www1.ncdc.noaa.gov/pub/data/paleo/paleolimnology/europe/poland/stazki2008dwt.txt HTTP Download NCEI Direct Download Direct download links for dataset files. download asNeeded This metadata record was translated from DIF using dif-9x-to-iso-19115-2.xsl Version: 2018-10-25