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  <Entry_ID>noaa-lake-26690</Entry_ID>
  <Entry_Title>Waccamaw/Savannah River Wetlands Late Holocene Multiproxy Sediment Data</Entry_Title>
  <Data_Set_Citation>
    <Dataset_Creator>Jones, M.C.; Bernhardt, C.E.; Krauss, K.W.; Noe, G.B.</Dataset_Creator>
    <Dataset_Title>Waccamaw/Savannah River Wetlands Late Holocene Multiproxy Sediment Data</Dataset_Title>
    <Dataset_Release_Date>2019-05-01</Dataset_Release_Date>
    <Dataset_Publisher>NCDC-Paleoclimatology</Dataset_Publisher>
    <Data_Presentation_Form>ONLINE Files</Data_Presentation_Form>
    <Dataset_DOI>Pending</Dataset_DOI>
    <Online_Resource>https://www.ncdc.noaa.gov/paleo/study/26690</Online_Resource>
  </Data_Set_Citation>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>M.C.</First_Name>
    <Last_Name>Jones</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>C.E.</First_Name>
    <Last_Name>Bernhardt</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>K.W.</First_Name>
    <Last_Name>Krauss</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>G.B.</First_Name>
    <Last_Name>Noe</Last_Name>
  </Personnel>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleolimnology</Term>
    <Variable_Level_1>population abundance</Variable_Level_1>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleolimnology</Term>
    <Variable_Level_1>physical properties</Variable_Level_1>
  </Parameters>
  <ISO_Topic_Category>geoscientificInformation</ISO_Topic_Category>
  <Paleo_Temporal_Coverage>
    <Paleo_Start_Date>5820 cal yr BP</Paleo_Start_Date>
    <Paleo_Stop_Date>-61 cal yr BP</Paleo_Stop_Date>
  </Paleo_Temporal_Coverage>
  <Data_Set_Progress>Complete</Data_Set_Progress>
  <Spatial_Coverage>
    <Southernmost_Latitude>32.17</Southernmost_Latitude>
    <Northernmost_Latitude>33.55564</Northernmost_Latitude>
    <Westernmost_Longitude>-81.155</Westernmost_Longitude>
    <Easternmost_Longitude>-79.08943</Easternmost_Longitude>
  </Spatial_Coverage>
  <Location>
    <Location_Category>Continent</Location_Category>
    <Location_Type>North America</Location_Type>
    <Location_Subregion1>United States Of America</Location_Subregion1>
    <Location_Subregion2>Georgia</Location_Subregion2>
    <Detailed_Location>Savannah12-12-9-3&gt;LATITUDE 32.24&gt;LONGITUDE -81.15</Detailed_Location>
  </Location>
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    <Location_Type>North America</Location_Type>
    <Location_Subregion1>United States Of America</Location_Subregion1>
    <Location_Subregion2>South Carolina</Location_Subregion2>
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    <Location_Category>Continent</Location_Category>
    <Location_Type>North America</Location_Type>
    <Location_Subregion1>United States Of America</Location_Subregion1>
    <Location_Subregion2>South Carolina</Location_Subregion2>
    <Detailed_Location>Waccamaw11-11-2-3&gt;LATITUDE 33.34001&gt;LONGITUDE -79.34166</Detailed_Location>
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    <Location_Type>North America</Location_Type>
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    <Location_Subregion2>South Carolina</Location_Subregion2>
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    <Location_Subregion2>South Carolina</Location_Subregion2>
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  <Location>
    <Location_Category>Continent</Location_Category>
    <Location_Type>North America</Location_Type>
    <Location_Subregion1>United States Of America</Location_Subregion1>
    <Location_Subregion2>Georgia</Location_Subregion2>
    <Detailed_Location>Savannah12-12-10-3&gt;LATITUDE 32.17&gt;LONGITUDE -81.14</Detailed_Location>
  </Location>
  <Access_Constraints>None</Access_Constraints>
  <Use_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.</Use_Constraints>
  <Data_Set_Language>English</Data_Set_Language>
  <Data_Center>
    <Data_Center_Name>
      <Short_Name>DOC/NOAA/NESDIS/NCEI</Short_Name>
      <Long_Name>National Centers for Environmental Information, NESDIS, NOAA, U.S. Department of Commerce </Long_Name>
    </Data_Center_Name>
    <Data_Center_URL>https://www.ncdc.noaa.gov/data-access/paleoclimatology-data</Data_Center_URL>
    <Personnel>
      <Role>DATA Center Contact</Role>
      <First_Name>Bruce</First_Name>
      <Last_Name>Bauer</Last_Name>
      <Email>bruce.a.bauer@noaa.gov</Email>
      <Email>paleo@noaa.gov</Email>
      <Phone>303-497-6280</Phone>
      <Fax>303-497-6513</Fax>
      <Contact_Address>
        <Address>325 Broadway, E/NE31</Address>
        <City>Boulder</City>
        <Province_or_State>CO</Province_or_State>
        <Postal_Code>80305-3328</Postal_Code>
        <Country>USA</Country>
      </Contact_Address>
    </Personnel>
  </Data_Center>
  <Distribution>
    <Distribution_Media>online</Distribution_Media>
    <Distribution_Format>ASCII</Distribution_Format>
  </Distribution>
  <Reference>
    <Author>Miriam C. Jones, Christopher E. Bernhardt, Ken W. Krauss, Gregory B. Noe</Author>
    <Publication_Date>2017</Publication_Date>
    <Title>The Impact of Late Holocene Land Use Change, Climate Variability, and Sea Level Rise on Carbon Storage in Tidal Freshwater Wetlands on the Southeastern United States Coastal Plain</Title>
    <Series>Journal of Geophysical Research: Biogeosciences</Series>
    <Volume>122</Volume>
    <Issue>12</Issue>
    <Pages>3126-3141</Pages>
    <DOI>10.1002/2017JG004015</DOI>
    <Online_Resource>https://agupubs.onlinelibrary.wiley.com/doi/full/10.1002/2017JG004015</Online_Resource>
  </Reference>
  <Summary>
    <Abstract>This study examines Holocene impacts of changes in climate, land use, and sea level rise (SLR) on sediment accretion, carbon accumulation rates (CAR), and vegetation along a transect of tidal freshwater forested wetlands (TFFW) to oligohaline marsh along the Waccamaw River, South Carolina (four sites) and along the Savannah River, Georgia (four sites). We use pollen, plant macrofossils, accretion, and CAR from cores, spanning the last 1,500-6,000 years to test the hypothesis that TFFW have remained stable throughout the late Holocene and that marshes transitioned from TFFW during elevated SLR during the Medieval Climate Anomaly, with further transformation resulting from colonial land use change. Results show low and stable accretion and CAR through much of the Holocene, despite moderate changes associated with Holocene paleoclimate. In all records, the largest observed change occurred within the last ~400 years, driven by colonial land clearance, shifting terrigenous sediment into riparian wetlands, resulting in order-of-magnitude increases in accretion and C accumulation. The oligohaline marshes transitioned from TFFW ~300-500 years ago, coincident with colonial land clearance. Postcolonial decreases in CAR and accretion occur because of watershed reforestation over the last century. All sites show evidence of recent (decades to century) swamp forest decline due to increasing salinity and tidal inundation from SLR. This study suggests that allochthonous sediment input during colonialization helped maintain TFFW but that current SLR rates are too high for TFFW to persist, although higher accretion rates in oligohaline marshes increase the resilience of tidal wetlands as they transition from TFFW to marsh. 
          STUDY NOTES: Multiproxy (pollen, plant macrofossils, sediment accretion, and carbon accumulation) data from river wetlands sediment cores. Cores are from 2 transects ranging from tidal freshwater forested wetlands (TFFW) to oligohaline marsh, along the Waccamaw and Savannah  Rivers (South Carolina and Georgia, USA) for the late Holocene (~6,000 - 1,500 years BP).</Abstract>
  </Summary>
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    <Description>NOAA Template File; Waccamaw River Core 11-11-2-3 Macrofossil Percentage Data</Description>
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