<DIF xmlns="http://gcmd.gsfc.nasa.gov/Aboutus/xml/dif/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://gcmd.gsfc.nasa.gov/Aboutus/xml/dif/ http://gcmd.gsfc.nasa.gov/Aboutus/xml/dif/dif_v9.8.4.xsd">
  <Entry_ID>noaa-tree-9910</Entry_ID>
  <Entry_Title>South America 180 Year Tree Ring Stable Isotope Data</Entry_Title>
  <Data_Set_Citation>
    <Dataset_Creator>Ballantyne, A.; Baker, P.A.; Chambers, J.Q.; Villalba, R.; Argollo, J.</Dataset_Creator>
    <Dataset_Title>South America 180 Year Tree Ring Stable Isotope Data</Dataset_Title>
    <Dataset_Release_Date>2010-12-16</Dataset_Release_Date>
    <Dataset_Publisher>NCDC-Paleoclimatology</Dataset_Publisher>
    <Data_Presentation_Form>ONLINE Files</Data_Presentation_Form>
    <Dataset_DOI>10.25921/p9f9-ck54</Dataset_DOI>
    <Online_Resource>https://www.ncdc.noaa.gov/paleo/study/9910</Online_Resource>
  </Data_Set_Citation>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>A.</First_Name>
    <Last_Name>Ballantyne</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>P.A.</First_Name>
    <Last_Name>Baker</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>J.Q.</First_Name>
    <Last_Name>Chambers</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>R.</First_Name>
    <Last_Name>Villalba</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>J.</First_Name>
    <Last_Name>Argollo</Last_Name>
  </Personnel>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>tree ring</Term>
    <Detailed_Variable>delta 18O,alpha cellulose,null,per mil SMOW,null,tree ring,null,isotope ratio mass spectrometry,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>tree ring</Term>
    <Detailed_Variable>delta 13C,alpha cellulose,null,per mil PDB,null,tree ring,null,isotope ratio mass spectrometry,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>tree ring</Term>
    <Detailed_Variable>age,null,null,year Common Era,null,tree ring,null,null,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>tree-ring</Term>
    <Variable_Level_1>carbon isotopes</Variable_Level_1>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>tree-ring</Term>
    <Variable_Level_1>oxygen isotopes</Variable_Level_1>
  </Parameters>
  <ISO_Topic_Category>geoscientificInformation</ISO_Topic_Category>
  <Keyword>Monsoon</Keyword>
  <Keyword>PAGES 2k Network</Keyword>
  <Keyword>PAGES LOTRED SA2k</Keyword>
  <Keyword>Tropics</Keyword>
  <Keyword>drought</Keyword>
  <Keyword>CEOD</Keyword>
  <Keyword>Cedrela odorata L.</Keyword>
  <Paleo_Temporal_Coverage>
    <Paleo_Start_Date>1820 AD</Paleo_Start_Date>
    <Paleo_Stop_Date>2004 AD</Paleo_Stop_Date>
  </Paleo_Temporal_Coverage>
  <Paleo_Temporal_Coverage>
    <Paleo_Start_Date>130 cal yr BP</Paleo_Start_Date>
    <Paleo_Stop_Date>-54 cal yr BP</Paleo_Stop_Date>
  </Paleo_Temporal_Coverage>
  <Data_Set_Progress>Complete</Data_Set_Progress>
  <Spatial_Coverage>
    <Southernmost_Latitude>-22</Southernmost_Latitude>
    <Northernmost_Latitude>-12.6</Northernmost_Latitude>
    <Westernmost_Longitude>-69.2</Westernmost_Longitude>
    <Easternmost_Longitude>-66</Easternmost_Longitude>
    <Minimum_Altitude>265</Minimum_Altitude>
    <Maximum_Altitude>3500</Maximum_Altitude>
  </Spatial_Coverage>
  <Location>
    <Location_Category>Continent</Location_Category>
    <Location_Type>South America</Location_Type>
    <Location_Subregion1>Peru</Location_Subregion1>
    <Detailed_Location>Puerto Maldonado&gt;LATITUDE -12.6&gt;LONGITUDE -69.2</Detailed_Location>
  </Location>
  <Location>
    <Location_Category>Continent</Location_Category>
    <Location_Type>South America</Location_Type>
    <Location_Subregion1>Argentina</Location_Subregion1>
    <Detailed_Location>Volcan Granada&gt;LATITUDE -22&gt;LONGITUDE -66</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>Ballantyne, A.P., P.A. Baker, J.Q. Chambers, R. Villalba, 
and J. Argollo. 2011. 
Regional differences in South American monsoon precipitation 
inferred from the growth and isotopic composition of tropical trees. 
Earth Interactions.  doi: 10.1175/2010EI277.1 
</Reference>
  <Summary>
    <Abstract>We present results on the relationship between tree ring proxies 
and regional precipitation for several sites in tropical South 
America. The responsiveness of oxygen isotopes (d18O) and seasonal 
growth as precipitation proxies was first validated by high- 
resolution sampling of a Tachigali myrmecophila from Manaus, 
Brazil (3.1ºS, 60.0ºW).  Monthly growth of Tachigali spp. was 
significantly correlated with monthly precipitation. Intra-annual 
measurements of cellulose d18O in Tachigali spp. were also 
significantly correlated with monthly precipitation at a lag of 
approximately one month. The annual ring-widths of two tropical 
tree taxa, Cedrela odorata growing in the Amazon (12.6ºS, 69.2ºW) 
and Polylepis tarapacana growing in the Altiplano (22.0ºS, 66.0ºW), 
were validated using bomb-derived radiocarbon 14C. Estimated dates 
were within two to three years of bomb inferred 14C dates, 
indicating that these species exhibit annual rings but uncertainties 
in our chronologies remain. A multi-proxy record spanning 180 years 
from Cedrela spp. showed a significant negative relationship between 
cellulose d18O and January precipitation. A 150-year record obtained 
from Polylepis spp. also showed a significant negative relationship 
between d18O and March precipitation, whereas annual ring width 
showed a significant positive correlation with December precipitation. 
These proxies were combined in a multivariate framework to reconstruct 
past precipitation, revealing a significant increase in monsoon 
precipitation at the Amazon site since 1890 and a significant decrease 
in monsoon precipitation at the Altiplano since 1880.  Proxy time 
series also showed spatial and temporal coherence with precipitation 
variability due to El Niño forcing, suggesting that oxygen isotopes 
and ring widths in tropical trees may be important diagnostics for 
identifying regional differences in the response of the tropical 
hydrologic cycle to anthropogenic warming. 
 
          STUDY NOTES: Tree ring isotope data from two South American locations and species, 
Cedrela odorata from the upper Amazon Basin and Polylepis tarapacana 
from the Altiplano.  The isotope data correlate with seasonal 
precipitation and provide a monsoon strength signal for the Amazon 
and Altiplano for the past 180 years. 
IITRDB006</Abstract>
  </Summary>
  <Related_URL>
    <URL_Content_Type>
      <Type>GET DATA</Type>
    </URL_Content_Type>
    <URL>https://www1.ncdc.noaa.gov/pub/data/paleo/treering/isotope/southamerica/ballantyne2011tr-iso.xls</URL>
  </Related_URL>
  <Related_URL>
    <URL_Content_Type>
      <Type>GET DATA</Type>
    </URL_Content_Type>
    <URL>https://www1.ncdc.noaa.gov/pub/data/paleo/treering/isotope/southamerica/ballantyne2011tr-iso.txt</URL>
  </Related_URL>
  <IDN_Node>
    <Short_Name>USA/NOAA</Short_Name>
  </IDN_Node>
  <Metadata_Name>DIF</Metadata_Name>
  <Metadata_Version>Version 9.8.4</Metadata_Version>
  <DIF_Creation_Date>2019-03-01</DIF_Creation_Date>
  <Last_DIF_Revision_Date>2019-03-01</Last_DIF_Revision_Date>
</DIF>
