<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-ocean-12504</Entry_ID>
  <Entry_Title>Gulf of Lions 7000 Year Mediterranean Paleostorm Data </Entry_Title>
  <Data_Set_Citation>
    <Dataset_Creator>Sabatier, P.; Dezileau, L.; Colin, C.; Briqueu, L.; Bouchette, F.; Martinez, P.; Siani, G.; Raynal, O.; von Grafenstein, U.</Dataset_Creator>
    <Dataset_Title>Gulf of Lions 7000 Year Mediterranean Paleostorm Data </Dataset_Title>
    <Dataset_Release_Date>2012-02-13</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/12504</Online_Resource>
  </Data_Set_Citation>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>P.</First_Name>
    <Last_Name>Sabatier</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>L.</First_Name>
    <Last_Name>Dezileau</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>C.</First_Name>
    <Last_Name>Colin</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>L.</First_Name>
    <Last_Name>Briqueu</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>F.</First_Name>
    <Last_Name>Bouchette</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>P.</First_Name>
    <Last_Name>Martinez</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>G.</First_Name>
    <Last_Name>Siani</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>O.</First_Name>
    <Last_Name>Raynal</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>U.</First_Name>
    <Last_Name>von Grafenstein</Last_Name>
  </Personnel>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleoceanography</Term>
    <Detailed_Variable>age,null,null,calendar year before present,null,paleoceanography,null,null,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleoceanography</Term>
    <Detailed_Variable>mineral index,sediment,null,dimensionless,null,paleoceanography,null,null,N,smectite/(illite plus chlorite)</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleoceanography</Term>
    <Detailed_Variable>depth,null,null,centimeter,null,paleoceanography,null,null,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleocean</Term>
    <Variable_Level_1>geochemistry</Variable_Level_1>
  </Parameters>
  <ISO_Topic_Category>geoscientificInformation</ISO_Topic_Category>
  <Keyword>PAGES 2k Network</Keyword>
  <Keyword>PAGES Euro-Med 2k</Keyword>
  <Paleo_Temporal_Coverage>
    <Paleo_Start_Date>7845 cal yr BP</Paleo_Start_Date>
    <Paleo_Stop_Date>-57 cal yr BP</Paleo_Stop_Date>
  </Paleo_Temporal_Coverage>
  <Data_Set_Progress>Complete</Data_Set_Progress>
  <Spatial_Coverage>
    <Southernmost_Latitude>43.5078</Southernmost_Latitude>
    <Northernmost_Latitude>43.5078</Northernmost_Latitude>
    <Westernmost_Longitude>3.8708</Westernmost_Longitude>
    <Easternmost_Longitude>3.8708</Easternmost_Longitude>
    <Minimum_Altitude>-1</Minimum_Altitude>
    <Maximum_Altitude>-1</Maximum_Altitude>
  </Spatial_Coverage>
  <Location>
    <Location_Category>Ocean</Location_Category>
    <Location_Type>Atlantic Ocean</Location_Type>
    <Location_Subregion1>North Atlantic Ocean</Location_Subregion1>
    <Location_Subregion2>Mediterranean Sea</Location_Subregion2>
    <Detailed_Location>PB06&gt;LATITUDE 43.5078&gt;LONGITUDE 3.8708</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>Sabatier, P., L. Dezileau, C. Colin, L. Briqueu, F. Bouchette, 
P. Martinez, G. Siani, O. Raynal, and U. Von Grafenstein. 2012. 
7000 years of paleostorm activity in the NW Mediterranean Sea 
in response to Holocene climate events. 
Quaternary Research, Vol. 77, Issue 1, January 2012, pp. 1-11. 
doi: 10.1016/j.yqres.2011.09.002</Reference>
  <Summary>
    <Abstract>A high-resolution record of paleostorm events along the French 
Mediterranean coast over the past 7000 years was established 
from a lagoonal sediment core in the Gulf of Lions. 
Integrating grain size, faunal analysis, clay mineralogy 
and geochemistry data with a chronology derived from radiocarbon 
dating, we recorded seven periods of increased storm activity 
at 6300-6100, 5650-5400, 4400-4050, 3650-3200, 2800-2600, 1950-1400 
and 400-50 cal yr BP (in the Little Ice Age). In contrast, our 
results show that the Medieval Climate Anomaly (1150-650 cal yr BP) 
was characterised by low storm activity. The evidence for high 
storm activity in the NW Mediterranean Sea is in agreement with 
the changes in coastal hydrodynamics observed over the Eastern 
North Atlantic and seems to correspond to Holocene cooling in
the North Atlantic. Periods of low SSTs there may have led to 
a stronger meridional temperature gradient and a southward 
migration of the westerlies. We hypothesise that the increase 
in storm activity during Holocene cold events over the North 
Atlantic and Mediterranean regions was probably due to an 
increase in the thermal gradient that led to an enhanced 
lower tropospheric baroclinicity over a large Central 
Atlantic-European domain.
 
          STUDY NOTES: A 7000-yr high-resolution record of past storm events 
using a multi-proxy analysis of sedimentary deposits 
from a lagoonal environment in the Gulf of Lions 
in the North-Western Mediterranean Sea.

Core PB06 is a 7.9-m-long well-dated piston core 
from the Pierre Blanche lagoon in the Palavasian 
wetland complex on the Gulf of Lions shore line, 
water depths ~60 cm.  Clay minerals were identified 
by X-ray diffraction (XRD). The ratios of smectite/
(illite+chlorite) were used as indicators to reconstruct 
changes in the sedimentation sources from the Mosson 
drainage basin versus the marine environment, and have 
been shown to be strongly linked to paleostorm events. 
Low values of SM/(Il+Cl) ratio correspond to periods 
of high storm activity in the NW Mediterranean Sea. 
</Abstract>
  </Summary>
  <Related_URL>
    <URL_Content_Type>
      <Type>GET DATA</Type>
    </URL_Content_Type>
    <URL>https://www1.ncdc.noaa.gov/pub/data/paleo/contributions_by_author/sabatier2012/sabatier2012.txt</URL>
  </Related_URL>
  <Related_URL>
    <URL_Content_Type>
      <Type>GET DATA</Type>
    </URL_Content_Type>
    <URL>https://www1.ncdc.noaa.gov/pub/data/paleo/contributions_by_author/sabatier2012/sabatier2012.xls</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>2018-12-11</DIF_Creation_Date>
  <Last_DIF_Revision_Date>2018-12-11</Last_DIF_Revision_Date>
</DIF>
