<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-10419</Entry_ID>
  <Entry_Title>California Margin ODP1018 600KYr Multiproxy Data </Entry_Title>
  <Data_Set_Citation>
    <Dataset_Creator>Lyle, M.; Heusser, L.E.; Ravelo, A.C.; Olivarez Lyle, A.; Andreasen, D.H.; Diffenbaugh, N.</Dataset_Creator>
    <Dataset_Title>California Margin ODP1018 600KYr Multiproxy Data </Dataset_Title>
    <Dataset_Release_Date>2010-07-19</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/10419</Online_Resource>
  </Data_Set_Citation>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>M.</First_Name>
    <Last_Name>Lyle</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>L.E.</First_Name>
    <Last_Name>Heusser</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>A.C.</First_Name>
    <Last_Name>Ravelo</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>A.</First_Name>
    <Last_Name>Olivarez Lyle</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>D.H.</First_Name>
    <Last_Name>Andreasen</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>N.</First_Name>
    <Last_Name>Diffenbaugh</Last_Name>
  </Personnel>
  <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>hydrology</Keyword>
  <Paleo_Temporal_Coverage>
    <Paleo_Start_Date>613570 cal yr BP</Paleo_Start_Date>
    <Paleo_Stop_Date>2680 cal yr BP</Paleo_Stop_Date>
  </Paleo_Temporal_Coverage>
  <Data_Set_Progress>Complete</Data_Set_Progress>
  <Spatial_Coverage>
    <Southernmost_Latitude>36.989</Southernmost_Latitude>
    <Northernmost_Latitude>36.989</Northernmost_Latitude>
    <Westernmost_Longitude>-123.276</Westernmost_Longitude>
    <Easternmost_Longitude>-123.276</Easternmost_Longitude>
    <Minimum_Altitude>-2477</Minimum_Altitude>
    <Maximum_Altitude>-2477</Maximum_Altitude>
  </Spatial_Coverage>
  <Location>
    <Location_Category>Ocean</Location_Category>
    <Location_Type>Pacific Ocean</Location_Type>
    <Location_Subregion1>Eastern Pacific Ocean</Location_Subregion1>
    <Detailed_Location>ODP1018&gt;LATITUDE 36.989&gt;LONGITUDE -123.276</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>Lyle, M., L. Heusser, C. Ravelo, A. Olivarez Lyle, D. Andreassen, and N. Diffenbaugh</Author>
    <Publication_Date>2010</Publication_Date>
    <Title>The Pleistocene water cycle and eastern boundary current processes  along the California continental margin</Title>
    <Series>Paleoceanography</Series>
    <Volume>25</Volume>
    <Report_Number>PA4211</Report_Number>
    <DOI>10.1029/2009PA001836 </DOI>
  </Reference>
  <Summary>
    <Abstract>Coastal marine sediments contain mixtures of terrestrial and marine 
paleoclimate proxies that record how the coastal water cycle has 
behaved over long time frames. We explore a 600-kyr marine record 
from ODP Site 1018, located due west of Santa Cruz, California, 
to identify coastal wet and dry periods, and to associate them 
with oceanographic processes. Wet periods in central California, 
identified by increased tree pollen relative to pollen from 
grasslands and scrublands, are found on every major deglaciation 
in the last 600 kyr. Sea surface temperature (SST) data were collected 
for the last 2 deglaciation.  Wet periods are associated with a rapid 
rise in SST off central California. SST gradients along the California 
margin and changes in biogenic deposition show that wet periods in 
central California are associated with a weakening of the California 
Current and weakened coastal upwelling. High carbonate production 
suggests that there was significant curl-of-windstress upwelling 
offshore. We propose that wet periods in Central California are 
associated with a meteorological connection to the tropical Pacific 
and weakened southward flow in the California Current that shunted 
temperate Pacific water northward into the Alaska gyre. We do not 
observe evidence for a south-shifted westerly storm track at the 
last glacial maximum but find that wet periods are diachronous 
along the California margin. The wettest period around the Santa 
Barbara Basin peaked at 16 ka, preceding the wet peak in central 
and northern California by 4 kyr. 
 
          STUDY NOTES: Multiproxy data from ODP Site 1018 off the central California coast. 
Data include stable isotopes, alkenone SST, carbon, biogenic silica, 
and terrestrial pollen data. 

Total organic carbon and carbonate data were measured from 
0 to 114.6 mbsf (2.8 to 614 ka). Age model is from oxygen 
isotope stratigraphy using a spline age model developed 
using Analyseries software (see Lyle et al. 2010). 
Sediments were freeze-dried, a split was analyzed for 
total carbon, and a second split was acidified and analyzed 
for organic carbon. The difference between total carbon and 
organic carbon was assigned to be inorganic carbon in CaCO3. 
CaCO3 was estimated by multiplying the inorganic carbon 
by 8.33, the CaCO3/C weight ratio. 

Alkenone sea surface temperature data were measured from 
0 to 31.9 mbsf (2.7 to 160 ka). Age model is from oxygen 
isotope stratigraphy using a spline age model developed 
using Analyseries software (see Lyle et al. 2010). 
Alkenones were extracted from sediments using methylene 
chloride-methanol, analyzed via gas chromatography, 
and reported as SST using the Muller et al (1998) 
calibration equation. 

Oxygen isotopes for Site 1018 are reported in Andreasen 
et al., [2000]. The &gt;250-um-size fraction was sampled 
for benthic foraminiferal species Cibicidoides wuellerstorfi, 
Cibicidoides pachyderma, and Uvigerina spp. Most analyses 
were conducted using one or two C. wuellerstorfi or three 
or four Uvigerina spp. tests.  However, the number of tests 
of C. wuellerstorfi analyzed ranged from shell fragments to 
four specimens. Occasional analyses were done using species 
C. pachyderma when C.wuellerstorfi were scarce. 
All values reported here are relative to VPDB. 

Pollen data were obtained using standard processing procedures. 
KOH and HF digestion and acetolysis were preceded and succeeded 
by sieving through 7-mm nylon screening [Heusser and Stock, 1984]. 
An exotic tracer (Lycopodium) was added prior to sieving to 
determine pollen concentration per gram of sediment. Taxonomic 
identification of pollen was based on comparison with modern pollen 
reference collections from western North America, and pollen counts 
were continued until at least 300 pollen grains were identified 
from each sample. 

Biogenic silica was measured by the method described in Anderson 
and Ravelo [2001]. Samples were freeze-dried, lightly ground, 
and sieved. Splits were extracted for biogenic Si by the Mortlock 
and Froelich [1989] extraction technique using Na2CO3 and 
analyzed via an automated spectrophotometric flow injection 
analysis system [Lachat QuickChem 8000]. 

</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/lyle2010/lyle2010.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/lyle2010/lyle2010.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>
