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        <identifier>doi:10.1594/pangaea.858994</identifier>
        <datestamp>2024-07-20T14:42:32Z</datestamp>
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  <identifier identifierType="DOI">10.1594/PANGAEA.858994</identifier>
  <creators>
    <creator>
      <creatorName>Warny, Sophie</creatorName>
      <givenName>Sophie</givenName>
      <familyName>Warny</familyName>
      <nameIdentifier nameIdentifierScheme="ORCID" schemeURI="http://orcid.org/">0000-0002-3451-040X</nameIdentifier>
    </creator>
    <creator>
      <creatorName>Askin, R A</creatorName>
      <givenName>R A</givenName>
      <familyName>Askin</familyName>
    </creator>
    <creator>
      <creatorName>Hannah, Mike J</creatorName>
      <givenName>Mike J</givenName>
      <familyName>Hannah</familyName>
    </creator>
    <creator>
      <creatorName>Mohr, Barbara A R</creatorName>
      <givenName>Barbara A R</givenName>
      <familyName>Mohr</familyName>
    </creator>
    <creator>
      <creatorName>Raine, J Ian</creatorName>
      <givenName>J Ian</givenName>
      <familyName>Raine</familyName>
      <nameIdentifier nameIdentifierScheme="ORCID" schemeURI="http://orcid.org/">0000-0001-5294-2102</nameIdentifier>
    </creator>
    <creator>
      <creatorName>Harwood, David M</creatorName>
      <givenName>David M</givenName>
      <familyName>Harwood</familyName>
      <nameIdentifier nameIdentifierScheme="ORCID" schemeURI="http://orcid.org/">0000-0002-9449-2127</nameIdentifier>
    </creator>
    <creator>
      <creatorName>Florindo, Fabio</creatorName>
      <givenName>Fabio</givenName>
      <familyName>Florindo</familyName>
      <nameIdentifier nameIdentifierScheme="ORCID" schemeURI="http://orcid.org/">0000-0002-6058-9748</nameIdentifier>
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  <titles>
    <title>(Supplement) Concentration in palynomorphs per gram of dry sediment in ANDRILL core AND-2A</title>
  </titles>
  <publisher>PANGAEA</publisher>
  <publicationYear>2009</publicationYear>
  <subjects>
    <subject subjectScheme="Parameter">Core</subject>
    <subject subjectScheme="Parameter">DEPTH, sediment/rock</subject>
    <subject subjectScheme="Parameter">Palynomorpha</subject>
    <subject subjectScheme="Parameter">Nothofagidites spp.</subject>
    <subject subjectScheme="Parameter">Podocarpidites sp.</subject>
    <subject subjectScheme="Parameter">Palynomorpha, terrestrial</subject>
    <subject subjectScheme="Parameter">Algae, freshwater</subject>
    <subject subjectScheme="Parameter">Pyxidinopsis braboi</subject>
    <subject subjectScheme="Parameter">Operculodinium centrocarpum</subject>
    <subject subjectScheme="Method">Drilling/drill rig</subject>
    <subject subjectScheme="Campaign">SMS</subject>
    <subject subjectScheme="Basis">McMurdo Station</subject>
    <subject subjectScheme="Project">Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas (SPP1158)</subject>
  </subjects>
  <dates>
    <date dateType="Collected">2007-10-10T12:00:00/2007-11-30T12:00:00</date>
  </dates>
  <resourceType resourceTypeGeneral="Dataset">Supplementary Dataset</resourceType>
  <relatedIdentifiers>
    <relatedIdentifier relationType="IsSupplementTo" relatedIdentifierType="DOI">10.1130/G30139A.1</relatedIdentifier>
  </relatedIdentifiers>
  <sizes>
    <size>348 data points</size>
  </sizes>
  <formats>
    <format>text/tab-separated-values</format>
  </formats>
  <rightsList>
    <rights rightsURI="https://creativecommons.org/licenses/by/3.0/" schemeURI="https://spdx.org/licenses/" rightsIdentifierScheme="SPDX" rightsIdentifier="CC-BY-3.0">Creative Commons Attribution 3.0 Unported</rights>
  </rightsList>
  <descriptions>
    <description descriptionType="Abstract">An exceptional triple palynological signal (unusually high abundance of marine, freshwater, and terrestrial palynomorphs) recovered from a core collected during the 2007 ANDRILL (Antarctic geologic drilling program) campaign in the Ross Sea, Antarctica, provides constraints for the Middle Miocene Climatic Optimum. Compared to elsewhere in the core, this signal comprises a 2000-fold increase in two species of dinoflagellate cysts, a synchronous five-fold increase in freshwater algae, and up to an 80-fold increase in terrestrial pollen, including a proliferation of woody plants. Together, these shifts in the palynological assemblages ca. 15.7 Ma ago represent a relatively short period of time during which Antarctica became abruptly much warmer. Land temperatures reached 10 °C (January mean), estimated annual sea-surface temperatures ranged from 0 to 11.5 °C, and increased freshwater input lowered the salinity during a short period of sea-ice reduction.</description>
    <description descriptionType="TechnicalInfo">Another version of this data can be found at http://www.geosociety.org/pubs/ft2009.htm with number 2009235.</description>
    <description descriptionType="Other">Supplement to: Warny, Sophie; Askin, R A; Hannah, Mike J; Mohr, Barbara A R; Raine, J Ian; Harwood, David M; Florindo, Fabio (2009): Palynomorphs from a sediment core reveal a sudden remarkably warm Antarctica during the middle Miocene. Geology, 37(10), 955-958</description>
  </descriptions>
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      <geoLocationPoint>
        <pointLongitude>165.276765</pointLongitude>
        <pointLatitude>-77.758141</pointLatitude>
      </geoLocationPoint>
    </geoLocation>
    <geoLocation>
      <geoLocationPlace>McMurdo Sound</geoLocationPlace>
    </geoLocation>
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  <fundingReferences>
    <fundingReference>
      <funderName>German Research Foundation</funderName>
      <funderIdentifier funderIdentifierType="Crossref Funder ID">https://doi.org/10.13039/501100001659</funderIdentifier>
      <awardNumber awardURI="https://gepris.dfg.de/gepris/projekt/5472008">5472008</awardNumber>
      <awardTitle>Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas</awardTitle>
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