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        <identifier>doi:10.1594/pangaea.735745</identifier>
        <datestamp>2025-11-04T01:21:31Z</datestamp>
        <setSpec>PANGAEA</setSpec>
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          <dc:title>Geochemical and palynological results of IODP Hole 302-M0004A from Lomonosov Ridge, Arctic Ocean</dc:title>
          <dc:creator>Sluijs, Appy</dc:creator>
          <dc:creator>Schouten, Stefan</dc:creator>
          <dc:creator>Donders, Timme H</dc:creator>
          <dc:creator>Schoon, Petra L</dc:creator>
          <dc:creator>Röhl, Ursula</dc:creator>
          <dc:creator>Reichart, Gert-Jan</dc:creator>
          <dc:creator>Sangiorgi, Francesca</dc:creator>
          <dc:creator>Kim, Jung-Hyun</dc:creator>
          <dc:creator>Sinninghe Damsté, Jaap S</dc:creator>
          <dc:creator>Brinkhuis, Henk</dc:creator>
          <dc:publisher>PANGAEA</dc:publisher>
          <dc:date>2010</dc:date>
          <dc:date>Collected: 2004-08-27T00:00:00</dc:date>
          <dc:date>Issued: 2010</dc:date>
          <dc:relation>doi:10.1038/ngeo668</dc:relation>
          <dc:relation>igsn:10.58100/IBCR0302RHVS001</dc:relation>
          <dc:subject>Exp302</dc:subject>
          <dc:subject>CCGS Captain Molly Kool (Vidar Viking)</dc:subject>
          <dc:subject>Integrated Ocean Drilling Program / International Ocean Discovery Program (IODP)</dc:subject>
          <dc:description>Several episodes of abrupt and transient warming, each lasting between 50,000 and 200,000 years, punctuated the long-term warming during the Late Palaeocene and Early Eocene (58 to 51 Myr ago) epochs**1,2. These hyperthermal events, such as the Eocene Thermal Maximum 2 (ETM2) that took place about 53.5 Myr ago**2, are associated with rapid increases in atmospheric CO2 content. However, the impacts of most events are documented only locally**3,4. Here we show, on the basis of estimates from the TEX86' proxy, that sea surface temperatures rose by 3-5 °C in the Arctic Ocean during the ETM2. Dinoflagellate fossils demonstrate a concomitant freshening and eutrophication of surface waters, which resulted in euxinia in the photic zone. The presence of palm pollen implies**5 that coldest month mean temperatures over the Arctic land masses were no less than 8 °C, in contradiction of model simulations that suggest hyperthermal winter temperatures were below freezing**6. In light of our reconstructed temperature and hydrologic trends, we conclude that the temperature and hydrographic responses to abruptly increased atmospheric CO2 concentrations were similar for the ETM2 and the better-described Palaeocene-Eocene Thermal Maximum**7,8, 55.5 Myr ago.</dc:description>
          <dc:description>Supplement to: Sluijs, Appy; Schouten, Stefan; Donders, Timme H; Schoon, Petra L; Röhl, Ursula; Reichart, Gert-Jan; Sangiorgi, Francesca; Kim, Jung-Hyun; Sinninghe Damsté, Jaap S; Brinkhuis, Henk (2009): Warm and wet conditions in the Arctic region during Eocene Thermal Maximum 2. Nature Geosciences, 2, 777-780</dc:description>
          <dc:language>en</dc:language>
          <dc:type>Collection</dc:type>
          <dc:type>Supplementary Publication Series of Datasets</dc:type>
          <dc:format>application/zip</dc:format>
          <dc:rights>Creative Commons Attribution 3.0 Unported</dc:rights>
          <dc:rights>https://creativecommons.org/licenses/by/3.0/legalcode</dc:rights>
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