<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:creator>Raddatz, Jacek</dc:creator>
  <dc:creator>Liebetrau, Volker</dc:creator>
  <dc:creator>Trotter, Julie</dc:creator>
  <dc:creator>Rüggeberg, Andres</dc:creator>
  <dc:creator>Flögel, Sascha</dc:creator>
  <dc:creator>Dullo, Wolf-Christian</dc:creator>
  <dc:creator>Eisenhauer, Anton</dc:creator>
  <dc:creator>Voigt, Silke</dc:creator>
  <dc:creator>McCulloch, Malcolm</dc:creator>
  <dc:date>2016-10-01</dc:date>
  <dc:description xmlns:ns0="xml" ns0:lang="en">High-latitude cold-water coral (CWC) reefs are particularly susceptible due to  enhanced CO₂ uptake in these regions. Using precisely dated (U/Th) CWCs (Lophelia  pertusa) retrieved during research cruise POS 391 (Lopphavet 70.6°N, Oslofjord  59°N) we applied boron isotopes (δ¹¹B), Ba/Ca, Li/Mg, and U/Ca ratios to reconstruct  the environmental boundary conditions of CWC reef growth. The sedimentary record  from these CWC reefs reveals a lack of corals between ~6.4 and 4.8 ka. The question  remains if this phenomenon is related to changes in the carbonate system or other  causes. The initial postglacial setting had elevated Ba/Ca ratios, indicative of meltwater  fluxes showing a decreasing trend toward cessation at 6.4 ka with an oscillation pattern  similar to continental glacier fluctuations. Downcore U/Ca ratios reveal an increasing  trend, which is outside the range of modern U/Ca variability in L. pertusa, suggesting  changes of seawater pH near 6.4 ka. The reconstructed bottom water temperature at  Lopphavet reveals a striking similarity to Barent sea surface and subsea surface  temperature records. We infer that meltwater pulses weakened the North Atlantic  Current system, resulting in southward advances of cold and CO₂-rich Arctic waters.  A corresponding shift in the δ¹¹B record from ~25.0‰ to ~27.0‰ probably implies  enhanced pH up-regulation of the CWCs due to the higher pCO₂ concentrations of  ambient seawater, which hastened mid-Holocene CWC reef decline on the Norwegian  margin.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>https://folia.unifr.ch/global/documents/305505</dc:identifier>
  <dc:identifier>https://folia.unifr.ch/documents/305505/files/rug_ech.pdf</dc:identifier>
  <dc:language>eng</dc:language>
  <dc:relation>info:eu-repo/semantics/altIdentifier/doi/10.1002/2016PA002974</dc:relation>
  <dc:rights>info:eu-repo/semantics/openAccess</dc:rights>
  <dc:rights>License undefined</dc:rights>
  <dc:source>Paleoceanography. - 2016, vol. 31, no. 10, p. 1350–1367</dc:source>
  <dc:subject xmlns:ns1="xml" ns1:lang="en">cold-water corals</dc:subject>
  <dc:subject xmlns:ns2="xml" ns2:lang="en">Lophelia pertusa</dc:subject>
  <dc:subject xmlns:ns3="xml" ns3:lang="en">boron isotopes</dc:subject>
  <dc:subject xmlns:ns4="xml" ns4:lang="en">Holocene</dc:subject>
  <dc:subject xmlns:ns5="xml" ns5:lang="en">pH upregulation</dc:subject>
  <dc:subject xmlns:ns6="xml" ns6:lang="en">Li/Mg</dc:subject>
  <dc:subject>info:eu-repo/classification/udc/574</dc:subject>
  <dc:title xmlns:ns7="xml" ns7:lang="en">Environmental constraints on Holocene cold‐water coral reef growth off Norway: Insights from a multiproxy approach</dc:title>
  <dc:type>http://purl.org/coar/resource_type/c_6501</dc:type>
</oai_dc:dc>
