<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>Feenstra, Eline Juliette</dc:creator>
  <dc:creator>Birgel, Daniel</dc:creator>
  <dc:creator>Heindel, Katrin</dc:creator>
  <dc:creator>Wehrmann, Laura M.</dc:creator>
  <dc:creator>Jaramillo‐Vogel, David</dc:creator>
  <dc:creator>Grobéty, Bernard</dc:creator>
  <dc:creator>Frank, Norbert</dc:creator>
  <dc:creator>Hancock, Leanne G.</dc:creator>
  <dc:creator>Van Rooij, David</dc:creator>
  <dc:creator>Peckmann, Jörn</dc:creator>
  <dc:creator>Foubert, Anneleen</dc:creator>
  <dc:date>2020-02-03</dc:date>
  <dc:description xmlns:ns0="xml" ns0:lang="en">Cold‐water coral (CWC) mounds are build‐ups comprised of coral‐dominated intervals  alternating with a mixed carbonate‐siliciclastic matrix. At some locations, CWC  mounds are influenced by methane seepage, but the impact of methane on CWC  mounds is poorly understood. To constrain the potential impact of methane on CWC  mound growth, lipid biomarker investigations were combined with mineralogical and  petrographic analyses to investigate the anaerobic oxidation of methane (AOM) and  authigenic carbonate formation in sediment from a seep‐affected CWC mound in the  Gulf of Cadiz. The occurrence of AOM was confirmed by characteristic lipids found  within a semi‐lithified zone (SLZ) consisting of authigenic aragonite, high‐magnesium  calcite and calcium‐excess dolomite. The formation of high‐Mg calcite is attributed to  AOM, acting as a lithifying agent. Aragonite is only a minor phase. Ca‐excess  dolomite in the SLZ and upper parts may be formed by organoclastic sulphate  reduction, favouring precipitation by increased alkalinity. The AOM biomarkers in the  SLZ include isoprenoid‐based archaeal membrane lipids, such as abundant glycerol  dibiphytanyl glycerol tetraethers (GDGTs) dominated by GDGT‐2. The δ13C values of  GDGT‐2, measured as ether‐cleaved monocyclic biphytanes, are as low as −100‰  versus V‐PDB. Further, bacterial dialkyl glycerol diethers with two anteiso‐C15 alkyl  chains and δ13C values of −81‰ are interpreted as biomarkers of sulphate‐reducing  bacteria. The lipid biomarker signatures and mineralogical patterns suggest that  anaerobic methane‐oxidizing archaea of the ANME‐1 group thrived in the subsurface  at times of slow and diffusive methane seepage. Petrographic analyses revealed that  the SLZ was exhumed at some point (e.g. signs of bioerosion of the semi‐lithified  sediment), providing a hard substrate for CWC larval settlement. In addition, this work  reveals that AOM‐induced semi‐lithification likely played a role in mound stabilization.  Lipid biomarker analysis proves to be a powerful tool to disentangle early diagenetic  processes induced by microbial metabolisms.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>https://folia.unifr.ch/global/documents/308658</dc:identifier>
  <dc:identifier>https://folia.unifr.ch/documents/308658/files/fou_cfa.pdf</dc:identifier>
  <dc:identifier>https://folia.unifr.ch/documents/308658/files/fou_cfa_sm.pdf</dc:identifier>
  <dc:language>eng</dc:language>
  <dc:relation>info:eu-repo/semantics/altIdentifier/doi/10.1111/gbi.12373</dc:relation>
  <dc:rights>info:eu-repo/semantics/openAccess</dc:rights>
  <dc:rights>License undefined</dc:rights>
  <dc:source>Geobiology. - 2020, vol. 18, no. 2, p. 185–206</dc:source>
  <dc:subject>info:eu-repo/classification/udc/55</dc:subject>
  <dc:title xmlns:ns1="xml" ns1:lang="en">Constraining the formation of authigenic carbonates in a seepage-affected cold-water coral mound by lipid biomarkers</dc:title>
  <dc:type>http://purl.org/coar/resource_type/c_6501</dc:type>
</oai_dc:dc>
