<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>Fentimen, Robin</dc:creator>
  <dc:creator>Rüggeberg, Andres</dc:creator>
  <dc:creator>Lim, Aaron</dc:creator>
  <dc:creator>El Kateb, Akram</dc:creator>
  <dc:creator>Foubert, Anneleen</dc:creator>
  <dc:creator>Wheeler, Andrew J.</dc:creator>
  <dc:creator>Spezzaferri, Silvia</dc:creator>
  <dc:date>2018-10-01</dc:date>
  <dc:description xmlns:ns0="xml" ns0:lang="en">Cold-water coral ecosystems represent unique and exceptionally diverse  environments in the deep-sea. They are well developed along the Irish margin,  varying broadly in shape and size. The Moira Mounds, numerous small-sized mounds,  are nestled in the Belgica Mound Province (Porcupine Seabight, North-East Atlantic).  The investigation of living (Rose Bengal stained) and dead benthic foraminiferal  assemblages from these mounds allowed to describe their distribution patterns and to  evaluate their response to environmental variability. Quantitative data was statistically  treated to define groups of species/genera associated to specific habitats. The Moira  Mounds differ from their larger neighbours by the reduced spatial variability of benthic  foraminiferal assemblages, living assemblages only distinguishing coral-rich and  coral-barren areas. The ecological needs of corals are highlighted by the abundance  of Alabaminella weddellensis and Nonionella iridea, phytodetritus-feeding species in  coral supporting sediments. Living foraminifera in sediments from the Moira Mounds  concentrate in the upper first centimetre. Infaunal species may be affected by  bioturbation and/or reworking by the strong currents in the area. Dead foraminiferal  assemblages from the Moira Mounds resemble those described for the sandwave  facies in adjacent giant mounds, suggesting similar processes in facies deposition.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>https://folia.unifr.ch/global/documents/307325</dc:identifier>
  <dc:identifier>https://folia.unifr.ch/documents/307325/files/fou_bfd.pdf</dc:identifier>
  <dc:identifier>https://folia.unifr.ch/documents/307325/files/fou_bfd_sm.pdf</dc:identifier>
  <dc:language>eng</dc:language>
  <dc:relation>info:eu-repo/semantics/altIdentifier/doi/10.1007/s00015-018-0317-4</dc:relation>
  <dc:rights>info:eu-repo/semantics/openAccess</dc:rights>
  <dc:rights>License undefined</dc:rights>
  <dc:source>Swiss Journal of Geosciences. - 2018, vol. 111, no. 3, p. 561–572</dc:source>
  <dc:subject>info:eu-repo/classification/udc/55</dc:subject>
  <dc:title xmlns:ns1="xml" ns1:lang="en">Benthic foraminifera in a deep-sea high-energy environment: the Moira Mounds (Porcupine Seabight, SW of Ireland)</dc:title>
  <dc:type>http://purl.org/coar/resource_type/c_6501</dc:type>
</oai_dc:dc>
