<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>Lim, Aaron</dc:creator>
  <dc:creator>Huvenne, Veerle A.I.</dc:creator>
  <dc:creator>Vertino, Agostina</dc:creator>
  <dc:creator>Spezzaferri, Silvia</dc:creator>
  <dc:creator>Wheeler, Andrew J.</dc:creator>
  <dc:date>2018-09-01</dc:date>
  <dc:description xmlns:ns0="xml" ns0:lang="en">Currents play a vital role in sustaining and developing deep water benthic habitats by  mobilising food and nutrients to otherwise relatively barren parts of the seabed. Where  sediment supply is significant, it can have a major influence on the development and  morphology of these habitats. This study examines a segment of the Belgica Mound  Province, NE Atlantic to better constrain the processes affecting a small-sized cold  water coral (CWC) mound habitat and conversely, the hydrodynamic influence of  CWC mounds on their own morphological development and surroundings. Here, we  utilise ROV-mounted multibeam, ROV-video data, and sediment samples to  investigate current processes, mound morphology, density and development. Detailed  mapping shows that the area may have the highest density of coral mounds recorded  so far, with three distinct mound types defined based on size, morphology and the  presence and degree of distinct scour features. A residual current of 36–40 cm s−1 is  estimated while large scour features suggest low-frequency, high-magnitude events.  These 3 mound types are i) smaller mounds with no scour; ii) mounds with scour in  one to two distinct directions and; iii) larger mounds with mound encircling scour. The  differing mound types likely had a staggered initiation where younger mounds  preferentially developed near clusters of pre-existing mounds. Given the high density  of these small CWC mounds, we support the hypothesis that over time, this clustering  may eventually lead to these mounds coalescing into larger coral mound features.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>https://folia.unifr.ch/global/documents/307186</dc:identifier>
  <dc:identifier>https://folia.unifr.ch/documents/307186/files/spe_nif.pdf</dc:identifier>
  <dc:language>eng</dc:language>
  <dc:relation>info:eu-repo/semantics/altIdentifier/doi/10.1016/j.margeo.2018.06.006</dc:relation>
  <dc:rights>info:eu-repo/semantics/openAccess</dc:rights>
  <dc:rights>License undefined</dc:rights>
  <dc:source>Marine Geology. - 2018, vol. 403, p. 225–237</dc:source>
  <dc:subject>info:eu-repo/classification/udc/57</dc:subject>
  <dc:title xmlns:ns1="xml" ns1:lang="en">New insights on coral mound development from groundtruthed high-resolution ROV-mounted multibeam imaging</dc:title>
  <dc:type>http://purl.org/coar/resource_type/c_6501</dc:type>
</oai_dc:dc>
