<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>Wisshak, Max</dc:creator>
  <dc:creator>Neumann, Hermann</dc:creator>
  <dc:creator>Rüggeberg, Andres</dc:creator>
  <dc:creator>Büscher, Janina V.</dc:creator>
  <dc:creator>Linke, Peter</dc:creator>
  <dc:creator>Raddatz, Jacek</dc:creator>
  <dc:date>2019-11-18</dc:date>
  <dc:description xmlns:ns0="xml" ns0:lang="en">The Arctic Svalbard Archipelago hosts the world’s northernmost cold-water ‘carbonate  factories’ thriving here despite of presumably unfavourable environmental conditions  and extreme seasonality. Two contrasting sites of intense biogenic carbonate  production, the rhodolith beds in Mosselbukta in the north of the archipelago and the  barnacle-mollusc dominated carbonate sediments accumulating in the strong  hydrodynamic regime of the Bjørnøy-Banken south of Spitsbergen, were the targets of  the RV Maria S. Merian cruise 55 in June 2016. By integrating data from physical  oceanography, marine biology, and marine geology, the present contribution  characterises the environmental setting and biosedimentary dynamics of these two  polar carbonate factories. Repetitive CTD profiling in concert with autonomous  temperature/salinity loggers on a long-term settlement platform identified  spatiotemporal patterns in the involved Atlantic and Polar water masses, whereas  short-term deployments of a lander revealed fluctuations of environmental variables in  the rhodolith beds in Mosselbukta and at same depth (46 m) at Bjørnøy-Banken. At  both sites, dissolved inorganic nutrients in the water column were found depleted  (except for elevated ammonium concentrations) and show an overall increase in  concentration and N:P ratios toward deeper waters. This indicates that a recycling  system was fuelling primary production after the phytoplankton spring bloom at the  time of sampling in June 2016. Accordingly, oxygen levels were found elevated and  carbon dioxide concentrations (pCO2) markedly reduced, on average only half the  expected equilibrium values. Backed up by seawater stable carbon and oxygen  isotope signatures, this is interpreted as an effect of limited air-sea gas exchange  during seasonal ice cover in combination with a boost in community photosynthesis  during the spring phytoplankton bloom. The observed trends are enhanced by the  onset of rhodophyte photosynthesis in the rhodolith beds during the polar day upon  retreat of sea-ice. Potential adverse effects of ocean acidification on the local calcifier  community are thus predicted to be seasonally buffered by the marked drop in pCO2  during the phase of sea-ice cover and spring phyto-plankton bloom, but this effect will  diminish should the seasonal sea-ice formation continue to decline. Among the 25  macrobenthos taxa identified from images captured by the lander’s camera system, all  but three species were calcifiers contributing to the carbonate production. Biodiversity  was found to be much higher in Mosselbukta (21 taxa) compared to Bjørnøy-Banken  (8 taxa), which is considered as a result of enhanced habitat diversity provided in the  rhodolith beds by the bioengineering crustose alga Lithothamnion glaciale. Filter- feeding activity of selected key species did reveal group-specific but no common  activity patterns. Biotic disturbance of the filtering activity was common, in contrast to  abiotic factors, with hermit crabs representing the primary trigger. Motion tracking of  rhodoliths revealed a high frequency of dislocation, triggered not by abiotic factors but  by the activity of benthic invertebrates, in particular echinoids ploughing below or  moving over the rhodoliths. The echinoid Strongylocentrotus sp. is the most abundant  component of the associated fauna, thereby considerably contributing both to  carbonate production and to grazing bioerosion. Together, these results portray a high  degree of seasonal as well as short-term dynamics in environmental conditions that  despite many similarities support distinctly different communities and biodiversity  patterns in the calcifying macrobenthos at the two studied polar carbonate factories.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>https://folia.unifr.ch/global/documents/308440</dc:identifier>
  <dc:identifier>https://folia.unifr.ch/documents/308440/files/rue_ede.pdf</dc:identifier>
  <dc:language>eng</dc:language>
  <dc:relation>info:eu-repo/semantics/altIdentifier/doi/10.3389/fmars.2019.00667</dc:relation>
  <dc:rights>info:eu-repo/semantics/openAccess</dc:rights>
  <dc:rights>License undefined</dc:rights>
  <dc:source>Frontiers in Marine Science. - 2019, vol. 6, p. 667</dc:source>
  <dc:subject>info:eu-repo/classification/udc/57</dc:subject>
  <dc:title xmlns:ns1="xml" ns1:lang="en">Epibenthos dynamics and environmental fluctuations in two contrasting polar carbonate factories (Mosselbukta and Bjørnøy-banken, svalbard)</dc:title>
  <dc:type>http://purl.org/coar/resource_type/c_6501</dc:type>
</oai_dc:dc>
