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    <note>Funding for this research was provided by a small grant from the Marine Alliance for Science and Technology for Scotland (MASTS) and the Scottish Alliance for Geoscience, Environment and Society (SAGES) &quot;PECRE exchanges with Europe, North America, China, and India&quot;. The Leverhulme Trust Research Project Grant 2014-093 &quot;Calving Glaciers: Long Term Validation and Evidence&quot; funded field research activities and KMS at the University of Glasgow. JV was funded by the Natural Environment Research Council Centre for Doctoral Training in Oil &amp; Gas, received through Herriot-Watt University (James Watt Scholarship Scheme) and the British Geological Survey (British University Funding Initiative Scheme). JV would also like to acknowledge further support from Oil and Gas UK. AM was funded by the Environmental Protection Agency STAR Fellowship.</note>
    <abstract>Dataset included species abundance from 3 collection methods- transects, photo-quadrats, and benthic grabs. Carbonate and organic content was calculated via loss of ignition methodology in rhodoliths and that is included in the data sets as well.</abstract>
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