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	<journal>
		<journal_title>Ocean Science</journal_title>
		<journal_url>www.ocean-sci.net</journal_url>
		<issn>1812-0784</issn>
		<eissn>1812-0792</eissn>
		<volume_number>6</volume_number>
		<issue_number>2</issue_number>
		<publication_year>2010</publication_year>
	</journal>
	<doi>10.5194/os-6-539-2010</doi>
	<article_url>http://www.ocean-sci.net/6/539/2010/</article_url>
	<abstract_html>http://www.ocean-sci.net/6/539/2010/os-6-539-2010.html</abstract_html>
	<fulltext_pdf>http://www.ocean-sci.net/6/539/2010/os-6-539-2010.pdf</fulltext_pdf>
	<start_page>539</start_page>
	<end_page>548</end_page>
	<publication_date>2010-06-04</publication_date>
	<article_title content_type="html">The role of continental shelves in nitrogen and carbon cycling: Northwestern North Atlantic case study</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>K. Fennel</name>
			<email>katja.fennel@dal.ca</email>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Dalhousie University, Department of Oceanography, Halifax, Canada</affiliation>
	</affiliations>
	<abstract content_type="html">Continental shelves play a key role in the cycling of nitrogen and
      carbon. Here the physical transport and biogeochemical transformation
      processes affecting the fluxes into and out of continental shelf
      systems are reviewed, and their role in the global cycling of both
      elements is discussed.      Uncertainties in the magnitude of organic and inorganic matter exchange
      between shelves and the open ocean is a major source of uncertainty in
      observation-based estimates of nitrogen and carbon fluxes.      The shelf-open ocean exchange is
      hard to quantify based on observations alone, but can be inferred from
      biogeochemical models.      Model-based nitrogen and carbon budgets are
      presented for the Northwestern North Atlantic continental
      shelf. Results indicate that shelves are an important sink for fixed
      nitrogen and a source of alkalinity, but are not much more efficient
      in exporting organic carbon to the deep ocean than the adjacent open
      ocean for the shelf region considered.</abstract>
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</article>

