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<article language="en">
	<journal>
		<journal_title>Nonlinear Processes  in Geophysics</journal_title>
		<journal_url>www.nonlin-processes-geophys.net</journal_url>
		<issn>1023-5809</issn>
		<eissn>1607-7946</eissn>
		<volume_number>14</volume_number>
		<issue_number>6</issue_number>
		<publication_year>2007</publication_year>
	</journal>
	<doi>10.5194/npg-14-811-2007</doi>
	<article_url>http://www.nonlin-processes-geophys.net/14/811/2007/</article_url>
	<abstract_html>http://www.nonlin-processes-geophys.net/14/811/2007/npg-14-811-2007.html</abstract_html>
	<fulltext_pdf>http://www.nonlin-processes-geophys.net/14/811/2007/npg-14-811-2007.pdf</fulltext_pdf>
	<start_page>811</start_page>
	<end_page>821</end_page>
	<publication_date>2007-12-10</publication_date>
	<article_title content_type="html">Statistical measures of distribution patterns of silicon and calcium in marine sedimentary layers</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>K. Bube</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>T. Klenke</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>J. A. Freund</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>U. Feudel</name>
			<email>feudel@icbm.de</email>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Institut für Chemie und Biologie des Meeres, Carl von Ossietzky Universität Oldenburg, Germany</affiliation>
	</affiliations>
	<abstract content_type="html">We analyze electron microscope X-ray spectroscopy data of recent supratidal
  marine sediments. Statistical measures are used to characterize the
  distribution of silicon and calcium in different layers of the sediments. We
  also use cluster analysis and symbolic dynamics to filter measurement noise
  and to classify different density regions. This allows to calculate
  characteristic patch sizes which reflect the sizes of individual clastic
  grains and the corresponding pore sizes. Silicon indicates the independent
  processes in the sedimentation history of certain grains. Calcium is
  capable to monitor intrinsic early diagenetic processes of
  biogeochemical calcium mineralization of primary organic matter as
  documented in more organized distributions with higher clustering.</abstract>
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</article>

