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<article language="en">
	<journal>
		<journal_title>Climate of the Past Discussions</journal_title>
		<journal_url>www.clim-past-discuss.net</journal_url>
		<issn>1814-9340</issn>
		<eissn>1814-9359</eissn>
		<volume_number>6</volume_number>
		<issue_number>4</issue_number>
		<publication_year>2010</publication_year>
	</journal>
	<doi>10.5194/cpd-6-1311-2010</doi>
	<article_url>http://www.clim-past-discuss.net/6/1311/2010/</article_url>
	<abstract_html>http://www.clim-past-discuss.net/6/1311/2010/cpd-6-1311-2010.html</abstract_html>
	<fulltext_pdf>http://www.clim-past-discuss.net/6/1311/2010/cpd-6-1311-2010.pdf</fulltext_pdf>
	<start_page>1311</start_page>
	<end_page>1335</end_page>
	<publication_date>2010-07-09</publication_date>
	<article_title content_type="html">A ~400 ka supra-Milankovitch cycle in the Na, Mg, Pb, Ni, and Co records of a ferromanganese  crust from the Vityaz fracture zone, central Indian ridge</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>R. Banerjee</name>
			<email>banerjee@nio.org</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>S. M. Gupta</name>
		</author>
		<author numeration="3" affiliations="2">
			<name>H. Miura</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>D. V. Borole</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Geological Oceanography Division, National Institute of oceanography, CSIR, Dona Paula, Goa 403 004,  India</affiliation>
		<affiliation numeration="2" content_type="html">Department of Natural History Sciences, Graduate School of Science, Hokkaido University, Sapporo  060-0810, Japan</affiliation>
	</affiliations>
	<abstract content_type="html">A ~400 ka (kilo years) supra-Milankovitch cycle, recorded in the sodium, magnesium,
      lead, nickel and cobalt contents of a 32 mm thick ferromanganese crust from Vityaz
      fracture zone, central Indian ridge is reported here. To arrive at the geological ages, we
      used both &lt;sup&gt;230&lt;/sup&gt;Th&lt;sub&gt;execcs&lt;/sub&gt; and
      Co-chronometric datings. The correlation coefficient between the &lt;sup&gt;230&lt;/sup&gt;Th&lt;sub&gt;execcs&lt;/sub&gt;
      based dates and Co-chronometric dates for the top 0–8 mm is very high (&lt;i&gt;r&lt;/i&gt;=0.9734, at
      99.9% significance). The cobalt chronometric age for the bottom most oxide layer of this
      crust is computed as 3.5 Ma. Red-fit and multi-taper spectral analyses of time series data
      revealed the existence of the significant ~400 ka cycle, representing the changes in
      the hydrogeochemical conditions in the ocean due to the Earth&apos;s orbital eccentricity related
      summer insolation at the equator. This is the first report of such cycle from a hydrogenous
      ferromanganese crust from equatorial Indian ocean.</abstract>
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