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<article language="en">
	<journal>
		<journal_title>The Cryosphere Discussions</journal_title>
		<journal_url>www.the-cryosphere-discuss.net</journal_url>
		<issn>1994-0432</issn>
		<eissn>1994-0440</eissn>
		<volume_number>4</volume_number>
		<issue_number>3</issue_number>
		<publication_year>2010</publication_year>
	</journal>
	<doi>10.5194/tcd-4-1561-2010</doi>
	<article_url>http://www.the-cryosphere-discuss.net/4/1561/2010/</article_url>
	<abstract_html>http://www.the-cryosphere-discuss.net/4/1561/2010/tcd-4-1561-2010.html</abstract_html>
	<fulltext_pdf>http://www.the-cryosphere-discuss.net/4/1561/2010/tcd-4-1561-2010.pdf</fulltext_pdf>
	<start_page>1561</start_page>
	<end_page>1591</end_page>
	<publication_date>2010-09-02</publication_date>
	<article_title content_type="html">Glaciochemical investigations on the subterranean ice deposit of Vukušić Ice Cave, Velebit Mountain, Croatia</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>Z. Kern</name>
			<email>kern@geochem.hu</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>I. Fórizs</name>
		</author>
		<author numeration="3" affiliations="2">
			<name>N. Horvatinčić</name>
		</author>
		<author numeration="4" affiliations="3">
			<name>É. Széles</name>
		</author>
		<author numeration="5" affiliations="4">
			<name>N. Bočić</name>
		</author>
		<author numeration="6" affiliations="5">
			<name>B. Nagy</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Institute for Geochemical Research, Hungarian Academy of Sciences, Budapest, Hungary</affiliation>
		<affiliation numeration="2" content_type="html">Laboratory for Measurements of Low-level Radioactivity, Ruđer Bošković Institute, Zagreb, Croatia</affiliation>
		<affiliation numeration="3" content_type="html">Institute of Isotopes, Hungarian Academy of Sciences, Budapest, Hungary</affiliation>
		<affiliation numeration="4" content_type="html">Department of Geography, Faculty of Science, University of Zagreb, Zagreb, Croatia</affiliation>
		<affiliation numeration="5" content_type="html">Department of Physical Geography, Eötvös Loránd University, Budapest, Hungary</affiliation>
	</affiliations>
	<abstract content_type="html">The &lt;sup&gt;3&lt;/sup&gt;H activity, &lt;sup&gt;18&lt;/sup&gt;O/&lt;sup&gt;16&lt;/sup&gt;O and &lt;sup&gt;2&lt;/sup&gt;H/&lt;sup&gt;1&lt;/sup&gt;H ratio and
concentration of 33 metals and metalloids have been analysed on ice core
samples from the perennial subterranean cave ice deposit of Vukušić Ice
Cave, Velebit Mt. The tritium data suggested that the ice deposition at
2–2.4 m depth is build from precipitation fallen ~45 years before
sampling and the uppermost ice layer could be estimated between early 1970s
and early 1980s or between ~1954 and 1960. Both the fluctuation range
of stable water isotopes and the derived isotopic waterline of the ice agree
reasonably well with the corresponding data of the local precipitation. This
fact predicts that the potential of Vukušić Ice Cave&apos;s ice deposit is
superior for paleoclimatological studies to the nearby Ledena Pit. Principal
component analysis helped to select three groups of elements. The Ca-Mg
governed group (PC1) encompasses the bedrock related components; hence the
fluctuation of these elements might reflect the past intensities of the
dissolution process of the adjacent epikarst. The Zn governed group (PC2)
preserves probably an atmospheric deposition signal and related to the
emission of regional non-ferrous metallurgy. PC3 is governed by Al and Fe.
This probably carries the distal, non-karstic crustal signal hence might be
related to the past atmospheric circulation (i.e. wind direction and speed).</abstract>
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