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<front>
<journal-meta>
<journal-id journal-id-type="publisher">BG</journal-id>
<journal-title-group>
<journal-title>Biogeosciences</journal-title>
<abbrev-journal-title abbrev-type="publisher">BG</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">Biogeosciences</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1726-4189</issn>
<publisher><publisher-name>Copernicus Publications</publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/bg-5-1741-2008</article-id>
<title-group>
<article-title>Bacteria in Himalayan glacial ice and its relationship to dust</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Zhang</surname>
<given-names>S.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Hou</surname>
<given-names>S.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Wu</surname>
<given-names>Y.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Qin</surname>
<given-names>D.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>State Key Laboratory of Cryospheric Sciences, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Department of life science, Shangqiu Normal University, Shangqiu 476000, China</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>School of Life Science, Lanzhou University, Lanzhou 730000, China</addr-line>
</aff>
<pub-date pub-type="epub">
<day>15</day>
<month>12</month>
<year>2008</year>
</pub-date>
<volume>5</volume>
<issue>6</issue>
<fpage>1741</fpage>
<lpage>1750</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2008 S. Zhang et al.</copyright-statement>
<copyright-year>2008</copyright-year>
<license license-type="open-access">
<license-p>This work is licensed under the Creative Commons Attribution 3.0 Unported License. To view a copy of this licence, visit <ext-link ext-link-type="uri"  xlink:href="https://creativecommons.org/licenses/by/3.0/">https://creativecommons.org/licenses/by/3.0/</ext-link></license-p>
</license>
</permissions>
<self-uri xlink:href="https://bg.copernicus.org/articles/5/1741/2008/bg-5-1741-2008.html">This article is available from https://bg.copernicus.org/articles/5/1741/2008/bg-5-1741-2008.html</self-uri>
<self-uri xlink:href="https://bg.copernicus.org/articles/5/1741/2008/bg-5-1741-2008.pdf">The full text article is available as a PDF file from https://bg.copernicus.org/articles/5/1741/2008/bg-5-1741-2008.pdf</self-uri>
<abstract>
<p>Concentrations and community diversity of bacteria from 50 segments of a
108.83 m ice core drilled from the East Rongbuk (ER) Glacier (28.03&amp;deg; N,
86.96&amp;deg; E, 6518 m above sea level) on the northeast slope of Mt. Qomolangma
(Everest), covering the period 950–1963 AD, were investigated by
epifluorescence microscope, DGGE and Shannon-Weaver index analysis. Bacteria
in the ER core were identified as β, γ-&lt;i&gt;proteobacteria&lt;/i&gt;
and &lt;i&gt;Firmicutes&lt;/i&gt; group, with γ-&lt;i&gt;proteobacteria&lt;/i&gt; being the dominance. Different bacterial population was
identified along the core, reflecting the effects of climatic and
environmental changes on the bacterial distribution in the glacial ice.
There are four general periods of bacterial diversity, corresponding to four
phases of dust abundance revealed by Ca&lt;sup&gt;2+&lt;/sup&gt; concentrations. However, a
previously suggested positive correlation between bacterial and Ca&lt;sup&gt;2+&lt;/sup&gt; 
concentrations was not indicated by our observations. Instead, a weak
negative correlation was found between these two parameters. Our results
suggest that bacterial community diversity, rather than concentrations,
might be a suitable biological proxy for the reconstruction of past climatic
and environmental changes preserved in glacial ice.</p>
</abstract>
<counts><page-count count="10"/></counts>
</article-meta>
</front>
<body/>
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