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<front>
<journal-meta>
<journal-id journal-id-type="publisher">BGD</journal-id>
<journal-title-group>
<journal-title>Biogeosciences Discussions</journal-title>
<abbrev-journal-title abbrev-type="publisher">BGD</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">Biogeosciences Discuss.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1810-6285</issn>
<publisher><publisher-name></publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/bgd-10-851-2013</article-id>
<title-group>
<article-title>Biological soil crusts on initial soils: organic carbon dynamics and chemistry under temperate climatic conditions</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Dümig</surname>
<given-names>A.</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>Veste</surname>
<given-names>M.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Hagedorn</surname>
<given-names>F.</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>Fischer</surname>
<given-names>T.</given-names>
<ext-link>https://orcid.org/0000-0001-6235-2261</ext-link>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Lange</surname>
<given-names>P.</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Spröte</surname>
<given-names>R.</given-names>
</name>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Kögel-Knabner</surname>
<given-names>I.</given-names>
<ext-link>https://orcid.org/0000-0002-7216-8326</ext-link>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff6">
<sup>6</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Lehrstuhl für Bodenkunde, Department für Ökologie und Ökosystemmanagement, Wissenschaftszentrum Weihenstephan für Ernährung, Landnutzung und Umwelt, Technische Universität München, 85350 Freising-Weihenstephan, Germany</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Centrum für Energietechnologie Brandenburg e.V., Friedlieb-Runge-Strasse 3, 03046 Cottbus, Germany</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Department of Biogeochemistry, WSL, Swiss Federal Institute of Forest, Snow and Landscape Research, Zürcherstr. 111, 8903, Birmensdorf, Switzerland</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Brandenburg University of Technology at Cottbus, Faculty of Environmental Sciences and Process Engineering, Central Analytical Laboratory, Konrad-Wachsmann-Allee 6, 03046 Cottbus, Germany</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>Chair of Soil Protection and Recultivation, Brandenburg University of Technology, Konrad-Wachsmann-Allee 6, 03046 Cottbus, Germany</addr-line>
</aff>
<aff id="aff6">
<label>6</label>
<addr-line>Institute for Advanced Study, Technische Universität München, Lichtenbergstrasse 2a, 85748 Garching, Germany</addr-line>
</aff>
<pub-date pub-type="epub">
<day>16</day>
<month>01</month>
<year>2013</year>
</pub-date>
<volume>10</volume>
<issue>1</issue>
<fpage>851</fpage>
<lpage>894</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2013 A. Dümig et al.</copyright-statement>
<copyright-year>2013</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/preprints/10/851/2013/bgd-10-851-2013.html">This article is available from https://bg.copernicus.org/preprints/10/851/2013/bgd-10-851-2013.html</self-uri>
<self-uri xlink:href="https://bg.copernicus.org/preprints/10/851/2013/bgd-10-851-2013.pdf">The full text article is available as a PDF file from https://bg.copernicus.org/preprints/10/851/2013/bgd-10-851-2013.pdf</self-uri>
<abstract>
<p>Numerous studies have been carried out on the community structure and diversity of biological soil crusts (BSCs) as well as
      their important functions on ecosystem processes. However, the amount of BSC-derived organic carbon (OC) input into soils and
      its chemical composition under natural conditions has rarely been investigated. In this study, different development stages of
      algae- and moss-dominated BSCs were investigated on a~natural (&lt;17 yr old BSCs) and experimental sand dune (&lt;4 yr old BSCs) in northeastern Germany. We determined the OC accumulation in BSC-layers and the BSC-derived OC input
      into the underlying substrates for bulk materials and fractions &lt;63 &amp;mu;m. The chemical composition of OC was
      characterized by applying solid-state &lt;sup&gt;13&lt;/sup&gt;C NMR spectroscopy and analysis of the carbohydrate-C signature.&lt;sup&gt;14&lt;/sup&gt;C contents
      were used to assess the origin and dynamic of OC in BSCs and underlying substrates. Our results indicated a rapid BSC
      establishment and development from algae- to moss-dominated BSCs within only 4 yr under this temperate climate. The
      distribution of BSC types was presumably controlled by the surface stability according to the position in the slope. We found
      no evidence that soil properties influenced the BSC distribution on both sand dunes. &lt;sup&gt;14&lt;/sup&gt;C contents clearly indicated the
      existence of two OC pools in BSCs and substrates, recent BSC-derived OC and lignite-derived &quot;old&quot; OC (biologically
      refractory). The input of recent BSC-derived OC strongly decreased the mean residence time of total OC. The downward
      translocation of OC into the underlying substrates was only found for moss-dominated BSCs at the natural sand dune which may
      accelerate soil formation at these spots. BSC-derived OC mainly comprised O-alkyl C (carbohydrate-C) and to a lesser extent
      also alkyl C and N-alkyl C in varying compositions. Accumulation of alkyl C was only detected in BSCs at the experimental dune
      which may induce a~lower water solubility of BSC-derived extracellular polymeric substances when compared to BSCs at the
      natural sand dune indicating that hydrological effects of BSCs on soils depend on the chemical composition of the extracellular
      polymeric substances.</p>
</abstract>
<counts><page-count count="44"/></counts>
</article-meta>
</front>
<body/>
<back>
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