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<front>
<journal-meta>
<journal-id journal-id-type="publisher">EGUsphere</journal-id>
<journal-title-group>
<journal-title>EGUsphere</journal-title>
<abbrev-journal-title abbrev-type="publisher">EGUsphere</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">EGUsphere</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub"></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/egusphere-2022-1427</article-id>
<title-group>
<article-title>Bioturbation enhances C and N contents on near-surface soils in resource-deficient arid climate regions but shows adverse effects in more temperate climates</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Kraus</surname>
<given-names>Diana</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>Brandl</surname>
<given-names>Roland</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>Bendix</surname>
<given-names>Jörg</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>Grigusova</surname>
<given-names>Paulina</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>Köhler</surname>
<given-names>Sabrina</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>Larsen</surname>
<given-names>Annegret</given-names>
<ext-link>https://orcid.org/0000-0002-2241-0313</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>Pliscoff</surname>
<given-names>Patricio</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>Übernickel</surname>
<given-names>Kirstin</given-names>
<ext-link>https://orcid.org/0000-0002-3585-7309</ext-link>
</name>
<xref ref-type="aff" rid="aff6">
<sup>6</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Farwig</surname>
<given-names>Nina</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Department of Biology, Conservation Ecology, University of Marburg, 35043 Marburg, Germany</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Department of Biology, Animal Ecology, University of Marburg, 35043 Marburg, Germany</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Department of Geography, Laboratory for Climatology and Remote Sensing, University of Marburg, 35032 Marburg, Germany</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Department of Environmental Sciences, Soil Geography and Landscape, Wageningen University &amp; Research, 6708PB Wageningen, Netherlands</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>Department of Ecology and Biodiversity and Institute of Geography Center of Applied Ecology and Sustainability (CAPES), Catholic University of Chile, 8331150 Santiago, Chile</addr-line>
</aff>
<aff id="aff6">
<label>6</label>
<addr-line>Department of Geosciences, Earth System Dynamics, University of Tübingen, Tübingen, Germany</addr-line>
</aff>
<funding-group>
<award-group id="gs1">
<funding-source>Deutsche Forschungsgemeinschaft</funding-source>
<award-id>FA 925/12-1</award-id>
<award-id>BR 1293-18-1</award-id>
<award-id>BE1780/52-1</award-id>
<award-id>LA3521/1-1</award-id>
</award-group>
</funding-group>
<pub-date pub-type="epub">
<day>06</day>
<month>02</month>
<year>2023</year>
</pub-date>
<volume>2023</volume>
<fpage>1</fpage>
<lpage>21</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2023 Diana Kraus et al.</copyright-statement>
<copyright-year>2023</copyright-year>
<license license-type="open-access">
<license-p>This work is licensed under the Creative Commons Attribution 4.0 International License. To view a copy of this licence, visit <ext-link ext-link-type="uri"  xlink:href="https://creativecommons.org/licenses/by/4.0/">https://creativecommons.org/licenses/by/4.0/</ext-link></license-p>
</license>
</permissions>
<self-uri xlink:href="https://egusphere.copernicus.org/preprints/2023/egusphere-2022-1427/">This article is available from https://egusphere.copernicus.org/preprints/2023/egusphere-2022-1427/</self-uri>
<self-uri xlink:href="https://egusphere.copernicus.org/preprints/2023/egusphere-2022-1427/egusphere-2022-1427.pdf">The full text article is available as a PDF file from https://egusphere.copernicus.org/preprints/2023/egusphere-2022-1427/egusphere-2022-1427.pdf</self-uri>
<abstract>
<p>&lt;p&gt;Bioturbating animals can affect physical and chemical soil properties on near-surface soil by either foraging for food or constructing suitable habitats. Thereby, bioturbation can influence the soil texture either sorting or mixing the different grain sizes clay, silt and sand during burrowing. Additionally, bioturbating animals can increase the macronutrients carbon (C), nitrogen (N) and phosphorus (P) through the transport of nutrients by vertically mixing the soil column and the addition of the bioturbators&amp;rsquo; feces to the soil surface. To date, it is not clear how the effects of bioturbation on soil properties vary along an ecological gradient. Therefore, we compared the physical properties clay, silt and sand and the chemical contents of the macronutrients C, N and P for soil samples from mounds and the surrounding area as controls in three different climatic regions (arid, semi-arid and Mediterranean) of coastal Chile. To do so, we calculated the difference between the concentrations of paired mound and control samples. When comparing soil texture, we did not find significant differences between mound and control soil samples. For the macronutrient contents, the difference between mound and control C and N contents increased in the arid site and decreased in the two other research sites with increasing vegetation cover. Since we aimed to cover bioturbation patterns on a broader scale, we additionally compared our findings to other bioturbation studies performed in different biomes. Thereby, we found that other studies also show small differences in soil properties caused by bioturbation which are already sufficient to increase soil fertility.&lt;/p&gt;</p>
</abstract>
<counts><page-count count="21"/></counts>
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