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Pacaldo, Renato S.; Aydin, Mirac; Amarille, Randell Keith
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<identifier identifierType="URL">https://aperta.ulakbim.gov.tr/record/276025</identifier>
<creators>
<creator>
<creatorName>Pacaldo, Renato S.</creatorName>
<givenName>Renato S.</givenName>
<familyName>Pacaldo</familyName>
</creator>
<creator>
<creatorName>Aydin, Mirac</creatorName>
<givenName>Mirac</givenName>
<familyName>Aydin</familyName>
<affiliation>Kastamonu Univ, Fac Forestry, TR-3700 Kastamonu, Turkiye</affiliation>
</creator>
<creator>
<creatorName>Amarille, Randell Keith</creatorName>
<givenName>Randell Keith</givenName>
<familyName>Amarille</familyName>
</creator>
</creators>
<titles>
<title>Soil Respiration And Controls In Warmer Winter: A Snow Manipulation Study In Postfire And Undisturbed Black Pine Forests</title>
</titles>
<publisher>Aperta</publisher>
<publicationYear>2024</publicationYear>
<dates>
<date dateType="Issued">2024-01-01</date>
</dates>
<resourceType resourceTypeGeneral="Text">Journal article</resourceType>
<alternateIdentifiers>
<alternateIdentifier alternateIdentifierType="url">https://aperta.ulakbim.gov.tr/record/276025</alternateIdentifier>
</alternateIdentifiers>
<relatedIdentifiers>
<relatedIdentifier relatedIdentifierType="DOI" relationType="IsIdenticalTo">10.1002/ece3.11075</relatedIdentifier>
</relatedIdentifiers>
<rightsList>
<rights rightsURI="http://www.opendefinition.org/licenses/cc-by">Creative Commons Attribution</rights>
<rights rightsURI="info:eu-repo/semantics/openAccess">Open Access</rights>
</rightsList>
<descriptions>
<description descriptionType="Abstract"><p>Climate change impacts drive warmer winters, reduced snowfall, and forest fires. In 2020, a wildfire scorched about 1508 hectares of black pine (Pinus nigra Arnold) forests in T &amp; uuml;rkiye. Whether the combined effects of lack of snow and forest fires significantly alter winter soil respiration (R-s) and soil temperature remains poorly understood. A field experiment was conducted in the postfire and undisturbed black pine forests during the winter to quantify R-s rates as affected by lack of snow and forest fire. We applied four treatments: snow-exclusion postfire (SEPF), snow postfire (SPF), snow-exclusion-undisturbed forest (SEUF), and snow undisturbed forest (SUF). The SEPF exhibited the significantly lowest mean R-s rates (0.71 mu mol m(-2) s(-1)) compared to the SPF (1.02 mu mol m(-2) s(-1)), SEUF (1.44 mu mol m(-2) s(-1)), and SUF (1.48 mu mol m(-2) s(-1)). The R-s also showed significant variations with time (p &lt; .0001). However, treatments and time revealed no statistically significant interaction effects (p = .6801). Total winter R-s (January-March) ranged from 4.47 to 4.59 Mt CO2 ha(-1) in the undisturbed forest and 2.20 to 3.16 Mt CO2 ha(-2) in the postfire site. The R-s showed a significantly positive relationship (p &lt; .0001) with the soil (0.59) and air (0.46) temperatures and a significantly negative relationship (p = .0017) with the soil moisture (-0.20) at the 5 cm depth. In contrast, the R-s indicated a negative but not statistically significant relationship (p = .0932) with the soil moisture (-0.16) at the 10 cm soil depth. The combined effects of lack of snow and forest fire significantly decreased R-s, thus conserving the soil's organic carbon stocks and reducing the CO2 contribution to the atmosphere. In contrast, a warmer winter significantly increased R-s rates in the undisturbed forest, suggesting an acceleration of soil organic carbon losses and providing positive feedback to climate change.</p></description>
</descriptions>
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