Dynamics of soil organic carbon during natural forest succession in the Polish Carpathian Mountains
Authors: Józefowska Agnieszka , Sokołowska Justyna , Zaleski Tomasz 
Published: March 2021

&lt;p&gt;The main driver of the Carpathian landscape is the process of natural forest succession, which causes the overgrowing of the unique semi-natural meadows. Land-use changes influence the balance of organic carbon in the soil, simultaneously may cause carbon sequestration or CO&lt;sub&gt;2&lt;/sub&gt; emission. Whereas, there is still a lack of knowledge covering the impact of natural forest succession on organic carbon cycling. The purpose of this study was to investigate the dynamics of organic carbon in the different land-use soils. The selected properties showing the rate of mineralization process as well as soil biological activity were taken into account.&lt;/p&gt;&lt;p&gt;This study was located in three selected Carpathians&amp;#8217; national parks. Soil samples were taken from 0-10 cm and 10-20 cm soil layers of ten transects each consisting three different land use: semi-natural meadow, succession (30-75 aged trees), and old-growth forest (more than 150 years). Measurements of microbial biomass carbon (MBC), dissolved organic carbon (DOC), dehydrogenase (DHA) and invertase (INW) activity and microbial respiration were made on fresh soil samples. Based on the first-order kinetic model of microbial respiration the cumulative respiration was calculated. Additionally, the metabolic quotient (qCO&lt;sub&gt;2&lt;/sub&gt;), the microbial quotient (qMIC), and the mineralization quotient (qM) were calculated.&lt;/p&gt;&lt;p&gt;The mean C&lt;sub&gt;org&lt;/sub&gt; content ranged from 17.6 g kg&lt;sup&gt;-1&lt;/sup&gt; in the 10-20 cm layer of succession to 41.5 g kg&lt;sup&gt;-1&lt;/sup&gt; in the 0-10 cm layer of forest. Considering the individual land use variants in the 0-10 cm layer meadow characterised the highest MBC, DHA and qM, and the lowest qCO&lt;sub&gt;2&lt;/sub&gt; values. In the succession, the highest cumulative respiration and qCO&lt;sub&gt;2&lt;/sub&gt; and the lowest MBC and INW were noted. Whereas the forest characterised the highest INW and the lowest cumulative respiration, DHA, qMIC and qM. Similarity, in the 10-20 cm layer meadow the highest MBC and DHA as well as qMIC were found. The succession characterised the highest cumulative respiration, qCO&lt;sub&gt;2&lt;/sub&gt; and qM and the lowest qMIC. However, in the forest the highest INW and the lowest qCO&lt;sub&gt;2&lt;/sub&gt;, qMIC and qM were noticed.&lt;/p&gt;&lt;p&gt;Overall, for all investigated soils the positive correlations between C&lt;sub&gt;org&lt;/sub&gt; and MBC, DHA and negative correlations C&lt;sub&gt;org&lt;/sub&gt; with qMIC, qCO&lt;sub&gt;2&lt;/sub&gt; and DOC were shown. Whereas, when we take into consideration the individuals land use variants and depths can be stated that the content of organic carbon was shaped by different properties. In the 0-10 cm content of C&lt;sub&gt;org&lt;/sub&gt; in meadow and forest positive correlated with cumulative respiration and DHA, and negative with qM. Additionally, in forest negative correlations C&lt;sub&gt;org&lt;/sub&gt; with DOC, INW and qCO&lt;sub&gt;2&lt;/sub&gt; were found. While in succession the positive correlations C&lt;sub&gt;org&lt;/sub&gt; with MBC and INW and negative correlations C&lt;sub&gt;org&lt;/sub&gt; with DHA, qMIC and DOC were noted. In the 10-20 cm layers of meadow and succession C&lt;sub&gt;org&lt;/sub&gt; positive correlated with MBC, INW, qCO&lt;sub&gt;2&lt;/sub&gt; and negative with qM and DOC. Additionally, the qMIC positive correlation with C&lt;sub&gt;org&lt;/sub&gt; in meadow and negative correlation in succession was found. Whereas, in forest C&lt;sub&gt;org &lt;/sub&gt;positive correlated with qM and MBC, while negative correlations between C&lt;sub&gt;org&lt;/sub&gt; and qMIC, DOC and qCO&lt;sub&gt;2&lt;/sub&gt; were noticed.&lt;/p&gt;