How will a drier climate change carbon sequestration in soils of the deciduous forests of Central Europe?

Abstract

Global warming is accompanied by increasing water stress across much of our planet. We studied soil biological processes and changes in soil organic carbon (SOC) storage in 30 Hungarian oak forest sites in the Carpathian Basin along a climatic gradient (mean annual temperature (MAT) 9.6–12.1 °C, mean annual precipitation (MAP) 545–725 mm) but on similar gently sloped hillsides where the parent materials are loess and weathered dust inputs dating from the end of the ice age. The purpose of this research was to understand how a drying climate, predicted for this region, might regulate long-term SOC sequestration. To examine the effects of decreasing water availability, we compared soil parameters and processes in three categories of forest that represented the moisture extremes along our gradient and that were defined using a broken-stick regression model. Soil biological activity was significantly lower in the driest (“dry”) forests, which had more than double the SOC concentration in the upper 30 cm layer (3.28 g C/100 g soil ± 0.11 SE) compared to soils of the wettest (“humid”) forests (1.32 g C/100 g soil ± 0.09 SE), despite the fact that annual surface litter production in humid forests was ~ 37% higher than in dry forests. A two-pool SOM model constrained to fit radiocarbon data indicates that turnover times for fast and slow pools are about half as long in the humid soil compared to the dry soil, and humid soils transfer C twice as efficiently from fast to slow pools. Enzyme activity and fungal biomass data also imply shorter turnover times associated with faster degradation processes in the soils of humid forests. Thermogravimetry studies suggest that more chemically recalcitrant compounds are accumulating in the soils of dry forests. Taken together, our results suggest that the predicted climate drying in this region might increase SOC storage in Central European mesic deciduous forests even as litter production decreases.

Field-flow fractionation and gel permeation methods for total soil fungal mass determination

“…SOC concentration was 0.52% (Makádi, 2010) in this Arenosol, thus we expect total fungal mass to be low as well. SOC concentration in the Luvisols from the Síkfőkút Forest is significantly higher at 3.68% (Świtoniak et al, 2014), while that of Chernozem soil in Kerecsend Forest is 5.22% (Fekete et al, 2020b). The effect of SOC content on total fungal mass was clear in the soil types we examined (Table 4).…”

Impact of agriculture intensification on forest degradation and tree carbon stock; promoting multi‐criteria optimization for restoration in Central India

“…Soil is one of the major sinks for forest carbon storage and is a major factor in the regulation of all belowground ecological nutrient cycling (Fekete et al, 2021). The soil organic carbon potential varies with forest type, vegetation composition, litter quality, bulk density, and climatic variations (Chauhan et al, 2020; Saha & Bera, 2020).…”

The effect of mineral composition on soil organic matter turnover in temperate forest soils

“…However, SOM is not a single homogeneous pool; it can be divided into carbon pools with different decomposition kinetics: pools with fast turnover and others with slow turnover. Therefore, the residence time of SOM is very diverse, ranging from a few hours, weeks or months to as much as 10,000 years (Trumbore 2000;Kuzyakov 2006;Schmidt et al 2011;Fekete et al 2021) depending on many factors. The main mechanisms, which provides the resistance of organic matter -even over a longer timescaleagainst microbial decomposition are chemical and physical stabilization processes of SOM (Angst et al 2021).…”