Effect of Changes in Throughfall on Soil Respiration in Global Forest Ecosystems: A Meta-Analysis

Abstract

To date, there has been limited knowledge about how soil carbon dioxide (CO2) emissions from forest ecosystems at a global scale respond to the altered precipitation, and the key influencing mechanisms involved. Thirty-seven studies conducted under throughfall manipulation conditions in forest ecosystems around the globe were selected in this meta-analysis, with a total of 103 paired observations. Experimental categories such as climate types, forest types, soil texture, and the area size of changes in throughfall manipulation were included to qualify the responses of annual soil CO2 emissions to the altered throughfall. The responses of the annual soil CO2 emissions to the altered throughfall would be more sensitive in temperate forests than those in tropical and subtropical forests, probably due to the relatively long residence time of soil carbon (C) and the seasonal freeze–thaw events in temperate forests, as well as the relatively high concentration of non-structural carbohydrates in the belowground part of temperate terrestrial plants. A relatively large positive response of the soil CO2 emissions to the increased throughfall was observed in Mediterranean forests due to small precipitation during the growing season and mostly coarse-textured soils. Besides climate types, the sizes of the effect of the altered throughfall on the soil CO2 emissions (lnRCO2) varied with forest types and soil texture categories. Based on the regression analysis of the lnRCO2 values against the changes in throughfall, the annual soil CO2 emissions in forest ecosystems at a global scale would be increased by 6.9%, provided that the change in annual precipitation was increased by 10%. The results of structural equation modeling analysis indicate that fine root biomass and soil microbial biomass, along with the changes in annual precipitation, would substantially affect the altered throughfall-induced annual soil CO2 emissions in global forest ecosystems. The findings of this meta-analysis highlight that the measurement of soil respiration components, the priming effects of soil organic C decomposition, and C allocation between the aboveground and belowground parts of different tree species under the altered precipitation conditions, deserve more attention in the future.

Effect of In Situ Large Soil Column Translocation on CO2 and CH4 Fluxes under Two Temperate Forests of Northeastern China

“…These results indicate that changes in soil moisture induced by throughfall can, to some extent, affect the response to climate change in soil CO 2 emissions under temperate forests [11,15]. Based on various recent metaanalyses, soil CO 2 emissions in temperate forests are becoming more sensitive to climate changes, such as warming and precipitation, compared to those in boreal forests [13,14]. Hence, more field experiments on warming should be carried out at various specific sites in temperate forests, to precisely characterize the response of soil CO 2 emissions, especially soil heterotrophic respiration, to climate change.…”

“…Apart from soil C loss as CO 2 , well-drained forest soils are a major sink for atmospheric CH 4 and can play an important role in modulating the global CH 4 budget [8,9]. Climate warming and its attendant changes in precipitation are known to remarkably affect soil CO 2 emissions and CH 4 uptake in forest ecosystems across different climate zones, especially in temperate forests [2,4,5,8,[10][11][12][13][14]. The interaction between soil temperature and soil moisture can make the responses of soil CO 2 and CH 4 fluxes to climate change more complicated [5,12,15,16].…”