Temperature and soil organic matter decomposition rates - synthesis of current knowledge and a way forward

TLDR

Soil organic matter decomposition’s response to rising temperatures is pivotal for ecosystem change, yet studies show contradictory results, especially for long‑lived carbon pools that dominate soil stocks. The study aims to clarify how long‑term soil carbon pools respond to climate change to improve predictions of soil carbon storage. We synthesize diverse recent studies and propose a conceptual model that links soil OM availability to chemical conformation and physical protection, defining resistance via depolymerization, adsorption/desorption, and aggregate turnover. We conclude that better understanding of temperature sensitivity in substrate availability, depolymerization, microbial efficiency, and enzyme production is essential to predict soil carbon fate under warming.

Abstract

The response of soil organic matter (OM) decomposition to increasing temperature is a critical aspect of ecosystem responses to global change. The impacts of climate warming on decomposition dynamics have not been resolved due to apparently contradictory results from field and lab experiments, most of which has focused on labile carbon with short turnover times. But the majority of total soil carbon stocks are comprised of organic carbon with turnover times of decades to centuries. Understanding the response of these carbon pools to climate change is essential for forecasting longer-term changes in soil carbon storage. Herein, we briefly synthesize information from recent studies that have been conducted using a wide variety of approaches. In our effort to understand research to-date, we derive a new conceptual model that explicitly identifies the processes controlling soil OM availability for decomposition and allows a more explicit description of the factors regulating OM decomposition under different circumstances. It explicitly defines resistance of soil OM to decomposition as being due either to its chemical conformation (quality) or its physico-chemical protection from decomposition. The former is embodied in the depolymerization process, the latter by adsorption/desorption and aggregate turnover. We hypothesize a strong role for variation in temperature sensitivity as a function of reaction rates for both. We conclude that important advances in understanding the temperature response of the processes that control substrate availability, depolymerization, microbial efficiency, and enzyme production will be needed to predict the fate of soil carbon stocks in a warmer world.