| Literature DB >> 33168153 |
Dolly N Kothawala1, Anne M Kellerman2, Núria Catalán3, Lars J Tranvik4.
Abstract
The global carbon cycle connects organic matter (OM) pools in soil, freshwater, and marine ecosystems with the atmosphere, thereby regulating their size and reactivity. Due to the complexity of biogeochemical processes and historically compartmentalized subdisciplines, ecosystem-specific conceptualizations of OM degradation have emerged independently of developments in other ecosystems. Recent discussions regarding the relative importance of molecular composition and ecosystem properties on OM degradation have diverged in opposing directions across subdisciplines, leaving our understanding inconsistent. Ecosystem-dependent theories are problematic since properties unique to an ecosystem may change in response to anthropogenic stressors, including climate change. The next breakthrough in our understanding of OM degradation requires a shift in focus towards developing a unified theory of controls on OM across ecosystems.Entities:
Keywords: biogeochemical cycles; degradation rates; dissolved organic matter; freshwater; global carbon cycle; marine; organic matter; organic matter persistence; soil
Year: 2020 PMID: 33168153 DOI: 10.1016/j.tree.2020.10.006
Source DB: PubMed Journal: Trends Ecol Evol ISSN: 0169-5347 Impact factor: 17.712