Limnology/Department of Ecology and Genetics, Uppsala University, Norbyvägen18D, Uppsala 75236, Sweden.
National High Magnetic Field Laboratory Geochemistry Group and Department of Earth, Ocean, and Atmospheric Science, Florida State University, Tallahassee, FL 32306, USA.
Trends Ecol Evol. 2021 Feb;36(2):113-122. doi: 10.1016/j.tree.2020.10.006. Epub 2020 Nov 6.
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 disciplines, 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.
全球碳循环将土壤、淡水和海洋生态系统中的有机物质 (OM) 库与大气联系起来,从而调节它们的大小和反应性。由于生物地球化学过程的复杂性和历史上的学科分隔,OM 降解的生态系统特定概念已经独立于其他生态系统的发展而出现。最近关于分子组成和生态系统特性对 OM 降解相对重要性的讨论在不同的子学科中朝着相反的方向发展,导致我们的理解不一致。依赖于生态系统的理论存在问题,因为生态系统特有的特性可能会因人为胁迫(包括气候变化)而发生变化。要想深入了解 OM 降解,下一个突破需要将重点转移到开发跨生态系统 OM 控制的统一理论上来。