生物地球化学
永久冻土
碳循环
湿地
原性土壤
土壤碳
环境科学
土壤呼吸
碳纤维
生态系统呼吸
分解者
通气组织
植被(病理学)
生态系统
地球科学
水文学(农业)
地质学
初级生产
土壤科学
生态学
土壤水分
生物
病理
复合材料
医学
岩土工程
材料科学
复合数
作者
Benjamin Poulter,Etienne Fluet‐Chouinard,Gustaf Hugelius,C. D. Koven,Lola Fatoyinbo,Susan Page,Judith A. Rosentreter,Lindsey S. Smart,Paul J. Taillie,Nathan Thomas,Zhen Zhang,Lahiru S. Wijedasa
出处
期刊:Geophysical monograph
日期:2021-10-15
卷期号:: 1-20
被引量:11
标识
DOI:10.1002/9781119639305.ch1
摘要
Wetlands have unique soil, vegetation, and biogeochemistry that arises from their landscape position and wetland hydrology, which creates low oxygen levels in the soil. With reduced oxygen availability, plants develop adaptations to survive, such as aerenchyma, that allow transport of atmospheric oxygen to their roots, and soil microbial communities become dominated by anaerobic respiration processes that are less efficient in oxidizing carbon. Combined, the above- and belowground carbon stocks of wetlands play a key role in the global carbon cycle at varying time scales. This chapter provides a comprehensive assessment of wetland carbon stocks, research methodologies, and their historical and future trajectories. We estimate wetland carbon stocks range between 520–710 PgC (and 1792 to 1882 PgC with permafrost carbon) globally.
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