Earth System Science Center (CCST), National Institute for Space Research (INPE), São Paulo, Brazil.
School of GeoSciences, University of Edinburgh, Edinburgh, UK.
Glob Chang Biol. 2021 Feb;27(3):489-505. doi: 10.1111/gcb.15408. Epub 2020 Dec 4.
Peatlands are carbon-rich ecosystems that cover 185-423 million hectares (Mha) of the earth's surface. The majority of the world's peatlands are in temperate and boreal zones, whereas tropical ones cover only a total area of 90-170 Mha. However, there are still considerable uncertainties in C stock estimates as well as a lack of information about depth, bulk density and carbon accumulation rates. The incomplete data are notable especially in tropical peatlands located in South America, which are estimated to have the largest area of peatlands in the tropical zone. This paper displays the current state of knowledge surrounding tropical peatlands and their biophysical characteristics, distribution and carbon stock, role in the global climate, the impacts of direct human disturbances on carbon accumulation rates and greenhouse gas (GHG) emissions. Based on the new peat extension and depth data, we estimate that tropical peatlands store 152-288 Gt C, or about half of the global peatland emitted carbon. We discuss the knowledge gaps in research on distribution, depth, C stock and fluxes in these ecosystems which play an important role in the global carbon cycle and risk releasing large quantities of GHGs into the atmosphere (CO and CH ) when subjected to anthropogenic interferences (e.g., drainage and deforestation). Recent studies show that although climate change has an impact on the carbon fluxes of these ecosystems, the direct anthropogenic disturbance may play a greater role. The future of these systems as carbon sinks will depend on advancing current scientific knowledge and incorporating local understanding to support policies geared toward managing and conserving peatlands in vulnerable regions, such as the Amazon where recent records show increased forest fires and deforestation.
泥炭地是富含碳的生态系统,覆盖了地球表面 1.85 亿至 4.23 亿公顷。世界上大多数泥炭地位于温带和北方地区,而热带泥炭地总面积仅为 9000 万至 1.70 亿公顷。然而,碳储量估计仍然存在相当大的不确定性,而且关于深度、体积密度和碳积累率的信息也很缺乏。特别是在南美洲,热带泥炭地的数据很不完整,据估计,那里拥有热带地区最大的泥炭地面积。本文展示了有关热带泥炭地及其生物物理特征、分布和碳储量、在全球气候中的作用、直接人为干扰对碳积累率和温室气体(GHG)排放的影响的现有知识状况。根据新的泥炭扩展和深度数据,我们估计热带泥炭地储存了 152 亿至 288 亿吨碳,约占全球泥炭地排放碳的一半。我们讨论了这些在全球碳循环中起着重要作用的生态系统在分布、深度、碳储量和通量方面的研究知识差距,并存在大量温室气体(CO 和 CH)释放到大气中的风险(例如排水和森林砍伐)。最近的研究表明,尽管气候变化对这些生态系统的碳通量有影响,但直接的人为干扰可能会起到更大的作用。这些系统作为碳汇的未来将取决于推进当前的科学知识,并结合当地的了解,以支持旨在管理和保护脆弱地区(如亚马逊地区)泥炭地的政策,最近的记录显示该地区森林火灾和森林砍伐有所增加。