Faculty of Engineering, construction and Habitat, Universidad Veracruzana Bv. Adolfo Ruíz Cortines 455, Costa Verde, Boca del Rio C.P., Veracruz 94294, Mexico.
Division of Research, Postgraduate Studies and Innovation, Tecnológico Nacional de México/Instituto Tecnológico Superior de Misantla, Veracruz C.P., Misantla 93821, Mexico.
Int J Environ Res Public Health. 2020 Oct 9;17(20):7372. doi: 10.3390/ijerph17207372.
Wetland soils are important stores of soil carbon (C) in the biosphere, and play an important role in global carbon cycles in the response strategy to climate change. However, there areknowledge gaps in our understanding of the quantity and distribution in tropical regions. Specifically, Mexican wetlands have not been considered in global carbon budgets or carbon balances for a number of reasons, such as: (1) the lack of data, (2) Spanish publications have not been selected, or (3) because such balances are mainly made in the English language. This study analyzes the literature regarding carbon stocks, sequestration and fluxes in Mexican forested wetlands (Forest-W). Soil carbon stocks of 8, 24.5 and 40.1 kg cm were detected for flooded palms, mangroves, and freshwater or swamps (FW) wetland soils, respectively, indicating that FW soils are the Forest-W with more potential for carbon sinks ( = 0.023), compared to mangroves and flooded palm soils. While these assessments of carbon sequestration were ranged from 36 to 920 g-C m year, C emitted as methane was also tabulated (0.6-196 g-C m year). Subtracting the C emitted of the C sequestered, 318.2 g-C m year were obtained. Such data revealed that Forest-W function is mainly as carbon sink, and not C source. This review can help to inform practitioners in future decisions regarding sustainable projects, restoration, conservation or creation of wetlands. Finally, it is concluded that Forest-W could be key ecosystems in strategies addressing the mitigation of climate change through carbon storage. However, new studies in this research line and public policies that protect these essential carbon sinks are necessary in order to, hopefully, elaborate global models to make more accurate predictions about future climate.
湿地土壤是生物圈中土壤碳(C)的重要储存库,在应对气候变化的全球碳循环中发挥着重要作用。然而,我们对热带地区土壤碳的数量和分布了解还存在知识空白。具体来说,由于以下原因,墨西哥湿地在全球碳预算或碳平衡中并未被考虑在内:(1)缺乏数据;(2)西班牙出版物未被选中;(3)因为此类平衡主要用英语进行。本研究分析了有关墨西哥森林湿地(Forest-W)土壤碳储量、固存和通量的文献。受水淹的棕榈、红树林和淡水或沼泽(FW)湿地土壤的碳储量分别为 8、24.5 和 40.1 kg cm,这表明 FW 土壤是 Forest-W 中具有更大碳汇潜力的湿地( = 0.023),与红树林和受水淹的棕榈土壤相比。虽然这些碳固存评估范围从 36 到 920 g-C m year,但也列出了作为甲烷排放的碳(0.6-196 g-C m year)。扣除固存的碳排放量,得到 318.2 g-C m year。这些数据表明,Forest-W 的功能主要是作为碳汇,而不是碳源。本综述可以帮助未来在可持续项目、恢复、保护或湿地创建方面做出决策的从业者了解情况。最后得出结论,森林湿地可以成为通过碳储存来缓解气候变化的关键生态系统。然而,为了制定更准确的未来气候预测全球模型,需要在该研究领域开展新的研究,并制定保护这些重要碳汇的公共政策。