Increase in CH4 emissions in Pantanal wetland lagoon due to extreme drought and sediment exposure

Published: 28 February 2025| Version 1 | DOI: 10.17632/br8kfpkpzn.1
Contributors:
,
, Ricardo Taniwaki

Description

The Pantanal is one of the largest and most unique wetlands on the planet, holding significant carbon stocks in its soils, freshwater and saline-alkaline ecosystems. Despite its importance, it faces threats from natural and man-induced fires, inadequate soil management, deforestation, and the impacts of climate change, such as severe drought-heat events, which may increase CH4 emissions. Given the importance of this ecosystem, we investigated methane (CH4) emissions from limnetic zone, sediments, and marginal soils in a drying lagoon in the Pantanal during a drought period unprecedented in over 75 years. The highest emissions occurred during the drying event, primarily when the water column decreased (7.05 mg CH₄ m⁻² day⁻¹) and along the margins (2.98 mg CH₄ m⁻² day⁻¹). This indicates that the lowering of the water column and exposed sediments became a significant source of CH₄ emissions. Our results suggest that these environments can become large CH₄ emitters during drying events, although current CH₄ emission models underestimate their contribution. With the expected increase in drying events in the Pantanal, it is likely that CH₄ emissions will rise in the coming years, exacerbating global warming and intensifying climate change.

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Institutions

Universidade de Sao Paulo, Universidade Federal do ABC, Universidade Federal de Sao Carlos

Categories

Aquatic Ecosystem, Wetlands, Tropical Ecosystem, Greenhouse Gas Emission

Funding

Fundação de Amparo à Pesquisa do Estado de São Paulo

2016/14227-5

Fundação de Amparo à Pesquisa do Estado de São Paulo

Process #2018/10290-0

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