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Biogeochemistry of Mediterranean Wetlands: A Review about the Effects of Water-Level Fluctuations on Phosphorus Cycling and Greenhouse Gas Emissions

Journal

WATER
Volume 13, Issue 11, Pages -

Publisher

MDPI
DOI: 10.3390/w13111510

Keywords

biogeochemistry; phosphorus; greenhouse gases emissions; sediment; water level fluctuations; Mediterranean wetlands

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Mediterranean wetlands are expected to experience amplified water level fluctuations due to global climate change, which will impact phosphorus dynamics and greenhouse gas emissions. While desiccation may increase CO2 emissions and inundation decrease cumulative CO2 emissions and N2O emissions while increasing CH4 emissions, there is still a lack of knowledge on the net effect of water level fluctuations on greenhouse gas emissions. Further research is needed to assess the role of these ecosystems as a source of greenhouse gases and as a feedback mechanism for global warming.
Although Mediterranean wetlands are characterized by extreme natural water level fluctuations in response to irregular precipitation patterns, global climate change is expected to amplify this pattern by shortening precipitation seasons and increasing the incidence of summer droughts in this area. As a consequence, a part of the lake sediment will be exposed to air-drying in dry years when the water table becomes low. This periodic sediment exposure to dry/wet cycles will likely affect biogeochemical processes. Unexpectedly, to date, few studies are focused on assessing the effects of water level fluctuations on the biogeochemistry of these ecosystems. In this review, we investigate the potential impacts of water level fluctuations on phosphorus dynamics and on greenhouse gases emissions in Mediterranean wetlands. Major drivers of global change, and specially water level fluctuations, will lead to the degradation of water quality in Mediterranean wetlands by increasing the availability of phosphorus concentration in the water column upon rewetting of dry sediment. CO2 fluxes are likely to be enhanced during desiccation, while inundation is likely to decrease cumulative CO2 emissions, as well as N2O emissions, although increasing CH4 emissions. However, there exists a complete gap of knowledge about the net effect of water level fluctuations induced by global change on greenhouse gases emission. Accordingly, further research is needed to assess whether the periodic exposure to dry-wet cycles, considering the extent and frequency of the cycles, will amplify the role of these especial ecosystems as a source of these gases and thereby act as a feedback mechanism for global warming. To conclude, it is pertinent to consider that a better understanding about the effect of water level fluctuations on the biogeochemistry of Mediterranean wetlands will help to predict how other freshwater ecosystems will respond.

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