Biogeochemistry of Mediterranean Wetlands: A Review about the Effects of Water-Level Fluctuations on Phosphorus Cycling and Greenhouse Gas Emissions
Metadatos
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MDPI
Materia
Biogeochemistry Phosphorus Gases emissions Sediment Water level fluctuations Mediterranean wetlands
Fecha
2021-05-27Referencia bibliográfica
de Vicente, I. Biogeochemistry of Mediterranean Wetlands: A Review about the Effects of Water-Level Fluctuations on Phosphorus Cycling and Greenhouse Gas Emissions. Water 2021, 13, 1510. [https://doi.org/10.3390/w13111510]
Resumen
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.