Abstract

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.

Highlights

  • Wetlands are among the world’s most productive and valuable ecosystems [1]

  • In the essential to clarify the last effect of hydrological fluctuations in Mediterranean wetlands on context of global change, it is essential to clarify the last effect of hydrological fluctuations the release or retention of sedimentary phosphorus and on their role as a sink or a source in Mediterranean wetlands on the release or retention of sedimentary phosphorus and on of greenhouse gases

  • Even though Mediterranean water bodies are characterized by natural extreme water level fluctuations in response to irregular precipitation patterns [21], global climate change is projected to amplify this pattern by shortening precipitation seasons and increasing the frequency and intensity of summer droughts in this area [49]

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Summary

Introduction

Wetlands are among the world’s most productive and valuable ecosystems [1]. Despite covering only 1.5% of the Earth’s surface, wetlands provide 40% of ecosystem services worldwide, such as provisioning, regulating, habitat and cultural services [2]. First review focused on Mediterranean present study is theamong first review focused on Mediterranean whichchange are among lands, which are the most threatened ecosystems wetlands, due to climate and the natmost due to climate change natural habitat lossecosystems [19]. In the essential to clarify the last effect of hydrological fluctuations in Mediterranean wetlands on context of global change, it is essential to clarify the last effect of hydrological fluctuations the release or retention of sedimentary phosphorus and on their role as a sink or a source in Mediterranean wetlands on the release or retention of sedimentary phosphorus and on of greenhouse gases. Their role as a sink or a source of greenhouse gases

Sensitivity of Mediterranean Wetlands to Global Change Factors
The Sediment as an Essential Compartment of Mediterranean Wetlands
Impact of Sediment Desiccation and Re-Flooding on the Phosphorus Cycle
Consequence of Sediment Desiccation and Re-Flooding on Greenhouse
Findings
Concluding Remarks
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