In that respect, besides defining the CO2 assimilation capacity of the studied thicket area, Serranos thesis has proved how rain distribution conditions the functional nature of the studied ecosystem and how the duration of the drought period and, therefore, the water content, determinates the duration of the CO2 geochemical emissions, through soil ventilation.
It proves that CO2 production is not only related to vegetation, but also to geochemical emissions which increase in dry seasons.
The hypothesis formulated in this work -says Serrano- is that the emissions are a consequence of a ventilation phenomenon of the carbonated systems macro-pores, which appear to be connected with wind speed. In this line, certain studies on degasification phenomenon in caves and turbulent CO2 interchanges with the atmosphere, carried out by Sergio Snchez Moral and Soledad Cuezva Robleo (Spanish Museum of Natural Sciences, CSIC) in the Altamira Cave, endorse the theory of the existence of CO2 geochemical flows in ecosystems situated in karst substrate.
Politics and ecology
CO2 is one of the main greenhouse gases which contributes to the rise of earths temperature. Serrano Ortizs study is the first one focused on carbonated semiarid ecosystems and has proved that they act as CO2 drains, due to the action of the thickets, and as CO2 geochemical generators in dry periods (especially worrying if we reach the temperature rise predicted by climatic change models).
His work provides data of C (carbon) flows in key ecosystems for biodiversity conservation, as well as for the
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| Contact: Penlope Serrano Ortiz penelope@ugr.es 34-958-242-928 Universidad de Granada Source:Eurekalert |