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Precipitation pulses enhance respiration of Mediterranean ecosystems: the balance between organic and inorganic components of increased soil CO 2 efflux
Author(s) -
INGLIMA I.,
ALBERTI G.,
BERTOLINI T.,
VACCARI F. P.,
GIOLI B.,
MIGLIETTA F.,
COTRUFO M. F.,
PERESSOTTI A.
Publication year - 2009
Publication title -
global change biology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 4.146
H-Index - 255
eISSN - 1365-2486
pISSN - 1354-1013
DOI - 10.1111/j.1365-2486.2008.01793.x
Subject(s) - environmental science , soil respiration , ecosystem , mediterranean climate , shrubland , eddy covariance , soil water , environmental chemistry , autotroph , soil carbon , ecology , soil science , chemistry , biology , genetics , bacteria
In regions characterized by arid seasons, such as the Mediterranean basin, soil moisture is a major driver of ecosystem CO 2 efflux during periods of drought stress. Here, a rain event can induce a disproportional respiratory pulse, releasing an amount of CO 2 to the atmosphere that may significantly contribute to the annual ecosystem carbon balance. The mechanisms behind this pulse are unclear, and it is still unknown whether it is due to the stimulation of autotrophic, heterotrophic and/or inorganic CO 2 fluxes. On the Mediterranean island of Pianosa, eddy flux measurements showed respiratory pulses after rain events following prolonged drought periods, which occurred in the summer of 2003 and 2006. To investigate the mechanisms of this observed enhanced respiration fluxes and partition of the soil CO 2 sources, two water manipulation experiments were performed. The first was designed to estimate the effect of soil rewetting on soil CO 2 efflux, in the different ecosystem types existing on the island (i.e. woodland, ex‐agricultural and Mediterranean shrubland). The second was a soil CO 2 partitioning experiment to investigate the relative contribution of inorganic and organic CO 2 sources to soil respiration, under dry and wet soil conditions. Our results suggest that the pulse in the CO 2 efflux is primarily due to the enhancement of heterotrophic respiration, likely caused by the degradation of easily decomposable substrates, accumulated in soils during the dry period. In fact, the vegetation at the site was senescent and did not play any significant role in CO 2 exchange, as suggested by the absence of diurnal CO 2 uptake in eddy covariance measurements. In addition, soil rewetting did not significantly enhance inorganic CO 2 efflux.