Does pore scale biogeography exist in different soil types?
Résumé
Microbial activity is largely controlled by the abiotic conditions prevailing in their habitats, which are very
heterogeneous at the microscopic scale. A few studies have demonstrated a microbial biogeography at the
pore scale. Different regions in the soil pore network can be considered to be different microbial habitats and
these different regions have been shown to be well correlated with organic carbon mineralization rates. We
aimed to test whether such a functional biogeography exists for different soil types and whether it is consistent
across soils. We selected six topsoils with contrasted texture, soil organic matter content and pH (2 cambisols,
3 luvisols and 1 podzol under different managements). We added a 13C labelled, easily mineralisable organic
substrate, pyruvate, to soil samples previously equilibrated at different matric potentials, in order to place the
substrate preferentially in soil pores with neck diameters of 3 to 10 μm or 30 to 10μm, according to the Jurin-
Laplace law. The soil samples were then incubated at pF 1.5 for 3 weeks and CO2 and 13C-CO2 were
monitored. At the end of incubation, total and 13C-PLFA were extracted and analysed. Basal mineralisation,
expressed as % total organic C was affected by soil type, mainly related soil pH and the quality[NN1] of the
organic matter. The 6 soils exhibited contrasted microbial community composition, as shown by their PLFA
profiles. The addition of pyruvate did not induce any priming effect in soils, except in the long term bare fallow
soil, where the mineralization of SOM was presumably limited by energy. In the long term bare fallow soil,
pyruvate mineralization was the same whatever the region it was placed in, suggesting other controls of its
mineralization than the characteristics of pore scale habitats. In four soils out of six, the mineralization of
pyruvate was more rapid when it was initially placed in large pores (30 to 100μm) than in small pores (3 to 10
μm), suggesting that pore scale biogeography may be a general feature in soils and that coarser pores are more
favourable habitats for soil organic matter mineralization.
Domaines
Sciences du Vivant [q-bio]Origine | Fichiers produits par l'(les) auteur(s) |
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