Elevated carbon dioxide and irrigation effects on water stable aggregates in a Sorghum field: a possible role for arbuscular mycorrhizal fungi

Citation
Mc. Rillig et al., Elevated carbon dioxide and irrigation effects on water stable aggregates in a Sorghum field: a possible role for arbuscular mycorrhizal fungi, GL CHANGE B, 7(3), 2001, pp. 333-337
Citations number
27
Categorie Soggetti
Environment/Ecology
Journal title
GLOBAL CHANGE BIOLOGY
ISSN journal
13541013 → ACNP
Volume
7
Issue
3
Year of publication
2001
Pages
333 - 337
Database
ISI
SICI code
1354-1013(200103)7:3<333:ECDAIE>2.0.ZU;2-S
Abstract
While soil biota and processes are becoming increasingly appreciated as imp ortant parameters for consideration in global change studies, the fundament al characteristic of soil structure is a neglected area of research. In a s orghum [Sorghum bicolor (L.) Moench] field experiment in which CO2 [supplie d using free-air CO2 enrichment (FACE) technology] was crossed factorially with an irrigation treatment, soil aggregate (1-2 mm) water stability incre ased in response to elevated CO2. Aggregate water stability was increased b y 40% and 20% in response to CO2, at ample and limited water supply treatme nts, respectively. Soil hyphal lengths of arbuscular mycorrhizal fungi (AMF ) increased strongly (with a threefold increase in the dry treatment) in re sponse to CO2, and the concentrations of one fraction (easily extractable g lomalin, EEG) of the AMF-produced protein glomalin were also increased. Two fractions of glomalin, and AMF hyphal lengths were all positively correlat ed with soil aggregate water stability. The present results further support the hypothesis that AMF can become important in global change scenarios. A lthough in this field study a causal relationship between hyphal length, gl omalin and aggregate stability cannot be demonstrated, the present data do suggest that AMF could mediate changes in soil structure under elevated CO2 . This could be of great importance in agricultural systems threatened by e rosional soil loss.