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Phenotypic structure of Pseudomonas populations is altered under elevated pCO"2 in the rhizosphere of perennial grasses [An article from: Soil Biology and Biochemistry]

Author S. Tarnawski, J. Hamelin, M. Jossi, M. Aragno, Fro
Publisher Elsevier
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Book Details
PublisherElsevier
ISBN / ASINB000RR8HGU
ISBN-13978B000RR8HG8
AvailabilityAvailable for download now
Sales Rank99,999,999
MarketplaceUnited States 🇺🇸

Description

This digital document is a journal article from Soil Biology and Biochemistry, published by Elsevier in 2006. The article is delivered in HTML format and is available in your Amazon.com Media Library immediately after purchase. You can view it with any web browser.

Description:
The increasing atmospheric CO"2 content (pCO"2) is likely to modify the ecosystem functioning including rhizosphere bacteria that are directly dependent on rhizodeposition. This may include alteration of Pseudomonas populations that display phenotypic traits in relation with plant fitness. In the present study, 1228 Pseudomonas strains were isolated from the non-rhizosphere soil, rhizosphere soil and root fractions of perennial grassland systems: Lolium perenne and Molinia coerulea. Both plants were grown under ambient (36Pa) and elevated (60Pa) pCO"2 in the Swiss Free Air CO"2 Enrichment (FACE) system. Pseudomonas spp. were tested for their ability to produce auxin, siderophores and hydrogen cyanide, and to dissimilate nitrate. No effect of root proximity and elevated pCO"2 was observed on the proportions of auxin producers. For L. perenne and M. coerulea, siderophore and hydrogen cyanide Pseudomonas producers were stimulated in the root fraction. In contrast lower frequencies of nitrate reducers were observed in the root fraction compared to non-rhizosphere soil. The frequencies of siderophore producers and nitrate dissimilating strains were higher, and those of hydrogen cyanide producers lower, under elevated pCO"2 for L. perenne. This alteration of the phenotypic structure of Pseudomonas guild in the root fraction is discussed in relation with the physico-biochemical modifications of the rhizosphere condition via rhizodeposition and environmental changes occurring under elevated pCO"2.