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  Tree-mycorrhiza symbiosis accelerate mineral weathering: Evidences from nanometer-scale elemental fluxes at the hypha-mineral interface

Bonneville, S., Morgan, D. J., Schmalenberger, A., Bray, A., Brown, A., Banwart, S. A., Benning, L. G. (2011): Tree-mycorrhiza symbiosis accelerate mineral weathering: Evidences from nanometer-scale elemental fluxes at the hypha-mineral interface. - Geochimica et Cosmochimica Acta, 75, 22, 6988-7005.
https://doi.org/10.1016/j.gca.2011.08.041

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 Creators:
Bonneville, S.1, Author
Morgan, D. J.1, Author
Schmalenberger, A.1, Author
Bray, A.1, Author
Brown, A.1, Author
Banwart, S. A.1, Author
Benning, Liane G.2, Author                 
Affiliations:
1External Organizations, ou_persistent22              
20 Pre-GFZ, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum, ou_146023              

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Free keywords: pinus-sylvestris seedlings term carbon-cycle ectomycorrhizal fungi biotite dissolution paxillus-involutus atmospheric co2 in-situ soil ph plants Geochemistry & Geophysics
 Abstract: In soils, mycorrhiza (microscopic fungal hypha) living in symbiosis with plant roots are the biological interface by which plants obtain, from rocks and organic matter, the nutrients necessary for their growth and maintenance. Despite their central role in soils, the mechanism and kinetics of mineral alteration by mycorrhiza are poorly constrained quantitatively. Here, we report in situ quantification of weathering rates from a mineral substrate, (001) basal plane of biotite, by a surface-bound hypha of Paxillus involutus, grown in association with the root system of a Scots pine, Pinus sylvestris. Four thin-sections were extracted by focused ion beam (FIB) milling along a single hypha grown over the biotite surface. Depth-profile of Si, O, K, Mg, Fe and Al concentrations were performed at the hypha-biotite interface by scanning transmission electron microscopy-energy dispersive X-ray spectroscopy (STEM-EDX). Large removals of K (50-65%), Mg (55-75%), Fe (80-85%) and Al (75-85%) were observed in the topmost 40 nm of biotite underneath the hypha while Si and O are preserved throughout the depth-profile. A quantitative model of alteration at the hypha-scale was developed based on solid-state diffusion fluxes of elements into the hypha and the break-down/mineralogical re-arrangement of biotite. A strong acidification was also observed with hypha bound to the biotite surface reaching pH < 4.6. When consistently compared with the abiotic biotite dissolution, we conclude that the surface-bound mycorrhiza accelerate the biotite alteration kinetics between pH 3.5 and 5.8 to similar to 0.04 mu mol biotite m(-2) h(-1). Our current work reaffirms that fungal mineral alteration is a process that combines our previously documented bio-mechanical forcing with the mu m-scale acidification mediated by surface-bound hypha and a subsequent chemical element removal due to the fungal action. As such, our study presents a first kinetic framework for mycorrhizal alteration at the hypha-scale under close-to-natural experimental conditions. (C) 2011 Elsevier Ltd. All rights reserved.

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Language(s): eng - English
 Dates: 2011
 Publication Status: Finally published
 Pages: -
 Publishing info: -
 Table of Contents: -
 Rev. Type: -
 Identifiers: Other: WOS:000296579600016
DOI: 10.1016/j.gca.2011.08.041
ISSN: 0016-7037
URI: ://WOS:000296579600016
 Degree: -

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Title: Geochimica et Cosmochimica Acta
Source Genre: Journal, SCI, Scopus
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Pages: - Volume / Issue: 75 (22) Sequence Number: - Start / End Page: 6988 - 7005 Identifier: CoNE: https://gfzpublic.gfz.de/cone/journals/resource/journals161