2018
DOI: 10.1007/s11104-018-3573-1
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Biocontrolled soil nutrient distribution under the influence of an oxalogenic-oxalotrophic ecosystem

Abstract: Background and Aims The oxalate-carbonate pathway (OCP) has been observed in acidic tropical soils with low alkaline cation content where compartments are transient and fed by the rapid turnover of organic matter. By acting on edaphic parameters, the OCP may influence soil nutrient distribution. This study aims at assessing the influence of the OCP on soil nutrients within an agroforestry system associated to oxalogenic iroko trees. Methods Soil nutrient distribution was studied in a 30 m long and 1 m deep tra… Show more

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Cited by 11 publications
(3 citation statements)
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References 45 publications
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“…Among our strains, only eight were able to solubilize inorganic phosphate, suggesting a minor contribution of the OCP fungi to the P cycle. This is in line with in situ measurements of phosphorus content in an OCP system, where this content was mostly influenced by soil depth but not by the OCP [62].…”
Section: Discussionsupporting
confidence: 89%
See 1 more Smart Citation
“…Among our strains, only eight were able to solubilize inorganic phosphate, suggesting a minor contribution of the OCP fungi to the P cycle. This is in line with in situ measurements of phosphorus content in an OCP system, where this content was mostly influenced by soil depth but not by the OCP [62].…”
Section: Discussionsupporting
confidence: 89%
“…We reported here the first evidence of an active OCP in Madagascar. To date, the OCP has been observed in numerous tropical and semiarid environments, with different tree species, and across various geographical areas, such as Israel [ 60 ], the USA [ 61 ], Bolivia [ 30 ], India [ 23 ], Cameroon [ 62 ], the Ivory Coast [ 13 ], Haiti, and Mexico [ 63 ]. Here we identified T. indica as an oxalogenic tree driving an active OCP.…”
Section: Discussionmentioning
confidence: 99%
“…The microbial metabolism of oxalic acid exchanges a strong acid-oxalic acid (pK a 1 ¼ 1.25 and pK a 2 ¼ 4.27)-for a weak one-carbonic acid (pK a 1 ¼ 6.35 and pK a 2 ¼ 10.33)-which may lead to a strong local increase of pH. Such an influence on the soil pH prevents cation leaching from soil as a result of low pH (Pons et al, 2018) and can eventually promote the precipitation of calcium carbonate (CaCO 3 ) if pH increases above 8 (Aragno & Verrecchia, 2012;Verrecchia et al, 2006). In this latter process, for each mole of calcium oxalate oxidized, 1 mol of CO 2 is released in the atmosphere, while the other one is sequestered in soils as biomineralized CaCO 3 .…”
Section: Cell-to-cell Interactionsmentioning
confidence: 99%