%0 Journal Article
%9 ACL : Articles dans des revues avec comité de lecture répertoriées par l'AERES
%A Akerman, A.
%A Poitrasson, F.
%A Oliva, P.
%A Audry, S.
%A Prunier, J.
%A Braun, Jean-Jacques
%T The isotopic fingerprint of Fe cycling in an equatorial soil-plant-water system : The Nsimi watershed, South Cameroon
%D 2014
%L fdi:010063516
%G ENG
%J Chemical Geology
%@ 0009-2541
%K Iron isotopes ; Swamp zone soil ; Stream water ; Vegetation ; Chemical weathering ; Lateritic regolith
%K CAMEROUN
%M ISI:000345440900010
%P 104-116
%R 10.1016/j.chemgeo.2014.07.003
%U https://www.documentation.ird.fr/hor/fdi:010063516
%> https://horizon.documentation.ird.fr/exl-doc/pleins_textes/divers18-07/010062731.pdf
%V 385
%W Horizon (IRD)
%X Following an initial study of a tropical lateritic hillside system showing little iron isotope fractionation despite a strong accumulation within the soil profile, the present work investigates iron isotope signatures within the organic matter rich swamp system that represents 20% of the studied watershed surface (from Nsimi, South Cameroon). This study considers the soil-plant-water continuum in order to better understand the Fe elemental and isotopic transfer out of the ecosystem. Within the swamp system, the iron isotope compositions of gleysol samples (delta Fe-57(IRMM-14) similar to+ 0.6 parts per thousand) are significantly heavier than both the continental crust baseline and the reference lateritic soils from the hillslope (delta Fe-57(IRMM-14) = + 0.1 parts per thousand). This enrichment towards heavy isotopes is attributed to a preferential removal of light iron isotopes during soil forming processes. Pedogenic transformations (i.e., gleyzation, organic complexation of metal and leaching) are responsible for the reductimorphic features observed in ferralitic horizons (i.e., incomplete degradation of organic matter in surface and soil whitening favored by good draining conditions). The organic carbon-rich waters of the swamp system are prone to redox processes and strong metal chelation. The dissolved iron (i.e., fraction < 0.22 mu m) of the Mengong stream shows positive delta Fe-57 signatures, with a down-stream enrichment in heavy isotopes, from + 0.511 +/- 0.266 parts per thousand to + 1.076 +/- 0.240 parts per thousand. The binding of iron (Fe-III) with organic matter can explain the observed enrichment in heavy isotopes in the dissolved fraction. On the contrary, plant leaves are significantly enriched in light Fe (delta Fe-57 of -0.665 +/- 0.035 and -1.119 +/- 0.080 parts per thousand) relative to (i) the litter compartment (-0.166 +/- 0.078 to -0.262 +/- 0.013% for delta Fe-57) and (ii) the most superficial soils. Iron isotopic compositions in plants and litter vary as a function of both plant species and season. Hence, the differences in Fe isotopic compositions between the various studied compartments suggest that Fe isotopes can be used (i) to study elemental transfers during soil pedogenesis in tropical environment and (ii) to better appraise and constrain iron biogeochemical cycle between surface horizon of soils, surface waters and the vegetation.
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