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Microbial reduction of Fe(III) and turnover of acetate in Hawaiian soils

Title data

Küsel, Kirsten ; Wagner, Christine ; Trinkwalter, Tanja ; Gößner, Anita S. ; Drake, Harold L.:
Microbial reduction of Fe(III) and turnover of acetate in Hawaiian soils.
In: FEMS Microbiology Ecology. Vol. 40 (2002) Issue 1 . - pp. 73-81.
ISSN 1574-6941
DOI: https://doi.org/10.1111/j.1574-6941.2002.tb00938.x

Abstract in another language

Soils contain anoxic microzones, and acetate is an intermediate during the turnover of soil organic carbon. Due to negligible methanogenic activities in well-drained soils, acetate accumulates under experimentally imposed anoxic conditions. In contrast to forest, agricultural, and prairie soils, grassland soils from Hawaii consumed rather than formed acetate when incubated under anoxic conditions. Thus, alternative electron acceptors that might be linked to the anaerobic oxidation of soil organic carbon in Hawaiian soils were assessed. Under anoxic conditions, high amounts of Fe(II) were formed by Hawaiian soils as soon as soils were depleted of nitrate. Rates of Fe(II) formation for different soils ranged from 0.01 to 0.31 µmol (g dry wt soil)-1 h-1, but were not positively correlated to increasing amounts of non- or poorly crystallized iron oxides. In general, sulfate-reducing and methanogenic activities were negligible. Supplemental acetate was rapidly oxidized to CO2 via the sequential reduction of nitrate and Fe(III) in grassland soil [obtained near Kaena State Park]. Supplemental H2 stimulated the formation of Fe(II), but H2-utilizing acetogens appeared to also be involved in the consumption of H2. Approximately 270 µmol Fe(III) (g dry wt. soil)-1 was available for Fe(III)-reducing bacteria, and acetate became a stable end product when Fe(III) was depleted in long-term incubations. Most probable number estimates of H2- and acetate-utilizing Fe(III) reducers and of H2-utilizing acetogens were similar. These results indicate that (i) the microbial reduction of Fe(III) is an important electron-accepting process for the anaerobic oxidation of organic matter in Fe(III)-rich Hawaiian soils of volcanic origin, and (ii) acetate, formed by the combined activity of fermentative and acetogenic bacteria, is an important trophic link in anoxic microsites of these soils.

Further data

Item Type: Article in a journal
Refereed: Yes
Additional notes: BAYCEER9561
Institutions of the University: Research Institutions > Research Centres > Bayreuth Center of Ecology and Environmental Research- BayCEER
Faculties > Faculty of Biology, Chemistry and Earth Sciences > Department of Biology > Chair Ecological Microbiology
Faculties
Faculties > Faculty of Biology, Chemistry and Earth Sciences
Faculties > Faculty of Biology, Chemistry and Earth Sciences > Department of Biology
Research Institutions
Research Institutions > Research Centres
Result of work at the UBT: Yes
DDC Subjects: 500 Science
Date Deposited: 24 Sep 2015 09:38
Last Modified: 24 Sep 2015 09:38
URI: https://eref.uni-bayreuth.de/id/eprint/19607