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THE MICROBE-MINERAL INTERACTIONS IN THE ACIDIC PODZOL SOIL
Stockholms universitet, Naturvetenskapliga fakulteten, Institutionen för geologiska vetenskaper.
Stockholms universitet, Naturvetenskapliga fakulteten, Institutionen för geologiska vetenskaper.
2013 (Engelska)Ingår i: Mineralogical magazine, ISSN 0026-461X, E-ISSN 1471-8022, Vol. 77, nr 5, s. 564-Artikel i tidskrift, Meeting abstract (Övrig (populärvetenskap, debatt, mm)) Published
Abstract [en]

Iron is a key component of the chemical architecture of the biosphere. Due to the low bioavailability of iron in the environment, microorganisms have developed specific uptake strategies, like siderophores, which are operationally defined as low-molecular-mass biogenic Fe(III)-binding compounds, that can increase iron’s bioavailability by promoting the dissolution of iron-bearing minerals. In the present study, we aimed to investigate the composition of hydroxamate siderophores in the soil horizons of the acidic podzol, and study how they are affected by the presence of specific mineral types and microbial communities.

 Three different minerals (apatite, biotite and oligioclase) were inserted in the soil horizons (O (organic), E (eluvial), B (upper illuvial), and C (mineral)). After two years, soil samples were collected from both the bulk soil (next to the minerals) and from the soil attached to the mineral surfaces. The concentration of ten different fungal tri-hydroxamates and five bacterial ones were determined by high-performance liquid chromatography coupled to electrospray ionization mass spectrometry (HPLC-ESI-MS). In addition, total microbial composition and diversity were studied.

Our field experiment succeeded in describing the relationship between the presence of siderophores, soil horizon and mineral type, in addition to understanding the interaction between mineral type and soil microbial composition. A wide range of fungal and bacterial hydroxamates were detected throughout the soil profile. On the other hand, the presence of the minerals completely altered the diversity of siderophores. In addition, each mineral had a unique interaction with hydroxamates in the different soil horizons. There were also a good relationship between the microbial diversity and the siderophore distribution. 

Ort, förlag, år, upplaga, sidor
2013. Vol. 77, nr 5, s. 564-
Nyckelord [en]
Podzol soil, Siderophores, Weathering
Nationell ämneskategori
Mikrobiologi Geokemi
Forskningsämne
biogeokemi
Identifikatorer
URN: urn:nbn:se:su:diva-97150OAI: oai:DiVA.org:su-97150DiVA, id: diva2:675896
Konferens
Goldschmidt Conference
Tillgänglig från: 2013-12-04 Skapad: 2013-12-04 Senast uppdaterad: 2017-12-06Bibliografiskt granskad

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Ahmed, EngyHolmström, Sara
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