Iron reduction and gley formation by nitrogen-fixing clostridia.

Abstract:

:Studies on iron reduction and the mechanism of gley formation by nitrogen-fixing clostridia are reported. Up to 106 cells/g soil of anaerobic, nitrogen-fixing clostridia, capable of reducing iron (III)-oxide, were counted in samples taken from various top soils. In a gleyed subsoil as many as 105 bacteria per g soil, capable of reducing and fixing nitrogen, were enumerated using the most probable number technique. In general, the ratio of the auxotrophic iron reducing clostridia (glucose+yeast extract fermenters) to the prototrophic iron reducing flora (glucose fermenters) was found much larger in the top soil samples than in those derived from various gleyed subsoils.An enrichment method for the isolation of nitrogen-fixing, iron reducing clostridia of the butyric-butyl type is described. The iron reducing capacity of this type of clostridia as well as of Clostridium pasteurianum was determined quantitatively. Generally, the presence of soil or soil extract enhanced the amount of dissolved ferrous iron, both with butyric acid fermenters and with Cl. pasteurianum.When enriched iron reducing clostridia were incubated anaerobically under N2-atmosphere in a sterile, red-colored, lateritic type of soil with glucose, intense gleying occurred within a few days. Microscopic observations indicated the presence of sporeforming bacteria of the Clostridium butyricum type or related species.The biological and chemical mechanism of gley formation is discussed.

journal_name

Oecologia

journal_title

Oecologia

authors

Ottow JC

doi

10.1007/BF00345718

subject

Has Abstract

pub_date

1971-01-01 00:00:00

pages

164-175

issue

2

eissn

0029-8549

issn

1432-1939

pii

10.1007/BF00345718

journal_volume

6

pub_type

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