BIOGEOCHEMICAL CYCLES

SOIL MICROBIOLOGY

BIOL/CSES 4684



THE SULFUR CYCLE




Compound Chemical Form Valence
Sulfide H2S -2
Sulfur S 0
Hyposulfite S2O4 -2
Sulfite SO3 -2
Thiosulfite S2O3 -2
Dithionate S2O6 -2
Trithionate S3O6 -2
Tetrathionate S4O6 -2
Petathionate S5O6 -2
Sulfate SO4 -2

The Sulfur Cycle: Steps in the Cycle

The above table lists the forms of sulfur that can occur in soil. Notice that the net valence of each chemical form is minus 2, except for elemental sulfur which has a valence of zero. Sulfate, sulfide, and sulfur are the major and most important forms, all others are minor.



Mineralization of Organic Sulfur

Most organic sulfur in living tissue is in S-containing amino acids and sulfate esters. As an example, consider the degradation of cysteine:

R-HS-CH2-CHNH2-CO2H (cysteine) -------> NH3 + R-HS-CH2-CO-CO2H (Beta-mercaptopyruvic acid)------> H2S + CH3-CO-C2H (pyruvic acid) ------> utilized in a number of ways for metabolism

The H2S and NH3 are released into the atmosphere, contributing to the characteristc smell associated with putrefaction. In soil, 90% of the sulfur present is organic: 50% is C-O-S linkages (sulfate esters), 20% is S-amino acids, and 20% as a wide range of different sulfur compounds.



Sulfur Immobilization

Also called Assimilatory Sulfate Reduction
In general, sulfate is converted to a protein containing sulfur by:
SO42 + PAP(phosphoadenosine-5-phosphate)------> PAPS(phosphoadenosine-5-phosphosulfate------->PAPS + reduction------>PAPS-reductase------> Sulfite---->Thiosulphate---->Sulfide---->a series of biochemical steps---->methionine----> sulfur containing protein.

Sulfate must be 'activated' initially by PAP before the reaction can proceed. Assimilatory sulfate reduction occurs anaerobically as well as aerobically, and can be performed by microbes, plants, and animals.


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Materials on the this webpage were created by Katie Corbin.