4.1 Taxonomy of Microorganisms in Aquatic Environments 73
Biologicaly bound
Sulfur
SO 42 -
S^2 -
S^0
1
2
3
4 5
6
7
8
Assimilatory
section
Dissimilatory
section
Sulphuretum
(Organisms in the dissimilatory section
make up the sulphuretum)
Fig. 4.17 The biological sulfur cycle (After Luptakova 2007 ).
Key: 1 – Assimilatory sulfate reduction by plants, fungi and
bacteria; 2 – Death and decomposition by fungi and bacteria;
3 – Sulfide assimilation by bacteria and some plants; 4 – Excretion
of sulfate by animals; 5 – Dissimilatory sulfatereducing
bacteria; 6 – Dissimilatory sulfurreducing bacteria; 7 –
Phototrophic and chemotrophic sulfide-oxidizing bacteria; 8 –
Phototrophic and chemotrophic sulfuroxidizing bacteria
Fig. 4.16 General
circulation of sulfur on
Earth (Modified from
Yamanaka 2008 )
H 2 S
S^0
H 2 SO 4
FeS 2
Pyrite
Sulfur-oxidizing bacteria
Photosynthetic bacteria
Volcanoes,
factories
Algae, Cyanobacteria
in oceans
(CH 3 ) 2 S
Dimethyl sulphide
Hot springs,
Volcanoes
Acidophilic iron-
oxidizing bacteria
Sulfate-reducing SO 2
bacteria
Animals Plants
Absorption
Excreta Death Death
Bacteria
H 2 O
O 2
Assimilatio&excretionn Bacteria
sulfur is not converted into organic compounds. The
rotten egg odor of hydrogen sulfide in the environment
usually indicates the presence of sulfatereducing bac
teria in nature. Sulfatereducing bacteria are responsi
ble for the rotten egg odors of salt marshes, mud flats,
and intestinal gas. They slowly degrade materials that
are rich in cellulose in anaerobic environments. Apart
from soil, sulfate reducing bacteria are found in various
habitats such as seas and oceans, mud and sediments
of freshwaters (rivers, lakes), waters rich in decaying
organic material, thermal or nonthermal sulfur springs,
mining waters from sulfide deposits, waters from
deposits of mineral oil and natural gas, industrial waste
waters from metallurgical industry, as well as in the
gastrointestinal tract of man and animals (Barton and
Hamilton 2007 ).