Transcript Document
University of Essex
BIODEEP-WP5
Understanding of ecological relations between
the
microbial
communities
and
the
functioning of DHAB environments
Andrea Sass , Terry McGenity, Boyd McKew
Proteobacteria:
mostly from interfaces
some sulfur-oxidizing bacteria
many related to bacteria found in deep-sea environments
all grow on sea water medium, some extremely halotolerant
isolates are marine bacteria derived from the oxic
water column
some isolates could benefit from the conditions in
the interface (particularly sulfur-oxidizing bacteria)
Future: investigation of an extremely halotolerant,
aerobic, aerotactic strainn from Urania basin interface
Bacillus related isolates:
almost all derived from sediments
no correlation between phylogeny and basin of origin
vast majority of tested strains only halotolerant
(some very halotolerant and also facultatively anaerobic)
probably derived from dormant spores
six strains obligately halophilic (no growth
below 3.5% salt, optimum at 5-10% salt)
two strains isolated anaerobically in highly
saline medium
Strain AS4
0.5
Series1
3%
O.D.
0.4
Series2
5%
0.3
10%
Series3
0.2
15%
Series4
0.1
20%
Series5
0
0
5
10
15
20
25
30
Time (h)
0.6
0.5
O.D.
0.4
Series1
20%
25 %
Series2
0.3
30%
Series3
0.2
0.1
0
0
100
200
Time (h)
300
400
Strain US13
0.5
Series1
5%
Series2
10%
0.4
O.D.
Series3
15%
0.3
20%
Series4
22%
Series5
0.2
25%
Series6
0.1
27%
Series7
30%
Series8
0
0
100
200
300
400
Time (h)
0.4
Series1
5%
0.3
Series2
10%
O.D.
15%
Series3
20%
Series4
0.2
22%
Series5
25%
Series6
27%
Series7
0.1
30%
Series8
0
0
10
20
Time (h)
30
other characteristics:
anaerobic growth, also at high salt concentrations
favours moderate temperatures and pH
substrates used: amino acids, betaine, organic acids,
yeast extract
possibly active in situ
Future: characterization of Halobacillus-related
strains growing anaerobically at 20% salt
Physiological properties of anerobic isolates
Halanaerobiaceae :
all except one (from DS) extremely halophilic
distinct species from each basin, some isolated repeatedly
strains derived from BI similar to isolate from another DHAB (Red Sea)
CFB: moderately halophilic
Clostridia: moderately halophilic
Methanogens: extremely halophilic
e-Proteobacterium: moderately halophilic, reduces sulfur compounds and nitrate
Halorhabdus sp.: facultative anaerobe, extremely halophilic
Active in situ?
Methanogens, Haloanaerobiaceae and
Halobacterium possibly active in situ in the
brines
e-Proteobacterium and CFB could thrive in
the interface
Clostridia probably derived from dormant
spores
Sequences similar to three cultivates strains
were also found in clone libraries made from the basins
Archaea:
AN-AI3 (Halorhabdus utahensis 99%):
!
99% identity to clone DLIA-31
AN-AS7 (Methanohalophilus mahii 99%):
!
99% identity to clones ULIA-84, DLIA-189,
ALIA-123, ABBA-51
Eubacteria:
AN-BI4 (CFB):
! 98% identity to clone BBBB-69
(tRFLP-fragments with lengths analogous to fragments
derived from AN-BI4 occur in samples from interfaces and
brines)
l‘Atalante sediment:
extremely halophilic fermenting organisms
isolated from top layers
Bannock sediment:
only organisms probably not active in situ isolated
t-RFLP profile like that from brine
no anaerobic isolates from brines
l‘Atalante basin upper sediments contain bacterial
population different from brine
some organisms possibly active in the brines/interfaces
could be cultivated
vast majority of organisms inhabiting the DHAB
remain uncultivated
cultivation-independent approaches needed
for understanding the function of DHAB
environments