Phylogenetic and Physiological Diversity of Sulphate-Reducing Bacteria Isolated from a Salt Marsh...

12
System. Appl. Microbiol. 21, 557-568 (1998) SYSTEI\t1ATIC AND _©_G_us_ta_v F_is_ch_er_V_erl_a g ________________ APPLIED MICROBIOLOGY Phylogenetic and Physiological Diversity of Sulphate-Reducing Bacteria Isolated from a Salt Marsh Sediment JULIETIE N. ROONEy-VARGA *, BARBARA R. SHARAK GENTHNER!, RICHARD DEVEREUX 2 , STEPHANIE G. WULIS 2 , STEPHANIE D. FRIEDMAN 2 , and MARK E. HINES!,3 lInstitute for the Study of Earth, Oceans, and Space, University of New Hampshire, Durham 2Gulf Ecology Division, U.S. Environmental Protection Agency, National Health and Environmental Effects Research Laboratory, Gulf Breeze 3Present address: Department of Biology Sciences, University of Alaska Anchorage, Anchorage Received September 1, 1998 Summary The phylogenetic and physiological diversity of sulphate-reducing bacteria inhabiting a salt marsh rhizo- sphere were investigated. Sulphate-reducing bacteria were isolated from a salt marsh rhizosphere using enrichment cultures with electron donors thought to be prevalent in the rhizosphere of Spartina alterni flora. The relationship between phylogeny and nutritional characteristics of 10 strains was investigated. None of the isolates had 16S rRNA sequences identical to other delta subclass sulphate-reducers, shar- ing 85.3 to 98.1 % sequence similarity with 16S rRNA sequences of their respective closest relatives. Phylogenetic analysis placed two isolates, obtained with ethanol as an electron donor, within the Desul fovibrionaceae. Seven isolates, obtained with acetate, butyrate, propionate, or benzoate, were placed within the Desulfobacteriaceae. One isolate, obtained with butyrate, fell within the Desulfobulbus as- semblage, which is currently considered part of the Desulfobacteriaceae family. However, due to the phylogenetic breadth and physiological traits of this group, we propose that it be considered a new fami- ly, the "Desulfobulbusaceae." The isolates utilised an array of electron donors similar to their closest rel- atives with a few exceptions. As a whole, the phylogenetic and physiological data indicate isolation of several sulphate-reducing bacteria which might be considered as new species and representative of new genera. Comparison of the Desulfobacteriaceae isolates' 16S rRNA sequences to environmental clones originating from the same study site revealed that none shared more than 86% sequence similarity. The results provide further insight into the diversity of sulphate-reducing bacteria inhabiting the salt marsh ecosystem, as well as supporting general trends in the phylogenetic coherence of physiological traits of delta Proteobacteria sulphate reducers. Key words: sulphate-reducing bacteria - SRB - 16S rRNA phylogeny - salt-marsh - rhizosphere - Desulfobacteriaceae - Desulfovibrionaceae Introduction Until the 1970's, the dissimilatory sulphate-reducing bacteria (SRB) were thought to be comprised of a few species in two genera that were capable of utilising only lactate or pyruvate as energy sources (BARTON and TOMEI, 1995). However, SRB are now known to be both physio- logically and phylogenetic ally diverse. Close to 100 elec- tron donors for sulphate reduction have been described 'f Present address of corresponding author: Department of Bio- logical Sciences, University of Massachusetts Lowell, 1 Univer- sity Ave., Lowell, MA 01854, U.S.A. Telephone: (978) 934-4715; Fax: (978) 934-3044; e-mail: [email protected]. (HANSEN, 1993) and the capacity for dissimilatory sul- phate reduction has been demonstrated in bacteria from three major eubacterial lines of descent and one genus within the Archaea domain (STACKEBRANDT et aI., 1995). To date, the majority of characterised SRB are members of the Gram-negative non-sporeforming mesophilic SRB within the delta subclass of the Proteobacteria, and it ap- pears that this group is the most widely distributed in na- ture (WIDDEL and BAK, 1992). In addition, the delta sub- class SRB have been extensively studied using comparative 16S rRNA sequence analysis and were found to form phy- logenetic groups that are consistent with various physio- logical traits, particularly in the utilisation of electron

Transcript of Phylogenetic and Physiological Diversity of Sulphate-Reducing Bacteria Isolated from a Salt Marsh...

System. Appl. Microbiol. 21, 557-568 (1998) SYSTEI\t1ATIC AND _©_G_us_ta_v F_is_ch_er_V_erl_ag ________________ APPLIED MICROBIOLOGY

Phylogenetic and Physiological Diversity of Sulphate-Reducing Bacteria Isolated from a Salt Marsh Sediment

JULIETIE N. ROONEy-VARGA *, BARBARA R. SHARAK GENTHNER!, RICHARD DEVEREUX2, STEPHANIE G. WULIS2,

STEPHANIE D. FRIEDMAN2, and MARK E. HINES!,3

lInstitute for the Study of Earth, Oceans, and Space, University of New Hampshire, Durham 2Gulf Ecology Division, U.S. Environmental Protection Agency, National Health and Environmental Effects Research Laboratory, Gulf Breeze

3Present address: Department of Biology Sciences, University of Alaska Anchorage, Anchorage

Received September 1, 1998

Summary

The phylogenetic and physiological diversity of sulphate-reducing bacteria inhabiting a salt marsh rhizo­sphere were investigated. Sulphate-reducing bacteria were isolated from a salt marsh rhizosphere using enrichment cultures with electron donors thought to be prevalent in the rhizosphere of Spartina alterni­flora. The relationship between phylogeny and nutritional characteristics of 10 strains was investigated. None of the isolates had 16S rRNA sequences identical to other delta subclass sulphate-reducers, shar­ing 85.3 to 98.1 % sequence similarity with 16S rRNA sequences of their respective closest relatives. Phylogenetic analysis placed two isolates, obtained with ethanol as an electron donor, within the Desul­fovibrionaceae. Seven isolates, obtained with acetate, butyrate, propionate, or benzoate, were placed within the Desulfobacteriaceae. One isolate, obtained with butyrate, fell within the Desulfobulbus as­semblage, which is currently considered part of the Desulfobacteriaceae family. However, due to the phylogenetic breadth and physiological traits of this group, we propose that it be considered a new fami­ly, the "Desulfobulbusaceae." The isolates utilised an array of electron donors similar to their closest rel­atives with a few exceptions. As a whole, the phylogenetic and physiological data indicate isolation of several sulphate-reducing bacteria which might be considered as new species and representative of new genera. Comparison of the Desulfobacteriaceae isolates' 16S rRNA sequences to environmental clones originating from the same study site revealed that none shared more than 86% sequence similarity. The results provide further insight into the diversity of sulphate-reducing bacteria inhabiting the salt marsh ecosystem, as well as supporting general trends in the phylogenetic coherence of physiological traits of delta Proteobacteria sulphate reducers.

Key words: sulphate-reducing bacteria - SRB - 16S rRNA phylogeny - salt-marsh - rhizosphere -Desulfobacteriaceae - Desulfovibrionaceae

Introduction

Until the 1970's, the dissimilatory sulphate-reducing bacteria (SRB) were thought to be comprised of a few species in two genera that were capable of utilising only lactate or pyruvate as energy sources (BARTON and TOMEI, 1995). However, SRB are now known to be both physio­logically and phylogenetic ally diverse. Close to 100 elec­tron donors for sulphate reduction have been described

'f Present address of corresponding author: Department of Bio­logical Sciences, University of Massachusetts Lowell, 1 Univer­sity Ave., Lowell, MA 01854, U.S.A. Telephone: (978) 934-4715; Fax: (978) 934-3044; e-mail: [email protected].

(HANSEN, 1993) and the capacity for dissimilatory sul­phate reduction has been demonstrated in bacteria from three major eubacterial lines of descent and one genus within the Archaea domain (STACKEBRANDT et aI., 1995). To date, the majority of characterised SRB are members of the Gram-negative non-sporeforming mesophilic SRB within the delta subclass of the Proteobacteria, and it ap­pears that this group is the most widely distributed in na­ture (WIDDEL and BAK, 1992). In addition, the delta sub­class SRB have been extensively studied using comparative 16S rRNA sequence analysis and were found to form phy­logenetic groups that are consistent with various physio­logical traits, particularly in the utilisation of electron

558 ]. N. ROONEy-VARGA et al.

donors. Due to this correlation, 165 rRNA-based analyses provide potentially powerful tools for inferring physiolog­ical traits of both cultivated and uncultivated SRB.

5RB are ubiquitous and are known to play ecological­ly important roles in such diverse habitats as freshwater ponds, oil production facilities, animal intestines, rice paddies, and estuarine and marine sediments (GIBSON, 1990; SMITH, 1993; WIDDEL and BAK, 1992). In particu­lar, SRB have been found to exhibit high sulphate-reduc­ing activity and to play an extremely important role in organic carbon remineralisation, below-ground geo­chemistry, and plant-microbe interactions in salt marsh environments (HINES et a!., 1989; HOWARTH, 1993). As the dominant terminal electron accepting process, it has been estimated that sulphate reduction accounts for up to 50% of organic carbon remineralisation in these eco­systems (HOWARTH and Hobbie, 1982).

Sulphate reduction rates in organic-rich salt marsh sediments are among the highest of any natural system (HOWARTH, 1993). Since plant root exudates and decom­posing plant litter may provide a complex mixture of electron donors in salt marsh sediments, it is likely that diverse populations of 5RB exist therein. As discussed by ROONEy-VARGA et a!. (1997) and HINES et a!. (submitted), the application of 165 rRNA probes and sequence com­parisons to the study of 5RB community structure in this ecosystem has suggested that as yet undescribed species are present in significant numbers. In the current study, physiological and phylogenetic analyses of 5RB isolated from a salt marsh sediment were undertaken in order to: (i) compare the phylogenetic diversity of cultivated iso­lates to 'molecular isolates' (i.e., 16S rRNA of uncultivat­ed organisms) from the same study site (ROONEY-VARGA et a!. 1997); (ii) investigate the phylogenetic and nutri­tional diversity of cultivable SRB in a salt marsh sedi­ment and rhizosphere of Spartina alterniflora, and (iii) further investigate the correlation between 165 rRNA phylogeny and nutritional characteristics of delta Pro­teobacteria SRB and the application of the currently available probes for 5RB (Devereux et a!., 1992).

Materials and methods

Source of inocula and techniques used to obtain isolates: Iso­lates were obtained from dilution series prepared with rhizo­sphere cores taken from Chapman's Marsh in the Great Bray re­gion of New Hampshire (HINES et aI., 1989) in August and Oc­tober 1993 and April 1994 (HINES et aI., submitted). The medium described by WIDDEL and BAK (1992) was used, except that the gas phase was 90% N2 with 10% CO2 and the medium was prepared in serum-stoppered bottles or tubes using anaerobic techniques as previously described (SHARAK GENTHNER et aI., 1989). To prevent precipitation during autoclaving, concentrat­ed stocks of CaCI2 . 2 H20, MgCI2 . 6 H20, and NaCI were pre­pared as separate, sterile anaerobic solutions under 100% N2 and were added to individual bottles or tubes of sterile, cooled solution containing the remaining salts, trace metals, and sodi­um bicarbonate. The salinity of the medium was adjusted to that of the overlying marsh water at the time of sampling (August 1993, 29 ppt; October 1993,26 ppt; April 1994, 8 ppt) by modifying the amount of NaCI and MgCI . 6 H20 added in

appropriate ratios (WIDDEL and PFENNIG, 1981). Before inocula­tion, the electron donor and filter-sterilised vitamin solution were added, and the medium was reduced with sodium sul­phide. Each dilution set contained one of the following electron donors: acetate, 20 mM; ethanol, 20 mM; benzoate, 5 mM; butyrate, 10 mM; malate, 10 mM; and propionate, 10 mM. All incubations were at 20 DC.

A most probable number (MPN) dilution series (RODINA, 1972) (10-2 to 10-9 ) was prepared from each sample with each electron donor. Tubes were observed for growth, and active di­lutions were considered those that showed both visible growth and reduction of sulphate as measured by ion chromatography (SHARAK GENTHNER et aI., 1994). The 10-5 through 10-7 dilu­tions were inoculated into triplicate anaerobic roll tubes of the same composition as the initial MPN (SHARAK GENTHNER et aI., 1981) and were incubated at 20 DC until well-formed colonies became visible. Colonies were picked with a sterile needle (1.5", 20 g) attached to a 1 ml glass syringe that had been flushed with NzlC02 (90:10). The colony was immediately transferred into a bottle of fresh liquid medium. Cultures positive for growth, i.e., increase in optimal density at 600 nm and reduction of sul­phate, were examined by phase-contrast microscopy. Pure cul­tures were maintained in liquid medium of the same composi­tion as the MPN medium.

Restriction fragment length polymorphism (RFLP) analysis: Prior to characterisation of the isolates, comparison of restric­tion digest patterns of their 16S rRNA gene (16S rDNA) and those of previously described pure cultures was undertaken. One ml of turbid anaerobic culture was collected, centrifuged 5 min at 8,000xg, decanted and resuspended in 500 pi of PBS (145 mM NaCI, 100 mM NaP04, pH 7.4). This wash step was repeated and the cells were resuspended in 500 pi of O.lxTE (1 mM Tris, 0.1 mM EDTA, pH 8.0). Cells were subjected to three freeze-thaw cycles at -70 DC and 65 DC.

Primers fD1 and rP2 (WEISBURG et aI., 1991) were used to amplify near-complete 16S rRNA gene (16S rDNA) sequences from celllysates. PCR mixtures contained 50 mM KCI, 10 mM Tris-CI pH 8.3, 3 mM MgCI2, 200 pM each dNTP (dATP, dCTP, dGTP, dTTP), 0.2 pM each primer, and 3-5 pi cell lysate in a total volume of 100 pI. The 'hot-start' method was used by heating the PCR mixture to 94 DC for 2 min, and then adding 2 U Taq DNA polymerase to each reaction mixture. The reac­tion mixtures were then subjected to 35 cycles, each consisting of 1 min at 94 DC, 0.5 min at 55 DC, and 2 min at 72 DC, fol­lowed by 5 min at 72 DC, using a Perkin Elmer Thermal Cycler (Perkin Elmer-Cetus, Norwalk, CT). 5 pi of each PCR product was analysed by electrophoresis in 1 % agarose using standard methods (SAMBROOK et aI., 1989). The remaining 95 pi of PCR product was ethanol precipitated (SAMBROOK et ai, 1989), washed with an Ultra free MC filter (10,000 NMWL; Millipore Inc., Bedford, MA), and resuspended in 20 pi distilled H 20. 10 pi of each PCR product was digested separately with the tetrameric endonucleases Mspl, Hhal, and HinfI (SAMBROOK et aI., 1989). The restriction fragments were resolved by gel elec­trophoresis in 2.5% MetaPhor agarose (FMC Bioproducts, Rockland ME) at 12.7 V!cm; 2% SynergeJTM-0.8% agarose at 4.5 V!cm, or 1.7% agarose in 1xTBE (90 mM Tris-borate, 20 mM EDTA, pH 8.0). pGem and PhI X 174 HinfI molecular weight markers (Promega Corp., Madison, WI) were included on each gel. The 0.5xTBE running buffer was chilled to 14 DC with a Bio-Rad mini chilled and recirculated using a Bio-Rad re­circulating pump. The gels were stained with ethidium bromide and photographed under UV transillumination (SAMBROOK et aI., 1989). Fragment sizes were estimated using the DIGIGEL software availabe with the DNASTAR programs (DNASTAR, Inc., Madison, WI). The numbers and sizes of the bands ob­tained were used to place isolates into RFLP categories.

16S rDNA analysis: Sequences of near-complete 16S rDNA from representatives of RFLP categories were obtained directly from PCR products or from inserts cloned into plasmid pNoTAff7 (Five Prime Three Prime, Inc., Boulder, CO) using a PRISM Ready Reaction Dye Deoxy Terminator Cycle Sequenc­ing Kit (Perkin-Elmer Cetus) and an ABI 373A automated se­quencer (Applied Biosystems, Foster City, CAl as previously de­scribed (ROONEY-VARGA et al., 1997). Primers that anneal to conserved regions of 16S rDNA genes were used in sequencing reactions. These included primers fDl (WEISBURG et al., 1991), 926F (BRITSCHGI and FALLON, 1994), 1115F (DORSCH and STACKEBRANDT, 1992), 357R (DORSCH and STACKEBRANDT, 1992), 536R (DEVEREUX et al., 1989), and rP2 (WEISBURG et al., 1991). In addition, primers M13-20, and M13 reverse (Strata­gene, Inc., La Jolla, CAl were used for sequencing cloned 16S rDNA (i .e., BG6, BG8, BG18, BG23, BG33, and BG74). The se­quences were deposited in GenBank under accession numbers U85468 through U85477.

The newly determined sequences were aligned with 16S rRNA sequences of other delta subclass Proteobacteria sul­phate-reducing bacteria and E. coli. Unambiguously aligned base positions were used to calculate Jukes-Cantor distances and construct phylogenetic trees with the maximum parsimony, neighbour-joining, and least-squares methods available in the phylogenetic analysis package PHYLIP 3.57 (FELSENSTEIN, 1989). For maximum parsimony and neighbour-joining trees, 100 bootstrapped data sets were analysed.

Electron donor utilisation by new SRB strains: The ability of the isolated SRB strains to use hydrogen and eleven different or­ganic compounds as electron donors for sulphate reduction was determined in the medium described above, modified by the ad­dition of 0.02 % yeast extract to provide additional nutritional factors. Electron donors were added from concentrated (100x), anoxic stock solutions (pH 7.0, 100% N2) to final concentra­tions of 20 mM acetate, ethanol, fumarate, lactate, malate, pyruvate or succinate; 10 mM butyrate or propionate; 80 mM formate; or 2.5 mM benzoate. Medium containing 2x bicarbon­ate (final concentration 26 mM) and a gas phase of 80:20 N/C02 was used with H2 as an electron donor. The gas phase was flushed with Hz/C02 (90:10) for 2 min and brought to 2 at­mospheres before reducing and inoculating this medium. Cul­tures containing H2 were shaken during incubation. Growth was scored visually and sulphate reduction was determined by ion chromatography as previously described (SHARAK GENTH­NER et aI., 1994).

Results and discussion

Isolation and initial screening of SRB strains

Sixty-one isolates were obtained from the salt marsh sediment samples following the dilution series enrich­ments and colony purifications with roll tubes. Electron donors used for isolations represented compounds that are present in the S. alterni{lora rhizosphere (i.e., malate, ethanol, and acetate) (HINES et al., 1994; MENDELSSOHN and McKEE, 1987; NEDWELL and ABRAM, 1979; SMITH and AP REES, 1979), as well as common products of fer­mentation that are know to be utilised by SRB (WIDDEL and BAK, 1992). RFLP analyses provided a rapid means to assess the purity of each culture by comparing the sum of the lengths of the restriction fragments generated from each culture to the expected length of 16S rDNA (i.e., about 1,500 bp). The potential limitations of this ap-

Salt Marsh SRB Diversity 559

Table 1. Sampling dates, electron donors, and salinities used for enrichment and isolation of sulphate-reducing bacteria.

Isolate Sampling Electron Salinity Number of strains date donor (ppt) in OTU group

BG6 Oct. 1993 ethanol 26 2 BG8 Oct. 1993 propionate 26 6 BG14 Oct. 1993 butyrate 26 2 BG18 Aug. 1993 butyrate 28 8 BG23 Aug. 1993 butyrate 28 7 BG25 Aug. 1993 butyrate 28 1 BG33 Oct. 1993 benzoate 26 2 BG45 April 1994 malate 8 9 BG50 April 1994 ethanol 8 16 BG72 April 1994 acetate 8 5 BG74 April 1994 benzoate 8 3

proach include difficulty in detecting contamination with a closely related strain and difficulty in distinguishing be­tween different 16S rRNA sequences from the same strain. However, we found that RFLP analysis with the three enzymes used here is sufficient to distinguish be­tween 16S rRNA genes that differ by more than 5% and, after analysing about 80 isolates with this approach, we have not observed more than one RFLP pattern per iso­late. In addition, comparison of 16S rDNA RFLP pat­terns was useful for sorting strains into operational taxo­nomic units (OTUs). The RFLP analysis revealed four unique OTUs among strains isolated on butyrate, 2 OTUs each among strains isolated on benzoate and ethanol, and one OTU each among strains isolated on propionate, malate, and acetate (Table 1). Comparison of RFLPs from the isolates to those of eighteen SRB ref­erence strains showed that all but one of the isolate OTUs differed from the analysed SRB reference strains (Table 2). Strain BG45, obtained from a culture enriched with malate, had an RFLP pattern identical to that of Desulfovibrio desulfuricans subsp. aesturii.

Correlation between phylogenetic and physiological characteristics

Analysis of nearly complete 16S rRNA gene sequences from the ten new SRB isolates revealed that they were all members of the delta subclass of the Proteobacteria and were closely related to other known SRB within this group (Fig. 1 and 2). As mentioned above, two distinct lineages of SRB are known to exist within this group, the first being defined by the family Desulfovibrionaceae (DEVEREUX et al., 1990) and the second by the proposed family Desulfobacteriaceae (WIDDEL and BAK, 1992). All the SRB isolates in the current study appear to be mem­bers of these two lineages (Fig. 1 and 2). This result lends support to the hypothesis that the Gram-negative, non­sporeforming, mesophilic SRB are a phylogenetically co­herent group and is consistent with the general observa­tion that most SRB isolated to date are members of this group (STACKEBRANDT et al., 1995).

Tab

le 2

. F

ragm

ent s

izes

(ba

se p

airs

) ob

tain

ed b

y en

donu

clea

se d

iges

tion

of 1

6S r

DN

A.

Spec

ies

or s

trai

n

Des

ulfo

mic

robi

um n

orve

gicu

m

Des

ulfo

vibr

io g

igas

D

esul

fom

icro

bium

bac

ulat

us

Des

ulfo

vibr

io v

ulga

ris

subs

p. v

ulga

ris

Des

ulfo

vibr

io v

ulga

ris

Mar

burg

D

esul

fovi

brio

des

ulfu

rica

ns

Des

ulfo

vibr

io d

esul

furi

cans

sub

sp.

aest

uari

i D

esul

vofi

brio

pig

er

Des

ulfo

vibr

io s

alex

igen

s D

esul

fom

onil

e ti

edje

i D

esul

foar

culu

s ba

arsi

i D

esul

fobu

lbus

pro

pion

icus

D

esul

fobo

tulu

s sa

povo

rans

D

esul

foco

ccus

mu

ltiv

ora

ns

Des

ulfo

bact

eriu

m a

uto

tro

ph

icu

m

Des

ulfo

bact

eriu

m v

acu

ola

tum

D

esul

foba

cter

ium

nia

cini

D

esul

foba

cter

sp.

str

ain

3ac1

0 D

esul

foba

cter

sp.

str

ain

4ac1

1 D

esul

foba

cter

lat

us

BG

6 B

G8

BG

14

BG

15

BG

23

BG

25

BG

33

BG

45

BG

50

BG

72

BG

74

Res

tric

tion

Enz

yme

Use

d (a

)

Hin

fI

36

0,3

15

,24

5,1

85

, 14

5 (c

) 7

35

,24

5,2

20

,18

5

36

0,3

15

,24

5,1

85

, 14

5 (c

) 6

36

,24

5,2

22

,18

5,1

10

,10

5

63

6,2

45

,22

2,1

85

,11

0,1

05

6

36

,31

5,2

45

,18

5,1

10

7

18

,24

0,2

32

,19

0,1

10

6

36

,24

5,2

22

,18

5,1

10

,10

5

32

1,3

15

,24

9,2

32

,18

5

46

5,3

60

,24

9,2

15

,19

0

56

5,3

00

,29

0,1

85

4

65

,37

0,2

70

,22

5

81

0,2

60

,18

5,1

10

6

68

,22

6,1

85

,16

0,1

45

,14

0

66

8,2

62

,18

5,1

50

,10

0

66

8,3

11

,25

5,1

85

,11

0

66

8,3

11

,25

5,1

85

,11

0

80

0,3

65

,19

5,1

90

,16

0

80

0,3

65

,19

0

80

0,3

65

,21

0,2

00

, (1

90),

160

(d)

3

40

,33

6,2

49

,22

2,1

85

,11

0

66

0,3

65

,26

5,

110

56

0,2

25

,21

5,1

90

,17

0,1

50

560,311,255,19~ 1

10

80

0,3

60

,19

0,1

38

8

00

,36

0,1

90

,13

8

66

0,3

11

,22

5,1

85

,11

0

718,240,232,19~ 1

10

62

0,2

55

,22

2,1

90

,11

0,1

00

8

00

,19

0,1

60

(c)

51

0,3

00

,18

5,

155,

114

(c)

Ha

e II

I

25

8,2

10

,19

0,1

75

,14

5,1

40

,11

8 (

c)

ND

(b)

25

8,2

10

,19

0,1

75

,14

5,1

40

,11

8 (

c)

51

7,2

58

,22

5,2

10

,17

9,9

2,8

9

51

7,2

58

,22

5,2

10

,17

9,9

2,8

9

40

0,2

58

, 18

5, 1

75,

145

(c)

56

0,2

80

,20

5,1

79

,14

0

ND

410,258,215,140~)

45

0,2

65

,25

0,8

0 (c

) 305,250,170,168,138~)

51

7,2

65

,22

2,

150

(c)

25

0,1

68

, 16

1, 1

79,

118

(c)

51

7,2

65

,22

2,1

97

,15

0,1

45

5

20

,26

8,2

62

,17

9,1

50

5

10

,27

3,2

62

,17

9,1

50

5

10

,27

0,2

62

,17

9,1

50

5

10

,26

6,2

62

,17

5,1

46

,14

0

51

0,2

66

,26

2,1

75

,14

6,1

40

5

10

,26

6,2

62

,17

9,1

51

,14

8

27

0,2

60

,20

0,1

85

,17

9,1

35

,12

8

51

0,2

70

,22

2,1

44

,12

8 (

c)

44

0,3

15

,27

0,1

85

,17

9,1

40

5

10

,29

0,2

70

,17

9,1

51

5

10

,29

0,2

70

,17

9,1

51

,14

0

51

0,2

85

,27

0,1

79

,15

1

51

0,2

90

,27

0,1

79

,15

1

56

0,2

80

,20

5,1

79

,14

0

31

0,3

80

,22

2,1

85

,17

9,1

38

5

10

,29

0,2

70

,17

9,1

51

,14

0

67

6,2

80

,17

0,1

38

(c)

(a)

Pare

nthe

ses

indi

cate

ban

ds t

hat

stai

ned

wit

h et

hidi

um b

rom

ide

to a

less

er i

nten

sity

tha

n th

e ot

her

band

s.

(b)

Not

det

erm

ined

. (c

) L

ow m

olec

ular

wei

ght

band

s w

ere

obse

rved

but

thei

r si

zes

coul

d no

t be

acc

urat

ely

dete

rmin

ed.

(d)

Ban

ds w

ith

less

er i

nten

sity

wer

e ca

used

by

part

ial

dige

stio

n of

16S

rD

NA

fra

gmen

t.

Msp

I

43

5,3

45

,22

5,1

75

,14

0

ND

4

35

,34

5,2

25

,17

5,1

40

3

11

,25

5,1

98

,17

0,1

60

, 14

7 (c

) 3

11

,25

5,

198,

170

, 16

0, 1

47 (c

) 4

15

,34

5,1

75

,16

0,1

49

,13

8

50

0,4

40

,22

0,1

47

,13

2

ND

3

45

,32

0,2

25

,17

9,1

49

,13

8

190,

166

, 14

5, 1

18 (

c)

517,

(43

0),

32

5,1

75

,14

0,1

26

,12

6 (d

) 3

60

,29

0,1

81

,17

5,1

70

,14

5,1

30

51

7, (

430)

, 36

0, 2

22

,18

1,1

46

,12

5 (

d)

36

0,3

00

,22

2,1

81

,14

5,1

40

,12

0,1

10

3

60

,24

0,

151,

145

, 14

0 (c

) 3

60

,34

0,

181,

138

, 11

0 (c

) 3

60

,34

0,

181,

138

, 11

0(c)

3

60

,34

0,

(179

), 1

75 (

c)

36

0,3

40

,22

2,

(179

), 1

75

36

0,2

22

, (1

79),

175

, (1

60),

148

, 13

8, 1

10

33

8,3

20

,25

8,

175

(c)

66

0,3

38

,17

7,1

38

3

55

,33

8,3

00

,18

7,1

49

,11

2

34

5,3

11

,18

1,1

38

,11

2 (

c)

36

5,3

45

,30

0,1

81

,14

6,1

32

,11

0

36

5,3

45

,30

0,1

81

,14

7,1

32

,11

0

34

5,3

11

,23

0,1

81

,13

8,1

12

5

00

,44

0,2

20

,14

7,1

32

5

17

,42

7,1

45

,13

2,1

20

3

65

,34

0,

(18)

, 17

5, (

145)

, 13

5, 1

12

51

7,3

15

,17

5,1

40

, 12

6 (c

)

V,

G\

o ':"-' ~

:::0

o o Z

m ~ ;:: ;:

0 ~ ~ ~

69

2S

98

100

87

43

20 31

36

21

100

0.02

Myx

ococ

cuS)

Des

u

Des

uljo

vibr

io g

Des

uljo

vib1

Des

uljo

vibr

io

Des

u/ft

Des

uljo

vibr

.

Des

uljo

v

Des

ljov

ibl

BG

50

Des

uljo

vibr

io s

c

BG

6

Des

ulfn

v

D.

De,

Des

'anl

hus

Ijoh

alob

ium

rel

baen

se

bone

nsis

o gi

gas

fair

fiel

dens

is

vibr

io p

iger

o de

su/f

uric

ans

brio

vul

gari

s

o sp

, st

r. P

T-2

o lo

ngre

achi

i

Des

uljo

vibr

io s

p. s

tr.

MIT

87-

599

cale

doni

ensi

s

'exi

gens

brio

hal

ophi

lus

'ong

us

'esu

ljuri

cans

str.

EI

Agh

eila

Z

'ric

anus

'um

nor

vegi

cum

um b

acul

alus

ium

esc

ambi

ense

Esc

heri

chia

col

i

Fig

. 1.

1

65

rR

NA

ph

ylo

gen

etic

tre

e o

f is

olat

es B

G6

and

BG

50

an

d m

emb

ers

of

the

Des

ul­

fovi

brio

nace

ae f

amil

y co

nst

ruct

ed u

sing

a m

axim

um

par

sio

mo

ny

met

ho

d.

86

7 b

ase

po

si­

tio

ns

wer

e co

nsi

der

ed i

n th

e an

alys

is.

Bo

ots

trap

val

ues

(ou

t o

f 1

00

tree

s) a

re s

ho

wn

ad

jace

nt

to n

od

es.

Th

e sc

ale

bar

is i

n fi

xed

nu

cleo

tid

e su

bst

itio

ns

per

seq

uen

ce p

osi

tio

n.

100 41

95

95

Des

uljo

bulb

us e

long

atus

Des

uljo

bulb

us p

ropi

onic

us

981

Des

uljo

caps

a th

iozy

mog

enes

D

esul

jorh

opal

us v

acuo

laoo

.-------------

Des

u(fo

mon

ile

tieq

iei

28

98

76

59

97

Des

uljo

bact

eriu

m v

acuo

latu

m

BG

18

Des

ulfo

bact

eriu

m a

utot

roph

icum

23

Des

uljo

bact

er c

urva

tus

BG

72

-D

esul

foba

cter

hyd

roge

noph

ilus

34

'

91 D

esul

joba

cter

latu

s D

esul

foba

cter

sp.

str.

4ac

ll

96

Des

ulfo

bact

ersp

. st

r. 3

acl0

Des

ulfo

bact

er p

ostg

atei

'-

----

-Desu

lfo

ba

cu

la to

luol

ica

Jr- 3-7-------

Des

ulfo

botu

Jus

sapo

vora

ns

.... ---------

BG

14

21.

Des

ulfo

nem

a li

mic

ola

57

r D

esu(

foco

ccus

mul

tivo

rans

L-.

....

.:7 .;;:2.

... D

esul

fone

ma

mag

num

1

-_

__

_ D

esul

fosa

rcin

a va

riab

ilis

L _

__

__

__

-.:1.

;::O

.::,0

tr==

_

_ -=

Des

ulfo

arcu

lus

boar

sii

'----

BG

74

1--

----

----

----

Myx

ococ

cus

xant

hus

0.02

E

sche

rich

ia c

oli

Fig

. 2

. 1

65

rR

NA

ph

ylo

gen

etic

tre

e o

f is

ola

tes

BG

8,

BG

14

, B

G1

8,

BG

23

, B

G2

5,

BG

33

, B

G7

2,

and

BG

74

, an

d m

emb

ers

of

the

Des

ulfo

bact

eria

ceae

fa

mil

y c

on

stru

cted

usi

ng

a m

axm

imu

m p

arsi

mo

ny

met

ho

d.

89

6 b

ase

po

si­

tio

ns

wer

e co

nsi

der

ed i

n th

e an

aly

sis

sho

wn

her

e. B

oo

tstr

ap v

alu

es (

ou

t o

f 1

00

tre

es)

are

sho

wn

ad

jace

nt

to n

od

es.

Th

e sc

ale

bar

is

in f

ixed

nu

cleo

tid

e su

bst

itio

ns

per

seq

uen

ce p

osi

tio

n.

Vl ~

2:::

~ C/O ::r­

Vl

:;0

O:l o :;: (1) '"' ~.

'<

Vo

~

,....

562 J. N. ROONEy-VARGA et al.

Desulfovibrionaceae isolates

165 rRNA comparisons placed the two isolates ob­tained by enrichment with ethanol, BG6 and BG50, with­in the Desulfovibrionaceae (Fig. 1). BG6 branched at a deep level (Fig. 1) and shared 89.0% 165 rRNA sequence similarity with Desulfovibrio desulfuricans str. El Agheila Z (1,204 base positions compared), 88.9% with Desul­fovibrio gabonensis(1,400 base positions compared), and 88.7% with Desulfovibrio africanus (1,163 base posi­tions compared). The branching order of BG6 and other deep-branching Desulfovibrionaceae remains unclear, as reflected in bootstrapping values (Fig. 1) and differences in branching order among parsimony, neighbour-joining, and least-squares trees (data not shown). Isolate BG50 shared 98.1 sequence similarity (1,422 base positions compared) with its closes relative (Fig. 1), Desulfovibrio caledoniensis, a halophilic 5RB isolated from an oil field brine. Physiological characterisation of isolates BG6 and BG50 corresponds well with their phylogenetic place­ment. Both exhibited a vibroid morphology (Fig. 3) and were able to utilise lactate, pyruvate, ethanol, a malate, and fumarate (Table 3). In addition, their inability to utilise fatty acids, such as acetate, propionate, and bu­tyrate (Table 3), was consistent with other Desulfovibrio species. However, the rather low 165 rRNA sequence similarity between strain BG6 and its closest relative, D. desulfuricans str. El Agheila Z, suggests that strain BG6 may represent a new genus. Additional physiological in­vestigations are necessary to confirm this hypothesis.

The Desulfovibrionaceae form a physiologically co­herent, yet phylogenetic ally broad, group (DEVEREUX et aI., 1990). Organic substrates most commonly utilised by Desulfovibrionaceae members are lactate, pyruvate, ethanol, and, frequently, malate and fumarate (WIDDEL and BAK, 1992). While utilisation of H2 as an electron donor is quite common within this family, growth on H2 is not autotrophic as it requires acetate in addition to CO2 (WIDDEL and BAK, 1992). In addition, most of the members of the genus Desulfovibrio exhibit a vibroid morphology, although rod-shaped cells also occur within this genus (DEVEREUX et aI., 1990; POSTGATE and CAMP­BELL, 1966). The Desulfovibrionaceae are differentiated from other Gram negative 5RBs by an inability to com­pletely oxidise lactate to CO2 or to utilise fatty acids as growth substrates (DEVEREUX et aI., 1990; WIDDEL and BAK, 1992). These characteristics are consistent with those of BG6 and BG50.

While studying ethanol-utilising Desulfobulbus species, LAANBROEK et al. (1982) also found that ethanol­sulphate enrichments yielded Desulfovibrio species, ap­parently because they were able to out-compete other ethanol-utilisers, even though the Desulfovibrio species were not necessarily more numerous in the environment. Probing studies of Chapman's march sediment indicated that Desulfovibrionaceae were relatively less abundant than other ethanol-utilisers, such as Desulfobulbus species (HINES et aI., in prep.; DEVEREUX et aI., 1996), suggesting that in our study, Desulfovibrio spp. had a competitive advantage in the ethanol MPN.

A

B G

H

o I

E J

Fig. 3. Phase-contrast (lOOOx) photomicrographs of new SRB genera/species from Chapman's marsh. (A) strain BG6; (B) strain BG8; (C) strain BG14; (D) strain BG18; (E) strain BG23; (F) strain BG25; (G) strain BG33; (H) strain BG50; (I) strain BG72; (J) strain BG74. Bar equals 10 ]lm and is the scale for all BG strains.

Desulfobacteriaceae isolates

Phylogenetic analysis placed the remammg isolates (BG8, BG14, BG18, BG23, BG25, BG33, BG72, and BG75) within the second Gram-negative mesophilic 5RB family, the Desulfobacteriaceae (Fig. 2). This family en­compasses a phenotypically diverse group of sulphate re­ducers, with a broad phylogenetic diversity approximately equivalent to the family Desulfovibrionaceae. Metabolic traits possessed by various members include both com-

Salt Marsh SRB Diversity 563

Table 3. Electron donors utilised for sulfate reduction by new SRB isolates and selected species.

Strain or Species Electron donor References

A B E F FU H L M P S FN,b

Desulfovibrio africans nr + + + + + + nr POSTGATE, 1984a, b desulfuricans nr + + + + + + + nr POSTGATE, 1984a, b longus + + + + MAGOT et aI" 1992 salexigens nr + + + + + + nr POSTGATE, 1984a, b BG6 + + + + + + + This study BG50 + + + + + + + + This study

Desulfobulbus elongatus nr + + + nr nr 3 WIDDEL and BAK, 1992 marinus + + + + + nr 3 WIDDEL, 1982 propionicus nr + + + + 3 WIDDEL, 1982 2pr4 nr + nr + + nr + nr 3-4 WIDDEL, 1982 BG25 + + + + + 4 This study

Desulfobacterium autotrophicum + nr + + + + + + + + 3-16 BRYSCH et aI" 1987 indolicum + + + + + + + 3 BAK and WIDDEL, 1986 niacini + + + + + + + + 3-16 IMHOFF-STUCKLE and

PFENNIG, 1983 vacuolatum + + + + + + + nr + 3-16 WIDDEL and BAK, 1992 BG18 + + + + + + + + + 4 This study BG33 + + + + + + + + + + 3-4 This study

Desulfobacter curvatus + + + + nr WIDDEL, 1987 hydrogenophilus + + + nr nr WIDDEL, 1987 latus + nr nr WIDDEL, 1987 postgatei + WIDDEL and PFENNIG, 1982 BG8 + + + + + + + 3-4 This study BG23 + + + + + + 3-4 This study BG72 + + This study

Desulfococcus multivorans + + + + + nr nr 3-16 WIDDEL and BAK, 1992

Desulfosarcina variabilis + + + + + + + nr nr 3-14 WIDDEL and BAK, 1992

Desulfonema limicola + + + + + + + 3-14 WID DEL et aI" 1983 magnum + + + + 3-10 WIDDEL et aI" 1983 BG14 + + 4 This study

Desulfobotulus sapovorans + nr 4-16 WIDDEL and BAK, 1992,

FAUQUE, 1995 Desulfoarculus

baarsii + + nr nr 3-18 WIDDEL and BAK, 1992 BG74 4 This study

A - acetate; B - benzoate; E - ethanol; F - formate (not necessarily autotrophic growth); FU - fumarate; H - hydrogen (not necessar-ily autotrophic); L -lactate; M - malate; P - pyruvate; S - succinate; FA - fatty acids; nr - not reported,

'Only propionate and butyrate utilisation were determined in the current study, bThe number of C atoms in fatty acids utilised is shown,

plete and incomplete oxidation of organic compounds; an ability to utilise fatty acids; autotrophic growth on H2 and formate; and diverse morphologies that include vibrios, cocci, rods, and filaments (WIDDEL and BAK, 1992).

Isolate BG25, obtained by enrichment with butyrate, was found to be closely related to members of the genus Desulfobulbus and to form a monophyletic group with the more distantly related genera Desulfocapsa and

Desulforhopalus (Fig. 2). The Ribosomal Database Pro­ject (RDP) (MAIDAK et aL, 1994) currently separates 16S rRNA sequences of Desulfobulbus-related species from those of the Desulfovibrionaceae and Desulfobacteri­aceae under the heading "Desulfobulbus Assemblage." In addition to divergence in 16S rRNA sequence (no more than 86% similarity to other delta subclass sul­phate reducers), Desulfobulbus species differ from other

564 J. N. ROONEy-VARGA et al.

sulphate reducers in the major menaquinone (COLLINS and WIDDEL, 1986), G+C content of genomic DNA (WIDDEL and Bak, 1992), and physiological traits (WID­DEL and BAK, 1992) described below. This assemblage is phylogenetic ally diverse as demonstrated by the deep branches shown in Fig. 2 and additional deep branches (not shown) of sequences cloned from environmental samples taken in northwest Florida (DEVEREUX and MUNDFROM, 1994) and a Danish fjord (TESKE et aI., 1996). Recent description of the new genera Desulfocap­sa (JANSSEN et aI., 1996) and Desulforhopalus (ISAKSEN and TESKE, 1996) and characterisation of the isolate BG25 in this study lead to the emergence of this assem­blage as a distinct group of delta subclass sulphate reduc­ers which should be considered for recognition as a new bacterial family, the "Desulfobulbusaceae."

BG25 and its closest relative, Desulfobulbus marinus, shared 95.6% sequence similarity (1,208 base positions compared). These sequence data and the physiological characteristics of the strain suggest that BG25 should be considered a separate species within the genus Desulfob­ulbus. BG25 was similar to all Desulfobulbus species in an ability to utilise ethanol and pyruvate and an inability to oxidise acetate. It was able to utilise both butyrate and formate, which may be used by Desulfobulbus sp. strain 2pr4 and Desulfobulbus marinus, respectively (Table 3). However, BG25 does differ from other members of the genus Desulfobulbus in several phenotypic traits that were heretofore considered characteristic of the genus (Table 3). In particular, its inability to utilise propionate (Table 3) and its vibroid sigmoidal shape (Fig. 3) are not consistent with characteristic traits of the genus. In addi­tion, BG25 is incapable of growth on two electron donors, hydrogen and lactate, that other characterised Desulfobulbus species utilise and, conversely, is capable of growth on two electron donors, fumarate and malate, that are not utilised by other Desulfobulbus species (Table 3) (WIDDEL, 1982).

Phylogenetic analysis of isolates BG18 and BG33 re­vealed that both fell within the bifurcation of Desulfobac­terium autotrophicum and Desulfobacterium vacuolatum (Fig. 2). BG18 shared a 16S rRNA sequence similarity with its two closest relatives of 96.4% (1,102 base posi­tions compared) with Desulfobacterium niacini and 98.0% (1,525 base positions compared) with BG33. Sim­ilarly, BG33 shared 96.6% (over 1,102 base positions) se­quence similarity with D. niacini. The level of sequence divergence observed suggests that each isolate represents a novel species within the genus Desulfobacterium.

The genus Desulfobacterium was defined by BAK and WIDDEL (1986) to consist of non-sporeforming, com­pletely oxidising sulphate-reducers that utilise a number of fatty acids, may grow autotrophically, and are widespread in marine sediments. Many members of the genus are nutritionally versatile. Cellular morphologies within this genus include the ovoid shape of the type strain (D. autotrophicum) (BRYSCH et aI., 1987), the spherical shape of the bacterium D. niacini (IMHOFF­STICKLE and PFENNIG, 1983), and curved cells. The mor­phologies of both BG18 and BG33 were ovoid (Fig. 3)

and were therefore consistent with those of other mem­bers of the genus. "Nicks and gaps" that probably repre­sented gas vacuoles were also present in BGI8, making it the second species in this genus, after D. vacuolatum, that possesses gas vacuoles.

Electron donors that are commonly utilised by mem­bers of this genus include acetate, ethanol, formate, fu­marate, malate, succinate, and fatty acids (Table 3). Au­totrophic growth on hydrogen is also frequently ob­served within the genus (BRYSCH et aI., 1987; WIDDEL and BAK, 1992). Like its closest relatives, BG33 was quite nutritionally versatile and was capable of utilising ac­etate, ethanol, formate, fumarate, malate, and succinate, as well as benzoate, butyrate, propionate, and pyruvate (Table 3). Benzoate utilisation is not common among Desulfobacterium species, but other members are known to utilise aromatic compounds such as phenol and indole (BAK and WIDDEL, 1986; WIDDEL and BAK, 1992). BG18 only differed from BG33 in its inability to utilise acetate and propionate (Table 3). While its inability to utilize ac­etate was unusual among Desulfobacterium species, it should be noted that other members of the genus are ca­pable of only slight growth on acetate (WIDDEL and BAK, 1992). Thus, 16S rRNA analysis, nutritional analysis, and morphology of isolates BG18 and BG33 permit placement of both strains within the genus Desulfobac­terium.

Isolates BG8, BG23, and BG72 clustered within the genus Desulfobacter (Fig. 2), with isolates BG8 and BG23 most closely related to Desulfobacter curvatus, sharing sequence identifies of 96.6% and 96.4%, respec­tively (over 1,337 base positions compared). BG8 and BG23 were extremely closely related to each other, with 99.8% sequence similarity (over 1,337 base positions). BG72 was most closely related to Desulfobacter post­gatei and Desulfobacter hydrogenophilus, sharing 97.1 % (over 1,371 base positions) and 97.0% (over 1,349 base positions) sequence similarity, respectively.

Morphologies exhibited by the three Desulfobacter isolates were straight thick rod-shaped cells for BG8 and vibroid to sigmoidal cells for BG23 and BG72 (Fig. 3). While these morphologies were consistent with other Desulfobacter species (which include oval-, rod-, and vibrio-shaped cells) (WIDDEL, 1987), preliminary nutri­tional characterisation revealed some marked differences between the isolates BG8 and BG23 and their Desul­fobacter relatives. The characteristic traits of Desul­fobacter species include their ability to utilise acetate (which is commonly used to enrich Desulfobacter species) more effectively than other SRB and their lack of nutritional versatility (Table 3) (WIDDEL and BAK, 1992). BG8 and BG23, however, did not utilise acetate, and did utilize several other electron donors such as fumarate, malate, and propionate that are not commonly used by Desulfobacter species (Table 3). BG23 also utilised bu­tyrate and formate, which are not utilised by other char­acterised Desulfobacter species. BG72's substrate utilisa­tion patterns were more similar to those of other Desul­fobacter species and consisted of utilisation of acetate and hydrogen, but not any other electron donors tested

thus far (Table 3). Thus, based on 16S rRNA analysis and physiological traits, it appears that BG8 and BG23 represent two strain of a species, while BG72 represents a second species, all within the genus Desulfobacter.

Interestingly, BG8 and BG23 were isolated on propi­onate and butyrate, respectively, while other Desulfobac­ter species, including BG72, have been isolated on ac­etate (WIDDEL, 1987; WIDDEL and PFENNIG, 1982). While butyrate and propionate utilisation has been reported among Desulfobacterium, Desulfococcus, Desulfosarci­na, Desulfonema, Desulfobotulus, Desulfoarculus, De­sulfobulbus, and Desulforhabdus species (BAK and WIDDEL, 1986; BEEDER et aI., 1995; BRYSCH et aI., 1987; FAUQUE, 1995; IMHOFF-STUCKLE and PFENNIG, 1983; WIDDEL 1982; WIDDEL and BAK, 1992; WIDDEL et aI., 1983) (Table 3), butyrate has not been commonly used for enrichmentlisolation of SRB and propionate has only been used for isolation of Desulfobulbus species (WIDDEL, 1982; WID DEL and BAK, 1992). Perhaps it was use of these substrates that enabled the isolation of these novel phenotypes within the Desulfobacter genus.

Phylogenetic analysis of BG74 revealed that its closest relative was Desulfoarculus baarsii (formerly Desul­fovibrio baarsii) (Fig. 2). BG74 and D. baarsii shared 95 .3% sequence similarity (1,350 base positions com­pared). BG74 likely represents the second species ob­tained in the genus Desulfoarculus. At the time of writ­ing D. baarsii was the only known member of the genus Desulfoarculus and was considered a separate lineage within the Desulfobacteriaceae family (DEVEREUX et aI., 1989; STACKEBRANDT et aI., 1995). Desulfoarculus is characterised by its ability to carry out complete oxida­tion of organic carbon, its vibroid morphology, and its ability to utilise C1-C18 fatty acids but few other electron donors (WIDDEL and BAK, 1992).

D. baarsii and BG73 appear to be nutritionally limited - both are incapable of utilising benzoate, ethanol, fu­marate, hydrogen, lactate, and malate (Table 3). In fact, of all the substrates tested so far, BG74 was only capable of growth on butyrate, the electron donor used for its isolation (Table 1). This trait is consistent with D. baarsi­i's ability to utilise fatty acids. Further characterisation of BG74 should include tests of its abilities to completely oxidise organic carbon and to utilise higher fatty acids which, as mentioned above, are considered characteristic of the genus Desulfoarculus.

Phylogenetic analysis of isolate BG 14 separated it from other members of the Desulfobacteriaceae family at what can be considered the genus level (Fig. 2). It shared 85.3% sequence similarity with its closest relative, Desulfobotulus sapovorans (1,215 base positions com­pared). The branching order of BG14, D. sapovorans, Desulfomonile tiedjei, D. baarsii, and the Desulfobacter­Desulfobacterium and Desulfococcus-Desulfosarcina lin­eages is unclear, as reflected in bootstrap values for phy­logenetic trees constructed by maximum parsimony (Fig. 2) and neighbour-joining methods (data not shown). Phenotypic traits of BG14 include its capacity to utilise butyrate, hydrogen, and pyruvate, but no other electron donors tested (Table 3).

Salt Marsh SRB Diversity 565

Comparison of isolate sequences to environmental clones

Comparison of the Desulfobacteriaceae isolates' 16S rRNA sequences to 'molecular isolates' A01, 2B14, and 4D19 originating from the same study site (ROONEY­VARGA et aI., 1997) revealed that none of the isolates shared more than about 86% (over 754 base positions compared) sequence similarity with the environmental clones. All three clones fell within the Desulfococcus­Desulfosarcina-Desulfonema assemblage (ROONEY­VARGA et aI., 1997); a group which did not include the isolates described here. The results from the two methods of surveying SRB phylogenetic diversity (i.e., direct re­trieval of 16S rRNA gene fragments and 16S rRNA anal­ysis of novel isolates) provide further evidence of the great diversity of SRB inhabiting the salt marsh sediment. The fact that phylotype A01, which was shown to ac­count for 7.5% of the total bacterial rRNA (ROONEY­VARGA et aI., 1997), was not isolated is likely indicative of biases in isolation techniques. By now, discrepancies between molecular and cultivation based investigations of microbial diversity have been well-documented (e.g., HEAD et aI., 1998; PACE et aI., 1986) and there are many potential sources of bias in cultivation techniques. For example, an organism's nutrient or cofactor require­ments, syntrophic relationships with other microorgan­ism, or specific temperature, pH, or redox potential re­quirements may not be provided in the culture media used. In the current study, an additional source of culti­vation bias may have been that the medium used did not provide a solid sub-stratum for microorganisms to ad­here to. A01 was closely related to members of the genus Desulfonema (ROONEY-VARGA et aI., 1997), which is comprised of filamentous SRB that require a solid sur­face for growth (WIDDEL et aI., 1983). Therefore, if A01 is also a filamentous bacterium, it may also require a solid surface for healthy growth.

Evaluation of SRB probes

A series of oligonucleotide probes intended to specifi­cally target various groups or genera within the Gram­negative mesophilic SRB were designed by DEVEREUX et a1. (1992) and are re-evaluated here against 16S rRNA sequences of the new SRB isolates. Several probes were found to contain a single mismatch with isolates that are members of the target group or genus. Probe 129 was de­signed to target the genus Desulfobacter and while it has no mismatches with sequences of Desulfobacter isolates BG8 and BG23, it does have a single mismatch with the sequence of Desulfobacter isolate BG72. This mismatch is fairly centrally located within the target site (Fig. 4) and sufficient to significantly destabilise the probe-target hybrid (STACKEBRANDT et aI., 1995; WARD et aI., 1992). A mismatch with probe 129 was also reported in the tar­get sequence of Desulfobacter-related strain WN by VAN DER MAAREL et a1. (1996) . Probe 221, for the genus Desulfobacterium, has one mismatch with Desulfobac­terium isolates BG18 and BG33. This mismatch, howev-

566 J. N. ROONEy-VARGA et al.

er, is very close to the 3' end of the target site and may not have a significant effect on probe-target hybridisa­tion. In both cases, adding a mixed based position to the probe sequence allows for inclusion of the new isolates in

the probe target groups, while maintaining specificity for the group in question. Specifically, changing probe 129 to 5'-CAGGCTTGAAGSCAGATT-3' (where S is C or G) results in a probe that targets both previously charac-

Probe 687 (Desulfovibrionaceae)

Target AGGAGUGAAAUCCGUA

BG6 AGGAGUGAAAUCCGUA

Probe 804 (mixed Desulfobacteriaceae)

UCCACGCAGUAAACGUUG UCCACGCYGUAAACG!UG

terised Desulfobacter species and isolates BGS, BG23, and BGn. By using the RDP Check Probe utility (MAIDAK et aI., 1994), the modified probe was checked against all 16S rRNA sequences

BG8 AGAGGUGAAAUYCGUA UCCACGCAGUAAACGUUG in the unaligned RDP database BG14 AGCGGUGAAAU~GUA

BG18 AGAGGUGAAAUYCGUA

BG23 AGAGGUGAAAUYCGUA

BG25 AGAGGUGAAAUYCGUA

BG33 AGAGGUGAAAUYCGUA

BG50 AGGAGUGAAAUCCGUA

BG72 AGAGGUGAAAUYCGUA

BG74 AGAGGUGAAAUYCGUA

Probe 660 (Desulfobulbus)

Target CAGAGGGGAAAGUGGAAUUC

BG6 UGGAG!GGGUGG~GGAAUNC

BG8 GGGAG!GGA~AG!GGAAUUC

BG14 GGUAG!GGAAAG~GGAAUUC

BG18 GGGAG!GGAAAG~GAAUUC

BG23 GGGAG!GGA~AG!GGAAUUC

BG25 CAGAGGGGAAAGUGGAAUUC BG33 GGGAG!GGAAAG~GAAUUC

BG50 CgGAG!GGUUGG~GGAAUUC

BG72 GGGAG!GGAAAG~AAUUC

BG74 UGGAG!GGA~AGUGGAAUUC

Probe 221 (Desulfobacterium)

Target UUUGAAGAUGAGUCCGCGCA BG6 UUUCCAGAUGAGUCCGCGUC

BG8 UUUGGGGAUGAGUUUGCGYA BG14 !U~G~AG~UGAGCUUGCGUC

BG18 UUUGAAGAUGAGUCCGCG~A

BG23 UUUGGGGAUGAGUUUGCGYA BG25 CAUG~AGA~~UCYGCGYA

BG33 UUUGAAGAUGAGUCCGCG~A

BG50 ~UUUUGGAUGAGUCCGCGUC

BG72 UUUGGGGAUGAGUUUGCGYA BG74 CCCUUAGA~GAG~CCGCGUC

UCCAYGCAGUAAACGUUG UCCACGCAGUAAACGUUG UCCACGCAGUAAACGUUG UCCACGCCGUAAACG!UG UCCACGCAGUAAACGUUG UCCACGCYGUAAACG!UG UCCACGCAGUAAACGUUG UCCACGCCGUAAACG~UG

Probe 129 (Desulfobacter)

AAUCUGCCUUCAAGCCUG AAUCUCCCUGGAAAUUCG AAUCUGCCUUCAAGCCUG AAUCUGYCU~C~AAUC~G

AAUCU!CCUUCAAAUCgG AAUCUGCCUUCAAGCCUG AA~CU!CCU~CAYGUUUG

AAUCU!CCUUCAAAUCgG AAUCUGCCCUGAAGAUCG AAUCUG~UUCAAGCCUG

AAUCU!CCUAAA~UACG

Probe 814 (Desulfococcus-Desulfosarana-

Desulfobotulus) AAACGUUGAUCACUAGGU AAACG!UGGAUGCUAGGU AAACGUUGUACACU~GGU

AAACGUUGAUYACUAGGU AAACGUUGUAUGCUAGGU AAACGUUGUACACU~GGU

AAACG!UGUCAACUAG!U AAACGUUGUAUGCUAGGU AAACG!UGGAUAYUAGGU AAACGUUGUACACU~GGU

AAACG~UGUCCACUAGGU

Fig. 4. Comparison of probe 687,804,660,129,221, and 814 target sites with aligned 16S rRNA sequences of SRB isolates. Mismatches with the probe target site are shown in boldtype and underlined.

and found to be specific for Desulfobacter species. Similarly, probe 221 could be modified to 5'-TSCGCGGACTCAT­CTTCAAA-3', and once again, the CheckProbe utility was used to show that this modified probe targeted characterised Desulfo­bacterium and new Desulfobac-terium isolates to the exclusion of other 16S rRNA molecules.

Probe S14, designed to target the Desulfococcus-Desulfosarci­na-Desulfobotulus assemblage contains one centrally located mis­match with BG14. However, while this assemblage constitutes BG14's closest relatives, as discussed above, BG14 appeared to repre­sent a separate lineage not includ­ed in the group originally intended to be targeted by probe S14. Probe S04 was designed to target all members of the Desulfobacte­riaceae family except Desulfo­bulbus and Desulfoarculus. Iso­lates BGS, BG18, BG23, BG33, and BGn, all members of this group, contained the target se­quence. Isolate BG14 and De­sulfoarculus isolate BG74 each had single mismatches with 804 that were centrally located. The former finding may be lend sup­port to the placement of BG 14 in a separate lineage, while the latter is consistent with expected speci­ficity of probe S04. As previously described (DEVEREUX et aI., 1992), the target site for probe S04 is more conserved than sites targeted by probes 129 and 221. Probe 804 is therefore expected to detect the rRNAs of bacteria with mismatch­es to the more specific probes.

The target sequence for the De­sulfobulbus probe 660 was found in Desulfobulbus isolate BG25, as was the target sequence for the

Desulfovibrionaceae probe 687 in Desulfovibrionaceae iso­lates BG6 and BG50 (Fig. 4). It should be noted that the lat­ter probe was recently found to also target members of the Geobacteraceae family (LONERGAN et al., 1996) and is no longer considered specific for its originally intended targets.

Conclusions

Using various electron donors thought to be prevalent in their native habitat, sixty-one SRB strains were isolated from a salt marsh sediment. Ten of these were chosen for further analysis based on unique RFLPs generated by di­gesting their 16S rRNA genes with tetrameric restriction enzymes. Analysis of near-complete 16S rRNA gene se­quences from these ten isolates placed all the isolates with­in the delta Proteobacteria SRB. Isolates BG6 and BG50 were both members of the family Desulfovibrionaceae, with BG6 possibly representing a novel genus and BG50 representing a novel species within the genus Desulfovib­rio. Isolates that were members of the Desulfobacteriaceae family were distributed among the genera Desulfobacter (BG8, BG23, and BG72), Desulfobacterium (BG18 and BG33), Desulfoarculus (BG74) and a novel genus repre­sented by isolate BG14. Based on 16S rRNA analysis, all isolates were distinct from characterised Desulfobacteri­aceae at the species or genus levels. One isolate (BG25) was placed within the Desulfobulbus assemblage, a group that should be considered for recognition as a new family, the "Desulfobulbusaceae." With the exception of several traits of BG25, BG8, and BG23, physiological characteris­tics of the isolates corresponded well with those of their closest relatives. None of the isolates shared more than 86% sequence similarity with environmental clones ob­tained from the same study site (ROONEY-VARGA et al., 1997), thereby providing further evidence of the diversity of SRB inhabiting salt marsh sediments. In addition, eval­uation of currently available probes for SRB (DEVEREUX et al., 1992) against the isolates' 16S rRNA sequences re­vealed that, with the addition of mixed base positions to

probes 129 and 221, SRB-directed probes could still be used against their originally intended targets.

Acknowledgements This work was supported by the u.s. Environmental Protec­

tion Agency Cooperative Agreement #CR-820062 and the National Science Foundation Ecology Program grant #DEB-9520272. Use of trade names does not imply endorsement by the U.S. E.P.A.

References

BAK, F. and WIDDEL, F.: Anaerobic degradation of indolic com­pounds by sulfate-reducing enrichment cultures and descrip­tion of Desulfobacterium indolicum gen. nov., sp. nov. Arch. Microbio!. 146, 170-176 (1986).

BARTON, L. L. and TOMEI, F. A.: Characteristics and Activities of Sulfate-Reducing Bacteria, pp. 1-32. In: Sulfate-Reducing Bacteria (L. L. BARTON, ed.). Plenum Press, New York (1995).

BEEDER, J., TORSVIK, T and LIEN, T: Thermodesulforhabdus norvegicus gen. nov., sp. nov., a novel thermophilic sulfate-

Salt Marsh SRB Diversity 567

reducing bacterium from oil field water. Arch. Microbiol. 164,331-336 (1995).

BRITSCHGI, T. B. and FALLON, R. D.: PCR-Amplification of mixed 16S rRNA genes from an anaerobic, cyanide-degrad­ing consortium. FEMS Microbiol. Ecol. 13,225-231 (1994).

BRYSCH, K., SCHNEIDER, c., FUCHS, G. and WIDDEL, F.: Litho­autotrophic growth of sulfate-reducing bacteria, and descrip­tion of Desulfobacterium autotrophicum gen. nov., sp. nov. Arch. Microbiol. 148,264-278 (1987).

COLLINS, M. D. and WIDDEL, F.: Respiratory qui nones of sul­phate-reducing and sulphur-reducing bacteria: a systematic study. Syst. Appl. Microbiol. 8, 8-18 (1986).

DEVEREUS, R., DELANEY, M., WIDDEL, F. and STAHL, D. A.: Nat­ural relationships among sulfate-reducing eubacteria . ]. Bac­teriol. 171,6689-6695 (1989).

DEVEREUX, R., HE, S.-H., DOYLE, C. L., ORKLAND, S., STAHL, D. A., LEGALL, J. and WHITMAN, W. B.: Diversity and origin of Desulfovibrio species: Phylogenetic definition of a family. J. Bacteriol. 172,3609-3619 (1990).

DEVEREUX, R., HINES, M. E. and STAHL, D. A.: S cycling: Char­acterization of natural communities of sulfate-reducing bac­teria by 16S rRNA sequence comparisons. Microb. Ecol. 32, 283-292 (1996).

DEVEREUX, R. , KANE, M. D., WINFREY, J. and STAHL, D. A.: Genus- and group-specific hybridization probes for determi­native and environmental studies of sulfate-reducing bacte­ria. System. Appl. Microbiol. 15,601-609 (1992).

DEVEREUX, R. and MUNDFROM, G. W.: A phylogenetic tree of 16S rRNA sequences from sulfate-reducing bacteria in a sandy marine sediment. Appl. Environ. Microbiol. 60, 3437-3439 (1994).

DORSCH, M. and STACKEBRANDT, E.: Some modifications in the procedure of direct sequencing of PCR amplified 16S rDNA. J. Microbiol. Methods 16,271-279 (1992).

FAUQUE, G. D.: Ecology of Sulfate-Reducing Bacteria, pp. 217-242. In : Sulfate-Reducing Bacteria (L. L. BARTON, eds) New York, Plenum Press 1995.

FELSENSTEIN, J. : PHYLIP - phylogeny inference package. Cladis­tics 5, 164-166 (1989).

GIBSON, G. R.: Physiology and ecology of sulphate-reducing bacteria. J. Appl. Bacteriol. 69, 769-797 (1990).

HANSEN, T. A.: Carbon Metabolism of Sulfate-Reducing Bacte­ria, pp. 21-40. In: The Sulfate-Reducing Bacteria: Contem­porary Perspectives (J. M. ODOM and R. SINGLETON, Jr., eds.) Springer-Verlag, New York (1993) .

HEAD, I. M., SAUNDERS, J. R. and PICKUP, R. W.: Microbial evo­lution, diversity, and ecology: A decade of ribosomal RNA analysis of uncultivated microorganisms. Microb. Eco!. 35; 1-21 (1998).

HINES, M. E., BANTA, G. T, GIBLIN, A. E., HOBBIE, ]. E. and TUGEL, ]. T.: Acetate concentrations and oxidation in salt marsh sediments. Limnol. Oceanogr. 39, 140-148 (1994).

HINES, M. E., EVANS, R. S., SHARAK GENTHNER, B. R., WILLIS, S. G., FRIEDMAN, S. and DEVEREUX, R.: Molecular phylogenetic and biogeochemical studies of sulfate-reducing bacteria in the rhizosphere of Spartina alterniflora. (submitted to App!. Environ. Microbiol.) .

HINES, M. E., KNOLLMEYER, S. L. and TUGEL, J. B.: Sulfate reduc­tion and other sedimentary biogeochemistry in a northern New England salt marsh. Limnol. Oceanogr. 34, 578-590 (1989).

HOWARTH, R. W.: Microbial processes in salt-marsh sediments, pp. 239-260. In: Aquatic Microbiology: an Ecological Ap­proach (T. E. FORD, ed.) Blackwell Scientific Publications, Boston (1993).

HOWARTH, R. W. and HOBBIE, J. E.: The regulation of decompo­sition and heterotrophic microbial activity in salt marh soils: a review, pp. 103-127. In: Estuarine Comparisons (Y. S. KENNEDY, ed.) Academic Press, New York (1982).

568 J. N. ROONEy-VARGA et a!.

IMHOFF-STUCKLE, D. and PFENNIG, N.: Isolation and characteri­zation of a nicotinic acid-degrading sulfate-reducing bacte­rium, Desulfococcus niacini sp. nov. Arch. Microbio!. 136, 194-198 (1983).

ISAAKSEN, M. E and TESKE, A.: Desulforhopalus vacuolatus gen. nov., sp., nov., a new moderately psychrophilic sulfate-reduc­ing bacterium with gas vacuoles isolated from a temperate estuary. Arch. Microbio!. 166, 160-168 (1996).

JANSSEN, P. H., SCHUHMANN, A., BAK, E, and LiESACK, W.: Dis­proportion of inorganic sulfur compounds by the sulfate-re­ducing bacterium Desulfocapsa thiozymogenes gen. nov., sp. nov. Arch. Microbio!. 166, 184-192 (1996).

LAANBROEK, H. J., ABEE, T. and VOOGD, I. L.: Alcohol conver­sions by Desulfobulbus propionicus Lindhorst in the pres­ence and absence of sulfate and hydrogen. Arch. Microbio!. 133,178-184 (1982).

LANE, D., PACE, B., OLSEN, G. J., STAHL, D. A., SOGIN, M. L. and PACE, N. R.: Rapid determination of 16S ribosomal RNA se­quences for phylogenetic analyses. Proc. Nat!' Acad. Sci. USA 82, 6955-6959 (1985).

LONERGAN, D. J., JENTER, H. L., COATES, J. D., PHILLIPS, E. J. P., SCHMIDT, T. M. and LOVLEY, D. R.: Phylogenetic analysis of dissimilatory Fe(III)-reducing bacteria. J. Bacterio!' 178, 2402-2408 (1996).

MAGOT, M., CAUMEITE, P., DESPERRIER, J. M. and MATHERON, R.: Desulfovibrio longus sp. nov., a sulfate-reducing bacte­rium isolated from an oil-producing wei!. Int. j. Syst. Bacte­rio!. 42, 398-403 (1992).

MAIDAK, B. L., LARSEN, N., MCCAUGHEY, M. J., OVERBEEK, R., OLSEN, G. J., FOGEL, K., BLANDY, J. and WOESE, e. R.: The Ribosomal Database Project. Nucleic Acids Res. 22, 3485-3487 (1994).

MENDELSSOHN, I. A. and McKEE, K. L.: Root metabolic re­sponse of Spartina alternif/ora to hypoxia, pp. 239-353. In: Plant Life in Aquatic and Amphibious Habitats (R. M. M. CRAWFORD, ed.), British Eco!. Soc. Spec. Pub!. No.5 (1987).

NEDWELL, D. B. and ABRAM, J. W.: Relative influence of temper­ature and electron donor and electron acceptor concentra­tions on bacterial sulfate reduction in salt marsh sediment. Microb. Eco!. 5, 67-72 (1979).

PACE, N. R., STAHL, D. A., LANE, D. J. and OLSEN, G. J.: The analysis of natural microbial populations by ribosomal RNA sequences, pp. 1-55. In: Advances in Microbial Ecology (K. e. MARSHALL, ed.) Plenum Press, New York (1986).

POSTGATE, J. R.: Genus Desulfovibrio, pp. 666-672. In: Bergey's manual of systematic bacteriology (N. R. KRIEG and j. G. HOLT, eds.) Williams and Wilkins, Baltimore (1984).

POSTGATE, J. R.: The Sulphate-Reducing Bacteria, 2nd ed., Cambridge University Press, Cambridge, UK (1984).

POSTGATE, J. R. and CAMPBELL, L. L.: Classification of Desul­fovibrio species, the nonsporulating sulfate-reducing bacte­ria. Bacterio!' Rev. 30, 732-738 (1966).

RODINA, A. G.: pp. 177-180. In: Methods in Aquatic Micro­biology. University Park Press Baltimore (1982).

ROONEy-VARGA, j. N., DEVEREUX, R., EVANS, R. A. and HINES, M. E.: Seasonal changes in the relative abundances of rRNA from uncultivated sufi ate-reducing bacteria in the rhizo­sphere of Spartina alternif/ora. App!. Environ. Microbio!. 63, 3895-3901 (1997).

SAMBROOK, J., FRITSCH, E. E and MANIATIS, T.: Molecular Cloning: A Laboratory Manual, 2 ed., Cold Spring Harbor Laboratory Press, Cold Spring Harbor (1989).

SHARAK GENTHNER, B. R., DAVIS, e. L. and BRYANT, M. P.: Fea­tures of rumen and sewage sludge strains of Eubacterium limosum, a methanol- and Hz-C02-utilizing species. App!. Environ. Microbio!. 42,12-19 (1981).

SHARAK GENTHNER, B. R., MUNDFROM, G. and DEVEREUX, R.: Characterization of Desulfomicrobium escambium sp. nov.

and proposal to assign Desulfovibrio desulfuricans strain Norway 4 to the genus Desulfomicrobium. Arch. Microbiol. 161,215-219 (1994).

SHARAK GENTHNER, B. R., PRICE, W. A. and PRITCHARD, P. H.: Anaerobic degradation of chI oro aromatic compounds in aquatic sediments under a variety of enrichment conditions. Appl. Environ. Microbiol. 55,1466-1471 (1989).

SMITH, A. M. and AP REES, T.: Pathways of carbohydrate fer­mentation in the roots of marsh plants. Planta 146,327-334 (1979).

SMITH, D. W.: Ecological actions of sulfate-reducing bacteria, pp. 161-188. In: The Sulfate-Reducing Bacteria: Contempo­rary Perspectives (J. M. ODOM and R. SINGLETON, Jr., eds.) Springer-Verlag, New York (1993).

STACKEBRANDT, E., STAHL, D. A. and DEVEREUX, R.: Taxonomic Relationships, pp. 49-87. in: Sulfate-Reducing Bacteria (L. L. BARTON, ed.) Plenum Press, New York (1995).

TESKE, A., WAWER, e., MUYZER, G. and RAMSING, N.: Distri­bution of sulfate-reducing bacteria in a stratified fjord (Mariager Fjord, Denmark) as evaluated by most-probable­number counts and denaturing gradient gel electrophoresis of PCR-amplified ribosomal DNA fragments. Appl. Environ. Microbiol. 62, 1405-1415 (1996).

VAN DER MAAREL, M. J. E. e., JANSEN, M., HAANSTRA, R., MEI­JER, W. G. and HANSEN, T. A.: Demethylation of dimethyl sul­fonioproprionate to 3-s-methylmercaptopropionate by ma­rine sulfate-reducing bacteria. App!. Environ. Microbiol. 62, 3978-3984 (1996).

WARD, D., BATESON, M., WELLER, R. and RUFF-ROBERTS, A.: Ri­bosomal RNA analysis of microorganisms as they occur in nature, pp. 219-286. In: Advances in Microbial Ecology (K. MARSHALL, eds.) Plenum Press, New York (1992).

WEISBURG, W. G., BARNS, S. M., PELLEITIER, D. A. and LANE, D. J.: 16S ribosomal DNA amplification for phylogenetic study. J. Bacteriol. 173,697-703 (1991).

WIDDEL, E: Studies on dissimilatory sulfate-reducing bacteria that decompose fatty acids. II. Incomplete oxidation of pro­pionate by Desulfobulbus propionicus gen. nov., sp. nov. Arch. Microbio!. 131,360-365 (1982).

WID DEL, E: New types of acetate-oxidizing, sulfate-reducing Desul­fabaeter species, D. hydrogenaphilus sp. nov., D. latus sp. nov., and D. eurvatus sp. nov. Arch. Microbio!. 148,286-291 (1987).

WIDDEL, E and BAK, E: Gram-Negative Mesophilic Sulfate-Re­ducing Bacteria, pp. 3352-3378. In: The Prokaryotes (A. BALOWS, H. G. TRUPER, M. DWORKIN, W. HARDER and K.-H. SCHLEIFER, eds.) 2nd, New York, Springer-Verlag 1992.

WIDDEL, E, KOHRING, G.-W. and MAYER, E: Studies on dissimi­latory sulfate-reducing bacteria that decompose fatty acids III. Characterization of the filamentous Desulfonema limico­la gen. nov. sp. nov. and Desulfonema magnum sp. nov. Arch. Microbio!. 134,286-294 (1983).

WID DEL, E and PFENNIG, N.: Studies on dissimilatory sulfate-re­ducing bacteria that decompose fatty acids. I. Isolation of new sulfate-reducing bacteria enriched with acetate from saline environments. Description of Desulfobacter postgatei gen. nov. sp. nov. Arch. Microbio!. 129,395-400 (1981).

WIDDEL, E and PFENNIG, N.: Studies on dissimilatory sulfate-re­duzing bacteria that decompose fatty acids. I. Isolation of new sulfate-reducing bacteria enriched with acetate from saline environments. Description of Desulfobacter postgatei gen. nov. sp. nov. Arch. Microbio!. 129,395-400 (1982).

Corresponding author: J. N. ROONEy-VARGA, Department of Biological Sciences, Uni­versity of MAssachusetts Lowell, 1 University Ave., Lowell, MA 01854,. U.S.A. Telephone: (978) 934-4715; Fax: (978) 934-3044; e-mail: juliette_RooneyVarga@um!.edu.