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Transcript
APPLIED AND ENVIRONMENTAL MICROBIOLOGY, Apr. 1980, p. 913-918
0099-2240/80/04-0913/06$02.00/0
Vol. 39, No. 4
Immunofluorescent Assay for the Marine AmmoniumOxidizing Bacterium Nitrosococcus oceanust
B. B. WARD* AND M. J. PERRY
Department of Oceanography, University of Washington, Seattle, Washington 98195
Nitrification is one of the important microbiological transformations of nitrogen
in the ocean. Traditional enrichment-culture methods for enumerating the autotrophic bacteria which oxidize ammonium to nitrite are very time consuming
(months) and are believed to seriously underestimate natural abundances. A
fluorescent-antibody assay for a marine ammonium-oxidizing bacterium was
developed to provide a rapid and direct means of identifying these microorganisms. Antibodies to Nitrosococcus oceanus were prepared and tested against
pure cultures of marine, freshwater, and soil ammonium oxidizers and against
bacteria from natural seawater samples. Cell counts of culture samples determined
by the fluorescent-antibody assay agreed with hemacytometer and acridine
orange counts. Our results demonstrated that the immunofluorescent assay is a
powerful tool for the detection of Nitrosococcus in the marine environment.
Nitrite occupies a key position in the nitrogen
cycle in the ocean as an intermediate in nitrification, denitrification, and nitrate respiration.
The rates of these processes are important in
determining the distribution and abundance of
inorganic nitrogen in the ocean. Microbial production of nitrite is mediated by two very different biochemical transformations: oxidation of
ammonium to nitrite by autotrophic nitrifying
bacteria (7, 29) and reduction of nitrate to nitrite
by both heterotrophic denitrifying bacteria (13)
and nitrate-respiring facultative anaerobes (9).
Phytoplankton release nitrite under conditions
of light limitation (6, 15, 27). The relative importance of the oxidative and reductive transformations is a function of environmental parameters in a specific oceanic regime (6, 16, 21).
Denitrification, for example, is believed to be
the prime mechanism of nitrite production in
waters with low dissolved-oxygen concentrations
(13); nitrate respiration also occurs under these
conditions (9, 11). The occurrence of autotrophic
nitrification is not as well documented, nor are
the specific environmental conditions favoring
nitrification well defined (7).
Ammonium-oxidizing bacteria have been isolated from the Atlantic (S. W. Watson, Abstract,
Int. Congr. Microbiol. 8th, Montreal, B,6:12,
1962) and Pacific (10) oceans. In culture media
with environmentally realistic concentrations of
ammonium, rates of both growth and nitrite
production are very low. Watson (29) and Carlucci and Strickland (10) have estimated from
ammonium enrichment studies that in situ
abundances of nitrifying bacteria in the ocean
may be as low as one bacterium per liter, and
certainly less than 103 cells per liter. Such low
abundances, coupled with low estimated rates of
nitrification, lead these investigators to conclude
that in situ nitrification is insufficient to account
for the observed nitrite distribution in the sea.
The ammonium enrichment techniques used
for enumerating nitrifying bacteria, however, require long incubations and may seriously underestimate in situ abundances. We developed an
immunofluorescent-antibody assay as an alternative to the enrichment methods and as a more
direct approach for determining in situ concentrations of nitrifying bacteria in the ocean. The
fluorescent-antibody (FA) technique is successfully used by Schmidt and co-workers to study
Rhizobium (25) and nitrifying bacteria (2, 12) in
freshwater and soils; Apel and co-workers (1)
and Reed and Dugan (24) use a similar approach
for enumerating Thiobacillus and methylotrophs, respectively, in their natural environments. In this paper we describe the preparation
and testing of an immunofluorescent assay of
sufficient sensitivity and specificity for the detection and enumeration of low concentrations
of nitrifiers in the marine environment.
MATERIALS AND METHODS
Cultures. Isolates of marine nitrifying bacteria
were kindly supplied by A. F. Carlucci, Scripps Institution of Oceanography (Nitrosococcus [Nitrosocystis] oceanus and an unidentified marine ammoniumoxidizing isolate, no. 5), and by S. W. Watson, Woods
Hole Oceanographic Institution (N. oceanus). Soil and
freshwater isolates were obtained from E. L. Schmidt,
Department of Microbiology and Soil Science, UniNitrosomt Contribution no. 1147 from the Department of Oceanog- versity of Minnesota (Nitrosomonas Tara,Nitrosomoonas europaea, Nitrosomonas E-K, and
raphy, University of Washington.
913
914
nas
APPL. ENVIRON. MICROBIOL.
WARD AND PERRY
WH-2). The marine isolates
were
maintained in
two seawater culture media: (i) C medium which was
modified from Carlucci and Strickland (10) to contain
0.3 g of CaCO3, 0.05 g of K2HPO4, 0.16 g of NH4C1, and
1.0 ml of chelated metals solution (3) per liter of
filtered seawater; and (ii) W medium (29), containing
0.635 g of NH4Cl, 0.02 g of CaCl2.2H20, 0.357 g of
MgSO4.7H20, 0.043 g of K2HPO4, 0.005 g of phenol
red, and 1.0 ml of chelated metals solution per liter of
filtered seawater. W medium required periodic adjustment to pH 7.5 with sterile 0.1 M K2CO3. Nitrosomonas isolates were grown in a medium containing 0.5 g
of (NH4)2SO4, 0.04 g of MgSO4. 7H20, 0.2 g of KH2PO4,
0.04 g of CaCl2.2H20, 1.0 ml of basic phenol red
solution (0.05% phenol red in 0.0014 N NaOH), and
1.0 ml of chelated metals solution per liter of distilled
water (26); pH was maintained by periodic addition of
0.47 M Na2CO3 when indicated by color change of the
phenol red indicator. All the above isolates were maintained in liquid culture (50- or 100-ml volumes in 125or 250-ml Erlenmeyer flasks) at 20°C in the dark and
were transferred to fresh media every 3 weeks. Freedom of the cultures from heterotrophic bacterial or
fungal contaminants was monitored by inoculating a
sample of the culture into sterility-test medium (after
Carlucci and Pramer [8]; modified CP medium: 2.5 g
of bacto-tryptone, 0.1 g of yeast extract, 0.1 g of
K2HPO4, and 1.0 ml of chelated metals solution per
liter of distilled water or 90% seawater).
The bacterial isolates used in heterologous testing
of the assay specificity were maintained in appropriate
media. Escherichia coli (supplied by D. Cramer, Department of Microbiology, University of Washington)
was maintained on agar plates or slants on a basal
salts solution with 1.0 g of glucose per liter (20).
Beneckea gazogenes, BV1-SJG (another marine pigmented vibrio, supplied by S. J. Giovannoni, Department of Biology, Boston University), and unidentified
marine heterotrophs (isolated from waters off the
Washington coast by the senior author) were all maintained on plates or in liquid culture of modified CP
medium. Thiosulfate-oxidizing isolate Ml was isolated
from a Massachusetts salt marsh by the senior author
and maintained on the Thiobacillus thioparus medium of Vishniac and Santer (28). Nitrobacter agilis
(supplied by E. L. Schmidt) was grown in the Nitrobacter medium of Fliermans et al. (12).
Field samples. Seawater samples were collected in
40-liter polyvinyl chloride water bottles during several
cruises off the Washington coast. Seawater was prefiltered through 10-,um Nitex netting to remove zooplankton and large phytoplankton and then concentrated by continuous-flow centrifugation at 27,000 x g
at 4°C on board ship using a gimbal-mounted, highspeed centrifuge. Pellets were suspended in 200 to 400
ml of filtered seawater and preserved in 2% Formalin
(sodium acetate buffered) for subsequent fluorescentantibody staining in the laboratory.
Immunization procedure. A total of 137 liters of
N. oceanus (Carlucci isolate) culture were grown in
several 12- and 20-liter glass carboys, filed to 75%
capacity, and were harvested by continuous-flow centrifugation at 27,000 x g. The pellets were washed in
saline solution (0.15 M NaCl), respun at 39,000 x g for
30 min, covered with saline, and frozen at -40°C until
A 3-ml sample of this saline cell suspension,
containing 10 mg of protein per ml (assayed according
to Lowry et al. [19]), was used for the immunization of
use.
each of two female New Zealand white rabbits. A
modification of the immunization schedule of Kenny
(18) was followed (Table 1). A sample of blood was
drawn before immunization to test for reactions between N. oceanus and this pre-immunization serum.
At 7 days after the last injection, antisera were collected (by cardiac puncture) directly into sterile vacuum bottles. The whole blood was allowed to coagulate for 24 h at room temperature, after which the
supernatant serum was poured off and centrifuged for
10 min at 3,000 x g. The clear serum was frozen at
-40°C and used without further purification in all
subsequent antibody-antigen reactions.
Double immunodiffusion procedure. Antigenantiserum reactions were tested by a thin-layer gel
diffusion technique (23). Melted agarose (1.2 ml of
0.5% [wt/vol], Sigma Chemical Co., St. Louis, Mo.) in
Veronal buffer (0.0167 M barbital, 0.0834 M sodium
barbital, pH 8.6) with 0.5% Triton X-100 was plated
on a 25- by 75-mm glass slide. Once the agarose had
solidified, Plexiglas templates were placed on the gel
surface. Wells in the templates were filled with 10 to
12 pl of the appropriate test isolate or antiserum
preparation. The slides were placed in a humidified
chamber for 48 h and then in a TES-saline solution
[5 mM N-tris(hydroxymethyl)methyl-2-aminoethane
sulfonic acid in 0.15 M NaCl, pH 7.3] for 24 h, washed
in distilled water for 4 h, and dried overnight at 37°C.
Dried slides were stained with Coomassie brilliant blue
(1.0 g of Coomassie brilliant blue in 200 ml of destain
solution [95% ethanol-distilled water-glacial acetic
acid, 9:9:2]) for 7 min and then destained for 5 to 15
min in destain solution. Antigens used in the immunodiffusion procedure were obtained from large-volume cultures, which were harvested, washed, and
stored as described for N. oceanus.
FA staining procedure. An indirect FA staining
method (employing a fluorescent-labeled nonspecific
sheep anti-rabbit antibody) was used (Fig. 1). The
Day
0
1
TABLE 1. Immunization schedule
Protocol
Draw 15 ml of preblood from marginal ear
vein
Inject each flank intramuscularly with 1:1
emulsion of antigen: Freund incomplete
adjuvant (Difco Laboratories)
21
Inject increasing volumes of antigen
(without adjuvant) in marginal ear vein
0.1 ml
24
0.2 ml
27
0.3 ml
30
0.4 ml
37
Collect antisera by cardiac puncture
IMMUNOFLUORESCENT ASSAY FOR N. OCEANUS
VOL. 39, 1980
protocol was derived, in part, from Reed and Dugan's
(24) indirect FA method and, in part, from the direct
FA method (em'ploying a fluorescent-labeled specific
antibody) of Bohlool and Schmidt (5). Filters (0.40-,um
nominal pore size, Nuclepore Corp., Pleasanton, Calif.)
were dyed by immersion in Irgalan black (0.2% in 2.0%
acetic acid, Union Color and Chemical Co., Boston,
Mass.) for a minimum of 0.5 h, rinsed in distilled water,
placed on filter holders, and washed with phosphatebuffered saline (PBS: 8.0 g of NaCl, 0.2 g of KCI, 1.15
g of Na2HPO4, and 0.2 g of KH2PO4 per liter of distilled
water; pH adjusted to 7.4 with 1.0 N NaOH). Samples
of cultures or natural seawater containing material to
be FA stained were filtered and washed with PBS. For
field samples, filters were removed from holders and
placed on glass slides; a gelatin solution (0.2 ml of
alkaline hydrolyzed gelatin, pH 10.5 [4]) was placed
on the filters, and the slides were incubated at 50 to
60°C until nearly dry. When pure cultures were FA
stained, the filters were kept on the filter holders,
covered with 0.2 ml of 2% bovine serum albumin
(Sigma Chemical Co.) in PBS for 30 min, and then
dye filter
rinse filter in distilled water
place filter on holder
wash with PBS
filter sample under vacuum
A-
culture samples
4,
field samples
remove
place
ain filter on holder
filter from holder;
glass slide
rets
on
I^
r
filter vith 0.2 ml
2Z alkaline hydrolyzed
gelatine solution
cover
covet
on
2%
BSA
I
holder
vash filters with 30 ml PB's
add 10 ul specific antibod' y
incubate 30 min
wash vith 30 ml PBS
bit IgG
add 10-15 ul FITC-sheep anti-rabt
incubate 30 min
wash with 30 ml PBS
vash vith 20 ml carbonate bufffer
place filters
in
PBS
incubate 30 min
incubate at 50-60°C
until nearly dry ("30 min)
replace filter
filter with 0.2 ml
on
slides
add 2 drops mounting solution and
over slip
cc
view under blue illumination n
FIG. 1. FA staining proc(edure.
915
rinsed with PBS. At this point in the procedure, filters
of field samples were returned to holders and washed
with PBS. Slight positive pressure was then established by reversing vacuum pump connections; sufficient PBS was added to just submerge the filter, and
then 10 pl of the specific antiserum was added. The
filters were incubated for 30 min and washed with 30
ml of PBS. Positive pressure was reestablished, and
10 to 15 pl of fluorescein isothiocyanate-conjugated
sheep anti-rabbit immunoglobulin G (IgG; Miles Yeda
Ltd., Elkhart, Ind.) was added. The filters were incubated for 30 min and washed with 30 ml of PBS,
followed by 20 ml of 0.5 M carbonate buffer (pH 9.6).
Filters were then placed on clean slides, topped with
2 drops of mounting solution (glycerol-PBS, 9:1 [vol/
vol]), and mounted under a cover slip. FA-stained
slides were viewed with a Zeiss Universal research
microscope using an epifluorescence illuminator with
a 100-W tungsten halogen lamp (10x ocular, 40x
objective). A blue excitation filter (450 to 500 nm) and
a yellow-green fluorescence barrier filter (528 nm)
were used.
Enumeration. Counting efficiency and reliability
of the FA assay were tested by comparing it with two
independent methods of enumeration. Concentrated
pure culture samples were counted using a hemacytometer with Nomarsky optics at 400x magnification.
Dilutions of these samples were counted by the FA
assay described above and by acridine orange direct
counting (17).
RESULTS
The double immunodiffusion tests of the homologous system (N. oceanus, Carlucci isolate,
antigen and its specific anti-N. oceanus antiserum) yielded 10 to 12 precipitin bands. The
Watson isolate and the unidentified Carlucci
isolate no. 5 gave the second and third strongest
reactions for the double immunodiffusion test;
the soil and freshwater ammonium oxidizers also
showed positive reactions (Table 2). The nonammonium-oxidizing autotrophs and the heterotrophs showed little or no response to N.
oceanus antisera. A positive FA reaction was
observed only for the three marine ammoniumoxidizing isolates (Table 2). For controls, the
reactivity of fluorescein isothiocyanate sheep
anti-rabbit IgG was tested against saline solution, pre-immunization serum, and N. oceanus
antiserum; only the specific antiserum gave a
positive fluorescent result.
Auto- and nonspecific fluorescence did not
interfere in FA-stained culture samples, but
were adequately suppressed by bovine serum
albumin. Although a minimal amount of intense
localization of green or orange fluorescence was
often present, the bacteria were easily distinguished by characteristic size and shape. Careful
pretreatment of filters and pH control in washing the filtered samples resulted in a black background which contrasted well with the green
916
APPL. ENVIRON. MICROBIOL.
WARD AND PERRY
fluorescence of the FA-stained cells (Fig. 2).
Auto- and nonspecific fluorescence was more
severe in field samples; several methods of diTABLE 2. Immunodiffusion and FA reactions of
bacterial isolates to N. oceanus antiserum.
Immunodiffusion results were number ofprecipitin
bands formed; FA results were either a strong
fluorescence (+) or no detectable fluorescence (-)
Isolate
Immuno-
diffusion
FA
1. Nitrosococcus oceanus
10-12
+
9-10
5-6
+
3
3-4
-
(Carlucci)
2.
3.
4.
5.
6.
7.
8.
9.
10.
11.
12.
13.
14.
15.
16.
17.
18.
19.
20.
N. oceanus (Watson)
No. 5 (Carlucci)
Nitrosomonas Tara
Nitrosomonas europaea
Nitrosomonas WH-2
Nitrosomonas E-K
14-1
14-2"
14-3a
16-2a
18-2a
18-3a
20-1
20-3a
E. coli
Thiosulfate oxidizer Ml
Nitrobacter agilis
B. gazogenes
4-6
2-4
0
0-1
1-2
1
1
0
1
0
+
-
minishing this unwanted fluorescence were examined since incubation with bovine serum albumin proved ineffective. The procedure of Bohlool and Schmidt (4) was found to be a satisfactory method for attenuating auto- and nonspecific fluorescence; the gelatin coating gave a
nearly black background which allowed easy
detection of fluorescent cells in the presence of
noncellular particulate fluorescence.
The precision of the FA assay as a method for
enumerating ammonium-oxidizing bacteria was
tested by comparing counts of FA-stained cells
with both hemacytometer and acridine orange
cell counts for cell concentrations spanning four
orders of magnitude, and including concentrations likely to be encountered in field samples
(Fig. 3). There was no significant difference (P
> 0.95) from the predicted slope of 1 in the
regression of count data; FA counts gave good
replication (Fig. 3).
-
-
DISCUSSION
Only the marine ammonium-oxidizing isolates
gave a positive reaction with FA staining and
were visually indistinguishable from the homolNDb
ogous Carlucci strain of N. oceanus used to
ND
ND
produce the antibody. Both immunodiffusion
ND
and FA tests gave a positive reaction for the
ND
BV1-SJG
marine ammonium oxidizers but did not give
a Unidentified marine heterotrophs isolated off the identical results for Nitrosomonas isolates (Table 2). Although the FA test is considered genWashington coast.
bND, Not determined.
erally more sensitive than gel diffusion methods
-
-
FIG. 2. FA-stained cells of N. oceanus. Cells appeared bright green, especially at periphery; background
was black. Average cell diameter was 3.3 ,um.
IMMUNOFLUORESCENT ASSAY FOR N. OCEANUS
VOL. 39, 1980
917
-A
U,
z
4
D
0
LL.
3
-J
C,)
-j
w 2
u
-J
5
z
4
0
:3
0
3
-J
-J
2
-J
U)
w
0D-j
2
To be detectable by double immunodiffusion,
the antigen must be capable of both diffusing
through the agarose matrix and forming a precipitate with the antibody. Athough whole-cell
preparations which had been frozen and thawed
*0 e
* were used in the diffusion tests, only the soluble
e
-*@or
solubilized constituents can react. Thus, a
positive reaction by immunodiffusion and a negative one by FA, such as for Nitrosomonas isolates, were likely due to these species having
internal antigens in common with Nitrosococcus
but immunologically very different cell wall antigens.
e
Nitrifying bacteria share a unique pathway of
energy production: the oxidation of reduced nitrogen compounds. The results of our immuno,'"'I,asa
' "Ia
" ' "' 2" ' | ' "
l
logical studies also give support to the biochem3
4
LLOG 2
ical
basis for the systematic classification of amCELLS/ML, PREDICTED
monium-oxidizing bacteria. The strains of marine, freshwater, and soil ammonium oxidizers
we examined did exhibit antigenic similarity in
B
immunodiffusion tests, although the nitrate ox- o
idizer we examined did not (Table 2). Our results
*0*indicated that the nonspecific cross-reactions
observed by immunodiffusion did not contribute
to an FA-positive reaction and that the FA assay
|8°was specific for the detection of Nitrosococcus.
gI
Using the direct FA method, Belser and
Schmidt (2) compared cross-reactions of 16 soil
o@
ammonium-oxidizing strains from four genera.
Of the antibodies prepared from each of the six
strains of Nitrosomonas they tested, only two
were essentially species specific, i.e., did not
react with congeneric strains. The other four
e
strains had significant cross-reactions with each
e
other; i.e., heterologous
tests gave
positive
re-
actions. However, cross-reactions with other related
genera of ammonium-oxidizers were minieaiiIinaI,,,I,a,aI,,,Is IhII
4mal. Because these authors didnot perform gel
LOG
PREDICTED
diffusion tests, the specificity of their antisera
cannot be directly compared with specificity reFIG. 3. Log-log transformed count data showed no sults from immunodiffusion assays
(Table 2).
differe?nce between calculated regressions and preT
The usefulness of the FA assay as a technique
dicted line with slope 1 and intercept 0 (P2 0.95). (A)
FA ve, rsus predicted counts: cells/ml = 0.9761 FA + for enumerating concentrations of nitrifying bac0.0839, ! df= 11, r = 0.9733. (B) Acridine orange versus
teria in the ocean depends on the specificity of
predic ted counts: cells/ml = 1.003 acridine orange the antigenic reaction, the visual resolution of
(AO) 4 0.3874, df = 15, r = 0.9677.
the stained cell from background nonspecific
and autofluorescence, and precision of the actual
(14), our results suggested that the two tests did counting procedure. The antigenic reaction was
not n ecessarily measure the same set of antigens.
found to be specific for the marine ammonium
To d etect an antigen by the FA method used oxidizers tested (Table 2).The inclusion of a
here, the antigen-antibody complex formed by gelatin or bovine serum albumin treatment in
the sr:ecific reaction must be retained on a 0.40- the FA-staining protocol was important in sup,um iuclepore filter. A few outer membrane pressing background fluorescence and in attaincomp onents are important in FA staining of
ing sharp visual resolution of the FA-stained
whole cells (22); soluble cytoplasmic compo- cell. The final carbonate buffer rinse increased
nents are not visible in FA-stained whole cells
absolute fluorescein isothiocyanate fluorescence
and r nay also be lost through the filter if the and enhanced contrast between fluorescent cells
cells rupture during the FA staining procedure.
and background; in addition, the alkaline pH
CELLS/ML3
918
APPL. ENVIRON. MICROBIOL.
WARD AND PERRY
also aided in stabilizing fluorescence so that the
FA-stained filters could be stored for a few weeks
and recounted, if necessary. The results of the
comparison of enumeration methods-of counts
of FA-stained cells with hemacytometer and acridine orange counts-indicated that the FA
technique was both accurate and precise (Fig.
3). Nitrifying bacteria in field samples from the
primary nitrite maximum layer off the coast of
Washington have been identified and enumerated by the FA assay; these results will be reported in a subsequent publication.
ACKNOWLEDGMENTS
This work was conducted in partial fulfillment of the master's degree (for B.B.W.) at the University of Washington.
Thanks are due to S. I. Ahmed, G. C. Anderson, J. I. Hedges,
and G. E. Kenny for their involvement throughout the project
and for comments on the manuscript.
The project was supported by Department of Energy contract E-76-S-06-2225-TA26 #5 (RLO-2225-T26-77) with G. C.
Anderson.
LITERATURE CITED
11.
12.
13.
14.
15.
16.
17.
18.
19.
1. Apel, W. A., P. R. Dugan, J. A. Filppi, and M. S.
2.
3.
4.
5.
6.
7.
8.
9.
10.
Rheins. 1976. Detection of Thiobacillus ferrooxidans
in acid mine by indirect fluorescent antibody staining.
Appl. Environ. Microbiol. 32:159-165.
Belser, W. W., and E. L. Schmidt. 1978. Serological
diversity within a terrestrial ammonia-oxidizing population. Appl. Environ. Microbiol. 32:589-593.
Biebl, H., and N. Pfennig. 1978. Growth yields of green
sulfur bacteria in mixed cultures with sulfur and sulfate
reducing bacteria. Arch. Microbiol. 117:9-16.
Bohlool, B. B., and E. L. Schmidt. 1968. Non-specific
staining: its control in immunofluorescence examination
of soil. Science 162:1012-1014.
Bohlool, B. B., and E. L. Schmidt. 1973. A fluorescent
antibody technique for determination of growth rates
of bacteria in soil. Bull. Ecol. Res. Comm. (Stockholm)
17:336-338.
Carlucci, A. F., E. 0. Hartwig, and P. M. Bowes. 1970.
Biological production of nitrite in seawater. Mar. Biol.
7:161-166.
Carlucci, A. F., and P. M. McNally. 1969. Nitrification
by marine bacteria in low concentrations of substrate
and oxygen. Limnol. Oceanogr. 14:736-739.
Carlucci, A. F., and D. Pramer. 1957. Factors influencing the plate method for determining abundance of
bacteria in sea water. Proc. Soc. Exp. Biol. Med. 96:
392-394.
Carlucci, A. F., and H. R. Schubert. 1969. Nitrate
reduction in seawater of the deep nitrite maximum off
Peru. Limnol. Oceanogr. 14:187-193.
Carlucci, A. F., and J. D. H. Strickland. 1968. The
isolation, purification and some kinetic studies of ma-
20.
21.
22.
23.
24.
25.
26.
27.
28.
29.
rine nitrifying bacteria. J. Exp. Mar. Biol. Ecol. 2:156166.
Fiadeiro, M., and J. D. H. Strickland. 1968. Nitrate
reduction and the occurrence of a deep nitrite maximum
in the ocean off the west coast of South America. J.
Mar. Res. 26:187-201.
Fliermans, C. B., B. B. Bohlool, and E. L. Schmidt.
1974. Autecological study of the chemoautotroph Nitrobacter by immunofluorescence. Appl. Microbiol. 27:
124-129.
Goering, J. J. 1968. Denitrification in the oxygen minimum layer of the eastern tropical Pacific Ocean. DeepSea Res. 15:157-164.
Haaijmann, J. J., F. J. Bloemmen, and C. M. Ham.
1977. Microfluorometric immunoassays with antigens
bound to sepharose beads. Ann. N.Y. Acad. Sci. 254:
137-149.
Hattori, A. 1962. Light-induced reduction of nitrate, nitrite and hydroxylamine in a blue-green alga, Anabaena
cylindrica. Plant Cell Physiol. (Tokyo) 3:355-369.
Hattori, A., and E. Wada. 1971. Nitrite distribution and
its regulating processes in the equatorial Pacific Ocean.
Deep-Sea Res. 18:557-568.
Hobbie, J. E., R. J. Daley, and S. Jasper. 1977. Use of
Nuclepore filters for counting bacteria by fluorescence
microscopy. Appl. Environ. Microbiol. 33:1225-1228.
Kenny, G. E. 1971. Immunogenicity of Mycoplasma
pneumoniae. Infect. Immun. 3:510-515.
Lowry, 0. H., N. J. Rosebrough, A. L. Farr, and R. J.
Randall. 1951. Protein measurement with the Folin
phenol reagent. J. Biol. Chem. 193:265-275.
Martinsen, C. S., and P. K. Zachariah. 1978. Growth of
various bacteria on polycyclic aromatic hydrocarbons
and n-2-fluorenylacetamide. J. Appl. Bacteriol. 44:365371.
Miyazaki, T., E. Wada, and A. Hattori. 1973. Capacities
of Sagami Bay for oxidation and reduction of inorganic
nitrogen. Deep-Sea Res. 20:571-577.
Moller, G. 1961. Demonstration of mouse isoantigens at
the cellular level by the fluorescent antibody technique.
J. Exp. Med. 114:415-434.
Ouchterlony, 0. 1949. Antigen-antibody reactions in gels.
Ark. Kemi Mineral. Geol. B26:1.
Reed, W. M., and P. R. Dugan. 1978. Distribution of
Methylomonas methanica and Methylosinus trichosporium in Cleveland Harbor as determined by an indirect
fluorescent antibody-membrane filter technique. Appl.
Environ. Microbiol. 35:422-430.
Schmidt, E. L., R. 0. Bankole, and B. B. Bohlool.
1968. Fluorescent-antibody approach to study of rhizobia in soil. J. Bacteriol. 95:1987-1992.
Soriano, S., and N. Walker. 1968. Isolation of ammonia
oxidizing autotrophic bacteria. J. Appl. Bacteriol. 31:
493-497.
Vacarro, R. F., and J. H. Ryther. 1960. Marine phytoplankton and the distribution of nitrite in the sea. J.
Cons. Perm. Int. Explor. Mer 25:260-271.
Vishniac, W., and M. Santer. 1957. The thiobacilli.
Bacteriol. Rev. 21:195-214.
Watson, S. W. 1965. Characteristics of a marine nitrifying
bacterium, Nitrosocystis oceanus sp. n. Limnol. Oceanogr. 10:R274-289.