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Applied and Environmental Microbiology, April 2000, p. 1692-1697, Vol. 66, No. 4
0099-2240/00/$04.00+0
Copyright © 2000, American Society for Microbiology. All rights reserved.
Natural Assemblages of Marine Proteobacteria and
Members of the Cytophaga-Flavobacter Cluster Consuming Low-
and High-Molecular-Weight Dissolved Organic Matter
Matthew T.
Cottrell and
David L.
Kirchman*
College of Marine Studies, University of
Delaware, Lewes, Delaware 19958
Received 23 September 1999/Accepted 12 January 2000
 |
ABSTRACT |
We used a method that combines microautoradiography with
hybridization of fluorescent rRNA-targeted oligonucleotide probes to
whole cells (MICRO-FISH) to test the hypothesis that the relative contributions of various phylogenetic groups to the utilization of
dissolved organic matter (DOM) depend solely on their relative abundance in the bacterial community. We found that utilization of even
simple low-molecular-weight DOM components by bacteria differed across
the major phylogenetic groups and often did not correlate with the
relative abundance of these bacterial groups in estuarine and coastal
environments. The Cytophaga-Flavobacter cluster was
overrepresented in the portion of the assemblage consuming chitin,
N-acetylglucosamine, and protein but was generally
underrepresented in the assemblage consuming amino acids. The amino
acid-consuming assemblage was usually dominated by the
subclass of
the class Proteobacteria, although the representation of
-proteobacteria in the protein-consuming assemblages was about that
expected from their relative abundance in the entire bacterial
community. In our experiments, no phylogenetic group dominated the
consumption of all DOM, suggesting that the participation of a diverse
assemblage of bacteria is essential for the complete degradation of
complex DOM in the oceans. These results also suggest that the role of aerobic heterotrophic bacteria in carbon cycling would be more accurately described by using three groups instead of the single bacterial compartment currently used in biogeochemical models.
 |
TEXT |
Analysis of 16S rRNA gene sequences
(15) has greatly advanced our understanding of the
phylogenetic diversity of bacteria and archaea (18),
especially that of the vast majority of microbes in nature that have
resisted cultivation to date (2). There is little
information, however, on the metabolic function of specific bacterial
groups in natural assemblages since few culture-independent studies
have linked bacterial community structure and function (6).
Although information on phylogenetic relationships of uncultured
bacteria is readily accessible (14), the inability to
culture most microbes limits the opportunities to assess their metabolic diversity. Even if appropriate culture conditions were to be
found for the bulk of marine microbes, bacterial metabolism in the sea
would probably remain poorly described, since metabolic behavior in
culture is likely different from that in situ.
Extensive biogeochemical studies have shown that uptake and
mineralization of dissolved organic matter (DOM) by bacteria constitute a major component of carbon cycling in aquatic ecosystems
(11). Although the importance of DOM uptake is well
recognized, the relative contributions of the major phylogenetic groups
of bacteria to DOM uptake in the oceans are unknown (29).
Differences in usage of various DOM components may help explain the
distribution of the major bacterial groups among soil, freshwater, and
marine ecosystems (18). It may also be important to know the
minimum number of bacterial phylogenetic groups necessary to describe and explain DOM uptake in order to improve models of carbon cycling in
aquatic habitats. Currently these models implicitly assume that all
heterotrophic bacteria are the same and consist of a single
phylogenetic type (12).
The goal of this study was to determine whether the relative
contributions of various phylogenetic groups to the utilization of DOM
depend solely on their relative abundance in the bacterial community.
We used a novel approach, combining microautoradiography and
fluorescence in situ hybridization (MICRO-FISH) (22, 28) to
determine DOM uptake by the bacterial divisions and subclasses typically comprising marine assemblages (16). Since the
chemical composition and degradation of DOM differ as a function of
molecular weight (3, 4), different groups of bacteria may be
responsible for mineralizing low- and high-molecular-weight DOM. We
hypothesized that all heterotrophic bacteria use low-molecular-weight
DOM, specifically monomers that can be transported easily across cell membranes. High-molecular-weight DOM, on the other hand, may be consumed by a smaller, less-diverse group of bacteria since specific extracellular enzymes are required for the hydrolysis of biopolymers, a
component of high-molecular-weight DOM. To test these hypotheses, we
used MICRO-FISH to compare utilization of protein and chitin by various
phylogenetic groups with their utilization of amino acids and
N-acetylglucosamine (NAG). Protein and chitin were chosen because they represent potentially large components of
high-molecular-weight DOM (25).
Sample collection and incubation.
Seawater was collected from
the Delaware Bay estuary at the Roosevelt Inlet (salinity [S] = 30 ppt, temperature [T] = 14°C) and from the Atlantic Ocean at the
Indian River Inlet (S = 32 ppt, T = 12°C) in November and
December, respectively. Aliquots were incubated at 12 to 19°C and
tritiated amino acids, NAG, protein, and chitin were added. The final
concentrations of the amino acid mixture (47 Ci/mmol; Amersham) and NAG
(9.9 Ci/mmol; Amersham) additions were 2.1 and 10 nM, respectively.
Soluble chitin oligomers were prepared by mild acid hydrolysis (3 N
HCl, 70°C, 5 min) of tritiated chitin purified from the marine fungus
Paeosphaeria spartinicola (27) grown on medium
containing [3H]NAG (21). Tritiated protein was
prepared from Vibrio alginolyticus grown on medium
containing [3H]leucine (26). Subsamples were
filtered through 0.2-µm-pore-size polycarbonate filters to measure
the uptake of radiolabeled compounds in incubations lasting 1 to
26 h. Amino acid incubations were for 1 h, the protein
incubation with the assemblage from Roosevelt Inlet lasted 26 h,
and the remaining incubations were for 7 h. Bacterial abundance
was measured by determining 4',6'-diamidino-2-phenylindole (DAPI)
direct counts (30).
MICRO-FISH.
Samples were prepared for MICRO-FISH by using a
variation of methods combining microautoradiography and fluorescence in
situ hybridization. Unlike substrate-tracking autoradiographic
fluorescent in situ hybridization (28), but similar to the
protocol of Lee et al. (22), cells were transferred to glass
coverslips and probed with fluorescent oligonucleotides before being
coated with an autoradiographic film emulsion. After incubation with
tritiated compounds, samples were fixed with formaldehyde, subsamples
for MICRO-FISH were filtered through 0.2-µm-pore-size polycarbonate filters, and the cells were transferred to glass coverslips freshly treated with a 2% solution of 3-aminopropyltriethoxysilane (Sigma) (5). Immediately after filtration, the polycarbonate filter was placed face down on a coverslip, clamped together between two glass
slides by the use of a large paper clip, and incubated for 1 h at
42°C. The filter was then peeled away, and the cells were dehydrated
by passing the coverslip through a series of ethanol rinses and then
air dried. Unlike the protocol of Lee et al. (22), our
method does not require a special slide with a hole for viewing cells
attached to the back of the coverslip.
In situ hybridization was done by placing the cell-adherent side of the
coverslip in contact with a 30-µl drop of hybridization solution
containing 2 ng of probe/µl in the bottom of a polystyrene petri
dish. The probes used were as follows: for bacteria, Eub338 (positive
control) (1); for
-proteobacteria, Alf1b (24); for
-proteobacteria, Bet42a (24); for
-proteobacteria,
Gam42a (24); for the Cytophaga-Flavobacter
cluster of the Cytophaga-Flavobacter-Bacteroides division,
CF319a (23); and for gram-positive bacteria with high DNA
G+C content, HGC69a (32). The dish was sealed with Parafilm and incubated at 42°C for 2 h, after which the coverslip was
incubated for 30 min at 48°C in a wash solution containing NaCl at a
concentration appropriate for the probe (34). The coverslip
was then rinsed in deionized water, air dried, and mounted (by the use
of immersion oil) on a glass slide with the cell-adherent side of the
coverslip facing away from the slide.
Samples were prepared for microautoradiography by dipping the glass
slide, with coverslip attached, into a molten (43°C) NBT-2
emulsion
(Kodak) diluted to 2 parts emulsion and 1 part deionized
water. After
incubation at

20°C for 2 days, the slides were warmed
to room
temperature and the photographic emulsion was developed
by using Dektol
developer (Kodak), a deionized-water stop bath,
and fixer (Kodak) in
accordance with the manufacturer's instructions.
The slide was stained
in a 2-µg/ml solution of DAPI for 2 min,
dipped in deionized water,
and air dried. The coverslip was removed
from the glass slide and
mounted on a clean glass slide with the
cells facing the slide, using
Citifluor (Ted Pella Inc., Redding,
Calif.). Cells were examined by
using a fluorescence microscope
fitted with filter sets for DAPI (UV1A;
Nikon) and Cy3 (41007A;
Chroma). The average level of retention of
cells on the coverslip
through all steps of the procedure was 103%, as
determined by
DAPI counts of bacteria on black polycarbonate filters
(
30).
Phylogenetic groups consuming DOM compounds.
MICRO-FISH identifies bacteria that have taken up tritiated
compounds by determining the presence of silver grains adjacent to
cells (Fig. 1). The phylogenetic
classification of cells is determined by the binding of rRNA-targeted
oligonucleotide probes conjugated to the yellow-fluorescing
fluorochrome Cy3 (Fig. 1B). The sample shown in Fig. 1 was prepared by
using tritiated amino acids typically consumed by a large fraction of
cells (10, 19) and a positive-control probe complementary to
a region of the 16S rRNA conserved in most bacteria (Eub338)
(1), so all bacteria consuming free amino acids and having
sufficient numbers of ribosomes are visible. The eubacterial probe
detected on average 80% (standard deviation, 9.0) of the bacterial
abundance determined by DAPI direct counts.

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FIG. 1.
Micrograph of bacteria assayed by MICRO-FISH. (A)
DAPI-stained bacteria (UV excitation). Dark spots surrounding cells are
silver grains deposited in photographic emulsion around cells that took
up a mixture of tritiated free amino acids. Less than 0.6% of cells in
formaldehyde-killed controls had silver grains. (B) Bacteria hybridized
with Cy3-labeled oligonucleotide probe Eub338 for eubacteria (green
excitation). Cells with bound probe fluoresce yellow. Magnification,
×1,350.
|
|
Bacterial assemblages in Delaware estuarine and coastal waters were
dominated by proteobacteria and members of the
Cytophaga-Flavobacter cluster (Fig.
2A and
3A).
Proteobacteria, and to a lesser extent
the
Cytophaga-Flavobacter cluster, are typically abundant in
aquatic
systems (
31,
33). Three subclasses of proteobacteria
(

,

,
and

) were about equally abundant in the coastal sample,
while

-proteobacteria were most abundant in the estuarine sample.
The
relatively large abundance of members of the
Cytophaga-Flavobacter cluster may be a consequence of high
particle loads in these environments;
studies inferring community
composition from libraries of cloned
16S rRNA genes amplified by PCR
have found that this group is
enriched on particles (
9).
However, Glöckner et al. (
16),
using fluorescence in
situ hybridization, found that a large abundance
of bacteria in the
Cytophaga-Flavobacter cluster may be common
in marine
systems. Cells binding the probe for gram-positive bacteria
accounted
for less than 3% of the direct count, which is not significantly
different from counts of autofluorescent cells in controls without
a
probe. The probes for

-,

-, and

-proteobacteria and the
Cytophaga-Flavobacter cluster detected 70% (standard
deviation, 30) of the bacteria
visualized with the control probe
(Eub338) for all bacteria (Fig.
2A and
3A).

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FIG. 2.
Community composition and consumption of chitin, NAG,
protein, and amino acids by the major phylogenetic groups of
bacterioplankton in the Roosevelt Inlet, assayed by MICRO-FISH. (A)
Composition of bacterioplankton communities in incubations containing
tritiated compounds. (B) Relative abundance of phylogenetic groups of
bacteria consuming various tritiated compounds. Less than 3% of the
cells were gram positive. Cells binding none of the group-specific
probes are indicated (Not identified). Percentages were calculated
relative to total bacteria counted by using DAPI, although the
eubacterial probe (Eub338) detected on average 80% of bacterial
abundance. proteobact., proteobacteria; Flavobact.,
Flavobacter.
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|

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FIG. 3.
Community composition and consumption of chitin, NAG,
protein, and amino acids by the major phylogenetic groups of
bacterioplankton in the Indian River Inlet, assayed by MICRO-FISH. (A)
Composition of bacterioplankton communities in incubations containing
tritiated compounds. (B) Relative abundance of phylogenetic groups of
bacteria consuming various tritiated compounds. Less than 3% of the
cells were gram positive. Cells binding none of the group-specific
probes are indicated (Not identified). Percentages were calculated
relative to total bacteria counted by using DAPI, although the
eubacterial probe (Eub338) detected on average 80% of the bacterial
abundance.
|
|
Consumption of organic compounds differed among the phylogenetic
groups. Even uptake of low-molecular-weight DOM differed
greatly among
groups. The
Cytophaga-Flavobacter cluster accounted
for the
largest fraction of bacteria consuming chitin, NAG, and
protein but was
the smallest fraction consuming amino acids (Fig.
2B and Fig.
3B). In
contrast,

-proteobacteria comprised the largest
fraction of the
community consuming amino acids but the smallest
fraction consuming
protein. Differences between amino acid consumption
by

-proteobacteria and by members of the
Cytophaga-Flavobacter cluster occurred in both estuarine and
coastal environments (Fig.
2B and
3B), but consumption of amino acids
by these two groups
in the San Pedro Channel off the California coast
did not differ
(
28). In the San Pedro Channel, these two
groups were equally
abundant and about 80% of the cells in each group
actively took
up amino
acids.
Although a large (>50%) fraction of bacteria sometimes could not be
identified with the four group-specific probes used in
this study (Fig.
2A and
3A), usually only a small fraction (<20%)
of the bacteria
actively taking up the various
3H-labeled compounds
remained unidentified (Fig.
2B and
3B). The
single exception occurred
in the estuarine experiment examining
chitin utilization. Nearly 40%
of the bacteria assimilating
3H-chitin oligomers could not
be assigned to one of the four phylogenetic
groups examined (Fig.
2B).
There was no fixed relationship between utilization of polymers and
their constituent monomers by different phylogenetic groups.
The same
phylogenetic groups accounted for most of the cells consuming
chitin
and NAG, but protein and amino acids were largely consumed
by different
phylogenetic groups. Members of the
Cytophaga-Flavobacter cluster accounted for 30 and 47% of the community consuming chitin
and
NAG, respectively, and

-proteobacteria accounted for 22 and
45% of
the cells consuming these compounds, respectively. In contrast,
the
Cytophaga-Flavobacter cluster accounted for 45% of the
cells
consuming protein but only 3% of the cells consuming amino
acids,
while

-proteobacteria accounted for 45% of the cells
consuming
amino acids but only 10% of the cells consuming
protein.
Composition and activity of bacterial assemblages.
The
distributions of
- and
-proteobacteria are among the most
striking features of microbial diversity in aquatic environments. Although these two groups coexist in coastal environments
(31),
-proteobacteria are not found in the oligotrophic
ocean but are abundant in freshwater habitats, where they seem to
displace
-proteobacteria (16, 17). Variations in the
supply and composition of DOM in freshwater versus marine systems
(3, 13) may determine the distribution of
- and
-proteobacteria if these two groups differ in the capacity to
utilize various DOM components. Our hypothesis is based on the
observation that growth of the total bacterial community is often
limited by the availability of DOM (7, 8, 20). An
alternative hypothesis is that
- and
-proteobacteria use the same
compounds present in both oceanic and freshwater environments and that
-proteobacteria are restricted from the oligotrophic ocean by a
selection factor other than DOM.
Our results suggest that

- and

-proteobacteria are similar with
respect to DOM consumption. These two groups comprised the
smallest
fraction (15% or less) of bacteria consuming chitin and
NAG, and they
accounted for 19 to 29% of the cells consuming protein
and amino
acids. This analysis suggests that the availability
of DOM does not
explain the distributions of

- and

-proteobacteria
in aquatic
environments.
The relative abundance of phylogenetic groups of bacteria in
assemblages consuming various DOM components often differed from
their
relative abundance in the assemblage as a whole. The
Cytophaga-Flavobacter cluster was overrepresented in the
portion of the assemblage consuming
chitin (Fig.
4A), NAG (Fig.
4B), and protein (Fig.
4C). Among
the cells identified by the bacterial probe (Eub338), the
Cytophaga-Flavobacter cluster comprised 23 to 55% of the
cells consuming chitin, NAG,
and protein, but these bacteria made up
only 8 to 38% of the assemblage
(Fig.
4A to C). In contrast, the
Cytophaga-Flavobacter cluster
was greatly underrepresented
in the assemblage consuming amino
acids (Fig.
4D), accounting for only
2 to 4% of the amino acid-consuming
bacteria. All three subclasses of
proteobacteria were equally
or underrepresented among bacteria
consuming chitin (Fig.
4A),
but their participation in protein usage
was less clear. Protein
use by

-proteobacteria was about that
expected from their relative
abundance in the total bacterial
community, while

- and

-proteobacteria
were over and
underrepresented among the bacteria consuming protein
in the two
environments sampled in this study (Fig.
4C). The
and

subclasses of proteobacteria comprised a small portion of
the
assemblage (<10%) consuming NAG relative to their abundance
(10 to
25%) (Fig.
4B). Uptake of amino acids differed greatly
among the three
subclasses of proteobacteria and between experiments.
The percentage of
amino acid-consuming bacteria that were proteobacteria
sometimes was
greater than, equal to, and less than their contribution
to total
bacterial abundance (Fig.
4D).

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FIG. 4.
Relationship among the phylogenetic classifications of
bacteria consuming chitin (A), NAG (B), protein (C), and amino acids
(D) versus phylogenetic classification of cells identified as
eubacteria. Bacteria were classified by using rRNA-binding
oligonucleotide probes specific for -proteobacteria ( ),
-proteobacteria ( ), -proteobacteria ( ), and the
Cytophaga-Flavobacter group (C). Data points
falling above the 1:1 line indicate phylogenetic groups enriched in the
portion of the assemblage consuming the compound. Results are from
coastal (Fig. 2) and estuarine (Fig. 3) environments. Percentages were
calculated relative to the numbers of cells identified as eubacteria
with the Eub338 probe.
|
|
Changes in community structure due to protein addition were consistent
with the MICRO-FISH results. Addition of protein in
the Roosevelt Inlet
experiment caused a large increase in the
abundance of the same
bacterial groups revealed by MICRO-FISH
to consume protein.

-Proteobacteria initially dominated the community
(27% of the
total), but after incubation with protein, bacteria
in the
Cytophaga-Flavobacter cluster were the most abundant (35%
of the community) and

-proteobacteria were the least abundant
(Fig.
2A). MICRO-FISH indicated that 45% of the cells consuming
protein were
members of the
Cytophaga-Flavobacter cluster and
that only
2% were

-proteobacteria (Fig.
2B).
Cytophaga-Flavobacter cluster members did not dominate protein consumption simply because
they grow rapidly in bottle incubations while

-proteobacteria
grow
slowly. In a shorter incubation with an assemblage from the
Indian
River Inlet, there was no shift in the community composition
(Fig.
3A).
MICRO-FISH again revealed that members of the
Cytophaga-Flavobacter cluster accounted for most of the
cells consuming protein and
that

-proteobacteria accounted for the
smallest fraction (Fig.
3B).
In revealing the differences in DOM uptake by the various heterotrophic
bacteria, this study indicates the need to consider
more than a single
compartment for modeling the role of heterotrophic
bacteria in carbon
cycles. However, our results also suggest that
models may not require
inclusion of the entire diverse spectrum
of organisms found by
culture-independent studies (
15,
18).
We found that, with
one exception, all of the bacteria assimilating
DOM components could be
assigned to one of the four phylogenetic
groups examined, although
other bacterial groups undoubtedly assimilate
some DOM. Furthermore,
since

-proteobacteria are not commonly
found in oceans (
16,
18), and in any case their activity seems
similar to that of

-proteobacteria, it appears that uptake of
DOM may be explained by
three bacterial groups, with properties
represented by

- and

-proteobacteria and the
Cytophaga-Flavobacter cluster.
Our generalization about DOM uptake, however, may not
apply to other
environments (e.g., soils), where these three phylogenetic
groups
probably have different metabolic
capacities.
In general, the number of groups required to describe relationships
between bacterial community structure and function is
unclear. The
phylogenetic level on which to focus is also not
obvious. In our study,
we found that consumption of DOM could
be explained using a relatively
small number of phylogenetic groups
(at most four) at the division and
subclass levels. Understanding
other structure-function relationships,
however, may require examining
a larger number of more closely related
phylogenetic groups. For
example, temporal shifts in DOM consumption
might be explained
at the family or genus level, and more bacterial
groups may be
necessary for explaining DOM uptake in aquatic
environments (e.g.,
oligotrophic oceans) that differ greatly from the
eutrophic waters
of our study. Although more data are clearly needed,
our study
suggests that comparing DOM consumption across environments
at
the division and proteobacterial-subclass levels will enhance
our
understanding of this structure-function relationship in marine
bacterial
communities.
 |
ACKNOWLEDGMENTS |
This research was supported by the U.S. Department of Energy.
 |
FOOTNOTES |
*
Corresponding author. Mailing address: College of
Marine Studies, University of Delaware, 700 Pilottown Rd., Lewes, DE
19958. Phone: (302) 645-4375. Fax: (302) 645-4028. E-mail:
kirchman{at}udel.edu.
 |
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