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Microbiology and Molecular Biology Reviews, September 2005, p. 440-461, Vol. 69, No. 3
1092-2172/05/$08.00+0 doi:10.1128/MMBR.69.3.440-461.2005
Copyright © 2005, American Society for Microbiology. All Rights Reserved.
Fate of Heterotrophic Microbes in Pelagic Habitats: Focus on Populations
Jakob Pernthaler* and
Rudolf Amann
Max Planck Institute for Marine Microbiology, Bremen, Germany

SUMMARY
Major biogeochemical processes in the water columns of lakes
and oceans are related to the activities of heterotrophic microbes,
e.g., the mineralization of organic carbon from photosynthesis
and allochthonous influx or its transport to the higher trophic
levels. During the last 15 years, cultivation-independent molecular
techniques have substantially contributed to our understanding
of the diversity of the microbial communities in different aquatic
systems. In parallel, the complexity of aquatic habitats at
a microscale has inspired research on the ecophysiological properties
of uncultured microorganisms that thrive in a continuum of dissolved
to particulate organic matter. One possibility to link these
two aspects is to adopt a "Gleasonian" perspective, i.e., to
study aquatic microbial assemblages in situ at the population
level rather than looking at microbial community structure,
diversity, or function as a whole. This review compiles current
knowledge about the role and fate of different populations of
heterotrophic picoplankton in marine and inland waters. Specifically,
we focus on a growing suite of techniques that link the analysis
of bacterial identity with growth, morphology, and various physiological
activities at the level of single cells. An overview is given
of the potential and limitations of methodological approaches,
and factors that might control the population sizes of different
microbes in pelagic habitats are discussed.

INTRODUCTION
Units of Interest: Single Microbial Populations
Molecular biological methods centered on the rRNA gene have
developed into powerful tools for the cultivation-independent
identification of aquatic microorganisms. Over the last decades,
the composition and diversity of microbial assemblages in numerous
marine and freshwater environments have been studied by 16S
rRNA gene cloning and sequencing (
55,
76,
85,
91,
121,
303),
community fingerprinting (
36,
49,
156,
185,
254), hybridizations
with oligo- or polynucleotide probes (
2,
89,
136,
188,
218),
or by combinations of these approaches (
63,
144,
223,
266,
278).
A major goal of aquatic microbial ecology is to understand the specific roles of different microorganisms as mediators of element fluxes, e.g., during the remineralization of nutrients and organic carbon. So far, the novel molecular approaches have focused mainly on the occurrence and evolutionary relatedness of different bacteria, archaea, and picoeukaryotes. Clearly, there is a need to progress beyond a mere descriptive analysis of microbial diversity and community structure, to provide information about which microbes are involved in various biogeochemical processes. An integration of the more diversity-centered and the more biogeochemical perspectives in microbial ecology has been sought in the concept of the "structure and function" of microbial assemblages (73, 256). Such terminology might be fully appropriate for the study of technologically designed environments that serve particular functions, e.g., wastewater treatment plants, of coherent physiological groups, or of habitats like sediments or biofilms that feature a rigid physical structure (37, 257, 308). However, the concept of "structure and function" appears to overemphasize the "bottom-up" aspect of aquatic microbial assemblages, i.e., aspects that are related to microbial substrate and nutrient utilization. Pelagic habitats are also zones of high microbial mortality, and a substantial fraction of bacterial biomass may be transferred to higher trophic levels by predation (272). In order to understand the different heterotrophic microbes that inhabit the marine and freshwater plankton, it might thus be more adaeqate to consider both the specific "role" and the "fate" of microbial populations.
In many respects "aquatic microbial communities" are theoretical concepts rather than biologically real entities with (physical) structure, common genome or evolutionary history (66). Although ultimately there might be community assemblage rules also for the aquatic microbes (118), bacterioplankton assemblages could likewise be regarded as more or less loose collections of individual genotypic populations that change over time in features such as growth, mortality, and size. Here we discuss the advantages of adapting such a "Gleasonian" viewpoint (87), i.e., we focus on distinct bacterial populations that can be reliably identified and quantified in aquatic assemblages rather than on microbial community structure, diversity, or function as a whole. Specifically, we review current methodological approaches, and we assemble information about the occurrence, the phenotypic properties, and the possible role and fate of such defined microbial populations in the water column.
Marine Autotrophic Picoplankton as a Model
The advantages of a focus on single microbial populations can
be illustrated by looking at autotrophic marine picoplankton.
Prochlorococcus is an ubiquitous free-living phototrophic cyanobacterial
genus that is common in temperate to tropical marine waters
(
205), where it may account for a high fraction of total primary
production. This group was only discovered in 1989 by means
of a then-novel technology, flow cytometry (
38). The ability
to reliably distinguish
Prochlorococcus populations from other
species of autotrophic marine picoplankton (e.g.,
Synechococcus)
has resulted in concerted research about the ecology, physiology,
and genomic constitution of these organisms that is unparalleled
in aquatic microbial ecology. During the past 15 years, numerous
strains of
Prochlorococcus from various locations have been
isolated and studied in the laboratory (
205). The geographic
distribution limits and the contrasting vertical niches of physiologically
distinct genotypes have been established (
67,
205,
314). Recently,
the capacity of
Prochlorococcus to heterotrophically utilize
organic nitrogen sources has been described both in situ (
327)
and as a feature of its genome (
246). The successful unraveling
of the functional role of this particular bacterial group based
on its reliable in situ identification might also provide a
conceptual model for the study of heterotrophic microbes in
the water column.
Microbial Phenotypes
Major biogeochemical processes in the water column are related
to the activities of heterotrophic microbes, e.g., the mineralization
of organic carbon from photosynthesis or its transport to higher
trophic levels (
13). This is deduced from bulk measurements
of microbial growth, respiration, the rates of biomass production,
and its loss to predation or to viral lysis (
53,
74,
77,
142,
270). Such bulk parameters sum up the potentially different
rates of cell replication and mortality of various microbial
species. While this may be essential to follow the fate of organic
matter as a whole, it has also separated aquatic microbial ecology
from other fields of microbiology that insist on well-identified
microorganisms as the basic units of research. During the last
decade the complexity of microbial phenotypes has moved into
the focus of research that aims to explain biogeochemical processes.
Our view of microbes as mediators of element flow has matured
from the black-box approach of the early food web models to
a subtler understanding of the ecophysiology of organisms that
thrive in a heterogenous environment of dissolved and particulate
organic matter (
12).
The diversity of phenotypes within aquatic microbes reflects the complexity of the habitats at a microscale (3, 106, 206, 281). For example, a large fraction of cells in coastal bacterioplankton may be motile during particular seasons or times of the day, and the duration of their actual swimming periods may be affected by substrate availability and patchiness (103). This might be related to chemosensory functions that allow bacteria to actively accumulate in substrate-rich microniches such as the phycosphere of senescent algae (15, 23). The balance between particle colonization efficiencies and detachment dynamics may even reflect species-specific microbial life cycles (100, 140, 141). Culturable genera of aquatic bacteria harbor large numbers of facultative anaerobes, and ten percent of bacteria in oxic coastal marine waters could incorporate glucose both at oxic and at anoxic conditions (4, 243). Some strains isolated from the plankton are capable of degrading complex organic molecules or of utilizing organic sulfur compounds (94, 95). Other aquatic bacteria differ in the duration of the lag phase that precedes growth in batch culture (212), exhibit high tolerance to UV radiation (290), secrete or resist antibiotics (61, 161), or are capable of cell communication by quorum sensing (97). In addition, indications of microbial activity are found in the water column that presently cannot be assigned to particular bacterial groups, e.g., microbial exoenzymes with contrasting kinetic properties (9, 307).
Aquatic microbes have moreover developed a range of specific defense strategies. Some freshwater bacteria form threadlike morphotypes or microcolonies that secrete large amounts of exopolymerous substances, thereby obtaining protection against ingestion by bacterivorous protists (113, 223). In coastal North Sea surface waters >25% of prokaryotes were covered by a polysaccharidic capsule, a feature of many pathogenic species (288) which again might be related to grazing resistance. A high percentage of bacteria in different freshwaters are gram-positive (263), which enhances their protection against digestion by unicellular eukaryotes (114, 125).
However, one must not conceptually merge distinct microbial species into fictional chimeric "aquatic bacteria" (Fig. 1). More appropriately, the various phenotypic features should be regarded as individual elements of unique life strategies that explain the occurrence and distribution patterns of different genotypes in aquatic habitats. Some of these phenotypic features, such as motility or filament formation, may be widespread across very different phylogenetic lineages (115), whereas others, e.g., antibiotic production or resistance, may be highly characteristic for particular species or genera (100, 160). A single genotype may express a variety of phenotypic features or even phenotypic plasticity (90, 115), and identical features may be shared by numerous genotypes. Thus, a central task of microbial ecology is to assign the various physiological abilities and phenotypes observed in situ to particular microbial species or genotypes.
Operational Phylogeny-Based Definition of Microbial Populations
It is still the subject of debate whether there can be a natural
species concept in microbiology (
41,
248). Therefore, a definition
of "populations" in field investigations of microbial ecology
should be more flexible than, e.g., for laboratory studies of
ecophysiology or evolution (
27,
64,
128). In our view, which
is shaped by the available tools and the lack of information
about the ecology of 16S rRNA-defined populations in the environment,
almost any phylogenetically coherent group of microbes could
potentially qualify as a "meaningful" population. The phylogenetic
resolution that adequately delineates microbial populations
largely depends on the ecological goals of a specific investigation.
A meaningful population should represent a unit that (i) is
recognizable in subsequent investigations and (ii) exhibits
ecologically distinct features from other recognizable units
(Fig.
2).
Such genotypically defined populations with a shared set of
phenotypic and ecological properties ideally might be single
ecotypes sensu Cohan (
41) or almost identical clusters of 16S
rRNA sequence types (
1), e.g., the marine DE2 (
144) and NOR5
(
63), or the freshwater LD2 (
223,
328) clades. However, larger
entities may also represent meaningful populations, i.e., 16S
rRNA-based clades of sequence types such as the marine
Roseobacter (
63), SAR11 (
188), and SAR202 (
189) clusters or the freshwater
BET1 (
278), BET2 (
35), or AcI lineages (
309). Occasionally it
may even be sufficient to differentiate by subphylum (
47,
89)
or domain (
136).
The distinction of genotypic compartments within mixed microbial assemblages helps to compile ecologically relevant information about the abundances and activities of phylogenetically closely related groups of microorganisms, e.g., about their horizontal or vertical distribution patterns (210, 295), seasonality (63, 136), occurrence on particles (261), cell morphology (223), growth response to confinement (61, 72, 254), sensitivity to predation (16), incorporation of particular substrates (47, 169, 306), or growth under anoxic conditions (4). Our conceptual framework thus encompasses investigations of the seasonal occurrence of pathogenic Vibrio spp. in coastal waters (83, 117), of the response of a specific clade of freshwater betaproteobacteria to food web manipulations (278), but also of the differences in the vertical distribution of Bacteria and Archaea in the open ocean (136). On the other hand, it may also refer to the relative contributions of genotypic populations to a single biogeochemical process, e.g., the roles of planktonic members of the Roseobacter or SAR11 lineage in sulfur cycling (96, 169, 170, 306, 323).
It should be noted that a microbial population that is defined above the level of the single clone might represent an operational rather than a natural category. Therefore, such an operational taxonomic unit will be limited in its usefulness to a particular study context, and it should be refined or expanded if found inadequate for a specific purpose (Fig. 2). Some phylogenetic clades might harbor organisms with closely related or even identical 16S rRNA gene sequences but rather different ecophysiological properties (128). Sometimes it may be useful to merge such strains into larger categories, e.g., to study the occurrence of genera associated with particular phytoplankton blooms (96, 323). At other instances it might be necessary to distinguish between closely related strains, e.g., to understand the ecological significance of physiological variability (27, 109, 128) (Fig. 2).
Synoptic Discussion of Marine and Freshwater Assemblages
A number of fundamental similarities in the functioning of marine
and freshwater microbial assemblages have been described, in
particular carbon transfer and food web structure (
203,
251,
313) and the role of bacteria attached to aggregates (
105,
229).
This has traditionally led to a fruitful exchange between limnological
and oceanographic research on planktonic microbes, based on
shared concepts and on a common set of techniques (
79,
81).
Recently, the relationship between the two disciplines has somewhat
deteriorated, conspicuously paralleled by a shift in research
focus from food webs and element cycles to microbial biodiversity.
In fact, cultivation-independent approaches have revealed by
far more differences (
89,
180) than similarities (
14) in the
composition of the microbial assemblages in the two habitat
types.
Can identical ecological concepts be meaningfully applied to communities composed of bacterial groups from completely different phylogenetic lineages? Our review may in parts substantiate such doubts, e.g., with respect to the role of allochthonous (156) or filament-forming (130) microorganisms in the two habitat types. Yet at the same time we illustrate that a focus on individual microbial populations also provides a platform to compare the ecological value of particular phenotypic traits, e.g., of motility and small cell size (103, 221, 238), or of specific growth strategies (65, 68, 212) in very different genotypes and assemblages across aquatic habitats.
The scope of this review is limited in several dimensions. We do not attempt to draw an exhaustive picture of the microbial ecology of heterotrophic aquatic microbes. Instead we try to integrate a rather diverse range of facets, focusing on current methodological and experimental approaches, and on empirical findings related to traditional topics of population ecology. We argue that during the last decade the study of aquatic microbial populations has developed into a rewarding field of research that is based on mature methodology. Since our focus lies on the ecology of different populations rather than on the study of total assemblages, we only marginally touch the rich literature on genetic fingerprinting or on the diversity of aquatic communities. We limit our discussion to the "ordinary saprophytes", i.e., to the predominantly chemoorganoheterotrophic microbes (although admittedly the borders between purely heteroorganotrophic and photoautotrophic energy acquisition by pelagic microbes do become more and more fuzzy [20, 327]). We ignore microbial assemblages in sediments, biofilms, or in engineered systems, and we do not discuss in detail the physicochemical environments of aquatic microbes, but rather point to more specialized reviews, e.g., about macroscopic organic aggregates or exopolymerous substances (206, 281).

TOOLS, TECHNIQUES, AND STUDY CONCEPTS
During the last 15 years aquatic microbial ecology has been
shaped by a diversification of methods for the cultivation-independent
study of microbial identity, activity, and genomic constitution
(
11). This trend is reflected in the recent foundation of a
scientific journal on methods in limnology and oceanography
that is edited by a microbial ecologist (
http://aslo.org/lomethods/editor.html).
The following section does not give an exhaustive listing of
tools for the study of microbial populations in situ. Instead,
it covers a suite of complementary approaches which have been
applied in various combinations to analyze bacteria in environmental
samples. They can provide a coherent framework for ecological
investigations about the abundant microbes in the water column,
i.e., taxa that contribute approximately 1% or more to the total
picoplankton assemblages. Other approaches, e.g., quantitative
PCR (
17,
283), might be more appropriate to study microbial
populations that are substantially smaller.

16S rRNA Gene Clone Libraries: Essential but Prone to Bias
In order to define the important populations in a new environment
or at a particular time point, it is often necessary to conduct
a prior study about microbial diversity, most commonly of 16S
rRNA genes. Full or partial sequences can be amplified from
extracts of environmental DNA (
75,
301) or directly from cells
concentrated on membrane filters (
21,
145) by PCR with appropriate
primer sets (
84,
194). These fragments are then ligated into
plasmids, cloned into
Escherichia coli, and the sequences of
vector inserts from an appropriate number of clones are determined.
The PCR step is omitted altogether in so-called shotgun clone
libraries (
305). Since such libraries require a drastically
greater screening effort, they are used for obtaining metagenomic
information rather than for the mere collection of 16S rRNA
genes.
The diversity of sequences in PCR-generated clone libraries may often not quantitatively reflect the diversity of the sequence types that are present in the original sample (242, 294). Already the DNA extraction may introduce biases, e.g., against bacteria with gram-positive cell walls (69). Primers that are designed to target the majority of known bacterial 16S rRNA gene sequences may exhibit mismatches to unknown sequence types (45, 287), and the presence of particular sequence types in mixed DNA may influence the PCR amplification efficiencies of other templates (292).
As a consequence some phylogenetic groups of aquatic microorganisms are overrepresented in clone libraries, whereas others are absent. For example, bacteria affiliated to the Cytophaga/Flexibacter/Flavobacterium group of the Bacteroidetes were rarely found in 16S rRNA gene clone libraries from coastal marine water samples, yet they may represent one third of all bacteria in such habitats (47, 63). In a library of coastal North Sea surface waters 80% of sequence types were related to the marine SAR86 clade, whereas this group formed <10% of microbial cells (63). In addition, PCR may result in chimeric sequences from two templates, and it may thus even produce artificial sequence diversity (124, 155). These biases may affect not only clone libraries, but also PCR-based methods for the genotypic fingerprinting of microbial assemblages (183, 193).
Sometimes it is desirable to limit the analysis of microbial diversity to a defined phylogenetic subset, e.g., to marine archaea or to freshwater actinobacteria (173, 309). This can be achieved by PCR with primers that are specific for the 16S rRNA genes of the group of interest (287). Such primers may cause an underestimation of the potential diversity within a particular phylogenetic group, e.g., some uncultured freshwater actinobacteria show one or more mismatches with the available sets of specific primers (309). Moreover, sequences generated with specific primers often cover only a part of the total 16S rRNA gene, typically less than 1,000 base pairs (55, 287). Partial sequence information negatively affects the accuracy of phylogenetic reconstruction (163), and it limits the range of potential signatures for subsequent in situ population studies by hybridization. Preferably, clone libraries of almost complete 16S rRNA gene sequences should be produced with general bacterial or archaeal primers, and they should then be screened for particular groups of interest (173, 184, 309).
The potential target groups for population studies are defined from sequence data by reconstruction of phylogenetic relationships. This analysis aims at placing the new environmental sequence types into different clades or clusters and to establish stable branching patterns. It forms the base for a phylogenetically meaningful definition of single populations and for the design of the corresponding oligonucleotide probes. A discussion of the reconstruction of microbial phylogenies from 16S rRNA gene sequences would go beyond the range of this review, and we draw the reader's attention to specific publications on this subject (163, 164).

Single-Cell Identification
Since 16S rRNA gene clone libraries do not accurately reflect
the abundances of microbes from particular phylogenetic clades
in the environment, such analysis needs to be complemented by
other strategies for the study of single populations in situ.
Hybridization techniques against extracted rRNA or intact cells
have developed into an important tool of choice for this purpose.
Our review is particularly focused on whole-cell fluorescence
in situ hybridization (FISH) with rRNA-targeted oligo- or polynucleotide
probes (
6,
7,
58,
86,
211,
217). FISH allows the identification
and quantification of different microbial taxa in environmental
samples. It links information derived from molecular phylogeny
with epifluorescence microscopy, a research tool that has considerably
formed our understanding of water-column microbes (
13,
122,
231).
The FISH analysis can be carried out at two levels (Fig. 3). For one, investigators may draw upon the rapidly expanding set of available probes (162) (Table 1). Most frequently, probes have been applied that are targeted to higher taxonomic levels, i.e., to Bacteria, Archaea, Eucarya, subgroups of Proteobacteria, gram-negative sulfate-reducing bacteria, clades of ammonium-oxidizing bacteria, etc. In an earlier review on FISH, such an analysis was proposed as a first step of a larger "top-to-bottom" strategy (7).
The information obtained by FISH with probes for higher taxonomic
levels should guide researchers to choose among probes of increasing
phylogenetic specificity for a second and potentially third
layer of analysis. This stepwise approach has hardly been realized
for the study of pelagic microbial assemblages yet, and currently
there are only a few such nested probe sets available. Hierarchic
FISH analysis has been applied to distinguish between marine
Gammaproteobacteria that are favored at different enrichment
conditions (
16,
61,
175) and to study the seasonal community
contribution of a clade of freshwater
Betaproteobacteria (
35).
More frequently, probes for large taxonomic groups have been
applied as stand-alone tools for explorative investigations
of unknown communities. FISH analysis with such probes has revealed
that the microbial assemblages in marine and freshwater pelagic
habitats differ even at the level of subgroups of
Proteobacteria (
89), that actinobacteria form large populations in lakes (
263),
that
Crenarchaea are a major component of the deeper marine
water column (
136), that protistan and metazoan grazing may
influence microbial community structure (
132,
147,
275,
279),
and that members of the
Cytophaga/Flexibacter/Flavobacterium group form a substantial fraction of coastal marine communities
(
45,
63). FISH with probes for large phylogenetic groups has
also been used to study community transitions in rivers and
estuaries (
28,
52,
143)
The second level of FISH analysis is more technically demanding. It includes the design and optimization of new FISH probes for individual phylogenetic clades or single phylotypes based on sequence information from 16S rRNA gene clone libraries of environmental DNA (Fig. 3). This strategy has been termed the "full-cycle rRNA approach" by one of the authors (7). The procedure is comparable to the testing of a scientific hypothesis. Specifically, it is verified if a particular clade of sequence types obtained from environmental DNA after PCR amplification indeed harbors microbes that form a substantial fraction of the assemblage in the studied habitat. The lower limits for a reliable quantification of cell numbers by the FISH approach as set by counting effort and negative controls typically range around 0.1 to 2% of total counts (217). Consequently, researchers applying FISH may need to test a number of newly designed specific probes on field samples to discover microbial populations that are sufficiently abundant for subsequent quantitative population studies. This implicit risk of falsification of a working hypothesis represents a major conceptual difference between the full-cycle rRNA approach and other strategies that analyze microbial assemblages by molecular fingerprinting of PCR-amplified rRNA genes (185, 254).

Problems with FISH and Possible Solutions
In summary, FISH probes represent tools that are rather tedious
to construct but easy to apply. The specificity of oligonucleotides
for a particular range of phylotypes is deduced from the sequence
data that are available at the time of their design. Due to
the exponential growth of sequence databases, some probes may
lose their originally envisaged specificity or target group
coverage with time. For example, one commonly used probe for
Bacteria (EUB338) has been constructed on a set of <1,000
then-available bacterial 16S rRNA gene sequences (
6). At the
time of this review, the Ribosomal Database Project (
42) has
collected >170,000 full and partial bacterial sequences.
Thus, it is not surprising that the coverage of probe EUB338
is incomplete, and it has been modified accordingly (
51). This
points to the need to check the target range of existing FISH
probes on the latest data set before applying them to unknown
samples. A useful database about the current specificity and
coverage of many published probes is provided by the Molecular
Ecology department of the University of Vienna at
http://www.microbial-ecology.de/probebase (
162).
However, the replacement of some of the first generation of available FISH probes should be seen as a necessary optimization process in a rapidly progressing field rather than as an irresolvable problem of the FISH approach. Analyses of rRNA gene sequences from aquatic habitats indicate that only a limited number of well-defined phylogenetic clades of microorganisms might actually be common in the pelagic zones of marine and freshwater environments (55, 85, 91, 121, 240, 328). A substantial amount of diversity within several of these clades appears to be covered adequately by the presently available sequence data (108). Such knowledge will eventually provide a reliable base for a new generation of more "habitat-specific" FISH probes that discriminate well-established lineages of microbes in a particular environment (Table 1), e.g., the various marine SAR clades (62, 188, 189, 325) or the freshwater actinobacteria (91, 310).
Another drawback of FISH with fluorescently monolabeled oligonucleotide probes is the low fluorescence intensity of hybridized bacteria from natural water samples (214). Bacteria in oligotrophic water are often small, slow growing, or in stationary phase (187), and their ribosome content is typically low (65). Consequently, there are few rRNA target molecules for FISH staining. The fraction of microbial cells that can be visualized microscopically may thus vary with the physiological state of the studied assemblage. For example, a significantly smaller percentage of bacteria could be stained by FISH in coastal North Sea surface waters during the winter months than during the spring and summer seasons (63). In environments such as offshore marine waters, sometimes only a minor fraction of microbes can be visualized by FISH with fluorescently monolabeled oligonucleotide probes (214). Therefore, it is likely that the abundances of some slowly-growing microorganisms with small cell sizes, e.g., of members of the marine SAR86 clade, are underestimated by the standard FISH approach (210).
During the last decade, efforts have been made to increase the sensitivity of FISH, e.g., with peptide nucleic acid probes (320), brighter fluorochromes (88), image intensified video microscopy (78), preincubation with chloramphenicol (200), hybridization with more than one fluorescently labeled oligonucleotide probe (188), and helper probes (70). Two particularly promising alternative strategies to FISH with fluorescently monolabeled oligonucleotides are polynucleotide probes and enzymatic signal amplification (57, 149, 210). Fluorescently multilabeled rRNA-targeted polyribonucleotide probes yield significantly higher signal intensities than oligonucleotide probes (214). They have been successfully applied to discriminate between bacteria and different groups of archaea in coastal and open ocean environments (40, 136, 214). Limitations of polyribonucleotide probes as a routine tool for the identification of aquatic microbes are the relatively high effort and variability of enzymatic probe synthesis, and the rather low phylogenetic resolution. Only three large taxa have been distinguished by this technique in marine waters (57), although potentially a resolution at the genus level is possible (300).
A working alternative is catalyzed reporter deposition (CARD)-FISH (210, 211, 263), which combines in situ hybridization with horseradish peroxidase labeled oligonucleotide probes and enzymatic signal amplification with fluorescently labeled tyramides (24). This allows the quantitative detection of marine and freshwater pelagic bacteria with low ribosome content that are insufficiently visualized by fluorescently monolabeled probes (210, 263) (Fig. 4).

Quantification of Abundance and Biomass
In order to detect significant net growth or loss of populations,
the cell numbers of different microbes in situ have to be determined
at a standardized level of precision. This requires manual quantification
of the percentage of FISH-stained microbes by epifluorescence
microscopy (
217). Other potential counting approaches, e.g.,
flow cytometry (
5), so far have failed to provide working alternatives
to this tedious evaluation strategy. Eventually, a rapid quantification
of bacterial populations by means of automated microscopy (
219)
might allow us to expand the scale of investigations from a
few point measurements to a spatial or temporal resolution that
better reflects the true population dynamics of heterotrophic
aquatic picoplankton.
A conversion of cell numbers into biomass is required for the reconstruction of carbon fluxes through microbial food webs. Bacterial cell sizes and the relationship between cell size and dry mass can be determined empirically, e.g., by image analyzed microscopy (174, 274) and appropriate conversion factors (159, 197, 233). Some microbial taxa in the plankton form significantly larger cells than others (16), and population changes within such groups may thus contribute disproportionally to changes in total biomass (132, 222). The most extreme example are the filamentous bacteria in the water column of many lakes (130). Such morphotypes rarely form more than a few percent of total cell numbers, but they may temporarily constitute half of total microbial biomass or more (130, 286) (Fig. 5). Therefore, the biomasses of different microbial populations may need to be determined separately in order to assess their respective roles in the carbon flux through aquatic systems (46, 132, 216, 237).

Single-Cell Activities of Individual Populations
One important topic of aquatic microbial ecology has been the
physiological properties of total microbial assemblages, in
particular of the metabolic and respiratory processes that drive
biogeochemical transformations (
13,
53,
142). In contrast, traditional
microbiological research is mainly centered on the physiological
properties of bacterial strains in pure culture (
109,
127).
In between these two levels of analysis there is a conspicuous
gap of information. Little is known about the growth-related
characteristics of single microbial populations that are realized
at environmental conditions in the presence of competitors,
predators, viruses, substrate heterogeneity, chemical gradients
etc. For example, the genome of the marine planctomycte
Rhodopirellula baltica strain 1 contains >100 different sulfatases (
90),
but it is unclear which ecological advantage is associated with
this feature (it might, e.g., reflect in situ growth on a complex
mix of substrates such as sulfated polysaccharides). In order
to understand the stability or fluctuations of a particular
biogeochemical process, it would be important to distinguish
if it is mediated by a single, physiologically highly versatile
microbial population, or if it is carried out by several bacterial
groups that may provide a greater functional redundancy (
318).
With the exception of stable isotope analysis (236) or pulse-labeling of nucleic acids (302), physiological information is typically lost by methods that use DNA or rRNA extracts for microbial identification. By contrast, physiological properties can be readily related to a particular genotype at the single cell level. FISH by itself may already provide some information about the physiological state of a population, because the signal intensity of hybridization is proportional to cellular ribosome content. The ribosome content of marine isolates tends to increase with growth rate (138). However, rRNA concentration is a parameter that may sometimes be difficult to interpret. Some marine bacteria may maintain high numbers of ribosomes even during periods of prolonged starvation (68). This is probably essential to rapidly respond to changes in growth conditions in a patchy environment (212). Thus, ribosome content may allow a limited assessment of bacterioplankton "activity" at the community level (52, 80), but it needs to be interpreted with caution if single populations are to be compared. In addition, cell identification by FISH can be combined with a number of other methods that visualize particular physiological properties of individual cells, e.g., substrate uptake, DNA synthesis, respiration (47, 196, 213), and even with stable isotope probing (198).
Microautoradiography.
One of the most powerful approaches to study physiological activities in mixed microbial assemblages dates back to the 1960s. The uptake of radiolabeled tracer substrates into individual cells can be visualized by a photographic technique termed microautoradiography (30, 31) (Fig. 6a). In combination with cell identification by FISH, this approach allows us to assess the partitioning of substrate consumption between different microbial populations in mixed assemblages. Microautoradiography-FISH was first used to determine organic and inorganic substrate uptake of ammonia-oxidizing bacteria and of other groups in activated sludge (154), but has since then been adapted for microbes in lakes and in the marine water column (4, 47, 98, 169, 199, 296, 306). Recently, protocols have been developed that integrate the superior CARD-FISH staining with microautoradiography for the analysis of bacterial substrate uptake in environments such as the mesopelagic zone (4, 296). It has even been attempted to add a quantitative aspect to microautoradiography by estimating the amount of incorporated radiolabel from the number of grains that are formed around active cells (46, 168, 170).
Without wanting to diminish the potential of microautoradiography,
one should be aware of some limitations. Currently, there exist
a variety of more or less time-consuming protocols for microautoradiography-FISH
of water column bacteria, and some protocols likely cause a
high loss of bacterial cells (
47,
199). Moreover, it appears
rather difficult to standardize some aspects of the procedure
(the exposure time and photographic development) to an extent
that would meaningfully allow us to quantitatively compare results
from different studies. Finally, the choice of adequate tracer
substrates may not be trivial. Comparatively little is known
about the composition of the dissolved organic matter pool and
about the turnover and the concentrations of specific organic
carbon compounds in the water column. Sometimes the environmentally
relevant substrates are not commercially available and have
to be laboriously custom synthesized, e.g., chitin and proteins
(
47), or the marine algal osmolyte dimethylsulfonopropionate
(DMSP) (
306). In freshwater systems such as bog lakes much of
the dissolved organic matter consists of a complex mix of high
molecular weight substances (e.g., humic acids) (
299). In these
habitats it might be difficult to decide on appropriate model
substrates.
Fluorescent activity tracers and flow sorting
In order to study particular aspects of growth in individual microbial populations there are technically less demanding alternatives to microautoradiography. Pelagic bacteria with an active electron transport system of the respiratory chain reduce tetrazolium salts to water-insoluble crystals (322). Such formazan grains are deposited intracellularly, and they can be detected both microscopically (247) and by flow cytometry (54). In combination with FISH cell respiration can thus be visualized in single microbial populations, as was shown for filamentous bacteria from activated sludge (196). However, the tetrazolium reduction method appears to be a rather insensitive means to distinguish between growing and non-growing (or dead) bacteria in the plankton. Accordingly, bacteria with visible formazan deposits are regarded as the most highly active fraction within a larger set of growing cells (268). While there may be good reasons to identify such highly active bacterial populations, no investigation has combined tetrazolium reduction and FISH to study microbes in the water column of natural aquatic systems.
Bromodeoxyuridine is a halogenated nucleotide analogue of thymidine that is incorporated into newly synthesized DNA of bacteria and eukaryotes (213, 245, 302). It provides a non-radioactive alternative to microautoradiography with tritiated thymidine (207) and it allows us to quantify growth rates at the single-cell level (116). Bromodeoxyuridine incorporation has been combined with CARD-FISH to visualize de novo DNA synthesis in different freshwater and marine bacterial populations (209, 213, 310) (Fig. 6b). This offers a sensitive means to detect changes of growth rates in single microbial populations in situ. During bottle incubations of filtered seawater, a rise in the numbers of bromodeoxyuridine incorporating Alteromonas sp. cells clearly preceded cell multiplication (213). Significant seasonal differences and short-term variability of growth rates were observed in members of the Roseobacter spp. and NOR5 lineages from coastal North Sea picoplankton (209). High bromodeoxyuridine incorporation by actinobacteria in mountain lakes indicated that these bacteria were not passively introduced from soils, but autochthonously growing members of the bacterioplankton community (310).
Flow cytometry may provide an alternative means of detecting activity or substrate uptake in single microbial cells. It allows the physical sorting of particular bacterial populations of interest for further analyses (22, 72). So far, microbial cells from plankton samples have been mainly sorted by phenotypic features, e.g., cell volume or cellular DNA or protein content (72, 150, 267, 326). Sorted bacteria have been analyzed by molecular methods (21, 323) and for radiotracer incorporation (151, 327). In contrast to microautoradiography, the tracer uptake rates of specific cell populations can be readily quantified by this approach.
Direct sorting of microbial cells after FISH staining has first been shown in highly productive wastewater treatment systems (284). Recently this approach has also been adapted for bacterial cells from coastal marine bacterioplankton, taking advantage of the superior signal intensities of CARD-FISH staining (262). Such a combination of cell identification and flow sorting potentially offers the ability to quantitatively investigate substrate uptake of single populations in natural samples (327). Moreover, it might eventually provide a means of obtaining functional genes or larger genome fragments from phylogenetically coherent groups of microbes directly sorted from environmental samples.
Distribution and Dynamics of Different Populations
For unknown reasons, heterotrophic aquatic microbes form large
populations in particular habitats or at particular seasons,
and are rare at other locations or time points (
35,
63,
136,
144,
218,
280). One challenge of population ecology is to explain
the observed distribution patterns of different bacterial taxa
from their physiological properties and from their interactions
with other organisms. Admittedly this may appear a rather far-fetched
goal for a discipline that has just started to understand which
microbes are frequent in different aquatic environments. However,
the ability of macroecology to understand the role of individual
plant and animal species is to a large extent based on an understanding
of their distribution patterns and population dynamics at various
environmental conditions. So far, only a few studies have investigated
abundance changes of particular microbial taxa in the water
column in a context of physicochemical parameters or food webs
(
63,
132,
136,
147,
223,
278).
For the purpose of gaining ecological insight from spatial or temporal distribution patterns, binary information about the presence or absence of a particular bacterial group, as provided by cloning or fingerprinting techniques, is probably insufficient. Such approaches allow us to detect fundamental differences between communities, e.g., between marine and freshwater habitats (180), along rivers (264), or in mesocosm (244, 253), but they can hardly distinguish if a set of environmental variables is more or less favorable for a specific population. A too-coarse division of aquatic microbial assemblages, e.g., into subphyla of Proteobacteria by FISH with the respective probes (171), also suffers from drawbacks, since different populations with potentially contrasting dynamics might be put into ecologically meaningless categories (Fig. 2). Such studies may contribute to our understanding of large biogeographic divisions, e.g., between marine and freshwater habitats (89), and of basic discontinuities in the composition of microbial assemblages, e.g., along estuaries (28). However, both the qualitative community analyses by fingerprinting and investigations on large taxonomic units by FISH should be regarded as intermediate steps towards the quantitative study of ecologically coherent and phylogenetically more tightly-defined populations.
Experimental Enrichments in the Field
For decades, aquatic microbial ecologists have complemented
descriptive studies on the distribution of microbes in various
habitats with a range of simple field experiments. These have
been referred to as "bottles, bags and buckets" (
203), or more
respectfully, as micro- to mesocosms, limnocorrals, enclosures,
etc. Typically, various volumes of water are taken directly
from the environment studied and this water is incubated at
more or less in situ conditions after manipulation of, e.g.,
substrates and nutrients (
61,
152,
177,
202), or of particular
functional groups of the food web (
16,
133,
293,
317). Depending
on the container size, the duration of such experiments ranges
from days to weeks. Short-term incubations share a basic logic
with tracer uptake experiments: a measurable response to a manipulation
should allow a deduction about the original state of the assemblage
or some of its members. Sometimes dialysis bags with defined
pore sizes may provide a more advanced alternative to bottles
(
80,
172,
278). Such bags allow readier exchange of dissolved
substances if exposed directly in the water column. Even so,
some features of the original environment are probably irreversibly
destroyed, in particular the assumed continuum between the dissolved
and the particulate organic matter (
12). Larger containers may
provide a useful means to artificially induce blooms of specific
phytoplankton groups (
244) or to manipulate metazooplankton
densities (
129,
223).
Such investigations are often plagued by the mysterious "bottle effect," a hard-to-define concept that reflects the worry of whether phenomena observed in confined assemblages are nonspecific consequences of the confinement rather than a result of the planned manipulation. Nevertheless, experimental mesocosms are among the few tools available to microbial ecologists that go beyond a purely descriptive analysis of aquatic microbial assemblages. A number of well-defined hypotheses about microbial populations have been successfully addressed by such approaches (16, 61, 132, 223, 244, 278, 293).
Defined Laboratory Communities and Pure Culture Studies
Experimental systems such as the Winogradsky column (
316) have
fundamentally shaped our understanding of environmental microbiology.
However, concomitant with the rise of cultivation-independent
methods, laboratory investigations on experimental communities
have somewhat suffered from a lack of popularity among microbial
ecologists. This may have been in parts a consequence of Thomas
Brock's harsh words about studies on "mixed cultures of unknown
provenance ... at some ill-defined state" (
32). It may also
be related to the realization that many laboratory investigations
have been performed on microorganisms that are readily culturable
(
112,
212) but that are rare in the water column (
62,
312).
These drawbacks may no longer apply. For one, an increasing
number of aquatic microbes have been isolated during the past
years that also form large populations in situ (
63,
110,
238)
and that thus represent adequate model organisms for laboratory
investigations (
27,
109). Second, 16S rRNA-based molecular tools
now provide new means to precisely follow the population dynamics
of different bacteria in mixed experimental assemblages (
16,
221). An increasing wealth of genomic information from isolated
environmental bacteria may eventually even allow us to link
the performances of individual members of such model assemblages
to the expression of particular genes in the context of a well-defined
experimental setup.
Thus, laboratory investigations on bacterial isolates or model communities add another important dimension to the understanding of microbial population ecology. For example, particular physical structures within aquatic habitats cannot be preserved in experimental approaches in the field. Laboratory systems can artificially produce aggregated organic matter in natural water samples (101) and trap single flocs in a three-dimensional flux field (230). Such designs provide the adequate physical and chemical environment to study microbial activities and successions on organic aggregates and particles (100-102).
Laboratory studies may also provide a better control over parameters that might mask the hypothesized relationship between the studied population and the variable of interest. Continuous-cultivation systems, not necessarily chemostats (126), stabilize the composition of mixed assemblages by enforcing a minimal growth rate and by providing constant temperature, illumination, and input of substrates and nutrients. This allows us to experimentally sustain transient ecological phenomena over prolonged periods of time, e.g., the rise of particular predator populations (112, 221, 232, 234, 250, 279), bacterial-viral interactions (181), or the breakdown of cyanobacterial blooms (304).
Investigations on pure cultures offer the possibility to distinguish between phenotypic and physiological properties of different aquatic bacteria, e.g., in their interactions with algae (29, 99, 146), their chemotactic responses (15, 23), motility patterns (140), grazing sensitivity (27, 114), or cell filamentation (115, 273). This provides the opportunity to test hypotheses about the ecological relevance of such features.

OCCURRENCE OF MICROBIAL POPULATIONS IN PLANKTON
A Few Words on Diversity
Our knowledge of aquatic microbial diversity is largely derived
from the analysis of 16S rRNA gene sequences directly PCR amplified
from environmental DNA (
239) and from culture collections predominantly
established on rich solid media (
107). Both approaches have
revealed complementary and often nonoverlapping facets of diversity
(but see reference
228). Nevertheless, our perception of the
total diversity of aquatic microbes is most probably incomplete.
A recent investigation by shotgun cloning of large genome fragments
from Sargasso Sea picoplankton concentrates and high-throughput
genome analysis has produced >100 novel bacterial 16S rRNA
sequence types in a single sample (
305).
Evidence has accumulated that there is relatively little overlap between the phylogenetic groups that are present in marine and freshwater environments (89, 180, 241), e.g., specific groups of archaea appear to be entirely limited to the marine water column (59, 76, 173). Lineages of 16 rRNA gene sequence types that occur in both habitat types include the SAR11 clade of Alphaproteobacteria (14, 85, 329), and the ammonia-oxidizing Betaproteobacteria (123, 297). Even within these clades, distinct clusters of marine and freshwater sequence types can be distinguished (329). Some clades of actinobacteria typically found in freshwater habitats also contain sequences from estuaries and marine waters (48, 309), whereas other clades within this phylum are exclusively of either marine or freshwater origin (91, 240, 309, 328). Members of the very diverse Cytophaga/Flexibacter/Flavobacterium group are common in some coastal and offshore marine habitats (45, 63, 144, 280), but they also occur in rivers and lakes (28, 143, 218, 223). Bacteria from this group appear to have radiated across a range of aquatic habitats, including biofilms and sediments (34, 158).
The phylogenetic ties between freshwater and soil microbes are still unclear. Sequence types from both environments have, e.g., been found within the freshwater acIV lineage of the actinobacteria (309). There are furthermore indications that microbial assemblages in some lakes may be similar to those in the influx from the catchment (156).
In the context of this review we distinguish between the multitude of microbial phylogenetic lineages that may occur in various aquatic systems and the few groups of microbes that have been shown to form substantial populations in such environments. Clearly, archival listings of microbial diversity from different habitats are a crucial first step to investigate the role and fate of aquatic microbes, since they provide the essential fundament for subsequent studies about the ecology of particular populations. However, it is equally important to progress from a purely qualitative appreciation of microbial diversity to the quantification of the abundances, biomasses, and activities of different phylogenetic groups. For example, it is presently still unclear if members of the Verrucomicrobia are an important component of freshwater assemblages. Such bacteria are frequently detected in lakes by PCR-based methods (157, 330, 331). From all we know, their densities might be one in a million but potentially also >10% of all cells. The following sections thus specifically discuss investigations that have established the cell concentrations, spatial distributions, temporal successions, or physiological features of specific microbial taxa in the plankton of marine and freshwater systems.
Bacterial Populations in the Marine Water Column
Some groups of marine bacteria had been known for years from
their 16S rRNA gene sequences before their abundances in the
water column were determined. This is the case for bacteria
related to the marine SAR11 (
188), SAR86 (
210), SAR116 (
71),
SAR202 (
189), and SAR406 (
71) clades, whereas for the various
lineages of marine actinobacteria (
240) such evidence is still
lacking. Members of the SAR11 clade are believed to be among
the most common prokaryotes in the marine plankton. It has been
reported that these bacteria may seasonally represent >50%
of total bacterial abundances in surface waters of the northwestern
Sargasso Sea and 25% of subeuphotic microbial assemblages (
188).
Bacteria related to
Roseobacter sp. (also referred to as the
SAR83 cluster, (
241) are another common component of coastal
and offshore microbial assemblages, and they may constitute
up to 25% of the marine picoplankton (
63,
95,
295). The seasonal
abundance of
Roseobacter spp. in coastal North Sea picoplankton
closely followed the development of phytoplankton biomass (Fig.
7) (
63,
95,
295). The geographic distribution of one particular
subcluster from this lineage appears to be limited to temperate
and polar oceans (
266). In transects across the German Bight
Gammaproteobacteria related to the SAR86 lineage on average
formed 7% of total cell numbers (
210), and 3 to 6% of all bacterial
16S rRNA genes in Monterey Bay surface waters were affiliated
with this group during an upwelling event (
295). Genes encoding
proteorhodopsin were first described in members of the SAR86
clade (
19), but recent findings indicate that such light-driven
proton pumps might be a widespread feature of marine bacterioplankton
(
305).
In addition to the well-established clades of marine bacteria,
new groups have been described that may reach high densities
in the water column. The NOR5 lineage of the OM60 clade of
Gammaproteobacteria (
39) seasonally represented between 5 and 10% of coastal picoplankton
in the North Sea (
63) and 2-3% in the western Mediterranean
Sea (L. Alonso and J. Pernthaler, unpublished data). Uncultured
members of the novel DE2 cluster (
Cytophaga/Flexibacter/Flavobacterium group) accounted for 10% of total cells in samples from the
Delaware Estuary and from the Chukchi Sea (Arctic Ocean) (
144).
In brackish waters of the Baltic Sea and in samples from the
Skagerrak-Kattegat front, substantial populations of species
related to
Alphaproteobacteria and to the
Cytophaga/Flexibacter/Flavobacterium group were detected using radioactively labeled whole-genome
probes (
226,
228). Interestingly, these bacteria also readily
formed colonies on solid media, which clearly contrasts with
findings from other marine sites (
62).
The composition of microbial communities in more extreme habitats might sometimes be very simple. Hydrothermal circulation activities in deep sea environments produce buoyant plumes with substantially elevated levels of reduced chemicals. The bacterial assemblages within such a plume inside the caldera of the Suiyo Seamount volcano consisted almost entirely of two distinct phylogenetic populations that were related to sulfur-oxidizing symbionts of hydrothermal vent fauna (291). The caldera might thus represent a giant natural continuous-cultivation system for these two groups.
Sometimes, it may be necessary to define microbial populations at the level of single strains, e.g., for the study of pathogenic Vibrio spp. in marine waters. In coastal environments Vibrio cholerae can be found both attached on particles and free-living in the water column (44), and pronounced seasonal and horizontal differences in population sizes have been reported (83, 117). In microcosms spiked with V. cholerae, rapid growth of these bacteria was observed after addition of organic carbon (190). It is thus conceivable that anthropogenic eutrophication might indirectly favor the growth and dispersal of pathogenic Vibrio strains.
Marine Archaea
The two major pelagic lineages of
Crenarchaeota and
Euryarchaeota are among the most well studied phylogenetic group of uncultured
microbes in marine picoplankton. Both oligo- and polynucleotide
probes have been developed for the direct visualization of such
microbes in water samples (
57,
78,
192,
296). Recently, a protocol
for CARD-FISH staining of
Archaea in samples from the deep sea
has been described (
296). Originally it was believed that creanarchaeota
only form large populations in the meso- and bathypelagic layers
below the euphotic zone (
59,
76). In a seasonal study in the
North Pacific subtropical gyre, the mean annual abundances of
Crenarchaeota below 200 m water depth ranged between 20 and
40% of total picoplankton cells, which corresponded to 3
x 10
3 to 1
x 10
5 cells ml
1 (
136). Comparable abundances of
this archaeal group were also reported from the deeper waters
of the Antarctic circumpolar deep water (
40). However, the same
study also detected large crenarchaeal populations by FISH in
the surface waters of the Southern Ocean during the winter months.
Such contrasting vertical distribution patterns are currently
difficult to interpret.
The metabolic capacities of planktonic crenarchaea are unclear, but there are indications that members of this lineage might be auto- or mixotrophic (120, 321). The planktonic marine Euryarchaeota on the other hand appear to be a common element of coastal assemblages and surface waters. Members of this lineage seasonally formed >30% of all cells in the surface picoplankton of the North Sea (214) (Fig. 7). Seasonal blooms of Euryarchaeota were also observed during a long-term study in surface waters of the upper Santa Barbara Channel (191).
Numerically Important Bacteria in Freshwater
Seasonal dynamics of different freshwater bacterioplankton populations
have first been reported from an ultraoligotrophic mountain
lake (
218). So far, bacteria from two of the four typical freshwater
lineages of
Betaproteobacteria as defined by Glöckner et
al. (
91) have been detected in high abundance in the environment.
Bacteria affiliated with the beta I clade (also termed the "
Rhodoferax sp. BAL47 lineage") (
328) formed populations of >10% in the
summer plankton of a eutrophic reservoir (
278). A second lineage
of
Betaproteobacteria related to
Polynucleobacter necessarius (beta II) seasonally constituted up to 50% of all pelagic microbes
in the aerobic waters of a meromictic humic lake (
35). Filamentous
bacteria from the LD2 subclade (
328) that is closely related
to
Haliscomenobacter hydrossis (
255) (
Cytophaga/Flexibacter/Flavobacterium)
transiently formed >40% of total bacterial biomass in a mesotrophic
lake (
223). Actinobacteria from the uncultured acI clade (
91,
309,
328) are another ubiquitous group of freshwater prokaryotes
(
91,
309,
328) that seasonally occur in high densities in habitats
of very different limnological characteristics, e.g., humic
(
35) or high mountain lakes (
91,
263,
310).
Bacterial Populations Attached to Organic Particles
Microbial assemblages on suspended organic aggregates differ
from those of the water column (
56). So far the particle-attached
communities in marine habitats have only been investigated qualitatively
by fingerprinting and comparative sequence analysis (
48,
56).
More information is available about limnic and riverine aggregates.
Microbial populations on aggregates in fresh waters change with
the ageing of such particles (
101) or during their transport
from rivers into estuaries (
265). Three populations related
to the genera
Duganella,
Hydrogenophaga, and
Acidovorax formed
almost half of the
Betaproteobacteria on organic aggregates
obtained from Lake Constance at a depth of 50 m (
261). These
bacteria effectively colonized artificially produced microaggregates
within 24 h. Interestingly, members of the three genera were
rarely detected in the planktonic microbial assemblage, and
they were not affiliated with the presently defined clades of
typical freshwater
Betaproteobacteria (
91,
329). Instead, these
bacteria are known from highly eutrophic environments such as
activated sludge (
249,
258).
In contrast to the lake snow assemblages, riverine organic particles have been described to mainly harbor Betaproteobacteria related to the drinking water biofilm bacterium Aquabacterium commune. These bacteria formed up to 30% of all cells on lotic organic aggregates in the river Elbe (135). The composition of the microbial assemblages on such aggregates showed pronounced seasonal changes, and bacteria related to the Planctomycetales were absent in winter.

FACTORS CONTROLLING MICROBIAL POPULATION SIZES
Competition for Different Substrates
The shortness of the following section does not reflect the
importance we assign to the topic. Our current understanding
of the relationship between the growth of individual bacterial
populations and the availability of particular substrates or
nutrients is still rudimentary. For example, it is established
that pelagic bacteria and archaea may incorporate amino acids
(
201), but with a few exceptions (see below) it is unclear if
different genotypes show preferences for individual components
of such mixes. Studies on the interactions between bacteria
and specific algae indirectly suggest that substrate quality
may play a role in the competition between microbial populations.
Pure cultures of various algal species may harbor distinct microbial
assemblages (
252). Different microbial communities could be
established from identical inocula in seawater micrososms if
blooms of specific algal groups were induced (
225). Cottrell
and Kirchman reported (
47) that various cooccurring microbial
populations in pelagic habitats may be specialized on the degradation
and uptake of particular substrate classes. Using microautoradiography,
these authors showed that different bacterial genotypes also
differed in their uptake of
3H from radiolabeled chitin, proteins,
amino acids, and
N-acetylglucosamine. A preference for simple
monomers over proteins in bacteria from the SAR11 clade has
recently been reported by the same laboratory (
168).
A set of recent investigations on the transfer and processing of phytoplankton-derived organic sulfur compounds has provided a first model for future studies of the relationship between particular bacterial populations and a specific biogeochemical process. Dissolved dimethylsulfonopropionate (dDMSP) is an algal osmolyte that is released during viral lysis or sloppy zooplankton feeding (50, 167). dDMSP is a growth substrate for heterotrophic bacteria (153), and it represents an important precursor of protein-sulfur in marine bacterioplankton (139). An increasing body of evidence is pointing to a few groups of marine bacteria as key elements in dDMSP biogeochemistry. Laboratory studies on isolates of the diverse Roseobacter clade have indicated a widespread ability of members of this lineage to degrade dDMSP and to incorporate the sulfur derived from this organic compound into cellular protein (93). In addition, large populations of bacteria affiliated with the Roseobacter clade were observed during dDMSP-producing algal blooms in the North Atlantic. In two independent studies the horizontal or vertical distribution of microbes from this group was positively correlated to dDMSP concentrations or fluxes (96, 323). Direct evidence of DMSP uptake was recently obtained by microautoradiography (170, 306). This approach also revealed that DMSP uptake may be a feature of different bacterial populations, and bacteria from the SAR11 clade rather than Roseobacter mediated the bulk of DMSP turnover in an offshore planktonic assemblage (169).
Patchiness and Gradients
Selective preference for particular substrates may not be the
only factor affecting the competition between aquatic microbes.
Specialization on a single resource might in fact be disadvantageous
in an energy-deficient environment (
60), and the majority of
bacteria and archaea in pelagic marine environments are capable
of incorporating mixes of radiolabeled amino acids (
137).
A considerable proportion of the substrates and of bacterial productivity in freshwater and coastal habitats are distributed in organic particles and microscale patches (12). In contrast, the bathypelagic zone of the open oceans represents a rather desert-like environment poor in particulate organic matter. Individual microbial species or phylogenetic lineages within the bacterioplankton thus likely differ in their ability to succeed in habitats with steeper or flatter substrate gradients. An "opportunistic" growth strategy might be widespread among those bacterial groups that successfully colonize organic aggregates or other nutrient-rich microniches. A marine Pseudoalteromonas sp. strain exhibited a significantly shorter growth delay than an Oceanospirillum sp. under "feast-and-famine" batch culture conditions, but the former strain experienced a growth disadvantage if substrate changes were gradual (212). The importance of such bacteria may vary between habitats, and different species of "opportunistically" growing microbes are found in marine and freshwater environments (224).
Representatives of "opportunistic" genera of Gammaproteobacteria that are readily culturable on solid media were generally rare in the bacterioplankton of shallow North Sea waters (62). In contrast, colony-forming bacteria represented a prominent fraction of the microbial assemblages in brackish waters of the coastal Baltic Sea (227, 228). Readily enrichable bacteria were also found in high concentrations in the plankton of a lake with high irregular input of organic carbon from the catchment (35). The identification and quantification of such "r-strategists" within heterotrophic picoplankton assemblages might thus eventually allow deductions about short-term fluctuations in the availability of organic matter in aquatic habitats, e.g., for a biological monitoring of pollution effects. In contrast, many if not most of the typical free-living marine and freshwater bacteria appear to lack the ability to form colonies on solid media (282), and their growth is negatively affected by enhanced substrate levels (289).
It is likely that many bacterial species in the water column combine elements of the oligotrophic and the "opportunistic" growth strategies in their life cycles, e.g., by alternating between free-living and attached growth forms (141). Isolates from freshwater plankton that were initially oligocarbophilic could gradually be adapted to richer conditions (114). Bacteria from the marine NOR5 lineage, which are apparently free-living in the water column, also formed colonies on low-nutrient agar plates, albeit significantly later than other "opportunistic" strains (63). A dual-niche existence may also explain why facultatively anaerobic bacteria appear to be such a common component of coastal bacterioplankton assemblages (4, 243). In shallow waters of the North Sea >80% of free-living Roseobacter spp. cells were able to incorporate glucose at both oxic and anoxic conditions (4). Since the average depth of the German Bight is only 20 m, bacteria from the Roseobacter spp. lineage that colonize aggregated senescent algae (97) might experience temporary anoxia while settled on the sediment surface. These bacteria could be reintroduced into the water column by the periodic resuspension of particulate organic matter (179).
Mortality
So far there is little evidence that a lack of resources is
a major cause of bacterioplankton mortality. Cultured strains
that are thought to be representative for the pelagic environment
are often oligocarbophilic (
238,
259), or they survive extended
periods of starvation (
68). Predation and viral lysis are believed
to be the key factors that counterbalance microbial growth in
the water column (
13,
77,
271). Growth inhibition or cell damage
induced by UV radiation may be another important ecological
factor in some aquatic habitats (
10,
119,
285).
Nevskia ramosa,
a species inhabiting the neuston layer of fresh waters, exhibited
elevated resistance to UV (
290). Some alpine lakes exposed to
intense levels of UV-B radiation (
148) feature conspicuously
high abundances of actinobacteria, a phylogenetic lineage of
mainly gram-positive bacteria with a high genomic G+C content
(
91,
263,
310). Gram-positive bacterial isolates are often less
affected by UV radiation than gram-negative bacteria (
8), and
a high genomic G+C content has been suggested to mediate higher
resistance to radiation damage (
166).
Viral lysis.
The current concepts of specific viral-bacterial interaction in aquatic systems are largely shaped by theoretical models (298), and presently there are almost no investigations about the influence of viral lysis on the coexistence of individual microbial populations in the plankton (260, 317). Viral influence on the growth of different bacteria might act both directly by "killing the winner" (298), but also indirectly via the release of dissolved organic matter and nutrients from lysed pro- and eukaryotic cells (92, 182). Rapid development of resistance to viral infection has been observed in some bacterial strains during continuous-culture experiments (181), but it is unclear if such a process will also occur in natural aquatic assemblages. Recently, changes of the species richness of marine archaea have been reported as a likely consequence of experimentally manipulating viral densities (317). For a detailed discussion of the influence of viruses on aquatic microbial assemblages, readers should refer to specific reviews on the subject (311, 319).
Selective predation.
Hetero- and mixotrophic protists, in particular nanoflagellates and ciliates, are the main consumers of picoplankton in the marine and freshwater pelagic zone. Their role in controlling the abundance, biomass, and productivity of microbial assemblages has been amply documented (269, 298). Many of these predators are omnivorous, i.e., they can feed on a large range of bacterial species. However, they are not unselective feeders. In the following we will focus on predation selectivity that is related to prey cell morphology, in order to illustrate the influence of a phenotypic feature on the success of different genotypic microbial populations. Other aspects of microbial predator-prey interactions are discussed elsewhere (25, 82, 131, 215, 277).
Due to their specific particle uptake mechanisms and handling procedures, protistan predators cannot feed on all bacterial shapes or cell size classes with equal efficiency (26, 178). As a consequence, microbial cells within a length range of 1 to 3 µm are preferably ingested by heterotrophic flagellates and ciliates, whereas smaller or larger cells profit from reduced loss rates (130, 186, 276). Even small differences in cell sizes between strains of freshwater ultramicrobacteria may have large effects on their survival rates (27). Microbial assemblages that are exposed to high grazing pressure thus typically harbor high abundances of extremely small cells (222). In contrast, large filamentous bacterial morphotypes and bacteria that form microcolonies are substantially more protected from protistan grazing (115, 273). Filamentous morphotypes accumulate during periods of high predation in fresh waters (134), but they are rarely observed in marine systems. Some strains of freshwater Betaproteobacteria produce microcolonies within a sponge-like matrix of extrapolymerous substances that renders them resistant to flagellate predation (113).
Size-selective predation induces shifts in the genotypic composition of mixed assemblages by imposing different mortality rates on bacterial species with different mean cell sizes (Fig. 8) (221). First evidence for such community changes originated from continuous-cultivation experiments on microbial assemblages that formed stable associations with freshwater algae (221, 234). Selective grazing mortality is moreover believed to set an upper limit to the standing stocks of some microbial populations in the plankton. For example, bacteria from a cosmopolitan lineage of freshwater Betaproteobacteria (beta I) constituted approximately 10% of the summer assemblage in a eutrophic drinking-water reservoir (278). After removal of protists and in situ incubations in dialysis bags, members of the beta I clade increased to almost 30% of total cells within 24 h. It is thus likely that these bacteria contributed disproportionally to the flux of organic carbon from the picoplankton to the higher trophic levels. Some genera of "opportunistically" growing Gammaproteobacteria (Alteromonas, Vibrio, and Pseudoalteromonas) are probably rare in coastal surface picoplankton because they are almost completely suppressed by size-selective grazing (16). This mechanism might also play a role in eliminating pathogenic Vibrio spp. from the water column (165).
On the other hand, grazing-resistant genotypes rapidly accumulate
in assemblages exposed to high protistan predation. In nonaxenic
continuous cultures of the phytoflagellate
Cryptomonas sp.,
filamentous
Betaproteobacteria were only observed if protistan
predators were added (
279). A filament-forming
Comamonas acidovorans strain outcompeted a
Vibrio sp. strain after the addition of
bacterivorous flagellates to chemostat cocultures (
112). Grazing-resistant
bacterial morphotypes from different phylogenetic lineages increased
rapidly after food web manipulation in water from fishless ponds
(
132,
147). A substantial enrichment of filamentous
Flectobacillus sp. was observed during artificially induced blooms of nanoflagellates
in samples from a eutrophic freshwater reservoir (
278). Threadlike
bacteria of >99% 16S rRNA sequence similarity formed >40%
of total bacterial biomass in a mesotrophic lake during high
protistan grazing (
223). Such a natural enrichment of grazing-resistant
genotypes in fresh waters appears to be an ephemeral phenomenon,
as these bacteria are typically sensitive to predation by larger,
filter-feeding metazooplankton (
129).
The interplay between resource availability and mortality in determining the population sizes of different bacterial taxa is poorly understood. Changes in bacterial community composition might be related to changes in the ratio of bacterial mortality rate to growth rate (277). This would imply that communities with apparently stable taxonomic composition may be encountered at very different levels of total microbial productivity or mortality and that profound community changes are induced by shifts from top down to bottom up or vice versa (235). One type of natural model system to study such interactions might be freshwater reservoirs that feature pronounced longitudinal substrate and nutrient gradients between the river influx and the dam areas. Experiments that combine the transplant of water from different positions of the gradient with food web manipulations (80) might eventually shed more light on the complex control of different microbial populations by top-down and bottom-up forces.
OUTLOOK
The future of environmental microbiology will be shaped by the
current advances in genome sequence analysis of cultured and
uncultured microbes. This appears to create a favorable conceptual
environment for a population-based perspective in aquatic microbial
ecology. Already, the analysis of genomic information has strengthened
the interest in the cultivation of abundant heterotrophic microbes
from the water column (
39,
63,
110,
204,
238). Such activities
will probably draw increased attention to the unique physiological
features of different genotypes and thus to the potential ecological
differences between cooccurring microbial populations in mixed
assemblages.
Some genomic information will moreover doubtlessly be of direct interest for the study of aquatic microbial populations in situ. Emerging techniques such as a combined FISH staining of mRNA and rRNA (208) will allow us to detect the expression of metabolic genes within bacterioplankton populations defined at the level of single ecotypes (41). Ideally, such gene-specific probing could be applied in combination with other ecologically relevant features of bacterial cells, e.g., morphology (223), proliferation (213), substrate uptake and turnover (324), motility (104), exoenzyme activity (195), or polysaccharide sheath formation (288). Moreover, a more complete knowledge of microbial genomes will allow us to detect far more subtle phylogenetic differences between bacteria than what can presently be derived from the analysis of 16S rRNA genes (315). Questions addressing the biogeography (43, 315) and physiological or evolutionary adaptation of microbial ecotypes (27, 109, 128) might therefore form another area of future research in environmental microbiology.
However, the ties between environmental genomics and microbial population ecology should not be overstated. The population sizes of different microbes in the environment cannot be predicted from their genomic constitutions only, and the success of different bacterial taxa is codetermined by their interactions with competitors and predators in the context of the physicochemical environment. Moreover, while the existence of microbial biogeography arguably is debatable (66), this controversy cannot be a central concern of population ecology. Even if in principle "everything is everywhere" (18), it is known that different groups of heterotrophic aquatic microbes exhibit distinct temporal, spatial, and geographic distribution optima. Thus, a major challenge of the coming decade will be to understand the underlying reasons for the heterogenous distribution patterns of different microbial populations in marine and freshwater plankton.

ACKNOWLEDGMENTS
We thank our students and colleagues for all the fruitful discussions
and controversies that helped to shape our ideas and David Kirchman
and two anonymous reviewers for their helpful comments on the
manuscript.
We acknowledge the institutions that have supported our research on the topics discussed here, in particular the European Union (EVK3-2001-00194 BASICS), the German Ministry of Education and Research (BMBF01 LC0021/TP4), the German Research Foundation (PE-918/2-1), and the Max Planck Society.

FOOTNOTES
* Corresponding author. Present address: Limnological Station, Institute of Plant Biology, Seestrasse 187, CH-8802 Kilchberg, Switzerland. Phone: 41-1-716-1210. E-mail:
pernthaler{at}limnol.unizh.ch.


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Microbiology and Molecular Biology Reviews, September 2005, p. 440-461, Vol. 69, No. 3
1092-2172/05/$08.00+0 doi:10.1128/MMBR.69.3.440-461.2005
Copyright © 2005, American Society for Microbiology. All Rights Reserved.
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