Applied and Environmental Microbiology, July 2000, p. 3119-3124, Vol. 66, No. 7
Department of Biology, Rensselaer Polytechnic
Institute, Troy, New York 12180-3590
Received 14 December 1999/Accepted 27 March 2000
A modified nested reverse transcriptase PCR (RT-PCR) method was
used to detect the expression of nitrogenase genes in meso-oligotrophic Lake George, New York. Net (>20-µm pore size) plankton samples collected from two sites (Dome Island and Hague Marina) were extracted for total RNA and genomic DNA to determine the identity of diazotrophic organisms that were present and those that were actively expressing nitrogenase genes. Phylogenetic analysis of individual sequences cloned
from PCR amplifications showed that there were phylogenetically diverse
groups of bacteria that possessed a nifH gene, including representatives of unicellular and filamentous cyanobacteria, the Many aquatic communities are
deficient in fixed inorganic nitrogen (4, 11).
Nitrogen-fixing microorganisms can obtain nitrogen from atmospheric
dinitrogen (N2) and are important since they can alleviate
nitrogen limitation of productivity of aquatic and terrestrial
environments (4, 21). Nitrogen-fixing cyanobacteria often
form blooms in nitrogen-limited lakes and estuaries.
Nitrogen fixation is catalyzed by the enzyme nitrogenase. Nitrogenase
is highly conserved among diverse N2-fixing organisms (13). The phylogenetic analysis of molecular sequences of
nifH, which encodes the Fe protein component of nitrogenase,
yields tree topologies that are largely similar to 16S rRNA phylogeny (23) and are useful for identifying unknown diazotrophs
(24).
Recently, nitrogenase gene sequences (nifH) have been
amplified and sequenced from a number of environments, including rice roots, soils, and oceans, and invertebrates, such as zooplankton and
termites (1, 10, 12, 17, 19, 22, 25). However, the mere
presence of nitrogenase genes does not indicate that bacteria are
actively fixing nitrogen. Particularly in nutrient-limited aquatic
environments, it is important to know whether nitrogen-fixing microorganisms that are present are actually expressing the nitrogenase enzyme. Although 15N or acetylene-reduction techniques are
available for detecting nitrogen fixation activity, they involve
incubation of samples, can have limited sensitivity, and do not provide
information on which microorganisms are actively fixing nitrogen.
Culturing techniques have been used to determine the type of individual
species present, but these techniques yield biased results and a
misrepresentation of the types of bacterial species that are active in
the environment (10, 16).
The reverse transcriptase PCR (RT-PCR) makes it possible to assay for
cells that are actively expressing specific genes at the time of
sampling, and it has been used recently to detect expression of genes
in the environment, including nifH (5, 9). In
parallel, PCR of DNA obtained from the same samples can confirm the
presence of nitrogen fixers as well as detect microorganisms that have
the nitrogen fixation genes but that are not expressing nitrogenase at
the time of sampling. Comparison of sequences obtained by RT-PCR and
PCR can therefore be used to investigate the diversity of organisms
expressing genes under different environmental conditions and in
different habitats (5).
Several nutrients are often present in low concentrations in aquatic
environments, and it is usually difficult to determine the specific
nutrient(s) limiting productivity (4). Lake George is a
large meso-oligotrophic lake in northern New York State. During the
summer season, the lake is stratified with levels of nitrate, ammonium,
and soluble reactive phosphorus that are typically below the detection
limit in the epilimnion (7). While Lake George, like many
freshwater systems, has been assumed to be phosphorus limited, both
nitrogen and phosphorus are in short supply, making Lake George a good
candidate for the study of factors regulating the expression of
nitrogenase. Furthermore, Lake George is a long narrow lake divided
almost equally into two subbasins, with the major outflow from the
northernmost extent of the north basin (14). Previous
studies had suggested that the south basin had higher concentrations of
chlorophyll and productivity than the north basin (2),
although more recent analysis indicated only moderate differences that
were not statistically different (8). There are apparently
differences in composition of plankton communities between the two
basins (15). The primary objective of this study was to
determine if there were nitrogen-fixing microorganisms in the net
plankton of Lake George and if these microorganisms were actively
expressing nitrogenase, indicating that nitrogen may have been limiting
their growth.
Net plankton were collected from two sampling sites located in Lake
George (Hague Marina and Dome Island) on 1 June 1998. One-liter net
plankton samples were collected with a zooplankton net (20-µm mesh
size) from a vertical tow at a depth of 20 meters. A 500-ml sample of
the net concentrate was diluted in Lake George water and filtered
through a 0.45-µm-pore-size mixed-cellulose-ester membrane (Millipore
Corporation, Bedford, Mass.). Samples were then resuspended in 500 µl
of buffer QRL1 (Qiagen, Valencia, Calif.) and homogenized with an
electric pestle for 30 s. Samples were stored at Genomic DNA from the filter samples was extracted using a slight
modification of the method of Giovannoni et al. (3), as described by Braun et al. (1). Net plankton samples were
initially stored in buffer QRL1 (Qiagen) and then extracted with
phenol-chloroform. The DNA was precipitated with ammonium acetate (3 M,
pH 5.2) and ethanol. The precipitated DNA was resuspended in a solution
containing 10 mM Tris (pH 8.0) and 1 mM EDTA.
DNA was also extracted from a number of cultivated, but not axenic,
cyanobacterial isolates from Lake George in order to determine if they
contained nif genes that were related to the cyanobacterial nifH genes detected in the net plankton. DNA was extracted
from colonies grown on agar plates, using the method of Zehr et al. (25).
Total RNA was extracted from the filters using the RNeasy minikit
(Qiagen), purified with an RNeasy mini-spin column (Qiagen) according
to the manufacturer's protocol, and resuspended in 50 µl of
H2O. DNA in the samples was digested using RQ1 DNase
(Promega, Madison, Wis.) for 30 min at 37°C. The DNase enzyme was
removed from the sample using the RNeasy minikit protocol.
Two degenerate oligonucleotide PCR primers were designed to amplify an
approximately 460-bp segment of the nifH gene. This fragment
brackets the nifH1 (corresponding to Azotobacter vinelandii nucleotide positions 639 to 655; 5'-TGY GAY CCN AAR GCN GA-3') and
nifH2 (A. vinelandii positions 1000 to 984; 5'-AND GCC ATC ATY TCN CC-3') primer sites designed by Zehr and McReynolds
(26), and it is similar to the amplified region obtained
using primers designed by Ohkuma et al. (10). The additional
pair of primers nifH4 (A. vinelandii positions 546 to 562;
5'-TTY TAY GGN AAR GGN GG-3') and nifH3 (A. vinelandii
positions 1018 to 1002; 5'-ATR TTR TTN GCN GCR TA-3') were designed for
nested PCR based on conserved sequences outside of nifH1 and nifH2. All
four of these primers were degenerate (Y = T or C; R = A or
G; D = A, G, or T; and N = A, C, G, or T). The nested PCR
proved to be less affected by sample inhibition than in single-stage
PCR, with substantially increased sensitivity. The primer sites were
conserved throughout nifH genes in clusters I, II, III, and IV.
Reverse transcription reactions were performed in mixtures containing
28 µl of diethyl pyrocarbonate-treated H2O, 10 µl of 5× avian myeloblastosis virus buffer, 1 µl of a deoxynucleoside triphosphate (dNTP) mixture (a 10 mM concentration of each dNTP), and 1 pmol of primer nifH3. The reaction mixtures were exposed to UV light
(254 nm) for 20 min to prevent contamination. One microliter of avian
myeloblastosis virus RT (Promega) was then added along with 1 µl of
DNase-treated RNA. Reaction mixtures were incubated at 42°C for 30 min.
After reverse transcription, 1 µl of the cDNA was added to 49 µl of
the first-round PCR mixture (4 mM MgCl2, 10× reaction buffer, 10 mM dNTPs, 100 pmol each of nifH3 and nifH4 primers, and 2.5 U of Taq polymerase). The PCR was carried out with 30 cycles
of denaturation at 95°C (1 min), annealing at 55°C (1 min), and
extension at 72°C (1 min). The second round of the nested PCR was
performed with 1 µl of the first-round product in a mixture of 4 mM
MgCl2, 10× reaction buffer, 10 mM dNTPs, 100 pmol each of
nifH1 and nifH2 primers, and 2.5 U of Taq polymerase, with 30 cycles of the same temperature and time conditions as in the first
step of the nested PCR. DNA samples were amplified by nested PCR under
the same conditions as the RT-PCR but without the reverse transcription step.
Two types of negative controls confirmed that the RT-PCR results were
from RNA and not from contaminating DNA. The first control used direct
nested PCR of the RNA samples, and the second consisted of treating the
RNA samples with RNase and subjecting them to nested RT-PCR (see Fig. 3
and 4). The results of these two experiments showed that the
amplification products were derived from nifH transcripts in
the total RNA sample and not amplification from contaminant genomic
DNA. Thus, the RT-PCR method appears to be a useful assay for
nifH mRNA.
After the second round of PCR amplification, the amplified fragments
were gel purified and cloned into a pGEM-T vector (Promega). Clones
were screened by restriction digestion to detect those with the correct
size insert (approximately 359 bp). Recombinants were randomly picked
from each ligation to obtain equal numbers of clones from each sample
type (Hague Marina RNA, Hague Marina DNA, Dome Island DNA, and Dome
Island RNA). DNA isolated from the selected clones was sequenced on
both strands, by the Sanger dideoxynucleotide chain termination method.
The amplified partial Fe protein gene sequences were translated and
aligned using Genetic Data Environment software (Ribosomal Database
Project) (6). The amino acid sequences were aligned with
representative nitrogenase sequences obtained from GenBank. Distances
between pairs of sequences were calculated using the distance
correction of Tajima and Nei (18), followed by the construction of phylogenetic trees by neighbor joining using TREECON for Windows software (20).
The expected 359-bp fragment was amplified from all samples following
reverse transcription and PCR (Fig. 1).
Increasing the amount of added RNA resulted in increased amplification
product (Fig. 1, lanes 2 and 4).
0099-2240/00/$04.00+0
Copyright © 2000, American Society for Microbiology. All rights reserved.
Expression of nifH Genes in Natural
Microbial Assemblages in Lake George, New York, Detected by Reverse
Transcriptase PCR
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ABSTRACT
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Abstract
Text
References
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and
-subdivisions of the division Proteobacteria (
-
and
-proteobacteria), and a previously undefined group of bacteria. The phylotypes cloned from RT-PCR amplifications, which were actively expressing nifH transcripts, clustered with the unicellular
and filamentous cyanobacteria,
-proteobacteria, and the novel
bacterial cluster. No bacterial sequences were found which clustered
with sequences from cluster II (alternative nitrogenases), III
(nitrogenases in strict anaerobes), or IV (nifH-like
sequences). These results indicate that there were several distinct
groups of nitrogen-fixing microorganisms in the net plankton from both
sampling sites and that most of the groups had representative
phylotypes that were actively expressing nitrogenase genes.
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TEXT
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Abstract
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References
80°C.

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FIG. 1.
RT-PCR of net plankton samples obtained from two
sampling sites in Lake George, N.Y. The amount of RNA used in the
reverse transcription samples is indicated following the sample
description. RT and PCR positive control reaction mixtures consisted of
Trichodesmium sp. strain IMS101 RNA and DNA, respectively.
The RNA samples were tested for the presence of contaminating DNA using
nested PCR without the reverse transcription step. The expected-size
fragment was amplified only in the positive control lane containing
target DNA (Fig. 2). No amplification product was obtained from the Dome Island or Hague Marina RNA samples
without the reverse transcription step.
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The second test used to confirm the lack of DNA contamination was based
on treating the RNA samples with RNase followed by RT-PCR (Fig.
3). No amplification product was detected
in the RNA samples subjected to RNase treatment (Fig. 3).
|
The results of the phylogenetic analysis of the nifH genes
are shown in Fig. 4 and summarized in
Table 1. The Lake George set of sequences
consisted of 14 unique nifH sequences obtained from RNA and
14 unique sequences obtained from DNA from each site, for a total of 28 sequences from Dome Island and 28 sequences from Hague Marina (Table
2).
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The nifH sequences obtained from Dome Island clustered
in nine different phylogenetic groups (Fig. 4). The four sequences derived from the PCR assay clustered in three different groups that
included the cyanobacterial clade and a novel, previously undefined
cluster, which is a deeply branching cluster outside of cluster I. The
five sequences derived from the RT-PCR clustered with cyanobacterial
sequences and sequences from the
-subdivision of the division
Proteobacteria (
-proteobacteria) (Fig. 4). Corresponding sequences from PCR and RT-PCR were found to cluster together among the
cyanobacterial sequences.
The 28 nifH sequences obtained from Hague Marina contained
15 different sequence types. Nine sequence types were obtained from PCR
and six sequence types were obtained from RT-PCR. The DNA-derived
sequences tended to cluster with sequences from cyanobacteria,
-proteobacteria, and the novel cluster. The RT-PCR sequences clustered with sequences from cyanobacteria,
-proteobacteria, and
the novel cluster (Fig. 4). The novel nifH sequences
obtained from Hague Marina PCR and RT-PCR clustered together (Fig. 4).
As shown in Table 1, the nifH genes obtained from both
sample sites clustered among the
- and
-proteobacteria as well as the cyanobacteria (Fig. 4). Additional sequences derived from both
sampling sites formed a divergent group of sequences that clustered
together with a high bootstrap value. These sequences were detected in
both PCR and RT-PCR amplifications. This specific set of sequences
clustered independently of any other nifH clade (clusters
II, III, and IV) (Fig. 4). No sequences derived from the Lake George
net plankton samples were detected in cluster II, III, or IV.
Phylogenetic analysis of the nifH sequences obtained from both RT-PCR and PCR showed that nitrogen-fixing bacteria were present and were expressing nifH. The sequences obtained in this study were not identical to any previously published nifH sequences. The greatest similarity found was 99% similarity to a previously sequenced nifH gene from the Pacific Ocean (25). All of the sequences obtained in this study were from cluster I, and thus, no alternative (second alternative, non-molybdenum- or non-vanadium-containing) nitrogenase or Archaea nifH sequences were detected. Sequences from cluster III, which includes nif sequences from anaerobic bacteria, were not detected either, despite the fact that invertebrate plankton were collected and that cluster III sequences previously have been found to be associated with invertebrates (1, 25). It is possible that the anaerobe nif sequences were present but with only low relative abundance and, therefore, were not detected in this study.
The finding of unicellular-cyanobacterium nifH RNA and DNA sequences in the net plankton samples was unexpected. Unicellular cyanobacteria would be expected to pass through the plankton net during sample collection. Gleothece-like cells have been observed in Lake George, and a Dermocarpa-like cyanobacterium has been recovered in culture (J. L. Collier, unpublished data). The presence of these cyanobacterial nifH sequences suggests that cyanobacteria were present in aggregates and that they were expressing nitrogenase.
We tested unicellular cyanobacteria cultivated from Lake George for
nifH. Interestingly, although the cyanobacterial isolates did not contain the same cyanobacterial nifH genes as
detected in Lake George by PCR, bacteria associated with the isolates
contained
-proteobacterial nifH genes that clustered with
nifH sequences from Lake George. These types of bacteria may
have been associated with the aggregated cyanobacteria collected in the
net plankton.
More filamentous-cyanobacterium nifH sequences than unicellular-cyanobacterium sequences were recovered from Dome Island, by RT-PCR as well as PCR. These sequences were a fairly divergent group within the cyanobacteria but were probably most closely related to filamentous heterocystous cyanobacteria. In contrast, sequences obtained from Hague Marina DNA included a higher percentage of unicellular-cyanobacterium nifH sequences than filamentous-cyanobacterium sequences, but fewer sequences were obtained by RT-PCR (Table 1). Filamentous-cyanobacterium nifH sequences were not detected in the Hague Marina DNA samples. This could be due to a lower relative abundance of the filamentous cyanobacteria at this site or the relatively small number of sequences examined in this study.
Other types of nitrogen-fixing bacteria that were detected in the net
plankton samples expressed genes that were related to
- and
-proteobacterial nif genes. The bacteria containing these genes were most likely associated with small invertebrates (i.e., zooplankton), small particles, or phytoplankton aggregates that were
collected in the net. Some of the sequences found in this study are
related to sequences recently reported for termite-associated bacteria
(10). For example, clones LG1115 and LG1116 cluster most
closely with sequences obtained from termites and are 86% identical to
the termite-associated nifH sequences (Fig. 4). Braun et al.
(1) reported nifH sequences amplified from
microbial enrichments initiated with marine planktonic invertebrates
that grouped with cluster I sequences, branching closely to the same termite-associated nifH sequences as do sequences LG1115 and
LG1116. These sequences obtained from the Lake George net plankton may have been obtained from bacteria associated with invertebrate zooplankton.
Sequences that group with LG1107 and LG1109 form a deeply branching cluster of bacteria. The high bootstrap value, in addition to the deep branching, supports the conclusion that this set of sequences represents a new phylogenetic group of N2 fixers. This clade is closest to the proteobacterial clade shown in Fig. 4 and does not represent cluster II, III, or IV sequences (data not shown). Though it is difficult to determine the type of bacteria from which these sequences were derived, it is clear that these sequences were not artifacts.
Conclusions.
The results presented in this paper demonstrate
the effective use of a nested RT-PCR approach to detect bacteria
expressing nifH from environmental samples. Many
nitrogen-fixing bacteria were detected among the Lake George samples,
and cyanobacteria,
-proteobacteria, and a novel diazotrophic
proteobacterial clade expressed nifH transcripts.
Furthermore, all of the bacteria detected had type I nitrogenase, and
no sequences in group II, III, or IV were found. While nifH
expression does not necessarily indicate that the bacteria were
actively fixing N2, it does provide information on the
bacteria that could have been fixing nitrogen and also suggests that
nitrogen-fixing conditions existed for these phylotypes at the time of
sampling. It is also interesting that these microorganisms expressed
nitrogenase in a typical phosphorus-limited environment, suggesting
that the microorganisms may have been limited by multiple nutrients or
that microorganisms were limited by different nutrients in the same
environment. Future use of this nested RT-PCR approach can be used to
identify organisms actively expressing nitrogenase genes and also to
learn more about the environmental factors controlling nitrogenase
expression and nitrogen fixation in aquatic environments.
Nucleotide sequence accession numbers. All sequences obtained in this study were submitted to GenBank with accession numbers AF212868 to AF212891.
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ACKNOWLEDGMENTS |
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This work was supported by NSF grants OCE-9503593 and IBN-9629314 and the Department of Energy.
We thank L. Richardson for assistance in the field.
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FOOTNOTES |
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* Corresponding author. Present address: Ocean Sciences Department, Earth and Marine Sciences Building, Room A438, University of California, Santa Cruz, CA 95064. Phone: (831) 459-4009. Fax: (831) 459-4882. E-mail: zehrj{at}cats.ucsc.edu.
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