Previous Article | Next Article ![]()
Applied and Environmental Microbiology, August 2001, p. 3440-3444, Vol. 67, No. 8
Laboratoire d'Ecologie Microbienne, UMR CNRS
5557, Université Lyon I,1 and
Libragen,3 69622 Villeurbanne Cedex,
France, Centre de Génie Electrique de Lyon, UPRESA CNRS
5005, Ecole Centrale de Lyon, 69131 Ecully
Cedex,2 and Aventis Crop Science, 69623 Lyon,4 France
Received 16 January 2001/Accepted 18 May 2001
Electrical fields and current can permeabilize bacterial membranes,
allowing for the penetration of naked DNA. Given that the environment
is subjected to regular thunderstorms and lightning discharges that
induce enormous electrical perturbations, the possibility of natural
electrotransformation of bacteria was investigated. We demonstrated
with soil microcosm experiments that the transformation of added
bacteria could be increased locally via lightning-mediated current
injection. The incorporation of three genes coding for antibiotic resistance (plasmid pBR328) into the Escherichia
coli strain DH10B recipient previously added to soil was
observed only after the soil had been subjected to laboratory-scale
lightning. Laboratory-scale lightning had an electrical field gradient
(700 versus 600 kV m Ongoing sequencing and
comparison of bacterial genomes are gradually modifying our
understanding of how bacteria evolved. Although earlier ideas included
a point mutation-based evolution occurring slowly and regularly, new
theories propose a more erratic evolution in which drastic changes in
the genome are due to irregular acquisition of new genetic information
by horizontal gene transfers (HGT) (13). However, the
frequency of HGT would have had to be so high during bacterial
evolution that some evolutionists are questioning the accuracy of the
phylogenetic analyses (5). Moreover, these analyses
underestimate the actual number of transfers by missing the
oldest events. Their efficiency is also limited to the transferred
genes, which were successfully fixed in a microbial population by
increasing the overall fitness. These sequence-based tools also miss
the great majority of transfer events that conferred neutral or
deleterious traits and therefore were subsequently deleted. In
addition, numerous microcosm-based investigations devoted to studying
these events, and specifically natural genetic transformation in
environments, such as soil, sediment, and water, conclude that HGT
would occur at extremely low frequencies (10, 15).
Natural transformation of bacteria in soil by extracellular DNA is a
multistep process, precluding its occurrence at high frequency
(15). When released into the soil at the death of organisms (or more actively for some bacteria), naked DNA has to avoid
both enzymatic degradation and irreversible adsorption onto soil
particles (4). Moreover, when taken up into the cell, transforming DNA still has to resist the numerous restriction and
modification mechanisms and to be integrated into the host genome via
homologous or illegitimate recombination (or to replicate autonomously). The intermediate step between these extra- and intracellular states corresponds to the transformation mechanism sensu
stricto. When genetically encoded, this mechanism requires the
bacterial cells to be in a competent state, which is another major
limitation of transformation in situ (15).
The discrepancy between databases that indicate HGT has occurred
frequently (13) in the past and the extremely low
frequency measured in the environment (10, 15) has led to
questions about whether experiments have targeted the appropriate
bacteria, the important environmental habitats, and/or the correct
processes. For instance, the soil bacterium Ralstonia
solanacearum, a plant pathogen, exhibits a potential for HGT
several orders of magnitude higher in plant tissues than in bulk soils
(3). This is due to the rapid and extensive multiplication
of the pathogen, leading to the development in situ of the
physiological state of genetic competence. As a second example, some
transformants of Escherichia coli, a bacterium which is not
fitted with the appropriate molecular machinery to develop competence,
were detected in freshwater, indicating that transformation can also be
physically or chemically induced in situ (1). Therefore,
our objective was to evaluate the possibility of other processes being
involved in HGT.
Considerable data have already been collected concerning the mechanism
and efficiency of gene exchange in laboratory devices using electrical
fields and currents (6, 9, 11, 20). Thus, given that the
environment is regularly subjected to thunderstorms and lightning
discharges, our objective was to investigate whether the resulting
electrical perturbations could lead to the "natural" transformation
of bacteria. Thunderstorm development is a process which includes a
progressive accumulation of storm clouds followed by lightning
discharges. The electrical parameters related to each of these steps
have been investigated extensively and are now well characterized
(2). An electrical potential difference builds up
gradually with cloud growth. In temperate climates, clouds are
positively charged in the upper zone and negatively charged at the
bottom, resulting in a modification of the charge and of the electrical
field distribution on the ground. The voltage difference between the
cloud and the ground can reach up to 100 MV, corresponding to values
around 16 kV m
0099-2240/01/$04.00+0 DOI: 10.1128/AEM.67.8.3440-3444.2001
Copyright © 2001, American Society for Microbiology. All rights reserved.
Laboratory-Scale Evidence for Lightning-Mediated Gene
Transfer in Soil
![]()
ABSTRACT
Top
Abstract
Introduction
Materials and Methods
Results and Discussion
References
1) and current density (2.5 versus
12.6 kA m
2) similar to those of full-scale lightning.
Controls handled identically except for not being subjected to
lightning produced no detectable antibiotic-resistant clones. In
addition, simulated storm cloud electrical fields (in the absence of
current) did not produce detectable clones (transformation detection
limit, 10
9). Natural electrotransformation might be a
mechanism involved in bacterial evolution.
![]()
INTRODUCTION
Top
Abstract
Introduction
Materials and Methods
Results and Discussion
References
1 (0.016 kV
mm
1) for flat ground surfaces, increasing
considerably locally due to a tip effect (up to 0.7 kV
mm
1) (Table 1).
Our experimental objectives were to determine whether these electrical
fields related to cloud accumulation could be involved in the genetic
transformation of bacteria, and if not alone, perhaps with the addition
of electrical current in the form of lightning. Lightning discharges to
the soil are characterized by an injection of current with the peak
current intensity of the flashes varying from 10 to 200 kA
(2), which is considered to flow through about 2 m2 of soil surface. On average, this results in
about 13 kA m
2 (Table 1). Our initial approach
reported here was to test the possibility of this in situ
electrotransformation by subjecting artificially seeded soil microcosms
to electrical perturbations simulating both storm cloud electrical
fields and lightning.
TABLE 1.
Comparison of electrical parameters, averaged over the
current injection period, between electroporation and artificial
and natural lightninga
| |
MATERIALS AND METHODS |
|---|
|
|
|---|
The tests under simulated storm cloud electrical fields and lightning were performed in soil microcosms seeded with bacteria and plasmids. The laboratory-scale lightning system first simulated charge build up in clouds and then the lightning itself. Afterwards, selective medium was used in order to count those bacteria which had acquired the antibiotic resistance encoded by the plasmid. All of these components are described below. In addition, some comparison was made with electroporation in the presence and absence of soil.
Soil microcosms.
Microcosms consisted of 50-mm-diameter
petri dishes in which were placed 30 g (soil thickness, 10 mm) of
air-dried and sieved (pore size, 2 mm) samples of a sandy loam
soil (sand, 50%; silt, 41%; clay, 9%; organic matter, 40.6 g
· kg of dry soil
1; pH 6.8) collected at La
Côte Saint André (Isère, France). We adapted the
petri dishes to conduct electricity by sticking a steel wire through a
hole in the bottom of the dish and then placing a round piece of
aluminum paper inside the dish on the bottom. Thus, the wire went from
the aluminum foil at the bottom of the petri dish, through the hole in
the dish bottom and out to where it could be used as an electrical
ground in the simulated-lightning experiments. Sterile soil conditions
were obtained by gamma irradiating the microcosms with a 25-kGy dose
from a 60Co source (Conservatome, Dagneux,
France). The moisture content for cloud and lightning simulation tests
was 10% (wt/wt). The target moisture was achieved in part during the
bacterial and plasmid inoculation (2.5 ml per 30 g of dried soil)
and in part by adding sterile deionized water (0.5 ml per 30 g of
soil). The soil pH after inoculation and immediately before being
subjected to simulated lightning was maintained at 6.8. The soil
samples were inoculated with 2.5 ml of the bacterial suspensions and
mixed with a sterile pipette. Bacterial suspensions were made based on
the required final bacterial concentrations in the soil microcosms, which were 107, 108,
109, and 1010 cells g of
dry soil
1. Each bacterial concentration was
tested at least three times. The seeded soil samples were incubated at
28°C for 18 h before 100 µl of a
10-µg-ml
1 plasmid pBR328 (coding for
resistance to ampicillin, chloramphenicol, and tetracycline) solution
was added to the soil just prior to the lightning treatment. The
controls were (i) soil with the added bacteria but without the plasmid,
(ii) soil with both bacteria and plasmid added but not subjected to
lightning, and (iii) soil with nothing added. Both sterile and
nonsterile soils were tested.
Inoculum and plasmid preparation. The inoculum of Escherichia coli strain DH10B (Life Technologies, Cergy, France) was prepared by picking a colony maintained on agar and incubating it in 100 ml of liquid medium (Luria-Bertani [LB] medium) overnight, and then 2 ml of the culture was placed in 500 ml of LB medium and incubated for about 8 h. When the optical density (at 580 nm) of the liquid culture reached 1, the liquid was centrifuged for 15 min at 6,500 × g before resuspension in the appropriate volume of 0.8% NaCl in order to achieve the targeted final concentration in soil. Confirmation that E. coli strain DH10B could not be naturally transformed in vitro was done by mixing 40 µl of plasmid pBR328 DNA (Boehringer Mannheim, Meylan, France) and recipient cells on GTTP filters (Millipore, Bedford, Mass.) on solid LB medium. After incubation for 24 h at 37°C, the filters were resuspended in 2 ml of pure sterile water, and the suspensions were plated on selective medium (LB medium containing, per liter, ampicillin, 100 mg; chloramphenicol, 30 mg; and tetracycline, 12.5 mg). The plasmid pBR328 was isolated from E. coli by using the plasmid extraction kit from Qiagen Inc. (Chatsworth, Calif.).
Simulation of cloud-induced electrical field.
When only the
electrical field associated with clouds was tested without lightning,
conditions corresponding to natural cloud-induced electrical fields
were simulated by subjecting seeded soil samples to a static electrical
field created through a large planar capacitor structure; the distance
between the electrodes was 0.25 m. The apparatus was capable of
delivering DC voltages ranging from 4 to 140 kV. In these experiments,
when 140 kV (Vcrest) was used over the
250 mm between electrodes, the gradient
(Ecrest) was about 0.56 kV
mm
1, which is similar to that of storm clouds
(about 0.6 kV mm
1) that produce lightning
(Table 1). Soil samples were exposed to this field for different
periods (1, 5, 10, and 60 min).
Lightning simulation. The experimental system was based on a high-voltage generator which could deliver impulses of up to 1 MV with 50 kJ of energy. This generator was constructed in order to test the performance of the high-voltage apparatus and the ability of different electronic equipment to survive lightning hits (A. Ben Rhouma, P. Auriol, and P. Dumas, Proc. 9th Int. Symp. High Voltage Eng., abstr. 7630, 1995). For the soil application, the current flowed from an electrode through the soil to the aluminum foil at the bottom of the petri dish, which was sitting directly on a solid bronze disk (0.5 m in diameter and 2 cm thick) which itself was sufficiently grounded for the applied current. The electrode was a cylindrical cell (bronze; 2.5 cm in diameter and 3.5 cm high) that was capable of applying voltage impulses up to 8.9 kV with a time constant value equal to 6 ms. Under these conditions, the current flowing through the soil can reach more than 6 A. For typical natural lightning, the duration of the current impulse of each return stroke can vary significantly from 0.1 to 1 ms (19).
Detection of transformants. Following the lightning discharge, a subsample of soil (approximately 2 g) was recovered and treated with DNase I (Boehringer, Mannheim, Germany) to degrade any persistent extracellular DNA (incubation for 2 h at 28°C with 1,000 U of DNase I). Detection protocols consisted of either (i) quantitative analysis by direct plating of part of the soil subsample (and dilutions of the subsample with the selective medium) on selective medium (LB medium containing, per liter, ampicillin, 100 mg; chloramphenicol, 30 mg; tetracycline, 12.5 mg; and, in order to inhibit fungal growth, amphotericin B, 1.25 mg) to enumerate transformants or (ii) qualitative analysis by incubating the whole 30 g of soil in the microcosm overnight at 28°C in 20 ml of selective medium before plating 100 µl five times on selective medium. Although this technique did not allow exact counting of transformants, it increased detection sensitivity, as any transformants could develop over the incubation period and therefore its theoretical detection limit was 1 transformant per 30 g of soil. Any apparent transformants were confirmed to contain the added plasmid by using a plasmid extraction kit (Qiagen Inc.) according to the manufacturer's instructions. For experiments with sterile soils, recipient bacteria (both those that had incorporated the plasmid and those that had not) were enumerated on LB medium.
Electroporation.
Electrocompetent cells of E. coli strain DH10B were prepared as described by Drury
(7). Electroporations were carried out with a gene pulser
apparatus (Bio-Rad Laboratories, Richmond, Calif.) by using 40 µl of
recipient cells mixed with 1 µl of plasmid pBR328 solution (100 mg
liter
1), incubated 1 min on ice, and
electroporated in a 0.2-cm-diameter cuvette at 1.2 kV
mm
1 (crest value) for 4 to 5 ms. LB medium (960 µl) was then immediately added, and the suspension was incubated for
1 h at 37°C before the dilutions were plated on both LB medium
alone and LB medium with antibiotics (as described above) to estimate
survival and transformation frequencies, respectively. In addition, in
order to try to incorporate the soil aspect in the electroporation
tests, 75 mg of sterile soil was placed in the electroporation cuvette, 41 µl of the bacterium-plasmid suspension was added, and then an
additional 75 mg of soil was added before the electroporation was performed.
Comparison of electrical parameters for electroporation and
lightning current propagation in soils.
Three electrical
parameters were used to compare the two laboratory-scale systems
(electroporation and simulated lightning) and full-scale lightning
(Table 1). The first parameter was the crest value of the electrical
field (Ecrest) which is obtained for
natural conditions by dividing the maximum electrical tension value
reached during the electrical impulse by the electrode distance (Vcrest/d) or, for natural
lightning, by multiplying the maximum value of the current density by
the electrical resistivity of the soil tested
(Jcrest ×
). The second parameter
was the crest value of the current density
(Jcrest), which corresponds to the maximal current intensity divided by the cell cross section
(Icrest/s), which provides
data that can compare systems of different size scales. The third
parameter was the amount of electrical charge flowing through the cell
for a 1-m2 surface
(
j(t)dt). The
laboratory conditions simulated very closely those occurring in soil
during a lightning discharge. The crest values of the electrical field
(Ecrest) were nearly identical for
natural and artificial lightning and differed by less than a factor of
2 for electroporation. The crest values of the current densities
(Jcrest) and the amounts of charge
flowing through the soil were similar for the three different
conditions in a range from 4 to 22 C m
2,
although the surface area and volume of soil for natural lightning could be determined only approximately. The variations in Table 1 are
not significant with respect to our hypothesis when it is realized
that, during the lightning event, considerable variation in these
values occurs over the soil area hit by lightning (2, 19).
| |
RESULTS AND DISCUSSION |
|---|
|
|
|---|
Thunderstorm-related electrical parameters and potential biological
effects.
Simulated storm cloud electrical fields subjected soil
seeded with recipient bacteria, E. coli strain DH10B, and
donor DNA, plasmid pBR328, to static electrical fields as described
above. These experiments failed to provide any detectable transformants under the various conditions tested, which included a range of recipient bacterium concentrations (from 107 to
1010 g of dry soil
1),
donor DNA concentrations (from 1 to 100 µg of plasmid pBR328 g of dry
soil
1), and amplitudes (from 0.16 to 0.6 kV
mm
1) and durations (1 to 60 min) of the
generated electrical field. These results are consistent with the lack
of transformants in vitro when the electroporation cuvette was modified
to subject the bacteria only to electrical fields but without current.
The efficiencies of transformation of E. coli strain DH10B
(expressed as the number of transformants relative to that of recipient
cells) by 0.5 µg of plasmid pBR328 DNA dropped from 1.3 × 10
5 with standard electroporation conditions to
less than 7 × 10
9 (the detection limit)
with modified conditions, indicating the requirement for electrical
current in order to produce DNA transfer. These results imply that the
accumulation of clouds alone (an electrical field without current)
might not have any significant effect on HGT.
Artificial-lightning-related electrotransformation of bacteria in soil. Experiments were developed in order to subject soil samples seeded with recipient bacteria and donor DNA to laboratory-scale lightning delivered by a high-tension generator. The use of a non-naturally transformable bacterium such as E. coli DH10B and a plasmid harboring three antibiotic resistance marker genes (pBR328) allowed the easy detection of transformants.
Transformants were detected in all samples containing from 105 to 109 recoverable bacterial cells g of dry soil
1 when the plasmid
concentration was greater than 0.1 µg of DNA g of dry
soil
1 (Table 2).
When the plasmid concentration was 0.1 µg of DNA g of dry
soil
1, transformants were detected
qualitatively, but rarely in sufficient number to quantify the
transformation frequency (Table 2). The qualitative method appeared to
be quite sensitive to the presence of transformants, thus increasing
the certainty that "no-lightning" controls did not produce any
transformants (Table 2). Controls with lightning but without the
plasmid also lacked any detectable transformants. When nonsterile soils
were tested, E. coli DH10B was unable to maintain its
population at elevated levels, and therefore, the actual target
bacterial population was not identified and no clones were observed by
the quantitative method, although the qualitative method did provide
evidence of transformants.
|
Estimation of HGT levels in soils subjected to natural lightning. The experimental results indicate that bacteria in soils are affected by lightning-related electrical parameters, which, like those delivered by a standard electroporator, increase their permeability to extracellular DNA. The soils in our microcosms were homogenized in order to have the current delivered homogeneously throughout the soil sample. On the other hand, the current delivered by lightning discharges is going to flow along channels of reduced resistivity. These channels are characterized by very high current densities and a considerable increase in temperature, possibly subjecting bacteria to irreversible damage and death. Nevertheless, the magnitudes of the electrical parameters (current density and electrical field) decreases with distance from the axis of these conducting channels, creating electrical and thermic conditions compatible with bacterial survival and potentially with electrotransformation in a large volume of the soil surrounding these "overstressed" areas. Therefore, most lightning discharges would provide transformation-inducing electrical conditions at some places in the soil, independent of its structure, texture, and matrix characteristics, similar to that described here for the laboratory-scale lightning.
Another critical aspect of lightning-induced gene transfers in nature is the state of natural extracellular donor DNA. Significant amounts of indigenous extracellular DNA in a range from 5 to more than 35 µg g of dry soil
1, depending upon the soil
composition, can be routinely detected and even extracted
(8). There are, however, few data on the transformation
potential of these natural molecules. Even when a significant part of
the DNA inoculated into nonsterile soils is rapidly degraded, another
fraction could persist by adsorption onto soil particles and remain
available to transformation mechanisms (4, 18). Moreover,
the closed microhabitats due to soil aggregation (16) in
which most indigenous soil bacteria develop, die, and release DNA might
be much more favorable to natural electrotransformation than conditions
outside the soil aggregate. The electrophoretic forces that are
hypothesized to drive DNA into the transforming cells (11,
12) might be involved in the desorption of DNA molecules from
soil particles (14), contributing to their increased availability. Also, intracellular DNA present in living, dying, and
dead cells could be a major source of donor DNA, in addition to
extracellular DNA, based on evidence that electroporation was efficient
in vitro in generating protoplast fusion (17) and even in
transferring DNA between living bacterial cells (9). Finally, given that cells from nearly all bacterial taxa can be electroporated more or less efficiently and independently of their physiological state and with transforming DNA of prokaryotic or eukaryotic origin, the universality of this process needs to be considered.
Based on these varied experimental and theoretical data, the frequency
of natural lightning-mediated gene transfers in soils might not be
vastly different from a value of 10
9 resulting
from our simulation experiments (Table 2). Natural lightning discharges
are spread over 0.5 to 4 m3 of soil containing
more than 1012 to 1013
indigenous bacterial cells potentially affected by the electrical parameters, thus providing a theoretical number of transformants up to
104 at each discharge. The hundreds of lightning
flashes subjecting the environment to thousands of coulombs each second
on a world-wide scale could be participating in bacterial adaptation
and evolution.
| |
ACKNOWLEDGMENTS |
|---|
Thanks are expressed to Philippe Normand and Xavier Nesme (University of Lyon I) for fruitful discussions and a critical reading of the manuscript and to Stéphane Peyrard and Van Tran Van for technical assistance.
This work was supported by a grant from the Ministére de l'Education Nationale et de la Recherche et de la Technologie to S.D. and was part of a project funded by the Biotechnology Program (MENRT).
| |
FOOTNOTES |
|---|
* Corresponding author. Mailing address: Laboratoire d'Ecologie Microbienne, UMR 5557, Université Lyon I, 43 Blvd. du 11 Novembre 1918, 69622 Villeurbanne Cedex, France. Phone: 33 4 72 44 82 89. Fax: 33 4 72 43 12 23. E-mail: simonet{at}biomserv.univ-lyon1.fr.
| |
REFERENCES |
|---|
|
|
|---|
| 1. | Baur, B., K. Hanselmann, W. Schlimme, and B. Jenni. 1996. Genetic transformation in freshwater: Escherichia coli is able to develop natural competence. Appl. Environ. Microbiol. 62:3673-3678[Abstract]. |
| 2. | Ben Rhouma, A., and P. Auriol. 1997. Modelling of the whole electric field changes during a close lightning discharge. J. Phys. D 30:598-602[CrossRef]. |
| 3. | Bertolla, F., A. Frostegard, B. Brito, X. Nesme, and P. Simonet. 1999. During infection of its host, the plant pathogen Ralstonia solanacearum naturally develops a state of competence and exchanges genetic material. Mol. Plant-Microbe Interact. 12:467-472. |
| 4. |
Demanèche, S.,
L. Jocteur-Monrozier,
H. Quiquampoix, and P. Simonet.
2001.
Evaluation of biological and physical protection against nuclease degradation of clay-bound plasmid DNA.
Appl. Environ. Microbiol.
67:293-299 |
| 5. |
Doolittle, W. F.
1999.
Phylogenetic classification and the universal tree.
Science
284:2124-2129 |
| 6. |
Dower, W. J.,
J. F. Miller, and C. W. Ragsdale.
1988.
High efficiency transformation of E. coli by high voltage electroporation.
Nucleic Acids Res.
16:6127-6145 |
| 7. | Drury, L. 1996. Transformation of bacteria by electroporation, p. 249-256. In A. Harwood (ed.), Methods in molecular biology. Humana Press Inc., Totowa, N.J. |
| 8. |
Frostegard, A.,
S. Courtois,
V. Ramisse,
S. Clerc,
D. Bernillon,
F. P. Le Gall,
P. Jeannin,
X. Nesme, and P. Simonet.
1999.
Quantification of bias related to the extraction of DNA directly from soils.
Appl. Environ. Microbiol.
65:5409-5420 |
| 9. |
Gilchrist, A., and J. Smit.
1991.
Transformation of freshwater and marine caulobacters by electroporation.
J. Bacteriol.
173:921-925 |
| 10. |
Lorenz, M. G., and W. Wackernagel.
1994.
Bacterial gene transfer by natural genetic transformation in the environment.
Microbiol. Rev.
58:563-602 |
| 11. | Lurquin, P. F. 1997. Gene transfer by electroporation. Mol. Biotechnol. 7:5-35[Medline]. |
| 12. | Neumann, E. 1992. Membrane electroporation and direct gene transfer. Bioelectrochem. Bioenerg. 28:247-267[CrossRef]. |
| 13. | Ochman, H., J. G. Lawrence, and E. A. Groisman. 2000. Lateral gene transfer and the nature of bacterial innovation. Nature 405:299-304[CrossRef][Medline]. |
| 14. | Paget, E., L. Jocteur Monrozier, and P. Simonet. 1992. Adsorption of DNA on clay minerals: Protection against DNase I and influence on gene transfer. FEMS Microbiol. Lett. 97:31-40[CrossRef]. |
| 15. | Paget, E., and P. Simonet. 1994. On the track of natural transformation in soil. FEMS Microbiol. Ecol. 15:109-118. |
| 16. | Ranjard, L., F. Poly, J. Combrisson, A. Richaume, and S. Nazaret. 1998. A single procedure to recover DNA from the surface or inside aggregates and in various size fractions of soil suitable for PCR-based assays of bacterial communities. Eur. J. Soil. Biol. 34:89-97. |
| 17. | Reed, W. M. 1987. Protoplast fusion of Lactobacillus acidophilus and Streptococcus lactis via electric field or chemical induction. J. Gen. Appl. Microbiol. 33:287-294. |
| 18. |
Romanowski, G.,
M. G. Lorenz,
G. Sayler, and W. Wackernagel.
1992.
Persistence of free plasmid DNA in soil monitored by various methods, including a transformation assay.
Appl. Environ. Microbiol.
58:3012-3019 |
| 19. | Uman, M. A. 1987. The lightning discharge. Int. Geophysics Ser. 39:137. |
| 20. | Weaver, J. C., and Y. A. Chizmadzhev. 1996. Theory of electroporation: A review. Bioelectrochem. Bioenerg. 41:135-160. |
This article has been cited by other articles:
| |||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
Copyright © 2009 by the American Society for Microbiology. For an alternate route to Journals.ASM.org, visit: http://intl-journals.asm.org | More Info»