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Applied and Environmental Microbiology, October 2000, p. 4361-4365, Vol. 66, No. 10
0099-2240/00/$04.00+0
Copyright © 2000, American Society for Microbiology. All rights reserved.
Bacterial Functional Redundancy along a Soil Reclamation
Gradient
Bei
Yin,1
David
Crowley,2
Gerd
Sparovek,3
Wanderley Jose
De
Melo,4 and
James
Borneman1,*
Department of Plant
Pathology1 and Department of
Environmental Sciences,2 University of
California, Riverside, California 92521, and Department of
Soil Science, ESALQ, University of Sao Paulo, Piracicaba CP 9, CEP
13.418.900,3 and Department of
Technology, Universidade Estadual Paulista, Jaboticabal, SP, CEP
14870-000,4 Brazil
Received 17 March 2000/Accepted 18 July 2000
 |
ABSTRACT |
A strategy to measure bacterial functional redundancy was developed
and tested with soils collected along a soil reclamation gradient by
determining the richness and diversity of bacterial groups capable of
in situ growth on selected carbon substrates. Soil cores were collected
from four sites along a transect from the Jamari tin mine site in the
Jamari National Forest, Rondonia, RO, Brazil: denuded mine spoil, soil
from below the canopy of invading pioneer trees,
revegetated soil under new growth on the forest edge, and the forest
floor of an adjacent preserved forest. Bacterial
population responses were analyzed by amending these soil samples with
individual carbon substrates in the presence of bromodeoxyuridine
(BrdU). BrdU-labeled DNA was then subjected to a 16S-23S rRNA
intergenic analysis to depict the actively growing bacteria from each
site. The number and diversity of bacterial groups responding to four
carbon substrates (L-serine, L-threonine, sodium citrate, and
-lactose hydrate) increased along the
reclamation-vegetation gradient such that the preserved forest soil
samples contained the highest functional redundancy for each substrate.
These data suggest that bacterial functional redundancy
increases in relation to the regrowth of plant communities and may
therefore represent an important aspect of the restoration of soil
biological functionality to reclaimed mine spoils. They also suggest
that bacterial functional redundancy may be a useful indicator of soil
quality and ecosystem functioning.
 |
INTRODUCTION |
Identification of microbial
community characteristics that influence terrestrial ecosystem
performance is of considerable importance to ecology and conservation
biology. One long-standing assumption has been that ecosystem stability
and productivity are influenced by biodiversity (7, 16).
This concept has been particularly well supported by empirical studies
on plant communities (8, 15, 23, 31). For example, a
long-term study of grasslands showed that more diverse plant
communities were more resistant to a major drought
(24). Recently, this concept has been extended to
below-ground diversity, in which species loss at various trophic
levels was shown to negatively influence several parameters such
as respiration and organic-matter decomposition (19). When
assessing biodiversity, meaningful characterization must consider
not only the number and distribution of species but also
functional diversity and redundancy. Functional diversity can be
defined as the number of distinct processes or functions that are
carried out by a community, whereas functional redundancy is a
measure of the number of different species within the various
functional groups or guilds (10).
One of the best community-based approaches for indexing the functional
diversity of microbial communities has been the use of substrate or
metabolic fingerprinting. Here, microbial communities are typically
screened for their ability to utilize selected carbon substrates by
using MicroPlates (Biolog, Hayward, Calif.) (9, 33). A
potential limitation of this strategy is that the substrate utilization
patterns are examined in liquid media, which may introduce a culture
bias that can vary depending on the medium used (20, 22).
This bias may lead to a depiction of the functional diversity that does
not reflect the natural microbial community, since the majority of
microorganisms cannot be ready cultured in standard media. An
alternative technique that avoids this bias characterizes substrate
utilization patterns by measuring CO2 respiration after selected carbon substrates are added to soil (5).
Although potentially an important ecosystem performance parameter,
functional redundancy of microbial communities has not been well
studied. Culture-based methods have been used to study the impact of
heavy metals on the numbers of different species that are capable of
using selected rare substrates (28). This work showed that
elevated heavy metal levels resulted in a decline in the number of
different microorganisms that used these substrates. It also provided
the basis for concern about decreased reliability in the degradation of
possibly toxic compounds that might eventually accumulate to
undesirable levels in soils. Similar concern could also be expressed
about any activity that causes a disturbance or decline in functional redundancy.
This report presents a culture-independent strategy to examine
bacterial functional redundancy and tests its use with soils collected
along a vegetation gradient on reclaimed mine spoils. This study
focused on a tin mine spoil in Rondonia, Brazil, at a location that has
proved to be extraordinarily difficult to revegetate. On this site,
natural revegetation follows a pattern in which a few pioneer tree
species eventually become established in spot locations and begin to
deposit organic matter on the soil surface. Revegetation also proceeds
from the forest edge, where there is dense plant growth due to the
availability of light and seeds and from organic-matter deposition. As
the forest is reestablished, the canopy closes between the pioneer
community and the old forest growth. Introduction of organic matter
along the vegetation gradient should increase the range of different
niches that can be occupied by soil microorganisms. It was thus
hypothesized that functional redundancy of the soil bacterial community
on this mine spoil would increase in relation to the revegetation
pattern and plant succession. The site sampled within the preserved
forest had been previously characterized as one that was unusually rich
in organic matter, a consequence of its prior prehistoric use as an
Amazon Indian settlement. These anthropogenic soils (terra preta)
resulted from hunting, gardening, and agroforestry and are
distinguished by deep organic-rich soil profiles (6).
Other survey evidence in this area suggests that the Indian group
Karitiana, described as a small remnant population from Northern
Amazonas (4), probably developed the site. The soil transect
across the revegetation gradient thus provided a particularly
interesting sample set for testing of the functional-redundancy analysis.
 |
MATERIALS AND METHODS |
Soil collection.
Four intact soil cores measuring 10 cm deep
and 8 cm wide were collected using individual sterile soil-coring
devices that encase the soil in a stainless steel sleeve with a
removable ring on both the top and bottom of the core. The sleeved soil
samples were then excavated, and the top and bottom rings were removed so that the interfacing soil at either end could be aseptically removed. The cores were then wrapped in aluminum foil and placed in
boxes for transport to the laboratory. The soil cores were shipped to
the laboratory at the University of California, Riverside, which
required 3 days, and were then frozen at
70°C until used in the
experiment. Soil cores were collected from denuded mine spoil
approximately 100 m from the forest edge (soil site 1); from
underneath a pioneer tree, Cecropia sciadophylla, in the same location (soil site 2); from the forest edge in dense vegetation (soil site 3); and from a prehistoric Amazon Indian archaeological site
in the adjacent, mature preserved forest (soil site 4) (Fig. 1). The first three soils consisted of a
coarse mine spoil material consisting largely of crushed rock and sand.
The soil from the archeological site was characterized by a deep,
organic matter-enriched A soil horizon that was approximately 1 m
thick and overlaid a clay ultisol in the B horizon. In the laboratory,
soil samples that had been stored at
70°C were taken from the
freezer, removed from the cores, sieved to pass a 1.0-mm screen, and
then air dried at 30°C.

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FIG. 1.
Soil collection sites for samples analyzed in this
study. The x and y axes designate the map
coordinates for this site: 1, bare mine spoil approximately 100 m
from the forest edge; 2, mine spoil from underneath a pioneer tree,
Cecropia sciadophylla; 3, mine spoil from the forest edge in
dense vegetation; and 4, undisturbed soil from a prehistoric Amazon
Indian archaeological site in mature preserved forest.
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Soil incubation and DNA extraction.
Soil samples (0.5 g)
were amended with 5 mg of a single carbon substrate (either
L-serine, L-threonine, sodium citrate, or
-lactose hydrate), 5 µl of 100 mM bromodeoxyuridine (BrdU), and 60 µl of H2O and incubated in petri dishes (60 by 15 mm) at
room temperature in the dark. After 24 h, DNA was extracted from
the soil samples with the FastDNA Kit for Soil as described by the manufacturer (Bio 101, Vista, Calif.).
Immunocapture of BrdU-labeled DNA.
Immunocapture of
BrdU-labeled DNA was performed by a modification of previously
described methods (2, 27). A 9-µl volume of herring sperm
DNA (0.63 mg per ml in phosphate-buffered saline [PBS]) was heated at
95°C for 5 min, quickly cooled on ice for 5 min, mixed with 1 µl of
anti-BrdU antibody (Boehringer Mannheim, Indianapolis, Ind.), and
rotated at room temperature in the dark for 30 min. An 8-µl volume of
BrdU-labeled DNA was combined with 2 µl of PBS, heated at 95°C for
5 min, quickly cooled on ice for 5 min, mixed with the herring sperm
DNA-anti-BrdU antibody mixture, and rotated at room temperature for 30 min in the dark. Dynabeads (M-450) coated with sheep anti-mouse
immunoglobulin G (3.13 µl) were washed once with 50 µl of PBS
containing 0.1% bovine serum albumin per ml (PBS-BSA) as described by
the manufacturer (Dynal, Lake Success, N.Y.), resuspended in 3.13 µl
of PBS-BSA, and added to the BrdU-labeled DNA-anti-BrdU antibody
mixture. This was rotated at room temperature for 30 min in the dark
and washed three times each with 100 µl of PBS-BSA using magnetic
separation. The pellets were resuspended in 10 µl of 1.7 mM BrdU in
PBS-BSA and rotated at room temperature for 30 min in the dark, and the
BrdU-labeled DNA fraction (supernatant) was collected by magnetic separation.
Community structure analysis.
Bacterial 16S-23S rRNA
intergenic fragments were amplified in 10 µl of PCR mixture
containing the following final concentrations or amounts: 1 µl of
immunocaptured DNA or 1 µl of 1:40-diluted uncaptured soil DNA, 50 mM
Tris (pH 8.3), 2.5 mM MgCl2, 500 µg of BSA per ml, 250 µM concentrations of each deoxynucleoside triphosphate, 2 µM
forward primer 1406F (TGYACACACCGCCCGT) (11), 4 µM
reverse primer 23SR (GGGTTBCCCCATTCRG) (3), and 5 U of
Taq DNA polymerase. All reagents were combined and heated at
94°C for 2 min. Thirty-five cycles of PCR were performed at 94°C
for 0 s, 52°C for 10 s, and 72°C for 30 s, followed
by one episode at 72°C for 2 min. PCRs were performed in 10-µl
glass capillary tubes with a model 1002 Rapidcycler (Idaho
Technologies, Idaho Falls, Idaho).
Functional-redundancy analysis.
The 16S-23S rRNA
intergenic-region PCR products were resolved by electrophoresis on 2%
agarose gels and photographed. The DNA-banding profiles obtained from
the photographs were converted into computer digital images using an
image scanner. A peak analysis was performed to resolve the individual
peaks and quantify the band intensities using Scion Image (Scion Corp.,
Frederick, Md.). The number and diversity of bacteria capable of
utilizing each substrate were estimated by using the number of bands as
a representation of the number of different organisms (richness) and
the intensity of the bands as the number of individuals within an
organism type. The diversity index used was Shannon's index:
H = 
(ni/N) ln (ni/N), where ni is the
area of each peak and N is the sum of all peak area.
 |
RESULTS AND DISCUSSION |
A culture-independent strategy to measure bacterial functional
redundancy in environmental samples was developed. This approach is an
extension of the aforementioned Biolog (9) and
CO2 respiration (5) methods combined with a
technique that permits the identification of actively growing bacteria
(2). A carbon substrate and the thymidine analog BrdU are
added to soil (Fig. 2). After incubation, the organisms that grow in response to the amendment are identified by
a community structure analysis of the BrdU-labeled DNA, which is
isolated by immunocapture. In this study, the bacterial community analyses were performed by resolution of PCR amplified 16S-23S rRNA
intergenic-region fragments on 2% agarose gels, where the size
heterogeneity of these fragments provides a simple method to depict
bacterial community structure (3). The number of DNA bands
provides a measure of the number of different organisms (richness),
while the intensity of each band represents the number of individuals
within an organism type. Since functional redundancy can be defined as
the number of different species that perform a specified function, the
richness of bacteria capable of utilizing a selected substrate can be
used as a measure of this parameter. An alternative measure of
functional redundancy can be obtained by measuring the bacterial
diversity instead of the richness, providing an accounting of both the
number of different organisms that perform a specified function and
their distribution.
A test of the functional-redundancy analysis was done on four soils
taken along a vegetation gradient from a tin mine site in Brazil which
had been subjected to strip mining of the overburden (Fig. 1). With the
exception of the preserved forest soil adjacent to the mine, the soil
at this location was severely disturbed and depleted of organic matter
since all of the overburden was processed by crushing, sieving, and
washing of the gravel, which was then replaced over the mine spoil with
no further amendments or topsoil. Several attempts to revegetate
this site by tree plantings had failed, although after several
years a few pioneer species had become established. For the
functional-redundancy analysis, four different carbon substrates were
selected: two amino acids, L-serine and
L-threonine; one carboxylic acid, sodium citrate; and one
carbohydrate,
-lactose hydrate (Fig.
3A). The selected substrates are
representatives of different chemical groups commonly used in Biolog
MicroPlates. The community structure banding patterns show that the
soils capable of supporting more plant life also contain a greater
variety of bacteria that responded to the carbon substrate amendments.
The richness and diversity values, calculated from these data, confirm
this visual observation for all substrates (Fig.
4A).

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FIG. 3.
Bacterial community structure analysis of four soils
collected along a mine reclamation gradient in Rondonia, Brazil, were
performed on immunocaptured (A) and noncaptured (B) DNA. Lanes: 1, soil
site 1; 2, soil site 2; 3, soil site 3; 4, soil site 4. The carbon
substrates used were L-serine (S), L-threonine
(T), sodium citrate (C), and -lactose (L).
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FIG. 4.
Bacterial species richness and Shannon diversity indices
from four soils taken along a mine reclamation gradient were calculated
by using the community structure data from Fig. 3. Four substrate
amendments were used: L-serine ( ),
L-threonine ( ), sodium citrate ( ), and -lactose
( ). Values were obtained from immunocaptured (A) and noncaptured (B)
DNA. Error bars represent standard error measurements from three
replicate PCR experiments.
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For comparison, we also measured the total bacterial diversity of the
four soils by analyzing the uncaptured DNA isolated in the substrate
amendment experiments described in the previous paragraph. As expected,
the uncaptured DNA showed higher diversity and richness values (Fig.
4B) than did immunocaptured samples (Fig. 4A). The rDNA
fingerprints also showed that the four different carbon
amendments had little impact on the total bacterial communities within
each soil type (Fig. 3B) while revealing significant differences in the
populations that grew in response to the substrates (Fig. 3A). In
addition, these data showed that changes in soil quality, as evaluated
by the ability to support plant growth along the reclamation gradient,
correlated positively with bacterial functional redundancy whereas
total bacterial richness and diversity were relatively constant for all
soils except the denuded mine spoil (soil site 1). This result suggests
that bacterial functional redundancy increases in relation to the
regrowth of plant communities and may represent an important aspect of
the restoration of soil biological functionality to reclaimed mine
spoils in the Amazon forest.
Investigators in various disciplines such as agriculture, conservation,
and reclamation science have attempted to measure soil quality. Abiotic
measures of soil quality have included analyses of physical and
chemical parameters, whereas biotic indicators have included
measurements of enzyme activities, microbial biomass, and keystone
species and enumerations of culturable microorganisms on agar media.
Given the positive relationships between biodiversity and ecosystem
performance identified in other studies (see the introduction for
references), it may prove fruitful to use species diversity
(26) and functional redundancy (this report) as indicators of soil quality. The molecular approach of Torsvik et al.
(26) has been used to show that chemical pollutants decrease
the diversity of bacteria in soil (1) and marine sediment
(25). In our work, there was a clear positive correlation
between the bacterial functional redundancy of soils and the regrowth
of plant communities along a mine reclamation gradient. When evaluating
biological diversity, it is important to distinguish between these two
parameters, since changes in microbial diversity do not always
correspond to changes in functional redundancy (1) (see
above). Total bacterial diversity values provide a broad measure of
biological diversity, whereas functional diversity determinations yield
targeted assessments of the diversity within a functional group.
The extent and role of functional redundancy in microbial communities
are unknown. Its purpose and importance has been debated, with some
viewing it as an unnecessary luxury and others suggesting that it
promotes reliability and is therefore an essential component of
ecosystem productivity (12, 18, 31, 32). Determining the role of redundancy in ecosystem functioning is of significant importance and may provide the basis for more rational decisions concerning the value of biological diversity
(32). The work described in this report should advance
microbial ecology investigations by providing a new approach to examine
bacterial functional redundancy in soil. To optimize this strategy
toward a comprehensive functional-redundancy measurement, substrate
selection could encompass a wide range of chemical groups; for example,
the Eco MicroPlates (Biolog) use 31 different carbon substrates.
Alternatively, this strategy could be used for highly focused
investigations where only specific and narrowly defined substrates (not
necessarily carbon) are used (30).
One current limitation of this functional-redundancy method is the
resolving power of the community structure analysis. In this study, the
community data were obtained using ribosomal intergenic spacer analysis
(3). Other methods such as denaturing gradient gel
electrophoresis (17) and terminal restriction fragment
length polymorphism (13) could also be used. Unfortunately,
none of these methods can accurately depict the true diversity of
bacteria in a soil sample, since communities that may contain thousands of different species are resolved into approximately 10 to 50 groups. Thorough examination of rDNA clone libraries by extensive nucleotide sequence analysis, amplified rDNA restriction analysis (ARDRA) (14, 29), or future breakthroughs in DNA
microarray approaches may significantly increase the resolution of
this functional-redundancy analysis. Another potential limitation of
this method is the breadth of organisms that incorporate BrdU. A
definitive determination of this range will not be obtained without a
comprehensive examination of numerous bacteria from all taxonomic
groups. Thus far, with a few notable exceptions, it appears that the
majority of bacteria incorporate [3H]thymidine
(21). Since BrdU has been successfully used as a thymidine
analog in numerous applications, it is likely that most organisms will
also take up and incorporate BrdU. In addition, although the
purpose of this strategy is to identify the organisms that respond to
specified amendments, any organism that is growing at the time of the
analysis will also be identified. Finally, in this research we
attempted to preserve the soils as closely as possible by taking intact
cores and then minimizing storage and contamination problems by
freezing them. Ideally, samples such as these should be processed
immediately. Studies examining functional redundancy and community
structures will need to consider the best methods available for
preserving samples prior to their analysis.
 |
ACKNOWLEDGMENT |
We thank FAPESP (Fundação de Amparo à Pesquisa
do Estado de São Paulo) for financial support.
 |
FOOTNOTES |
*
Corresponding author. Mailing address: Department of
Plant Pathology, University of California, Riverside, CA 92521. Phone: (909) 787-3584. Fax: (909) 787-4294. E-mail:
borneman{at}ucrac1.ucr.edu.
 |
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Applied and Environmental Microbiology, October 2000, p. 4361-4365, Vol. 66, No. 10
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Copyright © 2000, American Society for Microbiology. All rights reserved.
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Hamasaki, K., Taniguchi, A., Tada, Y., Long, R. A., Azam, F.
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