- freely available
Diversity 2012, 4(4), 363-374; doi:10.3390/d4040363
Abstract: We characterized soil communities in the Mojave Desert across an elevation gradient. Our goal was to test the hypothesis that as soil quality improved with increasing elevation (due to increased productivity), the diversity of soil prokaryotes and nematodes would also increase. Soil organic matter and soil moisture content increased with elevation as predicted. Soil salinity did not correlate to elevation, but was highest at a mid-gradient, alluvial site. Soil nematode density, community trophic structure, and diversity did not show patterns related to elevation. Similar results were obtained for diversity of bacteria and archaea. Relationships between soil properties, nematode communities, and prokaryotic diversity were site-specific. For example, at the lowest elevation site, nematode communities contained a high proportion of fungal-feeding species and diversity of bacteria was lowest. At a high-salinity site, nematode density was highest, and overall, nematode density showed an unexpected, positive correlation to salinity. At the highest elevation site, nematode density and species richness were attenuated, despite relatively high moisture and organic matter content for the soils. Our results support emerging evidence for the lack of a relationship between productivity and the diversity of soil nematodes and prokaryotes.
The diversity of soil organisms is both massive and relatively poorly understood [1,2]. Conventionally, species diversity is thought to be related to the productivity of a habitat , which is determined primarily by abiotic factors such as rainfall and temperature . However, recent studies of soil communities suggest that soil biota and microorganisms may not share diversity patterns often exhibited by plants and animals [5,6,7].
We characterized the relationship between soil prokaryotic and nematode diversity at six sites in Death Valley National Park (Mojave Desert, California, USA). The Park includes the largest elevation gradient in the contiguous United States, ranging from the Badwater Basin at 86 m below sea level to Telescope Peak at 3,368 m above sea level (m.a.s.l.). The North American temperature record was measured in Death Valley in 1913 (56.7 °C), and daytime temperatures at the lower elevations exceed 37 °C daily from May to September, on average. Annual rainfall is generally less than 3 cm at the lowest elevation but can exceed 40 cm at higher locations . Death Valley National Park is a particularly valuable field site because natural variation in productivity exists within a small geographic area due to the large elevation change. Furthermore, a common plant species exists throughout much of the ecosystem (Larrea tridentata, creosotebush) so that the influence of varying plant species can be limited when sampling between sites.
We hypothesized that as soil quality improved with increasing elevation, the diversity of soil prokaryotes and the abundance and diversity of nematodes would also increase. We focused this study on communities within the surface soils beneath L. tridentata canopies. These resource islands are where significant decomposition and nutrient generation occur in desert ecosystems [9,10]. We included both bacteria and archaea in our analyses, as both are prey for the bacteria-feeding nematodes that dominate these communities [11,12], and archaea are increasingly recognized for their contribution to soil communities .
2. Results and Discussion
The six sites sampled in Death Valley National Park represented an elevation gradient (−8 to 1,610 m.a.s.l.), but the sites also varied with respect to un-quantified slope, mineralogy, and alluvial influences. Despite these potentially confounding factors, soils exhibited a significant gradient of improving quality with increasing elevation and amelioration of extreme environmental conditions. Soil organic matter and moisture content both increased with elevation as predicted, and soil pH decreased (Table 1). Soil organic matter content was low overall, as is typical of desert soils , ranging from 0.46–4.45% (Table 1). Soil moisture content was low as well, ranging from 0.16–6.2%, and varied between sites significantly (Table 1). Moisture content generally increased with elevation, but the second highest site at 1,010 m.a.s.l. had the highest mean moisture content (Table 1). Soil pH varied significantly between sites (Table 1) and decreased with increasing elevation. Desert soils usually have a slightly basic pH , and the decrease with elevation and corresponding increases in moisture and organic matter reflect soils becoming less desert-like.
Soil respiration rates during laboratory incubations (a measure of potential heterotrophic activity) did not vary significantly between sites. Electrical conductivity, a measure of salinity, did not vary, with the exception of the Darwin Falls site at 752 m.a.s.l., which was significantly more saline than all the other field sites (Table 1). This location is alluvial and likely experiences salt deposition due to evaporation of ephemeral stream water.
|Site||Elevation (m.a.s.l.) **||Organic Matter (%, LOI) ***||Gravimetric Soil Moisture (%) ***||pH ***||EC (μS) ***||Respiration (CO2μmol g−1d−1) ****|
|Sand Dunes||−8||0.62 ± 0.07 a||0.18 ± 0.006 a||8.66 ± 0.05 a||183.88 ± 18.76 a||0.12 ± 0.02 a|
|Unnamed Site||152||1.40 ± 0.10 b||0.48 ± 0.029 ab||8.40 ± 0.04 ab||189.63 ±18.55 a||0.13 ± 0.01 a|
|Jubilee Pass||394||1.97 ± 0.16 bc||0.89 ± 0.080 bc||8.12 ± 0.08 bcd||176.25 ± 15.72 a||0.10 ± 0.01 a|
|Darwin Falls||752||2.27 ± 0.38 c||0.97 ± 0.18 bc||8.03 ± 0.20 cd||667.00 ± 169.10 b||0.16 ± 0.03 a|
|SalsberryPass||1010||3.11 ± 0.18 d||2.71 ± 0.53 d||8.22 + 0.08 bc||241.63 ± 31.85 a||0.13 ± 0.03 a|
|Dantes View||1610||3.71 ± 0.22 d||1.50 ± 0.12 c||7.84 ± 0.07 d||355.13 ± 44.12 a||0.12 ± 0.02 a|
* Values are means ± the standard error of the mean (n = 8). Within each column, values with different letters are significantly different; ** m.a.s.l. = meters above sea level; *** (ANOVA, P≤ 0.0001); **** No significant differences (ANOVA, P = 0.65).
Nematode density varied significantly between sites, but these differences were not related to elevation (Figure 1a). Soils from −8,752 and 1,010 m.a.s.l. contained the highest densities of nematodes. Nematode density across the samples varied from 110–9,151 kg−1 soil.
Polymerase chain reaction-denaturing gradient gel electrophoresis (PCR-DGGE, ) of amplified ribosomal DNA from soil nematodes was used to assess the relative species richness of nematode communities. The number of distinct electrophoresis bands obtained for each sample was used as an estimate of richness. DGGE underestimates community richness due, in part, to the inability to resolve overlapping bands [15,16]. However, the technique is a simple and useful method for making relative assessments between communities [17,18,19]. Nematode species richness data was not analyzed statistically because nematodes extracted from site replicates were pooled in order to maximize representation of all species. However, there does not appear to be any trend in the data relating to elevation. The highest elevation site did have a markedly lower number of bands than the other sites (Figure 1b). Few studies have studied nematode diversity along productivity gradients, but Barrett and colleagues  found soil nematode diversity and abundance to be mostly unrelated to organic content in soils collected in the Antarctic Dry Valleys, at several field sites with varying latitude and productivity.
Nematode community structure varied between the sites (Figure 1c). Bacteria-feeding and fungal-feeding species dominated the nematode communities at all locations, consistent with prior work on Mojave Desert soils . The main groups of bacteria-feeders encountered were from the Cephalobidae family (Acrobeles, Acrobeloides, Cephalobus spp.), but Plectidae and Rhabtididae were also found. The main groups of fungal-feeders found were Anguinidae (Ditylenchus sp.) and Aphelenchidae/Aphelenchoididae. Omnivorous species made a small contribution to the communities, and did not vary significantly between sites (Figure 1c). Freckman and Mankau  studied soil nematode communities beneath L. tridentata in the Mojave Desert (Rock Valley, Nevada) and found plant-parasitic species in their samples, which we did not. These researchers sampled from a depth of 0–10 cm, whereas we confined our analyses to 0–5 cm. Plant-parasitic nematode species abundances are known to increase with depth in arid ecosystems, following the distribution of plant roots , so it seems likely that they would be found in Death Valley in deeper soil layers.
We found that bacteria-feeding nematode species generally were the most abundant across the sites, ranging from 36–98% of the nematodes found in each sample. Their contribution to the total community was lowest at the lowest elevation site (−8 m.a.s.l., Figure 1c). In tandem, the proportional representation of fungal-feeding species was significantly higher at −8 m.a.s.l. than at higher elevations (Figure 1c). The higher relative abundance of fungal-feeding nematodes at the lowest elevation was surprising, as was the high overall abundance of nematodes there. These results suggest that fungal-feeding nematodes (and likely fungi as well) flourish under the extreme conditions at that site, relative to bacteria-feeding nematodes. A common nematode genera encountered, Aphelenchus, is known to have excellent survival capabilities through its use of an anhydrobiotic strategy that has also been demonstrated for many bacteria-feeding nematode species [21,22]. In anhydrobiosis, or “life without water”, nematodes survive desiccating conditions in an ametabolic state . In the cold desert soils of the Antarctic Dry Valleys, a single species of nematode, Scottnema lindsayae, has a broad distribution and high abundance relative to the few other nematode species found in this ecosystem [24,25]. This nematode appears to be a dry soil specialist, facilitated by its ability to use anhydrobiosis . Nematode species in Death Valley soils likely are similarly adapted such that the extreme desiccation and low productivity of low elevation soils do not limit their distribution. The ability to use anhydrobiosis may be widespread among nematode species, allowing them to survive and maintain high densities even in the arid core of Death Valley.
Nematode communities have been studied in the Judean Desert (Israel), along a transect encompassing 650 to −60 m.a.s.l. . Here, nematode density declined with decreasing elevation and soil moisture content. Nematode diversity was unrelated to elevation, however, and shifts in trophic structure were not observed. In the Antarctic Dry Valleys, nematode communities were found with highest diversity at the lowest elevation sites, and diversity and abundance declined with elevation over 83–188 m.a.s.l. . At this site, soil moisture and organic matter were highest at the lowest elevations and decline moving upwards. The contrast between the results of these studies of desert nematode communities and the results of our study suggests the importance of site-specific factors in structuring nematode communities.
Relative species richness of bacteria, as estimated by the number of bands produced via DGGE analysis, was higher than that of archaea at all field sites (Figure 2). Bacteria richness varied significantly between sites, with the highest diversity found at 394 m.a.s.l. and the lowest at −8 m.a.s.l. (Figure 2a). Archaea richness did not vary significantly among the field sites (Figure 2b). Bryant and colleagues  demonstrated a negative linear trend in soil Acidobacteria richness with increasing elevation at sites (2,460–3,380 m.a.s.l.) in the Rocky Mountains (Colorado, USA). Singh and colleagues  demonstrated a hump-shaped soil bacteria diversity pattern on Mt. Fiji (Japan) over 1,000–3,760 m.a.s.l., with the lowest diversity at the highest elevations. In both of these studies, environmental conditions deteriorated with increasing elevation (opposite to our Death Valley sites), and communities with the lowest diversity were found under the most extreme conditions, as seen in our study. Recent work by Fierer and colleagues , however, failed to demonstrate any elevation gradient with respect to bacterial phylotype richness across a comprehensive 200–3,400 m.a.s.l. elevation transect in Peru. It appears that prokaryotic communities may not follow the same diversity patterns as those exhibited by animals and plants, yet whether these communities exhibit any patterns in relation to productivity remains to be clearly demonstrated.
Overall, relationships between soil properties, nematode communities, and prokaryotic diversity were site-specific in Death Valley and did not demonstrate patterns related to elevation. Desert soils are often saline due to low precipitation and the accumulation of salts through weathering and atmospheric deposition. High salinities have been shown to be sufficient to exclude soil microfauna in other ecosystems. Treonis and colleagues  found nematodes were absent from Antarctic Dry Valley soils with salinities greater than 2,500 µS. In Death Valley, the highest salinity measured was 1,401 µS and well below values found in Antarctica. Further, we found a significant positive correlation between electrical conductivity and nematode density in the Death Valley soils studied (Table 2). This relationship is likely to be indirect. High salinity soils in Death Valley were located at the 752 m.a.s.l. Darwin Falls site. Darwin Falls is one of only four perennial streams in Death Valley National Park, and while we sampled beyond the terminus of the stream, it is likely that the soils we sampled receive overflow stream water during rainstorms. These ephemeral moisture pulses could contribute to increasing soil salinity but also promote the establishment of higher density nematode communities (Figure 1).
In contrast to nematode density, electrical conductivity and archaea richness were negatively correlated across our Death Valley samples (Table 2). Archaea have been associated with extreme environments, and several taxa are known for their halophilic nature . Archaeal distribution is cosmopolitan in soils , however, and none of the soils we studied represent extremes of salinity. Archaea carry out important processes (e.g., methanogenesis) and have been shown to be prey for microbivorous nematodes . In Death Valley, their diversity may be negatively influenced by salinity in an unanticipated manner that warrants further research.
|Soil Property||Nematode Density||Bacteria Diversity||Archaea Diversity|
* Values are P-values for correlation analyses (n = 48); ** Correlation was positive (0.39); *** Correlation was negative (−0.29).
The diversity and abundance of consumer organisms such as soil nematodes is likely influenced by the diversity and abundance of food sources available to them , as niche differentiation is an important driver of species co-existence . We were unable to establish a relationship between nematode diversity and that of their prokaryotic prey in Death Valley soils, however. Barrett and colleagues  studied nematodes and bacterial diversity in the polar desert soils of the Antarctic Dry Valleys, where a relationship between bacterial richness and nematode density was also not apparent. In our study, at our highest elevation site in Death Valley, nematode density and species richness were attenuated and prokaryotic diversity was moderate, despite relatively high moisture and organic matter content for the soils. It is clear that other factors aside from elevation and soil quality influence the diversity of soil organisms in desert soils.
3. Experimental Section
Soil samples were collected April 2010 from six sites within Death Valley National Park (Table 1) that encompass an elevation gradient ranging from −8 to 1,610 m.a.s.l. (the highest elevation at which L. tridentata was found). For each sample, approximately 1.5 kg of soil was collected from multiple locations within the canopy of the dominant plant species (L. tridentata). The soils at most of these locations are extremely rocky, limiting the ability to collect soil using a soil corer. Samples were thereby collected using 50-mL plastic beakers as scoops. Surface litter was scraped away and then soil was collected from 0–5 cm. Soil was sieved (2 mm) on site to remove rocks and large pieces of litter and then transferred to a plastic bag (Whirl-Pak℘, Nasco, Fort Atkinson, WI). At each site, eight replicate samples were collected from eight individual shrubs within 100 m of each other. Soil samples were shipped in coolers from Las Vegas, NV to the University of Richmond and stored at 4 °C until analyzed.
Soil moisture was determined gravimetrically (48 h at 105 °C), and electrical conductivity (EC), used as an indicator of salinity, was measured on a 1:3 soil:water slurry. Soil organic matter was measured as loss on ignition (LOI, 400 °C, 12 h). Relative soil respiration rates (i.e., CO2 evolution) were determined by incubating 50 g soil samples at 22 °C inside of sealed pint-sized glass jars (473 mL). At the end of the incubation period (8 d), the CO2 concentration of a 25-mL headspace gas sample, withdrawn from each jar through a septum in the lid using a syringe, was determined using an infrared gas analyzer (LI-820, LI-COR, Inc., Lincoln, NE, USA ).
A Baermann funnel technique was used to extract nematodes from 100 ± 0.1 g soil at room temperature over 72 h . Nematodes were fixed in 5% formalin solution for future enumeration. An inverted microscope was used to count the total number of nematodes per sample. Nematodes (200 per sample, as available) were assigned to trophic groups based on morphology .
Nematodes also were extracted from 100 g of soil using sucrose flotation and centrifugation technique . The extracted nematodes from each of the eight replicates from each field site were combined for DNA extraction and analyses. A preliminary effort determined that this step was necessary in order to obtain adequate DNA and representation of diversity in the samples. Unfortunately, not enough collected soil was available for extraction from more than 100 g from each individual replicate. Following pooling and reduction of nematode samples to a small volume (≈0.5 µL), nematode DNA was extracted and purified using the MO BIO Powersoil™ DNA Isolation kit (MO BIO Laboratories Inc., Carlsbad, CA, USA) following the manufacturer’s instructions. A fragment of the 18S rDNA gene was amplified using the primers SSU18A and SSU9RGC  and the procedure of Okada and Oba . A GC-clamp was added to the 5’ end of the reverse primer SSU9RGC (CGCCCGCCGCGCGCGGCGGGCGGGGCGGGGGCACGGGGGG; 14). Reactions were carried out in a BioRad PTC-1148 Minicycler (Bio-Rad Laboratories, Hercules, CA, USA) with an initial denaturing step at 98 ºC for 3 min, 27 cycles of denaturing at 98 ºC for 10 s, annealing at 54 ºC for 15 s, and extension at 72 ºC for 40 s, and final extension at 72 ºC for 10 min.
PCR products were used for denaturing gradient gel electrophoresis (DGGE ) using the BioRad DCode Universal Mutation Detection System (Bio-Rad Laboratories, Hercules, CA, USA). An 6% (w v−1) polyacrylamide gel with a parallel denaturing gradient between 20%–50% (where 100% denaturant contains 7 M urea and 40% formamide) was cast using a GM-40 Gradient Maker (CBS Scientific Co., Del Mar, CA, USA) and an MPP-100 Mini Peristaltic Pump (CBS Scientific Co.) set at medium speed. 20 µL of PCR product (≈400 ng DNA) was mixed with 20 µL 2× gel loading dye (0.05% bromophenol blue, 0.05% xylene cyanol, 70% glycerol) and loaded into the gels. Electrophoresis was performed in 1X TAE at 60 ºC for 16 h at 75 V. The gel was stained in approximately 350 mL 1X TAE containing 5 µL ethidium bromide (10 mg mL−1) on a platform shaker at 25 rpm for 30 min, followed by destaining in water (2×, 15 min). The gel was photographed using a Gel Logic 200 photodocumentation system (Kodak/Carestream Health Inc., Rochester, NY, USA). Bands in each lane were quantified visually on a computer monitor.
Total DNA was extracted and purified from 0.25 g soil samples from each of the eight replicates from each of the six field sites as described above. For analysis of bacteria species richness, a nested PCR technique was used to amplify a 177 bp segment of the V3 hypervariable region of the bacterial 16S rDNA using the primer sets GM3F/GM4R  and EUB341GC/UNIV518R . A GC-clamp was added to the 5’ end of the forward primer EUB341GC, (CGCCCGCCGCGCGCGGCGGG-GGGGCGGGGGCACGGGGGG; 14). The PCR procedure for GM3F/GM4R consisted of an initial denaturing step at 95 ºC for 5 min, 30 cycles of denaturing at 94 ºC for 1 min, annealing at 50 ºC for 1 min, and extension at 72 ºC for 1.5 min, and final extension at 72 ºC for 10 min. The PCR procedure for EUB341GC/UNIV518R was the same as for GM3F/GM4R, apart from an annealing temperature of 60 ºC and an extension time of 1 min per cycle.
For analysis of archaea richness, a nested PCR procedure used was as described by  using the primers 21F/958R  and 344FGC/517R  to amplify a 192 bp fragment of the 16S rDNA. A GC-clamp was added to the 5’ end of the forward primer 344FGC (CGCCCGCCGCGCGCGGCGGG-CGGGGCGGGGGCACGGGGGG; 14). The PCR procedure for 21F/958R consisted of an initial denaturing step at 95 ºC for 5 min, 30 cycles of denaturing at 95 ºC for 1.5 min, annealing at 55 ºC for 1.5 min, and extension at 72 ºC for 1.5 min, and final extension at 72 ºC for 10 min. The PCR procedure for 344FGC/517R was a touchdown method that began with an initial denaturing step at 94 ºC for 3.5 min, followed by denaturing at 94 ºC for 45 s, then annealing for 45 s at 65–55 ºC (stepping down one degree every two cycles from 65 to 62 ºC and one degree per cycle from 62 to 55ºC) and extension at 72 ºC for 30 s. This was followed by 30 cycles of denaturing at 94 ºC for 45 s, annealing at 55 ºC for 45 s, and extension at 72 ºC for 30 s with a 5 min extension on the final cycle.
PCR products were subjected to DGGE. For the bacteria, an 8% (w v−1) polyacrylamide gel with a parallel denaturing gradient between 35–65% was cast and loaded with 20 µL of PCR product as described above (≈700 ng DNA). Electrophoresis of the bacteria gels was performed in 1× TAE at 60 ºC for 16.5 h at 75 V. For the archaea gels, 7% (w v−1) polyacrylamide and 40%–65% gradient, 20 µL of PCR product was loaded (≈300 ng DNA), and electrophoresis was performed at 47 V for 16 h. Bacterial and archaea DGGE gels were stained and analyzed as described above.
All statistical analyses were performed with Statview Version 5.0.01 (SAS Institute, Inc., Cary, NC, USA). Measured variables were compared between sites using one-factor analysis of variance (site only). The correlations between soil properties and nematode density, community trophic structure, and prokaryotic richness were explored through construction of a Pearsons Correlation Matrix.
In this study, we explored the relationship between productivity and the diversity of soil nematodes and their prokaryotic prey in desert soils. Overall, the gradient studied shows improving soil quality with increasing elevation, likely due to increased plant productivity and belowground inputs as the extreme environmental conditions ameliorate. However, our results fail to support the hypothesis that there is a positive relationship between diversity and productivity in soil communities, which is consistent with emerging research by others.
We thank Emily Archibald, Blake Bailey, Emily Boone, Charles Parsons, Lori Spicer, and Gabriela Timoney for assistance with sampling and laboratory work. Two anonymous reviewers are thanked for their comments. This research was supported by a Science Education grant to the University of Richmond from the Howard Hughes Medical Institute.
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