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Scott Ferrenberg,
Sean P O'Neill,
Joseph E Knelman,
Bryan Todd,
Sam Duggan,
Daniel Bradley,
Taylor Robinson,
Steven K Schmidt,
Alan R Townsend,
Mark W Williams,
Cory C Cleveland,
Brett A Melbourne,
Lin Jiang, Diana R Nemergut
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ABSTRACT: Although recent work has shown that both deterministic and stochastic processes are important in structuring microbial communities, the factors that affect the relative contributions of niche and neutral processes are poorly understood. The macrobiological literature indicates that ecological disturbances can influence assembly processes. Thus, we sampled bacterial communities at 4 and 16 weeks following a wildfire and used null deviation analysis to examine the role that time since disturbance has in community assembly. Fire dramatically altered bacterial community structure and diversity as well as soil chemistry for both time-points. Community structure shifted between 4 and 16 weeks for both burned and unburned communities. Community assembly in burned sites 4 weeks after fire was significantly more stochastic than in unburned sites. After 16 weeks, however, burned communities were significantly less stochastic than unburned communities. Thus, we propose a three-phase model featuring shifts in the relative importance of niche and neutral processes as a function of time since disturbance. Because neutral processes are characterized by a decoupling between environmental parameters and community structure, we hypothesize that a better understanding of community assembly may be important in determining where and when detailed studies of community composition are valuable for predicting ecosystem function.
The ISME Journal 02/2013; · 7.38 Impact Factor
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ABSTRACT: Global changes such as variations in plant net primary production are likely to drive shifts in leaf litterfall inputs to forest soils, but the effects of such changes on soil carbon (C) cycling and storage remain largely unknown, especially in C-rich tropical forest ecosystems. We initiated a leaf litterfall manipulation experiment in a tropical rain forest in Costa Rica to test the sensitivity of surface soil C pools and fluxes to different litter inputs. After only 2 years of treat-ment, doubling litterfall inputs increased surface soil C concentrations by 31%, removing litter from the forest floor drove a 26% reduction over the same time period, and these changes in soil C concentrations were associated with variations in dissolved organic matter fluxes, fine root biomass, microbial biomass, soil moisture, and nutrient fluxes. However, the litter manipulations had only small effects on soil organic C (SOC) chemistry, suggesting that changes in C cycling, nutrient cycling, and microbial processes in response to litter manipulation reflect shifts in the quantity rather than quality of SOC. The manipulation also affected soil CO 2 fluxes; the relative decline in CO 2 production was greater in the litter removal plots (À22%) than the increase in the litter addition plots (+15%). Our analysis showed that variations in CO 2 fluxes were strongly correlated with microbial biomass pools, soil C and nitrogen (N) pools, soil inorganic P fluxes, dissolved organic C fluxes, and fine root biomass. Together, our data suggest that shifts in leaf litter inputs in response to localized human disturbances and global environmental change could have rapid and important consequences for belowground C storage and fluxes in tropical rain forests, and highlight differences between tropical and temperate ecosystems, where belowground C cycling responses to changes in litterfall are generally slower and more subtle.
Global Change Biology 01/2012; · 6.86 Impact Factor
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ABSTRACT: Soil microorganisms are key drivers of terrestrial biogeochemical cycles, yet it is still unclear how variations in soil microbial community composi-tion influence many ecosystem processes. We investigated how shifts in bacterial community composition and diversity resulting from differ-ences in carbon (C) availability affect organic matter decomposition by conducting an in situ litter manipulation experiment in a tropical rain forest in Costa Rica. We used bar-coded pyrose-quencing to characterize soil bacterial community composition in litter manipulation plots and per-formed a series of laboratory incubations to test the potential functional significance of community
Ecosystems 01/2012; 15:284. · 3.49 Impact Factor
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ABSTRACT: One of the oldest ecological hypotheses, proposed by Darwin, suggests that the struggle for existence is stronger between more closely related species. Despite its long history, the validity of this phylogenetic limiting similarity hypothesis has rarely been examined. Here we provided a formal experimental test of the hypothesis using pairs of bacterivorous protist species in a multigenerational experiment. Consistent with the hypothesis, both the frequency and tempo of competitive exclusion, and the reduction in the abundance of inferior competitors, increased with increasing phylogenetic relatedness of the competing species. These results were linked to protist mouth size, a trait potentially related to resource use, exhibiting a significant phylogenetic signal. The likelihood of coexistence, however, was better predicted by phylogenetic relatedness than trait similarity of the competing species. Our results support phylogenetic relatedness as a useful predictor of the outcomes of competitive interactions in ecological communities.
Ecology Letters 06/2011; 14(8):782-7. · 17.56 Impact Factor
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Diana R Nemergut,
Elizabeth K Costello,
Micah Hamady,
Catherine Lozupone,
Lin Jiang,
Steven K Schmidt,
Noah Fierer,
Alan R Townsend,
Cory C Cleveland,
Lee Stanish,
Rob Knight
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ABSTRACT: Bacteria control major nutrient cycles and directly influence plant, animal and human health. However, we know relatively little about the forces shaping their large-scale ecological ranges. Here, we reveal patterns in the distribution of individual bacterial taxa at multiple levels of phylogenetic resolution within and between Earth's major habitat types. Our analyses suggest that while macro-scale habitats structure bacterial distribution to some degree, abundant bacteria (i.e. detectable using 16S rRNA gene sequencing methods) are confined to single assemblages. Additionally, we show that the most cosmopolitan taxa are also the most abundant in individual assemblages. These results add to the growing body of data that support that the diversity of the overall bacterial metagenome is tremendous. The mechanisms governing microbial distribution remain poorly understood, but our analyses provide a framework with which to test the importance of macro-ecological environmental gradients, relative abundance, neutral processes and the ecological strategies of individual taxa in structuring microbial communities.
Environmental Microbiology 01/2011; 13(1):135-44. · 5.84 Impact Factor
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ABSTRACT: a b s t r a c t Little is known about the organisms responsible for decomposition in terrestrial ecosystems, or how variations in their relative abundance may influence soil carbon (C) cycling. Here, we altered organic matter in situ by manipulating both litter and throughfall inputs to tropical rain forest soils, and then used qPCR and error-corrected bar-coded pyrosequencing to investigate how the resulting changes in soil chemical properties affected microbial community structure. The plot-scale manipulations drove significant changes in microbial community composition: Acidobacteria were present in greater relative abundance in litter removal plots than in double-litter plots, while Alphaproteobacteria were found in higher relative abundance in double-litter and throughfall reduction plots than in control or litter removal plots. In addition, the bacterial:archaeal ratio was higher in double-litter than no-litter plots. The relative abundances of Actinobacteria, Alphaproteobacteria and Gammaproteobacteria were positively correlated with microbial biomass C and nitrogen (N), and soil N and C pools, while acidobacterial relative abundance was negatively correlated with these same factors. Bacterial:archaeal ratios were positively correlated with soil moisture, total soil C and N, extractable ammonium pools, and soil C:N ratios. Additionally, bacterial:archaeal ratios were positively related to the relative abundance of Acti-nobacteria, Gammaproteobacteria, and Actinobacteria, and negatively correlated to the relative abun-dance of Nitrospira and Acidobacteria. Together, our results support the copiotrophic/oligotrophic model of soil heterotrophic microbes suggested by Fierer et al. (2007).
09/2010;
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Justin Kuczynski,
Elizabeth K Costello, Diana R Nemergut,
Jesse Zaneveld,
Christian L Lauber,
Dan Knights,
Omry Koren,
Noah Fierer,
Scott T Kelley,
Ruth E Ley,
Jeffrey I Gordon,
Rob Knight
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ABSTRACT: Culture-independent studies of human microbiota by direct genomic sequencing reveal quite distinct differences among communities, indicating that improved sequencing capacity can be most wisely utilized to study more samples, rather than more sequences per sample.
Genome biology 05/2010; 11(5):210. · 6.63 Impact Factor
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ABSTRACT: The role of biodiversity in ecosystem function receives substantial attention, yet despite the diversity and functional relevance of microorganisms, relationships between microbial community structure and ecosystem processes remain largely unknown. We used tropical rain forest fertilization plots to directly compare the relative abundance, composition and diversity of free-living nitrogen (N)-fixer communities to in situ leaf litter N fixation rates. N fixation rates varied greatly within the landscape, and 'hotspots' of high N fixation activity were observed in both control and phosphorus (P)-fertilized plots. Compared with zones of average activity, the N fixation 'hotspots' in unfertilized plots were characterized by marked differences in N-fixer community composition and had substantially higher overall diversity. P additions increased the efficiency of N-fixer communities, resulting in elevated rates of fixation per nifH gene. Furthermore, P fertilization increased N fixation rates and N-fixer abundance, eliminated a highly novel group of N-fixers, and increased N-fixer diversity. Yet the relationships between diversity and function were not simple, and coupling rate measurements to indicators of community structure revealed a biological dynamism not apparent from process measurements alone. Taken together, these data suggest that the rain forest litter layer maintains high N fixation rates and unique N-fixing organisms and that, as observed in plant community ecology, structural shifts in N-fixing communities may partially explain significant differences in system-scale N fixation rates.
Oecologia 05/2010; 164(2):521-31. · 3.41 Impact Factor
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ABSTRACT: Past work in recently deglaciated soils demonstrates that microbial communities undergo shifts prior to plant colonization. To date, most studies have focused on relatively 'long' chronosequences with the ability to sample plant-free sites over at least 50 years of development. However, some recently deglaciated soils feature rapid plant colonization and questions remain about the relative rate of change in the microbial community in the unvegetated soils of these chronosequences. Thus, we investigated the forelands of the Mendenhall Glacier near Juneau, AK, USA, where plants rapidly establish. We collected unvegetated samples representing soils that had been ice-free for 0, 1, 4, and 8 years. Total nitrogen (N) ranged from 0.00 approximately 0.14 mg/g soil, soil organic carbon pools ranged from 0.6 approximately 2.3 mg/g soil, and both decreased in concentration between the 0 and 4 yr soils. Biologically available phosphorus (P) and pH underwent similar dynamics. However, both pH and available P increased in the 8 yr soils. Nitrogen fixation was nearly undetectable in the most recently exposed soils, and increased in the 8 yr soils to approximately 5 ng N fixed/cm(2)/h, a trend that was matched by the activity of the soil N-cycling enzymes urease and beta-l,4-N-acetyl-glucosa-minidase. 16S rRNA gene clone libraries revealed no significant differences between the 0 and 8 yr soils; however, 8 yr soils featured the presence of cyanobacteria, a division wholly absent from the 0 yr soils. Taken together, our results suggest that microbes are consuming allochtonous organic matter sources in the most recently exposed soils. Once this carbon source is depleted, a competitive advantage may be ceded to microbes not reliant on in situ nutrient sources.
The Journal of Microbiology 12/2009; 47(6):673-81. · 1.10 Impact Factor
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ABSTRACT: Many studies have shown that changes in nitrogen (N) availability affect primary productivity in a variety of terrestrial systems, but less is known about the effects of the changing N cycle on soil organic matter (SOM) decomposition. We used a variety of techniques to examine the effects of chronic N amendments on SOM chemistry and microbial community structure and function in an alpine tundra soil. We collected surface soil (0-5 cm) samples from five control and five long-term N-amended plots established and maintained at the Niwot Ridge Long-term Ecological Research (LTER) site. Samples were bulked by treatment and all analyses were conducted on composite samples. The fungal community shifted in response to N amendments, with a decrease in the relative abundance of basidiomycetes. Bacterial community composition also shifted in the fertilized soil, with increases in the relative abundance of sequences related to the Bacteroidetes and Gemmatimonadetes, and decreases in the relative abundance of the Verrucomicrobia. We did not uncover any bacterial sequences that were closely related to known nitrifiers in either soil, but sequences related to archaeal nitrifiers were found in control soils. The ratio of fungi to bacteria did not change in the N-amended soils, but the ratio of archaea to bacteria dropped from 20% to less than 1% in the N-amended plots. Comparisons of aliphatic and aromatic carbon compounds, two broad categories of soil carbon compounds, revealed no between treatment differences. However, G-lignins were found in higher relative abundance in the fertilized soils, while proteins were detected in lower relative abundance. Finally, the activities of two soil enzymes involved in N cycling changed in response to chronic N amendments. These results suggest that chronic N fertilization induces significant shifts in soil carbon dynamics that correspond to shifts in microbial community structure and function.
Environmental Microbiology 10/2008; 10(11):3093-105. · 5.84 Impact Factor
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S K Schmidt,
Sasha C Reed, Diana R Nemergut,
A Stuart Grandy,
Cory C Cleveland,
Michael N Weintraub,
Andrew W Hill,
Elizabeth K Costello,
A F Meyer,
J C Neff,
A M Martin
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ABSTRACT: Global climate change has accelerated the pace of glacial retreat in high-latitude and high-elevation environments, exposing lands that remain devoid of vegetation for many years. The exposure of 'new' soil is particularly apparent at high elevations (5000 metres above sea level) in the Peruvian Andes, where extreme environmental conditions hinder plant colonization. Nonetheless, these seemingly barren soils contain a diverse microbial community; yet the biogeochemical role of micro-organisms at these extreme elevations remains unknown. Using biogeochemical and molecular techniques, we investigated the biological community structure and ecosystem functioning of the pre-plant stages of primary succession in soils along a high-Andean chronosequence. We found that recently glaciated soils were colonized by a diverse community of cyanobacteria during the first 4-5 years following glacial retreat. This significant increase in cyanobacterial diversity corresponded with equally dramatic increases in soil stability, heterotrophic microbial biomass, soil enzyme activity and the presence and abundance of photosynthetic and photoprotective pigments. Furthermore, we found that soil nitrogen-fixation rates increased almost two orders of magnitude during the first 4-5 years of succession, many years before the establishment of mosses, lichens or vascular plants. Carbon analyses (pyrolysis-gas chromatography/mass spectroscopy) of soil organic matter suggested that soil carbon along the chronosequence was of microbial origin. This indicates that inputs of nutrients and organic matter during early ecosystem development at these sites are dominated by microbial carbon and nitrogen fixation. Overall, our results indicate that photosynthetic and nitrogen-fixing bacteria play important roles in acquiring nutrients and facilitating ecological succession in soils near some of the highest elevation receding glaciers on the Earth.
Proceedings of the Royal Society B: Biological Sciences 09/2008; 275(1653):2793-802. · 5.41 Impact Factor
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ABSTRACT: Much of our knowledge on biodiversity and ecosystem functioning comes from studies examining the effects of biodiversity on biomass production within a trophic group. A large number of these studies have found that increasing biodiversity tends to increase biomass production, leading many ecologists to believe that there exists a general positive relationship between biodiversity and ecosystem functioning. Here we argue that such a positive relationship may not be general, particularly for ecosystem functions other than biomass. Our argument centers on the potential importance of the negative selection effect, which operates where competitively dominant species do not contribute significantly to the function of interest. We suggest that negative selection effects may be potentially common for non-biomass functions, for which species competitive ability may often be a poor indictor of its functional impact. We conclude that diverse (positive, negative, and neutral) BEF relationships are possible for non-biomass functions and that for a particular function, the exact form of the BEF relationship may depend on how species functional impacts relate to their competitive abilities in the community.
Oikos 03/2008; 117(4):488 - 493. · 3.06 Impact Factor
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ABSTRACT: Detecting patterns of horizontal gene transfer (HGT) in genomic sequences is an important problem, with implications for evolution, ecology, biotechnology and medicine. Extensive genetic, biochemical and genomic studies have provided a good understanding of sequence features that are associated with many (though not all) known mobile elements and mechanisms of gene transfer. This information, however, is not currently incorporated into automated methods for gene transfer detection in genomic data. In this review, we argue that automated annotation of sequence features associated with gene transfer mechanisms could be used both to build more sensitive, mechanism-specific compositional models for the detection of some types of HGT in genomic data, and to ask new questions about the classes of genes most frequently transferred by each mechanism. We then summarize the genes and sequence features associated with different mechanisms of horizontal transfer, emphasizing those that are most useful for distinguishing types of transfer when examining genomic data, and noting those classes of transfers that cannot be distinguished in genomic data using existing techniques. Finally, we describe software, databases and algorithms for identifying particular classes of mobile elements, and outline prospects for better detection of HGT based on specific mechanisms of transfer.
Microbiology 02/2008; 154(Pt 1):1-15. · 3.06 Impact Factor
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ABSTRACT: Integrons are mechanisms that facilitate horizontal gene transfer, allowing bacteria to integrate and express foreign DNA. These are important in the exchange of antibiotic resistance determinants, but can also transfer a diverse suite of genes unrelated to pathogenicity. Here, we provide a systematic analysis of the distribution and diversity of integron intI genes and integron-containing bacteria.
We found integrons in 103 different pathogenic and non-pathogenic bacteria, in six major phyla. Integrons were widely scattered, and their presence was not confined to specific clades within bacterial orders. Nearly 1/3 of the intI genes that we identified were pseudogenes, containing either an internal stop codon or a frameshift mutation that would render the protein product non-functional. Additionally, 20% of bacteria contained more than one integrase gene. dN/dS ratios revealed mutational hotspots in clades of Vibrio and Shewanella intI genes. Finally, we characterized the gene cassettes associated with integrons in Methylobacillus flagellatus KT and Dechloromonas aromatica RCB, and found a heavy metal efflux gene as well as genes involved in protein folding and stability.
Our analysis suggests that the present distribution of integrons is due to multiple losses and gene transfer events. While, in some cases, the ability to integrate and excise foreign DNA may be selectively advantageous, the gain, loss, or rearrangment of gene cassettes could also be deleterious, selecting against functional integrases. Thus, such a high fraction of pseudogenes may suggest that the selective impact of integrons on genomes is variable, oscillating between beneficial and deleterious, possibly depending on environmental conditions.
BMC Genomics 02/2008; 9:261. · 4.07 Impact Factor
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ABSTRACT: Abstract Theories of macroevolution rarely have been extended to include microbes; however, because microbes represent the most ancient and diverse assemblage of organismal diversity, such oversight limits our understanding of evolutionary history. Our analysis of phylogenetic trees for microbes suggests that macroevolution may differ between prokaryotes and both micro- and macroeukaryotes (mainly plants and animals). Phylogenetic trees inferred for prokaryotes and some microbial eukaryotes conformed to expectations assuming a constant rate of cladogenesis over time and among lineages; nevertheless, microbial eukaryote trees exhibited more variation in rates of cladogenesis than prokaryote trees. We hypothesize that the contrast of macroevolutionary dynamics between prokaryotes and many eukaryotes is due, at least in part, to differences in the prevalence of lateral gene transfer (LGT) between the two groups. Inheritance is predominantly, if not wholly, vertical within eukaryotes, a feature that allows for the emergence and maintenance of heritable variation among lineages. By contrast, frequent LGT in prokaryotes may ameliorate heritable variation in rate of cladogenesis resulting from the emergence of key innovations; thus, the inferred difference in macroevolution might reflect exclusivity of key innovations in eukaryotes and their promiscuous nature in prokaryotes.
Evolution 05/2007; 58(5):946 - 955. · 5.15 Impact Factor
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ABSTRACT: Primary succession is a fundamental process in macroecosystems; however, if and how soil development influences microbial community structure is poorly understood. Thus, we investigated changes in the bacterial community along a chronosequence of three unvegetated, early successional soils ( approximately 20-year age gradient) from a receding glacier in southeastern Peru using molecular phylogenetic techniques. We found that evenness, phylogenetic diversity, and the number of phylotypes were lowest in the youngest soils, increased in the intermediate aged soils, and plateaued in the oldest soils. This increase in diversity was commensurate with an increase in the number of sequences related to common soil bacteria in the older soils, including members of the divisions Acidobacteria, Bacteroidetes, and Verrucomicrobia. Sequences related to the Comamonadaceae clade of the Betaproteobacteria were dominant in the youngest soil, decreased in abundance in the intermediate age soil, and were not detected in the oldest soil. These sequences are closely related to culturable heterotrophs from rock and ice environments, suggesting that they originated from organisms living within or below the glacier. Sequences related to a variety of nitrogen (N)-fixing clades within the Cyanobacteria were abundant along the chronosequence, comprising 6-40% of phylotypes along the age gradient. Although there was no obvious change in the overall abundance of cyanobacterial sequences along the chronosequence, there was a dramatic shift in the abundance of specific cyanobacterial phylotypes, with the intermediate aged soils containing the greatest diversity of these sequences. Most soil biogeochemical characteristics showed little change along this approximately 20-year soil age gradient; however, soil N pools significantly increased with soil age, perhaps as a result of the activity of the N-fixing Cyanobacteria. Our results suggest that, like macrobial communities, soil microbial communities are structured by substrate age, and that they, too, undergo predictable changes through time.
Microbial Ecology 02/2007; 53(1):110-22. · 2.91 Impact Factor
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ABSTRACT: Organic matter decomposition and soil CO2 efflux are both mediated by soil microorganisms, but the potential effects of temporal variations in microbial community
composition are not considered in most analytical models of these two important processes. However, inconsistent relationships
between rates of heterotrophic soil respiration and abiotic factors, including temperature and moisture, suggest that microbial
community composition may be an important regulator of soil organic matter (SOM) decomposition and CO2 efflux. We performed a short-term (12-h) laboratory incubation experiment using tropical rain forest soil amended with either
water (as a control) or dissolved organic matter (DOM) leached from native plant litter, and analyzed the effects of the treatments
on soil respiration and microbial community composition. The latter was determined by constructing clone libraries of small-subunit
ribosomal RNA genes (SSU rRNA) extracted from the soil at the end of the incubation experiment. In contrast to the subtle
effects of adding water alone, additions of DOM caused a rapid and large increase in soil CO2 flux. DOM-stimulated CO2 fluxes also coincided with profound shifts in the abundance of certain members of the soil microbial community. Our results
suggest that natural DOM inputs may drive high rates of soil respiration by stimulating an opportunistic subset of the soil
bacterial community, particularly members of the Gammaproteobacteria and Firmicutes groups. Our experiment indicates that
variations in microbial community composition may influence SOM decomposition and soil respiration rates, and emphasizes the
need for in situ studies of how natural variations in microbial community composition regulate soil biogeochemical processes.
Biogeochemistry 01/2007; 82(3):229-240. · 3.07 Impact Factor
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ABSTRACT: Cultivation-independent molecular phylogenetic techniques are now widely employed to examine environmental microbial diversity; however, the relationship between microbial community structure and ecosystem function is unclear. This review synthesizes cultivation-independent views of microbiological diversity with our current understanding of nutrient dynamics in alpine and arctic soils. Recently, we have begun to explore connections between microbial community structure and function in soils from the alpine Niwot Ridge LTER site in Colorado, USA, whose ecology has been extensively investigated for over 50 years. We examined the diversity of bacterial, eucaryal, and archaeal small subunit rRNA genes in tundra and talus soils across seasons in the alpine. This work has provided support for spatial and seasonal shifts in specific microbial groups, which correlate well with previously documented transitions in microbial processes. In addition, these preliminary results suggest that the physiologies of certain groups of organisms may scale up to the ecosystem level, providing the basis for testable hypotheses about the function of specific microbes in this system. These studies have also expanded on the known diversity of life, as these soils harbor bacterial and eucaryotic lineages that are distantly related to other known organisms. In contrast to the alpine, microbial diversity in the arctic has been little explored; only three published studies have used molecular techniques to examine these soils. Because of the importance of these systems, particularly to the global C cycle, and their vulnerability to current and impending climate change, the microbial diversity of these soils needs to be further investigated.
Research in Microbiology 09/2005; 156(7):775-84. · 2.76 Impact Factor
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ABSTRACT: Theories of macroevolution rarely have been extended to include microbes; however, because microbes represent the most ancient and diverse assemblage of organismal diversity, such oversight limits our understanding of evolutionary history. Our analysis of phylogenetic trees for microbes suggests that macroevolution may differ between prokaryotes and both micro- and macroeukaryotes (mainly plants and animals). Phylogenetic trees inferred for prokaryotes and some microbial eukaryotes conformed to expectations assuming a constant rate of cladogenesis over time and among lineages: nevertheless, microbial eukaryote trees exhibited more variation in rates of cladogenesis than prokaryote trees. We hypothesize that the contrast of macroevolutionary dynamics between prokaryotes and many eukaryotes is due, at least in part, to differences in the prevalence of lateral gene transfer (LGT) between the two groups. Inheritance is predominantly, if not wholly, vertical within eukaryotes, a feature that allows for the emergence and maintenance of heritable variation among lineages. By contrast, frequent LGT in prokaryotes may ameliorate heritable variation in rate of cladogenesis resulting from the emergence of key innovations; thus, the inferred difference in macroevolution might reflect exclusivity of key innovations in eukaryotes and their promiscuous nature in prokaryotes.
Evolution 06/2004; 58(5):946-55. · 5.15 Impact Factor
