@article {1417, title = {Land use change alters functional gene diversity, composition and abundance in Amazon forest soil microbial communities.}, journal = {Mol Ecol}, volume = {23}, year = {2014}, month = {2014 Jun}, pages = {2988-99}, abstract = {

Land use change in the Amazon rainforest alters the taxonomic structure of soil microbial communities, but whether it alters their functional gene composition is unknown. We used the highly parallel microarray technology GeoChip 4.0, which contains 83,992 probes specific for genes linked nutrient cycling and other processes, to evaluate how the diversity, abundance and similarity of the targeted genes responded to forest-to-pasture conversion. We also evaluated whether these parameters were reestablished with secondary forest growth. A spatially nested scheme was employed to sample a primary forest, two pastures (6 and 38 years old) and a secondary forest. Both pastures had significantly lower microbial functional genes richness and diversity when compared to the primary forest. Gene composition and turnover were also significantly modified with land use change. Edaphic traits associated with soil acidity, iron availability, soil texture and organic matter concentration were correlated with these gene changes. Although primary and secondary forests showed similar functional gene richness and diversity, there were differences in gene composition and turnover, suggesting that community recovery was not complete in the secondary forest. Gene association analysis revealed that response to ecosystem conversion varied significantly across functional gene groups, with genes linked to carbon and nitrogen cycling mostly altered. This study indicates that diversity and abundance of numerous environmentally important genes respond to forest-to-pasture conversion and hence have the potential to affect the related processes at an ecosystem scale.

}, keywords = {Agriculture, Carbon Cycle, Ecosystem, Genes, Bacterial, Genes, Fungal, Genetic Variation, Metagenome, Multigene Family, Nitrogen Cycle, Oligonucleotide Array Sequence Analysis, Soil Microbiology, Trees, Tropical Climate}, issn = {1365-294X}, doi = {10.1111/mec.12786}, author = {Paula, Fabiana S and Rodrigues, Jorge L M and Zhou, Jizhong and Wu, Liyou and Mueller, Rebecca C and Mirza, Babur S and Bohannan, Brendan J M and N{\"u}sslein, Klaus and Deng, Ye and Tiedje, James M and Pellizari, Vivian H} } @article {1419, title = {Links between plant and fungal communities across a deforestation chronosequence in the Amazon rainforest.}, journal = {ISME J}, volume = {8}, year = {2014}, month = {2014 Jul}, pages = {1548-50}, abstract = {

Understanding the interactions among microbial communities, plant communities and soil properties following deforestation could provide insights into the long-term effects of land-use change on ecosystem functions, and may help identify approaches that promote the recovery of degraded sites. We combined high-throughput sequencing of fungal rDNA and molecular barcoding of plant roots to estimate fungal and plant community composition in soil sampled across a chronosequence of deforestation. We found significant effects of land-use change on fungal community composition, which was more closely correlated to plant community composition than to changes in soil properties or geographic distance, providing evidence for strong links between above- and below-ground communities in tropical forests.

}, keywords = {Brazil, Conservation of Natural Resources, DNA Barcoding, Taxonomic, DNA, Fungal, DNA, Ribosomal, Ecosystem, Fungi, Phylogeny, Plant Roots, Soil Microbiology, Trees, Tropical Climate}, issn = {1751-7370}, doi = {10.1038/ismej.2013.253}, author = {Mueller, Rebecca C and Paula, Fabiana S and Mirza, Babur S and Rodrigues, Jorge L M and N{\"u}sslein, Klaus and Bohannan, Brendan J M} } @article {1420, title = {Response of free-living nitrogen-fixing microorganisms to land use change in the Amazon rainforest.}, journal = {Appl Environ Microbiol}, volume = {80}, year = {2014}, month = {2014 Jan}, pages = {281-8}, abstract = {

The Amazon rainforest, the largest equatorial forest in the world, is being cleared for pasture and agricultural use at alarming rates. Tropical deforestation is known to cause alterations in microbial communities at taxonomic and phylogenetic levels, but it is unclear whether microbial functional groups are altered. We asked whether free-living nitrogen-fixing microorganisms (diazotrophs) respond to deforestation in the Amazon rainforest, using analysis of the marker gene nifH. Clone libraries were generated from soil samples collected from a primary forest, a 5-year-old pasture originally converted from primary forest, and a secondary forest established after pasture abandonment. Although diazotroph richness did not significantly change among the three plots, diazotroph community composition was altered with forest-to-pasture conversion, and phylogenetic similarity was higher among pasture communities than among those in forests. There was also 10-fold increase in nifH gene abundance following conversion from primary forest to pasture. Three environmental factors were associated with the observed changes: soil acidity, total N concentration, and C/N ratio. Our results suggest a partial restoration to initial levels of abundance and community structure of diazotrophs following pasture abandonment, with primary and secondary forests sharing similar communities. We postulate that the response of diazotrophs to land use change is a direct consequence of changes in plant communities, particularly the higher N demand of pasture plant communities for supporting aboveground plant growth.

}, keywords = {Agriculture, Bacteria, Biota, Carbon, Cluster Analysis, Conservation of Natural Resources, Human Activities, Hydrogen-Ion Concentration, Molecular Sequence Data, Nitrogen, Nitrogen Fixation, Oxidoreductases, Phylogeny, Sequence Analysis, DNA, Soil, Soil Microbiology, South America, Trees}, issn = {1098-5336}, doi = {10.1128/AEM.02362-13}, author = {Mirza, Babur S and Potisap, Chotima and N{\"u}sslein, Klaus and Bohannan, Brendan J M and Rodrigues, Jorge L M} } @article {1423, title = {Conversion of the Amazon rainforest to agriculture results in biotic homogenization of soil bacterial communities.}, journal = {Proc Natl Acad Sci U S A}, volume = {110}, year = {2013}, month = {2013 Jan 15}, pages = {988-93}, abstract = {

The Amazon rainforest is the Earth\&$\#$39;s largest reservoir of plant and animal diversity, and it has been subjected to especially high rates of land use change, primarily to cattle pasture. This conversion has had a strongly negative effect on biological diversity, reducing the number of plant and animal species and homogenizing communities. We report here that microbial biodiversity also responds strongly to conversion of the Amazon rainforest, but in a manner different from plants and animals. Local taxonomic and phylogenetic diversity of soil bacteria increases after conversion, but communities become more similar across space. This homogenization is driven by the loss of forest soil bacteria with restricted ranges (endemics) and results in a net loss of diversity. This study shows homogenization of microbial communities in response to human activities. Given that soil microbes represent the majority of biodiversity in terrestrial ecosystems and are intimately involved in ecosystem functions, we argue that microbial biodiversity loss should be taken into account when assessing the impact of land use change in tropical forests.

}, keywords = {Agriculture, Animals, Bacteria, Biodiversity, Brazil, Cattle, Ecosystem, Humans, Phylogeny, Rain, Soil Microbiology, Trees, Tropical Climate}, issn = {1091-6490}, doi = {10.1073/pnas.1220608110}, author = {Rodrigues, Jorge L M and Pellizari, Vivian H and Mueller, Rebecca and Baek, Kyunghwa and Jesus, Ederson da C and Paula, Fabiana S and Mirza, Babur and Hamaoui, George S and Tsai, Siu Mui and Feigl, Brigitte and Tiedje, James M and Bohannan, Brendan J M and N{\"u}sslein, Klaus} } @article {746, title = {Comparative bacterial diversity in recent Hawaiian volcanic deposits of different ages.}, journal = {FEMS Microbiol Ecol}, volume = {60}, year = {2007}, month = {2007 Apr}, pages = {60-73}, abstract = {Volcanic activity creates new landforms that can change dramatically over time as a consequence of biotic succession. Nonetheless, volcanic deposits present severe constraints for microbial colonization and activity. We have characterized bacterial diversity on four recent deposits at Kilauea volcano, Hawaii (KVD). Much of the diversity was either closely related to uncultured organisms or distinct from any reported 16S rRNA gene sequences. Diversity indices suggested that diversity was highest in a moderately vegetated 210-year-old ash deposit (1790-KVD), and lowest for a 79-year-old lava flow (1921-KVD). Diversity for a 41-year-old tephra deposit (1959-KVD) and a 300-year-old rainforest (1700-KVD) reached intermediate values. The 1959-KVD and 1790-KVD communities were dominated by Acidobacteria, Alpha- and Gammaproteobacteria, Actinobacteria, Cyanobacteria, and many unclassified phylotypes. The 1921-KVD, an unvegetated low pH deposit, was dominated by unclassified phylotypes. In contrast, 1700-KVD was primarily populated by Alphaproteobacteria with very few unclassified phylotypes. Similar diversity indices and levels of trace gas flux were found for 1959-KVD and 1790-KVD; however, statistical analyses indicated significantly different communities. This study not only showed that microorganisms colonize recent volcanic deposits and are able to establish diverse communities, but also that their composition is governed by variations in local deposit parameters.}, keywords = {Bacteria, DNA, Bacterial, Ecosystem, Genes, rRNA, Genetic Variation, Hawaii, Molecular Sequence Data, Phylogeny, Polymerase Chain Reaction, RNA, Ribosomal, 16S, Sequence Analysis, DNA, Soil Microbiology, Time Factors, Volcanic Eruptions}, issn = {0168-6496}, doi = {10.1111/j.1574-6941.2006.00253.x}, author = {Gomez-Alvarez, Vicente and King, Gary M and N{\"u}sslein, Klaus} } @article {744, title = {Salinity constraints on subsurface archaeal diversity and methanogenesis in sedimentary rock rich in organic matter.}, journal = {Appl Environ Microbiol}, volume = {73}, year = {2007}, month = {2007 Jul}, pages = {4171-9}, abstract = {The diversity of microorganisms active within sedimentary rocks provides important controls on the geochemistry of many subsurface environments. In particular, biodegradation of organic matter in sedimentary rocks contributes to the biogeochemical cycling of carbon and other elements and strongly impacts the recovery and quality of fossil fuel resources. In this study, archaeal diversity was investigated along a salinity gradient spanning 8 to 3,490 mM Cl(-) in a subsurface shale rich in CH(4) derived from biodegradation of sedimentary hydrocarbons. Shale pore waters collected from wells in the main CH(4)-producing zone lacked electron acceptors such as O(2), NO(3)(-), Fe(3+), or SO(4)(2-). Acetate was detected only in high-salinity waters, suggesting that acetoclastic methanogenesis is inhibited at Cl(-) concentrations above approximately 1,000 mM. Most-probable-number series revealed differences in methanogen substrate utilization (acetate, trimethylamine, or H(2)/CO(2)) associated with chlorinity. The greatest methane production in enrichment cultures was observed for incubations with salinity at or close to the native pore water salinity of the inoculum. Restriction fragment length polymorphism analyses of archaeal 16S rRNA genes from seven wells indicated that there were links between archaeal communities and pore water salinity. Archaeal clone libraries constructed from sequences from 16S rRNA genes isolated from two wells revealed phylotypes similar to a halophilic methylotrophic Methanohalophilus species and a hydrogenotrophic Methanoplanus species at high salinity and a single phylotype closely related to Methanocorpusculum bavaricum at low salinity. These results show that several distinct communities of methanogens persist in this subsurface, CH(4)-producing environment and that each community is adapted to particular conditions of salinity and preferential substrate use and each community induces distinct geochemical signatures in shale formation waters.}, keywords = {Archaea, Base Sequence, Cloning, Molecular, DNA Primers, Genes, Archaeal, Genetic Variation, Geologic Sediments, Methane, Michigan, Molecular Sequence Data, Organic Chemicals, Phylogeny, RNA, Archaeal, RNA, Ribosomal, 16S, Sodium Chloride, Soil, Soil Microbiology, Water Microbiology}, issn = {0099-2240}, doi = {10.1128/AEM.02810-06}, author = {Waldron, Patricia J and Petsch, Steven T and Martini, Anna M and N{\"u}sslein, Klaus and N{\"u}slein, Klaus} } @article {748, title = {Distribution of extensive nifH gene diversity across physical soil microenvironments.}, journal = {Microb Ecol}, volume = {51}, year = {2006}, month = {2006 May}, pages = {441-52}, abstract = {The diversity of nitrogen-fixing bacteria is well described for aquatic environments; however, terrestrial analyses remain mostly biased to rhizobial plant-microbe associations. We maximized the level of resolution for this study through the use of nucleotide sequence information extracted from a series of soil microenvironments, ranging from macroaggregates at 2000 microm to the clay fraction at < 75 microm in diameter. In addition, we attempted to create an overview of the distribution of terrestrial nitrogen fixers across such microenvironments by combining culture-independent techniques with a suite of natural soil environments from uniquely different origins. Soil diazotroph diversity was analyzed phylogenetically for 600 terrestrial nifH sequences from 12 midsized clone libraries based on microenvironments of three separate soils across a global scale. Statistical analyses of nifH gene clone libraries were used to estimate coverage, establish degrees of sequence overlap, and compare cluster distributions. These analyses revealed an extensive diversity in a tropical (19 phylotypes) and an arctic soil (17 phylotypes), and moderate diversity in a temperate soil (11 phylotypes). Within each soil, comparisons across aggregate size fractions delineated nifH gene cluster shifts within populations and degrees of sequence overlap that ranged from significantly different (arctic, tropical) to significantly similar (temperate). We suggest that this is due to population separation across aggregates of different size classes, which results from differences in the temporal stability of aggregates as niches for microbial communities. This study not only provides new knowledge of the arrangement of diazotrophic communities at the soil microscale, but it also contributes to the underrepresented knowledge of soil nifH sequences in the public databases.}, keywords = {Bacteria, Base Sequence, DNA Primers, Genes, Bacterial, Multigene Family, Oxidoreductases, Phylogeny, Polymerase Chain Reaction, Soil Microbiology}, issn = {0095-3628}, doi = {10.1007/s00248-006-9044-x}, author = {Izquierdo, Javier A and N{\"u}sslein, Klaus} }