Antje Rusch

Activity and distribution of bacterial populations in Middle Atlantic Bight shelf sands

Abstract Spatiotemporal variation and metabolic activity of the microbial community were studied in coarse-grained Middle Atlantic Bight shelf sediments in relation to pools of dissolved and particulate carbon. Algal cells were present 8->70 mum) fraction of the sediment held the major share (61-98%) of benthic bacteria. Bacterial and algal cell abundances, exoenzymatic activity, and [DOC] generally showed higher values in May/July 2001 than in August/December 2000. Carbohydrates and proteins were hydrolyzed at potential rates of 1-12 nmol cm(-3) h(-1) (beta-glucosidase) and 3-70 nmol cm(-3) h(-1) (aminopeptidase), respectively. Fluorescence in situ hybridization analyses of the benthic microbes assigned 45-56% of DAPI-stained cells to Eubacteria and less than 2% to Eukarya. The prokaryotic community was dominated by planctomycetes and members of the Cytophaga/Flavobacterium cluster. Near the sediment surface, iodonitrotetrazolium violet reducing cells, that are considered actively respiring, amounted to 15-29% of total bacteria. Despite a low organic content (particulate organic carbon <0.03%) and relatively low bacterial abundances (<10(9) cm(-3)), the Middle Atlantic Bight shelf sediments showed organic matter turnover rates that are comparable to those found in organic-rich finer-grained deposits. Our findings suggest a high biocatalytic filtration activity in these coarse permeable sediments.

Bacteria, diatoms and detritus in an intertidal sandflat subject to advective transport across the water-sediment interface

This study focused on organic particles withrespect to their transport and sedimentarymineralisation in a North Sea intertidalsandflat previously characterised as stronglyinfluenced by advective transport across andbelow the water-sediment interface. Measuredpermeabilities of the sandy sediment rangedfrom 5.5 to 41⋅10−12 m2, andpermeabilities calculated from granulometricdata exceeded the measured values by a factorof 4.4 ∓ 2.8. Bacteria (2–9% of the POC)were highly variable in space and time. Theywere less mobile than interstitial fine (<70 µm) organic and inorganic particles, aspart of the population lived attached to large,heavy sand grains. The vertical distribution ofbacteria was closely related to the organiccarbon content of the fine-grained interstitialmaterial. In winter, bacterial numbers in theuppermost 5 cm amounted to 39–69% of thesummer ones. Carbon mineralisation rates rangedbetween 20 mg C m−2 d−1 in winter and580 mg C m−2 d−1 in summer, keepingstep with finer-grained sediments thatcontained an order of magnitude more organiccarbon. Sedimentary carbohydrates were mainlyintracellular or tightly bound to particles,and their concentrations were depth-invariantin winter, but exponentially decreasing withdepth in summer. Below 5 cm depth, the meanconcentration was (1590 ∓830) µg cm−3, without major downcoreor seasonal changes. Phytobenthos andphytodetritus were dominated by diatoms andcomprised merely minor amounts of other primaryproducers. Planktonic diatom depth profileswere related to weather and phytoplanktonconditions, and benthic diatoms showed similardepth distributions due to passive and activemotion. The penetration of relatively freshphytodetritus down to at least 5 cm, shown bychloropigment composition, emphasised the closecoupling between water column and sandysediment, facilitated by advective interfacialand subsurface flows.

An oligarchic microbial assemblage in the anoxic bottom waters of a volcanic subglacial lake

In 2006, we sampled the anoxic bottom waters of a volcanic lake beneath the Vatnajökull ice cap (Iceland). The sample contained 5 × 105 cells per ml, and whole-cell fluorescent in situ hybridization (FISH) and PCR with domain-specific probes showed these to be essentially all bacteria, with no detectable archaea. Pyrosequencing of the V6 hypervariable region of the 16S ribosomal RNA gene, Sanger sequencing of a clone library and FISH-based enumeration of four major phylotypes revealed that the assemblage was dominated by a few groups of putative chemotrophic bacteria whose closest cultivated relatives use sulfide, sulfur or hydrogen as electron donors, and oxygen, sulfate or CO2 as electron acceptors. Hundreds of other phylotypes are present at lower abundance in our V6 tag libraries and a rarefaction analysis indicates that sampling did not reach saturation, but FISH data limit the remaining biome to <10–20% of all cells. The composition of this oligarchy can be understood in the context of the chemical disequilibrium created by the mixing of sulfidic lake water and oxygenated glacial meltwater.

Order-specific 16S rRNA-targeted oligonucleotide probes for (hyper)thermophilic archaea and bacteria

New oligonucleotide probes were designed and evaluated for application in fluorescence in situ hybridization (FISH) studies on (hyper)thermophilic microbial communities—Arglo32, Tcoc164, and Aqui1197 target the 16S rRNA of Archaeoglobales, Thermococcales, and Aquificales, respectively. Both sequence information and experimental evaluation showed high coverage and specificity of all three probes. The signal intensity of Aqui1197 was improved by addition of a newly designed, unlabeled “helper” oligonucleotide, hAqui1045. It was shown that in addition to its function as a probe for Aquificales, Aqui1197 is suitable as a supplementary probe to extend the coverage of the domain-specific bacterial probe EUB338. In sediments from two hydrothermal seeps on Vulcano Island, Italy, the microbial community structure was analyzed by FISH with both established and the new oligonucleotide probes, showing the applicability of Arglo32, Tcoc164, and Aqui1197/hAqui1045 to natural samples. At both sites, all major groups of (hyper)thermophiles, except for methanogens, were detected: Crenarchaeota (19%, 16%), Thermococcales (14%, 22%), Archaeoglobales (14%, 12%), Aquificales (5%, 8%), Thermotoga/Thermosipho spp. (12%, 9%), Thermus sp. (12%, none), and thermophilic Bacillus sp. (12%, 8%).

Stable Sulfur Isotope Effects Related to Local Intense Sulfate Reduction in a Tidal Sandflat (Southern North Sea): Results from Loading Experiments

Abstract Anoxic sediment surfaces coloured black by iron monosulfides (“black spots”) evolve in tidal sandflats of the Wadden Sea (southern North Sea) as a result of the degradation of buried organic matter. To follow the short- and long-term effects of organic matter burial on pore water and sediment isotopic biogeochemistry, formation of artificial black spots was initiated on the Groninger Plate (site RP63) in the backbarrier tidal flats of Spiekeroog island. Changes in concentrations (DOC, TA, TOC, sulfate, sulfide, TRS, Fe) and isotopic compositions (sulfate, sulfide, TRS, pyrite, TOC) were followed for up to 12 months and compared to reference areas. 13°C ratios of TOC clearly mirror the early diagenetic degradation of organic matter. At least temporarily closed system sulfate reduction is inferred for the artificial black spot from the variation of sulfate concentrations and stable sulfur isotope partitioning, In the interstitial waters of the black spot, 34S/32S values of coexisting dissolved sulf...

Molecular Tools for the Detection of Nitrogen Cycling Archaea

Archaea are widespread in extreme and temperate environments, and cultured representatives cover a broad spectrum of metabolic capacities, which sets them up for potentially major roles in the biogeochemistry of their ecosystems. The detection, characterization, and quantification of archaeal functions in mixed communities require Archaea-specific primers or probes for the corresponding metabolic genes. Five pairs of degenerate primers were designed to target archaeal genes encoding key enzymes of nitrogen cycling: nitrite reductases NirA and NirB, nitrous oxide reductase (NosZ), nitrogenase reductase (NifH), and nitrate reductases NapA/NarG. Sensitivity towards their archaeal target gene, phylogenetic specificity, and gene specificity were evaluated in silico and in vitro. Owing to their moderate sensitivity/coverage, the novel nirB-targeted primers are suitable for pure culture studies only. The nirA-targeted primers showed sufficient sensitivity and phylogenetic specificity, but poor gene specificity. The primers designed for amplification of archaeal nosZ performed well in all 3 criteria; their discrimination against bacterial homologs appears to be weakened when Archaea are strongly outnumbered by bacteria in a mixed community. The novel nifH-targeted primers showed high sensitivity and gene specificity, but failed to discriminate against bacterial homologs. Despite limitations, 4 of the new primer pairs are suitable tools in several molecular methods applied in archaeal ecology.

Burkholderia insulsa sp. nov., a facultatively chemolithotrophic bacterium isolated from an arsenic-rich shallow marine hydrothermal system.

Enrichment cultures inoculated with hydrothermally influenced nearshore sediment from Papua New Guinea led to the isolation of an arsenic-tolerant, acidophilic, facultatively aerobic bacterial strain designated PNG-April(T). Cells of this strain were Gram-stain-negative, rod-shaped, motile and did not form spores. Strain PNG-April(T) grew at temperatures between 4 °C and 40 °C (optimum 30-37 °C), at pH 3.5 to 8.3 (optimum pH 5-6) and in the presence of up to 2.7% NaCl (optimum 0-1.0%). Both arsenate and arsenite were tolerated up to concentrations of at least 0.5 mM. Metabolism in strain PNG-April(T) was strictly respiratory. Heterotrophic growth occurred with O2 or nitrate as electron acceptors, and aerobic lithoautotrophic growth was observed with thiosulfate or nitrite as electron donors. The novel isolate was capable of N2-fixation. The respiratory quinones were Q-8 and Q-7. Phylogenetically, strain PNG-April(T) belongs to the genus Burkholderia and shares the highest 16S rRNA gene sequence similarity with the type strains of Burkholderia fungorum (99.8%), Burkholderia phytofirmans (98.8%), Burkholderia caledonica (98.4%) and Burkholderia sediminicola (98.4%). Differences from these related species in several physiological characteristics (lipid composition, carbohydrate utilization, enzyme profiles) and DNA-DNA hybridization suggested the isolate represents a novel species of the genus Burkholderia, for which we propose the name Burkholderia insulsa sp. nov. The type strain is PNG-April(T) ( = DSM 28142(T) = LMG 28183(T)).

Nitrogen‐cycling bacteria and archaea in the carbonate sediment of a coral reef

In the coarse-grained carbonate sediments of coral reefs, advective porewater flow and the respiration of organic matter establish redox zones that are the scene of microbially mediated transformations of N compounds. To investigate the geobiology of N cycling in reef sediments, the benthic microbiota of Checker Reef in Kaneohe Bay, Hawaii, were surveyed for candidate nitrate reducers, ammonifying nitrite reducers, aerobic and anaerobic ammonia oxidizers (anammox) by identifying phylotypes of their key metabolic genes (napA, narG, nrfA, amoA) and ribotypes (unique RNA sequences) of anammox-like 16S rRNA. Putative proteobacteria with the catalytic potential for nitrate reduction were identified in oxic, interfacial and anoxic habitats. The estimated richness of napA (≥202 in anoxic sediment) and narG (≥373 and ≥441 in oxic and interfacial sediment, respectively) indicates a diverse guild of nitrate reducers. The guild of nrfA hosts in interfacial reef sediment was dominated by Vibrio species. The identified members of the aerobic ammonium oxidizing guild (amoA hosts) were Crenarchaeota or close relatives of Nitrosomonadales. Putative anammox bacteria were detected in the RNA pool of Checker Reef sediment. More than half of these ribotypes show ≥90% identity with homologous sequences of Scalindua spp., while no evidence was found for members of the genera Brocadia or Kuenenia. In addition to exploring the diversity of these four nitrogen-cycling microbial guilds in coral reef sediments, the abundances of aerobic ammonium oxidizers (amoA), nitrite oxidizers (nxrAB), ammonifying nitrite reducers (nrfA) and denitrifiers (nosZ) were estimated using real-time PCR. Representatives of all targeted guilds were detected, suggesting that most processes of the biogeochemical N cycle can be catalyzed by the benthic microbiota of tropical coral reefs.