Patricia Bonin

Comparison of Methods for Quantification of Cytochrome cd1-Denitrifying Bacteria in Environmental Marine Samples

ABSTRACT Two PCR primer sets were developed for the detection and quantification of cytochrome cd1-denitrifying bacteria in environmental marine samples. The specificity and sensitivity of these primers were tested. Both primer sets were suitable for detection, but only one set, cd3F–cd4R, was suitable for the quantification and enumeration of the functional community using most-probable-number PCR and competitive PCR techniques. Quantification of cytochrome cd1 denitrifiers taken from marine sediment and water samples was achieved using two different molecular techniques which target the nirS gene, and the results were compared to those obtained by using the classical cultivation method. Enumerations using both molecular techniques yielded similar results in seawater and sediment samples. However, both molecular techniques showed 1,000 or 10 times more cytochromecd1 denitrifiers in the sediment or water samples, respectively, than were found by use of the conventional cultivation method for counting.

Influence of bioturbation on denitrification activity in Mediterranean coastal sediments: an in situ experimental approach

An in situ experiment was conducted in the French Mediterranean littoral (Gulf of Fos) from July 1993 to January 1994 using controls without macrofauna or natural sediments. After 1 . 4 and 6 mo, sediment reworhng and denitnfication activities (natural and potential rates) were studied. The bacterial processes were stimulated by the bioturbating activity of the autochthonous infauna The natural and potential denitrification rates were 160 and 280% higher, respectively, than in the controls. The increase of denitrification, occurring at different depths in the sediment with respect to time, was directly dependent on the macrofaunal activity.

Nitrogen-limited mangrove ecosystems conserve N through dissimilatory nitrate reduction to ammonium

Earlier observations in mangrove sediments of Goa, India have shown denitrification to be a major pathway for N loss1. However, percentage of total nitrate transformed through complete denitrification accounted for <0–72% of the pore water nitrate reduced. Here, we show that up to 99% of nitrate removal in mangrove sediments is routed through dissimilatory nitrate reduction to ammonium (DNRA). The DNRA process was 2x higher at the relatively pristine site Tuvem compared to the anthropogenically-influenced Divar mangrove ecosystem. In systems receiving low extraneous nutrient inputs, this mechanism effectively conserves and re-circulates N minimizing nutrient loss that would otherwise occur through denitrification. In a global context, the occurrence of DNRA in mangroves has important implications for maintaining N levels and sustaining ecosystem productivity. For the first time, this study also highlights the significance of DNRA in buffering the climate by modulating the production of the greenhouse gas nitrous oxide.

Isolation and characterization of Thermanaerothrix daxensis gen. nov., sp. nov., a thermophilic anaerobic bacterium pertaining to the phylum “Chloroflexi”, isolated from a deep hot aquifer in the Aquitaine Basin ☆

A new strictly anaerobic thermophilic multicellular filamentous bacterium (0.2-0.3μm×>100μm), designated GNS-1(T), was isolated from a deep hot aquifer in France. It was non-motile, and stained Gram-negative. Optimal growth was observed at 65°C, pH 7.0, and 2gL(-1) of NaCl. Strain GNS-1(T) was chemoorganotrophic fermenting ribose, glucose, galactose, arabinose, fructose, mannose, maltose, sucrose, xylose, raffinose, pyruvate, and xylan. Yeast extract was required for growth. The end products of glucose fermentation were lactate, acetate, CO(2), and H(2). The G+C content of the DNA was 57.6mol%. Its closest phylogenetic relative was Bellilinea caldifistulae with 92.5% similarity. Based on phylogenetic, genotypic and phenotypic characteristics, strain GNS-1(T) (DSM 23592(T), JCM 16980(T)) is proposed to be assigned to a novel species of a novel genus within the class Anaerolineae (subphylum I), phylum Chloroflexi, Thermanaerothrix daxensis gen. nov., sp. nov. The GenBank accession number is HM596746.

Aerobic and anaerobic metabolism of squalene by a denitrifying bacterium isolated from marine sediment

Abstract. The aerobic and anaerobic metabolism of the isoprenoid alkene squalene was investigated in a new type of marine denitrifying bacterium, strain 2sq31, isolated from marine sediment. Strain 2sq31 was identified as a species of Marinobacter. Under denitrifying conditions, the strain efficiently degraded squalene; of 0.7xa0mmol added per liter of medium, 77% was degraded within 120xa0days under anoxic conditions with nitrate as electron acceptor. Tertiary diols and methyl ketones were identified as metabolites, and an anaerobic pathway was suggested to explain the formation of such compounds. The first step in anaerobic degradation of squalene by strain 2sq31 involves hydration of double bonds to tertiary alcohols. Under oxic conditions, the degradation of squalene by strain 2sq31 was rapid and involved oxidative splitting of the C-10/C-11 or C-14/C-15 double bonds, in addition to the pathways observed under denitrifying conditions.

Caldilinea tarbellica sp. nov., a filamentous, thermophilic, anaerobic bacterium isolated from a deep hot aquifer in the Aquitaine Basin

An anaerobic, thermophilic, filamentous (0.45 × >100 µm) bacterium, designated D1-25-10-4(T), was isolated from a deep hot aquifer in France. Cells were non-motile and Gram-negative. Growth was observed at 43-65 °C (optimum 55 °C), at pH 6.8-7.8 (optimum pH 7.0) and with 0-5 g NaCl l(-1) (optimum 0 g NaCl l(-1)). Strain D1-25-10-4(T) was a chemo-organotroph and fermented ribose, maltose, glucose, galactose, arabinose, fructose, mannose, sucrose, raffinose, xylose, glycerol, fumarate, peptone, starch and xylan. Yeast extract was required for growth. Sulfate, thiosulfate, sulfite, elemental sulfur, nitrate, nitrite and fumarate were not used as terminal electron acceptors. The G+C content of the DNA was 61.9 mol%. The major cellular fatty acids of strain D1-25-10-4(T) were C(17 : 0), C(18 : 0,) C(16 : 0) and iso-C(17 : 0). The closest phylogenetic relative of strain D1-25-10-4(T) was Caldilinea aerophila STL-6-O1(T) (97.9 % 16S rRNA gene sequence similarity). DNA-DNA relatedness between strain D1-25-10-4(T) and Caldilinea aerophila DSM 14535(T) was 8.7 ± 1u200a%. On the basis of phylogenetic, genotypic and phenotypic characteristics, strain D1-25-10-4(T) represents a novel species within the genus Caldilinea, class Caldilineae, phylum Chloroflexi, for which the name Caldilinea tarbellica sp. nov. is proposed. The type strain is D1-25-10-4(T) (u200a=u200aDSM 22659(T) u200a=u200aJCM 16120(T)).

Potential alteration of U37K′ paleothermometer due to selective degradation of alkenones by marine bacteria isolated from the haptophyte Emiliania huxleyi

The unsaturation ratio of C(37) alkenones (U(37)(K)) produced by haptophyte microalgae such as Emiliania huxleyi is often used as proxy for past sea surface temperature. In this study, 29 bacterial strains were isolated from cultures of the strain E. huxleyi TWP1. Among alkenone-degrading isolates, the strain Dietzia maris sp. S1 appeared to be able to selectively degrade alkenones leading to increases in the palaeoenvironmental proxy U(37)(K) by +0.05 to +0.10 units, which is equivalent to the change seen when the growth temperature is increased by 1.5-3.0 degrees C. This degradation was shown to involve initial epoxidation of the alkenone double bonds presumably by a monooxygenase, which showed a preference for oxidation of the omega29 double bond. Inconsistencies observed in previous studies of the aerobic microbial degradation of alkenones may simply reflect which species of bacteria were present. Our results confirm that intense aerobic bacterial degradative processes can introduce a bias in palaeotemperature reconstructions especially when there is evidence of substantial aerobic bacterial degradation of the deposited organic matter. The widespread occurrence of epoxyalkenones in the marine environment strongly suggests that selective aerobic bacterial degradation could be major source of uncertainty for palaeotemperature estimation.

Effect of crude oil on denitrification and sulfate reduction in marine sediments

The denitrifying activity was measured in different types of sediment from the Mediterranean coast of France before, and after, a massive contamination (30–100 g kg-1 sediment) of hydrocarbons. A closed system was used in order to maintain anoxic conditions and to control substrates and gaseous products concentrations. We have demonstrated that the respiratory metabolism was inhibited in all cases following an incubation time of 20 to 50 days. At this time, the addition of lactate restore the denitrifying activity. The inhibitory effect of crude oil was not related to an alteration of bacterial cells, but to changes in environmental conditions allowing denitrification. The presence of hydrocarbons in the sediments causes a decrease in the redox potential and a concomitant stimulation of the sulfate reduction.

Production of a polyunsaturated isoprenoid wax ester during aerobic metabolism of squalene by Marinobacter squalenivorans sp. nov.

ABSTRACT This paper describes the production of 5,9,13-trimethyltetradeca-4E,8E,12-trienyl-5,9,13-trimethyltetradeca-4E,8E,12-trienoate during the aerobic degradation of squalene by a Marinobacter strain, 2Asq64, isolated from the marine environment. A pathway involving initial cleavage of the C10-C11 or C14-C15 double bonds of the squalene molecule is proposed to explain the formation of this polyunsaturated isoprenoid wax ester. The isoprenoid wax ester content reached 1.1% of the degraded squalene at the mid-exponential growth phase and then decreased during the stationary phase. The wax ester content increased by approximately threefold in N-limited cultures, in which the ammonium concentration corresponds to conditions often found in marine sediments. This suggests that the bacterial formation of isoprenoid wax esters might be favored in such environments. The bacterial strain is then characterized as a member of a new species, for which we propose the name Marinobacter squalenivorans sp. nov.

The anaerobic hydrocarbon biodegrading bacteria: An overview

Abstract Hydrocarbons are widespread in our environment. The number of bacteria known to oxidize hydrocarbons in the absence of oxygen has considerably increased during the last ten years. Anaerobic bacteria have been shown capable of utilizing hydrocarbons not only in consortia but also in pure cultures. The results obtained in the framework of MATBIOPOL project on anaerobic hydrocarbon degradation by denitrifying bacteria and by enrichment cultures maintained under methanogenic conditions are exposed together with the present knowledge on hydrocarbon biodegradation.