Factors affecting the distribution of stream macroinvertebrates in geothermal areas: Taupo Volcanic Zone,New Zealand

The distribution of macroinvertebrates was investigated among sites within five geothermally influenced and two non- or minimally-influenced streams in the Taupo Volcanic Zone, New Zealand, to examine the responses of communities to broad environmental gradients within and among habitats. To date, examination of geothermal stream macroinvertebrates has typically been from single habitats, and has not been examined over a regional scale. Sites within and among streams represented a range of sizes, depths, water velocities and substrate types. Sites with little or no geothermal influence typically had temperatures less than 15°C and pH between 5 and 8. Four of the geothermally influenced streams had temperatures greater than 25°C, and ranged from alkaline (pH 9.1) to highly acidic (pH 3.0). Most taxa recorded were typical inhabitants of non-geothermal streams that are tolerant to elevated temperatures, extreme pH conditions and/or high toxicant levels. Diptera, Coleoptera and Mollusca dominated geothermal sites, and Ephemeroptera, Plecoptera and Trichoptera were absent. In addition, an obligate dweller of geothermal habitats, Ephydrella thermarum, and a nonindigenous tropical gastropod, Melanoides tuberculata, were recorded. Canonical correspondence analysis implicated multiple factors in determining the distribution of invertebrates over the region. Overall, distribution was most strongly associated with temperature gradients, particularly longitudinally within streams. This distribution was likely directly related to species temperature tolerances, but also temperature effects on algal abundance and composition, its differential effects on species’ potential competitors and predators, and its effects on toxicant availability. Differences in invertebrate composition among streams were associated with major differences in pH and substrate. Increased acidity was associated with a significant decrease in invertebrate taxa richness, with acidic sites having a limited fauna dominated by dipterans (e.g., Naonella sp., Polypedilum sp.). Stability of flow and environmental conditions may enhance competitive interactions among taxa, enhancing the importance of substrate type in these systems. The presence of non-indigenous species (e.g., M. tuberculata, Poecilia reticulata), currently limited in distribution, also affected species composition. Overall, communities become less speciose, although more unusual in composition, with increased geothermal influence. Electronic supplementary material The online version of this article (doi:) contains supplementary material, which is available to authorized users. Handling editor: K. Martens     

A review on the occurrence and taxonomy of heterotrophic protists in extreme acidic environments of pH values ≤ 3

The occurrence and some important taxonomic problems of heterotrophic protists from extremely acidic (pH 3) environments are briefly discussed. Almost all information on the occurrence of heterotrophic protists from extremely acidic environments is restricted to acid mine drainage (AMD) or streams influenced by AMD. Most of the information is provided for ciliates. Very little information is available on the occurrence of flagellates, rhizopods and heliozoa in this environment. Within the ciliates Urotricha, Vorticella and Oxytricha dominate in acidic mining lakes. Actinophrys sp. is the most important heliozoan in these environments. There are many taxonomic problems which are not solved so far. Live observations and taxonomic methods adapted to the extreme chemical matrix are necessary for correct identification.     

Diversity of thermophilic fungi in Tengchong Rehai national park revealed by ITS nucleotide sequence analyses

The geothermal sites near neutral and alkalescent thermal springs in Tengchong Rehai National Park were examined through cultivation-dependent approach to determine the diversity of thermophilic fungi in these environments. Here, we collected soils samples in this area, plated on agar media conducive for fungal growth, obtained pure cultures, and then employed the method of internal transcribed spacer (ITS) sequencing combined with morphological analysis for identification of thermophilic fungi to the species level. In total, 102 strains were isolated and identified as Rhizomucor miehei, Chaetomium sp., Talaromyces thermophilus, Talaromyces byssochlamydoides, Thermoascus aurantiacus Miehe var. levisporus, Thermomyces lanuginosus, Scytalidium thermophilum, Malbranchea flava, Myceliophthora sp. 1, Myceliophthora sp. 2, Myceliophthora sp. 3, and Coprinopsis sp. Two species, T. lanuginosus and S. thermophilum were the dominant species, representing 34.78% and 28.26% of the sample, respectively. Our results indicated a greater diversity of thermophilic fungi in neutral and alkaline geothermal sites than acidic sites around hot springs reported in previous studies. Most of our strains thrived at alkaline growth conditions.     

Tetramitus thermacidophilus n. sp., an amoeboflagellate from acidic hot springs

ABSTRACT. Tetramitus thermacidophilus n. sp. is a novel thermophilic and acidophilic amoeboflagellate isolated from acidic hot springs in the Caldera Uzon (Kamchatka, Russia) and in Pisciarelli Solfatara (Naples, Italy). We describe it based on physiological, morphological, and sequence data. It was grown in monoxenic culture on the archaeon Acidianus brierleyi as food. Tetramitus thermacidophilus multiplies in a pH range from 1.2 to 5 and in a temperature range from 28 °C to 54 °C. The shortest doubling time was 4.5 h at pH 3 at 45 °C. Its spindle-shaped biflagellated stage was only rarely found in culture. The amoeboid stage shows the typical locomotive form of vahlkampfiid amoebae. Sequence comparisons of the internal transcribed spacer sequences and the small subunit rRNA genes confirm that T. thermacidophilus is a novel species within the genus Tetramitus and that both isolates belong to that species.     

Microbial biogeochemistry of Boiling Springs Lake: a physically dynamic,oligotrophic, low‐pH geothermal ecosystem

Boiling Springs Lake (BSL) in Lassen Volcanic National Park, California, is North America's largest hot spring, but little is known about the physical, chemical, and biological features of the system. Using a remotely operated vessel, we characterized the bathymetry and near‐surface temperatures at sub‐meter resolution. The majority of the 1.2 ha, pH 2.2 lake is 10 m deep and 50–52 °C, but temperatures reach 93 °C locally. We extracted DNA from water and sediments collected from warm (52 °C) and hot (73–83 °C) sites separated by 180 m. Gene clone libraries and functional gene microarray (GeoChip 3.0) were used to investigate the BSL community, and uptake of radiolabeled carbon sources was used to assess the relative importance of heterotrophic vs. autotrophic production. Microbial assemblages are similar in both sites despite the strong temperature differential, supporting observations of a dynamic, convectively mixed system. Bacteria in the Actinobacteria and Aquificales phyla are abundant in the water column, and Archaea distantly related to known taxa are abundant in sediments. The functional potential appears similar across a 5‐year time span, indicating a stable community with little inter‐annual variation, despite the documented seasonal temperature cycle. BSL water‐derived DNA contains genes for complete C, N, and S cycles, and low hybridization to probes for N and S oxidation suggests that reductive processes dominate. Many of the detected genes for these processes were from uncultivated bacteria, suggesting novel organisms are responsible for key ecosystem services. Selection imposed by low nutrients, low pH, and high temperature appear to result in low diversity and evenness of genes for key functions involved in C, N, and S cycling. Conversely, organic degradation genes appear to be functionally redundant, and the rapid assimilation of radiolabeled organic carbon into BSL cells suggests the importance of allochthonous C fueling heterotrophic production in the BSL C cycle.     

Podomonas kaiyoae n. sp., a novel apusomonad growing axenically

Apusomonadida (apusomonads) is a group of heterotrophic biflagellates that feed on bacteria and small protists. Their diversity is not fully understood, and several major lineages remain to be identified in natural environments. Here, we report Podomonas kaiyoae n. sp., which was isolated from deep-sea sediment and can be maintained as an axenic culture. While P. kaiyoae branched within one of the major unidentified lineages, the combination of the morphological characteristics is generally similar to that of Podomonas species, but can be distinguished from that of other Podomonas species based on the cell sizes.     

Two new Tetramitus species (Heterolobosea, Vahlkampfiidae) from cold aquatic environments

Characterisation of the protists of cold environments provides important background for assessing the effects of climate change on microbial communities. Tetramitus angularis n. sp., from aquatic environments in Iceland and Switzerland, is the first vahlkampfiid recognised to have a characteristic Tetramitus flagellate stage combined with pre-formed excystment pores, which are not typical of this genus. T. angularis amoebae have a typical vahlkampfiid locomotive form and contain prominent lipid inclusions. Flagellates have a collar and cytostome, and can be mono- to multi-nucleate with corresponding change in cell shape from cylindrical to ellipsoidal and variable number of flagella. Cysts are round to semi-angular and have 2-5 pores closed by protruding, translucent plugs. A second organism, T. parangularis n. sp. from Alaska, has similar cysts but a flagellate stage has not been recognised; ITS sequence divergence is consistent with species criteria in the Vahlkampfiidae. Phylogenetic analysis of sequence data for the 5.8S rDNA region clusters the new spp. with T. rostratus, T. entericus and T. waccamawensis.     

Different Marine Heterotrophic Nanoflagellates Affect Differentially the Composition of Enriched Bacterial Communities

We studied the effects of predation on the cytometric and phylogenetic features of two enriched bacterial communities obtained from two cultures of marine heterotrophic nanoflagellates: Jakoba libera and a mixed culture of Cafeteria sp. and Monosiga sp. Protists were harvested by flow cytometric cell sorting and eight different treatments were prepared. Each bacterial community was incubated with and without protists, and we added two treatments with protists and the bacteria present after the sorting procedure (cosorted bacteria). The bacterial community derived from the culture of Jakoba libera had higher green fluorescence per cell (FL1) than that derived from the mixed culture of Cafeteria sp. and Monosiga sp. When the experiment began all treatments presented bacterial communities that increase in fluorescence per bacterium (FL1); after that the FL1 decreased when bacteria attained maximal concentrations; and, finally, there was a new increase in FL1 toward the end of the experiment. Cosorted bacteria of Jakoba libera had the same fluorescence as the bacterial community derived from this protist, while the bacteria derived from the mixed culture of Cafeteria sp. and Monosiga sp. was nearly twice as fluorescent than that of the parental community. All treatments presented a general decline of SSC along the incubation. Therefore, there was a small influence of protists on the cytometric signature of each bacterial community. However, each bacterial community preyed by Jakoba libera or the mixed culture of Cafeteria sp. and Monosiga sp. led to four different phylogenetic fingerprint. Besides, the final Communities were different from the fingerprint of controls without protists, and most of them diverge from the fingerprint of cosorted bacteria. Our results confirm that changes in the phylogenetic composition of marine bacterial communities may depend on the initial communities of both bacteria and protists.     

Linking microbial oxidation of arsenic with detection and phylogenetic analysis of arsenite oxidase genes in diverse geothermal environments

The identification and characterization of genes involved in the microbial oxidation of arsenite will contribute to our understanding of factors controlling As cycling in natural systems. Towards this goal, we recently characterized the widespread occurrence of aerobic arsenite oxidase genes (aroA‐like) from pure‐culture bacterial isolates, soils, sediments and geothermal mats, but were unable to detect these genes in all geothermal systems where we have observed microbial arsenite oxidation. Consequently, the objectives of the current study were to measure arsenite‐oxidation rates in geochemically diverse thermal habitats in Yellowstone National Park (YNP) ranging in pH from 2.6 to 8, and to identify corresponding 16S rRNA and aroA genotypes associated with these arsenite‐oxidizing environments. Geochemical analyses, including measurement of arsenite‐oxidation rates within geothermal outflow channels, were combined with 16S rRNA gene and aroA functional gene analysis using newly designed primers to capture previously undescribed aroA‐like arsenite oxidase gene diversity. The majority of bacterial 16S rRNA gene sequences found in acidic (pH 2.6–3.6) Fe‐oxyhydroxide microbial mats were closely related to Hydrogenobaculum spp. (members of the bacterial order Aquificales), while the predominant sequences from near‐neutral (pH 6.2–8) springs were affiliated with other Aquificales including Sulfurihydrogenibium spp., Thermocrinis spp. and Hydrogenobacter spp., as well as members of the Deinococci, Thermodesulfobacteria and β‐Proteobacteria. Modified primers designed around previously characterized and newly identified aroA‐like genes successfully amplified new lineages of aroA‐like genes associated with members of the Aquificales across all geothermal systems examined. The expression of Aquificales aroA‐like genes was also confirmed in situ, and the resultant cDNA sequences were consistent with aroA genotypes identified in the same environments. The aroA sequences identified in the current study expand the phylogenetic distribution of known Mo‐pterin arsenite oxidase genes, and suggest the importance of three prominent genera of the order Aquificales in arsenite oxidation across geochemically distinct geothermal habitats ranging in pH from 2.6 to 8.     

Environmental gradients determining the distribution of benthic macroinvertebrates in Lake Takkobu, Kushiro wetland, northern Japan

Effects of environmental variables on the distribution of benthic macroinvertebrates inhabiting sediments were studied at 25 sites along the shoreline of Lake Takkobu in the Kushiro wetland of northern Japan in summer 2003. During the last decade, the lake’s status has undergone a drastic shift from clear water dominated by submerged macrophytes to turbid water dominated by phytoplankton. The canonical correspondence analysis showed that four environmental variables explained the significant variation in the macroinvertebrate species composition: submerged plant biomass, bottom sediment organic matter content (OMC), distance from the mouth of the Takkobu River, and bottom-layer pH. Five species of Chironomidae [Chironomus sp. (except plumosus group), Psectrocladius sp., Corynoneura sp., Parachironomus sp. arcuatus group, and Zavreliella sp.] occurred in sites with relatively lower pH and a high submerged plant biomass, whereas three species of Tubificidae (Tubifex tubifex, Aulodrilus limnobius and Aulodrilus sp.) and two of Chironomidae (Nanocladius sp. and Monodiamesa sp.) occurred in sites with high pH and little vegetation. The three Tubificidae species also preferred organic-rich sediments. Irrespective of aquatic vegetation, Sphaerium sp. (Bivalvia) and Monodiamesa sp. (Chironomidae) occurred in low-OMC sites, whereas Tanypus sp. (Chironomidae) preferred high-OMC sites. The number of macroinvertebrate taxa showed the highest correlation with the number of submerged plants, suggesting that macroinvertebrate species richness was related mostly to submerged plant species diversity in this lake. The quantity and species richness of submerged plants and OMC are thus important determinants of the community structure of macroinvertebrates inhabiting sediments in Lake Takkobu.     

Isolation and characterization of heavy metals resistant bacteria from Lagos Lagoon

A total of 228 bacteria with an ability to resist toxic heavy metals were isolated from 8 selected sites of the Lagos Lagoon. The bacteria isolated wereStaphylocaccus sp.,Bacillus sp.,Pseudomonas sp.,Streptococcus sp.,Moraxella sp.,Escherichia coli, Proteus sp.,Klebsiella sp. andSalmonella sp. The heavy metals to which resistance was recorded were mercury, lead, zinc, cobalt, copper and chromium. The lagoon sites from which the highest number of resistant bacteria were isolated were Marina and Ebute-Ero. The heavy metal to which most bacteria were resistant was cobalt, while the least was chromium. The significance of the result is discussed in relation to the Nigerian environment and human health.     

A geographical survey of littoral crustacea in Norway and their use in paleolimnology

Littoral Crustacea from 400 sites all over Norway were related to lake pH, conductivity, altitude and major biogeography. Being tolerant animals, littoral Crustacea do not fall into clear pH classes as do many Bacillariophyceae or Chrysophyceae. Littoral Crustacea were subdivided into 4 main pH classes: acidobiontic, acidophilous, circumneutral and indifferent, the last group containing most species. Species typical for acidic lakes in the region were: A. excisa, S. serricaudatus, A. curvirostris, A. nana, S. mucronata and D. brachyurum; whereas D. longispina, S. vetulus, A. intermedia and A. rectangula were more common in circumneutral waters. Many littoral Crustacea were shown to be related to altitude, which should be considered in studies on lake histories. Some species showed in addition a restricted geographical distribution. Conductivity, with values recorded in this study, played a minor role in distribution of taxa. More ecological studies are necessary to fully utilize the potential of cladoceran remains in understanding lake histories.     

Phylogenetic analysis of the archaeal community in an alkaline-saline soil of the former lake Texcoco (Mexico)

The soil of the former lake Texcoco is an extreme environment localized in the valley of Mexico City, Mexico. It is highly saline and alkaline, where Na⁺, Cl⁻, HCO₃⁻ and CO₃²⁻ are the predominant ions, with a pH ranging from 9.8 to 11.7 and electrolytic conductivities in saturation extracts from 22 to 150 dS m⁻¹. Metagenomic DNA from the archaeal community was extracted directly from soil and used as template to amplify 16S ribosomal gene by PCR. PCR products were used to construct gene libraries. The ribosomal library showed that the archaeal diversity included Natronococcus sp., Natronolimnobius sp., Natronobacterium sp., Natrinema sp., Natronomonas sp., Halovivax sp., “Halalkalicoccus jeotgali” and novel clades within the family of Halobacteriaceae. Four clones could not be classified. It was found that the archaeal diversity in an alkaline-saline soil of the former lake Texcoco, Mexico, was low, but showed yet uncharacterized and unclassified species. César Valenzuela-Encinas and Isabel Neria-González contributed equally to this publication.     

On the energetics of chemolithotrophy in nonequilibrium systems: case studies of geothermal springs in Yellowstone National Park

Chemolithotrophic micro‐organisms are important primary producers in high‐temperature geothermal environments and may catalyse a number of different energetically favourable redox reactions as a primary energy source. Analysis of geochemical constituents followed by chemical speciation and subsequent calculation of reaction free energies (ΔG_rxn) is a useful tool for evaluating the thermodynamic favourability and potential energy available for microbial metabolism. The primary goal of this study was to examine relationships among geochemical gradients and microbial population distribution, and to evaluate the utility of energetic approaches for predicting microbial metabolism from free‐energy calculations, utilizing as examples, several geothermal habitats in Yellowstone National Park where thorough geochemical and phylogenetic analyses have been performed. Acidic (pH ～ 3) and near‐neutral (pH ～ 6–7) geothermal springs were chosen for their range in geochemical properties. Aqueous and solid phase samples obtained from the source pools and the outflow channels of each spring were characterized for all major chemical constituents using laboratory and field methods to accurately measure the concentrations of predominant oxidized and reduced species. Reaction free energies (ΔG_rxn) for 33 oxidation–reduction reactions potentially important to chemolithotrophic micro‐organisms were calculated at relevant spring temperatures after calculating ion activities using an aqueous equilibrium model. Free‐energy values exhibit significant variation among sites for reactions with pH dependence. For example, free‐energy values for reactions involving Fe³⁺ are especially variable across sites due in large part to the pH dependence of Fe³⁺ activity, and exhibit changes of up to 40 kJ mol^?1 electron from acidic to near neutral geothermal springs. Many of the detected 16S rRNA gene sequences represent organisms whose metabolisms are consistent with exergonic processes. However, sensitivity analyses demonstrated that reaction free energies do not generally represent the steep gradients in local geochemical conditions resulting from air–water gas exchange and solid phase deposition that are important in defining microbial habitats and 16S rRNA gene sequence distribution within geothermal outflow channels.     

FATTY ACID AND LIPID COMPOSITION OF THE ACIDOPHILIC GREEN ALGA CHLAMYDOMONAS SP.1

The lipid and fatty acid compositions of Chlamydomonas sp. isolated from a volcanic acidic lake and C. reinhardtii were compared, and the effects of pH of the medium on lipid and fatty acid components of Chlamydomonas sp. were studied. The fatty acids in polar lipids from Chlamydomonas sp. were more saturated than those of C. reinhardtii. The relative percentage of triacylglycerol to the total lipid content in Chlamydomonas sp. grown in medium at pH 1 was higher than that in other cells grown at higher pH. A probable explanation might be that Chlamydomonas sp. has two low pH adaptation mechanisms. One mechanism is the saturation of fatty acids in membrane lipids to decrease membrane lipid fluidity, and the other is the accumulation of triacylglycerol, as a storage lipid, to prevent the osmotic imbalance caused by high concentrations of H₂SO₄.     

Purification,Characterization, and Molecular Cloning of Acidophilic Xylanase from Penicillium sp.40

Penicillum sp. 40, which can grow in an extremely acidic medium at pH 2.0 was screened from an acidic soil. This fungus produces xylanases when grown in a medium containing xylan as a sole carbon source. A major xylanase was purified from the culture supernatant of Penicillium sp. 40 and designated XynA. The molecular mass of XynA was estimated to be 25,000 by sodium dodecyl sulfate-polyacrylamide gel electrophoresis. XynA has an optimum pH at 2.0 and is stable in pH 2.0-5.0. Western blot analysis using anit-XynA antibody showed that XynA was induced by xylan and repressed by glucose. Also, its production was increased by an acidic medium. The gene encoding XynA (xynA) was isolated from the genomic library of Penicillium sp. 40. The structural part of xynA was found to be 721 bp. The nucleotide sequence of cDNA amplified by RT-PCR showed that the open reading frame of xynA was interrupted by a single intron which was 58 bp in size and encoded 221 amino acids. Direct N-terminal amino acid sequencing showed that the precursor of XynA had a signal peptide composed of 31 amino acids. The molecular mass caliculated from the deduced amino acid sequence of XynA is 20,713. This is lower than that estimated by gel electrophoresis, suggesting that XynA is a glycoprotein. The predicted amino acid sequence of XynA has strong similarity to other family11 xylanases from fungi.     

The taxonomic and ecological status of the environmentally restricted spongillid species of North America. IV. Spongilla heterosclerifera Smith 1918

The taxonomic status, present distribution and specific threats to the existence of the environmentally restricted freshwater sponge, Spongilla heterosclerifera Smith 1918 were investigated. This species, collected only from Oneida Lake, New York, has not colonized other habitats and continues to exhibit typical diagnostic characteristics, thus qualifying as a valid environmentally restricted species. Although the sponge presently colonizes two sites in the lake, both near the northwestern shore, the total absence of sponge fauna from other lake regions near more heavily populated areas of this species. Physicochemical data from Oneida Lake greatly extend the known environmental parameters of Spongilla heterosclerifera.     

Identification of acid-stress-tolerant proteins from promising cyanobacterial isolates

Cyanobacterial cultures were isolated from acidic (pH 4.9–6.2) rice grown soils in Tamil Nadu, India. The predominant genera were Anabaena (50%), Westiellopsis (17.5%), Nostoc (15%), Oscillatoria (5%) and others that were unicellulars (12.5%) viz., Microcystis, Calothrix and Phormidium. The levels of tolerance to acidity varied among these strains, which were tested and authenticated for their acid tolerance capacity under both in vitro and pot culture conditions. Westiellopsis sp. was found to predominate from pH 4.9 to pH 6.2, indicating its adaptability. Cultures tolerant to acidic conditions were characterized for growth, biomass production and biochemical constituents. Under acidic conditions, Westiellopsis sp. showed pronounced chlorophyll a content, phycobilin pigment content, ammonia excretion and nitrogenase activity compared to normal conditions. Molecular characterization, particularly isozyme and random amplified polymorphic DNA (RAPD) analysis, were also carried out. Three strains of Westielliopsis sp. strains were selected, of which two were able to grow at an acidity level of pH 4.0, while one strain was able to sustain growth at an acidity level of 5.0. These three cultures, along with acid susceptible strains of Westielliopsis sp. and Anabaena sp. PCC 7120 (standard check) were subjected to acid shock for different time intervals. Protein profiling of both the acid-tolerant and acid-susceptible strains was carried out with samples collected at different time intervals. Based on the presence/absence of protein bands in the tolerant/susceptible strains, some low- and medium-molecular weight proteins can be linked to conferring acid tolerance. Presented at the 6th Meeting of the Asian Pacific Society of Applied Phycology, Manila, Philippines.     

Isolation,Enumeration and Identification of Amebae from a Nebraska Lake*

A plaque technic was evaluated and used for the isolation and enumeration of small, free-living amebae in lake-bottom samples which were collected each month for one year from a Nebraska lake. Several culture media were evaluated, and a simple glucose-salts medium was chosen. The most frequent ameba in the lake-bottom samples was Acanthamoeba polyhaga which underwent marked increases and decreases in population densities during the collection period. This pattern was not correlated with water temperature, bacterial counts, and nitrate or phosphate levels. Other species of amebae of the genera Hartmannella, Vahlkampfia, Naegleria, Paratetramitus and Echinamoeba were isolated. Most of these were either found infrequently or remained at relatively low, constant densities throughout the year. In addition, 4 species of Acrasieae of the genera Dictyostelium and Polysphondylium were isolated from the lake-bottom samples.     

Iron and pH‐responsive FtrABCD ferrous iron utilization system of Bordetella species

A putative operon encoding an uncharacterized ferrous iron transport (FtrABCD) system was previously identified in cDNA microarray studies. In growth studies using buffered medium at pH values ranging from pH 6.0 to 7.6, Bordetella pertussis and Bordetella bronchiseptica FtrABCD system mutants showed dramatic reductions in growth yields under iron‐restricted conditions at pH 6.0, but had no growth defects at pH 7.6. Supplementation of culture medium with 2 mM ascorbate reductant was inhibitory to alcaligin siderophore‐dependent growth at pH 7.6, but had a neglible effect on FtrABCD system‐dependent iron assimilation at pH 6.0 consistent with its predicted specificity for ferrous iron. Unlike Bordetella siderophore‐dependent and haem iron transport systems, and in agreement with its hypothesized role in transport of inorganic iron from periplasm to cytoplasm, FtrABCD system function did not require the TonB energy transduction complex. Gene fusion analysis revealed that ftrABCD promoter activity was maximal under iron‐restricted growth conditions at acidic pH. The pH of human airway surface fluids ranges from pH 5.5 to 7.9, and the FtrABCD system may supply ferrous iron necessary for Bordetella growth in acidic host microenvironments in which siderophores are ineffective for iron retrieval.