Hemoglobin from a deep-sea hydrothermal-vent copepod

Deep-sea hydrothermal-vent fauna live in a highly variable environment where oxygen levels can be very low, and carbon dioxide and sulfide can reach high concentrations (1). These conditions are harsh for most aerobic metazoans, yet copepods can be abundant at hydrothermal vents. Here we report the structure and functional properties of hemoglobin extracted from the copepod Benthoxynus spiculifer, which was found in large numbers in a paralvinellid/gastropod community collection made during a cruise to the Juan de Fuca Ridge in 1998. Although hemoglobin has been reported in some littoral copepods (2), this is the first study of the structure and functional properties of copepod hemoglobin. Hemoglobin represents about 60% of the total soluble proteins extracted from B. spiculifer, and although it imparts a red color to the copepod, it does not provide a significant storage pool of oxygen. It is a 208-kDa protein, composed of 14 globin chains--7 of 14.3 kDa and 7 of 15.2 kDa. The hemoglobin has a very high and temperature-sensitive oxygen affinity, with no cooperativity or Bohr effect. These properties are adaptive for an animal living in a low-oxygen environment in which the primary function of the hemoglobin is most likely oxygen acquisition to support aerobic respiration.     

Chemical characterisation of eggs from deep-sea sharks

The chemical characterisation and nutritional value of eggs from the five deep-sea sharks leafscale gulper shark (Centrophorus squamosus), greater lantern shark (Etmopterus princeps), longnose velvet dogfish (Centroscymnus crepidater), Portuguese dogfish (Centroscymnus coelolepis) and black dogfish (Centrocyllium fabricii) captured at Hatton Bank in the North Atlantic were examined. The chemical composition was quite similar for all the eggs studied. The dominant fatty acid in all the eggs was the monounsaturated fatty acid C18:1, which varied from 27-39%. The eggs had a relatively high content of C16:0 (13.0-18.5%) and C22:6n-3 (10.3-15.1%). The two main lipid classes in the eggs were triacylglycerols (36-55%) and phospholipids (34-41%). The eggs had high amounts of vitamin A and E. The shark eggs were particularly rich in the amino acids aspartic acid, glutamic acid, leucine and arginine.     

Novel bacterial exopolysaccharides from deep-sea hydrothermal vents

Five bacterial strains recovered from deep-sea hydrothermal vents were studied for their ability to secrete extracellular polymers. A preliminary characterization displayed four different polysaccharides in terms of both chemical composition and rheological properties. One of them was secreted by Alteromonas macleodii subsp. fijiensis and exhibited similarities with xanthan, a commercial polysaccharide. Two of the three Pseudoalteromonas species were shown to produce the same polymer. The last polymer was secreted by a bacterium belonging to the Vibrio genus. They all contained glucose, galactose, mannose, glucuronic and galacturonic acids as the main sugars with the exception of the last one which was only constituted by uronic acids and hexosamines, in that similar to the structure of heparin, a glycosaminoglycan useful in pharmaceutical area. Applications for these polysaccharides could be expected in various biotechnological fields including the food industry, the wastewater treatment and pharmaceutical areas.     

Copepoda from deep-sea hydrothermal vents and cold seeps

Recent explorations of hydrothermal vents in the eastern Pacific (Juan de Fuca spreading zone, Guaymas Basin in the Gulf of California, East Pacific Rise at 21° N and 13° N, and Galapagos Rift) and on the Mid-Atlantic Ridge have revealed many copepods, mostly siphonostomatoids with few poecilostomatoids. In these habitats in depths from 1 808 to 3 650 m water temperatures may reach nearly 15 ° C. Among more than 22 000 copepods from vents examined two new families, 11 new genera, and 32 new species were represented.In addition, two new copepods were found in 3 260 m at cold seeps at the base of the West Florida Escarpment in the Gulf of Mexico, an environment not thermally active, with water temperatures about 4.39 °C.Some of these copepods were associated with host invertebrates such as a Nuculana-like protobranch bivalve, a polychaete, and two species of shrimps. Others were obtained from washings of bivalves or vestimentiferans or by means of corers or slurp guns.     

Bacterial diversity in deep-sea sediments from different depths

Seven sediment samples have been examined, taken from different depths of the deep-sea in the range of 1159m to 6482m. A total of 75 different 16S rDNA sequences (149 clones) analyzed clustered into the Proteobacteria, Gram-positive bacteria, Cytophaga, Planctomyces, and Actinomycetes and many sequences were from microorganisms that showed no phylogenetic affiliation with known bacteria. Clones identical to 16S rDNA sequences of members of the genus Pseudomonas were observed in all of the sediments examined. The second group of common sequences cloned from six sediment samples was related to the 16S rDNA sequence of a chemoautotrophic bacterium, the Solemya velum symbiont. Five 16S rDNA sequences from three sediments were related to those of the Alvinella pompejana epibiont which is a member of the -Proteobacteria. Only one sequence was obtained that was closely related to the 16S rDNA of the barophilic bacterium, Shewanella benthica, which might be a minor population in the deeper sediments. -Proteobacteria-related sequences were cloned from sediments obtained from sites near man-made garbage deposits and a Calyptogena community. These environments obviously would be richer in nutrients than other sites, and might be expected to show more types of bacteria than other deep-sea sediments. A large number of cloned sequences in this study showed very low identity to known sequences. These sequences may represent communities of as-yet-uncultivated microorganisms in the sediments.     

Characteristics of pullulanases from extremely thermophilic archaea isolated from deep-sea hydrothermal vents

Two out of three extremely thermophilic anaerobic archaea, isolated from deep-sea hydrothermal vents, produced pullulanase activity in the presence of maltose in the growth medium. Enzyme activities were mainly extracellular and characterized by optimum temperatures of 95°C and 80–95°C, optimum pH of 5.0–7.0 and a high degree of thermostability. One strain when grown in a fermenter with maltose as inducer produced pullulanase at 35 U/l. © Rapid Science Ltd. 1998     

Molecular analysis of the nitrogen cycle in deep-sea microorganisms from the Nankai Trough: genes for nitrification and denitrification from deep-sea environmental DNA

Nitrification and denitrification are bacterial functions, which are important for the global nitrogen cycle. Thus, it is important to study the diversity and distribution of bacteria in the environment, which are involved in the nitrogen cycle on the earth. Ammonia monooxygenase encoded by the amoA gene and nitrite reductase encoded by nirK or nirS are essential enzymes for nitrificaton and denitrification, respectively. These genes can be used as markers for the identification of organisms in the nitrogen cycle. In this study, we identified amoA (42 clones) and nirS (98 clones) genes in parallel from samples recovered from the deep-sea of the Nankai Trough. Genes for nirK could not be amplified from these samples. The obtained amoA sequences were not so closely related to those of amoA genes from previously isolated environmental organisms and those of genes from environmental DNAs. On the other hand, the nirS genes sequenced showed some relationship to some extent with the latter genes. However, some of the newly sequenced genes formed clusters, which contained no previously identified genes on a phylogenetic tree. These are likely present in specific denitrifiers from the deep-sea. The results of this study further suggest that nitrifiers and denitrifiers live in the same area of the Nankai Trough and the nitrogen cycle exists even in the deep-sea.     

Barophilic growth of bacteria from intestinal tracts of deep-sea invertebrates

Digestive tracts of abyssal scavenging amphipods and a deep-sea holothurian were examined for the presence of intestinal microflora capable of rapid proliferation under in situ pressures of 430 to 520 atmospheres (atm) and temperatures of 3–5°C. For two amphipod specimens, population doubling times of 5 and 6 hours were observed under in situ conditions, compared to 8 and 6 hours, respectively, at 1 atm. Growth enhancement under pressure was related inversely to initial population size and directly to concentration of available nutrient. In the case of the deposit-feeding holothurian, attached bacteria scraped from the intestinal lining showed a doubling time, under pressure, of 11 hours, compared to 36 hours for transient sediment bacteria that comprised the gut contents. These data suggest that deep-sea animals possess a commensal gut flora capable of responding to increased nutrient levels, via feeding of the host, without inhibition by the elevated hydrostatic pressures encountered in the deep ocean environment.     

Commonly stabilized cytochromes c from deep-sea Shewanella and Pseudomonas

Two cytochromes c₅ (SBcytc and SVcytc) have been derived from Shewanella living in the deep-sea, which is a high pressure environment, so it could be that these proteins are more stable at high pressure than at atmospheric pressure, 0.1 MPa. This study, however, revealed that SBcytc and SVcytc were more stable at 0.1 MPa than at higher pressure. In addition, at 0.1–150 MPa, the stability of SBcytc and SVcytc was higher than that of homologues from atmospheric-pressure Shewanella, which was due to hydrogen bond formation with the heme in the former two proteins. This study further revealed that cytochrome c₅₅₁ (PMcytc) of deep-sea Pseudomonas was more stable than a homologue of atmospheric-pressure Pseudomonas aeruginosa, and that specific hydrogen bond formation with the heme also occurred in the former. Although SBcytc and SVcytc, and PMcytc are phylogenetically very distant, these deep-sea cytochromes c are commonly stabilized through hydrogen bond formation.     

Larvae from deep-sea methane seeps disperse in surface waters

Many species endemic to deep-sea methane seeps have broad geographical distributions, suggesting that they produce larvae with at least episodic long-distance dispersal. Cold-seep communities on both sides of the Atlantic share species or species complexes, yet larval dispersal across the Atlantic is expected to take prohibitively long at adult depths. Here, we provide direct evidence that the long-lived larvae of two cold-seep molluscs migrate hundreds of metres above the ocean floor, allowing them to take advantage of faster surface currents that may facilitate long-distance dispersal. We collected larvae of the ubiquitous seep mussel “Bathymodiolus” childressi and an associated gastropod, Bathynerita naticoidea, using remote-control plankton nets towed in the euphotic zone of the Gulf of Mexico. The timing of collections suggested that the larvae might disperse in the water column for more than a year, where they feed and grow to more than triple their original sizes. Ontogenetic vertical migration during a long larval life suggests teleplanic dispersal, a plausible explanation for the amphi-Atlantic distribution of “B.” mauritanicus and the broad western Atlantic distribution of B. naticoidea. These are the first empirical data to demonstrate a biological mechanism that might explain the genetic similarities between eastern and western Atlantic seep fauna.     

Phylogenetic diversity of Gram-positive bacteria cultured from Antarctic deep-sea sponges

Gram-positive bacteria, specifically actinobacteria and members of the order Bacillales, are well-known producers of important secondary metabolites. Little is known about the diversity of Gram-positive bacteria associated with Antarctic deep-sea sponges. In this study, cultivation-based approaches were applied to investigate the Gram-positive bacteria associated with the Antarctic sponges Rossella nuda, Rossella racovitzae (Porifera: Hexactinellida), and Myxilla mollis, Homaxinella balfourensis, Radiella antarctica (Porifera: Demospongiae). In total, 46 Gram-positive strains were cultured. Phylogenetic analysis revealed that 24 strains were affiliated with the Actinobacteria, including six genera Streptomyces, Nocardiopsis, Pseudonocardia, Dietzia, Brachybacterium, and Brevibacterium. The other 22 strains were affiliated with the Firmicutes, and among them two (V17-1 and V179-1) only shared 92–95% 16S rRNA gene sequence identity with the nearest type strain. To our knowledge, this is the first report on the isolation of strains belonging to genera Dietzia and Brevibacterium from Antarctic sponges. All of the 46 strains were PCR screened for genes encoding polyketide synthases (PKS), and a selection of 36 isolates were used in subsequent bioassay analyses. Eighty-eight percentage of the isolates that possess a PKS gene were active against at least one test organism. The study confirms the existence of diverse bacteria in Antarctic sponges and their potential for producing active compounds.     

Diversity of Bacillus-like organisms isolated from deep-sea hypersaline anoxic sediments

Background

In spite of considerable efforts over past decades we still know relatively little regarding the biogeography of rotifers of inland waters in México. To help rectify this we undertook an extensive survey of the rotifer fauna of 48 water bodies in the Chihuahuan Desert of México.

Results

Of the sites surveyed, 21 had salinities ≥ 2000 μS cm^-1 and in these we found 57 species of monogonont rotifers and several bdelloids. Species richness in the saline sites varied widely, with a range in species richness of 1 to 27 and a mean (± 1SD) = 8.8 (± 6.2). Collectively all sites possess relatively high percent single- and doubletons, 33.3 and 21.7%, respectively. Simpson's Asymmetric Index indicated that similarity in rotifer species composition varied widely among a set of 10 sites. These were selected because they were sampled more frequently or represent unusual habitats. These SAI values ranged from 0.00 (complete dissimilarity) to 1.00 (complete similarity). The Jaccard Index varied between 0.00 and 0.35. This observation probably reflects similarities and differences in water chemistry among these sites. Inland saline systems differed in their chemical composition by region. Conductivity was related to hardness and alkalinity. In addition, hardness was positively associated with chloride and sulfate. RDA showed that several species were positively associated with chloride concentration. Other factors that were significantly associated with rotifer species included the presence of macrophytes, nitrate content, oxygen concentration, TDS, latitude and whether the habitat was a large lake or reservoir.

Conclusion

This study illustrates the diversity of the rotiferan fauna of inland saline systems and the uniqueness among waterbodies. Conservation of these systems is needed to preserve these unique sources of biodiversity that include rotifers and the other endemic species found in association with them.     

Bacterial diversity in deep-sea sediment from northeastern Pacific Ocean

16S rDNA sequencing method is one of the effectively used culture-independent techniques in recent years. In this study, 16S rDNA sequencing method was used to investigate the bacterial diversity in deep-sea sediment from northeastern Pacific polymetallic nodule province. Total DNAs were extracted by using 2 different methods (chemical method and DNA extracting kit method). After purification, genomic DNA was amplified by using 2 universal primers (27F and 1492R). Clones were selected and sequenced randomly. After the sequences were checked by using the Chimera Check Program of the RDP database, a bacterial 16S rRNA gene library of 79 clones was established. Phylogenetic analysis indicated that 79 clones could be divided into 11 phylotypes. Gamma Proteobacteria (22.8%) and alpha Proteobacteria (16.5%) were the dominant components of the sediment bacterial community, followed by Planctomycetacia (7.6%), delta Proteobacteria (6.3%), Nitrospira (6.3%), Actinobacteria (6.3%), beta Proteobacteria (5%), Acidobacteria (5.1%), Sphingobacteria (3.8%), Firmicutes (2.5%) and uncultured bacteria (17.7%). Gamma Proteobacteria also dominated at slices 0–2 cm and 4–6 cm. Different slices had different types of bacteria, alpha Proteobacteria, gamma Proteobacteria, delta Proteobacteria, Planctomycetacia, Nitrospira, Actinobacteria and Acidobacteria, however, appeared in all slices. Pseudomonas is common in many different deep-sea environments. In this study, it accounted for 22.2% of the total gamma Proteobacteria.     

Mercury adaptation among bacteria from a deep-sea hydrothermal vent

Since deep-sea hydrothermal vent fluids are enriched with toxic metals, it was hypothesized that (i) the biota in the vicinity of a vent is adapted to life in the presence of toxic metals and (ii) metal toxicity is modulated by the steep physical-chemical gradients that occur when anoxic, hot fluids are mixed with cold oxygenated seawater. We collected bacterial biomass at different distances from a diffuse flow vent at 9 degrees N on the East Pacific Rise and tested these hypotheses by examining the effect of mercuric mercury [Hg(II)] on vent bacteria. Four of six moderate thermophiles, most of which were vent isolates belonging to the genus Alcanivorax, and six of eight mesophiles from the vent plume were resistant to >10 microM Hg(II) and reduced it to elemental mercury [Hg(0)]. However, four psychrophiles that were isolated from a nearby inactive sulfide structure were Hg(II) sensitive. A neighbor-joining tree constructed from the deduced amino acids of a PCR-amplified fragment of merA, the gene encoding the mercuric reductase (MR), showed that sequences obtained from the vent moderate thermophiles formed a unique cluster (bootstrap value, 100) in the MR phylogenetic tree, which expanded the known diversity of this locus. The temperature optimum for Hg(II) reduction by resting cells and MR activity in crude cell extracts of a vent moderate thermophile corresponded to its optimal growth temperature, 45 degrees C. However, the optimal temperature for activity of the MR encoded by transposon Tn501 was found to be 55 to 65 degrees C, suggesting that, in spite of its original isolation from a mesophile, this MR is a thermophilic enzyme that may represent a relic of early evolution in high-temperature environments. Results showing that there is enrichment of Hg(II) resistance among vent bacteria suggest that these bacteria have an ecological role in mercury detoxification in the vent environment and, together with the thermophilicity of MR, point to geothermal environments as a likely niche for the evolution of bacterial mercury resistance.     

Thermostable amylolytic enzymes of thermophilic microorganisms from deep-sea hydrothermal vents

Microorganisms-grauling above 60 °C isolated from deep-sea hydrothermal vents were screened for amylolytic activity. Of the 269 strains tested, 70 were found to be positive. Nine archaea (including Thermococcus hydrothermalis AL662 and Thermococcus fumicolans ST557) and one thermophilic bacterium were selected for the determination of thermostability, and the temperature and pH optima of their amylolytic enzymes. Pullulanase, α-glucosidase and α-amylase activities were detected in four archaeal strains (including AL662 and ST557) related to the genus Thermococcus. The anaerobic hyperthermophilic archaeon, Thermococcus hydrothermalis was chosen for the further study of the α-glucosidase activity, and a preliminary characterization of this enzyme was carried out. The small number of highly thermostable α-glucosidases that has been described to date, combined with the very interesting properties of this enzyme, suggest a use for this enzyme in biotechnological processes.     

Late Holocene deep-sea benthic foraminifera from the Sea of Marmara

The benthic foraminiferal assemblages of two cores from the late-Holocene, organic-carbon-rich and carbonate-poor, deep-sea sediments of the eastern depression of the Sea of Marmara have been studied. They were deposited under high level of primary productivity and poorly oxygenated bottom-water conditions; they show low diversity and are dominated by a group of species adapted to an infaunal life style with wide bathymetric distribution (ca. 70–2000 m) in the Mediterranean Sea. Oxygen deficiency down to about 0.5 ml/l does not seem adversely to affect the rate of reproduction of the dominant species belonging to Melonis, Chilostomella, buliminids, and bolivinitids. Their distribution is primarily controlled by substrate conditions.Faunal similarities with fossil assemblages in association with some late-Quaternary sapropels and related facies from the eastern Mediterranean basins suggest that they were deposited under palaeo-oceanographic conditions closely similar to those of the modern Sea of Marmara.     

Characterization of a lysin from deep-sea thermophilic bacteriophage GVE2

Thermostable enzymes from thermophiles have attracted extensive studies. However, little is known about thermophilic lysin of bacteriophage obtained from deep-sea hydrothermal vent. In this study, a lysin from deep-sea thermophilic bacteriophage Geobacillus virus E2 (GVE2) was characterized for the first time. It was found that the GVE2 lysin was highly homologous with N-acetylmuramoyl-L-alanine amidases. After expression in Escherichia coli, the recombinant GVE2 lysin was purified. The recombinant lysin was active over a range of temperature from 40 °C to 80 °C, with an optimum at 60 °C. Its optimal pH was 6.0, and it was stable over a wide range of pH from 4.0 to 10.0. The lysin was highly active when some enzyme inhibitors or detergents (phenylmethylsulfonyl fluoride, Tween 20, Triton X-100, and chaps) were used. However, it was strongly inhibited by sodium dodecyl sulfate and ethylene diamine tetraacetic acid. Its enzymatic activity could be slightly stimulated in the presence of Na⁺ and Li⁺. But the metal ions Mg²⁺, Ba²⁺, Zn²⁺, Fe³⁺, Ca²⁺, and Mn²⁺ at concentrations of 1 or 10 mM showed inhibitions to the lysin activity. Our study demonstrated the first characterization of lysin from deep-sea thermophilic bacteriophage.