scholarly journals Conspicuous Smooth and White Egg-Shaped Sulfur Structures on a Deep-Sea Hydrothermal Vent Formed by Sulfide-Oxidizing Bacteria

Author(s):  
Marit R. van Erk ◽  
Viola Krukenberg ◽  
Pia Bomholt Jensen ◽  
Sten Littmann ◽  
Dirk de Beer

At the deep-sea Guaymas Basin hydrothermal vent system, sulfide-rich hydrothermal fluids mix with oxygenated seawater, thereby providing a habitat for microbial sulfur oxidation. Microbial sulfur oxidation in the deep sea involves a variety of organisms and processes and can result in the excretion of elemental sulfur.

2006 ◽  
Vol 56 (8) ◽  
pp. 1725-1733 ◽  
Author(s):  
Ken Takai ◽  
Masae Suzuki ◽  
Satoshi Nakagawa ◽  
Masayuki Miyazaki ◽  
Yohey Suzuki ◽  
...  

A novel mesophilic bacterium, strain GO25T, was isolated from a nest of hydrothermal vent polychaetes, Paralvinella sp., at the Iheya North field in the Mid-Okinawa Trough. Cells were motile short rods with a single polar flagellum. Growth was observed between 4 and 35 °C (optimum 30 °C; 13–16 h doubling time) and between pH 5.4 and 8.6 (optimum pH 6.1). The isolate was a facultatively anaerobic chemolithoautotroph capable of growth using molecular hydrogen, elemental sulfur or thiosulfate as the sole energy source, carbon dioxide as the sole carbon source, ammonium or nitrate as the sole nitrogen source and elemental sulfur, thiosulfate or yeast extract as the sole sulfur source. Strain GO25T represents the first deep-sea epsilonproteobacterium capable of growth by both hydrogen and sulfur oxidation. Nitrate or molecular oxygen (up to 10 % partial pressure) could serve as the sole electron acceptor to support growth. Metabolic products of nitrate reduction shifted in response to the electron donor provided. The G+C content of genomic DNA was 37.6 mol%. Phylogenetic analysis based on 16S rRNA gene sequences indicated that the novel isolate belonged to the genus Sulfurimonas and was most closely related to Sulfurimonas autotrophica OK10T (96.3 % sequence similarity). DNA–DNA hybridization demonstrated that the novel isolate could be differentiated genotypically from Sulfurimonas autotrophica OK10T. On the basis of the physiological and molecular properties of the novel isolate, the name Sulfurimonas paralvinellae sp. nov. is proposed, with strain GO25T (=JCM 13212T=DSM 17229T) as the type strain. Thiomicrospira denitrificans DSM 1251T (=ATCC 33889T) is phylogenetically associated with Sulfurimonas autotrophica OK10T and Sulfurimonas paralvinellae GO25T. Based on the phylogenetic relationship between Thiomicrospira denitrificans DSM 1251T, Sulfurimonas autotrophica OK10T and Sulfurimonas paralvinellae GO25T, we propose the reclassification of Thiomicrospira denitrificans as Sulfurimonas denitrificans comb. nov. (type strain DSM 1251T=ATCC 33889T). In addition, an emended description of the genus Sulfurimonas is proposed.


Author(s):  
Shasha Wang ◽  
Lijing Jiang ◽  
Qitao Hu ◽  
Xuewen Liu ◽  
Suping Yang ◽  
...  

2013 ◽  
Vol 63 (Pt_6) ◽  
pp. 1967-1971 ◽  
Author(s):  
A. I. Slobodkin ◽  
A.-L. Reysenbach ◽  
G. B. Slobodkina ◽  
T. V. Kolganova ◽  
N. A. Kostrikina ◽  
...  

A thermophilic, anaerobic, chemolithoautotrophic bacterium (strain S69T) was isolated from a deep-sea hydrothermal vent chimney located on the Eastern Lau Spreading Center and Valu Fa Ridge, Pacific Ocean, at a depth of 1910 m using anoxic medium with elemental sulfur as the only energy source. Cells of strain S69T were Gram-negative short rods, 0.4–0.6 µm in diameter and 1.0–2.5 µm in length, motile with a single polar flagellum. The temperature range for growth was 28–70 °C, with an optimum at 61 °C. The pH range for growth was 5.6–7.9, with optimum growth at pH 6.8. Growth of strain S69T was observed at NaCl concentrations ranging from 0.9 to 5.0 %, with an optimum at 1.8–2.7 (w/v). Strain S69T grew anaerobically with elemental sulfur as an energy source and bicarbonate/CO2 as a carbon source. Elemental sulfur was disproportionated to sulfide and sulfate. Growth was enhanced in the presence of poorly crystalline Fe(III) oxide (ferrihydrite) as a sulfide-scavenging agent. Strain S69T was also able to grow by disproportionation of thiosulfate and sulfite. Sulfate was not used as an electron acceptor either with H2 or with organic electron donors. Analysis of the 16S rRNA gene sequence revealed that the isolate formed a distinct phylogenetic branch within the Deltaproteobacteria . On the basis of its physiological properties and results of phylogenetic analyses, strain S69T is considered to represent a novel species of a new genus, for which the name Dissulfuribacter thermophilus gen. nov., sp. nov. is proposed. The type strain of Dissulfuribacter thermophilus is S69T ( = DSM 25762T = VKM B-2760T).


2018 ◽  
Author(s):  
Sonja Geilert ◽  
Christian Hensen ◽  
Mark Schmidt ◽  
Volker Liebetrau ◽  
Florian Scholz ◽  
...  

Abstract. The Guaymas Basin in the Gulf of California is an ideal site to test the hypothesis that magmatic intrusions into organic-rich sediments can cause the release of large amounts of thermogenic methane and CO2 that may lead to climate warming. In this study pore fluids close (~ 500 m) to a hydrothermal vent field and at cold seeps up to 20 km away from the northern rift axis were studied to determine the influence of magmatic intrusions on pore fluid composition and gas migration. Pore fluids close to the hydrothermal vent area show predominantly seawater composition, indicating a shallow circulation system transporting seawater to the hydrothermal catchment area rather than being influenced by hydrothermal fluids themselves. Only in the deeper part of the sediment core, composed of hydrothermal vent debris, Sr isotopes indicate a mixture with hydrothermal fluids of ~ 3 %. Also cold seep pore fluids show mainly seawater composition. Most of the methane is of microbial origin and consumed by anaerobic oxidation in shallow sediments, whereas ethane has a clear thermogenic signature. Fluid and gas flow might have been active during sill emplacement in the Guaymas Basin, but ceased 28 to 7 thousand years ago, based on sediment thickness above extinct conduits. Our results indicate that carbon release depends on the longevity of sill-induced, hydrothermal systems which is a currently unconstrained factor.


Sign in / Sign up

Export Citation Format

Share Document