scholarly journals Thalassobaculum fulvum sp. nov., isolated from deep seawater

2016 ◽  
Vol 66 (6) ◽  
pp. 2186-2191 ◽  
Author(s):  
Yue Su ◽  
Ruijun Wang ◽  
Cong Sun ◽  
Shuaibo Han ◽  
Jing Hu ◽  
...  
Keyword(s):  
Deep Seawater

scholarly journals Post-magmatic fracturing, fluid flow, and vein mineralization in supra-subduction zones: a comparative study on vein calcites from the Troodos ophiolite and the Izu–Bonin forearc and rear arc

2021 ◽  
Vol 110 (2) ◽  
pp. 627-649
Author(s):  
Dennis Quandt ◽  
W. Kurz ◽  
P. Micheuz
Keyword(s):  
Fluid Flow ◽  
Subduction Zones ◽  
Growth Dynamics ◽  
Pillow Lava ◽  
Published Data ◽  
Fracturing Fluid ◽  
Deep Seawater ◽  
Vein Formation ◽  
Mineralization Processes ◽  
Extensional Faulting

AbstractBased on the published data of pillow lava-hosted mineralized veins, this study compares post-magmatic fracturing, fluid flow, and secondary mineralization processes in the Troodos and Izu–Bonin supra-subduction zone (SSZ) and discusses the crucial factors for the development of distinct vein types. Thin section and cathodoluminescence petrography, Raman spectroscopy, fluid inclusion microthermometry, and trace element and isotope (87Sr/86Sr, δ18O, δ13C, Δ47) geochemistry indicate that most veins consist of calcite that precipitated from pristine to slightly modified seawater at temperatures < 50 °C. In response to the mode of fracturing, fluid supply, and mineral growth dynamics, calcites developed distinct blocky (precipitation into fluid-filled fractures), syntaxial (crack and sealing), and antitaxial (diffusion-fed displacive growth) vein microtextures with vein type-specific geochemical signatures. Blocky veins predominate in all study areas, whereas syntaxial veins represent subordinate structures. Antitaxial veins occur in all study areas but are particularly abundant in the Izu–Bonin rear arc where the local geological setting was conducive of antitaxial veining. The temporal framework of major calcite veining coincides with the onset of extensional faulting in the respective areas and points to a tectonic control on veining. Thus, major calcite veining in the Troodos SSZ began contemporaneously with volcanic activity and extensional faulting and completed within ~ 10–20 Myr. This enabled deep seawater downflow and hydrothermal fluid upflow. In the Izu–Bonin forearc, reliable ages of vein calcites point to vein formation > 15 Myr after subduction initiation. Therefore, high-T mineralization (calcite, quartz, analcime) up to 230 °C is restricted to the Troodos SSZ.

scholarly journals Wave Height Distributions and Rogue Waves in the Eastern Mediterranean

2021 ◽  
Vol 9 (6) ◽  
pp. 660
Author(s):  
Sagi Knobler ◽  
Daniel Bar ◽  
Rotem Cohen ◽  
Dan Liberzon
Keyword(s):  
Wave Height ◽  
Eastern Mediterranean ◽  
Rogue Waves ◽  
Distribution Model ◽  
Storm Events ◽  
Order Model ◽  
Deep Seawater ◽  
Wave Heights ◽  
Storm Characteristics ◽  
Buoy Data

There is a lack of scientific knowledge about the physical sea characteristics of the eastern part of the Mediterranean Sea. The current work offers a comprehensive view of wave fields in southern Israel waters covering a period between January 2017 and June 2018. The analyzed data were collected by a meteorological buoy providing wind and waves parameters. As expected for this area, the strongest storm events occurred throughout October–April. In this paper, we analyze the buoy data following two main objectives—identifying the most appropriate statistical distribution model and examining wave data in search of rogue wave presence. The objectives were accomplished by comparing a number of models suitable for deep seawater waves. The Tayfun—Fedele 3rd order model showed the best agreement with the tail of the empirical wave heights distribution. Examination of different statistical thresholds for the identification of rogue waves resulted in the detection of 99 unique waves, all of relatively low height, except for one wave that reached 12.2 m in height which was detected during a powerful January 2018 storm. Characteristics of the detected rogue waves were examined, revealing the majority of them presenting crest to trough symmetry. This finding calls for a reevaluation of the crest amplitude being equal to or above 1.25 the significant wave height threshold which assumes rogue waves carry most of their energy in the crest.

Complete genome sequence of Alcanivorax xenomutans P40, an alkane-degrading bacterium isolated from deep seawater

2018 ◽  
Vol 38 ◽  
pp. 1-4 ◽  
Author(s):  
Xiaoteng Fu ◽  
Qiliang Lai ◽  
Chunming Dong ◽  
Wanpeng Wang ◽  
Zongze Shao
Keyword(s):  
Genome Sequence ◽  
Complete Genome Sequence ◽  
Complete Genome ◽  
Deep Seawater ◽  
Degrading Bacterium

scholarly journals Research computer numerical simulation on heat dissipation model of submarine data centre based on TOPSIS model

2021 ◽  
Vol 2083 (4) ◽  
pp. 042062
Author(s):  
Rui Qin ◽  
Man Zhang ◽  
Lijie Chen ◽  
Xiao Liu ◽  
Zhengtao Lei ◽  
...  
Keyword(s):  
Data Centers ◽  
Heat Dissipation ◽  
Comprehensive Evaluation ◽  
Evaluation Model ◽  
Model Material ◽  
Physical Parameters ◽  
Deep Seawater ◽  
Dissipation Model ◽  
Computer Numerical Simulation ◽  
Optimal Evaluation

Abstract Due to the huge energy consumption of land-based data centers, it is necessary to establish undersea data centers as soon as possible in order to alleviate the problem of resource tension. In this paper, the uniformity of containers is assumed. Through force analysis, it is found that the stress of containers is uniformly distributed, so only the external stress should be considered. Hypothesis submarine data center in the 50 m deep seawater, calculate the container need to withstand stress is 76.417403 Mpa, common material in engineering field, then physical parameters of material to deal with the dimensional and normalization, and establishes a comprehensive evaluation model material, the Topsis method is adopted to solve, to solve the optimal evaluation of the results can be divided into: 7-4 PH Stainless Stee 0.7450 points, so choose it as IU server container material.

scholarly journals Solimonas marina sp. nov., isolated from deep seawater of the Pacific Ocean

2021 ◽  
Vol 71 (1) ◽  
Author(s):  
Xiupian Liu ◽  
Qiliang Lai ◽  
Fengqin Sun ◽  
Yaping Du ◽  
Yingbao Gai ◽  
...  
Keyword(s):  
Pacific Ocean ◽  
Type Species ◽  
Sequence Similarity ◽  
Rrna Gene ◽  
Chromosomal Dna ◽  
Deep Seawater ◽  
Content Type ◽  
Link Type ◽  
The Pacific ◽  
The Pacific Ocean

A taxonomic study was carried out on strain C16B3T, which was isolated from deep seawater of the Pacific Ocean. The bacterium was Gram-stain-negative, oxidase- and catalase- positive and rod-shaped. Growth was observed at salinities of 0–8.0 % and at temperatures of 10–45 °C. Phylogenetic analysis based on 16S rRNA gene sequences indicated that strain C16B3T belonged to the genus Solimonas , with the highest sequence similarity to Solimonas terrae KIS83-12T (97.2 %), followed by Solimonas variicoloris MN28T (97.0 %) and the other four species of the genus Solimonas (94.5 –96.8 %). The average nucleotide identity and estimated DNA–DNA hybridization values between strain C16B3T and the type strains of the genus Solimonas were 74.05−79.48 % and 19.5–22.5 %, respectively. The principal fatty acids (>5 %) were summed feature 8 (C18 : 1  ω7c/C18 : 1  ω6c; 20.9 %), iso-C16 : 0 (14.6 %), C16 : 1  ω5c (9.4 %), iso-C12 : 0 (8.4 %), summed feature 2 (C14 : 0 3-OH/iso I-C16 : 1 and C12 : 0 aldehyde; 6.8 %) and C16 : 0 (5.5 %). The G+C content of the chromosomal DNA was 65.37 mol%. The respiratory quinone was determined to be Q-8 (100 %). The polar lipids were diphosphatidylglycerol, phosphatidylethanolamine, phosphatidylglycerol, four unidentified aminolipids, six unidentified phospholipids and one unidentified polar lipid. The combined genotypic and phenotypic data show that strain C16B3T represents a novel species within the genus Solimonas , for which the name Solimonas marina sp. nov. is proposed, with the type strain C16B3T (=MCCC 1A04678T=KCTC 52314T).

Continuous culture with deep seawater of a benthic food diatom Nitzschia sp.

1997 ◽  
pp. 245-249
Author(s):  
Kimio Fukami ◽  
Shinya Nishimura ◽  
Masamichi Ogusa ◽  
Miki Asada ◽  
Toshitaka Nishijima
Keyword(s):  
Continuous Culture ◽  
Deep Seawater ◽  
Benthic Food

Mesoproterozoic oxygenated deep seawater recorded by early diagenetic carbonate concretions from the Member IV of the Xiamaling Formation, North China

2020 ◽  
Vol 341 ◽  
pp. 105667 ◽  
Author(s):  
Anqi Liu ◽  
Dongjie Tang ◽  
Xiaoying Shi ◽  
Xiqiang Zhou ◽  
Limin Zhou ◽  
...  
Keyword(s):  
North China ◽  
Deep Seawater ◽  
Carbonate Concretions ◽  
Xiamaling Formation

Fabibacter pacificus sp. nov., a moderately halophilic bacterium isolated from seawater

2013 ◽  
Vol 63 (Pt_10) ◽  
pp. 3710-3714 ◽  
Author(s):  
Ying-Yi Huo ◽  
Lin Xu ◽  
Chun-Sheng Wang ◽  
Jun-Yi Yang ◽  
Hong You ◽  
...  
Keyword(s):  
Phylogenetic Trees ◽  
Sequence Similarity ◽  
Halophilic Bacterium ◽  
Rrna Gene ◽  
Deep Seawater ◽  
Phenotypic Data ◽  
Content Type ◽  
Moderately Halophilic ◽  
Link Type ◽  
Moderately Halophilic Bacterium

A Gram-stain-negative, aerobic, moderately halophilic bacterium, strain DY53T, was isolated from a deep-seawater sample collected from the eastern Pacific Ocean. This isolate grew in the presence of 0.5–10.0 % (w/v) NaCl, at pH 6.5–8.5 and at 15–40 °C. The optimum NaCl concentration for growth of DY53T was 2 % (w/v) at 35 °C. Chemotaxonomic analysis showed MK-7 as the predominant menaquinone and iso-C15 : 0, summed feature 3 (iso-C15 : 0 2-OH and/or C16 : 1ω7c), iso-C15 : 1 G, iso-C15 : 0 3-OH and iso-C17 : 0 3-OH as major cellular fatty acids. The genomic DNA G+C content was 40.8 mol%. Phylogenetic trees based on 16S rRNA gene sequences revealed that Fabibacter halotolerans UST030701-097T was the closest neighbour, with 96.7 % sequence similarity. Based on phylogenetic, chemotaxonomic and phenotypic data, we propose that strain DY53T represents a novel species of the genus Fabibacter , for which the name Fabibacter pacificus sp. nov. is proposed. The type strain is DY53T( = CGMCC 1.12402T = JCM 18885T).

Sign in / Sign up

Export Citation Format

Share Document