Xinke Yu

Diversity and Community Structure of Archaea in Deep Subsurface Sediments from the Tropical Western Pacific

Archaeal 16S rRNA gene clone libraries using PCR amplicons from eight different layers of the MD06-3051 core were obtained from the tropical Western Pacific sediments. A total of 768 clones were randomly selected, and 264 representative clones were sequenced by restriction fragment length polymorphism. Finally, 719 valid clones and 104 operational taxonomic units were identified after chimera-check and ≥97% similarity analysis. The phylogenetic analysis of 16S rDNA sequences obtained from sediment samples were very diverse and showed stratification with depth. Majority of the members were most closely related to uncultivated groups and physiologically uncharacterized assemblages. All phylotypes were affiliated with Crenarchaeota (76%) and Euryarchaeota (24%), respectively. Deep-sea archaeal group (DSAG, 41% of total clones) and miscellaneous crenarchaeotic group (MCG, 29% of total clones) belonging to Crenarchaeota were the most predominant archaeal 16S rDNA phylotypes in clone libraries. Phylotypes in this study shared high similarity with those in subsurface sediments from Peru Margin sites, which indicated that different geographical zones might host similar members of archaeal populations based on similar sedimentary environments. In our study, members of DSAG and MCG seemed to dominate certain layers of the nonhydrate sediments, suggesting a wide ecophysiological adaptation than previously appreciated. The spatial distribution and community structure of these groups might vary with the different geochemical gradients of the environment.

Paleoenvironmental Changes in the Northern Okinawa Trough since 25 ka BP: REE and Organic Carbon Evidence

Paleoenvironmental changes in the northern Okinawa trough covering the last 25 ka were synthetically reconstructed using REE and organic carbon indices of core CSH1. Variations of these parameters revealed three distinct intervals of major sediment provenance changes that can be related to sea-level fluctuation and Tsushima Warm Current evolution. Interval 1 (16–24.7 ka BP) is characterized by dominantly fluvial discharge from the Changjiang (Yangtze River) and Huanghe (Yellow River) as well as high primary productivity. In Interval 2 (7.3–16 ka BP), the Changjiang and Huanghe mouths regressed with sea-level rising. The newly formed Tsushima Warm Current could carry some sediment loads of Taiwan to the study core, especially during its late phase (7.3–8.2 ka BP). Modern oceanographic conditions were finally established since the beginning of Interval 3, leading to more terrigenous contribution from Taiwan, whereas low sea-surface productivity in the study area.

Prauserella shujinwangii sp. nov., from a desert environment.

A Gram-positive, spore-forming, rod-shaped actinomycete, designated XJ46(T), was isolated from Xinjiang Uyghur Autonomous Region, China and subjected to a polyphasic taxonomic analysis. Morphological and chemotaxonomic characteristics of XJ46(T) were identified as being similar to those of members of the genus Prauserella. The phylogenetic tree based on 16S rRNA gene sequences showed that XJ46(T) shared the highest similarity (95.9%) with Prauserella marina MS498(T). Based on its phenotypic characteristics, chemotaxonomic analysis and 16S rRNA gene sequence analysis, strain XJ46(T) is proposed to represent a novel species of the genus Prauserella, named Prauserella shujinwangii sp. nov. The type strain is XJ46(T) ( =CGMCC 4.7125(T) =JCM 19736(T)).

Autotrophic potential in mesophilic heterotrophic bacterial isolates from Sino-Pacific marine sediments

Microbial carbon fixation is a paramount process in the ocean especially below the photic zone both in water and sedimentary ecosystems. Autotrophic microbes that fix carbon dioxide are renowned. However, the question whether heterotrophs can also fix carbon is intriguing. Ten heterotrophically grown, identified bacterial isolates from the Sino-Pacific marine sediments were tested for autotrophic uptake potential with and without addition of electron donors. Nine of the ten isolates showed carbon uptake capacity without addition of any substrate at very low rates in the order of 10–8 to 10–4 fmol/(cell·h). The addition of manganese and ammonium at 1 mmol/L final concentration enhanced the uptake potential. Addition of 1 mmol/L final concentrations of reduced iron (10–6 to 10–5 fmol/(cell·h) and sulfide (10–5 fmol/(cell·h) decreased the uptake potential significantly at p<0.1. Bacterial tolerance to formaldehyde suggested propensities of anaplerotic chemical reactions that form metabolic intermediates of C-1 metabolism pathways. The isolates displayed high metabolic flexibility. With the changes in electron donors, the isolates metabolically toggled between relatively anoxic reductive iron/sulfur cycles and the oxidative cycles of manganese/ammonium and vice-versa. This property makes these microbes successful survivors in the highly dynamic Sino-Pacific sediments.

Chengkuizengella sediminis gen. nov. sp. nov., isolated from sediment

A Gram-stain-positive, aerobic, motile, endospore-forming bacterium, designated strain J15A17T, was isolated from sediment of the South China Sea. The strain was oxidase-positive and catalase-negative. Optimal growth occurred at 33 °C, pH 7.5 and in the presence of 3 % (w/v) NaCl. On the basis of 16S rRNA gene sequence analysis, the strain showed closest similarity (92.8 %) to Paenibacillus puldeungensis strain CAU 9324T. Phylogenetic analysis based on 16S rRNA gene sequences showed that the isolate forms a separate branch within the family Paenibacillaceae, with the genus Cohnella as the most closely related genus. The DNA G+C content of strain J15A17T was 37.4 mol%. The strain contained MK-7 as the sole respiratory quinone; anteiso-C15 : 0 and iso-C16 : 0 were the major cellular fatty acids; and its polar lipid pattern consisted of diphosphatidylglycerol, phosphatidylglycerol, phosphatidylethanolamine, glycolipid and four unidentified phospholipids. The strain displayed the peptidoglycan type A4α l-Lys-d-Asp in the cell wall. Phylogenetic, physiological, biochemical and morphological differences between strain J15A17T and its closest relatives in the genera Cohnella, Fontibacillus and Paenibacillus suggest that strain J15A17T (=KCTC 33759T=MCCC 1H00137T) represents the type strain of a novel species in a new genus within the family Paenibacillaceae, Chengkuizengella sediminis gen. nov. sp. nov.

Corrigendum: Paraliobacillus sediminis sp. nov., isolated from East China sea sediment

The fourth author Anindita Das has three affiliations but only two were listed. Their full affiliation list is: Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, PR China MACS-Agharkar Research Institute, G.G. Agarkar Road, Pune 411004, Maharashtra, India (Present affiliation) Council of Scientific and Industrial Research (CSIR), National Institute of Oceanography, Dona Paula, Panaji 403004, India.

Paraliobacillus sediminis sp. nov., isolated from sediment in East China Sea.

A Gram-strain-positive, facultatively anaerobic, motile, endospore-forming, slightly halophilic bacterium, designated strain 126C4T, was isolated from sediment from the East China Sea. The strain was catalase-positive and oxidase-negative. Optimal growth occurred at 28-30 °C, pH 7.0-7.5 and in the presence of 3-5 % (w/v) NaCl. Phylogenetic analyses, based on 16S rRNA gene sequence comparisons, showed that strain 126C4T was a member of the genus Paraliobacillus, with 16S rRNA gene sequence similarities to Paraliobacillus quinghaiensis YIM-C158T and Paraliobacillus ryukyuensis O15-7T of 96.2 % and 95.3 %, repectively. The DNA G+C content was 39.6 mol%. The strain contained MK-7 as the sole respiratory quinone, anteiso-C15 : 0, C16 : 0, iso-C15 : 0 and iso-C16 : 0 as the major cellular fatty acids, and its polar lipid pattern comprised diphosphatidylglycerol, phosphatidylethanolamine, three glycolipids and four unknown phospholipids. On the basis of its phylogenetic position, phenotypic traits and chemotaxonomic characteristics, it is suggested that strain 126C4T represents a novel species of the genus Paraliobacillus, for which the name Paraliobacillus sediminis sp. nov. is proposed. The type strain is 126C4T (=KCTC 33762T=MCCC 1H00136T).