Phylogenetic diversity of culturable bacteria in surface seawater from the Drake Passage,Antarctica

The Drake Passage is located between the Antarctic Peninsula and Tierra del Fuego in the south of South America.Surface seawater samples were collected at seven sites in the Drake Passage during the austral summer of 2012.The 16 S rRNA sequences were analyzed from 187 isolated bacterial strains.Three phyla,29 genera and 56 species were identified.The three phyla were Actinobacteria,Firmicutes and Proteobacteria;the Proteobacteria included a-Proteobacteria,P-Proteobacteria and y-Proteobacteria.y-Proteobacteria,Actinobacteria and Firmicutes were the dominant class or phyla in terms of quantity and species.Gram-positive bacteria(Actinobacteria and Firmicutes) accounted for 57.8% of all types identified.There were nine dominant genera,including Curtobacterium,Staphylococcus,and Halomonas,and 14 dominant species including Curtobacterium flaccumfaciens,Curtobacterium pusillum,and Staphylococcus sciuri.Of the strains identified,87.2% were catalase positive or weakly positive.

Spatial variability ofδ^(18)O andδ^(2)H in North Pacific and Arctic Oceans surface seawater

This study presents new observations of stable isotopic composition(δ^(18)O,δ^(2)H and deuterium excess)in surface waters of the North Pacific and Arctic Oceans that were collected during the sixth Chinese National Arctic Research Expedition(CHINARE)from mid-summer to early autumn 2014.Seawaterδ^(18)O andδ^(2)H decrease with increasing latitudes from 39°N to 75°N,likely a result of spatial variability in evaporation/precipitation processes.This explanation is further confirmed by comparing theδ^(18)O-δ^(2)H relationship of seawater with that of precipitation.However,effects of freshwater inputs on seawater stable isotopic composition are also identified at 30°N-39°N.Furthermore,we find a non-significant relationship between the isotopic parameters(δ^(2)H andδ^(18)О)and salinity from 73°N northwards in the Arctic Ocean,implying that sea ice melting/formation may have some effect.These results suggest that the isotopic parametersδ^(2)H andδ^(18)Оare useful for tracing marine hydrological processes.

Study on the surface of hydrous titanium oxide adsorbent for extracting uranium from seawater-Ⅱ. The surface of HTO

This is second paper summarizing the study on the hydrous titanium oxide absorbent for extracting uranium fromseawater. The investigation is performed by means of X- ray photoelectronic energy spectroscopy for chemical analysis ( ESC A ) , determination of surface hydroxy radical, Fourier-transfer infrared spectrophotometry (FT-IR ) , electron paramagnetic resonance (EPR), inductively coupled Plasma torch (ICP), etc. The emphasis is laid upon the exploration of HTO surface and a discussion about the adsorption micromechanism.

Review of Global Ocean Intermediate Water Masses: 1.Part A, the Neutral Density Surface (the ‘McDougall Surface’) as a Study Frame for Water-Mass Analysis

This review article commences with a comprehensive historical review of the evolution and application of various density surfaces in atmospheric and oceanic studies. The background provides a basis for the birth of the neutral density idea. Attention is paid to the development of the neutral density surface concept from the nonlinearity of the equation of state of seawater. The definition and properties of neutral density surface are described in detail as developed from the equations of state of seawater and the buoyancy frequency when the squared buoyancy frequency N2 is zero, a neutral state of stability. In order to apply the neutral density surface to intermediate water-mass analysis, this review also describes in detail its practical oceanographic application. The mapping technique is focused for the first time on applying regularly gridded data in this review. It is reviewed how a backbone and ribs framework was designed to flesh out from a reference cast and first mapped the global neutral surfaces in the world’s oceans. Several mapped neutral density surfaces are presented as examples for each world ocean. The water-mass property is analyzed in each ocean at mid-depth. The characteristics of neutral density surfaces are compared with those of potential density surfaces.