نتایج جستجو برای: deep seawater

تعداد نتایج: 223348  

Journal: :FEMS microbiology ecology 2003
Julie A Huber David A Butterfield John A Baross

Abstract The bacterial diversity in a diffuse flow hydrothermal vent habitat at Axial Volcano, Juan de Fuca Ridge was examined shortly after an eruptive event in 1998 and again in 1999 and 2000 using PCR-amplified 16S rRNA gene sequence analyses. While considerable overlap with deep-sea background seawater was found within the alpha- and gamma-proteobacteria, unique subseafloor phylotypes were ...

2015
Jesse R. Farmer Bärbel Hönisch Laura F. Robinson Tessa M. Hill

The ocean is currently absorbing excess carbon from anthropogenic emissions, leading to reduced seawater-pH (termed ‘ocean acidification’). Instrumental records of ocean acidification are unavailable from well-ventilated areas of the deep ocean, necessitating proxy records to improve spatio-temporal understanding on the rate and magnitude of deep ocean acidification. Here we investigate boron, ...

Journal: :Proceedings of the National Academy of Sciences of the United States of America 2016
Aron Stubbins

Biology and the environment interact, one shaping the other (1). In the oceans, the chemistry of seawater and the chemistry of life are intimately linked (2). In 1958, Alfred Redfield (3) noted that the microscopic plankton of the surface ocean contain carbon, nitrogen, and phosphorous atoms in a stoichiometry of ∼105:16:1 and that as these organisms sink and decay, the deep waters of the ocean...

2016
Georg Steinert Michael W. Taylor Peter Deines Rachel L. Simister Nicole J. de Voogd Michael Hoggard Peter J. Schupp

Sponges (phylum Porifera) are important members of almost all aquatic ecosystems, and are renowned for hosting often dense and diverse microbial communities. While the specificity of the sponge microbiota seems to be closely related to host phylogeny, the environmental factors that could shape differences within local sponge-specific communities remain less understood. On tropical coral reefs, ...

Journal: :Energies 2022

Ocean thermal energy conversion (OTEC) aims to use the temperature difference between surface and deep seawater generate electricity (possibly) freshwater [...]

2013
Shingo Kato Michiyuki Nakawake Junko Kita Toshiro Yamanaka Motoo Utsumi Kei Okamura Jun-ichiro Ishibashi Moriya Ohkuma Akihiko Yamagishi

To directly access the sub-seafloor microbial communities, seafloor drilling has been done in a deep-sea hydrothermal field of the Suiyo Seamount, Izu-Bonin Arc, Western Pacific. In the present study, crustal fluids were collected from the boreholes, and the bacterial and archaeal communities in the fluids were investigated by culture-independent molecular analysis based on 16S rRNA gene sequen...

2017
Mackenzie E Gerringer Jeffrey C Drazen Thomas D Linley Adam P Summers Alan J Jamieson Paul H Yancey

Many deep-sea fishes have a gelatinous layer, or subdermal extracellular matrix, below the skin or around the spine. We document the distribution of gelatinous tissues across fish families (approx. 200 species in ten orders), then review and investigate their composition and function. Gelatinous tissues from nine species were analysed for water content (96.53 ± 1.78% s.d.), ionic composition, o...

Journal: :Proceedings of the National Academy of Sciences of the United States of America 2009
Cynthia Chen Peter N Sedwick Mukul Sharma

Osmium is one of the rarer elements in seawater, with typical concentration of approximately 10 x 10(-15) g g(-1) (5.3 x 10(-14) mol kg(-1)). The osmium isotope composition ((187)Os/(188)Os ratio) of deep oceans is 1.05, reflecting a balance between inputs from continental crust (approximately 1.3) and mantle/cosmic dust (approximately 0.13). Here, we show that the (187)Os/(188)Os ratios measur...

Journal: :Proceedings of the National Academy of Sciences of the United States of America 2015
Tristan J Horner Helen M Williams James R Hein Mak A Saito Kevin W Burton Alex N Halliday Sune G Nielsen

Biological carbon fixation is limited by the supply of Fe in vast regions of the global ocean. Dissolved Fe in seawater is primarily sourced from continental mineral dust, submarine hydrothermalism, and sediment dissolution along continental margins. However, the relative contributions of these three sources to the Fe budget of the open ocean remains contentious. By exploiting the Fe stable iso...

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