scholarly journals Characterization of benthic biogeochemistry and ecology at three methane seep sites on the Northern U.S. Atlantic margin

Author(s):  
D. McVeigh ◽  
A. Skarke ◽  
A.E. Dekas ◽  
C. Borrelli ◽  
W.-L. Hong ◽  
...  
2017 ◽  
Vol 4 ◽  
Author(s):  
Diva J. Amon ◽  
Judith Gobin ◽  
Cindy L. Van Dover ◽  
Lisa A. Levin ◽  
Leigh Marsh ◽  
...  

2018 ◽  
Vol 6 ◽  
Author(s):  
Simone S. Mantovanelli ◽  
Colombo C. G. Tassinari ◽  
Michel M. De Mahiques ◽  
Luigi Jovane ◽  
Everton Bongiolo

2001 ◽  
Vol 20 (1) ◽  
pp. 34-50 ◽  
Author(s):  
Jeffrey S. Ogilvie ◽  
Richard Crompton ◽  
Nicholas M. Hardy

PLoS ONE ◽  
2019 ◽  
Vol 14 (3) ◽  
pp. e0211616 ◽  
Author(s):  
D. Katharine Coykendall ◽  
Robert Scott Cornman ◽  
Nancy G. Prouty ◽  
Sandra Brooke ◽  
Amanda W. J. Demopoulos ◽  
...  

2010 ◽  
Vol 4 (10) ◽  
pp. 1326-1339 ◽  
Author(s):  
Thomas D Niederberger ◽  
Nancy N Perreault ◽  
Stephanie Tille ◽  
Barbara Sherwood Lollar ◽  
Georges Lacrampe-Couloume ◽  
...  

Tectonics ◽  
2018 ◽  
Vol 37 (9) ◽  
pp. 3303-3327 ◽  
Author(s):  
Carl McDermott ◽  
Lidia Lonergan ◽  
Jenny S. Collier ◽  
Kenneth G. McDermott ◽  
Paul Bellingham

2004 ◽  
Vol 70 (12) ◽  
pp. 7445-7455 ◽  
Author(s):  
Fumio Inagaki ◽  
Urumu Tsunogai ◽  
Masae Suzuki ◽  
Ayako Kosaka ◽  
Hideaki Machiyama ◽  
...  

ABSTRACT Samples from three submerged sites (MC, a core obtained in the methane seep area; MR, a reference core obtained at a distance from the methane seep; and HC, a gas-bubbling carbonate sample) at the Kuroshima Knoll in the southern Ryuku arc were analyzed to gain insight into the organisms present and the processes involved in this oxic-anoxic methane seep environment. 16S rRNA gene analyses by quantitative real-time PCR and clone library sequencing revealed that the MC core sediments contained abundant archaea (∼34% of the total prokaryotes), including both mesophilic methanogens related to the genus Methanolobus and ANME-2 members of the Methanosarcinales, as well as members of the δ-Proteobacteria, suggesting that both anaerobic methane oxidation and methanogenesis occurred at this site. In addition, several functional genes connected with methane metabolism were analyzed by quantitative competitive-PCR, including the genes encoding particulate methane monooxygenase (pmoA), soluble methane monooxygenase (mmoX), methanol dehydrogenese (mxaF), and methyl coenzyme M reductase (mcrA). In the MC core sediments, the most abundant gene was mcrA (2.5 × 106 copies/g [wet weight]), while the pmoA gene of the type I methanotrophs (5.9 × 106 copies/g [wet weight]) was most abundant at the surface of the MC core. These results indicate that there is a very complex environment in which methane production, anaerobic methane oxidation, and aerobic methane oxidation all occur in close proximity. The HC carbonate site was rich in γ-Proteobacteria and had a high copy number of mxaF (7.1 × 106 copies/g [wet weight]) and a much lower copy number of the pmoA gene (3.2 × 102 copies/g [wet weight]). The mmoX gene was never detected. In contrast, the reference core contained familiar sequences of marine sedimentary archaeal and bacterial groups but not groups specific to C1 metabolism. Geochemical characterization of the amounts and isotopic composition of pore water methane and sulfate strongly supported the notion that in this zone both aerobic methane oxidation and anaerobic methane oxidation, as well as methanogenesis, occur.


Author(s):  
B. L. Soloff ◽  
T. A. Rado

Mycobacteriophage R1 was originally isolated from a lysogenic culture of M. butyricum. The virus was propagated on a leucine-requiring derivative of M. smegmatis, 607 leu−, isolated by nitrosoguanidine mutagenesis of typestrain ATCC 607. Growth was accomplished in a minimal medium containing glycerol and glucose as carbon source and enriched by the addition of 80 μg/ ml L-leucine. Bacteria in early logarithmic growth phase were infected with virus at a multiplicity of 5, and incubated with aeration for 8 hours. The partially lysed suspension was diluted 1:10 in growth medium and incubated for a further 8 hours. This permitted stationary phase cells to re-enter logarithmic growth and resulted in complete lysis of the culture.


Author(s):  
A.R. Pelton ◽  
A.F. Marshall ◽  
Y.S. Lee

Amorphous materials are of current interest due to their desirable mechanical, electrical and magnetic properties. Furthermore, crystallizing amorphous alloys provides an avenue for discerning sequential and competitive phases thus allowing access to otherwise inaccessible crystalline structures. Previous studies have shown the benefits of using AEM to determine crystal structures and compositions of partially crystallized alloys. The present paper will discuss the AEM characterization of crystallized Cu-Ti and Ni-Ti amorphous films.Cu60Ti40: The amorphous alloy Cu60Ti40, when continuously heated, forms a simple intermediate, macrocrystalline phase which then transforms to the ordered, equilibrium Cu3Ti2 phase. However, contrary to what one would expect from kinetic considerations, isothermal annealing below the isochronal crystallization temperature results in direct nucleation and growth of Cu3Ti2 from the amorphous matrix.


Author(s):  
B. H. Kear ◽  
J. M. Oblak

A nickel-base superalloy is essentially a Ni/Cr solid solution hardened by additions of Al (Ti, Nb, etc.) to precipitate a coherent, ordered phase. In most commercial alloy systems, e.g. B-1900, IN-100 and Mar-M200, the stable precipitate is Ni3 (Al,Ti) γ′, with an LI2structure. In A lloy 901 the normal precipitate is metastable Nis Ti3 γ′ ; the stable phase is a hexagonal Do2 4 structure. In Alloy 718 the strengthening precipitate is metastable γ″, which has a body-centered tetragonal D022 structure.Precipitate MorphologyIn most systems the ordered γ′ phase forms by a continuous precipitation re-action, which gives rise to a uniform intragranular dispersion of precipitate particles. For zero γ/γ′ misfit, the γ′ precipitates assume a spheroidal.


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