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Articles 2971 - 3000 of 29947
Full-Text Articles in Geology
Mgrre_Thinsections_Mgrre-112_14, Mgrre
Mgrre_Thinsections_Mgrre-112_15, Mgrre
Mgrre_Thinsections_Mgrre-112_16, Mgrre
Mgrre_Thinsections_Mgrre-112_17, Mgrre
Mgrre_Thinsections_Mgrre-112_18, Mgrre
Mgrre_Thinsections_Mgrre-113_1, Mgrre
Mgrre_Thinsections_Mgrre-113_3, Mgrre
Mgrre_Thinsections_Mgrre-113_4, Mgrre
Mgrre_Thinsections_Mgrre-113_5, Mgrre
Mgrre_Thinsections_Mgrre-113_6, Mgrre
Mgrre_Thinsections_Mgrre-111_5, Mgrre
Mgrre_Thinsections_Mgrre-113_7, Mgrre
Mgrre_Thinsections_Mgrre-114_3, Mgrre
Mgrre_Thinsections_Mgrre-114_5, Mgrre
Mgrre_Thinsections_Mgrre-114_8, Mgrre
Mgrre_Thinsections_Mgrre-114_9, Mgrre
Mgrre_Thinsections_Mgrre-114_11, Mgrre
Mgrre_Thinsections_Mgrre-114_14, Mgrre
Mgrre_Thinsections_Mgrre-114_15, Mgrre
Mgrre_Thinsections_Mgrre-114_19, Mgrre
Mgrre_Thinsections_Mgrre-114_18, Mgrre
Mgrre_Thinsections_Mgrre-110_16, Mgrre
Mgrre_Thinsections_Mgrre-110_19, Mgrre
Mgrre_Thinsections_Mgrre-114_4, Mgrre
Mgrre_Thinsections_Mgrre-114_7, Mgrre
Mgrre_Thinsections_Mgrre-114_17, Mgrre
Mgrre_Thinsections_Mgrre-104_1, Mgrre
Mgrre_Thinsections_Mgrre-104_10, Mgrre
Microbial Ecology Of A Shallow Alkaline Hydrothermal Vent: Strýtan Hydrothermal Field, Eyjafördur, Northern Iceland, Katrina I. Twing, L. M. Ward, Zachery K. Kane, Alexa Sanders, Roy Edward Price, H. Lizethe Pendleton, Donato Giovannelli, William J. Brazelton, Shawn E. Mcglynn
Microbial Ecology Of A Shallow Alkaline Hydrothermal Vent: Strýtan Hydrothermal Field, Eyjafördur, Northern Iceland, Katrina I. Twing, L. M. Ward, Zachery K. Kane, Alexa Sanders, Roy Edward Price, H. Lizethe Pendleton, Donato Giovannelli, William J. Brazelton, Shawn E. Mcglynn
Geosciences: Faculty Publications
Strýtan Hydrothermal Field (SHF) is a submarine system located in Eyjafördur in northern Iceland composed of two main vents: Big Strýtan and Arnarnesstrýtan. The vents are shallow, ranging from 16 to 70 m water depth, and vent high pH (up to 10.2), moderate temperature (Tmax ∼70°C), anoxic, fresh fluids elevated in dissolved silica, with slightly elevated concentrations of hydrogen and methane. In contrast to other alkaline hydrothermal vents, SHF is unique because it is hosted in basalt and therefore the high pH is not created by serpentinization. While previous studies have assessed the geology and geochemistry of this site, the …