Comparison of microbial assemblages associated with the stalked barnacle Neolepas marisindica from two adjacent hydrothermal vent fields on the Central Indian Ridge. [PDF]
Lim JK, Kim JA, Lee N, Oh C, Woo S.
europepmc +1 more source
Global patterns of diversity and metabolism of microbial communities in deep-sea hydrothermal vent deposits. [PDF]
Zhou Z +3 more
europepmc +1 more source
Iron Sources and Cycling During Diagenetic Transformations of Negev Phosphorites (Israel)
Abstract The Late Cretaceous Negev area in the Levant was influenced by high productivity upwelling in southern Tethys, leading to massive deposition of phosphorites. The phosphorites occur in two facies: (a) pristine phosphorites with low phosphorous (P) content, formed under low‐energy, high‐productivity conditions, and (b) reworked phosphorites with
Irina Zweig +3 more
wiley +1 more source
Contrasting Genomic Responses of Hydrothermal Vent Animals and Their Symbionts to Population Decline After the Hunga Volcanic Eruption. [PDF]
Breusing C +7 more
europepmc +1 more source
Genome Study of α-, β-, and γ-Carbonic Anhydrases from the Thermophilic Microbiome of Marine Hydrothermal Vent Ecosystems. [PDF]
Gheibzadeh MS +5 more
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Responsible Science at Hydrothermal Vents [PDF]
Colin Devey +2 more
openaire +1 more source
Abstract The 9th International Conference on Arctic Margins, held in Ottawa, Canada, from 13–15 June 2022, convened under the theme Through the Arctic Lens, drawing renewed attention to the scientific, logistical, and environmental challenges inherent to geoscience research in the Arctic. This Special Collection presents a suite of studies spanning the
Marie‐Claude Williamson
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A deep-sea hydrothermal vent worm detoxifies arsenic and sulfur by intracellular biomineralization of orpiment (As2S3). [PDF]
Wang H +10 more
europepmc +1 more source
Candidatus Alkanophaga archaea from Guaymas Basin hydrothermal vent sediment oxidize petroleum alkanes. [PDF]
Zehnle H +6 more
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Abstract Our understanding of subduction initiation remains limited by the difficulty of making direct observations of geologically recent examples. In the geologic record, supra‐subduction zone ophiolites are often interpreted to record syn‐initiation slab rollback and upper plate extension. Unfortunately, many ophiolites are decoupled from records of
B. M. Keough +3 more
wiley +1 more source

