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1 at approximately 5,000 m, the deepest known hydrothermal vent.
2 of ancient lineage isolated from a deep-sea hydrothermal vent.
3 n that FeOB are abundant at certain deep-sea hydrothermal vents.
4 chemosynthetic environments: cold seeps and hydrothermal vents.
5 assuming that organic syntheses can occur in hydrothermal vents.
6 e long been used as experimental proxies for hydrothermal vents.
7 uses inhabited the subseafloor crust beneath hydrothermal vents.
8 a half kilometers below the ocean surface at hydrothermal vents.
9 bitable environments may have been submarine-hydrothermal vents.
10 idea that autotrophic metabolism emerged at hydrothermal vents.
11 across geochemically different diffuse fluid hydrothermal vents.
12 ulations in the warm subseafloor of deep-sea hydrothermal vents.
13 xylem and phloem, and surviving in deep-sea hydrothermal vents.
14 gales, an order well represented in deep-sea hydrothermal vents.
15 ose via thermodynamically directed events at hydrothermal vents.
16 e nanoscale tubes, brinicles, or chimneys at hydrothermal vents.
17 our observations provide direct evidence for hydrothermal vents acting as a source of old carbon to t
18 l reactor to simulate conditions in alkaline hydrothermal vents, allowing investigation of the possib
21 r previously unknown, diverse, and very deep hydrothermal vents along the approximately 110 km long,
24 ic Circumpolar Current, downstream of active hydrothermal vents along the Southwest Indian Ridge.
25 ative to the distribution and temperature of hydrothermal vents along this section of the ridge sugge
26 hree marine environments, including deep-sea hydrothermal vents (Alvinella pompejana), the temperate
27 lculate the relative contribution from dust, hydrothermal venting and reductive and non-reductive sed
30 ting that thermal hydrocarbon synthesis near hydrothermal vents and deeper in the magma-hydrothermal
31 ioning among the chemosynthetic symbioses at hydrothermal vents and illustrate the coupling between s
32 r, and flux estimates from atmospheric dust, hydrothermal vents and oceanic sediments vary by orders
33 ave identified environments as rich in H2 as hydrothermal vents and seafloor-spreading centres and ha
34 and possible antiquity of faunas at deep-sea hydrothermal vents and seeps have been debated since the
37 precipitation of ferrous iron emanating from hydrothermal vents and thus suggest that the original ro
39 fer insights into the effects of pressure on hydrothermal venting, and the biogeography of vent fauna
40 re we report an anion-selective CLR from the hydrothermal vent annelid worm Alvinella pompejana that
45 Natural CO2 releases from shallow marine hydrothermal vents are assumed to mix into the water col
47 r than 2000 m on continental slopes, whereas hydrothermal vents are found at greater depths along act
48 beworms to thrive in the harsh conditions of hydrothermal vents are hemoglobins that permit the seque
53 asses of the North Atlantic and diffuse flow hydrothermal vents are one to two orders of magnitude mo
57 hermal environments, such as hot springs and hydrothermal vents, are hotspots for carbon cycling and
58 stewaters, ore deposits, mining regions, and hydrothermal vents, as exemplified by the formation of n
59 omarina loihiensis, isolated recently from a hydrothermal vent at 1,300-m depth on the Loihi submarin
60 geochemical data for high-temperature active hydrothermal venting at Dragon Horn area (49.7 degrees E
61 ectively, these findings reveal multifaceted hydrothermal venting at Lucky B, driven by geological an
62 of hydrothermally-derived Mn, implying that hydrothermal venting at the Chicxulub structure may have
63 ion on the African margin (1-4 per cent) and hydrothermal venting at the Mid-Atlantic Ridge (2-6 per
65 on of the fauna is similar to that of Arctic hydrothermal vents at similar depths, including the Jotu
66 e observe that both high and low temperature hydrothermal vents at the 9 degrees 50' N; 104 degrees 1
69 is possible that early life diversified near hydrothermal vents, but hypotheses that life first occup
70 for microbial communities at two neighboring hydrothermal vents by examining the sequences of more th
71 his study characterizes mineral catalysts at hydrothermal vents by investigating the interactions bet
73 e vent source with sufficient magnitude that hydrothermal vents can have far-field effects on global
76 ntamination standard from Lake Erie and of a hydrothermal vent chimney sample from the Guaymas Basin
78 including sulfate-methane transition zones, hydrothermal vents, coastal sediments, and deep-sea surf
79 dosymbionts are the metabolic cornerstone of hydrothermal vent communities, providing invertebrate ho
80 ivity is particularly intriguing in deep-sea hydrothermal vent communities, where the habitat is patc
81 ino acids is changed for organisms living in hydrothermal vents compared with those living at the sea
82 few ancient sedimentary basins with numerous hydrothermal vent complexes (HTVCs) where craters appear
84 Pyruvate has been produced under simulated hydrothermal vent conditions from alkyl thiols and carbo
86 acting across thin FeS walls within alkaline hydrothermal vents could drive carbon assimilation, lead
87 hermophilic microorganism that is found near hydrothermal vents deep under the sea, where the pressur
89 olinae) are globally distributed at deep-sea hydrothermal vents, depend upon chemoautotrophic symbion
90 rge chemosynthetic mussels found at deep-sea hydrothermal vents descend from much smaller species ass
91 of Epsilonproteobacteria as episymbionts in hydrothermal vent ecosystems is a product of adaptive ca
92 and biogeochemical analysis of the deep-sea hydrothermal vent ecosystems rely on water sample recove
94 bionts are metabolically tuned for growth in hydrothermal vent ecosystems with genes encoding the com
96 nerated mesoscale eddies in the transport of hydrothermal vent efflux and of vent larvae away from th
97 rous mineral formations near subsea alkaline hydrothermal vents embed microenvironments that make the
99 cano that hosts a network of low-temperature hydrothermal vents enriched in ferrous iron that support
101 As, we characterized eukaryotic diversity in hydrothermal vent environments of Guaymas Basin in the G
108 hemical data from two gravity cores near the hydrothermal vent field Loki's Castle at the Arctic Mid-
109 show that hypocentres beneath a well-studied hydrothermal vent field on the East Pacific Rise cluster
110 red gastropod mollusc from the Kairei Indian hydrothermal vent field, which is unlike any other known
111 sive knowledge of the distribution of active hydrothermal vent fields along midocean ridges is essent
112 position of the bloom relative to two active hydrothermal vent fields along the Australian Antarctic
113 caris chacei) is a Bresiliid shrimp found at hydrothermal vent fields along the Mid-Atlantic Ridge.
115 s exiting the basaltic crust in and near two hydrothermal vent fields on the Endeavour Segment, Juan
117 lfurimonas spp. are widespread in sediments, hydrothermal vent fields, aquifers and subsurface enviro
118 Within the endemic invertebrate faunas of hydrothermal vents, five biogeographic provinces are rec
119 methanogenic archaeon isolated from deep-sea hydrothermal vent fluid was found to reduce N(2) to NH(3
120 ition metal sulfide minerals under simulated hydrothermal vent fluids at more moderate temperatures (
121 in situ extraction of organic compounds from hydrothermal vent fluids through a unique solid phase mi
122 ng freshwater from groundwater wells, marine hydrothermal vent fluids, and marine sediment porewaters
124 stimate of protistan grazing pressure within hydrothermal vent food webs, highlighting the important
128 ies present at the ESR and at other deep-sea hydrothermal vents globally indicate that vent biogeogra
130 iochemistry of many taxa inhabiting deep-sea hydrothermal vents have been elucidated; however, the ph
133 Based on recent abyssal dFe enrichments near hydrothermal vents, however, the leaky vent hypothesis a
134 lobsters, we collected ten specimens from a hydrothermal vent in the Guaymas Basin (Gulf of Californ
137 ery of chemosynthetic ecosystems at deep-sea hydrothermal vents in 1977 changed our view of biology.
138 s also been proposed as a gateway connecting hydrothermal vents in different oceans but is little exp
139 uge temperature gradients are present around hydrothermal vents in the deep ocean seafloor, this proc
143 xperiment-an injection of mantle helium from hydrothermal vents into the Circumpolar Current near Dra
144 corroborates a long-standing hypothesis that hydrothermal vent invertebrates affiliate with locally a
146 hat most of the dissolved iron discharged by hydrothermal vents is lost from solution close to ridge-
147 cology and evolution in globally distributed hydrothermal vents is shaped by endemism and thus may ha
148 es of manganese nodules, to the discovery of hydrothermal vents, it has been recognized that microorg
150 annelid family strictly endemic to deep-sea hydrothermal vents located on the ridge crests in the Pa
152 r and increases understanding of the role of hydrothermal vent microbial communities in deep ocean bi
155 chemosynthetic ecosystems in the vicinity of hydrothermal vents, molecular insights into its solvatio
156 B, ceramide-like metabolites of the deep-sea hydrothermal vent mussel Bathymodiolus thermophilus, was
159 nitial discovery of low-temperature alkaline hydrothermal vents off the Mid-Atlantic Ridge axis nearl
161 d microdistribution of faunal assemblages at hydrothermal vents often reflect the fine-scale spatial
166 Such findings reveal the important role of hydrothermal vents on surface biogeochemistry, potential
167 specialised fauna documented in this paper, hydrothermal vents on the AMOR should be regarded as vul
168 series of exit fluid temperatures from five hydrothermal vents on the East Pacific Rise axis, betwee
169 ubeworm, Riftia pachyptila, which lives near hydrothermal vents on the ocean floor, harbors a sulfur
172 isms are important in many habitats, such as hydrothermal vents, oxic-sulfidic interfaces, or oilfiel
174 rgy at depths ranging from 800 to 4,950 m in hydrothermal vent plumes and pelagic background seawater
175 lyzed oxidation of reduced sulfur species in hydrothermal vent plumes in the deep oceans supported th
176 se of filamentous microorganisms from modern hydrothermal vent precipitates and analogous microfossil
178 extreme and geographically isolated nature, hydrothermal vents provide a valuable window into the en
179 s sedimentary rocks, interpreted as seafloor-hydrothermal vent-related precipitates, from the Nuvvuag
181 49,962 viruses from 52 globally distributed hydrothermal vent samples (10 plume, 40 deposit, and 2 d
182 l hot spring sediments in China and deep-sea hydrothermal vent sediments in Guaymas Basin, Gulf of Ca
183 terium isolated from the Grandbonum deep-sea hydrothermal vent site at the East Pacific Rise (13 degr
185 y through quantification of symbionts at two hydrothermal vent sites and symbiont evolution using fun
189 ncluding sulfidic karst systems, shallow-sea hydrothermal vents, sites of acid mine drainage, and aci
190 nomic approaches to four species of deep-sea hydrothermal vent snails that live in association with c
191 Most of the new species from LCVF are either hydrothermal vent specialists or have been reported from
194 e stratigraphy to date the active phase of a hydrothermal vent system and find it to postdate massive
202 environmental samples ranging from deep-sea hydrothermal vents to insect guts, providing a powerful
204 channels within the mineral precipitates of hydrothermal vent towers have previously been proposed t
206 stal structure of the C1 hemoglobin from the hydrothermal vent tubeworm Riftia pachyptila has been de
210 ching thermophilic bacterium from a deep-sea hydrothermal vent, using a two-step cultivation strategy
211 tly hydrogenotrophic inhabitant of submarine hydrothermal vents, was cultivated in a reactor at two h
213 or the emergence of life at a warm submarine hydrothermal vent, we suggest that, within a hydrotherma
214 ansport across protocell membranes in Hadean hydrothermal vents, we consider both theoretically and e
216 Five extremely thermophilic Archaea from hydrothermal vents were isolated, and their DNA polymera
218 he highest oceanic temperatures are found at hydrothermal vents, where the polychaete Paralvinella su
220 results of two field deployments at deep-sea hydrothermal vents, wherein we examined changes in micro
222 s association with the periphery of isolated hydrothermal vents, which, although patchy and ephemeral
223 orts abundant faunal assemblages at deep-sea hydrothermal vents, with zonation of invertebrate specie
225 studies have predicted that the incidence of hydrothermal venting would be extremely low on ultraslow