ライフサイエンスコーパス: hot spring

1 he phylum Thermoproteota, from a terrestrial hot spring.

2 le are potentially taking place in As Burgas hot spring.

3 ini-metagenomic sequencing of samples from a hot spring.

4 ravertine stromatolites in a Southwest Japan hot spring.

5 e other when stromatolites protrude from the hot spring.

6 philic proteins to tolerate high-temperature hot springs.

7 in nearly every habitat, from permafrost to hot springs.

8 deep-sea hydrothermal vents and terrestrial hot springs.

9 ter Thomas Brock for his seminal research in hot springs.

10 al impact of geothermal energy production on hot springs.

11 Paoha Island's (Mono Lake, CA) arsenic-rich hot springs.

12 s dominated over oxyanions in many Icelandic hot springs.

13 nce for independent populations in different hot springs.

14 d As transformation in alkaline sulfide-rich hot springs.

15 distribution of P- and C-GDGTs in Tengchong hot springs.

16 silica under conditions similar to volcanic hot springs.

17 distributed among Yellowstone National Park hot springs.

18 at environments of Yellowstone National Park hot springs.

19 ain Pseudomonas alcaligenes Med1 from Medano hot spring (39.1 degrees C surface temperature, pH 7.1)

20 ated from Yellowstone National Park's acidic hot springs also exploits the host ESCRT machinery in it

21 n United States because of extremely dry and hot spring and summers; however, increased temperature a

22 NA-DNA hybrid virus recently identified in a hot spring and to an ssDNA virus infecting the diatom Ch

23 ae (Rhodophyta), has successfully thrived in hot springs and associated sites worldwide for more than

24 particles in air samples collected over YNP hot springs and by their detection in metacommunity sequ

25 Hydrogen (H(2) ) is enriched in hot springs and can support microbial primary production

26 They exist in diverse habitats, ranging from hot springs and deserts to glaciers and the open ocean.

27 Geothermal environments, such as hot springs and hydrothermal vents, are hotspots for car

28 the already studied arsenic and sulfide rich hot springs and soda lakes where it was discovered.

29 c processes that generate and source H(2) to hot springs and the distribution of organisms that use H

30 point to potential susceptibility of certain hot springs and their biodiversity to sustained, longer-

31 report noble gas signatures of groundwater, hot springs, and bedrock samples from a major fault syst

32 ans, lightless caves, noxious lakes, boiling hot springs, and nuclear waste sites.

33 m such inhospitable environments as deserts, hot springs, and polar seas.

34 water obtained from various sources (ocean, hot springs, and soil) produces mineralo-organic particl

35 ween low-temperature marine Archaea and some hot spring Archaea.

36 suggests that the resident Archaea in these hot springs are acclimated if not adapted to low pH by t

37 Acidic hot springs are colonized by a diversity of hyperthermop

38 lecular weight organic compounds in deep-sea hot springs are compelling owing to implications for the

39 esults indicate that geographically isolated hot springs are readily able to exchange viruses.

40 eal viruses found in high-temperature acidic hot springs around the world (pH </=4.0; temperature of

41 In some Icelandic hot springs, arsenic was nearly quantitatively thiolated

42 e phase during a wet-dry cycle in freshwater hot springs associated with subaerial volcanic landmasse

43 infects Sulfolobus solfataricus in volcanic hot springs at 80 degrees C and pH 3.

44 e examples of life's resilience, thriving in hot springs at boiling temperatures, in brine lakes satu

45 We chose viral metagenomes obtained from two hot springs, Bear Paw and Octopus, in Yellowstone Nation

46 f temporal hydrologic and geologic change on hot spring biodiversity is unknown.

47 vironmental data from the site of isolation (hot-spring biofilm) revealed (an)aerobic respiration as

48 rrent frog (Amolops tormotus) from Huangshan Hot Springs, China.

49 eport a long-term helium anomaly measured in hot springs close to the central cone.

50 iensis from the Rhynie and Windyfield cherts hot spring complex in Scotland, reveals details of head

51 Cyanobacteria in Yellowstone hot springs comprise several diverse species that have c

52 e rock surfaces of anoxic brine pools fed by hot springs containing arsenite and sulfide at high conc

53 genomic sequences obtained from well-studied hot spring cyanobacterial mats with genomic sequences of

54 f, Roman aqueduct, cave, deep subsurface and hot-spring deposits.

55 es likely emerge when the water level of the hot spring drops.

56 cal factors responsible for the emergence of hot springs during the LGM and argue that refugia of thi

57 features in the genome of this cellulolytic, hot-springs-dwelling prokaryote include a low occurrence

58 From both Bear Paw and Octopus hot springs, each assembled contig had more similarity t

59 While this study used an acidic hot spring environment to characterize a new archaeal vi

60 continental branchiopods are associated with hot spring environments [7] represented by the Early Dev

61 surface snowmelt runoff destabilize smaller hot spring environments with smaller populations and res

62 ropose, given the low host cell densities of hot spring environments, that the TSPV1 filaments serve

63 acid-sulfate leaching or precipitation from hot spring fluids was suggested previously.

64 H) are widely speculated to form in seafloor hot spring fluids.

65 Subseafloor mixing of high-temperature hot-spring fluids with cold seawater creates intermediat

66 states, and thioantimonates, in sulfide-rich hot springs from Yellowstone National Park and Iceland i

67 ogy associated with precipitation can impact hot spring geochemistry and microbial biodiversity.

68 , metabolism, and phylogeny as a function of hot spring geochemistry.

69 rt remarkably similar features within active hot spring/geyser discharge channels at El Tatio in nort

70 s (Archaea) dominate high-temperature acidic hot springs (>80 degrees C, pH <4).

71 es can be found in many acidic (pH <or= 4.0) hot springs (>or=70 degrees C) around the world.

72 for their distribution and ecology in their hot spring habitats.

73 These hot springs harbor low-complexity cellular communities d

74 Our finding of abiogenic formate in deep-sea hot springs has significant implications for microbial l

75 eavy metal-rich environments associated with hot springs have a major impact on biological processes

76 ly Sulfolobus) shibatae B12, isolated from a hot spring in Beppu, Japan in 1982, is one of the first

77 ow among genomes of 12 strains from a single hot spring in Kamchatka, Russia, demonstrate higher leve

78 ing from a metagenomic sample collected at a hot spring in Kirishima, Japan.

79 study examines SBCs from the Dusun Tua (DT) hot spring in Malaysia (75 degrees C, pH 7.6), where Aqu

80 from a Thermoproteales host isolated from a hot spring in Yellowstone National Park (USA).

81 drogenobacter, isolated from a circumneutral hot spring in Yellowstone National Park (YNP) capable of

82 Living stromatolites growing in a hot spring in Yellowstone National Park are composed of

83 es obtained from uncultivated organisms of a hot spring in Yellowstone National Park reveals several

84 At Conch Spring, an alkaline hot spring in Yellowstone National Park, trithioarsenate

85 rus (MTIV), that was isolated from an acidic hot spring in Yellowstone National Park, USA.

86 ed icosahedral virus (STIV), isolated from a hot spring in Yellowstone National Park, was the first i

87 s of Yellowstone National Park and the Rehai hot springs in China.

88 eochemical and molecular analysis from seven hot springs in five regions sampled over 3 years in Yell

89 equences of two ribovirus groups from acidic hot springs in Japan.

90 us spindle-shaped viruses (SSVs) from acidic hot springs in Kamchatka (Russia) and Yellowstone Nation

91 ons and the microbial communities inhabiting hot springs in Tengchong County, Yunnan Province, China.

92 iversity and functional potential within two hot springs in the caldera of Kamchatka.

93 e Magadi, a hypersaline alkaline lake fed by hot springs in the semi-arid southern Kenya Rift Valley.

94 ermal waters from the Semi, Dagejia and Kawu hot springs in the Shiquanhe-Yarlung Zangbo geothermal f

95 al conditions characteristic of the volcanic hot springs in which these archaeal extremophiles reside

96 genome segments from high-temperature acidic hot springs in Yellowstone National Park in the United S

97 trophic microbial mats of alkaline siliceous hot springs in Yellowstone National Park revealed the ex

98 nhabits microbial mats of alkaline siliceous hot springs in Yellowstone National Park, is the only kn

99 ales strains previously isolated from acidic hot springs in Yellowstone National Park, one of which a

100 5 degrees C) water and sediment samples from hot springs in Yellowstone National Park, Wyoming, USA (

101 irus isolated from an archaeal host found in hot springs in Yellowstone National Park.

102 Hot springs integrate hydrologic and geologic processes

103 ntrations in Yellowstone National Park (YNP) hot springs is presented.

104 In contrast, hot spring lineages have alternate pathways to increase

105 igh-temperature (80 degrees C) acidic (pH 2) hot spring located in Yellowstone National Park, followe

106 Hitherto, N2 fixation in hot spring mats was attributed either to filamentous cya

107 rtium using two representative isolates from hot spring mats: the unicellular oxygenic phototrophic c

108 the major Ca. C. thermophilum population in hot-spring mats.

109 study we retrieved viral sequences from six hot spring metagenomes isolated worldwide, revealing a w

110 ose first member EnvSia156 was isolated from hot spring metagenomes, defines an unusual structural fo

111 Phage polymerase, previously identified from hot spring metagenomic sampling, and additional thermost

112 x, in metagenomic sequence data derived from hot spring microbial mats.

113 alcaligenes Med1 from Central Andean Chilean hot spring of central Chile can be a useful additive for

114 , in red-pigmented microbial mats within the hot springs of Paoha Island.

115 Little is known about life in the boron-rich hot springs of Trans-Himalayas.

116 have identified crenarchaeal viruses in the hot springs of Yellowstone National Park and other high

117 ter channels, such as those found at Mammoth hot springs of Yellowstone National Park and the Rehai h

118 haeota, a symbiotic archaean found in acidic hot springs of Yellowstone National Park, USA.

119 hanges of microbial communities in Tengchong hot springs of Yunnan Province, China in response to geo

120 synthesized non-enzymatically in freshwater hot springs on the prebiotic Earth with sizes sufficient

121 The second group, denoted hot spring partiti-like viruses (HsPV), forms a distinct

122 s, an archaeal virus isolated from an acidic hot spring (pH 2-4, 72-92 degrees C) in Yellowstone Nati

123 Sulfolobus species that thrive in the acidic hot springs (pH 2.9 to 3.9 and 72 to 92 degrees C) of Ye

124 habitants of active seafloor and continental hot springs populate the deepest branches of the univers

125 idian Pool (OP), a Yellowstone National Park hot spring previously shown to contain remarkable archae

126 marinus, isolated from shallow water marine hot springs, produces a number of carbohydrate-degrading

127 Alkaline sulfide-rich hot springs provide a unique environment for microbial c

128 ted that wet-dry cycles simulating prebiotic hot springs provide sufficient energy to drive condensat

129 om Tibet, Yellowstone and the US Great Basin hot springs revealed a similar relationship between pH a

130 One group, denoted hot spring riboviruses (HsRV), consists of viruses with

131 c primary productivity in three co-localized hot springs (RSW, RSN, and RSE) in Yellowstone National

132 arallel water and sediment samples along the hot spring's outflow channel.

133 lfide (up to 5.87 mg/L), were present in the hot spring's pools, which suggested As(III) oxidation oc

134 We used this approach to analyze two hot spring samples from Yellowstone National Park and ex

135 rom viral populations isolated directly from hot spring samples.

136 River estuary and Yellowstone National Park hot spring sediment metagenomes.

137 ilable microbiome data and found that ocean, hot spring sediments and soil microbiomes use a more div

138 ne constructed from single cells sorted from hot spring sediments and the other derived from binned m

139 me-assembled genomes (MAGs) from terrestrial hot spring sediments in China and deep-sea hydrothermal

140 Therefore, physical abiotic features such as hot spring size and position in the landscape are import

141 te a chemosynthetic microbial community in a hot spring (SJ3) of Yellowstone National Park that exhib

142 hailand and Andaman Sea, shrimp pond sludge, hot spring soil and chicken feces.

143 on of SSU rRNA and mcrA transcripts from one hot spring suggested that predominant Bathyarchaeota wer

144 of genes from uncultured microorganisms in a hot spring suggests that the diversity of life on Earth

145 nd birds, an isolated population (South West Hot Springs, SWHS) of Magadi tilapia thrives in fast-flo

146 m the metagenome of a circumneutral, suboxic hot spring that contains high levels of sulfate, sulfide

147 ot Valley desert and the Icelandic Gunnuhver hot spring) that have been explored as analogs of Mars a

148 s and subsequently in terrestrial geothermal hot springs, the Nanoarchaeota species that have been de

149 rophic base for primary productivity in this hot spring, through hydrogen oxidation and sulfate reduc

150 , we explored virus diversity in the acidic, hot spring Umi Jigoku in Beppu, Japan.

151 st time evidence of life existing with these hot springs using a combination of morphological and mol

152 Five (n = 5) bacterial strains isolated from hot spring water and wet clay, Malaysia were screened fo

153 The recordings acquired close to a hot spring were of very high quality, implying that the

154 Hydrogen concentrations in the hot springs were measured and found to range up to >300

155 sahedral virus (STIV) was isolated in acidic hot springs where it infects the archeon Sulfolobus solf

156 he volcanisms have created the unique Dallol hot springs, which are highly acidic (pH ~ 0) and saline

157 he mcr-containing archaeal MAGs from several hot springs, which reveal further expansion in the diver

158 e (>70 degrees C) communities in Yellowstone hot springs with distinct chemistries, conducted paralle

159 l community analyses of three widely studied hot springs with local precipitation data in Yellowstone

160 s) from environmental DNA extracted from two hot springs within an active volcanic ecosystem on the K

161 e diversity of two archaeal viruses found in hot springs within Yellowstone National Park (YNP).

162 sampled in different seasons from Tengchong hot springs (Yunnan, China), which encompassed a pH rang

163 tudy, a representative alkaline sulfide-rich hot spring, Zimeiquan in the Tengchong geothermal area,