ライフサイエンスコーパス: hot spring

1 ravertine stromatolites in a Southwest Japan hot spring.

2 e other when stromatolites protrude from the hot spring.

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

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

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

6 silica under conditions similar to volcanic hot springs.

7 at environments of Yellowstone National Park hot springs.

8 philic proteins to tolerate high-temperature hot springs.

9 nce for independent populations in different hot springs.

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

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

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

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

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

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

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

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

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

19 Acidic hot springs are colonized by a diversity of hyperthermop

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

40 These hot springs harbor low-complexity cellular communities d

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

73 rom viral populations isolated directly from hot spring samples.

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

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

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

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

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

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

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

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

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

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

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

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

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