ライフサイエンスコーパス: cave

1 from Devils Hole and Laghetto Basso (Corchia Cave).

2 zero age of modern fluvial sediment near the cave.

3 aphus) recovered from the same level of Toll Cave.

4 ong nearby regions, and even within the same cave.

5 nthropological evolution associated with the cave.

6 ed to the rock art and human activity in the cave.

7 -resolution speleothem records from the same cave.

8 3,000 kilometers to the west of Chagyrskaya Cave.

9 iled bats (Tadarida brasiliensis) at Bracken Cave.

10 tation to the east and north-east of Bracken Cave.

11 took place in a structured space within the cave.

12 ective precipitation(6,7), ideally in closed caves.

13 minins and other fossils accumulated in open caves.

14 various convergent forms that live in nearby caves.

15 have been obtained at two artificial glacier caves.

16 mples collected from karst springs, wells or caves.

17 emical environment when they began to occupy caves.

18 y on sporadic food input from outside of the caves.

19 the hot summer in the cool climate of alpine caves.

20 ve been studied from a single site, Denisova Cave(1-3) in Siberia.

21 igated originating from 52 capture sites (22 caves, 18 buildings, and 12 outdoor sites) distributed o

22 recovered from an ice deposit accumulated in Cave 29, western New Mexico, provide unambiguous evidenc

23 cave-dense region, (3) good sample sizes per cave, (4) multiple taxa, and (5) genome-wide characteriz

24 Cave 465 at the northern end of the site is unique in it

25 ombustion of organic material, from Lusakert Cave, a MP site in Armenia.

26 results of recent excavations at Chiquihuite Cave-a high-altitude site in central-northern Mexico-tha

27 We amputated appendages in a variety of cave-adapted and surface-dwelling arthropods.

28 yanax mexicanus, comprises 29 populations of cave-adapted fish distributed across a vast karst region

29 cid and bulk stable carbon isotope values of cave-adapted shrimp suggest that carbon from methanotrop

30 n most species tested, including even albino cave-adapted species.

31 within populations decreases with increasing cave age challenges traditional views on founder effects

32 ratures which deviate significantly from the cave air temperature.

33 getation cover and at least partially closed caves allowed for undisturbed, semi-continuous growth of

34 The world heritage site of the Mogao caves, along the ancient Silk Road, consists of 492 rich

35 tive diversification, but does adaptation to caves also facilitate the evolution of reproductive isol

36 common in bacteria isolated from Lechuguilla Cave, an underground ecosystem that has been isolated fr

37 face-dwelling stock that colonized the Micos cave and also introgressed into the ancient Pachon cave

38 ell fragments from the South African Blombos Cave and Diepkloof Rock Shelter provide a unique window

39 m stalactite indicates wet conditions in the cave and humid climate from ~ 200 BCE to 100 CE, at the

40 These finds were made in a small area of the cave and in two separate occupation horizons.

41 30,000-22,000 y ago at Leang Bulu Bettue, a cave and rock-shelter site on the Wallacean island of Su

42 s from two caves in Western Georgia, Melouri Cave and Solkota.

43 is indicates that Datura was ingested in the cave and that the rock painting represents the plant its

44 Here, comparing the blind cave and the surface morphotypes of Astyanax mexicanus f

45 s in the Levant included the repeated use of caves and open landscape sites.

46 is has thus far only been detected in alpine caves and subarctic lake sediments.

47 Viability of BCG vaccine packaged in the caves and the mechanical strength of the powder-laden MN

48 io to more closely reflect conditions in the cave, and therefore, the true age of the fossils.

49 cal diversification in this system and other cave animals, further supporting the role of local adapt

50 t selective forces contribute to eye loss in cave animals?

51 The presence of the same allele in multiple caves appears to be due to selection from standing genet

52 rsal, we find that populations from separate caves are indeed highly genetically isolated.

53 Early cave artists recorded distinct morphological forms consi

54 Our results support the idea of caves as natural laboratories for the study of parallel

55 La Riera Cave (Asturias) has a rich geo-cultural sequence dating

56 tyrosine hydroxylase immunoreactive soma in cave Astyanax in the olfactory bulb, basal telencephalon

57 noradrenaline, in the brains of surface and cave Astyanax using immunohistochemistry.

58 before present, excavated in the El Portalon cave at Sierra de Atapuerca, Spain.

59 rsive virtual reality (VR) environment CAVE (cave automatic virtual environment), a room in which we

60 nsic resistome of Paenibacillus sp. LC231, a cave bacterial isolate that is resistant to most clinica

61 an adolescent and two children, entered the cave barefoot and illuminated the way with a bunch of wo

62 al genome sequence from a Middle Pleistocene cave bear (Ursus deningeri) bone excavated at Sima de lo

63 efacts, including pendants manufactured from cave bear teeth that are reminiscent of those later prod

64 Cave bears also took refuge in the cave until 33,000 y a

65 g signals of reliance on plants for Romanian cave bears based on the delta(15)N values of glutamate a

66 In contrast to cave bears from all other regions in Europe, some indivi

67 The cave bears from Toll Cave show a microwear pattern like

68 lk collagen delta(15)N values observed among cave bears in Romania reflects niche partitioning but in

69 The feeding behaviors of extinct cave bears living during Pleistocene cold periods at mid

70 ow lower values (delta(13)C & delta(15)N) in cave bears than in strict herbivores (i.e. Cervus elaphu

71 other megafauna species (e.g., mammoths and cave bears), relatively few ancient-DNA studies have foc

72 Three recent case studies of cave bears, horses, and maize provide examples of the wa

73 age to all Western European Late Pleistocene cave bears.

74 At Spy cave, Belgium, Neanderthal diet was heavily meat based a

75 dle Pleistocene mandible from Baishiya Karst Cave (BKC) on the Tibetan Plateau has been inferred to b

76 artefacts(2), from excavations at Bacho Kiro Cave (Bulgaria).

77 The stratigraphy at Bacho Kiro Cave, Bulgaria, spans the Middle to Upper Palaeolithic t

78 of these hominin remains accumulated in the cave by geological processes, coming from the adjacent s

79 the MP occupation from the occupation of the cave by H. sapiens, which extends to 34,000 cal BP.

80 short-faced bear, Arctodus simus, from Daisy Cave (CA-SMI-261), an important early human occupation s

81 y immersive virtual reality (VR) environment CAVE (cave automatic virtual environment), a room in whi

82 Oxygen isotope records from Chinese caves characterize changes in both the Asian monsoon and

83 found Chl f and d along the photic zones of caves characterized by low light enriched in NIR and inh

84 n-year-old G. blacki molar found in Chuifeng Cave, China(7,8).

85 m a 40,000-year-old individual from Tianyuan Cave, China, [1, 7] to study his relationship to ancient

86 Although the periods of cave closure leave temporal gaps in the South African fo

87 the Indian subcontinent from the Billasurgam cave complex.

88 anium associated with Acheulean bifaces in a cave context.

89 and Vi-208 Neanderthal remains from Vindija Cave (Croatia) led to the suggestion that Neanderthals s

90 eandertal from 50,000 years ago from Vindija Cave, Croatia, to 30-fold genomic coverage.

91 re we show that flowstones from eight Cradle caves date to six narrow time intervals between 3.2 and

92 mmon troglobionts from (2) nearby caves in a cave-dense region, (3) good sample sizes per cave, (4) m

93 Carbonate cave deposits (speleothems) have been used widely for pa

94 from Broken Hill (Kabwe) was recovered from cave deposits in 1921, during metal ore mining in what i

95 g the relationship between precipitation and cave drip water delta(18)O.

96 olling the temperature of speleothem-forming cave drip waters is vital for assessing the reliability

97 Europe's obligate cave-dwelling amphibian Proteus anguinus inhabits subter

98 raised offspring of wild-caught surface- and cave-dwelling ecotypes of the neotropical fish Poecilia

99 An exception is the cave-dwelling Rousettus aegyptiacus, which has a pronoun

100 d assembled a chromosome-level genome of the cave-dwelling species P. huaijiensis to study gene famil

101 trong reduction in parasite diversity in the cave ecosystem, and show that cavefish immune cells disp

102 r role of air velocity and distance from the cave entrance within a particular cave in driving the fe

103 ns were clearly accumulated by humans at the cave entrance, while the small-size mammals were gathere

104 obial communities across the photic zones of cave entrances resembles the light-driven species distri

105 rom the adjacent slope above the cave or the cave entry, as the palaeogeography and sedimentary chara

106 ral control that underlie adaptations to the cave environment.

107 A hallmark of cave environments is scarcity of food.

108 Subaqueous speleothems from similar deep-cave environments should be capable of providing palaeot

109 enic factors (e.g. combustion) in restricted cave environments.

110 Flowstones are ubiquitous cave features and provide a palaeoclimatic context, beca

111 ew study shows the eye and optic tectum of a cave fish consumes approximately 5-17% of the total ener

112 cos cavefish and phylogenetically old Pachon cave fish inherited this Oca2 allele from the ancestral

113 ong, accurate, and precisely dated record of cave flooding events from the northwest Australian tropi

114 inated mudstone units and sediment along the cave floor were eroded.

115 hinese and Brazilian subtropical speleothem (cave formations such as stalactites and stalagmites) rec

116 and dissolvable hyaluronic acid with a deep cave formed in the basal portion of each microneedle, in

117 Surface and cave forms are interfertile making this system amenable

118 to identify genes responsible for changes in cave forms of A. mexicanus.

119 eams that thrust through the darkness of the cave from floor to ceiling with a luster like moonlight

120 a comparison of ancient inscriptions in Dayu Cave from Qinling Mountains, central China, which descri

121 that some scrolls were brought to the Qumran caves from elsewhere; significantly, they demonstrate th

122 related to Neanderthal hearths from Gorham's Cave (Gibraltar), being one of the first milestones in t

123 The Level VII of Amalda I cave (Gipuzkoa, Spain) represents one of the latest Midd

124 d abundance patterns of these species within caves have not been fully recognized.

125 eys indicate, however, that bats may abandon caves having corrugated culvert entrances.

126 The melting of cave ice under current climate conditions is both uncove

127 btained drinking water by using fire to melt cave ice, and sheds light on one of many human-environme

128 another molar (Denisova 8) found in Denisova Cave in 2010.

129 prehistoric tsunami deposits from a coastal cave in Aceh, Indonesia.

130 he ~120,000-y-old Neanderthals from Scladina Cave in Belgium (Scladina I-4A) and Hohlenstein-Stadel C

131 and 22 thousand years (ka) ago from Yongxing Cave in central China characterizes changes in Asian mon

132 ient-limited mineral environment of a silica cave in comparison with P. fluorescens isolates from sur

133 m a previously unexplored shallow underwater cave in Corsica (France) harbouring the largest biomass

134 sent evidence from the newly excavated Fuyan Cave in Daoxian (southern China).

135 e from the cave entrance within a particular cave in driving the female choice.

136 ars, obtained using speleothems from Paraiso Cave in eastern Amazonia; we interpret the record as bei

137 lgium (Scladina I-4A) and Hohlenstein-Stadel Cave in Germany, as well as to a ~60,000- to 70,000-y-ol

138 tern engraved by Neanderthals, from Gorham's Cave in Gibraltar.

139 Now, fossils and stone tools from a cave in Morocco challenge the notion that East Africa wa

140 y resolved trace element record from Mawmluh Cave in Northeast India with forward modeling experiment

141 lian assemblage of the Tam Hay Marklot (THM) cave in northeastern Laos, to reconstruct the food web a

142 Palaeolithic group of people explored a deep cave in northern Italy about 14 ky cal.

143 e report delta(15)N analysis of guano from a cave in NW Romania with the intent of reconstructing pas

144 aminated Neandertal specimen from Okladnikov Cave in Siberia to isolate its endogenous DNA from moder

145 f broken stalagmites found deep in Bruniquel Cave in southwest France.

146 haic femur from the Hohlenstein-Stadel (HST) cave in southwestern Germany.

147 mblage and taphonomic data from Fa-Hien Lena Cave in Sri Lanka that demonstrates specialized, sophist

148 Bracken Cave in Texas (USA) holds one of the largest bat colonie

149 inger phalanx (Denisova 3) found in Denisova Cave in the Altai Mountains.

150 6,000-year-old barley grains excavated at a cave in the Judean Desert close to the Dead Sea.

151 pic analysis of an ice core recovered from a cave in the Romanian Carpathian Mountains.

152 Denisova Cave in the Siberian Altai (Russia) is a key site for un

153 novel nairoviruses from bats captured from a cave in Zambia.

154 olve (1) common troglobionts from (2) nearby caves in a cave-dense region, (3) good sample sizes per

155 DNA in eight archaeological layers from four caves in Eurasia.

156 eleothem growth in a north-south transect of caves in Siberia to reconstruct the history of permafros

157 A) from Late Quaternary stalagmites from two caves in Western Georgia, Melouri Cave and Solkota.

158 Figueira Brava cave, in the Arrabida range (Portugal), provides an exce

159 or example in the Midwest for Miscanthus and Cave-in-Rock and the upper southeastern U.S. for Alamo.

160 s more water, Alamo consumes less water, and Cave-in-Rock consumes approximately the same amount of w

161 tween potential bioenergy grass (Miscanthus, Cave-in-Rock, and Alamo) production, water quantity, and

162 rom ~ 100 CE to ~ 600 CE, evaporation in the cave increased in response to regional aridification tha

163 sence at 336 metres from the entrance of the cave indicates that humans from this period had already

164 resence of abundant charred material in this cave indicates that they periodically obtained drinking

165 ontroversial owing to the complex history of cave infilling.

166 The cave infills at Sterkfontein contain one of the richest

167 Kaldar Cave is a key archaeological site that provides evidence

168 Kaldar Cave is the first well-stratified Late Palaeolithic loca

169 ing, at the Lower Palaeolithic site of Qesem Cave (Israel).

170 al other Neolithic sites, and in Nahal Hemar cave (Israel, ca. 8200 -7300 cal.

171 of the mutation patterns that arise through CAVE iterations elucidates the manner in which specific

172 alcite and aragonite stalagmite samples from cave KNI-51 in the Australian tropics.

173 ed environments (landscape-like surfaces and cave-like interiors).

174 omly wrinkled morphology, mesoscale void- or cave-like pockets, high-exposed surface coverage sites,

175 Caveolae, the cave-like structures abundant in endothelial cells (ECs)

176 gusts similarly well in forest-, lake-, and cave-like visual environments.

177 alyse 31 mitochondrial genome sequences from cave lion individuals that, through a combination of (14

178 The cave lion is an extinct felid that was widespread across

179 ocally monophyletic mitogenome clades in the cave lion, and an additional third distinct lineage repr

180 ted the mitochondrial DNA divergence between cave lions and lions to be 1.85 Million ya (95% 0.52- 2.

181 ese results support previous hypotheses that cave lions existed as at least two subspecies during the

182 s during the Pleistocene, and that lions and cave lions were distinct species.

183 ous observations that Beringian and European cave lions were morphologically distinct.

184 rbonate deposits (speleothems) in a Siberian cave located at the southern edge of continuous permafro

185 y Aurignacian ones at the site of Bajondillo Cave (Malaga, southern Spain) is reported.

186 eleothem climate proxies such as delta(18)O, cave microecology and the use of heat as a tracer in kar

187 eus specimens recovered in Level 4 from Toll Cave (Moia, Catalonia, NE Iberian Peninsula).

188 lete reproductive failure in darkness, while cave molly females were not similarly affected in any tr

189 brate immune system, by comparing river with cave morphotypes.

190 were longer and more branched, while in both cave morphs the ventral dendrites were smaller or absent

191 ling morph and multiple populations of blind cave morphs.

192 atufian graves at the burial site of Raqefet Cave, Mt. Carmel, Israel.

193 4 CE, when a fire burned vegetation over the cave; n-alkanes were detected in all samples in the rang

194 gen isotope (delta(18)O) records from Shihua Cave, North China to reconstruct the EASM variability ov

195 h well-developed annual lamina from Xinglong Cave, northern China, covering DO 15 and 14.

196 oxygen isotope (delta(18)O) data from Bittoo cave, Northern India to reconstruct ISM variability over

197 As a result, cave-obligate taxa, termed troglobionts, are no longer v

198 The Cave of Giant Crystals in the Naica mine (Mexico) is one

199 roids from the late Acheulean (Bed 3) at the Cave of Hearths, South Africa afford being thrown so as

200 heavy metals in four renowned archaeological caves of the Iberian Peninsula spanning the last million

201 Caves offer selective pressures that are distinct from t

202 e complete history of the Chauvet-Pont d'Arc Cave on an absolute timescale.

203 DNA found with extinct fauna in a submerged cave on Mexico's Yucatan Peninsula.

204 m oxygen isotope (delta(18)O) records from a cave on the Atlantic coastline of northern Iberia, cover

205 , based on data from 163 drip sites, from 39 caves on five continents, showing that drip water delta(

206 ung subterranean insect lineage in lava tube caves on Hawai'i Island.

207 wo distinct periods of human activity in the cave, one from 37 to 33,500 y ago, and the other from 31

208 es, coming from the adjacent slope above the cave or the cave entry, as the palaeogeography and sedim

209 drial DNA from Minoan osseous remains from a cave ossuary in the Lassithi plateau of Crete dated 4,40

210 ead of Us") recovered from the On Your Knees Cave (OYKC) in southeastern Alaska (archaeological site

211 nd also introgressed into the ancient Pachon cave population.

212 Furthermore, these cave populations are natural replicates that can be used

213 tic analysis demonstrates that two different cave populations have evolved similar feeding postures t

214 The allele appears to be fixed in cave populations in which the overeating phenotype is pr

215 erence in metabolic rate between surface and cave populations of an amphipod.

216 school, while several, independently derived cave populations of the same species have lost schooling

217 rategies differs among independently derived cave populations.

218 darkness, and in two independent lineages of cave populations.

219 nections, extreme genetic divergence between cave populations.

220 that hominins preserved in the Sterkfontein Caves practiced two different locomotor repertoires.

221 Mines and caves provide essential roosting places for bats, but of

222 hagus hatchi, each from four closely located caves (ranging from 3 to 13 km apart) in the cave-rich s

223 Nevertheless, shifts in the White Moon Cave record that are synchronous within age uncertaintie

224 We find that, as compared with cave records from the western edge of the lowlands, the

225 e ancient drawings in the Chauvet-Pont d'Arc Cave revealed ages much older than expected.

226 caves (ranging from 3 to 13 km apart) in the cave-rich southern Cumberland Plateau of Tennessee, USA.

227 0 fragmented bones from the site of Denisova Cave, Russia, in order to facilitate the discovery of hu

228 nrichment of mitochondrial DNA, we show that cave sediments represent a rich source of ancient mammal

229 The cave bears from Toll Cave show a microwear pattern like that of extant bears

230 cent speleothem data collected from regional caves showed that persistent episodes of unusually low r

231 ther with the former, the Gibraltar Vanguard Cave, shows Zn and Cu pollution ubiquitous across highly

232 emus, all isopod crustaceans tested, and the cave shrimp Troglocaris anophthalmus did not melanize wo

233 The ancestors of these cave shrimps are believed to have inhabited the ancient

234 Cave shrimps from the genera Typhlatya, Stygiocaris and

235 Cave shrimps of the Typhlatya genus are common and wides

236 rom the lithic assemblage of the Guanyindong Cave site in southwest China, dated to approximately 170

237 using a set of 69 stones excavated from the cave site of Liang Bua (Flores, Indonesia).

238 speleothems indicates that permafrost at the cave site was absent at that time, becoming more frequen

239 y of the late Neandertals and UPMHs from the cave sites of the Troisieme caverne of Goyet and Spy in

240 the local hydroclimatic variability at both cave sites, inferred from carbon isotope and trace eleme

241 diagnostic fossil remains were found only at cave sites.

242 n archaeological assemblage from Chagyrskaya Cave, situated in the Altai foothills, where around 90,0

243 the Dinaledi Chamber within the Rising Star cave, South Africa, which contains the fossils of Homo n

244 (ITCZ) rainfall proxy records from Yok Balum Cave, southern Belize.

245 rania (Apidima 1 and Apidima 2) from Apidima Cave, southern Greece, were discovered in the late 1970s

246 speleothem oxygen isotope record from Dongge Cave, southwest China during the past 4.2 thousand years

247 This study has revealed distinct use of the cave space by Neanderthals and carnivores.

248 d in the diet of Neanderthals from El Sidron cave, Spain, and dietary components of mushrooms, pine n

249 pod lineages, ii) is retained in most albino cave species, and iii) has been lost several times durin

250 al-resolution oxygen isotope data from Soreq Cave speleothems suggest that summer monsoon rainfall pe

251 oratory experiments focusing on the European cave spider Meta menardi (Araneae, Tetragnathidae) and a

252 alyses of the sequence data from the Melouri Cave stalagmite revealed potential contamination and low

253 Surprisingly, deeper parts of caves still contained NIR, an effect likely attributable

254 delta(66)Zn values in fossil enamel from THM cave suggest an excellent long-term preservation potenti

255 The Rising Star cave system has produced abundant fossil hominin remains

256 cord based on five stalagmites from the same cave system in northwest Scotland, where precipitation i

257 More than 1500 fossils from the Rising Star cave system in South Africa have been assigned to a new

258 the Dinaledi Chamber within the Rising Star cave system, and represents a second depositional contex

259 ating of fossil remains from the Rising Star cave system, Cradle of Humankind, South Africa, have str

260 thin the Dinaledi Chamber of the Rising Star cave system, Cradle of Humankind, South Africa.

261 t hominin was recovered from the Rising Star cave system, South Africa.

262 within the photic zones of four terrestrial cave systems in concert with a detailed investigation of

263 ng those microbial ecosystems located within cave systems.

264 rivers and derived blind forms are found in cave systems.

265 ising surface fish under conditions found in caves taxes the HSP90 system, unmasking the same phenoty

266 In 2012, a new exploration of San Marcos cave (Tehuacan, Mexico) yielded nonmanipulated maize spe

267 rchaeological evidence for the dating of the cave temple paintings, narrowing it down to the late twe

268 oad, consists of 492 richly painted Buddhist cave temples dating from the fourth to fourteenth centur

269 we present an ancient DNA record from Hall's Cave, Texas, that documents 100 vertebrate and 45 plant

270 ross-hatching carved into the bedrock of the cave that has remained covered by an undisturbed archaeo

271 e microbial ecosystems within anthropogenic 'caves'; the Iron-Age, subterranean tombs of central Ital

272 tantric Buddhist style, and like many other caves, the date of its construction is still under debat

273 welling surface fish became entrapped in the caves, they were confronted with dramatic changes in the

274 3 cm-long gypsum stalactite from Sima Blanca Cave to reconstruct the climate history of SE Spain from

275 s in a subaqueous speleothem from an Italian cave track regional sea-surface temperatures over the la

276 e likely masticated and thus consumed in the cave under the paintings.

277 Cave bears also took refuge in the cave until 33,000 y ago.

278 pear to be consequences of bat migration, as cave use transitioned from summer maternity roost to aut

279 degrees of flaking were scanned in the 126th cave using a near-infrared (NIR) hyperspectral camera wi

280 's hydroclimate variability from Tonnel'naya cave, Uzbekistan, and Kesang cave, western China.

281 idered in these reconstructions, even though cave ventilation could bias speleothem growth toward the

282 is sensitivity may be enhanced by dry season cave ventilation.

283 phases of HIV viral transfer to T cells via cave/vesicular trafficking and de novo replication were

284 urposely made painted or engraved designs on cave walls--a means of recording and transmitting symbol

285 ific wavelengths by the surface materials of cave walls.

286 rein that the earliest maize from San Marcos cave was a partial domesticate diverging from the landra

287 a Californian rock art site called Pinwheel Cave was discovered alongside fibrous quids in the same

288 The use of CAVE was key to the observation of a nonrandom distribut

289 This small cave was used as storage for paraphernalia in the semi-a

290 ated from the recently discovered Herrenberg Cave, was investigated during its lifecycle by means of

291 In Denisova Cave, we retrieved Denisovan DNA in a Middle Pleistocene

292 and duration of bat activity outside of the cave were correlated with passage of cold fronts over th

293 rtial calvaria, recently discovered at Manot Cave (Western Galilee, Israel) and dated to 54.7 +/- 5.5

294 logical sites of Hayonim and Hilazon Tachtit Caves (western Galilee, Israel).

295 rom Tonnel'naya cave, Uzbekistan, and Kesang cave, western China.

296 orm, chemically accelerated viral evolution (CAVE), which provides an effective and robust method for

297 Lida Ajer is a Sumatran Pleistocene cave with a rich rainforest fauna associated with fossil

298 Adaptation to life in nutrient poor caves without predation includes the evolution of enhanc

299 and the recently discovered non-luminescent cave worm Neoditomiya sp as the main source of luciferin

300 und on the Tibetan Plateau in Baishiya Karst Cave, Xiahe, Gansu, China.