ライフサイエンスコーパス: cave

1 -resolution speleothem records from the same cave.

2 black stains that progressively invaded the cave.

3 lved in cutting meat from the bones at Qesem Cave.

4 nerve root exit zone in the pons to Meckel's cave.

5 e oldest ornament-bearing levels in Ucagizli Cave.

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

7 nthropological evolution associated with the cave.

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

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

10 full interglacial conditions in all studied caves.

11 perhaps Neandertals also engaged in painting caves.

12 mples collected from karst springs, wells or caves.

13 adapted to life in the perpetual darkness of caves.

14 neys at hydrothermal vents to soda straws in caves.

15 emical environment when they began to occupy caves.

16 ve (6.0 to 5.7 Ma), and three other hypogene caves (11.3 to 6.0 Ma) in the Guadalupe Mountains of New

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

18 NA sequence variation to identify roots from caves 5-65 m deep.

19 rs ago (Ma)], the upper level of Lechuguilla Cave (6.0 to 5.7 Ma), and three other hypogene caves (11

20 a different depositional environment: Hinds Cave (~8000 years B.P.) in the southern United States, C

21 wild cattle and tortoises at Hilazon Tachtit cave, a Late Epipaleolithic (12,000 calibrated years B.P

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

23 ng the reduction of eyes and pigmentation in cave-adapted animals are unknown; Darwin famously questi

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

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

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

27 he study of parallelism and the evolution of cave-adapted traits.

28 characters, which are random with respect to cave age and geographic distribution.

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

30 ratures which deviate significantly from the cave air temperature.

31 Cave alleles at every eye or lens QTL we detected caused

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

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

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

35 using the Zerner's INDO/S, together with the Cave and Newton methods.

36 Analysis using Cave and Newton's generalized Mulliken-Hush theory relat

37 delayed until the food could be moved to the cave and processed with the aid of blade cutting tools a

38 30,000-22,000 y ago at Leang Bulu Bettue, a cave and rock-shelter site on the Wallacean island of Su

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

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

41 ed in four separate crosses between surface, cave, and hybrid forms of A. mexicanus.

42 ocation of the feasting activity in a burial cave, and the manufacture of two structures for burial a

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

44 How cave animals adapt to life in darkness is a poorly under

45 Cave animals are one group with immense potential to add

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

47 ed multiple times in a diverse assemblage of cave animals.

48 icance in studies of regressive evolution in cave animals.

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

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

51 Paleolithic cave art is an exceptional archive of early human symbol

52 These minimum ages reveal either that cave art was a part of the cultural repertoire of the fi

53 Early cave artists recorded distinct morphological forms consi

54 lysis of coprolites recovered from an Oregon cave as evidence for a human presence in North America b

55 the cavity entrance prohibited access to the cave at least 21 ka ago.

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

57 whereas some others prefer to bind to a wide cave at the other end.

58 In the northernmost cave (at 60 degrees N), no growth has occurred since Mar

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

62 Comparison of cave bear and modern bear sequences revealed the evoluti

63 PCR amplification of 47,000-60,000-year-old cave bear DNA, these outperformed Taq DNA polymerase by

64 bear inserts, yielding 26,861 base pairs of cave bear genome sequence.

65 tamination, 5.8 and 1.1% of clones contained cave bear inserts, yielding 26,861 base pairs of cave be

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

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

68 age to all Western European Late Pleistocene cave bears.

69 letal remains of two 40,000-year-old extinct cave bears.

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

71 skeletons from Shanidar Cave, Iraq, and Spy Cave, Belgium.

72 ecord for the past 2000 years from Yok Balum Cave, Belize.

73 ove-binders competed against each other, but cave-binders did not compete against groove-binders, alt

74 c materials in the western half of Coxcatlan Cave, but they also indicate that the eastern half of th

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

76 A tooth found in Denisova Cave carries a mitochondrial genome highly similar to th

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

78 nce of eyed surface (surface fish) and blind cave (cavefish) dwelling forms in Astyanax also provides

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

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

81 n isotope records of stalagmites from Sanbao Cave, China, characterize Asian Monsoon (AM) precipitati

82 eistocene vertebrate sequence from Porcupine Cave, Colorado, which records at least 127 species and t

83 the Indian subcontinent from the Billasurgam cave complex.

84 halamus viridescens), in schistosomes and in cave crickets (Dolichopoda species).

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

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

87 s the earliest documented domesticate in the cave, dating to 7,920 calibrated calendrical (cal) years

88 ll-brained hominin found in Late Pleistocene cave deposits on the island of Flores, Indonesia were as

89 an (c. 310 million yr before present (MyBP)) cave deposits.

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

91 lant remains--that burning took place in the cave during the early Acheulean occupation, approximatel

92 t of the surface-dwelling (surface fish) and cave-dwelling (cavefish) forms of Astyanax.

93 ed surface-dwelling (surface fish) and blind cave-dwelling (cavefish) forms.

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

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

96 elling form (surface fish) and various blind cave-dwelling forms (cavefish) [2-4].

97 surface dwelling form and many con-specific cave-dwelling forms, some of which have evolved their re

98 leost with eyed surface-dwelling and eyeless cave-dwelling forms.

99 All cockroaches, with the exception of one cave-dwelling genus, harbor endosymbiotic bacteria, Blat

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

101 Since its discovery, the Chauvet cave elaborate artwork called into question our understa

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

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

104 volutionary forces driving adaptation to the cave environment.

105 ently high for eyes to be detrimental in the cave environment.

106 A hallmark of cave environments is scarcity of food.

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

108 is to develop an invertebrate model to study cave evolution so that, in combination with a previously

109 demonstrate that the tradition of decorating caves extends back at least to the Early Aurignacian per

110 elected visual pigments: the LWS pigments of cave fish (Astyanax fasciatus), frog (Xenopus laevis), c

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

112 Eye formation is initiated in cave fish embryos, but the eye subsequently arrests and

113 tic cup, restoring optic tissues lost during cave fish evolution.

114 ductive signal from the lens are involved in cave fish eye degeneration.

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

116 ransplantation of a surface fish lens into a cave fish optic cup or lens extirpation.

117 d development after transplantation into the cave fish optic cup, restoring optic tissues lost during

118 human (Homo sapiens);and the MWS pigments of cave fish, gecko (Gekko gekko), mouse (Mus musculus), sq

119 ythms in Caenorhabditis elegans and in blind cave fish.

120 st a role for selection in the regression of cave-fish eyes cited the insignificant cost of their dev

121 the role of natural selection in eye loss in cave fishes: "As it is difficult to imagine that eyes, a

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

123 Cave floor chiseling to accommodate the desired grave lo

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

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

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

127 -dwelling form (surface fish) and many blind cave forms (cavefish), to study the evolution of eye deg

128 Surface and cave forms are interfertile making this system amenable

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

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

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

132 g of fine-grained alunite that formed during cave genesis provides ages of formation for the Big Room

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

134 trate that the cliff overhanging the Chauvet cave has collapsed several times since 29 ka until the s

135 Analyses of surface x cave hybrids show that the alleles for reduced sleep in

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

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

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

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

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

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

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

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

144 The Lascaux Cave in France suffered an outbreak of the fungus Fusari

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

146 produced by late Neanderthals, from Gorham's Cave in Gibraltar: first, generally accepted estimates o

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

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

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

150 tracted from a finger bone found in Denisova Cave in southern Siberia, we have sequenced the genome o

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

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

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

154 6,000-year-old barley grains excavated at a cave in the Judean Desert close to the Dead Sea.

155 thal populations, recovered from Mezmaiskaya Cave in the northern Caucasus.

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

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

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

159 The Paisley Caves in Oregon record the oldest directly dated human r

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

161 xpansion and infection of most counties with caves in the contiguous United States by winter 2105-210

162 cies seen by using mammography are cutaneous caves in the underside of the dermis into which insert c

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

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

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

166 sits overlying or underlying art found in 11 caves, including the United Nations Educational, Scienti

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

168 ontroversial owing to the complex history of cave infilling.

169 The cave infills at Sterkfontein contain one of the richest

170 culus of Neanderthal skeletons from Shanidar Cave, Iraq, and Spy Cave, Belgium.

171 Kaldar Cave is a key archaeological site that provides evidence

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

173 ge in ecological conditions, from surface to cave, is correlated with a dramatic reduction in sleep i

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

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

176 Zooarchaeological research at Qesem Cave, Israel demonstrates that large-game hunting was a

177 t within the tricuspid annulus-inferior vena cave isthmus (IS) and either side of the crista terminal

178 Data from Border Cave (KwaZulu-Natal) show a strong pattern of technologi

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

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

181 d Astyanax cavefish collected from the Micos cave locality in 1970, in which albinism appeared over t

182 We found that cave mammillaries (water table indicator speleothems) fr

183 d to the anthropogenic changes introduced by cave management.

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

185 hat reservoir hosts of Marburg virus inhabit caves, mines, or similar habitats.

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

187 antibody topography classes are as follows: cave (mostly hapten binders), crater (mostly protein and

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

189 a trend for lower oxidation in samples from cave myotis bats (Myotis velifer) relative to mice.

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

191 f intact sediments at the site of Wonderwerk Cave, Northern Cape province, South Africa, provide unam

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

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

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

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

196 Native American coprolites found in the dry caves of Nevada, we showed that the sterol nucleus was s

197 Columnar stalagmites in caves of the Guadalupe Mountains during the late Holocen

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

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

200 species that occupied Liang Bua, a limestone cave on Flores in eastern Indonesia, during the Late Ple

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

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

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

204 Using speleothem encrustations from coastal caves on the island of Mallorca, we determined that west

205 dence has come mostly from deeply stratified caves on the south (Indian Ocean) coast.

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

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

208 due to their lightless spatial niches (e.g., caves or soil).

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 upancy, this study confirms that the Chauvet cave paintings are the oldest and the most elaborate eve

212 y elements of San material culture at Border Cave, places the emergence of modern hunter-gatherer ada

213 Moreover, Hawaiian cave planthoppers exhibit one of the highest speciation

214 nd also introgressed into the ancient Pachon cave population.

215 ntified in the geographically distant Pachon cave population.

216 s for reduced sleep in the Pachon and Tinaja cave populations are dominant in effect to the surface a

217 The cave populations are largely independent in their origin

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

219 geographically and phylogenetically distinct cave populations can evolve the same troglomorphic pheno

220 Thus, the two cave populations evolved albinism independently, through

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

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

223 tion in sleep in three independently derived cave populations of A. mexicanus.

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

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

226 adian rhythms in per1, which are retained in cave populations, but with substantial alterations.

227 xicanus, has eyed surface and numerous blind cave populations.

228 d to Oca2, a known pigmentation gene, in two cave populations.

229 rategies differs among independently derived cave populations.

230 0-year-old fallow deer assemblages from this cave provide early examples of prime-age-focused ungulat

231 ng of the cucurbit assemblage from Coxcatlan Cave provide information on the timing and sequence of t

232 The results from Qesem Cave raise new hypotheses about possible differences in

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

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

235 Correlations with cave records support the hypothesis that the Dole effect

236 species that has, in a series of independent caves, repeatedly evolved specialized characteristics ad

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

238 0 fragmented bones from the site of Denisova Cave, Russia, in order to facilitate the discovery of hu

239 evident by 2007 that they became one of the cave's major problems.

240 The data from the Hinds Cave samples largely represented unknown sources.

241 st, coprolite, peat extract, clay-rich soil, cave sediment and tar.

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

243 visible to the naked eye) in archaeological cave sequences.

244 mens and modern samples collected near Lamar Cave share mitochondrial cytochrome b sequences that are

245 Bones deposited in caves show that, before the arrival of humans, at least

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

247 However, data from Chica Cave shows complete repression of clock function, while

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

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

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

251 Cave shrimps from the genera Typhlatya, Stygiocaris and

252 Arbor3D can be displayed in "CAVE simulator" mode on an SGI workstation screen, or as

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

254 diagnostic fossil remains were found only at cave sites.

255 Sterkfontein cave, South Africa, has yielded an australopith skeleton

256 reanalysis of organic artifacts from Border Cave, South Africa, shows that the Early Later Stone Age

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

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

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

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

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

262 involved in the development and evolution of cave-specific traits in A. mexicanus.

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

264 . cooperii/gundlachii; flicker Colaptes sp.; Cave Swallow, Petrochelidon fulva; and Eastern Meadowlar

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

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

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

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

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

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

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

272 ion with a previously established vertebrate cave system, we can address genetic questions concerning

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

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

275 ionarily derived morphologies in the Mexican cave tetra, a species that has, in a series of independe

276 e and pigmentation regression in the Mexican cave tetra, Astyanax mexicanus, by mapping and quantitat

277 The blind Mexican cave tetra, Astyanax mexicanus, is a unique model system

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

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

280 ed on the northern Levantine coast, Ucagizli Cave (Turkey) and Ksar 'Akil (Lebanon) have yielded nume

281 Our analysis shows that: (i) at Border Cave two assemblages, dated to 45-49 and >49 ka, show a

282 Excavations at Guila Naquitz and Silvia's Cave, two dry rockshelters near Mitla, Oaxaca, Mexico, y

283 or-site symmetry, in the context of a Newton-Cave type analysis, to establish the relative importance

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

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

286 he Early Later Stone Age inhabitants of this cave used notched bones for notational purposes, wooden

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

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

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

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

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

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

293 y also indicate that the eastern half of the cave was largely undisturbed.

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

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

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

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

298 Roots from caves were identified by comparing their DNA sequences f

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

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

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

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