ライフサイエンスコーパス: present-day

1 ent storage from the late Pleistocene to the present day.

2 o-biology of odors remains unclear up to the present day.

3 y narrow circumtropical distributions in the present day.

4 ears ago, and between ~100 years ago and the present day.

5 om the point of genome duplication until the present day.

6 ing with initial applications through to the present day.

7 height of the last glaciation through to the present day.

8 r medical students and many others up to the present day.

9 n from the earliest LP (~130,000 ybp) to the present day.

10 rations of an extent similar to those of the present day.

11 chanisms that continue to be explored to the present day.

12 y-Holocene that were at least as warm as the present-day.

13 of the sites could be exposed annually to a present-day 100-year ESL event by 2050.

14 nds face a MSL rise by 2100 that exceeds the present-day 100-year event level.

15 cially important deep-sea fish species under present-day (1951-2000) environmental conditions and to

16 Further, we find that the present-day 50-year extreme water level (i.e., 2% annual

17 Looking even farther into the future, the present-day 50-year extreme water level will be exceeded

18 From their discovery to the present day, a major challenge faced by chemists has bee

19 ants that are equally acceptable compared to present-day aerosol observations.

20 Present-day African ecosystems serve as referential mode

21 We co-analyse these data with data from present-day Alaskan Inupiat and West Siberian population

22 de new strategies to overcome the pitfall of present day albumin detection methods as well as acceler

23 pre-Columbian tree domestication has shaped present-day Amazonian forest composition.

24 h large future aerosol emissions, similar to present day amounts, GHG emissions need to be reduced 8%

25 ical release' from its inception through the present day and find that current definitions are broad

26 studies shed light on how we arrived at the present day and help us search for sustainable trajector

27 ng-term dietary time series from 1890 to the present day and show that a significant dietary shift oc

28 e lifetime of such a subsurface ocean to the present day and to maintain ocean uplift, a rigid, condu

29 ditioned on the number of species sampled at present day and, in some cases, a specific time interval

30 We find that he is more related to present-day and ancient Asians than he is to Europeans,

31 viduals fall within the genetic diversity of present-day and ancient Polynesians, and we can reject t

32 studies of their atmospheric properties with present-day and future astronomical facilities.

33 ors of the above vector-borne diseases under present-day and future climates.

34 with the diatom Thalassiosira hyalina under present-day and future temperature and pCO(2) treatments

35 daptive algorithm for exact simulations with present-day and near-term quantum hardware.

36 n order of magnitude larger than that of the present day, and could have cooled the global climate by

37 ctly bimodal from the Neoarchaean era to the present day, and the average metamorphic T/P has decreas

38 This emission is ~10% and ~28% of present-day, annual natural and petroleum-industry metha

39 rovide valuable insights into the impacts of present-day anthropogenic climate change.

40 about one-third of the deposition caused by present-day anthropogenic emissions.

41 ondrial genomes of 52 ancient skeletons from present-day Armenia and Artsakh spanning 7,800 years and

42 ow that nearly all nucleation throughout the present-day atmosphere involves ammonia or biogenic orga

43 bly affect climate through nucleation in the present-day atmosphere.

44 logical past is of societal interest because present-day atmospheric CO2 concentrations have reached

45 Our approach predicts a present-day average crustal thickness of 40 +/- 25 kilom

46 d waters of this magnitude on a planet whose present-day average temperature is - 60 degrees C was th

47 xome sequence data from a diversity panel of present-day barley accessions showed the close affinity

48 o-European-speaking ones, and we reveal that present-day Basques are best described as a typical Iron

49 esults from two tidal simulations, using the present-day bathymetry and a palaeo-bathymetry.

50 abundant and phosphate-rich relative to the present day because of the lack of microbial phosphate s

51 The theory also informs present-day biases in a set of ESM simulations as well a

52 anding the forces shaping global patterns of present-day biodiversity and its response to ongoing and

53 extent deep-time dispersal limitation shapes present-day biodiversity at broad spatial scales remains

54 trast to a 0% difference implemented in most present-day biosphere emissions models (i.e., homogeneou

55 an substantially depart from census sizes of present-day breeding populations (N(C)) as a result of p

56 nderthal substitutions are found in ~0.4% of present-day Britons, where they are associated with heig

57 n concentrations are similar to those in the present-day bulk silicate Earth.

58 fluences, in particular, explain much of the present-day cancer risk across life, including in humans

59 e products is considered the "holy grail" of present-day cancer therapy, and recent discoveries of sm

60 This paper explores present-day cardiovascular competency components, assess

61 vial river types and quantification of their present-day catchment hydroclimates enables identificati

62 provide ways to jointly analyze the role of present-day climate and landscape configuration in curre

63 ous climate changes is essential for testing present-day climate models and projections.

64 Although most research has focused on present-day climate, a growing body of evidence indicate

65 st Asia will experience more TCs than in the present-day climate.

66 The present-day clinical practice of concentrating on the st

67 Present day coalescent simulations do not scale well, or

68 ased on trajectory backtracking, we identify present-day coastal retention, dominant flow and dispers

69 ld birch tar-hafted flint tool found off the present-day coastline of The Netherlands.

70 ely related to the indigenous inhabitants of present-day Colombia.

71 , plant-specific functions, resulting in the present-day complexity of the plant SBT family.

72 edicted to occur in 2050 and 2100 than under present-day conditions, (ii) that two macroalgae damage

73 gnificant impact when the climate is held at present-day conditions.

74 account for the observed differentiation of present-day continental Southern Balkan groups.

75 only one of several possibilities into which present-day coral reefs can transition.

76 ntrainment of melts in the mantle and in the present-day core-mantle boundary.

77 Model (HYCOM) spanning 2004-2012 represented present-day currents.

78 es of hydrogen prevailing on early Earth and present day deep-sea volcanoes, the potential for the F4

79 We introduce a model that shows that present-day delta morphology varies across a continuum b

80 arly, SMRs were calculated in parents of 128 present-day dilated cardiomyopathy probands with TTNtv u

81 ational scientific conferences exemplifies a present-day discussion topic usually occurring without f

82 The present-day distribution of velvet worms corresponds nea

83 Present day distributions of Encope are likely the resul

84 Their present-day diversity is the result of an evolutionary p

85 However, despite their extraordinary present-day diversity, our understanding of early passer

86 20 million years, the group declined to its present-day diversity.

87 These individuals result in 4.2 present-day donors (95% CI, 2.5-6.6) at a cost of US $72

88 Two possible present-day 'dormant' descendants of this population of

89 ), on top of a factor 1.7-2.8 increase above present-day due to socioeconomic developments.

90 total atmospheric mass comparable to that of present day Earth even at large distances ( 1 kiloparsec

91 The present-day Earth atmosphere contains 22 +/- 5% cometary

92 On present-day Earth, dust emissions are restricted only to

93 resent), and analyse them with data from 778 present-day East Asians and Oceanians.

94 le alleles associated with LP in ancient and present-day eastern African populations, the contexts fo

95 portance of deep phylogeny for understanding present-day ecological interactions.

96 We created a present-day ecological niche model (ENM) for C. picta an

97 is, even for residents of census tracts with present-day economic and racial privilege, whereas the b

98 rmalization schemes based on calculations of present-day economic damage.

99 ared more ancestry with Near Easterners than present-day Egyptians, who received additional sub-Sahar

100 but also in their kinematics, to evolve into present-day elliptical galaxies.

101 but that period is an imperfect analogue for present-day emissions owing to the large terrestrial ice

102 t time at global scale, the uncertainties in present-day ESL estimates, which have by default been ig

103 xplicit climate mitigation begins before the present day, estimating the total costs to date of delay

104 sourced to a region that encompasses much of present-day Ethiopia, Eritrea, and Djibouti, and portion

105 Present day eukaryotes employ at least two main defence

106 ns [4, 5] while others did not contribute to present-day Eurasian populations [3, 6].

107 e of these individuals have relationships to present-day Europeans [4, 5] while others did not contri

108 nly ~1-10 cm in areas with a narrow range of present-day extreme water levels can double the odds of

109 t changes to coastal flooding regimes (where present-day, extreme-but-rare events become common), whi

110 tionation trends that can be used to connect present-day fallout composition to past fireball composi

111 n during the first post-transplant year in a present-day, five-center lung transplant cohort.Methods:

112 The exceptional nature of the present-day flood-rich period calls for process-based to

113 r acceptance of brain death continues to the present day, focusing on the following: (1) what the Asi

114 osits are investigated with reference to the present-day foreshore of Annagh Head, NW Ireland, and th

115 sess the contribution of these activities to present-day forest structure and composition.

116 y, so we focus on the committed warming from present-day fossil fuel assets.

117 sent genetic landscape, but the territory of present-day France has yet to be connected to the broade

118 f interest of 243 individuals sampled across present-day France over a period spanning 7,000 y, compl

119 Present-day galaxies are surrounded by cool and enriched

120 are probably the progenitors of the largest present-day galaxies in massive groups and clusters.

121 ancestor 2 billion years ago, and while many present-day genes in these lineages predate this diverge

122 s of markers indicated a good concordance of present-day genetic structure with the reported history

123 way that could not be resolved by analyzing present-day genomes alone.

124 SNV archives 265 million SNVs across 220,147 present-day genomes and 1018 ancient genomes, including

125 crust-uppermost mantle structure supports a present-day geodynamics with a predominant Africa-Eurasi

126 , the DGIM is the largest medical society in present-day Germany.

127 sive production contributes significantly to present-day global anthropogenic CO(2) emissions, yet it

128 far, and its progenitor is distinct from the present-day globular cluster population in the local Uni

129 Future projections show that many present-day greater bamboo lemur populations will experi

130 The present-day grounding zones of the Pine Island and Thwai

131 ssure of carbon dioxide (pCO(2)) ranged from present-day (>400 parts per million volume, ppmv) to pre

132 Parsi DNA samples excavated from Sanjan, in present day Gujarat, the place of their original settlem

133 cosmological simulation of the formation of present-day haloes over the full range of observed halo

134 tomography (PET) is an important driver for present day healthcare.

135 Global climate models demonstrate that the present-day hemispheric contrast in cloud droplet number

136 hropogenic Hg emissions contribute 20-25% to present-day Hg deposition, and roughly two-thirds of pri

137 In present-day high-performance electronic components, the

138 The exons and exon-intron junctions of present day higher plant's Rca, which is conserved in mo

139 f the Sutlej River, the third largest of the present-day Himalayan rivers.

140 The presence of present-day human contaminating DNA fragments is one of

141 sed maximum likelihood method for estimating present-day human contamination in low-depth sequencing

142 cestries that delineate genetic structure of present-day human populations.

143 Denisovan source populations contributing to present-day human populations.

144 nts of Denisovan and Neanderthal ancestry in present-day humans and applied them to 257 high-coverage

145 aleolithic populations in Eastern Eurasia to present-day humans and their relationship to other early

146 While present-day humans are not strongly differentiated, vast

147 Some present-day humans derive up to approximately 5% [1] of

148 Neandertals that mixed with the ancestors of present-day humans living outside of sub-Saharan Africa

149 Present-day humans outside Africa descend mainly from a

150 measured DNA methylation maps of ancient and present-day humans, as well as of six chimpanzees, to de

151 20% more Neandertal DNA to be identified in present-day humans, including variants involved in low-d

152 een the two copies of her genome, fewer than present-day humans, suggesting that Neandertal populatio

153 7] to study his relationship to ancient and present-day humans.

154 o modern humans, interbred with ancestors of present-day humans.

155 Present-day hunter-gatherers (HGs) live in multilevel so

156 our individuals are most similar to those of present-day hunter-gatherers from western Central Africa

157 ls, the loss of more than 70 per cent of the present-day ice volume is triggered, mainly caused by th

158 ervation and occasional serendipity, and the present-day immunologists and surgeons exploring immune

159 res differing dramatically from those of the present day, implying that modern communities may not be

160 N by ~2 per mille between the 1890s and the present day, indicating that birds changed their diets m

161 ic evidence for Native American admixture in present-day indigenous inhabitants of Rapa Nui [5-8].

162 ance of archaic hominin DNA that persists in present-day individuals.

163 We find that present-day inner Eurasian populations are structured in

164 ditions on animals, yet understanding of the present-day interactive effects of multiple stressors re

165 The transition from the last ice age to the present-day interglacial was interrupted by the Younger

166 d around 1,000 years ago by ancestors of the present-day Inuit and Yup'ik(1-3).

167 ligions in the world, originating in Persia (present-day Iran) during the second millennium BCE.

168 share the highest number of haplotypes with present-day Iranians and we estimate that the admixture

169 d changes in daytime summer temperatures and present-day irrigation extent.

170 asymmetric oxidation catalysis (1970 to the present day) is covered; both transition-metal-based and

171 ixed and super-endemism, which suggests that present-day island biodiversity has frequently been shap

172 By comparing genetic patterns in the present-day Kuba, whose ancestors were part of the Kuba

173 Using an agent-based model, grounded on the present day landscape, we show that groundwater availabi

174 We show that present-day Lebanese derive most of their ancestry from

175 e locals (genetically indistinguishable from present-day Lebanese), and two individuals were a mixtur

176 sequenced the genomes of 99 individuals from present-day Lebanon to catalog modern Levantine genetic

177 bjects implies that O(2) must have been near present-day levels (~21%) within the altitude range wher

178 equatorial sea surface temperatures fell to present-day levels during the Middle Ordovician Darriwil

179 egained even if temperatures are reversed to present-day levels.

180 d rotational torques can explain the basin's present-day location, but requires the feature to be a p

181 e that this transport of water dominates the present-day loss of atomic hydrogen to space and influen

182 , and pH-values categorized as equivalent to present day (<=400 uatm pCO(2), pH > 7.89) and future (>

183 sovan admixture event(s) that contributed to present-day mainland Asians but are distinct from the De

184 deling, which incorporates tomography-based, present-day mantle heterogeneity to reconstruct mantle s

185 higher and lower (+/-20 ppm) values than the present-day mantle, demonstrating major silicate Earth d

186 globally, and particularly in regions at the present-day margins of habitat suitability such as the c

187 The present-day marine nitrogen (N) cycle is strongly regula

188 emonstrate that the abrasion of basalt under present day Martian rates of aeolian erosion is highly u

189 when evaluating the formation of recent and present-day martian mass wasting features, as much less

190 tion of past water mass exchange between the present day Mediterranean Sea and Indian Ocean via the M

191 ably as well as prediction markets, the best present-day method for predicting replicability.

192 Unfortunately, present-day methods for probing the performance of third

193 s associated with extracting palladium using present-day mining processes.

194 Present day mitochondria and plastids (chloroplasts) evo

195 lation of the Iceman s maternal lineage with present-day mitochondrial variation remains elusive.

196 Furthermore, present-day models compared to the near future (2038), s

197 In particular, it is unclear whether the present day 'modern' morphology rapidly emerged approxim

198 higher eastern Eurasian ancestry, resembling present-day Mongolic-speaking populations.

199 is on or after January 1, 2011, to represent present day monitoring and costs associated with AMD.

200 ion-related disease conditions that dominate present-day morbidity and mortality.

201 nturies, with global impacts reaching to the present day, more than a century and a half after slaver

202 The ancestry of present-day Moroccans is unknown and may be substantiall

203 ittle evidence of gene flow from European or present-day Native American peoples, and Inuit living ar

204 rs arrived in the ancient landmass of Sahul (present-day New Guinea and Australia) 55 thousand years

205 The present-day nitrogen isotopic compositions of Earth's su

206 ragments of Neandertal DNA in the genomes of present-day non-Africans [6, 7].

207 We estimate that the lineage leading to present-day North American pumas diverged from South Ame

208 ty (GPP) and latent heat fluxes (LE) against present-day observations.

209 hen DNA structure was just discovered to the present day of big data and epigenetics.

210 pite the greater luminosity (compared to the present-day) of its host star in its youth.

211 dertaken, from the seminal studies until the present day, of the key mechanistic aspects that influen

212 It is therefore possible that present-day organisms retain some record of the primordi

213 may prove advantageous when food is scarce, present-day overabundance of diets high in fat and sugar

214 Several populations in present-day Pakistan and India are thought to be the des

215 distinct from the Denisovan DNA segments in present-day Papuans and Aboriginal Australians.

216 We find a genetic signature in present-day Papuans that suggests that at least 2% of th

217 rational pedigrees and in close relatives of present-day patients.

218 Here, present-day patterns of genetic structure are thought to

219 ina helicina antarctica) through exposure to present day pCO2 conditions and two potential future OA

220 als, and be responsible for the diversity of present day placental structures.

221 Here we extrapolate models of present-day plate tectonics to the past and propose that

222 y heat loss, is manifested at the surface as present-day plate tectonics(1).

223 Accordingly, present-day population diversity is composed by multiple

224 storic and ecological factors in influencing present-day population structure of Palaearctic biota.

225 Nunavik Inuit to be distinct from any known present-day population.

226 ce with Y chromosome (chrY) distributions in present day populations of the Eastern Baltic, as well a

227 reflecting the much larger effective size of present day populations.

228 are genetically most similar to ancient and present-day populations from the north Peruvian coast lo

229 late Pleistocene hunter-gatherer groups and present-day populations of Europe.

230 Thus, the present-day populations of North Pacific killer whale ec

231 their origin and relationship to ancient and present-day populations remain unclear.

232 olves in the first group are most similar to present-day populations, although those in the second gr

233 previously existed occupied by ancestors of present-day populations, or were these regions occupied

234 Among present-day populations, the Parsis are genetically clos

235 Vanuatu and elsewhere in Oceania, as well as present-day populations.

236 that the K1f haplogroup is absent or rare in present-day populations.

237 glacier retreat here to less than 6 km from present-day positions.

238 A crucial issue in present-day prostate cancer (PCa) detection is the lack

239 However, all present-day protocols and strategies for the analysis of

240 Our work is readily applicable to present-day quantum experiments.

241 gross primary production, but maintenance of present-day radial growth also requires a 27% reduction

242 eractinian calcification of >50% relative to present-day rates.

243 appearing to reduce the likelihood that the present-day regional anomaly is a precursor to a global

244 Present day research takes the view on insomnia, i.e., p

245 Most present-day resonant systems, throughout physics and eng

246 ws that even small LGM ice caps can dominate present-day rock uplift in tectonically active regions.

247 richtian habitability decrease in areas with present-day rock-outcrop.

248 n rates with RSLR rates at the land surface (present-day RSLR rates are 12+/-8 mm per year) shows tha

249 Such analyses are not restricted to present-day samples and can also be applied to molecular

250 s, pairwise F(ST) values between archaic and present-day samples reflect both the spatial and tempora

251 We compare present-day samples with a pair of archaic samples taken

252 e made for the 2015 fires through the use of present-day satellite observations of the fire's radiati

253 essentially indistinguishable from those of present-day scorpions but share similarities with marine

254 re abundant in the late Pleistocene, whereas present-day sedimentation is dominated by calcitic biocl

255 er pattern of debris-flow lobes reaching the present-day shelf edge.

256 ocene period extended about 30 km beyond its present-day shore.

257 However, paleo sea-level markers on the present-day shoreline of Virginia and North Carolina dat

258 ther, short-statured phenotypes found in the present-day short grass prairies on the western peripher

259 n wolves, but not modern American wolves, to present-day sled dogs.

260 pted, by these groups with those confronting present-day societies, which also rely on tropical fores

261 that falls within the range of variation of present-day South Asians.

262 models' varying capability in simulating the present-day SPG stratification, whose realistic reproduc

263 hotochemical reactions characteristic of the present-day stratosphere.

264 ver the last 230 million years reproduce the present-day structure of the lower mantle, and show a Pe

265 t the dynamic history of Mars and reveal its present-day structure, by combining the study of thermal

266 by 2100 for scleractinian corals (30%-42% of present-day suitable habitat), even smaller refugia loca

267 from within rocks, by coupling estimates of present day surface wind abrasion with the methane conte

268 ivated by surface photochemistry, render the present-day surface more uninhabitable than previously t

269 structure of Mars are, by comparison to its present-day surface, poorly known-although evidence of r

270 table-marker horizon stations, to determine present-day surface-elevation change, vertical accretion

271 mias and whole-heart computational modeling, present-day system designs precludes its adoption by the

272 rsity with increasing T(jul) in regions with present-day T(jul) between 2.5 and 14 degrees C.

273 rconductivity(4)-and their critical roles in present-day technical devices.

274 reaction manifold circumvents limitations in present-day technologies for the stereoselective enoliza

275 e predicted based on two metrics: the reef's present-day temperature, and the proportion of recruits

276 difference to nearly 2 degrees C warmer than present-day temperatures.

277 Present-day terrestrial analogue sites are crucial groun

278 h's silicate mass, cannot solely account for present-day terrestrial halogen inventories.

279 on its high density of vulnerable assets and present-day tidal flooding issues.

280 es, being most rapid for CO2 (~10 years from present day) to 4 decades for nutrients.

281 he Cenozoic Era which incorporates models of present-day tomography-based mantle heterogeneity.

282 e that Himalayan ruptures may pass under the present-day trace of the MFT as blind faults inaccessibl

283 g and managing the potential side effects of present-day treatment regimens is therefore a cornerston

284 e mitochondrial DNA (mtDNA) variation of 545 present-day Umbrians (with 198 entire mitogenomes) and 2

285 ) may have reached about 20 metres above the present-day value(4,5).

286 The expansion of present-day variants in Eurasia could be the consequence

287 In present-day vertebrates, melanosome morphology correlate

288 Present-day volcano imaging and monitoring relies primar

289 onship between the projected warming and the present-day warm bias enables us to empirically correct

290 s decreases to zero at ~1.5 meters below the present-day water table, if one assumes linear variation

291 ow this original work to its fruition in the present day, where 2D halide perovskites are in the spot

292 ndividual studies took place between 1985 to present day with a duration of follow-up ranging from 9

293 as remained home to indigenous peoples until present day with only one apparent hiatus (3,400-2,800 Y

294 nt independent lineages similarly related to present-day wolves and dogs.

295 d branched off the lineage that gave rise to present-day wolves and dogs.

296 he relationships between Pleistocene canids, present-day wolves, and dogs, we resequenced the genomes

297 l dogs share a common ancestry distinct from present-day wolves, with limited gene flow from wolves s

298 a revised hypothesis for the origins of the present-day worldwide distribution of TAS2R38 haplotypes

299 on back to Africa where necessary to explain present-day Y-lineage distributions.

300 showing signatures of positive selection in present-day Zoroastrians that might correlate to the pre