ライフサイエンスコーパス: present-day

1 ccesses and failures that continue until the present day.

2 nd morphological stasis that persists to the present day.

3 xplain these phenomena that continues to the present day.

4 y-old last eukaryotic common ancestor to the present day.

5 t 0.2 to 0.5% of the host galaxy mass in the present day.

6 racing its origins over the centuries to the present day.

7 otes is similar to plants and animals at the present day.

8 mic diversification from the Cambrian to the present day.

9 wo archosaurian lineages that survive to the present day.

10 tion patterns from the Pliocene epoch to the present day.

11 rst chaperones, a role that continues to the present day.

12 s in imaging technology that continue to the present day.

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

14 ing with initial applications through to the present day.

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

16 ze, wheat and rice is similar by 2050 to the present-day.

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

18 A GCM's realization of present-day (1970-1999) and future (2070-2099) climate,

19 We used the model to compare Baltic Sea's present-day (2005-2014) eutrophic state to an oligo/meso

20 between reference conditions (1860) and the present day (2012) are needed.

21 olate mofetil, which has continued until the present day (22 months after the procedure).

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

23 One factor is the low sensitivity of present-day aerosol to natural emissions that determine

24 aboons along with geographic distribution in present day Africa to understand how the kidney risk var

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

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

27 solate is closely related to the most common present-day American haplotype and likely entered the Am

28 ctions is visible in the genetic ancestry of present-day Americans.

29 at needs to predict suitable habitat for the present day and 1950s.

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

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

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

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

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

35 hroughout Micronesia were moved according to present-day and future ocean circulation models.

36 concentrations in CR and AB increased toward present day, and ranged from 0.14 x 10(7) to 1.7 x 10(7)

37 ococci concentrations in CR increased toward present day, and ranged from approximately 0.03 x 10(5)

38 ur simulations represent the response of the present-day Antarctic ice-sheet system to the oceanic an

39 vealing deep westward flow equivalent to the present-day Antarctic Slope Current.

40 s is possible, and substantially faster than present-day approximate methods.

41 Many plant species comprising the present-day Arctic flora are thought to have originated

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

43 n Northern America, and that the ancestor of present-day asses and zebras dispersed into the Old Worl

44 bed by air pollution could be studied in the present--day atmosphere, but the pervasiveness of air po

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

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

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

48 re contained less than 0.001 per cent of the present-day atmospheric oxygen (O2) level, until the Gre

49 istent with observational constraints on the present-day atmospheric, oceanic, and soil Hg reservoirs

50 American skeletons, which share traits with present-day Australasians (indigenous groups in Australi

51 to identify the factors that most influence present-day AWP and to predict responses to medium-term

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

53 les they play, are effectively restricted to present day 'baseline' trends of BVOC production across

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

55 enes, could serve as molecular proxy linking present-day-behaviour to past exposures.

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

57 rocesses shaping the spatial distribution of present-day biodiversity.

58 involvement in species dispersal has shaped present-day biodiversity.

59 lope gene, with only syncytin-Opo1 being the present-day bona fide syncytin active in the opossum and

60 g results demonstrate that a conversion of a present-day boreal forest-wetland to a hypothetical homo

61 Our findings imply that the present-day bread wheat genome is a product of multiple

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

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

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

65 France has the lowest present-day cerebrovascular disease mortality for both m

66 zations that are only loosely constrained by present day changes.

67 ty is crucial to promote rapid adaptation to present-day climate change, not only for coral reefs, bu

68 support the notion that models that simulate present-day climate variability better are likely to mak

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

70 ntly discovered polyketide clostrubin from a present-day Clostridium bacterium, the Jurassic borolith

71 About half of present-day cloud condensation nuclei originate from atm

72 rates, even after being moved back to lower present day CO2 levels for hundreds of generations.

73 Present day coalescent simulations do not scale well, or

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

75 region of Kenya found 740 km inland from the present-day coastline of the Indian Ocean at an elevatio

76 predict warming-related loss of species from present-day communities over the next century.

77 The position of present-day communities was projected into ordination sp

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

79 th's radiation field from pre-industrial and present-day concentrations of these gases.

80 ion conditions (1000 muatm pCO2) compared to present day conditions (380 muatm pCO2).

81 umes can mitigate exposure to high CO2 under present-day conditions and that exposure mitigation is e

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

83 In contrast to present-day conditions, our speleothem data provide stro

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

85 tely -0.05 to -0.25 units below ambient) and present day controls (DeltapH = 0) for calcification rat

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

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

88 cations for microbial life strategies in the present-day deep biosphere as well as early life on Eart

89 ents, responsible for shaping major parts of present-day demographic structure in both Europe and Asi

90 ate that she originated from a place outside present day Denmark (the island of Bornholm excluded), a

91 0-12,600) years ago, and thus they represent present-day descendants of some of the earliest migrants

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

93 The present-day distribution of velvet worms corresponds nea

94 Present day distributions of Encope are likely the resul

95 immigration), is needed to better understand present-day diversity patterns and model future changes.

96 on from the archaic Taimyr wolf lineage into present-day dog breeds from northeast Siberia and Greenl

97 This demonstrates that the ancestry of present-day dogs is derived from multiple regional wolf

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

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

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

101 ronmental parameter space that binds life on present-day Earth and has been widespread for only about

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

103 trations may have been close to those of the present-day Earth, and that the ratio of oxygen to carbo

104 h, under redox conditions more oxidized than present-day Earth.

105 some Native Americans sharing ancestry with present-day East Asians (including Siberians) and, more

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

107 broad relationships in more detail; estimate present-day economic costs of DUDs; investigate hypothes

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

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

110 constrained by the geology, geochemistry and present-day environmental conditions of the Mt.

111 natural archives and direct measurements of present-day environmental Hg concentrations.

112 alysis shows that the aerosol system in many present-day environments looks and behaves like it did i

113 New TB control strategies in the present-day epidemiological climate call for important s

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

115 Present day eukaryotes employ at least two main defence

116 In present-day eukaryotes, the cell division cycle is contr

117 8) whose closest relatives are widespread in present-day Eurasia; we estimate from sequence data that

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

119 w Guineans and Andaman Islanders than to any present-day Eurasians or Native Americans.

120 a similar amount of Neanderthal ancestry as present-day Eurasians.

121 In present-day Europe, only two centers of biodiversity exi

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

123 2,345 contemporary humans to show that most present-day Europeans derive from at least three highly

124 e contributing to the genetic composition of present-day Europeans, all individuals between ~37,000 a

125 pulation which forms part of the ancestry of present-day Europeans.

126 mately 3,000 years ago, and is ubiquitous in present-day Europeans.

127 Present-day evolutionary theory, modern synthesis and ev

128 s and Woodward, respectively, through to the present day examples, such as the tetracyclines.

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

130 intensity yet only approximately 60% of the present-day field strength, with a long-term average vir

131 Success in reproducing present day flow patterns shows the potential for progno

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

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

134 e adult tree canopy, but regeneration of the present-day forests is unlikely because of the loss of s

135 dispersal limitation operates in structuring present-day fungal community composition and functional

136 Gas clouds in present-day galaxies are inefficient at forming stars.

137 Most present-day galaxies with stellar masses >/=10(11) solar

138 umps survive feedback and grow the bulges of present-day galaxies.

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

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

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

142 lternative modes of Helitron organization in present-day genomes, we have applied the novel computati

143 s to the New World, a foretaste, perhaps, of present day global transport of tropical diseases.

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

145 important questions about the history of the present-day Greenlandic population remain unanswered.

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

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

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

149 etre should undergo convection for estimated present-day heat-flow conditions on Pluto.

150 This suggests how present-day helicases diversified from an ancestral core

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

152 of compiled observations, we estimate global present-day Hg discharges from rivers to ocean margins a

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

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

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

156 9 in archaic hominins was closely related to present-day human alleles that are rare and specific to

157 d a phylogenetic approach to reconstruct how present-day human microbiomes have diverged from those o

158 We show that the ancestors of some pairs of present-day human populations were substantially separat

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

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

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

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

163 Comparisons with present-day humans from Africa, Europe, and Asia reveal

164 t genome-wide sequence data from ancient and present-day humans from Greenland, Arctic Canada, Alaska

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

166 contributed to the genetic diversity of some present-day humans outside of Africa [6-9].

167 amino acid substitutions in Neandertals and present-day humans that may underlie phenotypic differen

168 20% more Neandertal DNA to be identified in present-day humans, including variants involved in low-d

169 e findings, based on analysis of ancestry of present-day humans, reveal migration in the distant past

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

171 e about its relationship to Neanderthals and present-day humans.

172 g six Neandertals, but lower than that among present-day humans.

173 to alter protein structure or function than present-day humans.

174 7] to study his relationship to ancient and present-day humans.

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

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

177 ve arisen early and to have persisted to the present day in diverse organisms.

178 bly steeper meridional SST gradient than the present day in the central GBR.

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

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

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

182 ew population, representing the ancestors of present-day Inuit, with evidence of past gene flow betwe

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

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

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

186 dings suggest that barley landraces grown in present-day Israel have not experienced major lineage tu

187 thin the marsupial suborder Macropodiformes (present-day kangaroos, wallabies, and related macropodoi

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

189 rting points), and divergence in shaping the present-day latitudinal diversity gradients of marine bi

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

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

192 vity to atmospheric CO2 concentrations above present-day levels.

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

194 s about causes of long-term decline to their present-day low biodiversity.

195 cted distribution of water ice inferred from present-day lunar temperatures.

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

197 The present-day mantle, as sampled by oceanic basalts, shows

198 on (oxygen fugacity) higher than that of the present-day mantle.

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

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

201 d by the impact of an asteroid at Chicxulub, present-day Mexico.

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

203 Present day mitochondria and plastids (chloroplasts) evo

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

205 Consequently, the present-day mode and scale of dust production from the B

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

207 e, whereby the northeast Asian affinities of present-day Native Americans contrast with a distinctive

208 ide data, we found that the ancestors of all present-day Native Americans, including Athabascans and

209 00 years ago, a genetic component related to present-day Near Easterners became widespread in Europe.

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

211 rn Cameroon and non-Bantu speakers living in present-day Nigeria and Ghana.

212 ils from this period, these ancestors of all present-day non-African modern populations remain largel

213 ot present to the same extent, or at all, in present-day Northern and Central Americans or in a appro

214 from the ancestral condition represented by present-day oceanic stickleback.

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

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

217 peratures that were considerably warmer than present day ones and the impact of the cooling environme

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

219 ow they evolved and why they are retained in present-day organisms.

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

221 nturies in the Hindu Kush mountain ranges of present-day Pakistan.

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

223 This created a present-day pattern, much weaker or absent in the 1980s,

224 Sahelian Africa reflects historic as well as present-day patterns of riverine drainages.

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

226 but they have contributed 1-3% of the DNA of present-day people in Eurasia.

227 calculated forcing between preindustrial and present-day periods.

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

229 ogeneity, or the extent to which a country's present-day population descended from migration from num

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

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

232 last 10,000 years, such that ancestry across present-day populations is likely to be a mixture of sev

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

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

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

236 from a source nested within the variation of present-day populations speaking Austro-Asiatic language

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

238 ecological strategies and genomic traits in present-day populations, they do not rule out a major ro

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

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

241 is a rare complication of cholelithiasis in present-day practice.

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

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

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

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

246 ion of pregnant women in clinical studies to present-day rationale for inclusion of this group.

247 ctional space of the ancestral DBD among the present-day receptors, allowing a paralogous family of t

248 olled conditions simulating four climates: a present-day reference climate, an increased-temperature

249 ently well preserved to allow comparisons to present-day references, thus yielding molecular signatur

250 evels in the historic samples as compared to present-day references.

251 hypericinoid pigments both in fossil and in present-day representatives of the order Isocrinida indi

252 ing and planned river-sediment diversions at present-day river-sediment loads.

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

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

255 s collected during warm time periods, and in present-day rural forests compared to the same sites whe

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

257 This is true for present-day secondary metabolites, but even more for exc

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

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

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

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

262 Present-day soybeans consist of elite cultivars and land

263 We demonstrate that the present-day spatial distribution and orientation of the

264 from areas of geographic origin) can explain present-day species richness relative to current climate

265 roximity to thermal limits, as inferred from present-day species' distributional ranges, outweighs sp

266 provide unique information on the status of present-day species, communities, and biomes over the la

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

268 rts that can potentially enable going beyond present-day "standard" polymer dielectrics (such as biax

269 etal concentration, these sediments meet the present-day standards of "contaminated soil".

270 emerge as the primary factors underlying the present-day status of populations and communities; withi

271 hotochemical reactions characteristic of the present-day stratosphere.

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

273 n combining global plate reconstructions and present-day structure of the mantle.

274 onset of global plate tectonics because most present-day subduction initiation mechanisms require act

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

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

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

278 he discrepancies are not explained simply by present-day temperature differences.

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

280 Present-day terrestrial analogue sites are crucial groun

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

282 opical fluxes, suggest that up to 60% of the present-day terrestrial sink is caused by increasing atm

283 t, wealthy countries effectively limit their present-day threat by gross domestic product-enabled inf

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

285 Present day TOC concentrations are similar to VNIRS-reco

286 e involve losses of 400-1,400 Pcal (8-24% of present-day total) when CO2 fertilization effects are ac

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

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

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

290 a harbinger for possible consequences of the present-day warming of PF-C soils.

291 ochemical cycle; this results in a 27% lower present-day water column Hg reservoir.

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

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

294 es published since 1960 has caught up to the present day, with >95% of relevant published literature

295 on that diverged from the common ancestor of present-day wolves and dogs very close in time to the ap

296 at the ancestors of dogs were separated from present-day wolves before the Last Glacial Maximum.

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

298 ere, we present the complete genomes of nine present-day Yakutian horses and two ancient specimens da

299 A similar present-day Zambian fishery, documented here, appears st

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