ライフサイエンスコーパス: continental

1 ely demonstrates the existence of Calumma on continental Africa in the past.

2 Here we show that across continental Africa, the estimated geographic range of cl

3 r the single locus detected was the same for continental Africans (P=5.0x10(-111)) and for African Am

4 African-ancestry individuals, including 3754 continental Africans and 1867 African Americans.

5 This first GWAS of serum uric acid in continental Africans identified three associations at tw

6 formed the first GWAS for serum uric acid in continental Africans, with replication in African Americ

7 The continental air contained primary OA markers indicative

8 However, OHDCA formation in continental air was likely attributable to both biogenic

9 enes also exhibited higher concentrations in continental air, due to more emissions of their precurso

10 entified as the largest contributor of OA in continental air, with contributions fluctuating from 8%

11 We propose that the rapid rise of continental alkali basalts correlates with an abruptly d

12 o prior levels during the Silurian-a time of continental amalgamation-we further argue that plate tec

13 p it is that it is truly pristine, free from continental and anthropogenic influences, with the ocean

14 ces in the offshore marine atmosphere, where continental and marine air pollutants interact and atmos

15 ability is much weaker and its impact on the continental and maritime surface climate is largely insi

16 fall isotope ratios in the MAC region during continental and maritime TC tracks, with applications to

17 emispheric scales, there are few results for continental and subcontinental scales.

18 and even coastal ice-free areas in parts of continental Antarctica.

19 otoxin, are one of the main marine toxins in continental aquatic ecosystems.

20 stal thickness with the lowest Nb/Ta seen in continental arc magmas.

21 -seated magmatic differentiation, such as in continental arcs and other magmatic orogens, is thus nec

22 xplains why magmatism and differentiation in continental arcs, like the Andes, reach greater Li conte

23 ude with total anthropogenic PN emissions in continental areas.

24 ClNO(2) has been measured in continental areas; however, the sources of particulate c

25 to 3.3 Ma, which we attribute to periods of continental aridity.

26 Kenya represent the continental background level and are primarily influence

27 ater, a composition more typical of interior continental basin ground.

28 e use oceanographic modelling to predict how continental boundary currents are likely to change conne

29 ere, where ammonia can be convected from the continental boundary layer and nitric acid is abundant f

30 d in two major pulses that coincide with the continental breakup and the opening of the North Atlanti

31 ionary process from wide continental rift to continental breakup remains enigmatic due to the lack of

32 nd reflects the transition from wide rift to continental breakup.

33 After 6 Ma, however, continental carbon reservoirs contract rather than expan

34 Arctic cooling: Prior to 6 Ma, low-latitude continental carbon reservoirs expanded during astronomic

35 es from 11 cities across dry, temperate, and continental climate regions within the United States.

36 unts of leached substances were found in the continental climate zone, coinciding with the lowest pot

37 wn through marine records, the corresponding continental climatic conditions drive the evolution of t

38 the production area of Ogliarola campana: a continental cluster in the inner area of Irpinia and a c

39 nstructing crustal thickness through time in continental collisional belts.

40 cupy, evolution of the Saharides involved no continental collisions until the end of their developmen

41 This region is subjected to Mediterranean continental conditions, it encompasses wide climatic, to

42 surface type (land or ocean) and surrounding continental configuration.

43 area and volumes of tropical peat and their continental contributions.

44 bate is centered on the low Nb/Ta of Earth's continental crust (11-13) compared to basalts (15-16).

45 oduction of magma, earthquakes, formation of continental crust and mineral resources.

46 en enhancement in chemical weathering of the continental crust during the early Cambrian, which may b

47 th is currently a topic of debate, dry lower continental crust may be strong under high-grade conditi

48 Accurately quantifying the composition of continental crust on Hadean and Archean Earth is critica

49 solutes from the chemical weathering of the continental crust supplies a steady supply of essential

50 tion of metamorphic (P, T) conditions in the continental crust through time might therefore reflect t

51 corresponding element/Th ratio of the Upper Continental Crust) reveal maximum values 10 to 40 cm bel

52 e over the past 4.5 billion years formed the continental crust, and produced at least one complementa

53 osphere components in the evolution of upper continental crust, presenting critical information for l

54 direct evidence for the presence of a felsic continental crust, such as the elevated (49)Ti/(47)Ti ra

55 d metals from the mantle to the lower-to-mid continental crust, which leaves little footprint behind

56 le material forming some 5 million km(2) new continental crust.

57 elative to local clastic materials and upper continental crust.

58 m that may act throughout the quartz-bearing continental crust.

59 where the oceanic crust subducts beneath the continental crust.

60 land arc rocks, which are building blocks of continental crust.

61 magmatic systems emplaced at the base of the continental crust.

62 t and ocean island basalt samples as well as continental crustal rocks going back to 2 Ga are within

63 dinosaurs, relies heavily on the fossil-rich continental deposits of South America, their precise dep

64 ations of most PFAS, indicating that ongoing continental discharges are the major source to the marin

65 merica and Asia together with the continuous continental distribution of a limited number of European

66 processes and biotic interactions can shape continental diversity.

67 ermal and mechanical weakening of this broad continental domain allowed for the formation of metamorp

68 o arid gradient covering >1,800,000 km(2) of continental eastern and central Australia.

69 tinents and the accumulation of sediments at continental edges and in trenches has provided lubricati

70 We find that a resurgent continental epidemic could occur as many as 5 weeks earl

71 icillium stem striping in the UK, whereas in continental Europe Verticillium stem striping is predomi

72 from the Iberian Peninsula, British islands, Continental Europe, Africa and American zebu.

73 er is genetically closer to populations from continental Europe, such as Northern and Central Italian

74 th a continuum of lineages coexisting across continental Europe, while distinct lineages exist in iso

75 ium after they appeared in adjacent areas of continental Europe.

76 wn, but islands can also provide refuge from continental extinction.

77 ture being introduced to Britain by incoming continental farmers, with small, geographically structur

78 Large continental faults extend for thousands of kilometres to

79 Temporal correlation between some continental flood basalt eruptions and mass extinctions

80 of change within highly arid regions of the continental flyway increased their value to migratory wa

81 ave considered these effects at the scale of continental flyways.

82 an extensive trait database and a long-term continental forest plot network to map changes in commun

83 correlation between global biodiversity and continental fragmentation is not readily attributable to

84 atic consequences of this erosion for global continental freeboard.

85 is due to both ocean warming and increasing continental freshwater discharge.

86 Great Unconformity marks a major gap in the continental geological record, separating Precambrian ba

87 indicate that a 70 km-diameter crater into a continental glacier could release between 8.7 x 10(13) t

88 This includes the iconic continental ground sloths Megatherium, Megalonyx, Mylodo

89 Some reach high frequency and are private to continental groups or even individual populations, inclu

90 taneously impacting populations from distant continental habitats.

91 racture, enhancing stability and restraining continental ice discharge into the ocean, suture zones a

92 Whereas the presence of extensive continental ice sheets predicts a tidally energetic Snow

93 rise resulting from the instability of polar continental ice sheets represents a major socioeconomic

94 several population splits moved south of the continental ice sheets that covered Canada sometime betw

95 y, most of Antarctica remains in the grip of continental ice sheets, with only about 0.2% of its over

96 astodons than in endemic clades south of the continental ice sheets.

97 enter the Mediterranean during phases of low continental ice volume and high concentrations of atmosp

98 ted to be especially severe in high-latitude continental interiors.

99 orheic lakes and wetlands when crossing arid continental interiors.

100 ne 15 African populations covering all major continental linguistic groups, ecosystems, and lifestyle

101 rives continued underthrusting of the Indian continental lithosphere and shortening and thickening of

102 The long-term stability of Precambrian continental lithosphere depends on the rheology of the l

103 hanges in tectonic processes that formed the continental lithosphere in the Archean.

104 During extension, the continental lithosphere thins and breaks up, forming eit

105 frican sulfide inclusions: thickening of the continental lithosphere through horizontal processes aro

106 nism may typify rapid localised extension of continental lithosphere.

107 ther than the convecting upper mantle or sub-continental lithosphere.

108 architecture of the northern South China Sea continental margin is strikingly similar to the broad co

109 chemically and sedimentologically divergent, continental margin sites are highly similar but differ c

110 emplacement flexed down a previously rifted continental margin thereby contributing to subsidence of

111 m the coastline and >500 m depth, beyond the continental margin.

112 ontinental rift and highly extended (<15 km) continental margin.

113 curs as oceanic lithosphere is emplaced onto continental margins (ophiolites), and along the seafloor

114 Continental margins are disproportionally important for

115 oceanic surface waters in close proximity to continental margins are iron replete with respect to mar

116 nstrates the geologic significance of global continental margins for providing broadly-equitable, geo

117 tion of gas hydrates is pervasive across the continental margins of the Arctic Ocean.

118 FG) systems have been documented in numerous continental margins worldwide, their geometry, controls

119 organic carbon flux and preservation on deep continental margins worldwide.

120 % of the Mesoproterozoic ocean focused along continental margins.

121 tural hydrocarbon seeps are ubiquitous along continental margins.

122 The marine air and continental-marine mixed air had more abundant hydroxyl

123 separates regional-scale blocks of accreted, continental materials in southern Taiwan.

124 imatic conditions (Atlantic, alpine, boreal, continental, Mediterranean) and land uses (arable, fores

125 pre-existing lithospheric heterogeneities in continental microplate rotation.

126 st African Rift System is one of the largest continental microplates on Earth.

127 findings refine our current understanding of continental migration, identify gene flow and the respon

128 kely reflect new and emerging bottlenecks to continental migration.

129 er ecosystems, resulting in degradation of a continental migratory route.

130 ements and DOC-delta(13)C, particularly when continental moisture source contributions were high, ind

131 concentrations of I and Se were highest when continental moisture sources were dominant, indicating i

132 s indicate predominantly Aegean ancestry for continental Neolithic farmers, but also variable admixtu

133 alysed in relation to local climate across a continental network of study sites.

134 ch, brackish groundwater in a serpentinizing continental ophiolite to elucidate the role of sulfur co

135 Typically, impact studies are attempted at continental or global scales and use coarse-resolution m

136 ribution changes of freshwater megafauna, at continental or global scales, remain unclear.

137 er, the contribution of recycled moisture of continental origin to I and Se to precipitation has neve

138 f wintertime BC at two receptor sites of the continental outflow.

139 rsely correlated, suggesting the coupling of continental P input and marine P cycle.

140 ped by crossing a Mediterranean (103-2) to a Continental parent (R43-64).

141 The causes of continental patterns in species richness continue to spu

142 Continental pedogenic carbonates preserved in Neogene ba

143 cost: $35.7B-50B) is required to achieve the continental population goal of 4 M individuals under the

144 these nests were separate incursions from a continental population rather than belonging to a single

145 positive abundance trends in the coastal and continental population respectively.

146 effect on population growth rates, than the continental population.

147 have more delineated gene pools compared to continental populations.

148 The transition from maritime to continental precipitation regimes is revealed in the lon

149 nce time estimates support the hypothesis of continental range contraction to a single refugial area

150 of species ranges, ultimately controlled by continental range dynamics of individual species.

151 number concentration, especially in pristine continental regions and during the preindustrial period.

152 sols and that aerosol pH levels in populated continental regions are widely buffered by the conjugate

153 ortance of different multivariate CEs in six continental regions to highlight CEs posing the highest

154 onal extremes in temperature (e.g. temperate/continental regions) and precipitation (e.g. tropical sa

155 ology (harboring the highest biodiversity of continental regions).

156 atypical history of the island compared with continental regions.

157 nse of N deposition to N emission control on continental regions.

158 n human reference populations from the major continental regions.

159 By comparing one coastal and one 'continental' reindeer population over four decades, we s

160 how coordinated exit strategies could delay continental resurgence and limit community transmission

161 na Sea records the transition between a wide continental rift and highly extended (<15 km) continenta

162 elp to constrain the mechanical behaviour of continental rift systems as well as the related seismic

163 Continental rift systems form by propagation of isolated

164 Yet, the evolutionary process from wide continental rift to continental breakup remains enigmati

165 Continental rifts are important sources of mantle carbon

166 al margin is strikingly similar to the broad continental rifts in the North American Cordillera and i

167 extraction may increase CO(2) fluxes in some continental rifts, helping to control the production and

168 Wide continental rifts, which can reach 1,000 km across, have

169 Understanding the approach to faulting in continental rocks is critical for identifying processes

170 ical evidence for these relationships at the continental scale and across different soil depths is la

171 biological invasions and climate change on a continental scale and illustrates their strategic value

172 The approach is unique in the continental scale examined, the breadth of taxonomic gro

173 consistent patterns of climate drivers at a continental scale explaining latitudinal differences in

174 rovide the first machine-learning based near-continental scale identification of atmospheric circulat

175 pact of human expansion on fire rates at the continental scale in Africa, reducing the fire risk.

176 mated phenological monitoring in regional-to-continental scale observatory networks; and tracking res

177 The continental scale of forest alteration and extended time

178 but the changes in extent and density at the continental scale remain unclear.

179 ures in the turnover of biotic similarity at continental scale that are congruent among vertebrate cl

180 ic data for large-scale regions (national or continental scale) is next to impossible.

181 ern of decoupled host/virus coevolution on a continental scale, and highlight knowledge gaps about he

182 At the continental scale, phytoplankton evenness explained more

183 At the North America continental scale, the model predicted the average annua

184 if such river gradients were commonplace at continental scale, which is inconsistent with constraint

185 sights into colonisation and extinction at a continental scale.

186 nd physical constraints for a large taxon at continental scale.

187 rium abundance of a migratory species at the continental scale.

188 We quantified effects of continental-scale (climate, landscape greenness, and dis

189 onse to coeval atmospheric CO(2) decline and continental-scale Antarctic glaciation.

190 Here, we employed a multidecade, continental-scale approach of surveillance data to under

191 This study presents the first continental-scale assessment of recent changes in frost

192 struct variability in T(min), ice cover, and continental-scale atmospheric circulation patterns (r >=

193 ake Superior peak ice cover, and regional to continental-scale atmospheric winter pressure variabilit

194 es have been unable to identify a consistent continental-scale climatic-change signal in flood discha

195 otic factors apparently played a key role in continental-scale community assembly before the extincti

196 rveyed across the Neotropics to quantify the continental-scale extent and intensity of defaunation an

197 ation of ecosystem models, and assessment of continental-scale functional diversity.

198 United States and reveal distinct local- and continental-scale heterogeneity in community excretion r

199 climate predictions from seven GCMs to run a continental-scale hydrological model for a process-based

200 volume in the Aurora subglacial basin before continental-scale ice sheets were established about 34 m

201 tial scale of these impacts demonstrate that continental-scale megadroughts pose a major future threa

202 Continental-scale models of malaria climate suitability

203 Our continental-scale P mass balance results indicated that

204 These structures underline the importance of continental-scale processes for species richness in indi

205 Yet, a detailed, continental-scale risk assessment of climate-related imp

206 d soil microorganisms and microfauna using a continental-scale sampling effort combined with a global

207 tivity at northern high-latitudes and signal continental-scale shifts in the structure and function o

208 Collectively, this continental-scale study demonstrates the utility of drag

209 ing spatial synchrony between populations at continental scales and linked it to anthropogenic climat

210 xtract these indirect effects at regional to continental scales are not feasible.

211 emes of temperature and precipitation across continental scales, known as climate dipoles.

212 w studies have investigated these impacts on continental scales.

213 to their establishment do not match at large continental scales.

214 kes was spatially autocorrelated at local-to-continental scales.

215 rs that determine diversity likely varies at continental scales; thus, as climate change alters the c

216 ate Palaeozoic climate regimes and increased continental seasonality over approximately 40 Myr.

217 stal impact ejecta in situ, forming a unique continental seismite-ejecta couplet within a distance of

218 n CA-ID-TIMS dating of euhedral zircons from continental sequences of the Sydney Basin, Australia, to

219 Despite the continental setting, the isotopic signatures argue for t

220 Coastal and continental shelf (neritic) environments account for mor

221 uture research and conservation efforts: the continental shelf adjacent to east central Florida and t

222 rted in submarine canyons that intersect the continental shelf and directly connect to terrestrial pl

223 with losses of marine ice over high latitude continental shelf areas.

224 across and retreated from the Sabrina Coast continental shelf at least 11 times during the Oligocene

225 thropogenic disturbance than any other ocean continental shelf environment.

226 predominantly benthic forager on the shallow continental shelf of Bass Strait, and represents the gre

227 cycle in sulfate-reducing sediments from the continental shelf of the northern South China Sea.

228 elopment of offshore wind farms on the outer continental shelf of the United States has led to signif

229 Sea likely contributes to net export via the continental shelf pump and advection (34.4 +/- 6.0 Tg C

230 ine geological and geophysical data from the continental shelf seaward of the Aurora subglacial basin

231 of daily positions in oceanic waters off the continental shelf showed the greatest tendency for trans

232 n salinity observed at five locations on the continental shelf suggest that upstream preconditioning

233 onto and across the seabed of the Antarctic continental shelf towards the ice(4-6).

234 riability than the heat transported onto the continental shelf(9).

235 n up to 100 kilometers inland, extend to the continental shelf, and include ocean systems with waters

236 the inflow of warm water onto the Antarctic continental shelf, plays a key role in the ice sheet's m

237 mplex of grounding-zone wedges on the Larsen continental shelf, western Weddell Sea.

238 tic and Indian Oceans and over the Antarctic continental shelf.

239 re likely in adjacent waters of the Canadian continental shelf.

240 sequestered carbon in the benthos around the continental shelf.

241 se to the cold front passages over Louisiana continental shelf.

242 tion and associated processes over Louisiana continental shelf.

243 h available acoustic measurements in several continental-shelf environments using standard oceanograp

244 ypical operational ranges and frequencies in continental-shelf environments.

245 tatic, tectonic, and geomorphic processes on continental shelves and provide insight into shelf geoch

246 The emergence of continental shelves during ice ages and their flooding d

247 cial processes that drove water into exposed continental shelves during sea-level low stands and acti

248 inity submarine groundwater contained within continental shelves is a global phenomenon.

249 ago, as ice sheets grew, sea level fell, and continental shelves narrowed.

250 ines and fringing ice shelves extending onto continental shelves(8).

251 espread sedimentary denitrification on broad continental shelves.

252 a: see text]C) values accumulated on shallow continental shelves.

253 ate was the organic carbon burial on drowned continental shelves.

254 fate of the Irminger Current water from the continental slope to Labrador Sea interior are investiga

255 by a deep continuous trough extending to the continental slope.

256 at water depths between 956 and 1545 m over continental slopes in the northern South China Sea.

257 oisture sources indicate combined marine and continental sources of precipitation and Se, I, Br, and

258 uba and D. santomea Each pair consisted of a continental species and an island endemic.

259 and their genomes regressed to those of the continental species.

260 We discuss the importance of mitigating pan-continental spread in light of the fragile healthcare sy

261 opulations (called stock units, SU) from two continental stock groups (CSG) in North America (NA) and

262 ort new data on concentrations of iridium in continental strata of the Fundy, Deerfield, Hartford and

263 In this cross-continental study, we employ a theoretical framework in

264 advances on routine clinical practice across continental territories has not been clear.

265 processes but this congruence is lost at the continental to country extents.

266 0 dryland soils globally distributed and two continental to global-scale cross-biome datasets.

267 ciently monitor diffuse contamination at the continental to regional scale.

268 Continental transitions between forests dominated by ect

269 Inter- and intra-continental transmission events have resulted in the cur

270 ulate aerosol pH in 2011 and 2050 across the continental U.S.

271 s sourced from distinct latitudes within the continental United States (28 degrees N, Tampa, FL; 36 d

272 activity for 37 different regions across the continental United States and asked whether and how fire

273 t throughout the cotton-growing areas of the continental United States and northern Mexico a century

274 total nitrogen loading (+54% to -7%) for the continental United States by the end of the century.

275 y, Florida was the most affected area in the continental United States during the 2016 Zika virus out

276 estimate the average number of wells in the continental United States is 6.04 +/- 19.97 million well

277 ist within states and within counties in the continental United States, and the patterns differ by ra

278 ure at weekly and county resolution over the continental United States, combined with discussion of t

279 and organic carbon downslope annually in the continental United States.

280 tic assessment of technical potential in the continental United States.

281 he current daily NAAQS, and mortality in the continental United States.

282 across 18 species from eight studies in the continental United States.

283 ading cause of mosquito-borne disease in the continental United States.

284 ity at shorter periods (e.g. glacio-eustasy, continental uplift and erosion, volcanism, asteroid impa

285 ges, and, ultimately, consumption for the 66 continental US Balancing Authorities (BAs).

286 Among continental US breeds F(is) was consistently low suggest

287 h soil, species, and climate sampled from 20 continental US locations.

288 We analysed a lake dataset spanning the continental US to evaluate whether strong evenness effec

289 ons (feral populations from Pacific islands, continental US, and Chinese breeds) using 70,231 SNP fro

290 We analyzed protected areas in the continental USA to assess the extent to which they cover

291 ourly soil temperatures (5 depths, 90 sites, continental USA) and physiological data, and simulated c

292 tructure similar to that associated with sub-continental variation in forest types and eco-climatic z

293 brines in magmatic orogens, particularly in continental volcanic arcs.

294 nic magnesium cycle is largely controlled by continental weathering and marine authigenic mineral for

295 arge amount of nutrients due to the enhanced continental weathering and the contemporary increase of

296 to fit proxies the temperature dependence of continental weathering must be weaker than commonly assu

297 sited by silica-rich fluids derived from the continental weathering of the volcanic host rocks.

298 n (CIA) upon time sequence, suggest enhanced continental weathering that may be attributed to the inv

299 long-term decrease in nutrient delivery from continental weathering, coupled with a possible decrease

300 ne (34-6 Ma), potentially through changes in continental weathering.