ライフサイエンスコーパス: continental

1 ndinavians and French Canadians; groups with continental admixture such as Puerto Ricans; settlers su

2 try has individual variation in European and continental African contributions [36-39].

3 have likely played a pivotal role in shaping continental African forest diversity.

4 A recent study cataloging variation in continental African populations suggests this type of Af

5 ndard Reference Material (SRM) 1720 Northern Continental Air, were certified by NIST for ambient mole

6 ons to study climatic variations controls on continental and global vegetation productivity patterns.

7 Inter-continental and inter-taxonomic variation can be largely

8 ferent sources, namely, combustion; Northern Continental and Southern Oceanic Air and a gas well sour

9 ected substantial diversity and admixture in continental and subregional populations, corresponding t

10 luable features of landscapes at a regional, continental, and perhaps even worldwide scale.

11 del projections suggest refugia may exist in continental Antarctica beyond 2099, buffering species-wi

12 Continental Antarctica is devoid of insects, but elsewhe

13 Although most models suggest continental Antarctica was covered by ice during the Las

14 esozoic greenhouse climates, whereas reduced continental arc activity corresponds with icehouse clima

15 ctivity and major climate shifts: Widespread continental arcs correspond with prominent early Paleozo

16 higher delta(13)C and are located in mature continental arcs that have accreted carbonate platforms,

17 tions for its survival were displayed in sub-continental areas and not along the Mediterranean coasts

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

19 nce of relevant concealed introductions from continental Asia in Europe and North America.

20 ell as re-invasions of freshwater systems on continental basins by multiple lineages.

21 aphy was introduced in a landmark study of a continental biota.

22 versification and distributional dynamics in continental biotas has long been an interest of biogeogr

23 ess, with the biota as passive passengers on continental blocks.

24 ks are located at major subduction zones and continental boundaries, and mainshocks with all types of

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

26 Continental boundary currents are projected to be altere

27 The earliest known continental branchiopods are associated with hot spring

28 Melting of the mantle during continental breakup leads to magmatic intrusion and volc

29 hest and melting depths deepest early during continental breakup.

30 aging the mantle response during progressive continental breakup.

31 ce of Q. tomentella in the fossil records of continental California.

32 ee broad geographical groups consistent with continental climate regimes.

33 that GCR flux change had a greater impact on continental climate than on oceanic climate.

34 on rates can be a powerful proxy for ancient continental climates that lie beyond the reach of most l

35 Other nonmarginal populations with continental climates were predicted to be severely and n

36 ecological significance of this period, the continental climatic conditions associated with it remai

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

38 ia onto the Indian subcontinent after Eocene continental collision was not a uniform process, but was

39 tion of an orogen from oceanic subduction to continental collision.

40 ne-present) intermediate magmatic rocks from continental collisional belts and correlations between t

41 nstructing crustal thickness through time in continental collisional belts.

42 In the future, continental comparative phylogeographers will continue t

43 455 studies to explore the current scope of continental comparative phylogeography, including geogra

44 Continental conditions during the latest Miocene are of

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

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

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

48 ithospheric mantle, fused to the base of the continental crust and isolated from mantle convection.

49 a fivefold increase in the mass of the upper continental crust due to addition of granitic rocks, sug

50 tative index describing the fragmentation of continental crust during supercontinental coalescence-br

51 to constrain the chemical composition of the continental crust exposed to weathering and found that s

52 Typical intraplate continental crust has hydrostatic fluid pressure and a n

53 inite has developed over tectonically stable continental crust in response to deep weathering during

54 ures of trace elements and thus resemble the continental crust produced in modern subduction settings

55 epositional environments over thin (sinking) continental crust such as the Lake Eyre Basin.

56 Most exposed continental crust that can be dated back to the Archaean

57 ly of Rodinia from thickened mid-Proterozoic continental crust via two-sided subduction can account f

58 fic rocks were emplaced at low latitude onto continental crust within the tropical humid belt.

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

60 generating and/or modifying large volumes of continental crust, as observed in the continents today.

61 ty by changing the geographic arrangement of continental crust, but the data required to fully test t

62 ith changes in the geographic arrangement of continental crust, it is difficult to identify a specifi

63 ributed to recycled pelagic sediments, lower continental crust, or recycled subcontinental lithospher

64 rchean Eon witnessed the production of early continental crust, the emergence of life, and fundamenta

65 which leads to the formation of oceanic and continental crust, together with crust recycling through

66 The nature of the first continental crust, which was the interface between the s

67 location, distant from nuclear reactors and continental crust, would best reveal the mantle flux, ho

68 ent occurs in magmas that incorporate felsic continental crust.

69 d by the strength heterogeneity of the Asian continental crust.

70 he bulk MgO composition of the Archean upper continental crust.

71 r the Mohorovicic discontinuity in thickened continental crustal regions.

72 Here, we compiled a continental dataset on the distributions of African liza

73 n structure, with all lineages showing multi-continental distributions; demonstrating the highly disp

74 phalt surfaces in North America, east of the Continental Divide, are enriched in petroleum-derived co

75 Conversely, the reason why, in continental domains, co-seismic slip along faults can pr

76 ismic slip propagation during earthquakes in continental domains, possibly enhancing surface displace

77 es dramatically, with the burden shifting to continental East Africa-and away from Madagascar and por

78 nd Albertosaurus--were the apex predators in continental ecosystems in Asia and North America during

79 SITW spatial distribution presents typical "continental effect".

80 be more sensitive than previously thought to continental erosion (providing lithogenic particles to t

81 iogeographically unique regions southeast of continental Eurasia.

82 The absence of the allele in samples from continental Europe (including Scandinavia) at this time

83 ion of the cooling over central and northern continental Europe during the Little Ice Age period (LIA

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

85 sease on oilseed rape was mainly observed in continental Europe, but has recently emerged in the Unit

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

87 partite structure of the YDS in records from continental Europe.

88 portion of ash trees (Fraxinus excelsior) in continental Europe.

89 how faults formed in the earliest phases of continental extension control the subsequent structural

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

91 tral India constitute one of Earth's largest continental flood basalt provinces, whose eruption playe

92 ross-correlation indicates that the state of continental fragmentation at a given time is positively

93 est the hypothesis that temporal patterns of continental fragmentation have impacted global Phanerozo

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

95 There is also evidence to suggest that continental fragmentation promotes increasing marine ric

96 Together, these results suggest that continental fragmentation, particularly during the Mesoz

97 nt Glacier (UFG), Wyoming, is one of the few continental glaciers in the contiguous United States kno

98 with the advance and retreat of Pleistocene continental glaciers.

99 lly closer to Greek-speaking islands than to continental Greece.

100 ra differ substantially among species, human continental groups and even some closely related populat

101 ecially at high latitudes, eventually led to continental ice sheet development in Antarctica in the e

102 he last glacial maximum (LGM), the demise of continental ice sheets induced crustal rebound in tecton

103 During the Last Glacial Maximum, continental ice sheets isolated Beringia (northeast Sibe

104 The past rapid growth of Northern Hemisphere continental ice sheets, which terminated warm and stable

105 f Gulf of Mexico moisture northward into the continental interior from 70,000 to 55,000 years ago bas

106 ll-watered routes into the semiarid and arid continental interior were available throughout the perio

107 elt defines the plate boundaries beneath the continental interior.

108 moving nutrients away from hotspots into the continental interior.

109 s widely but unevenly distributed across the continental interior.

110 We modeled SS precursor waveforms from continental interiors and found a 7 to 9% velocity drop

111 regular vertical profile measurements within continental interiors are more sensitive to regional flu

112 tematic sampling of vertical profiles across continental interiors over the full annual cycle are req

113 cling nutrients from the ocean depths to the continental interiors, with marine mammals moving nutrie

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

115 er loss estimates enable a disaggregation of continental land mass changes and a quantification of th

116 ly discrete LIPs across a large low-latitude continental landmass.

117 Xenoliths suggest a chemical continental lithosphere 175 kilometers thick, whereas s

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

119 for quantifying the dynamic evolution of the continental lithosphere.

120 Farther north, in continental lowlands, numerous high-resolution records o

121 a proxy to track the spatial distribution of continental magmatic arc systems from the Cryogenian per

122 s higher than most DOC fluxes in coastal and continental margin sediments.

123 ith progressive oxygenation of the extensive continental margin.

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

125 Over the continental margins, persistent katabatic winds blow all

126 ralization, either in the water column or at continental margins.

127 high carbon export flux and regions close to continental margins.

128 eawaters that were widespread in Proterozoic continental margins.

129 nland waters would play an important role in continental N-cycling and mitigation of fixed nitrogen t

130 terglaciation, spreading from Alaska through continental North America; they have been continuously r

131 CTI velocity has only been investigated on a continental or national scale.

132 plified due to simultaneous disappearance of continental or sea ice.

133 o far such measurements have been limited to continental-plate boundary zones.

134 r north within the upper plate, where a wide continental plateau forms behind the orogeny.

135 xact thickness and defining mechanism of the continental plates are widely discrepant.

136 gressively less fractionated relative to the continental pool.

137 application of the method for studying four continental populations (European, Asian, African, and N

138 This is the first continental record of its type that clearly demonstrates

139 , the zone of oceanic islands separating the continental regions of Southeast Asia and Australia, has

140 The Amazon rainforest is one of the few continental regions where aerosol particles and their pr

141 Variable contributions differed between continental regions, but major roads within 100 m and sa

142 in the past six decades, especially over the continental regions.

143 ve evolved smaller flight muscles than their continental relatives.

144 Carbonatites, usually occurring within intra-continental rift-related settings, have strong light rar

145 Elevated melt production during continental rifting is likely due to localized thinning

146 welling of the mantle initiates early during continental rifting.

147 Seismic hazard in continental rifts varies as a function of strain accommo

148 is, derived from the weathering of Antarctic continental rocks.

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

150 D-induced impacts on forest C cycling at the continental scale and going beyond single agent-host sys

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

152 spatio-temporal pattern of shifting PPT on a continental scale and its determinants remain unclear.

153 etween markers and ecological variables at a continental scale can help in identifying local adaptati

154 changes in species abundance structures at a continental scale enables robust evaluation of climate c

155 nium (Se) spatial distribution in soils at a continental scale is essential to better understand it's

156 spatio-temporal patterns and drivers at the continental scale remain unknown .

157 underlying genetic and tissue responses at a continental scale that may be responsible for this.

158 understand and describe plant invasion at a continental scale, integrating repeated transport throug

159 Instagram-and quantify landscape values at a continental scale.

160 mpact of climate change on H. contortus at a continental scale.

161 icance of their dry forest at a regional and continental scale.

162 y to study transpiration partitioning at the continental scale.

163 species could potentially be suppressed on a continental scale.

164 climate signal in flood observations at the continental scale.

165 not related to any particular threat at the continental scale; likewise the effect of each stressor

166 Here, we provide a spatially explicit continental-scale assessment of the opportunities for Pl

167 emperate Forests played a major role for the continental-scale carbon balance in 2012.

168 malies are correlated with nest success in a continental-scale database of bird nests, suggesting avi

169 By linking a continental-scale dataset of 533 fish species from 8100

170 These previously unknown continental-scale differences in phenological strategies

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

172 A more stable, continental-scale ice sheet calving at the coastline did

173 Antarctica's continental-scale ice sheets have evolved over the past

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

175 The first continental-scale mineral maps generated from an imaging

176 ecipitation can be important in facilitating continental-scale moisture recycling but are poorly unde

177 We describe continental-scale patterns of recent tree mortality from

178 We investigate the continental-scale relationships between the diversity of

179 oductivity than previously thought, although continental-scale responses are substantial.

180 Using continental-scale sound models, we found that anthropoge

181 explored at local and regional scales, large continental-scale tests are lacking.

182 es from across North America, we partitioned continental-scale variation in biomass growth and mortal

183 Understanding freshwater fluxes at continental scales will help us better predict hydrologi

184 m were rare across Europe, at both local and continental scales.

185 w studies have investigated these impacts on continental scales.

186 latively difficult to measure, especially at continental scales.

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

188 differ from those found in coastal (0-20 m), continental shelf (20-200 m), and upper-slope (200-2,000

189 The SOI continental shelf (~44 000 km(2) ), was less than half c

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

191 the Fukushima plume spread onto the Canadian continental shelf and by 2015 and early 2016 it reached

192 e general knowledge of pristine areas of the continental shelf and identifies the eastern Weddell Sea

193 rrence of types varied, particularly between continental shelf and slope locations.

194 Sharks used both continental shelf areas and oceanic habitats, primarily

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

196 ter (CDW) incursions onto the West Antarctic continental shelf cause melting of the undersides of flo

197 clones that traversed the Mid-Atlantic Bight continental shelf during stratified summer conditions.

198 uitable climatic conditions onto the emerged continental shelf during the LGM, which would have allow

199 rsal, as the hydrodynamic regime of the wide continental shelf has potential to facilitate onshore re

200 ts to predict changes in hypoxic area on the continental shelf in relationship to changes in nutrient

201 The Louisiana continental shelf in the northern Gulf of Mexico experie

202 and surface sediments from the Amundsen Sea continental shelf including the Amundsen Sea Polynya.

203 ntial climate change refugial zone along the continental shelf of Washington State in the Northeaster

204 However, the role of the emerged continental shelf on the Atlantic Forest biodiversity ho

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

206 rogen to inert nitrogen gas are prominent in continental shelf sediments and represent a critical glo

207 isotopes as indicators of CAMP volcanism in continental shelf sediments, the primary archive of faun

208 on, in the 5 mm-250 mum size range, of Irish continental shelf sediments.

209 sediments changed gradually from the Arctic continental shelf to deep-sea basin.

210 tween 80 and 579 m water depth, spanning the continental shelf to the deep suboxic waters of the Sant

211 Continental shelf to upper-slope richness consistently p

212 ave been reported to decrease from the inner continental shelf towards the outer continental shelf.

213 ely more important in samples from Antarctic continental shelf waters, though the difference was not

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

215 on of anomalously warm water masses onto the continental shelf, are hypothesized to contribute to inc

216 States are most prevalent off-shore near the continental shelf-break but are also common near-shore a

217 or a palaeo-subglacial lake on the Antarctic continental shelf.

218 could be as productive as all the remaining continental shelf.

219 the Gulf Stream and northeast United States continental shelf.

220 up to 11 degrees C) over a wide swath of the continental shelf.

221 he inner continental shelf towards the outer continental shelf.

222 delivery of Circumpolar Deep Water onto the continental shelf.

223 nts and bottom water along the western Irish continental shelf.

224 taxa in benthic communities on the Antarctic continental shelf.

225 We reveal 18 continental-shelf and 12 offshore deep-sea realms, refle

226 Permeable sediments are common across continental shelves and are critical contributors to mar

227 ne from thawing subsea permafrost on shallow continental shelves and dissociation of methane hydrate

228 hways in the Arctic where 18% of the world's continental shelves are located.

229 Gas hydrates stored on continental shelves are susceptible to dissociation trig

230 The continental shelves are the most biologically dynamic re

231 It has been known that continental shelves around the Arctic Ocean play a major

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

233 of long-lived and habitat-forming species on continental shelves have attracted particular attention

234 imate, Antarctic ice sheet growth across the continental shelves, and associated seasonal sea-ice exp

235 retentive topographic features, such as wide continental shelves, can function as marine refugia for

236 try and models results, suggest that steeper continental shelves, such as the ones bordering the isla

237 ith the cyclic drowning and emergence of the continental shelves.

238 n stability once the ice sheets have reached continental size.

239 trawl survey at depths of 300-2030 m on the continental slope of the Rockall Trough, Northeast Atlan

240 d densities, confirmed the importance of the continental slope to large delphinoids and of canyons an

241 and dissociation of methane hydrate on upper continental slopes.

242 the observed differentiation of present-day continental Southern Balkan groups.

243 t from habitat filtering, whereby only a few continental species can become established.

244 ily affected Africa, although the origin and continental spread of the disease remain undefined.

245 conflicts, were likely drivers for the cross-continental spread of the HCV epidemics.

246 ccurred independently among each of the five continental superpopulations examined, at times of known

247 from differences in growth and mortality at continental to global scales.

248 and quantifying diffuse contamination at the continental to regional scale is based on the analysis o

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

250 Seismicity along continental transform faults is usually confined to the

251 We compiled a new pan-continental tree-ring width database from sites where bo

252 processes are implemented separately in the continental U.S. and hemispheric CMAQ domains, the latte

253 mbination of these processes within both the continental U.S. domain and from lateral boundary condit

254 We employ EPA's CMAQ model to the continental U.S. during the Southern Oxidant and Aerosol

255 onditions and coastal waters surrounding the continental U.S. is examined using the Community Multisc

256 or the period between 2008 and 2012 over the continental U.S. we also characterized the population si

257 ributor, approximately 72% on average in the continental U.S., to potential aqSOA mass due to Henry's

258 large spatial and temporal scales across the continental U.S.A.

259 lop climatology of smoke occurrence over the Continental United States (CONUS) region and to study th

260 0 hazardous air pollutants (HAPs) across the continental United States (CONUS) to support the 2011 ca

261 hydrologic unit (HUC8) watersheds within the continental United States (CONUS), focusing on the perio

262 errestrial water storage (TWS) change in the continental United States (US) from 2003 to 2012, and es

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

264 virus infection and outcomes reported in the continental United States and Hawaii from January 15 to

265 olar power] across all energy sectors in the continental United States between 2050 and 2055", with o

266 ) riverine total nitrogen loading within the continental United States by the end of the century for

267 Observed temperature extremes over the continental United States can be represented by the rati

268 cies, source sector, and source-state in the continental United States for 2005.

269 esidence PM2.5 exposure estimates across the continental United States for a 2000-2009 follow-up peri

270 We trained the neural network for the continental United States from 2000 to 2012 and tested i

271 re beneficiaries (60,925,443 persons) in the continental United States from the years 2000 through 20

272 seline and policy conditions across the full continental United States to estimate the distribution o

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

274 t the virus, seven of which are found in the continental United States, including Culex quinquefascia

275 Throughout the continental United States, the combination of projected

276 Across the continental United States, there are 1,153-1,359 Tg of S

277 d, shrubland, and grassland sites across the continental United States, to address how edaphic and cl

278 , Colombia, other Caribbean islands, and the continental United States.

279 f surface water and groundwater use over the continental United States.

280 d and nonforested systems across much of the continental United States.

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

282 expansion and now inhabit every state in the continental United States.

283 West Nile virus (WNV) is now endemic in the continental United States; however, our ability to predi

284 -borne ZIKV transmission was reported in the continental United States; since then, hundreds of local

285 site patterns between north and south of the continental US from 2003 to 2012, with the equivalent wa

286 exhibits good correlations with PHDI in the continental US, indicating its feasibility for drought m

287 mer Hydrological Drought Index (PHDI) in the continental US.

288 Samples from the continental USA segregate into a Northeast lineage and a

289 ic, and the first outbreaks were reported in continental USA, Africa, and southeast Asia.

290 clinical infections at endemic sites in the continental USA.

291 Variations in continental volcanic arc emissions have the potential to

292 tent coupled behavior provides evidence that continental volcanic outgassing drove long-term shifts i

293 nearly synchronous with Northern Hemisphere continental warming.

294 the capacity for long-wavelength changes in continental water storage to produce observable surface

295 In addition, continental weatherability has increased 1.7-3.3 times s

296 38)U provides global-scale information about continental weathering and is vital for marine uranium-s

297 The relative influences of tectonics, continental weathering and seafloor weathering in contro

298 a) surface warming is required to double the continental weathering flux, versus 3-10 degrees C in pr

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

300 t of biological invasions before they pose a continental-wide threat.