ライフサイエンスコーパス: shallow

1 itude of deep water acquisition (WA(deep) ), shallow absorptive root traits (diameter, specific root

2 during childhood, e.g., lack of remorse and shallow affect, are a key risk marker for antisocial beh

3 ied to a groundwater filter collected from a shallow alluvial aquifer in Colorado.

4 n southwestern Pennsylvania where brines are shallow and coal, oil, and gas all have been extracted e

5 eases lower tropospheric diabatic heating by shallow and congestus clouds ahead of the MJO center, en

6 We then use water baths combining shallow and deep areas of arbitrary shapes to spatially

7 This work tests the shallow and deep hypothesis: subsurface vertical chemica

8 In approximation theory both shallow and deep networks are known to approximate any c

9 transmissions and man-made structures in the shallow and deep oceans.

10 ingival samples from healthy individuals and shallow and deep sites from periodontitis patients were

11 subgingival microbiota were observed between shallow and deep sites, at baseline or at 90-days post-t

12 l C(org) sequestration capacity prevailed in shallow and deep vegetated areas (55 +/- 11 and 21 +/- 7

13 A total of 103 sites were studied, including shallow and deepwater offshore platforms and drillships.

14 st in developing specific E2 inhibitors, the shallow and exposed active site has proven recalcitrant

15 The RD was shallow and extended to the anterior equator in 7 eyes a

16 The high concordance between shallow and high coverage data validated the method.

17 This reliance on WM increased in a shallow and linear fashion and was associated with longe

18 a include relatively healthy, well-developed shallow and mesophotic (30-150 m) scleractinian communit

19 The relative local isolation of shallow and mesophotic M. cavernosa populations in Beliz

20 To study the differences between shallow and residual periodontal pockets in patients wit

21 Mean differences between shallow and residual pockets samples, as well as correla

22 when climatological oceanic mixed layers are shallow and winds are weak, but at a time preceding clim

23 nerated surface areas created upon damage by shallowing and widening wounds until healed.

24 derestimates BCP efficiencies when the Ez is shallow, and vice versa.

25 Then, both shallow- and deep-trap-assisted recombination can occur

26 with transport from a deep mafic source to a shallow andesitic reservoir controlled by stresses induc

27 which bound PNAG is weakly associated with a shallow anionic groove on the DspB protein surface with

28 bon (DOC) in groundwater are associated with shallow, anoxic water tables and soils enriched in organ

29 ye leukoma with anterior segment dysgenesis, shallow anterior chamber, and cataract were observed.

30 Pseudoexfoliation eyes without shallow anterior chamber, small pupils, or apparent zonu

31 suggest that the conversion of warm, salty, shallow Atlantic waters into colder, fresher, deep water

32 Shallow atmospheric circulations(6-8) affecting the lowe

33 ly affect multiple trophic levels, including shallow benthic filter-feeding communities, as the coupl

34 s for coastal fishes, drawing larvae towards shallow benthic habitats or inducing settlement.

35 Here, we examine the shallow benthic marine communities preserved in the late

36 nanopore analysis at pH 6.5 shows long-lived shallow blockades with a mean lifetime of 25 +/- 6 s.

37 nspiratory pressure generation and the rapid shallow breathing index) were also assessed.

38 nts) of 11 eyes (6 patients) with MPS VI had shallow but not closed angles (81.8%).

39 C-decoupling between global seawater DIC and shallow carbonate, without burying organic matter or gen

40 We explain elevated [Formula: see text]C in shallow carbonates with a diurnal carbon cycle engine, w

41 come spatial dominants across large areas of shallow Caribbean reefs, where they appear to deter the

42 ump in aniridia 15%, 10%, and 0% (P = .001), shallow central anterior chamber in 22.5%, 22.5%, and 7.

43 servations(9,10) and limited observations of shallow circulations(11) further obstruct our understand

44 odels studied, and is associated with strong shallow circulations.

45 ified within the clays, suggest that similar shallow clay deposits on Mars may contain biosignatures

46 regularized models significantly outperform shallow CNNs as well as k-mer methods in the discovery o

47 Pegmatites are shallow, coarse-grained magmatic intrusions with crystal

48 vessels with and without AIS (non-AIS) in a shallow coastal area within the Inner Danish waters.

49 ish exponentially, and are maximal only in a shallow coastal fringe.

50 fer velocities and (b) in a field study in a shallow coastal lagoon covering a range of transfer velo

51 Antarctic shallow coastal marine communities were long thought to

52 Shallow, coastal waters identified here should be consid

53 However, shallow complex structures and weathering layers at near

54 S) is a predominantly benthic forager on the shallow continental shelf of Bass Strait, and represents

55 metimes they talk past each other, make only shallow contributions, or make contributions that are un

56 ehaviour is further linked to differences in shallow convection, thus providing a focus for accelerat

57 nge-related coral mortality cause changes in shallow coral reef community structure through phase shi

58 entire communities, including in the case of shallow coral reefs the potential overgrowth of algae.

59 reefs may escape heat stress experienced by shallow corals.

60 sediments is understudied relative to their shallow counterparts, and this lack of understanding ham

61 formation to detect amplification quality in shallow coverage sequencing data.

62 the major regional Garlock fault, triggering shallow creep and a substantial earthquake swarm.

63 mation rate and mechanical properties of the shallow crust affect fault behavior.

64 he widespread hydrothermal alteration of the shallow crust caused by the intrusion of dikes and sills

65 aults slip and distribute deformation in the shallow crust hinders efforts to mitigate hazards where

66 s power the biogeochemical cycles of Earth's shallow crust, supporting life, stimulating substrate tr

67 660 kilometers) unaffected by degassing and shallow crustal contamination.

68 rt by aqueous fluids is a dynamic process in shallow crustal systems, redistributing nutrients as wel

69 Their stratigraphic context reveals upward-shallowing cycles from mud to interlaminated mud-magadii

70 f extreme size, Antarctic blue whales target shallow, dense krill swarms to maximise their energy int

71 s across the channel upon interaction with a shallow (depth ~ 700 nm) inclined guiding track ablated

72 on-land analog of the modern splay fault at shallow depths (~ 8 km) in the Nankai Trough.

73 Extreme slip at shallow depths on subduction zone faults is a primary co

74 ting females mainly rest while stationary at shallow depths within reach of the hull of commercial sh

75 c carbon in soils, and suboxic conditions at shallow depths, which suggested that denitrification in

76 st reptiles at a desert site overwintered at shallow depths.

77 across Canada, encompassing >1300 samples of shallow discharging groundwater collected principally du

78 The observed shallow distance dependence for tyrosine oxidation is pr

79 The shallow distance dependence observed here and extensions

80 these insights, this theory predicted a less shallow distance dependence of the PCET rate constant wh

81 ten exhibit complex shapes, which range from shallow domes to elongated tubular or pearl-like structu

82 ow that the presented technique yields ultra-shallow dopant profiles localised to the top few nanomet

83 wo-level atomic tunneling system exists in a shallow double-well potential of the Ti atom and is of s

84 Jackson shark Heterodontus portusjacksoni, a shallow-dwelling benthic species and generalist predator

85 otein-protein interfaces that involve large, shallow, dynamic, polar, and water-exposed protein surfa

86 ensitivity at Axial Volcano results from the shallow earthquake depths.

87 l simulations for a desert site predict that shallow ectotherms have increased opportunities for mid-

88 In warm localities shallow ectotherms have lowest energy costs and largest

89 acoustic waves (SAWs) strongly modulate the shallow electric potential in piezoelectric materials.

90 Although point defects often induce only shallow electronic states in the perovskite bandgap that

91 First, a shallow energy level traps a photoexcited electron.

92 originate from Si and C impurities occupying shallow energy levels in the bandgap.

93 t it at an advantage over other species from shallow epicontinental environments with higher metaboli

94 ecognizing domain that is characterized by a shallow epitope lacking defined binding pockets.

95 y on surfaces through partial confinement on shallow external-surface pockets, which are accessible t

96 CCL20 binds in a shallow extracellular pocket, making limited contact wit

97 each dominated by either co- or post-seismic shallow fault slip.

98 seismic data, finite element models indicate shallow faulting is more sensitive to lithologic layerin

99 d plasticity of WA(deep) were not related to shallow fine root economy traits, suggesting independent

100 ate, while overestimating nitrate removal in shallow flow paths.

101 w that this species is limited to narrow and shallow flowing waters with rapids and boulders.

102 At a depth that is too shallow for hydrate formation, existing theories suggest

103 ic diatoms are the main primary producers in shallow freshwater and coastal environments, fulfilling

104 Analysis of fragment length profiles by shallow genome-wide sequencing (<0.2x coverage) of host

105 motaxis assay in a 3D matrix, we show that a shallow gradient of 12-S-HETE enhances chemotaxis toward

106 leading edge of fibroblasts responding to a shallow gradient of PDGF, signifying polarization.

107 n initially positioned between a steep and a shallow gradient that rose in opposite directions, parti

108 en exposed to a steep gradient compared to a shallow gradient.

109 angstrom and the G-protein-binding site is a shallow groove rather than a cleft.

110 onsisting of two protofibrils separated by a shallow groove.

111 an buffer plant water stress; but only where shallow groundwater connections are present, and not ind

112 that high nitrate concentrations in modern, shallow groundwater have been sustained for decades, pos

113 , longer-chained hydrocarbons) dissolve into shallow groundwater or pass through groundwater systems

114 the balance between water supply and demand, shallow groundwater storage can buffer plant water stres

115 The direct response of shallow groundwater storage to warming demonstrates the

116 centrations of these constituents in modern, shallow groundwater than in older, deeper groundwater at

117 rologic model to evaluate the sensitivity of shallow groundwater to warming across the majority of th

118 o flow depletion caused by surface water and shallow groundwater withdrawals, especially in a high-wi

119 orts manganese reduction and mobilization in shallow groundwater.

120 fecal indicator bacteria (FIB) leaching into shallow groundwater.

121 sidies are not rare, occurring most often at shallow, heavily exploited seamounts, suggesting an impo

122 lass-specific connections are organized in a shallow hierarchy within the mouse corticothalamic netwo

123 iment oxygen fluxes, the main oxygen sink in shallow hypolimnia.

124 obial activity typically associated with the shallow HZ.

125 structure due to its sampling limitation and shallow imaging depth.

126 However, it becomes shallow in the sense that the rate of escape from this s

127 resist coated GaAs and developed followed by shallow inductively coupled plasma etching.

128 al and hydraulic applications concerned with shallow inertial flows.

129 es reveal cryptic druggable hot spots in the shallow inhibitor binding site of MraY that were not pre

130 Shallow invasion increases the risk of pregnancy complic

131 We term these collective features as a shallow, irregular RPE elevation (SIRE).

132 ogical time lags in the transient phase of a shallow lake highlights opportunities for restoration th

133 Here we used a shallow lake mesocosm experiment to test the combined ef

134 ce are uncommon, likely restricted to select shallow lakes directly exposed to urban or agricultural

135 hat allocation to deep roots traded off with shallow lateral root investment, and that drought-sensit

136 In this report, we show first results of shallow layers of NVs created using plasma immersion ion

137 oduce several per mil isotopic excursions in shallow lentic and lothic inland waters of high-latitude

138 in plagioclase after stalling and cooling in shallow-level chambers.

139 with the highest probability of detection at shallow, low-latitude seamounts.

140 s around 17% of Pacific seamounts and 45% of shallow (< 100 m) seamounts, with the highest probabilit

141 constraints, are typically most sensitive to shallow (<5 km) storage and/or have insufficient resolut

142 ferentiation was observed between relatively shallow M. cavernosa populations (10 m, 16 m) and relati

143 gnificant genetic structure across the seven shallow M. cavernosa sampling sites, the SNP analyses re

144 imbalanced learning problem; but few current shallow machine learning-based methods are designed to h

145 Moreover, DeepEP is better than shallow machine learning-based methods.

146 DystoniaNet significantly outperformed shallow machine-learning algorithms in benchmark compari

147 are described for the first time in historic shallow marine backwash deposits and lead us to propose

148 Sheltered shallow marine environments in areas repeatedly impacted

149 idation at the sediment-water interface of a shallow marine methane seep.

150 an by illustrating that it took place on the shallow marine shelf coevally with deeper water, below-w

151 cologic window established in an oxygenated, shallow-marine environment represents an exceptional rec

152 tinuous 800-metre-thick Pliocene sequence of shallow-marine sediments from Whanganui Basin, New Zeala

153 re photochemically impacted MeHg, supporting shallow MeHg production and bioaccumulation in high Arct

154 confined particles with various shapes in a shallow microfluidic channel via stop flow lithography.

155 ansition, at a critical Debye length, with 2 shallow minima of the order of thermal energy at L/W >>

156 e 'radiogenomic' studies often use linear or shallow models, depend on feature selection, or consider

157 Much higher nitrate concentrations in shallow modern groundwater were observed at both the Col

158 e eACC, showed substantial responses even at shallow modulation depths.

159 in lobster settlement densities observed at shallow monitoring sites correlate with the expanded are

160 mples, this confirms that the deep plume and shallow MORB mantles have remained distinct from one ano

161 In shallow mucus films, we observe bacteria reversing their

162 Florida Bay is home to a network of shallow mud-banks which act as barriers to circulation c

163 serology-positive cases were mostly flat to shallow (n = 18/26), medium-sized (n = 19/26), and eithe

164 an intensification in the stratification of shallow nearshore waters (0-200 m), that affects both th

165 tor characteristics of most neurons define a shallow network architecture of the pharyngeal connectom

166 We show that the LFL of a DNN in the shallow network or data-abundant limit is funneled, and

167 We used machine learning (shallow neural network) to assess the statistical signif

168 ells search for resources by chemotaxis in a shallow, noisy gradient.

169 proves when escalating from linear models to shallow-nonlinear models, and further improves with deep

170 Applications to shallow NVs could capitalize on the greater physical pro

171 This causes a shallowing of the MLD which prevents nutrients from reac

172 Such a scenario implies expansion and shallowing of the oxygen minimum zone across a very broa

173 nation, regardless of whether they introduce shallow or deep trap states.

174 g gases per impactor mass than either a very shallow or near-vertical impact.

175 to show that the short cycles were driven by shallow outgassing, whereas longer cycles were pressure-

176 oxic environments, which differ greatly from shallow oxic environments where U(IV) is readily reoxidi

177 We found shallow Palaearctic population structure in subpolar bog

178 Additionally, a shallow palatal vault height (PVH) was associated with a

179 weighted Unifrac places more emphasis on the shallow parts of the phylogeny.

180 ed that overcomes the limitations imposed by shallow penetration depth of ultraviolet excitation, pho

181 er in 22.5%, 22.5%, and 7.5% (P = .003), and shallow peripheral anterior chamber in 65%, 60%, and 17.

182 highly crystalline, with mush regions in the shallow plumbing system, where an exsolved volatile phas

183 ere also found in the functionally-validated shallow pocket of other KREPs including that of the canc

184 the last six residues of P11 inserted into a shallow pocket on Stx2A1 and interacted with Arg-172, Ar

185 conserved patch in K13 KREP overlaps with a shallow pocket that displays a differential electrostati

186 tural destabilization of KREP but not in its shallow pocket.

187 atic linkers direct the capping group toward shallow pockets defined by the L1 loop, the L2 loop, or

188 ng a large internal cavity, interacting with shallow pockets that can influence selectivity.

189 centrations of IL-1beta and IL-6 in GCF than shallow pockets.

190 rcass was buried could be characterized as a shallow pond or lake inhabited mainly by taxa which are

191 estyle is adapted to the ephemeral nature of shallow pools on the African savannah.

192 he occurrence of the giant earthquake at the shallow portion of the megathrust may be attributed to t

193 inding site of Hsp90 cochaperones includes a shallow, positively charged groove that poses a signific

194 icles (10% greater overall biomass) than the shallow prey layer.

195 obscured by overprinting of deep signals by shallow processes.

196 mally high threshold values (P = 0.0053) and shallow psychometric slopes in patients (P = 0.0015).

197 ltant estimated accretion rates (EAR) of the shallow reef zone of leeward Bonaire - between 5 and 12

198 ommunities over five years at three sites on shallow reefs (~9-m depth), and test for the effects of

199 In this ~40 y study of shallow reefs in the eastern Indian Ocean, we show that

200 We used a temporal dataset from shallow reefs in the northern GBR to estimate coral conv

201 rf algae and Halimeda, but absolute cover on shallow reefs increased annually by 1.3% (east), 2.3% (w

202 evious similar measurements from aquaria and shallow reefs using a standard benchtop system.

203 ) larger corals have higher disease risk; 2) shallow reefs with low herbivorous fish abundance, limit

204 cult accessing or surviving in wave-battered shallow reefs.

205 misrepresentation of heat stress exposure at shallow reefs.

206 ectotherms overwintered: on warm days, only shallow reptiles could detect warming soils and become a

207 cquisitive deep roots were more crucial than shallow roots in shaping species' extreme isohydric beha

208 fter a period when magadiite precipitated in shallow saline waters.

209 n endorheic (limited drainage) basin and has shallow, saline-alkaline waters.

210 nd younger and was formed on what was once a shallow sea.

211 ironments, including sulfidic karst systems, shallow-sea hydrothermal vents, sites of acid mine drain

212 These refuges were identified as remote and shallow seabed features, such as seamounts, submerged ba

213 We estimate that shallow seagrass meadows (<5 m depth) had significantly

214 sign and lag between the time series, either shallow sealing or magma influx could drive Domuyo's ong

215 ement paths were spatially structured around shallow seamounts (<200 m).

216 me significantly increased with proximity to shallow seamounts, while dive depth increased in the vic

217 Full recovery at the shallow seaward locations may take at least five more ye

218 residue-residue contact prediction even for shallow sequence alignments.

219 ng budget: deep sequencing of a few cells or shallow sequencing of many cells?

220 Qualities were estimated from shallow sequencing with coverage as low as 0.3x per cell

221 udy serpentinization in the mantle wedge and shallow serpentine alteration to authigenic clays by sea

222 Despite substantially less effort in the shallow-set sector of the fishery (~60 m depth), DFG sta

223 ) and favour the abiotic genesis of CH(4) in shallow settings.

224 n precipitation around chert granules on the shallow shelf of one of the oldest supracratonic environ

225 In each patient, a palatal shallow site (<=3 mm) and a residual site (>=5 mm) were

226 Trench subduction zone, which hosted 50 m of shallow slip during the M(w)9.1 2011 Tohoku-Oki earthqua

227 ecessarily determine the likelihood of large shallow slip or seismic hazard.

228 reat earthquake seismicity that caused large shallow slip.

229 ental profiles started off with surprisingly shallow slopes that seemed to defy the quasi-exponential

230 n-cycle hysteresis that is most amplified in shallow, sluggishly mixed waters with high rates of phot

231 ude and plasticity of WA(deep) interact with shallow soil and aboveground resource acquisition traits

232 Further analysis indicated that improved shallow soil connectivity conditions might enhance the w

233 nductivity (EC) (negative) in the relatively shallow soil profile (up to 40 cm).

234 inated with their water foraging capacity in shallow soil, the more acquisitive deep roots were more

235 f soil resource acquisition between deep and shallow soil.

236 etabolism and carbon degradation in deep and shallow soils, respectively.

237 ermogenic CH(4) (2.6 mg/L) from a relatively shallow source (Catskill/Lock Haven Formations) that app

238 dives; averaging depth of 260.4 m) and short shallow Square-shaped dives (16%; averaging depth of 22.

239 a framework to understand U mobility in the shallow subsurface, and, in particular, emphasizes roles

240 Second, in marine systems, shallow subtidal and intertidal areas will experience th

241 nt of a cohort of Mytilus cf. platensis in a shallow subtidal habitat of the South Shetland Islands i

242 ced microbial methane production with a very shallow sulphate-methane transition zone.

243 periods, and how topographic affiliation (to shallow - SWTs - or deep - DWTs - water tables), togethe

244 ional Park suggest that the ratio of deep to shallow taproot diameters provides a reasonable proxy fo

245 We found that in shallow temperature gradients with narrow temperature ra

246 loidal nanoparticle onto a substrate using a shallow-template-assisted, DNA-mediated assembly approac

247 The liquid layer is shaped like a shallow tent with its height at the center set by the se

248 When traveling along a shallow thermocline, these waves can reach past topograp

249 optical fibers that can only interface with shallow tissue volumes adjacent to the fiber.

250 -from the tropics to high latitudes and from shallow to deep water-which better align with species di

251 ivity and 3 orders of magnitude longer-lived shallow-trapped charges.

252 provide consistent evidence that long-lived shallow-trapped electrons that exist at about the micros

253 6, a small single domain protein harboring a shallow trefoil knot, we allow the protein to refold fro

254 s, lead to the formation of massive reefs in shallow tropical and subtropical seas.

255 in allowing corals to dominate nutrient-poor shallow tropical seas worldwide.

256 sed the possibility of cancer prognosis with shallow tumor RNA-seq, which would potentially enable co

257 We found generally shallow U-shaped relations between GWG z score and SMM i

258 quencies were largest for aquifers with more shallow, unconfined wells producing modern-age groundwat

259 osition of the posterior lens capsule, and a shallow unilateral optic disk excavation.

260 , there was no difference in selectivity for shallow- versus deep-diving gentoo penguins.

261 ive relationship between export patterns and shallow-versus-deep concentration contrasts, underscorin

262 has been proposed that rainfall can modulate shallow volcanic activity(2,3), but it remains unknown w

263 urbation has amplified chemical contrasts in shallow water (e.g., soil water) versus deep waters (e.g

264 ms to be a prerequisite for the formation of shallow water aragonite-rich sediments on the NWS.

265 a linear array of hydrophones was built in a shallow water area to experimentally investigate the pro

266 as been shown to have serious impacts on the shallow water areas adjacent to waterways.

267 dox assumes that the [Formula: see text]C of shallow water carbonates reflects the [Formula: see text

268 nstrating the potential application to other shallow water ecosystems and chemical species.

269 Atlantic margin using new shallow water electromagnetic geophysical methods.

270 ns within phoshorites indicates reworking in shallow water environments.

271 We model the vortices using the shallow water equations, which describe a single layer o

272 disproportionately high emissions from large shallow water facilities.

273 d apposition eyes suggests an allochthonous, shallow water origin.

274 actors that both underestimate emissions for shallow water platforms and do not account for dispropor

275 t laboratory experiments in weakly turbulent shallow water reveal a remarkable transition from Gaussi

276 stent with recent laboratory experiments for shallow water waves across an abrupt depth change, where

277 maritime economies will suffer as monitored shallow water young-of-year lobsters decline and landing

278 the GHGI in deep water but appear higher for shallow water.

279 ce of atmospheric methane in terrestrial and shallow-water areas; in deep-water areas, in contrast, h

280 The orange coral Astroides calycularis is a shallow-water bioconstructor species endemic to the Medi

281 ilience, these communities differ from other shallow-water carbonate ecosystems, such as reef communi

282 virtually unexplored in comparison to their shallow-water counterparts.

283 Light levels in terrestrial and shallow-water environments can vary by ten orders of mag

284 sity in some abyssal regions exceeds that of shallow-water environments.

285 trophic relationships and the oxygenation of shallow-water habitats required for the subsequent ascen

286 Shallow-water marine organisms are among the first to su

287 they had moderate emission rates compared to shallow-water sites.

288 e dominated by low-relief wetlands and other shallow-water systems, are accumulating Hg and MeHg.

289 he vicinity of navigation channels in a wide shallow waterbody.

290 ence, with dolphins showing a preference for shallow waters (5-15 m) less than 2 km from the coast.

291 ld have formed abiotically on the surface in shallow waters and on continents during the Archean eon

292 They start in very shallow waters at the shelf break and reach deeper water

293 oppler current profiler (ADCP) at relatively shallow waters off the west coast of Ireland.

294 nhancements also suggests a source region in shallow waters.

295 PolGZ and NoPolGZ crowns exhibited shallow wear scars, where material loss remained within

296 and, on farms with seasonal pans (temporary, shallow wetlands) and perennial rivers and in recently v

297 single nucleotide polymorphisms derived from shallow whole-genome sequencing of 468 Eucalyptus polybr

298 Shallow whole-genome sequencing of 777 biopsies, sampled

299 We performed whole-exome and shallow whole-genome sequencing to identify genes and pa

300 onary age of interacting species, plumage at shallow (within-family) timescales, and song at deeper (