ライフサイエンスコーパス: shelf

1 subglacial lake on the Antarctic continental shelf.

2 n amplitude and timing to those on the Sunda Shelf.

3 xy records from Belitung Island on the Sunda Shelf.

4 productive as all the remaining continental shelf.

5 ream and northeast United States continental shelf.

6 current grounding-line position on the inner shelf.

7 Circumpolar Deep Water onto the continental shelf.

8 om water along the western Irish continental shelf.

9 e Kuroshio intrusion onto the East China Sea shelf.

10 hic communities on the Antarctic continental shelf.

11 se melting of the undersides of floating ice shelves.

12 elevant to a broad spectrum of Antarctic ice shelves.

13 logical production, and the melt rate of ice shelves.

14 ic drowning and emergence of the continental shelves.

15 ion and prevent approximation of the palatal shelves.

16 and 3) expression in mouse embryonic palatal shelves.

17 arly in the posterior regions of the palatal shelves.

18 ar tracts of thin ice found on Antarctic ice shelves.

19 those found in coastal (0-20 m), continental shelf (20-200 m), and upper-slope (200-2,000 m) waters.

20 arable to that measured across the wider GBR shelf (9%).

21 Using a simple procedure and off-the-shelf additives and precursors, we developed a structure

22 rotein and mRNA levels peaked as the palatal shelves adhered.

23 ch and conservation efforts: the continental shelf adjacent to east central Florida and the Great Bah

24 n 2008, retailers pulled products from store shelves after reports of bisphenol A (BPA) leaching from

25 We reveal 18 continental-shelf and 12 offshore deep-sea realms, reflecting the wi

26 The presence of coarctation shelf and aortic arch hypoplasia were more common in fet

27 a plume spread onto the Canadian continental shelf and by 2015 and early 2016 it reached (137)Cs valu

28 methylation of probes lying in the shore and shelf and enhancer regions of striatal and cerebellar ge

29 Kuroshio transport, moving it closer to the shelf and enhancing its intrusion into the East China Se

30 s of denitrification and anammox differed in shelf and estuarine sediments from coastal Rhode Island

31 present observations from near Filchner Ice Shelf and from the Filchner Depression, which show that

32 owledge of pristine areas of the continental shelf and identifies the eastern Weddell Sea as a hotspo

33 that allow these sharks to exploit multiple shelf and offshore habitats.

34 on in CpG islands and demethylation at shore/shelf and open sea.

35 pes varied, particularly between continental shelf and slope locations.

36 of glaciers, disintegration of floating ice shelves and a 'greening' through the expansion in range

37 able sediments are common across continental shelves and are critical contributors to marine biogeoch

38 ing subsea permafrost on shallow continental shelves and dissociation of methane hydrate on upper con

39 which is expressed in the developing palatal shelves and encodes another secreted antagonist of canon

40 beneath the floating Pine Island Glacier ice shelf, and constrain the date at which the grounding lin

41 kilometers inland, extend to the continental shelf, and include ocean systems with waters up to 50 me

42 er (PIG) terminates in a rapidly melting ice shelf, and ocean circulation and temperature are implica

43 ctic ice sheet growth across the continental shelves, and associated seasonal sea-ice expansion acros

44 Gas hydrates stored on continental shelves are susceptible to dissociation triggered by env

45 The continental shelves are the most biologically dynamic regions of the

46 ously warm water masses onto the continental shelf, are hypothesized to contribute to increases in th

47 Sharks used both continental shelf areas and oceanic habitats, primarily in the upper

48 It has been known that continental shelves around the Arctic Ocean play a major role in the

49 and led to the growth and fusion of palatal shelves, as marked by an increase in cell proliferation

50 to one year, and displayed (1) predominantly shelf associated activity (2) occupancy of the Yucatan C

51 retreated from the Sabrina Coast continental shelf at least 11 times during the Oligocene and Miocene

52 ly adhesion and fusion of the paired palatal shelves at the midline to separate the oral cavity from

53 clinical use for soft tissue repair, off-the-shelf availability, and zero autogenous donor tissue bur

54 iacaran-Cambrian boundary preserved in intra-shelf basin, slope, and slope basin deposits of the Yang

55 ation of the deep basins as a consequence of shelf-basin exchange.

56 roshio when it flows northeastward along the shelf break in the East China Sea.

57 Although implicated in ice-shelf break up, the consequences of such ponding for ice

58 d larger decreases in the Northeast Channel, Shelf Break, and Central Gulf of Maine.

59 ost prevalent off-shore near the continental shelf-break but are also common near-shore and 2) in imp

60 t that incorporate meltwater's impact on ice shelves, but ignore the movement of water across the ice

61 Because these ice shelves buttress glaciers feeding into them, their ocean

62 and four of their prey in the U.S. Northeast Shelf by examining species overlap under historical cond

63 pographic features, such as wide continental shelves, can function as marine refugia for pelagic faun

64 efficient, safe, and broad-spectrum off-the-shelf cancer immunotherapeutics with no need for a tumor

65 cursions onto the West Antarctic continental shelf cause melting of the undersides of floating ice sh

66 crease in ocean heat influx into ASE sub-ice-shelf cavities took place in the mid-2000s.

67 ascent of the meltwater outflow from the ice shelf cavity triggers a centrifugal overturning instabil

68 ilchner Depression and into the Filchner Ice Shelf cavity.

69 Because ice-shelf channels are loci where intense melting occurs to

70 Ice-shelf channels are long curvilinear tracts of thin ice f

71 inked systems of subglacial conduits and ice-shelf channels have been changing over the past few cent

72 to infer that the morphology of several ice-shelf channels is seeded upstream of the grounding line

73 years ago until 7,500 years ago-when an ice-shelf collapse may have caused rapid ice-sheet thinning

74 This ice-shelf collapse results in an increased flux of ice from

75 ets, forming melt ponds that can trigger ice-shelf collapse, acceleration of grounded ice flow and in

76 This is based on miniature off-the-shelf components such as syringe pumps, valves, and pres

77 tzer), which can be constructed from off the shelf components.

78 o 21d and during subsequent simulated market shelf conditions at 20 degrees C for 5d.

79 However, surface rivers forming on ice shelves could potentially export stored meltwater and pr

80 The hypothesis of a km-thick ice shelf covering the entire Arctic Ocean during peak glaci

81 egions >1-km thick, central Arctic Ocean ice shelf dated to marine isotope stage 6 ( approximately 14

82 ot occupy oxygen impoverished regions of the shelf, demonstrating that oxygen availability (probably

83 metric highs were likely critical in the ice-shelf development by acting as pinning points where stab

84 ncreased nasal septum width, delayed palatal shelf development, and subepidermal blebbing.

85 The number of icebergs produced from ice-shelf disintegration has increased over the past decade

86 red on the ice surface where it triggers ice-shelf disintegration.

87 ical trials that combine allogeneic "off-the-shelf" DRibble vaccines together with antibodies against

88 traversed the Mid-Atlantic Bight continental shelf during stratified summer conditions.

89 atic conditions onto the emerged continental shelf during the LGM, which would have allowed forests a

90 The emergence of continental shelves during ice ages and their flooding during interg

91 arge quantities, easily administered off-the-shelf early after an acute myocardial infarction, comply

92 penetrating radar data from Roi Baudouin Ice Shelf, East Antarctica, to infer that the morphology of

93 gule dispersal for species inhabiting global shelf ecosystems, using a high-resolution global ocean m

94 heet (WAIS) advanced to the eastern Ross Sea shelf edge during the Last Glacial Maximum (LGM) and eve

95 nd spread 120 km apart along the south Texas shelf edge.

96 in the developing palate and mutant palatal shelves elevate above the tongue, demonstrating morpholo

97 prior to the developmental stage of palatal shelf elevation in wild-type littermates, Golgb1 mutant

98 ynamic cellular processes underlying palatal shelf elevation, adhesion, and fusion.

99 ated in playing an important role in palatal shelf elevation-80% of Pax9(del/del);Wise(-/-) double-mu

100 nt embryos have intrinsic defects in palatal shelf elevation.

101 (del/del) embryos exhibit defects in palatal shelf elevation/reorientation and significant reduction

102 mutant mouse embryos exhibit rescued palatal shelf elevation/reorientation, accompanied by restored h

103 factors controlling the East Siberian Arctic Shelf (ESAS) methane (CH4) emissions, yet these factors

104 ntic Layer water, ice sheet, sea-ice and ice-shelf feedbacks, and sensitivity to higher post-MBE inte

105 metres from grounded ice onto and across ice shelves, feeding vast melt ponds up to 80 kilometres lon

106 ation leading to early overgrowth of palatal shelves followed by defects in their horizontalization.

107 f ponding and hitherto used in models of ice-shelf fracture and flow.

108 (+/-12 years); final ungrounding of the ice shelf from the ridge occurred in 1970 (+/-4 years).

109 ic processes, including outgrowth of palatal shelves from the oral side of the embryonic maxillary pr

110 ctor as a key intrinsic regulator of palatal shelf growth and morphogenesis.

111 ultiple transcription factors during palatal shelf growth and patterning.

112 lular and morphogenetic processes of palatal shelf growth, patterning, elevation, adhesion, and fusio

113 Alteration in palatal shelves growth resulted in clefting of the secondary pal

114 es in minutes rather than days using off-the-shelf hardware.

115 d and habitat-forming species on continental shelves have attracted particular attention given their

116 streams, ponds and rivers-on the Nansen Ice Shelf in Antarctica that export a large fraction of the

117 Similar networks are present on the ice shelf in front of Petermann Glacier, Greenland, but othe

118 The Louisiana continental shelf in the northern Gulf of Mexico experiences bottom

119 at the base of the large Filchner-Ronne Ice Shelf in the southern Weddell Sea is currently low, but

120 ased in the posterior regions of the palatal shelves in embryonic day 13.5 Pax9-deficent embryos in c

121 ly to form on a wider range of Antarctic ice shelves in response to climatic warming in forthcoming d

122 (delta(18)O-shell), from the North Icelandic shelf, in relation to seawater density variability and d

123 Relict features on the shelf indicate that these linked systems of subglacial c

124 Geological records from the Sabrina Coast shelf indicate that, in addition to ocean temperature, a

125 undary between grounded ice and floating ice shelf-is underway.

126 r, the first-generation ICG-NPs have a short shelf life (<1 month).

127 antioxidant capacity of food influences its shelf life and human health.

128 iniaturized sensors have demonstrated higher shelf life and stability at temperatures up to 40 degree

129 C-NFs confer high loading capacity, enhanced shelf life and strong antibacterial activity of linalool

130 er harvest and 9months storage plus 7days of shelf life at 20 degrees C.

131 Thus, silk fibroin coatings enhance fruits' shelf life at room conditions by reducing cell respirati

132 nal quality of gluten-free bread during 5day shelf life by means of chemico-physical and nutritional

133 constantly, can extend Tarocco "Sant'Alfio" shelf life enhancing total anthocyanin content.

134 An improved quality benchmarking and shelf life evaluation of freshly harvested black tiger s

135 ivities on-par with benchtop equipment and a shelf life exceeding 6 months.

136 ckaging strategies gave the best result (83% shelf life extension at 25 degrees C).

137 were obtained with 0%O2/40%CO2, promoting a shelf life extension of almost 12 days more comparing to

138 The aim of this study was the shelf life extension of whole-wheat breadsticks through

139 t the rosemary extract addition yields a 42% shelf life extension, higher than that observed using ni

140 sulforaphane significantly increased during shelf life in E. sativa cultivars.

141 le conclusions about the evaluation of a new shelf life indicator.

142 d that altered ripening in WLT fruits during shelf life is probably due, in part, to cold-induced des

143 of 4-37 degrees C, with an estimated ambient shelf life of 200 days.

144 tandard temperature of heat treatment with a shelf life of 21days.

145 d packed in 25mu polypropylene bags showed a shelf life of 21days.

146 s C, and 90% RH for 60days, plus a simulated shelf life of 2days at 20 degrees C.

147 over a commercial storage simulation using a shelf life of 56days at two preservation temperature (7

148 Based on microbiological data, shelf life of beef was 5-6days for AP samples packaged u

149 e, aerobic, vacuum or high O2, to extend the shelf life of beef.

150 ucting multi-site studies and increasing the shelf life of biological data beyond the original study

151 n find their applicability for extending the shelf life of bread by 2 days as compared with the unmod

152 nfluence of the Au/TiO2 on the extending the shelf life of bread was observed.

153 rogels without FA, potentially extending the shelf life of butter.

154 es, thus being a promising way to extend the shelf life of fresh minced meat for about two days.

155 both the elicitors were able to increase the shelf life of fruits as evidenced by the increased level

156 The shelf life of milk and its products is strongly influenc

157 ombination of pretreatment with packaging on shelf life of minimally processed cilantro leaves (MPCL)

158 Furthermore, the shelf life of more than 24 h and the scanning window of

159 quality indicators for the estimation of the shelf life of opened cans using the migration of specifi

160 ctive film was also measured to evaluate the shelf life of packaged meat.

161 d (QIM) to further assess both freshness and shelf life of the studied shrimp samples.

162 Shelf life of the studied shrimp was most likely to be 8

163 Based on safe limits of microbial load, the shelf life of treated juice was extended by 6days as com

164 ed significantly over time and peaked during shelf life storage.

165 , harvesting and processing, with subsequent shelf life storage.

166 Ps were more active and stable with a longer shelf life than native enzyme molecules.

167 This 72 h shelf life under ambient conditions represents an opport

168 Controlling the rate of softening to extend shelf life was a key target for researchers engineering

169 Shelf life was studied at four temperatures (20, 27, 35,

170 r response to achieve stable data, excellent shelf life, and its economical production.

171 technology can be applied to increase their shelf life, as also for phytosanitary purposes.

172 ng mutations' that slow ripening and improve shelf life, but adversely affect flavor and color.

173 L.) are highly perishable and have a limited shelf life, due to postharvest desiccation and senescenc

174 lute need, uncertain daily demand, and short shelf life, platelet products are frequently wasted due

175 e) were used to evaluate chemical effects on shelf life, quality and sensory acceptability of fresh-c

176 to potential overages to cover losses during shelf life, the actual vitamin D concentration of fortif

177 ees C and during cold storage and subsequent shelf life, the main effect being observed for those fru

178 ed significantly after processing and during shelf life.

179 in and fat content) and increase the product shelf life.

180 se found for control fruits at the estimated shelf life.

181 PHNPs showed high serum stability and a long shelf life.

182 control microorganism in order to extend its shelf life.

183 essing technology to improve food safety and shelf life.

184 time could provide a tool for assessment of shelf life.

185 NPs was also evaluated as a means to improve shelf life.

186 index of fresh cut apples and prolonged the shelf life.

187 to compensate for expected losses during the shelf life.

188 idic biochip was found to have a much longer shelf life.

189 the anthocyanin content decreased during the shelf-life (72%) regardless of the treatment.

190 programs aimed to improve fruit quality and shelf-life and for addressing the cultivation of a speci

191 The safety and shelf-life are related to the presence of food spoilage

192 om temperature, RT), was studied to evaluate shelf-life comparatively to refrigeration (RF, 4 degrees

193 dine-doped tomatoes were also maintained for shelf-life concerns.

194 ropical fruit highly perishable with a short shelf-life due to intense metabolic activity after harve

195 der in vitro gastrointestinal conditions and shelf-life during storage were compared with the most co

196 In conclusion, HS increased watermelon juice shelf-life for at least 58days, indicating a great poten

197 play, eight compounds were proposed as odour shelf-life markers.

198 0min can significantly increase refrigerated shelf-life of abalone without affecting chemical or phys

199 d D were the best formulations for extending shelf-life of guava up to 40days versus seven days of un

200 The shelf-life of the compound chocolate with the incorporat

201 hibited specific ripening delay and extended shelf-life phenotypes, including delayed color developme

202 ter quality and health attributes during the shelf-life than did the control samples.

203 ent against lipid peroxidation to extend its shelf-life up to two months.

204 ilized to minimize contamination and enhance shelf-life, and administered intravenously to mimic, lev

205 estigated for five months, under accelerated shelf-life, compared to the synthetic antioxidant, butyl

206 ility, high cost, contamination risks, short shelf-life, low portability, performance variability, an

207 heological properties, sensorial attributes, shelf-life, physical properties such as melting, crystal

208 ging systems on industrial durum wheat bread shelf-life, with regard to thermoformed packaging (TF) a

209 Seafood is highly perishable and has a short shelf-life.

210 be used in acid beverages with an acceptable shelf-life.

211 nt of meat products without shortening their shelf-life.

212 ty traits such as brightness and postharvest shelf-life.

213 store red fresh meat during its refrigerated shelf-life.

214 ontent with no significant variations during shelf-life.

215 serving microbiological safety and extending shelf-life.

216 up to 5.9 +/- 0.2% and stable performance on shelf-lifetime studies at 60 degrees C for at least 280

217 ns where stability, throughput, and extended shelf lives are needed.

218 the most variable in daily usage, have short shelf lives, and are also the most expensive to produce,

219 senescence of flowers thereby reducing their shelf lives.

220 On the shallow shelves (<100 m water depth), methane released from the

221 potential sensitivity of Filchner-Ronne Ice Shelf melt rates to changes in wind forcing.

222 ed compression ratios as compared to off-the-shelf methods such as zip programs.

223 close-up work or finding things on a crowded shelf), mobility (ie, walking down steps, stairs, or cur

224 kkopf (DKK) activity in utero during palatal shelf morphogenesis partly rescued secondary palate deve

225 al morphology of the oesophagus with off-the-shelf non-biological scaffold and stimulation of regener

226 been warm ocean water underneath coastal ice shelves, not a warmer atmosphere.

227 alkenone-inferred Atlantic Water SSTs on the shelf occurred at times of reduced solar activity during

228 dge, forming an ocean cavity beneath the ice shelf, occurred in 1945 (+/-12 years); final ungrounding

229 year hourly time series from the New England shelf of data on the coastal phytoplankter Synechococcus

230 ng grounding zone wedges (GZWs) on the outer shelf of the Whales Deep Basin.

231 metasomatism during rifting of the southern shelf of the Zimbabwe Craton.

232 e change refugial zone along the continental shelf of Washington State in the Northeastern Pacific Oc

233 mness marker SOX2 was altered in the palatal shelves of Tmem107(-/-) animals, and differences in mese

234 However, the role of the emerged continental shelf on the Atlantic Forest biodiversity hotspot of eas

235 exons, 5'UTRs, 3'UTRs, CpG islands, shores, shelves, open seas and FANTOM5 enhancers.

236 experimental results with commercial off the shelf parts are presented which demonstrated non-recipro

237 r plant phenotyping that, relying on off-the-shelf parts, provides an easy to install and maintain pl

238 crocontroller boards and only a few "off-the-shelf" parts to deliver a simple yet powerful EC-SPM equ

239 a unique record close to the Pine Island Ice Shelf (PIIS), that there is considerable oceanic variabi

240 Floating ice shelves preserve few direct traces after their disappear

241 decorin, that were expressed in the palatal shelves prior to adhesion.

242 ver been targeted previously with an off-the-shelf product.

243 of HSCT as an immediately available off-the-shelf product.

244 BsAbs are an "off-the-shelf" product that is easily scalable in contrast to ad

245 and seven interferences chosen from off-the-shelf products.

246 in the caudomedial nidopallium (NCM) and HVC shelf (proper name) but not in the caudolateral nidopall

247 atogenesis occurs when the bilateral palatal shelves (PS), arising from maxillary prominences, fuse a

248 ts the use of shelf-stable and ready-to-use (shelf-ready) reagents to greatly simplify the bioanalysi

249 wide range of target proteins using off-the-shelf reagents.

250 e Bellingshausen, South Georgia and Amundsen shelves, respectively.

251 ntify translatable biomarkers for an off-the-shelf responsive neurostimulation system, we record loca

252 stems, such as on the Larsen C and Amery Ice Shelves, retain surface water at present.

253 sformation is readily promoted by an off-the-shelf [Ru(bpy)3 ]Cl2 6 H2 O complex in air at ambient te

254 tica that export a large fraction of the ice shelf's meltwater into the ocean.

255 teeth, thereby providing a potential off-the-shelf scaffold for whole tooth regeneration.

256 d inventories of DDTs in water of the Arctic shelf seas and the interior basin are presented.

257 ver the past century, are likewise impacting shelf seas worldwide and may increase in the future; the

258 al and geophysical data from the continental shelf seaward of the Aurora subglacial basin, that marin

259 indicators of CAMP volcanism in continental shelf sediments, the primary archive of faunal data.

260 mm-250 mum size range, of Irish continental shelf sediments.

261 behavior across the entire Arctic, in fjord, shelf, slope and open sea, where vertical migrations of

262 potential consequences to the entire Arctic shelf/slope marine ecosystems.

263 dure can easily be implemented using off-the-shelf software and is illustrated using a reanalysis of

264 oach offers a potential of having an off-the-shelf solution for the immediate application.

265 n subglacial drainage, sedimentation and ice-shelf stability.

266 This assay platform exploits the use of shelf-stable and ready-to-use (shelf-ready) reagents to

267 The preparation of shelf-stable crystalline salts of tert-butylmethylphosph

268 ometric log-ratio transform to allow off-the-shelf statistical tools to be safely applied to microbio

269 es of such ponding for ice formation and ice-shelf structure have not been evaluated.

270 ls results, suggest that steeper continental shelves, such as the ones bordering the island of Bonair

271 e rivers could export melt off the large ice shelves surrounding Antarctica-contrary to present Antar

272 onclusions about the efficiencies of off-the-shelf technologies are fundamentally flawed and inaccura

273 nferior in efficiency to alternative off-the-shelf technologies.

274 hermore, using state-of-the-art, yet off-the-shelf telecommunications components, we introduce a cohe

275 re retreat of the Antarctic Ice Sheet if ice shelves that buttress grounding lines more than 800 metr

276 rkedly before 2002 but regularly reached the shelf thereafter.

277 where intense melting occurs to thin an ice shelf, these findings expose a novel link between subgla

278 roviding sufficient back stress to allow ice shelf thickening.

279 LGG in vitro and in vivo, leading to longer shelf time and enhancing the functions of LGG in the gas

280 protection of bioactivity, and steadily long shelf time.

281 hanged gradually from the Arctic continental shelf to deep-sea basin.

282 mporally but also spatially from the shallow shelf to deep-water environments in tandem with progress

283 from beneath a rapidly melting Antarctic ice shelf to identify the mechanism responsible for the dept

284 of the initially vertically oriented palatal shelves to the horizontal position above the embryonic t

285 y Triassic, using multiple sections across a shelf-to-basin transect on the Arabian Margin (Neo-Tethy

286 ds and crevasses can weaken and fracture ice shelves, triggering their rapid disintegration.

287 Here we present an 'off-the-shelf' vascular graft grown from donor fibroblasts in a

288 dielectrics as the sensing layer and off-the-shelf versus IC fabricated transistors as the basis of t

289 drainage could deliver water to areas of ice shelves vulnerable to collapse, as melt rates increase t

290 l profiles from the Central Arctic Ocean and shelf water, snow and meltwater samples were collected i

291 's estuaries, bays, lagoons, inland seas and shelf waters influenced by runoff.

292 ide San Francisco Bay with those in adjacent shelf waters of the California Current System (CCS) that

293 ortant in samples from Antarctic continental shelf waters, though the difference was not statisticall

294 s are relatively well documented on some ice shelves, we have discovered that ponds often form part o

295 a family in front of the Filchner Ronne Ice Shelf (Weddell Sea) by means of quantitative analysis of

296 bon would remain immobilized and the 2.3% of shelf which are shallows could be as productive as all t

297 warming, particularly on the Northeast U.S. Shelf, which is in the southern portion of its range.

298 radar sounding of the Dotson and Crosson ice shelves, which buttress the rapidly changing Smith, Pope

299 uniform change throughout the Northeast U.S. Shelf, while the high-resolution model showed larger dec

300 We show a sea-bed landform imprint of a shelf-wide last glacial advance and progressive deglacia