ライフサイエンスコーパス: shelves

1 directly, mostly through its effects on ice shelves.

2 n satellite imagery across all Antarctic ice shelves.

3 axis and outgrowth of the developing palatal shelves.

4 ick removal of tainted food items from store shelves.

5 surrounding the CpG islands, i.e. shores and shelves.

6 ies from about 10 to 90 per cent between ice shelves.

7 organic carbon burial on drowned continental shelves.

8 anic forcing, especially of the floating ice shelves.

9 modulating the growth orientation of palatal shelves.

10 ciated with defects intrinsic to the palatal shelves.

11 within Earth's subglacial volcanoes and ice shelves.

12 ble in addition to severely deformed palatal shelves.

13 hich are expressed in the developing palatal shelves.

14 n the MEE of the beta-catenin mutant palatal shelves.

15 mal mortalities have occurred on continental shelves.

16 ng centers to pattern the elongating palatal shelves.

17 merging of the mesenchyme from both palatal shelves.

18 nt is not dependent on fusion of the palatal shelves.

19 altered cell proliferation in mutant palatal shelves.

20 shear zones of Pine Island and Thwaites ice shelves.

21 s drastically reduced in Irf6 mutant palatal shelves.

22 nd nutrient-rich deep water onto continental shelves.

23 anterior and middle portions of the palatal shelves.

24 h as the Middle East to offshore continental shelves.

25 during orientation and fusion of the palate shelves.

26 Index, and thinning of southeast Pacific ice shelves.

27 (ECM), and subsequent fusion of the palatal shelves.

28 posture which blocks closure of the palatal shelves.

29 mary defect in the mesenchyme of the palatal shelves.

30 te and fusion of the tongue with the palatal shelves.

31 m resulting from the exposure of continental shelves.

32 r can be used in the farm and on supermarket shelves.

33 elationship varied substantially between ice shelves.

34 itate mass losses by eroding the coastal ice shelves.

35 m the field can be detected on grocery store shelves.

36 tially following the collapse of several ice shelves.

37 sses local to shelf seas surrounding the ice shelves.

38 d marine mammals collected across the Arctic shelves.

39 isms in oceanic cavities below permanent ice shelves.

40 heat transport, causing further melt of ice shelves.

41 mentary denitrification on broad continental shelves.

42 increasing melting on the undersides of ice shelves.

43 C) values accumulated on shallow continental shelves.

44 and carbonate rich (0.037) and poor (0.0002) shelves.

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

46 arly in the posterior regions of the palatal shelves.

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

48 se melting of the undersides of floating ice shelves.

49 elevant to a broad spectrum of Antarctic ice shelves.

50 ic drowning and emergence of the continental shelves.

51 ion and prevent approximation of the palatal shelves.

52 and 3) expression in mouse embryonic palatal shelves.

53 form intermittently on several Antarctic ice shelves.

54 nging ice shelves extending onto continental shelves(8).

55 showed an incomplete closure of the palatal shelves accompanied by a delay in ossification along the

56 Mass lost from West Antarctica's ice shelves accounted for more than 30% of that region's tot

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

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

59 al of the restraining forces of floating ice-shelves after their break-up.

60 omogram from their origins on 14.5-nm-spaced shelves along the thick filament to their thin filament

61 which caused fusion between the -/- palatal shelves also induced the appearance of these filopodia o

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

63 ociated with the collapse of a number of ice shelves and accelerating glacier mass loss.

64 motes greater mass loss by destabilizing ice shelves and accelerating the discharge of upstream groun

65 lting in attenuated outgrowth of the palatal shelves and altered development of cNCC-derived skeletal

66 in the delta(13) C-POC values between arctic shelves and arctic basins likely driven by differences i

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

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

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

70 y important but overlooked process on Arctic shelves and highlights the role of the Arctic as a signi

71 thelium of the horizontally oriented palatal shelves and in the epithelial seam during fusion.

72 ur cycle by reducing the area of continental shelves and increasing the oxidative weathering of pyrit

73 tion and concomitant flooding of continental shelves and interior basins.

74 nt, where expression is found in the palatal shelves and is highest prior to elevation to a horizonta

75 teroposterior axis of the developing palatal shelves and its expression is specifically downregulated

76 m intervals with dispersed continents, broad shelves and moderately extensive continental seas.

77 thelial seam (MES) forms between two palatal shelves and must be removed to allow mesenchymal conflue

78 gen-depleted waters impinging on continental shelves and platforms.

79 resulted in destabilization of grounded ice shelves and possible surging in the Weddell Sea region o

80 nic, and geomorphic processes on continental shelves and provide insight into shelf geochemistry, bio

81 derstanding the catastrophic collapse of ice shelves and rapid hydraulic connection between the surfa

82 ming with hydrofracturing of buttressing ice shelves and structural collapse of marine-terminating ic

83 with the expansion and fusion of the palatal shelves and that Dlx5 is required for the O-N patterning

84 spread over nutrient-rich Arctic continental shelves and that satellite-based estimates of annual pri

85 clusters: Florida together with the Carolina Shelves and the Scotian Shelf.

86 consequence of adhesion between the palatal shelves and the tongue.

87 r to the initial contact of opposing palatal shelves and thereafter selectively disappear from the mi

88 ut this could increase if the retreat of ice shelves and tidewater glaciers further enhances the loss

89 Suture zones are abundant on Antarctic ice shelves and widely observed to impede fracture propagati

90 bsence of the anterior region of the palatal shelves and, subsequently, cleft palate.

91 However, the storage of fresh water in ice shelves and/or groundwater reserves implies that glacial

92 in regions flanking CpG islands (shores and shelves) and gene bodies.

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

94 water discharge from nearby glaciers and ice shelves, and re-examination of some previous diene II do

95 points-local bathymetric highs on which ice shelves are anchored(6).

96 decay over the past 11,000 yr, but these ice shelves are at the climatic limit of ice shelf viability

97 mammals, adhesion and fusion of the palatal shelves are essential mechanisms during the development

98 Arctic where 18% of the world's continental shelves are located.

99 t to mediate palatal fusion once the palatal shelves are placed in close contact in vitro.

100 for the proper growth and fusion of palatal shelves are presented.

101 Altogether, the viruses under Antarctic ice shelves are putatively involved in programming the metab

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

103 Floating ice shelves are the Achilles' heel of the Antarctic Ice Shee

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

105 lankton blooms over Arctic Ocean continental shelves are thought to be restricted to waters free of s

106 in the thickness and extent of Antarctic ice shelves are triggering increased discharge of marine-ter

107 come sequestration because polar continental shelves are typically deeper than most modern iceberg sc

108 s to the expansion and fusion of the palatal shelves are unknown.

109 the buttressing regions of Antarctica's ice shelves are vulnerable to hydrofracture if inundated wit

110 access to grounding lines, glaciers and ice shelves are vulnerable to ongoing increases in ocean tem

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

112 g tissue fusion, using the secondary palatal shelves as a model.

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

114 ssed in the mesenchyme of the murine palatal shelves at E12.5, prior to palate closure.

115 edial halves of the downward growing palatal shelves at E13.5, which results in retarded, mediolatera

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

117 ial tissue of the medial edge of the palatal shelves at the time of shelf fusion in mice.

118 e interior of the Antarctic Ice Sheet to ice shelves, at rates controlled by conditions at the ice-be

119 eaches nearly 12 degrees C by 2300, many ice shelves become non-viable once global warming exceeds 4.

120 n retarded, mediolaterally symmetric palatal shelves before palatal shelf elevation.

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

122 riability in SGL volume is >200% on some ice shelves, but patterns are highly asynchronous.

123 ts of conservative behavior over continental shelves, but the only knowledge we have about removal is

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

125 Floating ice shelves buttress inland ice and curtail grounded-ice dis

126 Antarctic ice shelves buttress the grounded ice sheet, mitigating glob

127 t TGF-beta3 can rescue fusion in -/- palatal shelves by inducing such filopodia, illustrating that th

128 Conversely, 60 +/- 10 per cent of ice shelves (by area) both buttress upstream ice and are vul

129 as, large expanses of productive continental shelves can be vulnerable to the risk of extreme low-oxy

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

131 nd earlier volume gain by East Antarctic ice shelves ceased.

132 helium (MEE) of the developing mouse palatal shelves, consistent with the expression patterns of beta

133 by the thinning and loss of buttressing ice shelves continues for centuries, regardless of bedrock a

134 d from 17 passive margin basins, continental shelves contribute fluid exchanges comparable to hydroth

135 e advection of particulate material from the shelves contributes to scavenging of reactive materials

136 ge of ecosystems, including rocky intertidal shelves, coral reefs, the nearshore ocean, streams, lake

137 Antarctic continental shelves could become sites of significant carbon sequest

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

139 nt cold-cavity Ross, Filchner, and Ronne ice shelves covering two-thirds of the total ice-shelf area

140 of species that live beyond the continental shelves date back more than 60 y, and the sheer size of

141 ponses is not sufficient to induce fusion of shelves deficient in Tgf-beta3.

142 Comparison across a diverse set of ice shelves demonstrates that iceberg calving increases with

143 W toward Antarctica to melt its floating ice shelves, destabilize the glaciers, and raise sea level.

144 the embryonic primary and secondary palatal shelves develop as outgrowths from the medial nasal and

145 al ice cliffs can rapidly collapse after ice shelves disintegrate, as a result of surface and sub-she

146 During embryonic development, palatal shelves display oronasal (O-N) and anteroposterior polar

147 nd the exposure of carbonates on continental shelves due to low sea levels may increase this rate.

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

149 es that drove water into exposed continental shelves during sea-level low stands and active connectio

150 ans were 99.9% covered by light-blocking ice shelves during two discrete, self-reversing Snowball Ear

151 e epithelia with carboxyfluorescein, palatal shelves (E8-9) with or without beak were dissected and c

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

153 ddition, the anterior portion of the palatal shelves emerged from the mandibular arch instead of the

154 ther reduce the buttressing potential of ice shelves, enhancing ice discharge and accelerating the co

155 ss loss and surface elevation change for ice shelves experiencing surface lowering and enhanced disch

156 riods, with grounding lines and fringing ice shelves extending onto continental shelves(8).

157 Pairs of -/- and -/- shelves failed to fuse over 72 hours of culture whereas

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

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

160 feedback potentially preconditions these ice shelves for disintegration and enhances grounding line r

161 nt embryos, the bilateral primordial palatal shelves formed and elevated normally, but they often fai

162 the annual mass budget of all Antarctic ice shelves from 1997 to 2021.

163 s that includes the elevation of the palatal shelves from a vertical to horizontal position, a proces

164 Palatal shelves from E13 mouse embryos were maintained in organ

165 Finally, palatal shelves from prefusion wild-type mouse embryos cultured

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

167 eterozygote) and +/-, as well as +/+ and -/- shelves, fused within the first 48 hour period.

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

169 Mesenchyme of Adamts9(+/-);bt/bt palatal shelves had reduced cell proliferation, a lower cell den

170 ely because the thinning of its floating ice shelves has allowed the outflow of grounded ice to accel

171 The stability of large Antarctic ice shelves has important implications for global sea level,

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

173 mundsen and Bellingshausen regions, some ice shelves have lost up to 18% of their thickness in less t

174 first signs that the shear zones of both ice shelves have structurally weakened over the past decade.

175 ABSTRACT: Continental shelves have the potential to remove atmospheric carbon

176 Some smaller Antarctic ice shelves have undergone periodic growth and decay over th

177 Antarctica's ice shelves help to control the flow of glacial ice as it dr

178 Sedimentation filling space beneath ice shelves helps to stabilize ice sheets against grounding-

179 ea ratio is found for six East Antarctic ice shelves, implying undocumented strong ocean thermal forc

180 the volume flux divergence of Antarctic ice shelves in 2007 and 2008 with 1979 to 2010 surface accum

181 The stability of the Antarctic ice shelves in a warming climate has long been discussed, an

182 mate the mass balance components for all ice shelves in Antarctica, using satellite measurements of c

183 ayed by basal channels beneath Antarctic ice shelves in both ice shelf stability and freshwater input

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

185 regulated in the posterior region of palatal shelves in Foxf2(-/-) mouse embryos.

186 unding Meckel's cartilage and in the palatal shelves in Med23(fx/fx);Wnt1-Cre mutant embryos compared

187 Here, we show that since 1978, ice shelves in North Greenland have lost more than 35% of th

188 of exogenous Tgfbeta3 to the mutant palatal shelves in organ culture rescues the midline seam phenot

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

190 reat and collapse of Antarctic Peninsula ice shelves in tandem with a regional atmospheric warming ha

191 consequence, most maritime glaciers and ice shelves in the region have significantly retreated over

192 possible implication of our data is that ice shelves in this region have been thinning for at least ~

193 escue the fusion between -/- and -/- palatal shelves in vitro, either recombinant human (rh) TGF-beta

194 ionship, or simply increased access on store shelves, in the media, and on the Internet have all led

195 lines and ~60% (>80% by area) develop on ice shelves, including some potentially vulnerable to collap

196 land (increased surface melt), Antarctic ice shelves (increased ocean melting), and Greenland and Ant

197 hering caused by the exposure of continental shelves, indicating that chemical weathering rates remai

198 The Shox2-/- palatal shelves initiate, grow and elevate normally, but the ant

199 ine groundwater contained within continental shelves is a global phenomenon.

200 ring the geological imprint of Antarctic ice shelves is summarised, including advances in dating meth

201 Enhanced basal melting of the ice shelves is thought to be the ultimate driver of change(2

202 t proportion of ice mass loss from these ice shelves is through ocean-driven melting which is control

203 Palatal shelves isolated from Adamts9(+/-);bt/bt mice fused in c

204 aspect of palatal epithelium of the vertical shelves; later in the medial edge epithelium of the hori

205 ould prevent normal elevation of the palatal shelves leading to a cleft palate.

206 um carbonate accumulation on the continental shelves, leading to an increase in pelagic burial via pe

207 Continental shelves likely contribute Ca(2+) and K(+) to the oceans

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

209 At many ice shelves, mass losses due to basal melting or iceberg cal

210 ted, bioturbated sediment under receding ice shelves may oxidize Fe within surface porewaters, decrea

211 t traps along the inner parts of continental shelves, may host significant depositional hotspots for

212 Antarctic ice shelves moderate the contribution of the Antarctic Ice S

213 sheets grew, sea level fell, and continental shelves narrowed.

214 nd that the late-Holocene development of ice shelves near James Ross Island was coincident with prono

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

216 10 small, warm-cavity Southeast Pacific ice shelves occupying 8% of the area.

217 te, that is inadequate fusion of the palatal shelves, occurs with an annual incidence of 1 in 700 to

218 arine heatwaves (BMHW) along the continental shelves of North America.

219 Palatal shelves of Tgfb1 knockin homozygote mice adhere, interca

220 T. nanhaiensis) that inhabit the continental shelves of the East China and northern South China Seas

221 marine prosobranch gastropods living on the shelves of the western Atlantic and eastern Pacific Ocea

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

223 further enhance the vulnerability of the ice shelves off the Antarctic Peninsula.

224 resuspension events on the extensive shallow shelves off the eastern U.S. coast.

225 The continued retreat of ice shelves on the Antarctic Peninsula has been widely attri

226 The collapses of the Larsen A and B ice shelves on the Antarctic Peninsula in 1995 and 2002 conf

227 t warming for several centuries rendered ice shelves on the northeastern Antarctic Peninsula vulnerab

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

229 ost of these glaciers flow into floating ice shelves over bedrock up to hundreds of meters deeper tha

230 Ice shelves play a key role in the mass balance of the Antar

231 dback that may accelerate future melt of ice shelves, potentially further destabilizing the West Anta

232 uce the thickness and extent of floating ice shelves, potentially limiting their ability to buttress

233 Floating ice shelves preserve few direct traces after their disappear

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

235 d near-future ocean warming may push the ice shelves protecting Earth's polar ice sheets into a new r

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

237 The disintegration of ice shelves, reduced sea-ice and glacier extent, and shiftin

238 ically productive Pacific Arctic continental shelves remain underexplored.

239 , and in particular, under the Antarctic Ice Shelves, remains limited.

240 By 2150 and 2300, 26 and 38 ice shelves, respectively, become likely non-viable.

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

242 Ice shelves restrain grounded ice discharge into the ocean,

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

244 recent collapse of the Antarctic Larson ice shelves revealed a slow growing benthic community on the

245 In our exploration, lifting lobate lava shelves revealed adult tubeworms and other vent animals

246 Seafloor imprints of ice shelves should, however, exist where ice grounded along

247 hibit skeletal defects affecting the palatal shelves, shoulder girdle, vertebrae, and sternum.

248 logical examination of the fused +/+ and +/+ shelves showed complete disappearance of the midline epi

249 ral ecosystems in deep waters on continental shelves, slopes, seamounts, and ridge systems around the

250 midline epithelial seam whereas -/- and +/+ shelves still had some seam remnants.

251 n growth or fusion of the developing palatal shelves, submucous cleft palate is characterized by defe

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

253 GL volume on some potentially vulnerable ice shelves, suggesting large increases in SGLs should be ex

254 dict that on large portions of Antarctic ice shelves supraglacial lakes are likely to, on average, st

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

256 The floating ice shelves surrounding the Antarctic Ice Sheet restrain the

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

258 sheet is fringed by vulnerable floating ice shelves that buttress the fast flow of inland ice stream

259 The collapse of ice shelves that buttress(11-13) the ice sheet accelerates i

260 ing ocean waves over the shallow continental shelves that drive the hum of the Earth.

261 For the floating ice shelves that remain we observe a widespread increase in

262 arning, we provide evidence over several ice shelves that the flow law follows a grain size-sensitive

263 s, mainly at the three largest Antarctic ice shelves - the Ross (McMurdo), Filchner-Ronne and Amery.

264 h's climate, as it influences melting of ice shelves, the formation of bottom water, and thus the glo

265 f the nasal septum that fuses to the palatal shelves, the mesenchyme from which tooth buds develop, a

266 As with other ice shelves, the physical processes that led to the activati

267 Product B was removed from store shelves, the public were warned not to eat product B, pr

268 to permit correct positioning of the palatal shelves, the remodeling of the extracellular matrix (ECM

269 However, across the Northeast Atlantic shelves, there has been an ongoing summertime decline of

270 or of each ice sheet and is spreading as ice shelves thin by ocean-driven melt.

271 urface melting and collapse of Antarctic ice shelves, through ocean upwelling in the Amundsen and Bel

272 t palate resulting from a failure of palatal shelves to appropriately elevate and fuse.

273 exencephalic embryos, which allowed palatal shelves to elevate and fuse despite their defect.

274 d the mandible and thereby allow the palatal shelves to elevate, defects similar to those seen in the

275 is due to a failure of the elevated palatal shelves to fuse.

276 he greater horn thereby allowing the palatal shelves to lift and fuse above the flattened tongue.

277 hen it becomes almost impossible for the ice shelves to maintain their present-day shape.

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

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

280 present, collapse of the major Antarctic ice shelves triggers a centennial- to millennial-scale respo

281 Antarctic ice shelves typically comprise continental meteoric ice, in

282 ept for Totten Ice Shelf, East Antarctic ice shelves typically have cold ice cavities with low basal

283 demonstrate that immense, Antarctic-type ice shelves up to 1 kilometre thick and hundreds of kilometr

284 ere warm water at depth can access thick ice shelves via submarine troughs crossing the continental s

285 dhesion and subsequent fusion of the palatal shelves via their medial edge epithelia remain obscure.

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

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

288 For organ culture, palatal shelves were dissected from embryonic day 13.5 (E13.5) m

289 Shelves were placed in homologous (+/+ vs +/+, -/- vs -/

290 Palatal shelves were placed singly or in pairs on Millipore filt

291 cores possibly originated from the Siberian shelves, western Arctic and central Arctic.

292 to date has occurred over polar continental shelves, which are richly, but patchily, colonised by be

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

294 causes melting and ultimately breakup of ice shelves, which could escalate ocean-bound ice discharge

295 targets of YAP/TAZ in the posterior palatal shelves, which included Ibsp and Phex, genes involved in

296 ivide toward the Filchner-Ronne and Ross ice shelves, which initiates grounding-line retreat there.

297 o undergo transformation, and paired palatal shelves with intact beaks do not adhere or undergo trans

298 anterior-posterior patterning in the palatal shelves with respect to TGF-beta3 signaling and the mech

299 es revealed aberrant adhesion of the palatal shelves with the tongue in the anterior and fusion with

300 ilar increase in drawdown, polar continental shelves would represent Earth's largest negative feedbac