ライフサイエンスコーパス: shelves

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

2 modulating the growth orientation of palatal shelves.

3 ciated with defects intrinsic to the palatal shelves.

4 within Earth's subglacial volcanoes and ice shelves.

5 ble in addition to severely deformed palatal shelves.

6 hich are expressed in the developing palatal shelves.

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

8 mal mortalities have occurred on continental shelves.

9 ng centers to pattern the elongating palatal shelves.

10 merging of the mesenchyme from both palatal shelves.

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

12 altered cell proliferation in mutant palatal shelves.

13 nd nutrient-rich deep water onto continental shelves.

14 anterior and middle portions of the palatal shelves.

15 h as the Middle East to offshore continental shelves.

16 during orientation and fusion of the palate shelves.

17 Index, and thinning of southeast Pacific ice shelves.

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

19 posture which blocks closure of the palatal shelves.

20 mary defect in the mesenchyme of the palatal shelves.

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

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

23 m resulting from the exposure of continental shelves.

24 se melting of the undersides of floating ice shelves.

25 elevant to a broad spectrum of Antarctic ice shelves.

26 ic drowning and emergence of the continental shelves.

27 ion and prevent approximation of the palatal shelves.

28 and 3) expression in mouse embryonic palatal shelves.

29 arly in the posterior regions of the palatal shelves.

30 form intermittently on several Antarctic ice shelves.

31 axis and outgrowth of the developing palatal shelves.

32 ick removal of tainted food items from store shelves.

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

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

35 anic forcing, especially of the floating ice shelves.

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

96 Antarctic continental shelves could become sites of significant carbon sequest

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

114 Palatal shelves from E13 mouse embryos were maintained in organ

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

144 10 small, warm-cavity Southeast Pacific ice shelves occupying 8% of the area.

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

146 Palatal shelves of Tgfb1 knockin homozygote mice adhere, interca

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

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

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

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

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

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

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

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

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

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

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

158 Floating ice shelves preserve few direct traces after their disappear

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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