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1 elate with temporal variation in volcanic or metamorphic activity.
2         The MGC forms during early stages of metamorphic adult development through a stereotyped sequ
3 sets of centrally derived glial cells during metamorphic adult development.
4 om a bilaterally organized larva into a post-metamorphic adult with pentaradial body symmetry.
5  contributed by met: continuous variation of metamorphic age and expression of discrete, alternate mo
6  Bd infection is limited to the skin in post-metamorphic amphibians, routine skin sloughing may regul
7 evolution of novel paedomorphic species from metamorphic ancestors via selection of TH-response allel
8 val period, is rapidly elaborated during the metamorphic and early juvenile periods to form the adult
9 ed in our work emphasize the need to include metamorphic and fluid transport processes in geodynamic
10                                         Both metamorphic and igneous models of apatite formation sugg
11 lpha and TRbeta genotypes was determined for metamorphic and non metamorphic offspring from backcross
12 iscrete, environmentally induced phenotypes: metamorphic and paedomorphic individuals.
13 amorphic core complexes are domal uplifts of metamorphic and plutonic rocks bounded by shear zones th
14 to FV3 kidney infections than cohort-matched metamorphic and postmetamorphic froglets and that this r
15 mental expression of Sox2 and Sox19 genes in metamorphic and postmetamorphic specimens and young adul
16 age specificity is reiteratively used during metamorphic and reproductive responses to ecdysone.
17 re completed in bedrock composed of granite, metamorphic, and mafic rocks.
18 s are subdivided into four types: A-1 (tuff, metamorphic, and magmatic rocks-dominated gravel-support
19  this study we present new in situ U-Pb age, metamorphic, and morphological data on these titanite mi
20  including obligate metamorphic, facultative metamorphic, and obligate metamorphic-failure taxa.
21 using the characteristics of the surrounding metamorphic aureole, and apply it to the Skiddaw granite
22 e introduce a computational model to predict metamorphic behavior in proteins using only knowledge of
23 %, suggesting that it is possible to predict metamorphic behavior in proteins using only sequence inf
24 e information critical for understanding the metamorphic behavior of RfaH and other chameleon protein
25  outgassing from ocean ridges, volcanoes and metamorphic belts and increased carbon burial.
26 re as metamorphic T/P) in the form of paired metamorphic belts(5), which is attributed to metamorphis
27 gle InAs/GaAs quantum dot grown on an InGaAs metamorphic buffer layer emitting photons in the C-band.
28  phase equilibria modeling predicts that the metamorphic carbon flux was likely ~1.7 times greater in
29                                     Although metamorphic cell death is perturbed in Atg7 mutants, the
30 ic profile of bite-force performance in post-metamorphic Ceratophrys cranwelli.
31                           In winged insects, metamorphic changes either are limited to a few tissues
32  process reported to date in the sequence of metamorphic changes in anurans.
33                                              Metamorphic changes in the amphibian olfactory system pr
34 d D2 expression contributes to the timing of metamorphic changes in these tissues.
35 ndicate that the intestine undergoes similar metamorphic changes in X. laevis and X. tropicalis, maki
36 alpha are resistant to a wide variety of the metamorphic changes induced by TH.
37 luding wing discs and eye primordia initiate metamorphic changes, such as pupal commitment, patternin
38  growing tissues nearing completion of their metamorphic changes, suggesting a role for the deiodinas
39                  XCL1/lymphotactin, a unique metamorphic chemokine, was recently identified as a broa
40 n mRNA is down regulated at the beginning of metamorphic climax (NF62) and reexpressed again near the
41  TH secretion) but was present just prior to metamorphic climax (stage 58, during TH secretion).
42  peak concentration of T4 that is reached at metamorphic climax cannot induce the final morphological
43 re down-regulated in the tail at the peak of metamorphic climax just before it is resorbed are suppre
44                                       During metamorphic climax when the exocrine pancreas dedifferen
45 e development of the coccyx initiates before metamorphic climax whereas the ossifying hypochord under
46                                       During metamorphic climax, best frequencies significantly incre
47                                           At metamorphic climax, both TH-induced cell division and D2
48                                           By metamorphic climax, limb movement is impaired, ranging f
49                                   Before the metamorphic climax, most of the cells have already trans
50                  Shortly before the onset of metamorphic climax, there is a brief "deaf" period durin
51 definitive nuclear configuration through the metamorphic climax.
52 loproteinase 11) in the exocrine pancreas at metamorphic climax.
53 s lateral line projections degenerate during metamorphic climax.
54 rmis and finally appears in the tail only at metamorphic climax.
55 evelopment revealed greater expression after metamorphic climax.
56 as soon as they became free-swimming through metamorphic climax.
57 rphic CO(2) release; thus, it is likely that metamorphic CO(2) degassing has not been constant throug
58  exert a strong control on the efficiency of metamorphic CO(2) release; thus, it is likely that metam
59                        An extended period of metamorphic competence is an adaptive feature of numerou
60 fifth instar and coincided with the onset of metamorphic competence of these discs.
61                                          The metamorphic conditions and mechanisms required to induce
62 ng Laramide orogenesis, consistent with peak metamorphic conditions and synchronous peraluminous gran
63 nd TC if the temperature and age at the peak metamorphic conditions are known.
64                                          For metamorphic conditions of cooling from 612 degrees +/- 1
65 ions in metasomatized ophicarbonates at peak metamorphic conditions.
66 e possible only with moderate diagenetic and metamorphic conditions.
67  readily react with their wall-rocks forming metamorphic contact aureoles.
68 as that underlie the detachment fault in the metamorphic core complex of the Whipple Mountains yielde
69 t, at least in this case, the development of metamorphic core complexes and the accommodation of high
70                                              Metamorphic core complexes are domal uplifts of metamorp
71 ections and stress magnitudes in the belt of metamorphic core complexes during topographic collapse.
72          Here we develop a general model for metamorphic core complexes formation and demonstrate tha
73 nds of Papua New Guinea are actively forming metamorphic core complexes located within a continental
74 ast, here we present seismic observations of metamorphic core complexes of the western Woodlark rift
75 tinental domain allowed for the formation of metamorphic core complexes, boudinage of the upper crust
76 r crust exhumes mid-crustal rocks, producing metamorphic core complexes.
77 es have addressed this problem and therefore metamorphic decarbonation in subduction zones remains la
78 he CO(2) in subducting crust is released via metamorphic decarbonation reactions at forearc depths.
79 , both of which would be expected to enhance metamorphic decarbonation.
80 geogenic methane oxidation, and volcanic and metamorphic degassing.
81 to high pore pressure that might result from metamorphic dehydration.
82 tinental foreland basin sediments containing metamorphic detritus eroded from the Himalaya orogeny th
83             The effects of BR-C mutations on metamorphic development are highly pleiotropic, yet litt
84 iscs showed that BRC-Z1 expression and early metamorphic development are rendered steroid-independent
85                                        Early metamorphic development in Drosophila melanogaster is in
86 sted the hypothesis that BRC is required for metamorphic development of MN1-MN5.
87 med cell death (PCD) of neurons during early metamorphic development of the central nervous system (C
88 n the glomeruli during the last one-third of metamorphic development were revealed.
89                   During the final stages of metamorphic development, auditory function and neural co
90                                       During metamorphic development, ranid frogs exhibit rapid reorg
91 quire significant planetesimal degassing, as metamorphic devolatilization on chondrite-like precursor
92                Here, we show that this shock metamorphic dichotomy is a consequence of impact-driven
93 in the developing Drosophila eye is an early metamorphic, ecdysteroid-dependent event.
94  distinct populations of melanophores: early metamorphic (EM) melanophores arise widely dispersed and
95                          Smoltification is a metamorphic event in salmon life history, which initiate
96   A full characterization of low-temperature metamorphic events and alternative biosignatures in gree
97 u geochemistry will allow us to date ancient metamorphic events and determine the terrestrial Pu/U ra
98 enes have putative functions relevant to key metamorphic events including the differentiation of smoo
99  an ancient martian meteorite record thermal metamorphic events with ages that group around and/or do
100 on formation and axonal outgrowth, two early metamorphic events, also occur prematurely.
101               It is commonly employed during metamorphic events, such as the tissue thinning coupled
102 e established a sequence of bacteria-induced metamorphic events: MACs induce larval settlement; then,
103 an obligate metamorphic-failure species) and metamorphic F1 hybrids (A. mexicanum x A. tigrinum tigri
104 d salamander populations, including obligate metamorphic, facultative metamorphic, and obligate metam
105 mode of development that is characterized by metamorphic failure (paedomorphosis), an adaptation for
106 ses between Ambystoma mexicanum (an obligate metamorphic-failure species) and metamorphic F1 hybrids
107 rphic, facultative metamorphic, and obligate metamorphic-failure taxa.
108                        These minerals buffer metamorphic fluids to extremely reducing conditions that
109 reduce the requirements for large volumes of metamorphic fluids to form orogenic ore deposits.
110  idea that this tremor is excited by flow of metamorphic fluids.
111 hing events seen in some marginally stable ("metamorphic") folded proteins in response to mutation or
112 ibed herein, mounting evidence suggests that metamorphic folding is an adaptive feature, preserved an
113 egions of sequence space are compatible with metamorphic folding.
114 ly in groundwater from fractured igneous and metamorphic formations throughout the Piedmont region.
115 ee were expressed widely throughout the post-metamorphic frog nervous system, but with distinctly dif
116 notactic responses as animals developed from metamorphic froglets to reproductive adults.
117 on of metamorphosis, ecdysteroids acquired a metamorphic function that exploited the repressor capaci
118  a number of genes, collectively forming the Metamorphic Gene Network.
119 rocks of prehnite-pumpellyite to greenschist metamorphic grade between 3.2 and 2.75 billion years ago
120 the progressive decrease in delta(66)Zn with metamorphic grade is correlated with a decrease in sulfu
121 hat felsic rocks in both Archaean high-grade metamorphic ('grey gneiss') and low-grade granite-greens
122  other appendages, it is required for normal metamorphic growth of the mandibles.
123  the gut and liver but increased in the post-metamorphic heart and hindlimb.
124 ision, indicating that conductive models for metamorphic heat transfer in Barrovian terrains are inco
125 stent larval neurons exhibiting two distinct metamorphic histories.
126                          The linkage between metamorphic history, boulder size, and channel steepness
127 ns have been preserved despite a complicated metamorphic history.
128                                              Metamorphic hydration and oxidation of ultramafic rocks
129 pentinization of Martian crust suggests that metamorphic hydration reactions played a critical part i
130                Our work not only establishes metamorphic InAsSb/InSb as a promising and competitive m
131                               Here, by using metamorphic InAsSb/InSb superlattices (SLs), we demonstr
132 aining on opposite sides of the head in post-metamorphic individuals.
133                                              Metamorphic inefficiency and compositional relationships
134  to show that the early atrial siphon of the metamorphic juvenile, including its aperture and lining,
135 and/or OA across three developmental stages (metamorphic, juvenile, and adult) or as adults only, and
136 eveloping embryos, tornaria larvae, and post-metamorphic juveniles and show that the tornaria larva o
137 site pattern with the highest levels in post-metamorphic juveniles.
138 s and cell numbers in late embryonic and pre-metamorphic larval stages.
139 n, but this capacity is abrogated during the metamorphic larval-to-adult switch.
140 acceleration, surface downdrop, and specific metamorphic lithologies and large plutonic intrusions.
141  and then migrate into stripes, whereas late metamorphic (LM) melanophores arise already within strip
142                                          The metamorphic Mad2 protein acts as a molecular switch in t
143 00 Ma magmatic core surrounded by a ~4070 Ma metamorphic mantle.
144 isotopic compositions for ultrahigh pressure metamorphic marbles and enclosed carbonated eclogites fr
145 es and the applied load could inspire novel, metamorphic materials with pre-programmed mechanisms acr
146 how that kit functions during a late step in metamorphic melanophore development in both species.
147 re both autonomous and non-autonomous to the metamorphic melanophore lineage.
148  lineages, including a dramatic reduction of metamorphic melanophore precursors.
149 ow that one such mutant, picasso, lacks most metamorphic melanophores and results from mutations in t
150 ontributing to the evolutionary reduction in metamorphic melanophores and the increased contribution
151 o-adult transformation by the recruitment of metamorphic melanophores from latent precursors.
152  crest cells, as well as from post-embryonic metamorphic melanophores that are derived from latent pr
153 r tyrosine kinase, as well as late-appearing metamorphic melanophores that depend on both the G-prote
154 otes the development of both early-appearing metamorphic melanophores that depend on the kit receptor
155 phores are replaced by newly differentiating metamorphic melanophores that form the adult stripes.
156 orphosis at the same time as wild-type fish, metamorphic melanophores that normally appear during the
157  for erbb3b in the development of much later metamorphic melanophores, and suggest complex modes by w
158 s in five additional species also arise from metamorphic melanophores, identifying this as an ancestr
159 maintain or recruit the latent precursors to metamorphic melanophores.
160  stages, with a diminished contribution from metamorphic melanophores.
161                                          The metamorphic mineral assemblages in relatively FeO-rich M
162  extremely low delta(18)O records of igneous/metamorphic minerals from South China.
163 tion pathways play in the crystallization of metamorphic minerals, the distribution of porphyroblasts
164                    Neither the timing of the metamorphic molt nor the duration of larval growth was a
165  by the pulse of ecdysone that initiates the metamorphic molt.
166 ought to have been eroded from the Himalayan metamorphic mountain belt.
167 In tunicates, Mymk is expressed only in post-metamorphic multinucleated muscles, but is absent from m
168 , we show that transcription of Mymk in post-metamorphic muscles of the tunicate Ciona requires the c
169                                By the end of metamorphic nerve shortening, one-quarter of all myelin
170 types was determined for metamorphic and non metamorphic offspring from backcrosses between Ambystoma
171 ed within the host rock as inclusions within metamorphic olivine while the bulk elemental and isotope
172 ly abiotic porphyroblasts of thermal contact metamorphic origin that record late-stage retrograde coo
173 come whereby longer growing seasons favoured metamorphic outcomes.
174 lance between carbon input from volcanic and metamorphic outgassing and its removal by weathering fee
175        Changes in the global distribution of metamorphic (P, T) conditions in the continental crust t
176                                    Comparing metamorphic patterning in T. castaneum to embryonic and
177                           Here, we study the metamorphic patterning of mandibulate mouthparts of the
178 rey (Petromyzon marinus) during the critical metamorphic period during which sea lamprey increase osm
179 ult (frog) stage, both connected through the metamorphic period in which drastic morphological and ph
180         The collisional shortening, prograde-metamorphic phase of the Orogeny lasted 8 my, extensiona
181                                 Here, we use metamorphic phase transitions and the onset of melting t
182           Subsequently, they display a novel metamorphic phenotype, involving collapse of the head an
183       We used thyroid hormone (TH) to rescue metamorphic phenotypes in paedomorphic salamanders and t
184       HIV-1 reverse transcriptase utilizes a metamorphic polymerase domain that is able to adopt two
185  fabrication approach through the control of metamorphic polymers' amorphous-crystalline transition t
186 tic pressure paradigm enables converting the metamorphic pressure directly into the rock's burial dep
187 c unit, Western Alps, considerably different metamorphic pressures are determined in adjacent rocks.
188 for muscle and neural development during the metamorphic process.
189                             Hydrothermal and metamorphic processes could have abiotically produced or
190 e transition is one of the major geochemical-metamorphic processes typifying the subduction zone, whi
191 ffering insights into diagenetic and hydrous-metamorphic processes, and mass transfer cycles in deep
192 s exhibit temporal misregulation of specific metamorphic processes.
193 cations from postdepositional diagenetic and metamorphic processes.
194 5 results in temporal delays in two distinct metamorphic processes: the terminal cell-cycle exit in t
195                          They reveal how the metamorphic properties of KaiB, a protein that adopts tw
196 drophobic effects in each well-characterized metamorphic protein pair and a description of how these
197 likely monomorphic proteins and a set of 201 metamorphic protein structures taken from the literature
198            Thus, IscU may be classified as a metamorphic protein.
199 urveying the landscape of well-characterized metamorphic proteins and noting that a significant fract
200                                        These metamorphic proteins are characterized by having two or
201 a category that enhances biological fitness, metamorphic proteins are likely to employ fold switching
202          It was previously hypothesized that metamorphic proteins arose as intermediates in the evolu
203                                  So far, ~90 metamorphic proteins have been identified in the Protein
204                          Naturally occurring metamorphic proteins have the ability to interconvert fr
205 might drive the global folding transition in metamorphic proteins in general.
206 ers hypothesize that a far greater number of metamorphic proteins remain undiscovered.
207                                              Metamorphic proteins switch between different folds, def
208                                              Metamorphic proteins switch reversibly between multiple
209                                              Metamorphic proteins switch reversibly between two diffe
210 l heterogeneity, defining a new category of "metamorphic proteins".
211  during stochastic excursions by polymorphic/metamorphic proteins, enabled RNAs and proteins to mutua
212                                              Metamorphic proteins, including proteins with high level
213 viding a unique thermodynamic perspective on metamorphic proteins.
214 evolution, and de novo design strategies for metamorphic proteins.
215 d of the increasingly recognized concept of "metamorphic proteins."
216  transcripts within the liver of exposed pre-metamorphic R. catesbeiana tadpoles within 6 d.
217                While the LC50 of IBF for pre-metamorphic Rana catesbeiana tadpoles is 41.5 mg/L (95%
218 dy mass, body size and weight and growth and metamorphic rates.
219 otopic and elemental compositions, degree of metamorphic re-equilibration and sulphide-rich nature of
220 ay microtomography we have imaged a complete metamorphic reaction and show how chemical transport evo
221                             High-temperature metamorphic reaction rates were measured using strontium
222                                              Metamorphic reactions influence the evolution of the Ear
223  arc magmatism, which reflect differences in metamorphic reactions occurring in subducting oceanic cr
224 in-building episode which is consistent with metamorphic reactions produced by long-term cooling.
225  step for crystallization, the energetics of metamorphic reactions.
226 e Proterozoic also has a unique magmatic and metamorphic record; massif-type anorthosites and anoroge
227 th in intact F protein and in 6HB, suggest a metamorphic region around these residues with dual struc
228 geting, branching patterns, territories, and metamorphic remodeling are controlled in specific ways,
229  To identify molecular mechanisms underlying metamorphic remodeling, we conducted a neuropeptidergic
230  nerve (ON) shortening during Xenopus laevis metamorphic remodeling.
231 n factors (BRC-Z1-Z4) that are essential for metamorphic reorganization of the central nervous system
232                                   During the metamorphic reorganization of the insect central nervous
233 ecdysone receptor isoforms induces different metamorphic responses in various larval tissues.
234 ding the roles of BR-C proteins in directing metamorphic responses to ecdysone.
235                                 In the past, metamorphic rock preferred by N. chlorobranchius was mor
236 lated in tributaries farther upstream, where metamorphic rock remained.
237 erature-time paths obtained from minerals in metamorphic rocks allow the reconstruction of the geodyn
238 rine biominerals and thus of sedimentary and metamorphic rocks and it plays a major role in the globa
239 nsiderations and N contents of high pressure metamorphic rocks imply massive addition of subducted N
240 icrom in size discovered in the 1980s within metamorphic rocks related to continental collisions clea
241 onvergent plate margins are characterized by metamorphic rocks that show a bimodal distribution of ap
242 erals, the distribution of porphyroblasts in metamorphic rocks, and, in cases in which nucleation is
243                                              Metamorphic rocks-rocks that have experienced solid-stat
244 ons to produce eclogites and eclogite facies metamorphic rocks.
245 en rock specimens made up of sedimentary and metamorphic rocks.
246           Our experiments indicated that the metamorphic role of T3 is through genomic action of the
247  into the relationship between embryonic and metamorphic segmental identity specification, we have co
248 the terminal growth zone that generates post-metamorphic segments, however, CapI-hes1 has a non-overl
249 ic deposits from magmatic, hydrothermal, and metamorphic settings.
250  of protein kinase C, two other steps in the metamorphic signal transduction pathway.
251 xamined larval (duration, survival) and post-metamorphic (size) traits of both species after manipula
252                High-temperature low-pressure metamorphic soles are vestiges of subduction initiation,
253 servations indicate that the majority of the metamorphic soles likely formed during induced subductio
254                                              Metamorphic species are likely to experience more dynami
255                                              Metamorphic species, such as C. riparius, may act as a v
256 he most heavily infected species at the post-metamorphic stage.
257 ion dose treatments at both larval and post- metamorphic stages and quantified infection load on day
258 tonergic cells in the embryonic, larval, and metamorphic stages of the life cycle of Aplysia.
259                                           At metamorphic stages Xenopus displays a superficial granul
260 f adult tissue progenitors during larval and metamorphic stages, and gametogenesis in adults.
261 ental variability on species with vulnerable metamorphic stages.
262 ologic variability during aquatic larval and metamorphic stages.
263 n shown to shift the equilibrium between the metamorphic states.
264 hology, with higher mortality on igneous and metamorphic substrates, and to regional reductions in gr
265  superomniphobicity and shape memory effect, metamorphic superomniphobic (MorphS) surfaces that trans
266 aean era to the present day, and the average metamorphic T/P has decreased since the Palaeoproterozoi
267             We find that the distribution of metamorphic T/P has gradually become wider and more dist
268 atistical evaluation of the distributions of metamorphic T/P through time.
269 ure change with depth; parameterized here as metamorphic T/P) in the form of paired metamorphic belts
270                                          Pre-metamorphic tadpoles have abundant lectin-labeled perice
271 ) and showed that it was present in pre- and metamorphic tadpoles.
272  often contain a mixture of paedomorphic and metamorphic taxa, indicating that geographic isolation h
273 tions of peak conditions in high-temperature metamorphic terranes define relatively narrow ranges of
274 ible with observations from high-temperature metamorphic terranes exhumed in orogens.
275 a minor component in many very high-pressure metamorphic terranes that formed during continental subd
276 ociated with amphibian life cycle evolution: metamorphic timing and adult body size.
277  selection of TH-response alleles that delay metamorphic timing and increase adult body size.
278 ge influence of Mendelian dominance on size, metamorphic timing and predation rate of hybrid tiger sa
279                 Repeatedly during evolution, metamorphic timing has been delayed to exploit growth-pe
280 s associated with genetic changes that delay metamorphic timing in biphasic life cycles.
281 n responsiveness to TH and additively affect metamorphic timing.
282 -history traits in amphibians: body size and metamorphic timing.
283 locus (QTL) that contributes to variation in metamorphic timing.
284 lopment may occur through genetic changes in metamorphic timing.
285 t study demonstrating Se transference during metamorphic tissue remodelling.
286 ella germanica, BgE93 is highly expressed in metamorphic tissues, and RNA interference (RNAi)-mediate
287 early in the season, and was not mediated by metamorphic traits (age and mass at emergence).
288 essures drive clinal variation in larval and metamorphic traits in this species.
289  the larval stage and may not be captured by metamorphic traits, and (ii) be strongly modulated by eg
290 in premetamorphic tadpoles led to precocious metamorphic transformations.
291  larvae, then increased significantly in mid-metamorphic transformers (stage 3); thereafter, levels s
292                                   During the metamorphic transition, these structures degrade, and be
293 Ns undergo drastic reconstruction during the metamorphic transition.
294                                          The metamorphic translocation of ganglia, which included a c
295  to assign protein sequences as likely to be metamorphic versus monomorphic (i.e., having just one fo
296    Our model is able to classify proteins as metamorphic versus monomorphic with a Matthews correlati
297  growing and regenerating adult retina, of a metamorphic vertebrate, the winter flounder.
298 olatile contents could reflect post-magmatic metamorphic volatile addition or growth from a late-stag
299 ulation on Delta and Notch expression during metamorphic wing vein development, and that the resultan
300 lf-correction of craniofacial defects in pre-metamorphic X. laevis tadpoles.
301 in this study we examined the ability of pre-metamorphic Xenopus laevis tadpoles to self-correct malf
302 ation after partial retinal resection in pre-metamorphic Xenopus laevis.

 
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