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4 contributed by met: continuous variation of metamorphic age and expression of discrete, alternate mo
5 Bd infection is limited to the skin in post-metamorphic amphibians, routine skin sloughing may regul
6 evolution of novel paedomorphic species from metamorphic ancestors via selection of TH-response allel
7 val period, is rapidly elaborated during the metamorphic and early juvenile periods to form the adult
8 ed in our work emphasize the need to include metamorphic and fluid transport processes in geodynamic
10 lpha and TRbeta genotypes was determined for metamorphic and non metamorphic offspring from backcross
11 amorphic core complexes are domal uplifts of metamorphic and plutonic rocks bounded by shear zones th
12 mental expression of Sox2 and Sox19 genes in metamorphic and postmetamorphic specimens and young adul
15 this study we present new in situ U-Pb age, metamorphic, and morphological data on these titanite mi
24 ndicate that the intestine undergoes similar metamorphic changes in X. laevis and X. tropicalis, maki
26 luding wing discs and eye primordia initiate metamorphic changes, such as pupal commitment, patternin
27 growing tissues nearing completion of their metamorphic changes, suggesting a role for the deiodinas
29 n mRNA is down regulated at the beginning of metamorphic climax (NF62) and reexpressed again near the
31 peak concentration of T4 that is reached at metamorphic climax cannot induce the final morphological
32 re down-regulated in the tail at the peak of metamorphic climax just before it is resorbed are suppre
50 as that underlie the detachment fault in the metamorphic core complex of the Whipple Mountains yielde
51 t, at least in this case, the development of metamorphic core complexes and the accommodation of high
53 nds of Papua New Guinea are actively forming metamorphic core complexes located within a continental
54 ast, here we present seismic observations of metamorphic core complexes of the western Woodlark rift
56 es have addressed this problem and therefore metamorphic decarbonation in subduction zones remains la
58 tinental foreland basin sediments containing metamorphic detritus eroded from the Himalaya orogeny th
60 iscs showed that BRC-Z1 expression and early metamorphic development are rendered steroid-independent
63 med cell death (PCD) of neurons during early metamorphic development of the central nervous system (C
68 distinct populations of melanophores: early metamorphic (EM) melanophores arise widely dispersed and
69 A full characterization of low-temperature metamorphic events and alternative biosignatures in gree
70 u geochemistry will allow us to date ancient metamorphic events and determine the terrestrial Pu/U ra
71 enes have putative functions relevant to key metamorphic events including the differentiation of smoo
72 an ancient martian meteorite record thermal metamorphic events with ages that group around and/or do
74 e established a sequence of bacteria-induced metamorphic events: MACs induce larval settlement; then,
75 an obligate metamorphic-failure species) and metamorphic F1 hybrids (A. mexicanum x A. tigrinum tigri
76 d salamander populations, including obligate metamorphic, facultative metamorphic, and obligate metam
77 mode of development that is characterized by metamorphic failure (paedomorphosis), an adaptation for
78 ses between Ambystoma mexicanum (an obligate metamorphic-failure species) and metamorphic F1 hybrids
82 hing events seen in some marginally stable ("metamorphic") folded proteins in response to mutation or
83 ee were expressed widely throughout the post-metamorphic frog nervous system, but with distinctly dif
85 rocks of prehnite-pumpellyite to greenschist metamorphic grade between 3.2 and 2.75 billion years ago
86 the progressive decrease in delta(66)Zn with metamorphic grade is correlated with a decrease in sulfu
87 hat felsic rocks in both Archaean high-grade metamorphic ('grey gneiss') and low-grade granite-greens
89 ision, indicating that conductive models for metamorphic heat transfer in Barrovian terrains are inco
93 pentinization of Martian crust suggests that metamorphic hydration reactions played a critical part i
96 to show that the early atrial siphon of the metamorphic juvenile, including its aperture and lining,
97 eveloping embryos, tornaria larvae, and post-metamorphic juveniles and show that the tornaria larva o
100 acceleration, surface downdrop, and specific metamorphic lithologies and large plutonic intrusions.
101 and then migrate into stripes, whereas late metamorphic (LM) melanophores arise already within strip
104 isotopic compositions for ultrahigh pressure metamorphic marbles and enclosed carbonated eclogites fr
105 how that kit functions during a late step in metamorphic melanophore development in both species.
108 ow that one such mutant, picasso, lacks most metamorphic melanophores and results from mutations in t
109 ontributing to the evolutionary reduction in metamorphic melanophores and the increased contribution
111 crest cells, as well as from post-embryonic metamorphic melanophores that are derived from latent pr
112 r tyrosine kinase, as well as late-appearing metamorphic melanophores that depend on both the G-prote
113 otes the development of both early-appearing metamorphic melanophores that depend on the kit receptor
114 phores are replaced by newly differentiating metamorphic melanophores that form the adult stripes.
115 orphosis at the same time as wild-type fish, metamorphic melanophores that normally appear during the
116 for erbb3b in the development of much later metamorphic melanophores, and suggest complex modes by w
117 s in five additional species also arise from metamorphic melanophores, identifying this as an ancestr
126 types was determined for metamorphic and non metamorphic offspring from backcrosses between Ambystoma
127 ly abiotic porphyroblasts of thermal contact metamorphic origin that record late-stage retrograde coo
128 lance between carbon input from volcanic and metamorphic outgassing and its removal by weathering fee
137 5 results in temporal delays in two distinct metamorphic processes: the terminal cell-cycle exit in t
145 otopic and elemental compositions, degree of metamorphic re-equilibration and sulphide-rich nature of
146 ay microtomography we have imaged a complete metamorphic reaction and show how chemical transport evo
149 arc magmatism, which reflect differences in metamorphic reactions occurring in subducting oceanic cr
150 in-building episode which is consistent with metamorphic reactions produced by long-term cooling.
151 th in intact F protein and in 6HB, suggest a metamorphic region around these residues with dual struc
152 geting, branching patterns, territories, and metamorphic remodeling are controlled in specific ways,
153 To identify molecular mechanisms underlying metamorphic remodeling, we conducted a neuropeptidergic
155 n factors (BRC-Z1-Z4) that are essential for metamorphic reorganization of the central nervous system
159 nsiderations and N contents of high pressure metamorphic rocks imply massive addition of subducted N
160 icrom in size discovered in the 1980s within metamorphic rocks related to continental collisions clea
163 into the relationship between embryonic and metamorphic segmental identity specification, we have co
164 the terminal growth zone that generates post-metamorphic segments, however, CapI-hes1 has a non-overl
167 xamined larval (duration, survival) and post-metamorphic (size) traits of both species after manipula
170 ion dose treatments at both larval and post- metamorphic stages and quantified infection load on day
175 superomniphobicity and shape memory effect, metamorphic superomniphobic (MorphS) surfaces that trans
177 tions of peak conditions in high-temperature metamorphic terranes define relatively narrow ranges of
179 a minor component in many very high-pressure metamorphic terranes that formed during continental subd
182 ge influence of Mendelian dominance on size, metamorphic timing and predation rate of hybrid tiger sa
190 ella germanica, BgE93 is highly expressed in metamorphic tissues, and RNA interference (RNAi)-mediate
192 the larval stage and may not be captured by metamorphic traits, and (ii) be strongly modulated by eg
196 olatile contents could reflect post-magmatic metamorphic volatile addition or growth from a late-stag
197 ulation on Delta and Notch expression during metamorphic wing vein development, and that the resultan
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