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1  profile, rate capability and stability upon cycling).
2 butes significantly to global biogeochemical cycling.
3 hibit delays in growth of cell size and cell cycling.
4  of genes that control intracellular calcium cycling.
5 volved in hair fiber morphogenesis during HF cycling.
6 a potential for high molecular weight carbon cycling.
7 cade through the food web and shape nutrient cycling.
8 communities and, subsequently, on carbon (C) cycling.
9  200 cycles, demonstrating stable, long-term cycling.
10 pact coupled processes controlling Cr and Mn cycling.
11 3)C for longer lifetimes by using zero field cycling.
12 part by fungal respiration and/or iron redox cycling.
13 arrangement of layers for a long-term stable cycling.
14 e volume fluctuation of Li electrodes during cycling.
15 nding the ocean's role in Pleistocene carbon cycling.
16 photosynthesis on Pacific AMZ biogeochemical cycling.
17 anionic and cationic redox potentials during cycling.
18 edbacks to regional and global marine carbon cycling.
19 ual life history; other genotypes were rapid-cycling.
20 their role in global marine inorganic carbon cycling.
21 nsoluble form, but must be soluble for redox cycling.
22 tion of Southern Ocean ecosystems and carbon cycling.
23 can affect biotic soil feedback and nutrient cycling.
24 ane stability, deep-sea circulation, and CO2 cycling.
25  from agricultural soils during nitrogen (N) cycling.
26 itical contributors to marine biogeochemical cycling.
27 croorganisms that govern carbon and nitrogen cycling.
28 ATP production required for synaptic vesicle cycling.
29  loop, aquatic food webs, and biogeochemical cycling.
30  sulfur cathodes to achieve stable full-cell cycling.
31 zooplankton community structure and nutrient cycling.
32 s upon temperature, stress or magnetic field cycling.
33 comprehensive understanding of global carbon cycling.
34 rn facilitates hair follicle development and cycling.
35 ducts and understanding of Se biogeochemical cycling.
36 anced stability and high-Columbic efficiency cycling.
37 h zone) display significantly different cell cycling.
38 ols whole-body energy homeostasis via Ca(2+) cycling.
39 O3 and delta(18)ONO3 to investigate nitrogen cycling.
40  environmental corrosion during handling and cycling.
41  morphology evolution of the Li anode during cycling.
42 ide sufficient oxygen to drive polyphosphate cycling.
43 rocesses, including contaminant mobility and cycling.
44 ences for the Antarctic food web and element cycling.
45 ng no Fe loss during its reduction-oxidation cyclings.
46 in microbial evolution(1,2), marine nutrient cycling(3) and human disease(4).
47 , the ClockDelta19 mouse exhibits rapid mood cycling (a manic-like phenotype during the day followed
48  carbon isotope data suggests biogeochemical cycling across a dynamic redox boundary, with primary pr
49 gen diffusion is able to maintain phosphorus cycling activity associated with the enrichment of polyp
50 n vitro treated with the reduction-oxidation cycling agent menadione.
51 opsis counterparts reported earlier to cease cycling altogether upon cold treatment.
52 ption in host cell assemblages revealed diel cycling among many different viral types.
53 Polymerase Chain Reaction (PCR) with thermal cycling among three different temperatures on a single s
54 OS levels result in defective Foxo3(-/-) HSC cycling, among many other deficiencies.
55 cks is directly associated with high-voltage cycling, an electrochemically driven and diffusion-contr
56           Citric acid cycle fluxes, pyruvate cycling, anaplerosis, and cataplerosis were also elevate
57 em cell population exhibiting increased cell cycling and a myelomonocytic differentiation bias.
58  understanding of global carbon and nitrogen cycling and a reduction in the uncertainty of carbon-cli
59 ca and has potential to dramatically alter C cycling and accumulation in these ecosystems.
60 versely correlated with the fraction of slow cycling and apoptotic cells within the four TPA subsets.
61  also found an effect of scopolamine on both cycling and behavior.
62               Microorganisms catalyze carbon cycling and biogeochemical reactions in the deep subsurf
63 S, which could significantly affect nutrient cycling and carbon (de)stabilization.
64 ature restoration the efficiency of nutrient cycling and carbon uptake can increase by a shift in fun
65 es in ecosystem functioning, global nutrient cycling and climate regulation, but are declining in the
66 sity, population dynamics and biogeochemical cycling and contribute to the daily flux of billions of
67    The capacity remains fairly stable during cycling and decreases by only about 8 % when the charge/
68 ysiological conditions with minimal pyruvate cycling and detects increased hepatic V CS following tre
69 rk ocean has a major impact on global carbon cycling and ecological relationships in the ocean's inte
70 suggest a key role for intracellular calcium cycling and excitation-transcription coupling in the dys
71 tivity, which can negatively impact nutrient cycling and food production, upon which future generatio
72  to assess SR and FGR effects on ecosystem N cycling and its response to elevated carbon dioxide (CO2
73 nigral afferents is essential for the normal cycling and maintenance of neural stem cells (NSCs) in t
74 e critical for plant fitness, biogeochemical cycling and other processes.
75 uss the role of microbiota in biogeochemical cycling and outline ecological and hydrological connecti
76 ear drivers of differences in biogeochemical cycling and resulted in substantially different carbon p
77 iver ecosystem, which may influence nutrient cycling and river food webs at decadal time scales.
78  This thickening/thinning is reversible with cycling and shows the SEI is a dynamic structure.
79 e rhizosphere effects that regulate nutrient cycling and SOM decomposition.
80 ale evidence for changing conditions of iron cycling and stability of iron minerals it does not provi
81 moautotrophs can play a large role in carbon cycling and that this carbon is heavily influenced by la
82 roving our understanding of supraglacial DOM cycling and the biogeochemical and ecological impacts of
83 ogen (N)-fixing trees can drive N and carbon cycling and thus are critical components of future clima
84                   In aquatic ecosystems, the cycling and toxicity of nickel (Ni) are coupled to other
85 population of melanoma cells, which are slow-cycling and treatment-resistant.
86 t is also sensitive to land and ocean carbon cycling and uptake.
87 major contributions to global biogeochemical cycling, and ameliorate atmospheric accumulation of carb
88  ecosystem processes, including nitrogen (N) cycling, and how those influences might be moderated by
89 , how biodiversity interacts with population cycling, and how to effectively manage wildly fluctuatin
90 ire reproductive lifespan, disrupted vaginal cycling, and hypergonadotropic hypogonadism.
91 diminishes the formation of dendrites during cycling, and thus Sn4P3 is a relatively safe anode mater
92    The mechanics of DNA replication and cell cycling are well-characterized in model organisms, but l
93 ts performed at rest and after 30 minutes of cycling at 70% of maximal power output in hypoxia and eq
94 rgoes 1e(-) electrochemical charge-discharge cycling at low potential (-1.21 V vs Fc/Fc(+)) to a 95%
95 assessment of BD-induced impacts on forest C cycling at the continental scale and going beyond single
96 4 desensitization is required for quiescence/cycling balance of murine short-term hematopoietic stem
97                                    The redox-cycling behavior of this device was modeled using COMSOL
98       Moreover, beta-Li2IrO3 presents a good cycling behaviour while showing neither cationic migrati
99 e rate is increased to 10000 mA g(-1) during cycling between 2.25 and 5.0 V.
100 tiandrogen therapy, and paradoxically, rapid cycling between high and low serum testosterone concentr
101                                      Calcium cycling between the sarcoplasmic reticulum (SR) and the
102 o be capable of successful thermally-induced cycling, between amorphous and crystalline states, of la
103 -reaching impacts on carbon and hydrological cycling, biodiversity, and ecosystem services.
104 ar disorder, but it is unclear whether rapid cycling bipolar disorder is linked to highly altered mem
105 atients with a history of psychosis or rapid-cycling bipolar disorder were excluded.
106                    In 17 patients with rapid cycling bipolar disorder, time-series analyses detected
107  degrees C), high rainfall slowed rates of C cycling, but in warm tropical forests (> 20 degrees C) i
108 e molecular details of O2 -tolerant hydrogen cycling by a soluble NAD(+) -reducing [NiFe] hydrogenase
109 o identify and explore the importance of EES cycling by a wide range of microorganisms so that their
110 d measurements of supraglacial DOM and their cycling by microbes is critical for improving our unders
111 and amorphous phases that are present during cycling by Rietveld and pair distribution function (PDF)
112  that involves enhanced ATP-dependent Ca(2+) cycling by sarco/endoplasmic reticulum Ca(2+)-ATPase 2b
113     Comparison to freezing time, freeze-thaw cycling caused much more damage to the coal strength.
114        Spermatogenesis is a classic model of cycling cell lineages that depend on a balance between s
115             Transcriptome analysis from slow cycling cells identified differentially expressed genes
116 ) to localize, purify, and characterize slow cycling cells in the cornea.
117                                         Slow-cycling cells with high Notch activity and histone demet
118 P1a are specifically observed in the mitotic cycling cells, but not in the endocycling cells.
119 TR kinase activation in non-replicating, non-cycling cells.
120 e established and regulated through nutrient cycling, competition, antagonism, and chemical communica
121 these incubations shed new light on nitrogen cycling complexity and possible factors underlying varia
122 erface is consistent with the cryptic sulfur cycling concept.
123 ht conditions, but renders cells inviable in cycling conditions when light and dark periods alternate
124 iability of the rpaA(-) strain in light/dark cycling conditions.
125 overy from anemic stress and persistent cell cycling consistent with a role for KLF3 in dampening KLF
126 e doses and suggest that the rapid change in cycling could be used to predict efficacy of novel agent
127        These large changes in C and nutrient cycling could not have been predicted from the physiolog
128 etylcysteine reduces ROS levels, rescues HSC cycling defects, and partially mitigates HSPC DNA damage
129 to the plasma membrane where it undergoes re-cycling/degradation in a separate receptor pool, one tha
130 g deposition) and atmospheric Hg sources and cycling (delta(202)Hg, Delta(199)Hg).
131      The precise control of intracellular Ca cycling depends on the relationships between the various
132 ed computational model, to understand the Ca cycling dynamics of an atrial cell subjected to rapid pa
133 s triggered by re-engagement of the TCR on a cycling effector T cell, resulting in apoptosis.
134 oplasm where it associates with early and re-cycling endosomes.
135 cessfully predicts clock behavior under many cycling environments.
136 HEJ) repairs DNA double strand breaks in non-cycling eukaryotic cells.
137                     At least six miRNAs show cycling expression levels within the pigment dispersing
138                                     Male and cycling female rats were exposed to a 7 day CVS paradigm
139 tween serum E2 levels and pLTF expression in cycling female rats.
140 [7]: male aggression (1) is greatest against cycling females, (2) is costly and represents the main s
141 d represents the main source of injuries for cycling females, and (3) increases male mating success w
142  investigate the role of ovarian E2 in young cycling females, and to identify a role for nongenomic e
143  CVS did not enhance the startle response in cycling females.
144                     This is because ER-Golgi-cycling FKBP proteins contain a C-terminal KDEL-like seq
145 ower limit of 345 +/- 70 PgC year(-1) on the cycling flux between the terrestrial biosphere and atmos
146 archaeota were also active, and that methane cycling genes are expressed by the Euryarchaeota, Verstr
147 sing a suite of stress response and nutrient cycling genes to fix carbon under the fluctuating condit
148  cell death via down-regulation of GPP130, a cycling Golgi membrane protein that serves as an endosom
149 le tools for the further study of this key N-cycling guild in all estuarine systems.
150 including community collapse, diversity, and cycling, have characteristic evolutionary dynamics that
151 air-type-dependent functions of NF-kappaB in cycling HFs.
152 n phytoplankton and hence for biogeochemical cycling, higher trophic levels and biodiversity.
153  the understanding of mercury biogeochemical cycling; however, there is a lack of consensus on the un
154 s3, a potent inhibitor of Jak2 signaling, in cycling HSCs.
155 of key cell-cycle proteins in asynchronously cycling human cells.
156                            The effects of pH cycling immersion on the corrosion of glass-based cerami
157 n of precipitation in regulating ecosystem C cycling in arid and semiarid regions.
158                We engineered colony-wide DNA cycling in Escherichia coli in the form of plasmid copy
159  bacteria might contribute to biogeochemical cycling in natural habitats.
160 alisms, including those important for carbon cycling in nutrient-limited anaerobic environments.
161 terferon (IFN) pathways, which enforced cell cycling in quiescent HSPCs, resulting in their apoptotic
162 ations for forest composition and carbon (C) cycling in relation to dry season intensity remain poorl
163 cantly advance the understanding of nutrient cycling in remote systems, where the dynamics of nutrien
164 ved organic carbon (DOC) affects both carbon cycling in surface waters and drinking water production.
165 e mouse brain to define the role of O-GlcNAc cycling in the central nervous system.
166 transitions to understand the onset of rapid cycling in the chaotic predator-prey dynamics.
167 e need for a reevaluation of how we view N2O cycling in the ETNA.
168 fluences on terrestrial ecosystem carbon (C) cycling in the future.
169 led with a rapid transient rise in glutamate cycling in the medial prefronal cortex (mPFC) of awake r
170 he probability flux associated with devices' cycling in the mixed (discrete, switch on/off, and conti
171 specific antibody fragment to monitor GTPase cycling in the presence of a guanine nucleotide exchange
172 ons for understanding mineral controls on As cycling in the soil-rice nexus, and the sampling approac
173 e breakdown products that are observed after cycling in the standard ethylene carbonate-based electro
174 cators to elucidate the complexity of carbon cycling in these ecosystems.
175 uantified and understood component of carbon cycling in tropical forests, especially outside of the A
176      Global carbon models assume that carbon cycling in upland soils is entirely driven by aerobic re
177 d diverse mechanisms for growth and nutrient cycling, including pathways for CO2 and N2 fixation, ana
178 vironments with sulfur, nitrogen and methane cycling, indicating that these novel Nitrospirae bacteri
179                   The NM myosin cross-bridge cycling inhibitor blebbistatin suppressed adhesome compl
180                                         This cycling initially involves SR release of Ca via the ryan
181  warm and wet climate with active hydrologic cycling involving an ocean.
182                                   Population cycling is a widespread phenomenon, observed across a mu
183                                 Within-range cycling is an overlooked process by which fluctuating se
184 r the Earth's surface, and their geochemical cycling is globally important.
185 n the extent to which the oxygen loss during cycling is mitigated.
186 surface relaxation via electrochemical redox cycling is reported.
187               In order to characterize how C cycling is shaped by tree size and drought adaptations a
188 utes to PLN's inhibitory activity on calcium cycling is unknown.
189               The transcriptomes of multiple cycling ISC populations closely resembled Lgr5(+) ISCs,
190 tantial implications for nutrient and carbon cycling, land productivity and in turn, worldwide socio-
191 ion of double-stranded DNA (dsDNA) breaks in cycling large pre-B cells.
192 ate reactive oxygen species in vivo by redox cycling, leading to oxidative stress and adverse health
193 battery based on this strategy exhibits long cycling life (1000 cycles) and good capacity retention.
194 MB-HSCs and progenitors into the cell cycle; cycling MB-HSCs fail to revert into quiescence in the ab
195 n that the marker gene for anaerobic methane cycling (mcrA) is more widespread in the Archaea than pr
196 l nutrient content, indicating that nutrient-cycling mechanisms other than the direct absorption from
197                       Here, relevant methane-cycling microbial groups were investigated at two remote
198 thological conditions of dysregulated Ca(2+) cycling, mitochondrial Ca(2+) overload activates cellula
199 anges on the oceanic CO2 sink using a carbon cycling model.
200 show that the terminally differentiated, non-cycling neutrophils repurpose cell-cycle proteins and pa
201                            Moreover, loss of cycling NG2(+) glia and pericytes caused significant mul
202           We reasoned that targeting a redox cycling nitroxide to mitochondria could prevent reactive
203                                Most abortive cycling occurs in the slower phase (>10 s), when stalled
204                                              Cycling of aPKC between these distinct functional assemb
205  ecological interactions, and biogeochemical cycling of both cellular and acellular community compone
206 ) /Ca(2+) exchanger inextricably couples the cycling of Ca(2+) and Na(+) in cardiac myocytes.
207 cating that Endozoicomonas contribute to the cycling of carbohydrates and the provision of proteins t
208 cosystems have less abundance, diversity and cycling of carbon and nitrogen than 'undisturbed' ecosys
209 on due to its implications for human health, cycling of carbon and other nutrients in Earth system.
210 y, geochemistry, and biology controlling the cycling of carbon, nitrogen, oxygen, iron, sulfur, and u
211 cytoplasmic conductivity that depends on the cycling of cytoplasmic K(+) levels.
212 e, but that depolarization facilitates rapid cycling of extracellular calcium through the endoplasmic
213 een suggested that sea-salt-induced chemical cycling of Hg (through 'atmospheric mercury depletion ev
214 (FeS2) plays a significant role in the redox cycling of iron and sulfur on Earth and is the primary c
215 stalline forms, affecting the biogeochemical cycling of iron and the behavior of any species adsorbed
216 nd-modified electrolyte can lead to a stable cycling of lithium | lithium symmetrical cells up to 150
217 utational studies found no evidence of redox cycling of manganese or cobalt in the enzymatic reaction
218 wed to significantly contribute to biosphere cycling of methane, a potent greenhouse gas.
219                                          The cycling of Navs through open, closed and inactivated sta
220  microbial processes may be important in the cycling of not only C, but other elements such as N, S,
221 ical forest productivity is sustained by the cycling of nutrients through decomposing organic matter.
222 he historical controls on the biogeochemical cycling of silicic acid [Si(OH)4] on the west Antarctica
223  appear to participate in the biogeochemical cycling of sulfur and nitrogen, filling previously unass
224  age also implicitly models the preferential cycling of sulfur that they are disputing.
225 with a large microbe-mediated soil sink, yet cycling of this compound throughout ecosystems is poorly
226 ere proposed to account for the effect of pH cycling on glass-ceramic corrosion.
227 terphase (SEI) formed during electrochemical cycling on silicon anodes was analyzed with a combinatio
228 ransfer to achieve efficient and very stable cycling operation over 300 cycles with a low discharge-c
229 bility of the intracellular Ca(2+) ( Ca i2+) cycling, or both.
230 on without prior sample preparation, thermal cycling, or enzymes are of interest due to their simplic
231  also point towards a major shift in the N2O cycling pathway in the core of the low oxygen eddy discu
232  and anammox was the most sensitive nitrogen cycling pathway responding to variation of the abiotic e
233 implications for our understanding of soil N cycling pathways and N2 O production.
234 table stripping/plating profiles, and better cycling performance ( approximately 150 h at 3 mAcm(-2))
235 ned a high rate performance and an excellent cycling performance approaching 100% of its initial capa
236 cal energy density (45.5 Wh/L) and excellent cycling performance from 40 to 100 mA/cm(2).
237 bles Zn-air batteries to achieve a long-term cycling performance of over 480 h at 10 mA cm(-2) with h
238                       Significantly improved cycling performance under bending conditions is achieved
239 0 and 9.9 Wh/L) exhibited unprecedented long cycling performance, 700 cycles at 60 mA/cm(2) with 99.9
240 ong-term structural integrity, and high-rate cycling performance.
241 i-ion battery anode materials with excellent cycling performance.
242  morphology renders enhanced electrochemical cycling performance.
243                      Its remarkable rate and cycling performances are attributed to the elimination o
244 hat GSCs can reversibly transition to a slow-cycling, persistent state in response to targeted kinase
245 eport that neoblasts arise from an anarchic, cycling piwi-1+ population wholly responsible for produc
246 or a 'deep carbonated biosphere' with carbon cycling potential.
247                   We conclude that increased cycling precedes the antidepressant action at behavioral
248 ed from hysterectomy specimens from normally cycling premenopausal women with uterine fibroids, who w
249 racellular structures with models of calcium cycling, presenting the possibility to directly assess t
250 aerobic photosynthesis is therefore a carbon cycling process that could take place in anoxic environm
251 hical gradients greatly affect soil nutrient cycling processes.
252 optimized and maintained using rigid thermal cycling programs and stringent sample preparation proced
253 nged action potentials, (2) disrupted Ca(2+) cycling properties, and (3) diminished Ca(2+)/CaM-depend
254 lower basal phosphorylation levels of Ca(2+)-cycling proteins including ryanodine receptor type 2.
255                Using a dry-wet environmental cycling protocol, hundreds of proto-peptide sequences we
256           Based on a conceptually novel auto-cycling proximity recording (APR) mechanism, it continuo
257  greater plant N uptake, but decrease soil N cycling rates because of greater soil carbon inputs and
258                                        Rapid cycling (RC) bipolar disorder is considered as a severe
259 hemistry throughout realistic sediment redox cycling regimes.
260 apid eye movement - rapid eye movement (REM) cycling, REM sleep reduction or loss, and REM sleep inst
261 iration are a key component of global carbon cycling, resulting in the transfer of 40-70 Pg carbon fr
262 chniques utilize complex geometries or phase cycling schemes to isolate non-linear signals.
263 , sea ice, species diversity, biogeochemical cycling, seafloor methane stability, deep-sea circulatio
264                                       Two pH cycling sequences (pH 2, 7, 10 and pH 10, 2, 7) were emp
265 omethanesulfonyl)imide) and realize the best cycling stability among all reported Mg/S batteries by s
266 ery-level energy density and capacitor-level cycling stability and power density.
267 the SiNPs@C composites demonstrate excellent cycling stability and rate performance, which is ascribe
268 ulfur and lithium-oxygen batteries with long cycling stability are realized.
269 e capacity secured at >0.45 V, and excellent cycling stability for more than 500 cycles.
270         We show that PEDOT-BQ determines the cycling stability of the device while PEDOT-AQ provides
271 does not necessarily degrade electrochemical cycling stability or performance in aprotic electrolytes
272 ent rate performance, and superior long-term cycling stability over 200 cycles at a high current dens
273 1 A/g, a maximum power density >3 kW/kg, and cycling stability over 7000 cycles.
274 hodes are assembled and achieve good initial cycling stability with high energy density.
275  in the order of 850 Wh L(-1) with excellent cycling stability.
276 1), superior rate performance, and excellent cycling stability.
277 s in terms of capacity, rate capability, and cycling stability.
278 and energy densities and promising long-term cycling stability.
279 he RNA-binding protein Mex3a labels a slowly cycling subpopulation of Lgr5+ ISCs that contribute to a
280 crobiome of H. heliophila represent nitrogen cycling taxa that have the potential to contribute to a
281           The galvanostatic charge-discharge cycling tests reveal that at low current, the HyLIC exhi
282 ts on both plant N pools and rates of soil N cycling that were independent of those of species richne
283 ransport of water through the membranes when cycling the battery.
284 myocardial redox state, intracellular Ca(2+) cycling, the electrophysiological and contractile proper
285 cludes an additional class of biogeochemical cycling, this being the flow and transformation of genet
286                       People who are rapidly cycling through jail facilities are particularly vulnera
287 viously unrecognized roles in biogeochemical cycling through mechanisms that include extracellular el
288                  We demonstrate that Si(OH)4 cycling through the Holocene alternates between being pr
289                                   Precise Ca cycling through the sarcoplasmic reticulum (SR), a Ca st
290 imination of the P2-O2 phase transition upon cycling to 4.5 V.
291     Here we harness narrow-range temperature cycling to cause repeated breakup of droplets to higher-
292 forest, we documented changes in soil carbon cycling to investigate the potential consequences for th
293  shows that the response of ecosystem carbon cycling to rising CO2 concentration (eCO2 ) and climate
294 turbation - a key mediator of biogeochemical cycling - to determine whether post-extinction compensat
295 gation into the role of AM fungi in nutrient cycling via decomposing organic material in tropical for
296  report the first evidence for potential N2O cycling via the denitrification pathway in the open Atla
297                                        Redox cycling within the crystal was visualized by color chang
298 ated microorganisms that could affect sulfur cycling within the holobiont.
299 rbations to intermediates shuttling into and cycling within the TCA cycle.
300 dynamics and the role of viruses in nutrient cycling would benefit from direct observations at the si

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