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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.
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
53 Polymerase Chain Reaction (PCR) with thermal cycling among three different temperatures on a single s
55 cks is directly associated with high-voltage cycling, an electrochemically driven and diffusion-contr
58 understanding of global carbon and nitrogen cycling and a reduction in the uncertainty of carbon-cli
60 versely correlated with the fraction of slow cycling and apoptotic cells within the four TPA subsets.
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
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
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
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
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
100 tiandrogen therapy, and paradoxically, rapid cycling between high and low serum testosterone concentr
102 o be capable of successful thermally-induced cycling, between amorphous and crystalline states, of la
104 ar disorder, but it is unclear whether rapid cycling bipolar disorder is linked to highly altered mem
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
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
123 ht conditions, but renders cells inviable in cycling conditions when light and dark periods alternate
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
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
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
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
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
150 including community collapse, diversity, and cycling, have characteristic evolutionary dynamics that
153 the understanding of mercury biogeochemical cycling; however, there is a lack of consensus on the un
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.
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
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
190 tantial implications for nutrient and carbon cycling, land productivity and in turn, worldwide socio-
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
198 thological conditions of dysregulated Ca(2+) cycling, mitochondrial Ca(2+) overload activates cellula
200 show that the terminally differentiated, non-cycling neutrophils repurpose cell-cycle proteins and pa
205 ecological interactions, and biogeochemical cycling of both cellular and acellular community compone
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
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
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
225 with a large microbe-mediated soil sink, yet cycling of this compound throughout ecosystems is poorly
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
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
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
237 bles Zn-air batteries to achieve a long-term cycling performance of over 480 h at 10 mA cm(-2) with h
239 0 and 9.9 Wh/L) exhibited unprecedented long cycling performance, 700 cycles at 60 mA/cm(2) with 99.9
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
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
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.
257 greater plant N uptake, but decrease soil N cycling rates because of greater soil carbon inputs and
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
263 , sea ice, species diversity, biogeochemical cycling, seafloor methane stability, deep-sea circulatio
265 omethanesulfonyl)imide) and realize the best cycling stability among all reported Mg/S batteries by s
267 the SiNPs@C composites demonstrate excellent cycling stability and rate performance, which is ascribe
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
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
282 ts on both plant N pools and rates of soil N cycling that were independent of those of species richne
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
287 viously unrecognized roles in biogeochemical cycling through mechanisms that include extracellular el
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
300 dynamics and the role of viruses in nutrient cycling would benefit from direct observations at the si
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