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1 system functions such as carbon and nutrient cycling.
2  role in tropical forest dynamics and carbon cycling.
3 close linkage between soil microbial C and N cycling.
4 standing how changes in dose impact hormonal cycling.
5 sivation) even after high-rate and long-term cycling.
6 ant consequences for biogeochemical nitrogen cycling.
7 ed, may play an important role in global DOC cycling.
8 lly important consequences for global carbon cycling.
9 associated with decoupling of litter C and N cycling.
10 es were driven by both N speciation and diel cycling.
11 stabilized cob(II)alamin and promoted futile cycling.
12 r from strand passage, manifesting in futile cycling.
13 stinct copiotrophic bacterial taxa to carbon cycling.
14 es), and in functions important for nutrient cycling.
15 nisms play a critical role in biogeochemical cycling.
16 n and higher capacity retention upon battery cycling.
17 to stabilize the oxygen lattice in prolonged cycling.
18 ighlighting the role of DOM in global carbon cycling.
19 nd sulfur assimilation, and aerobic nitrogen cycling.
20 and local extirpation in response to glacial cycling.
21 t role in freshwater and marine nitrogen (N) cycling.
22 stry to study interactions between HSs and N cycling.
23 ntial effects on carbon (C) and nitrogen (N) cycling.
24 verse effects on biogeochemical nitrogen (N) cycling.
25 d feedbacks to ecosystem carbon and nutrient cycling.
26 d myocyte contractility and disrupted Ca(2+) cycling.
27 from one device to another and after thermal cycling.
28  volume change during lithium-sulfur battery cycling.
29  in understanding marine carbon and nitrogen cycling.
30 plications ranging from defense to global Si cycling.
31 the symbiotic lifestyle and aids in nutrient cycling.
32 hemical models in simulating global nitrogen cycling.
33 nsight into climate change effects on carbon cycling.
34 te forest ecosystem functioning and nutrient cycling.
35 und 43 randomized controlled trials (nine on cycling, 14 on neuromuscular electrical stimulation alon
36 andomly allocated into AT (n = 14, 40 min of cycling, 50-75% heart rate reserve), RT (n = 14, 6 resis
37     Conversion over time data is obtained by cycling a discrete reaction slug back and forth between
38 tem processes underlying carbon and nutrient cycling: (a) algal biomass accrual; (b) microbial respir
39 tractile defects, which then lead to calcium-cycling abnormalities, resulting in aftercontractions an
40 er and monomer photoreception, dimer/monomer cycling, abundance of native COP1 and RUP proteins, and
41 r decomposition plays a key role in nutrient cycling across ecosystems, yet to date, we lack a compre
42 weight organic products, contributing to its cycling across environmental compartments.
43 ese expanded synovial CD8 T cells to express cycling, activation, tissue-homing and tissue residency
44                                 Endogenously cycling adult cardiomyocytes increase after myocardial i
45 y to distant habitats and for inshore carbon cycling and (potentially) carbon sequestration.
46 als, which is 75 % reversible during initial cycling and 63 % retained after 10 cycles.
47 ies, we use a global model of atmospheric Se cycling and a database of more than 600 sites where Se i
48 carbon to Lake Untersee, evaluate the carbon cycling and assess the metabolic functioning of microbia
49  the response of soil microbial nitrogen (N) cycling and associated functional genes to elevated temp
50 how oxygen deficiency affects organic carbon cycling and burial.
51 nfected cells and viral lysis alter nutrient cycling and carbon export in the oceans, although the ne
52  ability of a vegetation model to simulate C cycling and community composition during 100 years of fo
53        For a better understanding of battery cycling and degradation, operando analytical measurement
54 than PD-1 blockade alone in enhancing T cell cycling and differentiation, expanding effector-memory T
55 observed worldwide alters ecosystem nutrient cycling and ecosystem functioning.
56 photoreduction plays an important role in Fe cycling and Fe(II) bioavailability in the upper ocean.
57  methane production drives a cryptic methane cycling and fuels AOM coupled to the reduction of sulfat
58 nd disrupts microtubule organization in both cycling and G2/M arrested cells.
59 change drivers on grassland ecosystem carbon cycling and highlight a crucial role for positive or neg
60    Viruses play a key role in biogeochemical cycling and host mortality, metabolism, physiology and e
61 e two pathways, impede normal conformational cycling and metal transport.
62 o integrate the complex interplay of element cycling and microbial communities into biogeochemical mo
63 d in our collective knowledge of both carbon cycling and microbial strategies to valorize lignin to v
64 active transport (i.e. transport by walking, cycling and other active modes) may reduce greenhouse ga
65 e are an essential link in soil nitrogen (N) cycling and plant N supply.
66  implications for marine carbon and nutrient cycling and provide a greater depth of understanding reg
67 ion plays an important role in terrestrial N cycling and represents a key driver of terrestrial net p
68 ortant ecological functions such as nutrient cycling and sediment stabilization.
69  contributions of different algal glycans to cycling and sequestration of carbon remain unknown, part
70  "anti-aging" effect in high-voltage battery cycling and successfully stopping the escape of oxygen f
71 ich reforestation affects terrestrial energy cycling and thus surface temperature directly by alterin
72  epidermal differentiation and hair follicle cycling and, in so doing, to promote barrier function, w
73 en the cell produced electrical power during cycling) and exhibited similar efficiencies when we assu
74 n the anaerobic steps of carbon- and sulphur-cycling); and (iv) that species richness and habitat sta
75  including forage production, biogeochemical cycling, and biodiversity.
76 actual emissions associated with walking and cycling, and high variability based on country economic
77 fects the global carbon (C) budget, nutrient cycling, and vegetation composition.
78                                Emissions for cycling are approximately half those of walking.
79 ominant mechanisms that determine the carbon cycling are different between the consolidated gully and
80 Emissions from food required for walking and cycling are not negligible in economically developed cou
81 crobial communities involved in nitrogen (N) cycling are structured, in large part, by the compositio
82 n the process of building their survival and cycling armamentarium, the presence of BRB affects this
83 e geomicrobiology of environmental metalloid cycling as well as informing applied approaches for Se a
84 s able to facilitate wood decay and nutrient cycling as well as tolerate latex and utilize resinous e
85 being controlled by traits related to carbon cycling (assimilation and respiration) in well-watered t
86 he algorithm identified shifts in population cycling associated with variations in resource availabil
87 The symmetric rGO@3D-Cu cells exhibit stable cycling at 0.1-2 mA cm(-2) , while baseline Cu premature
88 y (with 92% capacity retention over 116 h of cycling at 0.3 M concentration in a symmetrical flow cel
89                                 The closed N cycling became pronounced during the first 3 years of wa
90 g points, community structuring and nutrient cycling) because the extreme physical environment drasti
91 is is that logging influences phosphorus (P) cycling, because this scarce nutrient is removed in extr
92 estigate their galvanostatic electrochemical cycling behaviors.
93 tial and lineage-specific separation in cell-cycling behaviour.
94 ific gene expression, concurrent with slowed cycling behaviour.
95 hat might be involved in carbon- and sulphur-cycling between and within the lake's three main water m
96 tivity in ascorbate oxidation based on redox cycling between Cu(I) and Cu(II) , as well as their resi
97 al feedback in this circuit generates robust cycling between growth and dormancy in the interior of t
98  that downward migration of Pu may be due to cycling between Pu(V) and Pu(IV).
99                      Therefore, the chemical cycling between the elemental and oxidized Hg forms in t
100 toxicological aspects (the concept of "redox cycling"), biochemical pharmacology (ebselen), nutrition
101 nctional for either cell polarity or nuclear cycling but not both.
102 uence soil water dynamics, as well as carbon cycling by changing soil CO(2) emission and uptake rates
103 hytoplankton primary productivity and carbon cycling by supplying bioavailable Fe to remote areas of
104 2), although we obtained no evidence of SOC2 cycling by transcription, translation or degradation.
105                 This work shows that wet-dry cycling can alter the phase behavior and protocell-relev
106 es [8, 9] impacting food webs, macronutrient cycling, carbon storage, and human disease risk [10-12],
107 g-refractory cells constitute a pool of slow-cycling cells that can either regain drug sensitivity up
108 T/MEK inhibitors suppress pre-RC proteins in cycling cells, triggering stalled replication, DNA damag
109 l regulator of centriole elongation in human cycling cells.
110 ed into chromatin and only when expressed in cycling cells.
111                     Analogous to the thermal cycling commonly employed for nucleic acid melting and a
112 tly bridging tin and copper to survive harsh cycling conditions in sodium ion batteries.
113  burrows implies that benthic biogeochemical cycling could have been maintained at pre-extinction sta
114 ycles (1950 h) at 0.5 mA cm(-2) , with 98.9% cycling Coulombic efficiency and 0.085 V overpotential.
115             These functions include nutrient cycling, decomposition, plant production, and reduced po
116 y active and long-inactive sediments, sulfur-cycling Deltaproteobacteria became more dominant after 3
117 S utilization in genes upregulated in slowly cycling, differentiating tissues, associated with enhanc
118 itro VDR-knockdown impaired myogenesis (cell cycling, differentiation and myotube formation).
119  ~40% of the Mesoproterozoic ocean, nitrogen cycling dominated.
120 A localization to centrosomes in the rapidly cycling Drosophila melanogaster embryo.
121 rovide novel insights into nuances of carbon cycling dynamics by alleviating important uncertainties
122 excellent combination of capacity, rate, and cycling endurance.
123 tinction vortex comprising 15 generations of cycling environmental and genetic stresses.
124 ated by >=48 h: (i) 60 min of semi-recumbent cycling (EX; 50% workload max) and (ii) 75 min of passiv
125 and neurovascular coupling during submaximal cycling exercise and temperature-matched passive heat st
126 end-tidal PCO2 was held constant) Submaximal cycling exercise and temperature-matched passive heat st
127 ibacterial effect was confirmed via a 5-d pH-cycling experiment and a saliva-derived biofilm aging mo
128                                Galvanostatic cycling experiments demonstrate Li-metal batteries with
129 ous adipose tissue potently activates Ca(2+) cycling fat thermogenesis and increases whole-body energ
130 ological malignancy unit: monthly antibiotic cycling for febrile neutropenia that included cefepime (
131  a distinctive example of a main-group redox cycling for the catalytic activation of N(2)O.
132 tion, and inspiratory inflation contour) and cycling frequency.
133 nstrating that elevated temperature shifts N cycling from microbial immobilization to enhanced minera
134 icrobial communities and methane- and sulfur-cycling gene abundances in Arctic marine sediments, we c
135 o show that when DI splicing of the O-GlcNAc-cycling genes fails to restore O-GlcNAc homeostasis, the
136                       Greater abundance of N-cycling genes was predicted by greater soil ammonium (N-
137                                More nitrogen cycling genes were detected in the rare members than in
138 ite had lower abundance of N-oxidisers and N cycling genes.
139  reaction of archaeal and bacterial nitrogen cycling genes.
140  services such as water filtration, nutrient cycling, habitat stabilization, and food web enhancement
141 tus, leisure time physical exercise, walking/cycling, height, energy intake, smoking habits, baseline
142 cognized as an important process for element cycling, however, related silicon fluxes are unknown.
143                                During active cycling, Hsp104 transits repeatedly between whole hexame
144 cted CO(2) emissions and alter soil nutrient cycling, if not countered by greater labile C inputs.
145 tic field strength as provided by fast field cycling imaging scanners.
146 ished the power-duration relationship during cycling in 18 trained participants (eight females).
147 lants' water use for global water and carbon cycling in a changing climate.
148 en cycle is influenced by autotrophic carbon cycling in addition to organic matter oxidation and anam
149  FeOx structure affect coupled iron-nutrient cycling in aquatic ecosystems.
150 g a central imbalance of glutamate-glutamine cycling in depression, our results suggest that aberrant
151 used to elucidate the effect of soil pH on P cycling in grasslands.
152 le before and after 30 min of unilateral arm cycling in healthy volunteers.
153 e is an overlooked factor influencing carbon cycling in peatlands, which is relevant to global carbon
154  micro-flow imaging (MFI) during freeze-thaw cycling in phosphate buffered solutions.
155 s the lead to quantify the ecosystem C and N cycling in response to warming and advances our capacity
156 out how reactive Fe and Al minerals affect C cycling in restored wetlands.
157 logic cycle, which will likely accelerate Hg cycling in tandem with changing inputs from thawing perm
158 opogenic factors have altered biogeochemical cycling in the lake over the last 2,000 y.
159        Here, we present a record of nutrient cycling in the lake, derived from the silicon isotope co
160 died the impact of NAMPT on synaptic vesicle cycling in the neuromuscular junction (NMJ), end-plate s
161 a greater mechanistic understanding of redox cycling in the ocean.
162 evidence of EM fungal suppression of C and N cycling in the Pinus-dominated site, but no suppression
163            We thus hypothesize that nitrogen cycling in the Pliocene-Pleistocene Mediterranean resemb
164  Each surface loop was evolved by infectious cycling in the presence of a helper adenovirus to yield
165 d by major U speciation changes due to redox cycling in the wetland.
166 studied the longer-term impact of fires on C cycling in tropical PSFs, hence we quantified the magnit
167 ulated triacylglycerol (TAG)/fatty acid (FA) cycling in WAT through impacting lipogenesis and lipolys
168 rate that a single session of unilateral arm cycling induces short-term plasticity in corticospinal p
169 est, and that, correspondingly, cross-bridge cycling is defectively suppressed under diastolic/low Ca
170 d that simple galvanostatic charge-discharge cycling is inadequate for assessing capacity fade when f
171 bout the effect of soil pH on phosphorus (P) cycling is limited.
172 vironment, focusing on the ocean, in which N cycling is more generalizable than in terrestrial system
173 rformance degradation during electrochemical cycling is not yet fully understood.
174 dynamics of composite evolution during redox cycling is still very limited, yet critical to maximisin
175 rinciple QTL determining SET (SET1: dormancy cycling) is physically close on chromosome 5, but is dis
176 s of weight loss and regain, known as weight cycling, is often seen when people try to lose weight.
177 ious stimuli allosterically regulate PKM2 by cycling it between highly active and less active states.
178  within secondary particle is disrupted upon cycling, it triggers charge distribution from homogeneit
179                                 In contrast, cycling juvenile BM HSCs preferentially located close to
180 a(2+) sensitivity and increased cross-bridge cycling (k(tr)) at submaximal [Ca(2+)].
181 e high-performance nonaqueous RFBs with long cycling life and high capacity.
182  capacities, high rate performance, and long cycling life.
183 d will inspire future studies to prolong the cycling lifetime of Li-ion batteries.
184 ctive organics and organometallics for which cycling lifetime results have been reported: quinones, v
185 co-factor Lmo4 was found regulated by weight cycling; Lmo4 enhanced preadipocyte proliferation, in vi
186 ogenic brown and beige adipose tissue futile cycling may be an important strategy to increase energy
187  global-scale selection for microbial ligand cycling may have occurred to maintain "just enough" iron
188 f a lithotrophic or organotrophic consortium cycling methane or nitrogen.
189 del, we find that pre-photosynthetic methane-cycling microbial ecosystems are much less productive th
190 ch enable modeling of kinematic loops (e.g., cycling models) and complex anatomy (e.g., patellar moti
191 ng interlinkages between carbon and nitrogen cycling must be considered.
192           During activation, combinations of cycling myosin that contribute insufficient activation e
193  of 91 fecal samples from 15 females (n = 16 cycling, n = 36 pregnant, n = 39 lactating) using 16S rR
194 ent advances in understanding cryptic oxygen cycling, namely the ubiquitous one-electron reduction of
195                       Informed by the (234)U cycling observed in the Laurentide Ice Sheet, where (234
196 obial communities play key roles in nitrogen cycling of boreal forests.
197 ime of terrestrial-to-aquatic biogeochemical cycling of C.
198  oceanic phytoplankton, impacting the global cycling of carbon through both photosynthesis and calcif
199               P2X7 stimulation affected cell cycling of effector T cells and resulted in generation o
200 trained assumptions regarding the biological cycling of iron, which is the main limiting resource for
201 ilization by accelerating the biogeochemical cycling of iron.
202 gen species produced by NQO1-dependent redox cycling of KP372-1 cause robust DNA damage, including DN
203 rey interactions play important roles in the cycling of marine organic matter.
204 mmonia and is of critical importance for the cycling of nitrogen in the biosphere and for the sustain
205 eedbacks within the internal iron and sulfur cycling of the ocean.
206 e these compounds play in the biogeochemical cycling of trace and nutrient elements.
207 ommon but cryptic mechanism that facilitates cycling of volatiles and metals from the mantle to the l
208                                      Wet-dry cycling on the early Earth is thought to have facilitate
209 processes and some aspects of biogeochemical cycling, our mechanistic understanding of the emergent r
210 d NCA is demonstrated, which exhibits stable cycling over 50 cycles with high Coulombic efficiencies.
211                                              Cycling P-eIF2alpha levels required rhythmic activation
212 lanar Li layers as the anode exhibits stable cycling performance and high specific energy and power d
213 , such liquid metal batteries deliver stable cycling performance and negligible self-discharge.
214 ate a small interfacial resistance with good cycling performance at 35 degrees C.
215 lectrodes, our operando cells show realistic cycling performance at practical rates, which allows us
216 lectrolyte and achieve a remarkably enhanced cycling performance of more than 2000 cycles for lithium
217 ion of active materials but also enhance the cycling performance.
218  thus result in rapid decomposition and poor cycling performance.
219 charge conditions and unsatisfying long-term cycling performance.
220 ~765 Wh kg(-1) respectively, with impressive cycling performances over up to 1200 cycles.
221               Inhibiting p53 blocks the slow-cycling phenotype and sensitizes melanoma cells to BRAF/
222  to permanent state change in biogeochemical cycling, primary production, and biological diversity by
223 d their mediated carbon (C) and nitrogen (N) cycling processes at the local scale.
224 ular level interrogation of labile SOM and C-cycling processes in soils.
225 ed temperatures, suggesting that microbial N cycling processes were associated with enhanced microbia
226 peratures have a profound impact on global N cycling processes with implications of a positive feedba
227 and geochemical assays of microbial nitrogen cycling processes, including autotrophic and heterotroph
228                       Finally, our half-cell cycling protocol also offers a method for evaluating the
229 23,040 PCR products) during a single thermal cycling protocol.
230 advantages in either theoretical capacity or cycling/rate performance, manifesting a trade-off trend
231 ather, the PROMISE concept considers how SOC cycling rates are governed by the stochastic processes t
232 viruses are important contributors to carbon cycling, recycling nutrients and organic material throug
233        We consider separately symmetric cell cycling results, the interpretation of which is simplifi
234 ore, recent models of weight loss and weight cycling reveal additional roles for ATMs in systemic met
235 ications have examined leaf-trait and carbon-cycling shifts along an Amazon-Andes transect spanning 3
236      Microbial functions related to nitrogen cycling showed increased spatial variability under nutri
237  seafloor habitat and modified global carbon cycling since the Cambrian.
238              As the engine of biogeochemical cycling, soil microorganisms exert a critical role in me
239 u hybridization, we identify a population of cycling Sox5/6/9+ perichondral progenitor cells that gen
240  this stereotyped regime of motif dominance "cycling", spiking activity truncates early.
241  326 F g(-1) (419 F cm(-3)) and ultra-stable cycling stability (96.6% after 5000 cycles).
242                      Moreover, the excellent cycling stability (99.9 % capacity retention after 100 c
243 m 4.4% to 40.2% at 100 mV s(-1)) and boosted cycling stability (from 21 to 71% over 600 cycles).
244 ) = +1.19 V vs Fc(+/0)) and charge-discharge cycling stability (with 92% capacity retention over 116
245 and the full cell exhibits remarkably better cycling stability and capacity retention as well as capa
246 s with high voltage, fast kinetics, and long cycling stability are comprehensively covered and evalua
247 battery with excellent energy efficiency and cycling stability as an air-cathode, outperforming that
248 anostructures have been used to increase the cycling stability by providing an inner void space to ac
249           We also demonstrate that half-cell cycling stability is consistent with full cell desalinat
250 at 0.5 C with 99.5% coulombic efficiency and cycling stability up to 1000 cycles at 2 C.
251 y, a superior rate capability, and excellent cycling stability with a Coulombic efficiency of ~100%.
252 demonstrating reasonable rate capability and cycling stability with ~80% capacity retention after 100
253 non-aqueous proton full cells exhibit better cycling stability, higher Coulombic efficiency, and less
254 tes, catalytic mechanisms, and the long-term cycling stability.
255  usually leads to sacrifices in capacity and cycling stability.
256 ic energy density (775 Wh kg(-1) ), and good cycling stability.
257  Wh kg(-1) at 5 mA cm(-2) together with good cycling stability.
258 far limited in terms of useable capacity and cycling stability.
259 and consequently offers good capacitance and cycling stability.
260 -life of p53 and uses p53 to initiate a slow-cycling state following stress (DNA damage, targeted the
261 e a subset of cells can transition to a slow-cycling state, rendering them resistant to most targeted
262                                      Estrous cycling status was evaluated in PND90 and PND365 rats.
263                   Upon removal of 5-Fu, slow-cycling stem cells regenerated both the structure and ba
264  agent 5-fluorouracil (5-Fu) eliminated fast-cycling stem cells, which caused JE degeneration, PDL de
265 of overstory trees, leading to predictable N-cycling syndromes, with consequences for emissions of vo
266 in both macrophages and, to a lesser extent, cycling T cells.
267 nor the change in testosterone level after a cycling task.
268           Here we illustrate that key sulfur-cycling taxa, including Dethiobacter, Desulfitispora and
269 feedstocks and the benefit of converting and cycling the greenhouse gas CO(2) on a large scale.
270                             During potential cycling, the oxide layer evolves into detrimental featur
271                              After prolonged cycling, the TMs displayed different levels of inactivit
272 ished the power-duration relationship during cycling, then assessed fatigability during critical powe
273 odels (ESMs) to project future global carbon cycling; these models have been criticized for not accur
274 gment populations of different precursors by cycling through segments of a predefined precursor m/z r
275 le deformation mechanisms during loading and cycling through the phase transformation.
276              These reductions in temperature cycling time will likely be highly advantageous for the
277  process that is crucial for continuous cell cycling to fuel rapid midgut elongation.
278          The coupling of anoxic nitrogen (N) cycling to the function of HSs as a redox battery, howev
279 acquired early during the evolution of rapid cycling trait in rice subspecies.
280 ccomplished using fluorescence on an optical cycling transition; however, Er(3+) and other rare earth
281  other rare earth ions generally lack strong cycling transitions.
282 lly recurrent prostate cancer (PCa), whereby cycling treatment on and off can reduce cumulative dose
283 lar soils and have pivotal roles in nutrient cycling-typically being close to this temperature, previ
284                                   The stable cycling under a high concentration of 1 M is also realiz
285 ol to investigate the effect of pH on soil P cycling under field conditions as it highlights that dif
286                  A promising tool to study P cycling under field conditions is the (18)O:(16)O ratio
287 on hotspots and seasonal differences in MeHg cycling unique to Arctic ecosystems.
288 It however suffers from a voltage decay upon cycling, urging for an in-depth understanding of the par
289                                       A fast cycling variant enables the stimulation of transient pul
290 devices; we will illustrate that the thermal cycling variations strongly determine the type of damage
291 nced their highest levels of cortisol during cycling (versus lactation), and this effect increased wi
292 on that is mediated by regulation of calcium cycling via 12,13-diHOME and NOS1.
293 lume change of active materials upon battery cycling, which largely limit the large-scale application
294          Notably, SICI reduced after the arm cycling, while CMEPs remained the same.
295       It is capable to achieve a stable long cycling with a low capacity decay of 0.014% per cycle an
296  of successful potassium metal battery anode cycling with an aluminum-based rather than copper-based
297 aordinary stability to adsorption-desorption cycling with simulated humid flue gas and enables regene
298 e-free and close to theoretical density when cycling with the SAW.
299 spheric climate variability on global carbon cycling within centuries and millennia.
300 in the JE that supported both fast- and slow-cycling Wnt-responsive stem cells that contributed to se

 
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