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1 hase increases monotonically with increasing Ca concentration.
2 d that it is only detectable at low external Ca concentration.
3 cts of several PLB mutants, as a function of Ca concentration.
4 also be affected by changes in intracellular Ca concentration.
5  critical point is observed as a function of Ca concentration.
6 A formation is strongly influenced by marine Ca concentrations.
7  (NCX) is determined by Vm as well as Na and Ca concentrations.
8 annel endocytosis and the overall effects on Ca concentrations.
9 ttributed to its higher PA and lower initial Ca concentrations.
10 hat significantly increased with higher Rheb(CA) concentrations.
11 a was distributed contained a relatively low Ca++ concentration.
12 bited parallel changes in intracellular-free Ca(++) concentration.
13  are linear (r > 0.999) over a wide range of CA concentrations (5-400 pmol).
14  sCAX1 gene reduces cytosolic and apoplastic Ca concentrations, affecting plasma membrane structure a
15 unitary conductance (gamma) to physiological Ca concentration and compare it to barium ion (Ba) condu
16 onditions, with relatively subtle changes in CA concentration and molecular crowding influencing self
17                A recently completed model of Ca concentration and movements in the cardiac cell diadi
18  determined at 12.5 min OP, 50 C CT and 2.5% CA concentration and this was 63% higher than the contro
19                 Measurements using different CA concentrations and HgCl(2) indicated that liposome P(
20        There was no effect of treatment on S-Ca concentrations and no incidence of hypercalcemia (S-C
21 , the diadic cleft, with respect to calcium (Ca) concentration and movement.
22 Ca++ thus reveal heterogeneity in luminal ER Ca++ concentration and permit observation of receptor- a
23 informatics pathogenicity triage, mean serum Ca concentrations, and mode of inheritance to identify p
24 d cells, a finding consistent with very high Ca++ concentrations (approximately 10(-5)-10(-3) M Ca++
25 ccurately not only the PLB effects on K(Ca) (Ca concentration at half-maximal activity) of the Ca-ATP
26                  ABSTRACT: The intracellular Ca concentration ([Ca(2+) ]i ) must be sufficently low i
27 ity is regulated by changes in intracellular Ca concentration ([Ca(2+)]i).
28 -induced changes in intramitochondrial total Ca concentration ([Ca](mito)) obtained by x-ray microana
29  of MUC1 (ADTKD-MUC1) exhibit reduced plasma Ca concentrations compared to control individuals with m
30 this although accurate measurement of stable Ca concentrations coupled with precise half-life data ar
31 position is a globally widespread freshwater Ca concentration decline towards critically low levels f
32 its effects by influencing the local luminal Ca concentration-dependent gating of the Ca-release chan
33         The findings revealed that different CA concentrations enhanced Mb's thermal stability, while
34 xchange alone is unlikely to raise cytosolic Ca concentration enough to directly activate the myofila
35            Changes in intracellular calcium (Ca) concentration following synaptic and suprathreshold
36                          It was prevented by Ca++ concentrations greater than 50 mM, but was not alte
37                    We found that sedimentary Ca concentrations had been declining steadily for 900 y
38 at past and future changes in available soil Ca concentrations have important and previously unrecogn
39 s have increased or remained constant, while Ca concentrations have rapidly declined towards or even
40 ncentrations, lower apoplastic and cytosolic Ca concentrations, higher membrane leakage, and Ca accum
41                         Especially, the high Ca concentration in finger millet, compared to in other
42 map a quantitative trait locus that controls Ca concentration in rice grains and identify the causal
43 h the action potential duration and the peak Ca concentration in the cell can exhibit well known peri
44 pulse voltammetry (DPV) varies linearly with CA concentration in the range 1x10(-7)-3x10(-3) M.
45 label from [3H]IAA increased with increasing Ca concentration in the receiver up to 5 to 10 millimola
46 ethod detected elevated total alkalinity and Ca concentrations in soil pore waters from feedstock-ame
47             Similarly, OEA induced a rise in Ca(+) concentration in wild-type but not TRPV1-deficient
48                            Although calcium (Ca) concentration in cellular compartments has been sugg
49                     In the batch experiment, Ca concentrations increase until calcite saturation is r
50                   Natural variation in grain Ca concentration is attributed to the variable expressio
51 ut of GCSC1 results in increased chloroplast Ca concentration, lower stomatal conductance in leaves a
52 rp had higher total tissue and water-soluble Ca concentrations, lower apoplastic and cytosolic Ca con
53 (-1) with 20.7% of the water samples showing Ca concentrations <= 1.5 mg L(-1), a threshold considere
54 sumption of ATP and the increase in cellular Ca concentration may result in mitochondrial Ca (mCa) ov
55                             Exposure to high Ca concentrations may influence the development of low-t
56                               The effects of CA concentration, molecular crowding, and the conformati
57 33 mmol/L, pH = 7.4, 37 degrees C) yielded a Ca concentration of (0.65 +/- 0.02) mmol/L and PO(4) of
58 erroelectric transition is observed around a Ca concentration of approximately 1/8, where a new pseud
59 g CRUs, which helps to maintain the local SR Ca concentration of the firing CRUs above a critical lev
60 sions in genomes, have allele-specific shoot Ca concentration phenotypes compared with their segregat
61 significance using a large database of shoot Ca concentration phenotypes of Arabidopsis thaliana.
62 psis gene identifiers tagged to robust shoot Ca concentration phenotypes, 21 mapped to 27 B. rapa eQT
63 ynaptic activity that produced intracellular Ca++ concentration spikes that were measured by indo-1-b
64 luorescence imaging revealed fluctuations in Ca concentration that coincide with daily growth increme
65               After a sudden imposed drop in Ca concentration, the effect of recoverin switched off w
66 has been previously shown to contain similar Ca concentrations to wild-type (WT) plants, but lower ox
67  global variation and controls of freshwater Ca concentrations, using 440 599 water samples from 43 1
68              We found that the global median Ca concentration was 4.0 mg L(-1) with 20.7% of the wate
69 tions, and preparations exposed to different Ca concentrations was estimated by electron microscopy.
70                Under air-excluded conditions Ca concentrations were controlled by dicalcium silicate
71                        Spatially, freshwater Ca concentrations were strongly and proportionally linke
72 -linking temperature (CT), and caffeic acid (CA) concentration were investigated.
73 eal doses (0.25, 1.0, and 4.0 mg/kg), plasma CAS concentrations were assayed by high-performance liqu
74  decoupling between carbonate alkalinity and Ca concentrations, which we attributed mainly to the inf
75 marily explained by changes in foliar Mg and Ca concentrations, which were negatively affected by N a
76 t the observed time-trace of contrast-agent (CA) concentration within a voxel, corresponds to a singu