ライフサイエンスコーパス: on ice

1 ure when it is followed by a 30-min chilling on ice.

2 n lipid and protein oxidation during storage on ice.

3 th Dome A, 24% of the base by area is frozen-on ice.

4 mug/ml), both of which were stored for 24 hr on ice.

5 tionally inactivated by prolonged incubation on ice.

6 stant to overnight digestion in chymotrypsin on ice.

7 no staining was observed at 23 degrees C or on ice.

8 matrigel for protection and stored in medium on ice.

9 tase (trxB) null mutant following incubation on ice.

10 of susceptibility to neuraminidase trimming on ice.

11 r preservation involves cooling of the organ on ice (0-4 degrees C).

12 is unusual import of Mtf1p was also observed on ice (3 degrees C).

13 established the importance of this feedback on ice age AIS evolution.

14 where ice retreat has no significant impact on ice-algae peak timing, suggesting that changes in pel

15 ition to keeping any solution of free DiTags on ice, an analysis of the GC content should be performe

16 hundreds of per cent, depending sensitively on ice and cloud cover as well as seasonal variations.

17 ng no reducing agents was essentially stable on ice and had a half-life of approximately 90 min at 37

18 EPS effects on ice and pore microstructure improve sea ice habitabil

19 as effective as simple postmortem treatment on ice and therefore not essential.

20 The [3H]2ME binds avidly to tubulin even on ice, and it is readily displaced by other colchicine

21 of experimentation, the animals were stored on ice at 4 degrees C for 0, 7, 14, and 21days.

22 ATP or Mg(2+) to otherwise complete mixtures on ice, ATP-initiated excision and final error correctio

23 Sliding speed depends on ice/bed coupling, dictated by the configuration and p

24 lenges to the field and various perspectives on ICE biology.

25 n food rotation and inadequate refrigeration on ice-chilled salad bars may have facilitated growth of

26 ht the importance of heterogeneous chemistry on ice clouds, and imply an additional Bry source from t

27 in the SU during the period 1935-1991 based on ice-core concentration records from Belukha glacier i

28 sion history for the Andean Altiplano, based on ice-core records from Illimani glacier in Bolivia, pr

29 Twenty years ago, measurements on ice cores showed that the concentration of carbon dio

30 g considered proxies for possible life forms on ice-covered extraterrestrial bodies.

31 on, we found that survival is less dependent on ice-crystal formation than expected.

32 should be collected, kept at 4 degrees C or on ice during transportation, and extracted ideally with

33 find that frontal ablation is not dependent on ice dynamics, nor reduced by glacier surface freeze-u

34 n kinase activity of Mos was lost within 6 h on ice even though the Mos protein was not degraded and

35 at Ca(2+) uptake was sensitive to incubation on ice, extremely labile in the absence of protease inhi

36 r system that may exert an important control on ice flow and mass balance.

37 ystems of Thwaites Glacier and their control on ice flow have not been characterized by geophysical a

38 We propose that sedimentary control on ice flow is a viable alternative to existing models o

39 magnitude larger, seasonal melt's influence on ice flow is likely confined to those regions dominate

40 diverse subglacial landscapes have an impact on ice flow, and present a challenge for modelling ice-s

41 ngle-chain antibody (Hu-P4G7) and incubating on ice for 15 min.

42 sence of Vi under ultraviolet (365 nm) light on ice for 60 min.

43 d storage techniques, pig livers were stored on ice for either 2 or 16 hr, after which phosphorus-31

44 y could partially compensate for the loss of on-ice foraging opportunities caused by climate change.

45 , no direct influence of the plasma channels on ice formation or precipitation processes could be det

46 mpact of twenty-first century climate change on ice-free areas under two Intergovernmental Panel on C

47 AGTATCTATGAG) and the 12-mer d(CTCATAATACTC) on ice gave a major product that could be reverted to th

48 of the aqueous solutions or vapor deposition on ice grains, exhibited unequivocal bathochromic shifts

49 Similar to their effects on ice growth, the AF(G)Ps can inhibit MDM crystal growt

50 Blood samples were placed on ice immediately after collection and analyzed within

51 iles of the product HA were to chill samples on ice in the presence of both EDTA and UDP.

52 i membranes during a second-stage incubation on ice is fully sensitive to Tris extraction, indicating

53 dividual samples and show that keeping blood on ice markedly reduces changes to the transcriptome.

54 Left atrial thrombus identified on ICE may occur during LA catheter ablation procedures

55 However, the impact of hydrodynamic coupling on ice motion over decadal timescales remains poorly con

56 the solvation and ionization of HCl adsorbed on ice nanoparticles kept at progressively higher temper

57 This study focused on ice nucleation and propagation, related water shifts

58 may help to explain why experimental results on ice nucleation rates yield different results in diffe

59 An association rate constant on ice of 1.9 x 10(2) M-1s-1 was obtained.

60 le changes in the environment (e.g., walking on ice) or in ourselves (e.g., injury).

61 d impact of cirrus clouds on climate depends on ice particle number, size, morphology, and compositio

62 This suggests that modelling based on ice physics may be the best way of matching isotopic

63 The fourth reconstruction, which is based on ice physics, has a low enough Mississippi-routed melt

64 rature of -1.5 degrees C or directly chilled on ice prior to 144h of ice storage.

65 port the discovery of an ion-specific effect on ice recrystallization.

66 ealed in 10 min, whereas 60% of cells placed on ice remained propidium-permeable even in 30 min.

67 ant to understanding heterogeneous catalysis on ice, remains an experimental challenge.

68 We collected a multiyear data set on ice scouring frequency from Antarctica by using uniqu

69 streams exerted progressively less influence on ice sheet mass balance during the retreat of the Laur

70 methane sequestration and subsequent release on ice sheet retreat that led to the formation of a suit

71 th the Antarctic Ice Sheet but their control on ice-sheet dynamics and their ability to harbour life

72 -water environments and CO2-climate feedback on ice-sheet growth.

73 e caused glacial cycles through their impact on ice-sheet mass balance.

74 at magmatic flux acts as a negative feedback on ice-sheet size.

75 ulations cluster mainly on coasts and rarely on ice sheets.

76 ing glaciers contrast with steady velocities on ice-shelf-terminating glaciers and slow speeds on lan

77 However, surface rivers forming on ice shelves could potentially export stored meltwater

78 ce Sheet that incorporate meltwater's impact on ice shelves, but ignore the movement of water across

79 ioligand in binding assays with intact cells on ice, similar to that for the wild-type receptor.

80 expected if subglacial erosion rate depends on ice sliding velocity.

81 ion rate, with most of this growth occurring on Ice Stream C.

82 Tidally induced motion on ice streams has previously been thought to be limited

83 In fact, the transformation of HCl adsorbed on ice surfaces from a predominantly molecular form to i

84 cess also occurs in small water clusters and on ice surfaces, and recent attention has focused on the

85 l melting, our simulations put a lower limit on ice thickness at the locations and times of impact.

86 estimation of dCHO concentrations from data on ice thickness, salinity, and vertical position in cor

87 nd the band areas showed a linear dependence on ice thickness.

88 proximately 5.1 m, respectively, which based on ice thicknesses at the summit drill sites in 2000 rep

89 polyether chain length has a profound effect on ICE, tissue iron decorporation, and ligand physiochem

90 ion for 30 s, followed by cooling the sample on ice to room temperature (~40 s) and then intermittent

91 ardiac surgery and stored in saline solution on ice until transplantation.

92 the present, implying that tropical controls on ice volumes were asynchronous with those in the North

93 rt-term storage of freshly collected samples on ice was effective without interfering with the chemis

94 ane at 37 degreesC, followed by AP-1 binding on ice, we find that the high-affinity nucleating sites

95 Thrombi on ICE were mobile, averaged 18 +/- 5.9 mm long by 4.4 +

96 helix (minihelix(Phe)) when annealed rapidly on ice, while the same molecule formed a duplex structur

97 s of age were preserved in Optisol, received on ice within 24 to 36 hours of death, and immediately f