ライフサイエンスコーパス: iceberg

1 ne, with seizures being just the 'tip of the iceberg'.

2 uropa, in which we find evidence for mobile 'icebergs'.

3 the available data show only the tip of the iceberg.

4 t these likely represent only the tip of the iceberg.

5 tory responses analogous to the CARD protein ICEBERG.

6 enes it contained proved to be the tip of an iceberg.

7 atory compounds, we know just the tip of the iceberg.

8 ular domain is merely the tip of a molecular iceberg.

9 , this is just the tip of the research waste iceberg.

10 these efforts represent only the tip of the iceberg.

11 istance at both QTLs originate from cultivar Iceberg.

12 at we have now merely reached the tip of the iceberg.

13 intersections represent only the tip of the iceberg.

14 l iron inputs are thought to be dominated by icebergs.

15 red only by perennial sea ice with scattered icebergs.

16 glacial halocline related to melt water from icebergs.

17 ert with the flux of freshwater from melting icebergs.

18 he freshwater flux that results from melting icebergs.

19 ion, similar to that identified in Antarctic icebergs.

20 -1)) associated with suspended sediment than icebergs (0-241 kg km(-2) a(-1)).

21 (<0.45 mum) iron (6-81 kg km(-2) a(-1)) than icebergs (0.0-1.2 kg km(-2) a(-1)).

22 Two free-drifting icebergs, 0.1 and 30.8 square kilometers in aerial surfa

23 Data on whether icebergs affect bacterioplankton function and compositio

24 Cultivars Iceberg and Grand Rapids that were released in the 18th

25 CARD-8 binds also to ICEBERG and pseudo-ICE, two other recently identified pr

26 and water viscosity, winter calm and summer (iceberg and storm) disturbance and resources.

27 terize the meltwater field around individual icebergs and integrate the results with regional- and gl

28 uses, and nematodes represent the tip of the iceberg, and few details of their host-parasite relation

29 ially contributed to the melting of sea ice, icebergs, and terminal ice-sheet margins.

30 e newer treatments represent the "tip of the iceberg," and as our basic knowledge increases, so too w

31 c solute, water forms transient microscopic "icebergs" arising from strengthened water hydrogen bondi

32 tides played a catalytic role in liberating iceberg armadas during that time.

33 our glacial cycles, implying that in general icebergs arrived too late to have triggered cooling.

34 acterized by small numbers of large, tabular icebergs as is observed today, which would produce wide,

35 The arrival and grounding of Iceberg B9B in Commonwealth Bay in March 2011 led to the

36 this site in the past after the grounding of Iceberg B9B.

37 een North Atlantic cold events and increased iceberg calving and dispersal from ice sheets surroundin

38 ergs, has been accompanied by an increase in iceberg calving and ice mass loss.

39 s of iceberg-keel plough marks, we find that iceberg calving during the most recent deglaciation was

40 Iceberg calving has been assumed to be the dominant caus

41 diverse set of ice shelves demonstrates that iceberg calving increases with the along-flow spreading

42 half of Greenland's mass loss occurs through iceberg calving, but the physical mechanisms operating d

43 hical perturbations introduced by a drifting iceberg can affect activity, composition, and substrate

44 the characteristic size-frequency scaling of icebergs can be explained by the emergence of a dominant

45 Although the size-frequency distributions of icebergs can provide insight into how they disintegrate,

46 These results suggest that free-drifting icebergs can substantially affect the pelagic ecosystem

47 results from the horizontal force caused by iceberg capsize and acceleration away from the glacier f

48 ce of a dominant set of driving processes of iceberg degradation towards the open ocean.

49 silica in Greenland Ice Sheet meltwaters and icebergs, demonstrating the potential for high ice sheet

50 e past five glaciation cycles, indicators of iceberg discharge and sea-surface temperature display dr

51 ntic region, beginning with the catastrophic iceberg discharge Heinrich event H1, 17,500 yr ago, and

52 lacial cycle, leading to the hypothesis that iceberg discharge may be a consequence of stadial condit

53 The model generates a time series of iceberg discharge that closely agrees with ice-rafted de

54 riggering rapid margin retreat and increased iceberg discharge.

55 Episodic iceberg-discharge events from the Hudson Strait Ice Stre

56 ly 4 degrees to 6 degreesC, and catastrophic iceberg discharges begin alternating repeatedly with bri

57 e last glacial period interpreted as massive iceberg discharges from the Laurentide Ice Sheet.

58 Massive iceberg discharges from the Northern Hemisphere ice shee

59 tennial-scale excursions during catastrophic iceberg discharges of the Heinrich stadials.

60 The mechanisms linking North Atlantic iceberg discharges with subantarctic productivity remain

61 est reductions during episodic Hudson Strait iceberg discharges, while sharp northern warming followe

62 zes observed is a product of fracture-driven iceberg disintegration and dimensional reductions throug

63 seismic monitoring to examine mechanisms of iceberg disintegration as a function of drift.

64 ize-frequency distribution required to model iceberg distributions accurately must vary according to

65 We assessed the influence of iceberg drift on bacterial community composition and on

66 e of the generator potential (the so-called "iceberg effect"), but not to maximize the transmission o

67 Unlike the iceberg effect, contrast invariance remains intact even

68 et, such fast errors are only the tip of the iceberg: electromyography (EMG) revealed fast subthresho

69 Meltwater and icebergs entering the North Atlantic alter oceanic and a

70 ophyll, krill, and seabirds surrounding each iceberg, extending out to a radial distance of approxima

71 We document eight events of increased iceberg flux from various parts of the AIS between 20,00

72 The proliferation of icebergs from Antarctica over the past decade has raised

73 r 'icehouse' world influenced by sea ice and icebergs from the middle Eocene epoch to the present.

74 lange, a floating aggregation of sea ice and icebergs, has been accompanied by an increase in iceberg

75 deposits of lysozyme are only the tip of an iceberg hiding a crowd of insoluble aggregates.

76 bal warming, increased frequency of drifting icebergs in polar regions holds the potential to affect

77 vidence for enhanced hydrogen bonding and/or icebergs in such solutions.

78 Extrapolating these results to all icebergs in the same size range, with the use of iceberg

79 s suggests that they were carved by grounded icebergs influenced by tidal and geostrophic ocean curre

80 to utilize specific carbon substrates in the iceberg-influenced waters compared with the undisturbed

81 erent community composition were observed in iceberg-influenced waters relative to the undisturbed wa

82 s associated with Heinrich events: Extensive iceberg influxes into the North Atlantic Ocean linked to

83 with this, enforced retroviral expression of ICEBERG inhibits lipopolysaccharide-induced IL-1beta gen

84 ICEBERG is a novel protein that inhibits generation of I

85 ICEBERG is induced by proinflammatory stimuli, suggestin

86 Iceberg-keel plough marks on the sea-floor provide geolo

87 rm shape and cross-sectional morphologies of iceberg-keel plough marks, we find that iceberg calving

88 Although the freshwater derived from melting icebergs may provide a positive feedback for enhancing a

89 These drifting icebergs mix the water column, influence stratification

90 We described these incidences in terms of an iceberg model of self-harm.

91 In contrast to the classical "iceberg" model of hydrophobic hydration, the favorable e

92 vide a physical picture of the long-debated "iceberg" model; we show that the slow, long-time compone

93 vide geological evidence of past and present iceberg morphology, keel depth and drift direction.

94 proteins are likely to be just the tip of an iceberg of multifunctional proteins that stabilize and c

95 ntified to date represent just the tip of an iceberg of risk variants likely to include hundreds of m

96 orphological changes are only the tip of the iceberg of the entire protective mechanisms.

97 ver, is this just the tip of a 'conservation iceberg' or do these sequences represent a specific clas

98 The CZS could be just "the tip of the iceberg", pending the documentation of a spectrum of dis

99 ergs in the same size range, with the use of iceberg population estimates from satellite surveys, ind

100 undamentally, there is a discrepancy between iceberg power-law size-frequency distributions observed

101 The number of icebergs produced from ice-shelf disintegration has incr

102 of icebergs smaller than the typical tabular icebergs produced today.

103 ure, when glaciers reach grounding lines and iceberg production diminishes, is as a major global sink

104 However, a Southern Ocean (Atlantic-sector) iceberg rafted debris event appears to have occurred syn

105 Marine records of iceberg-rafted debris (IBRD) provide a nearly continuous

106 analysed high-temporal-resolution records of iceberg-rafted debris derived from the Antarctic Ice She

107 alignment of key climate data sets spanning iceberg-rafted debris event Heinrich 3 and Greenland Int

108 The structure of ICEBERG reveals it to be a member of the death-domain-fo

109 correlated positively with the frequency of iceberg scour at the different sites with the highest re

110 helves are typically deeper than most modern iceberg scouring, bacterial breakdown rates are slow, an

111 Reduced fast ice after 2006 ramped iceberg scouring, killing half the encrusting benthos ea

112 ed on an exquisitely preserved set of buried iceberg scours seen in three-dimensional seismic reflect

113 rced ice losses are increasing potential for iceberg-seabed collisions, termed ice scour.

114 shift in the size-frequency distribution of iceberg sizes observed is a product of fracture-driven i

115 0 years ago, which produced large numbers of icebergs smaller than the typical tabular icebergs produ

116 ent only the clearance-resistant "tip of the iceberg." Such aberrantly circulating mucins could play

117 d in the Sahel region at the time of massive iceberg surges, leading to large freshwater discharges.

118 ed by the temporary grounding of two immense icebergs that (i) erected a veritable fence separating c

119 heet sporadically discharged huge numbers of icebergs through the Hudson Strait into the North Atlant

120 ationship between the meltwater field of the iceberg to the larger-scale marine ecosystem of the Sout

121 harge-charge interactions mediate binding of ICEBERG to the prodomain of caspase-1.

122 ies are likely to be the tip of an "invasion iceberg" to the NW Atlantic from Great Britain and Irela

123 nt less than previous estimates derived from iceberg tracking.

124 owever, this research is only the tip of the iceberg when it comes to writing an 'epigenetic instruct

125 y verified TMD, although that was a "symptom iceberg" when compared with the 19% annual rate of facia

126 ndeed likely to represent only the tip of an iceberg with hundreds or more of additional micro-RNAs (

127 fection may therefore reflect the tip of the iceberg with regard to the burden of colonization of a s

128 as characterized by large numbers of smaller icebergs with V-shaped keels.

129 n tissue samples reveal only the "tip of the iceberg", with most of the important changes occurring o