ライフサイエンスコーパス: warmth

1 narcissism is cultivated by lack of parental warmth).

2 atus and expertise but also trustworthiness (warmth).

3 may have punctuated this episode of extreme warmth.

4 nnel that functions as a molecular sensor of warmth.

5 xplain the maintenance of this unprecedented warmth.

6 rms that high [CO2]atm coincided with Eocene warmth.

7 ness of the extremities that is triggered by warmth.

8 lay an important role in determining, global warmth.

9 sequence, not the cause, of extreme Cenozoic warmth.

10 d pups to locomote farther to gain access to warmth.

11 ed to explain these past intervals of global warmth.

12 on dioxide emissions helped cause the global warmth.

13 et may have existed despite overall climatic warmth.

14 initiated the sustained interval of Pliocene warmth.

15 s are selectively activated by environmental warmth.

16 esteem, parental overvaluation, and parental warmth.

17 ental overvaluation, not by lack of parental warmth.

18 females co-occur in an intermediate zone of warmth.

19 stantial role in maintaining early Paleogene warmth.

20 the long early Cenozoic interval of elevated warmth.

21 appear particularly sensitive to drought and warmth.

22 te conditions and relative tropical Atlantic warmth.

23 The rate of severe warmth (2.1%) was significantly higher in group 3 (2.8%)

24 sensory neurons respond to chemicals but not warmth, a specificity conferred by a chemosensory-specif

25 tivity) among Met carriers, whereas parental warmth acted as a protective factor for good IGT perform

26 Here we identify a small set of warmth-activated anterior cell (AC) neurons located in t

27 The extreme warmth allowed species expansion and establishment of an

28 sms may allow discrimination of host-derived warmth--an attractant--from chemical repellents.

29 versely, higher amounts of reported parental warmth and affection during childhood was associated wit

30 Warmth and cold sensations are known to derive from sepa

31 imensions - and their associated attributes: warmth and competence - the sentiment framework cedes pr

32 bs, rated as American society views them, on warmth and competence dimensions, as well as relevant em

33 tional peace and conflict reflect ambivalent warmth and competence stereotypes: High-conflict societi

34 Furthermore, naltrexone reduced feelings of warmth and increased vasoconstriction during social incl

35 variable and unpredictable than the uniform warmth and moisture of the throat.

36 uing change in the magnitude of interglacial warmth and P(CO(2)) at around 430,000 years ago (430 ka)

37 Multiproxy evidence suggests extreme warmth and polar amplification during the middle Pliocen

38 rical correlations between cumulative summer warmth and riparian shrub height to reconstruct annual c

39 and feedback mechanisms that maintained this warmth and the broad dynamic range that these paleoclima

40 essment of their contribution to past global warmth and the equilibrium climate sensitivity of the Ea

41 xty participants experience painful heat and warmth and view photos of ex-partners and friends on sep

42 manic episodes was predicted by low maternal warmth and younger baseline age.

43 volves inferring both their apparent intent (warmth) and capability (competence).

44 l reactions (pain, erythema, induration, and warmth) and systemic reactions (chills, arthralgias, and

45 value, including social status, competence, warmth, and any other cues of one's ability or willingne

46 100-fold during the transition from cold to warmth, and no other mitochondrial proteins matched UCP1

47 d reveals three time intervals of comparable warmth: anno Domini (A.D.) 0-300, 850-1200, and post-180

48 Recent warmth appears anomalous for at least the past 1,300 yea

49 llen records suggest an onset of peak summer warmth around 9,000 years ago.

50 Although the significance of maternal warmth as a predictor is consistent with reports in adul

51 pose tissue (BAT) of animals that huddle for warmth as offspring.

52 by patient-reported increases in swelling or warmth at the procedure site.

53 ve invoked a denser atmosphere that provided warmth by nitrogen pressure broadening or enhanced green

54 nisms currently proposed to explain Pliocene warmth can simultaneously reproduce all three crucial fe

55 Existing studies of how evaluations of warmth, competence, and closeness shape people's reactio

56 ng past and, ultimately, future interglacial warmth could be produced by (10)Be and (26)Al records fr

57 hese included increased von Frey, bumps, and warmth detection thresholds as compared with healthy vol

58 al 3 (TRPV3), which has been implicated as a warmth detector, becomes responsive to warm temperatures

59 limate studies suggest that increased global warmth during the Eocene epoch was greatly amplified at

60 tage (MIS) 11, an unusually long interval of warmth during the ice age.

61 ied to a shift from relatively stable global warmth during the mid-Pliocene to the high-amplitude gla

62 Miocene Climatic Optimum, a period of global warmth during which average surface temperatures were 3-

63 bivalently perceived high-competence but low-warmth, "envied" professions included lawyers, chief exe

64 s a clinical diagnosis based on intermittent warmth, erythema, and pain in the distal extremities.

65 s a clinical diagnosis based on intermittent warmth, erythema, and pain in the distal extremities.

66 However, the warmth-evoked responses we observe most closely resemble

67 An indirect effect of GTF2I genotype on the warmth facet of extraversion was mediated by decreased t

68 yed a substantial role in the elicitation of warmth from parents and a more modest role in influencin

69 stimuli have yet been described for TRPV3, a warmth-gated ion channel expressed prominently in skin k

70 e rapid response of flies exposed to a steep warmth gradient does not require TRPA1; rather, the gust

71 Early Bolling-Allerod warmth halved the mass of the CIS in as little as 500 ye

72 pain in the extremities in response to mild warmth, has been linked to mutations in Nav1.7.

73 d by severe burning pain in response to mild warmth, has been shown to be caused by gain-of-function

74 specificity of the signature to pain versus warmth in a new sample.

75 pound camphor, which modulates sensations of warmth in humans, proved to be a specific activator of T

76 S and a limited glacial response to Pliocene warmth in the Aurora subglacial basin catchment.

77 ast 1200 years is the geographical extent of warmth in the middle to late 20th century.

78 rto reported, with somewhat greater Medieval warmth in the Northern Hemisphere, albeit still not reac

79 n association between genotype and increased warmth in women.

80 Ratings of perceived warmth increased in proportion to the increase in skin t

81 xclusion during the game reduced feelings of warmth, increased feelings of anger, and increased blood

82 Warmth is a characteristic but nondiagnostic feature of

83 re variability have demonstrated that recent warmth is anomalous relative to preceding centuries or m

84 Early Holocene (10,000 to 5000 years ago) warmth is followed by ~0.7 degrees C cooling through the

85 "Warmth" is the most powerful personality trait in social

86 pisodes of intense burning pain triggered by warmth, is caused by mutations in sodium channel Nav1.7,

87 We postulated that warmth-liking has a specific somatovisceral signature, w

88 Warmth-liking, as an emotion system, is activated during

89 Secure attachment predicted higher levels of warmth-liking, physiological quiescence, and less negati

90 sting that the pleasant thermal sensation of warmth may in fact just reflect reduced aversive input f

91 Five had a greater impact in women: parental warmth, neuroticism, divorce, social support, and marita

92 nding, self-esteem was predicted by parental warmth, not by parental overvaluation.

93 Warmth of affect demonstrated in the clinic setting was

94 latitude ocean is strongly stratified by the warmth of its surface water.

95 The extreme warmth of particular intervals of geologic history canno

96 The transition from the extreme global warmth of the early Eocene 'greenhouse' climate approxim

97 us), indicating that a large fraction of the warmth of the early Eocene greenhouse was driven by incr

98 Prior collapses during the warmth of the early Pliocene epoch and some Pleistocene

99 During the warmth of the early-mid Pliocene, we find evidence for e

100 The warmth of the Indian and west Pacific oceans was unprece

101 ter vapour feedbacks may help to explain the warmth of the late Miocene.

102 limate underwent a major transition from the warmth of the late Pliocene, when global surface tempera

103 of Arctic polar climate from the protracted warmth of the middle Pliocene into the earliest glacial

104 Periods of widespread warmth or cold are identified by positive or negative de

105 the total of pain-plus-thermal (sensation of warmth or cold) sites was the same in all areas.

106 we hypothesized that experiences of physical warmth (or coldness) would increase feelings of interper

107 ss) would increase feelings of interpersonal warmth (or coldness), without the person's awareness of

108 led the delivery of painful heat, nonpainful warmth, or no stimulation.

109 of carbon dioxide in combination with global warmth over this period.

110 A significant interaction of abuse and warmth (P < 0.05) was found, such that individuals repor

111 discriminating painful heat from nonpainful warmth, pain anticipation, and pain recall.

112 ient receptor potential channels account for warmth perception under injury-free conditions.

113 e North Pacific Ocean, and show that oceanic warmth persisted throughout the interval of low p(co(2))

114 Low maternal warmth predicted faster relapse after recovery from mani

115 ing for family psychopathology, low maternal warmth predicted relapse to mania, and more weeks ill wi

116 enotype and both parental negativity and low warmth predicting overall antisocial behavior, as well a

117 nses to warming, increasing the dominance of warmth-preferring taxa over cold-tolerant plants (a proc

118 kness upon humidity reduction to restore its warmth-preservation function.

119 Instrument produced three factors: parental warmth, protectiveness, and authoritarianism.

120 Although the role of the warmth receptors in epidermal homeostasis (EH) was eluci

121 gically recent interval of long-term average warmth relative to the last million years, and shares si

122 However, if warmth-requiring trees were able to migrate into current

123 , and behavioral (competence, dominance, and warmth) responses to the stressor.

124 nd/or thermogenesis), but it did not involve warmth-seeking behavior.

125 antitative sensory testing revealed impaired warmth sensation in the proband, father and brother.

126 nd reveal the molecular logic for peripheral warmth sensing.

127 This internal warmth-sensing pathway promotes avoidance of slightly el

128 diverse cell types, suggesting that it is a warmth sensor.

129 distinction between peripheral and internal warmth sensors in this tiny ectotherm reminiscent of the

130 importance to either internal or peripheral warmth sensors.

131 ate of recovery, and a low level of maternal warmth significantly predicted rate of relapse.

132 tween expectation and delivery of nonpainful warmth stimulation.

133 ould have operated through periods of global warmth such as the Early Cenozoic.

134 6 degrees C) and a longer period of extended warmth, suggesting that local insolation variations were

135 tissue, presenting with expanding erythema, warmth, tenderness, and swelling.

136 both parent and child are more important for warmth than for protectiveness or authoritarianism.

137 The Medieval period is found to display warmth that matches or exceeds that of the past decade i

138 pisodes of intense burning pain triggered by warmth, the effects of increased temperature on DRG neur

139 Pliocene warmth thus clearly represents a discrete interval which

140 peratures shows the spatial extent of recent warmth to be of greater significance than that during th

141 n a rapid transition from extensive regional warmth to the dramatic instability of the subsequent app

142 nts) and a protective factor (i.e., parental warmth) to influence affective decision making as measur

143 a system for the cell biological analysis of warmth transduction.

144 hannels, suggesting a cellular mechanism for warmth-triggered pain episodes in IEM patients.

145 in temperature suggests a cellular basis for warmth-triggered pain in IEM.

146 d from IEM patients, but the question of how warmth triggers episodes of pain in IEM has not been wel

147 both physical temperature and interpersonal warmth (trust) information.

148 ed, and the latency to escape to a region of warmth was measured.

149 twins as parents indicated that provision of warmth was substantially heritable, while resemblance be

150 ferase-based assay, and ratings of perceived warmth were taken at each temperature.

151 nce of genetic factors in eliciting parental warmth which was midway between that from parents' repor

152 ing host body temperatures, seeking relative warmth while avoiding both relative cool and stimuli exc

153 iminated between painful heat and nonpainful warmth with 93% sensitivity and specificity (95% CI, 84

154 he most recent period of greater-than-modern warmth within a continuously cooling trajectory.

155 that documents a period of extreme climatic warmth without seasonal ice, with minimum mean annual te