ライフサイエンスコーパス: transpiration

1 t with decreases in stomatal conductance and transpiration.

2 CO(2) availability with suppressed stomatal transpiration.

3 lic conductance partly counteracted those of transpiration.

4 sis and by reducing stomatal conductance and transpiration.

5 s, while stomata facilitate gas exchange and transpiration.

6 o changes in stomatal density that influence transpiration.

7 es to the atmosphere through evaporation and transpiration.

8 ng a watershed-scale fertilization effect on transpiration.

9 on maize yield, river flow, evaporation, and transpiration.

10 ke for photosynthesis and water loss through transpiration.

11 uard cells regulate plant photosynthesis and transpiration.

12 caused by lack of AtrbohF is dependent upon transpiration.

13 edistributes wax composition, and suppresses transpiration.

14 slowly when the shoot was covered to prevent transpiration.

15 e major function is to replace water lost to transpiration.

16 logical forcing as a result of reduced plant transpiration.

17 leaf for photosynthesis with water loss via transpiration.

18 ncy, germination, seedling growth, and plant transpiration.

19 pheric carbon dioxide (CO2) effects on plant transpiration.

20 greater interception of solar energy and low transpiration.

21 l homeostasis, stomatal dynamics, and foliar transpiration.

22 ynthesis and the loss of water vapour during transpiration.

23 photosynthesis and the loss of water during transpiration.

24 ve relationship between leaf temperature and transpiration.

25 es stomatal closure to prevent water loss by transpiration.

26 2ca mutants displayed a phenotype of reduced transpiration.

27 photosynthesis as well as water loss through transpiration.

28 mediate acclimation responses and to reduce transpiration.

29 lar system of trees during the diel cycle of transpiration.

30 eric CO2 influences plant photosynthesis and transpiration.

31 s, including stomata, the organs controlling transpiration.

32 which vascular land plants regulate daytime transpiration.

33 d guard cells and are affected in growth and transpiration.

34 plies parts of soil water recharge and plant transpiration.

35 her, stomatal conductance almost double, and transpiration 60% higher than for C3 plants.

36 cted E(max) compared well with measured peak transpiration across plant sizes and growth conditions (

37 ecycling of water and probably reduced plant transpiration, although the rainforest persisted through

38 oportional response of stomatally controlled transpiration and 'free' forest floor evaporation to cha

39 Under water deficit, plants reduce transpiration and are able to improve carbon for water e

40 ylem and phloem conduits required to sustain transpiration and assimilation, respectively, were calcu

41 Green (or biotic) metabolism is measured via transpiration and blue (or abiotic) metabolism through r

42 is 'leaves minimise the summed unit costs of transpiration and carboxylation' predicts leaf-internal/

43 g decline of LER began at very low light and transpiration and closely followed the stomatal opening

44 seed plants before being co-opted to control transpiration and CO2 exchange in derived seed plants.

45 in M. racemosum physiology (photosynthesis, transpiration and conductance) and allocation (carbon st

46 rates, larger stomatal apertures, more rapid transpiration and decreased tolerance to dehydration str

47 ponses are hard to anticipate because canopy transpiration and diffusive conductance (G) respond to d

48 consequently plants have decreased levels of transpiration and display drought tolerance.

49 HD2C-GFP transgenic plants displayed reduced transpiration and enhanced tolerance to salt and drought

50 Here we use the distinct isotope effects of transpiration and evaporation to show that transpiration

51 em declines markedly and the requirements of transpiration and further expansion are fulfilled primar

52 Transpiration and gas exchange occur through stomata.

53 sic acid, which leads to increased levels of transpiration and gas exchange, as well as better salicy

54 used to follow the fluid transport driven by transpiration and image the spatial distributions of sev

55 cry and phot are critical for the control of transpiration and photosynthesis rates in the field.

56 impacts of HR include increasing dry-season transpiration and photosynthetic rates, prolonging the l

57 eous WUE that was attributable to ~25% lower transpiration and stomatal conductance but equivalent CO

58 me drought synergistically reduced ecosystem transpiration and the resilience of key-stone oak tree s

59 carbon dioxide concentration, which reduces transpiration and thus leaves more water at the land sur

60 Recalibration of the transpiration and volatilisation parameters improved the

61 More rapid transpiration and water depletion can also explain the p

62 af is crucial for efficient gas exchange and transpiration and, therefore, for overall function.

63 sis, while the water balance is dominated by transpiration, and both fluxes are controlled by plant s

64 tate problem, in the context of peristomatal transpiration, and consider the relation of transpiratio

65 cry1 cry2 have reduced stomatal conductance, transpiration, and photosynthesis, particularly under th

66 worldwide and can enhance stomatal opening, transpiration, and plant carbon gain.

67 rd cells, higher rates of water loss through transpiration, and severe slowdown of stomatal closure.

68 conductance of CO2, photosynthesis, K(leaf), transpiration, and shoot biomass.

69 nesis, seed dormancy, root and shoot growth, transpiration, and stress tolerance.

70 h its control of stomatal aperture and water transpiration, and transgenic modulation of ABA levels t

71 ssume that groundwater, streamflow and plant transpiration are all sourced and mediated by the same w

72 cean warming, and changes in evaporation and transpiration are driving changes in the global hydrolog

73 uses an increase in stomatal conductance and transpiration as well as a decrease in plant biomass.

74 atmosphere radiative imbalance from enhanced transpiration (associated with the expanded forest cover

75 face layers, and this water subsidy sustains transpiration at rates that deep roots alone cannot acco

76 We conclude that the cuticular transpiration barrier is primarily formed by the intracu

77 tionships, we quantified the composition and transpiration barrier properties of the gl1 mutant leaf

78 The goal of this study was to localize the transpiration barrier within the layered structure of cu

79 xtends well beyond its primary function as a transpiration barrier, playing important roles in proces

80 the intracuticular wax was important for the transpiration barrier.

81 r waxes contributed equally to the cuticular transpiration barrier.

82 WUE, water-use efficiency (WUE, GPP/ET), and transpiration-based WUE (WUEt , the ratio of GPP and tra

83 Control of transpiration became possible through the development of

84 ving droughted trees maintained or increased transpiration because of reduced competition for water a

85 Here, inspired by the water transpiration behavior of trees, the use of carbon nanot

86 fect is related mainly to local increases in transpiration, but also to higher albedo.

87 nificantly increased maize yields by 12% and transpiration by 2% on average across South Africa.

88 stomata jointly regulate photosynthesis and transpiration by affecting carbon dioxide and water vapo

89 t HR increases dry season (July to November) transpiration by approximately 40% over the Amazon.

90 eliorates the effects of the slac1 mutant on transpiration by regulating the K(+) channels.

91 We demonstrate that increasing transpiration can enhance nutrient uptake when water is

92 ction opposite to the bulk flow under normal transpiration conditions.

93 omata, and correspondingly reduced levels of transpiration, conserve soil moisture and are highly dro

94 A partitioning analysis showed that transpiration contributed less to total ET for maize com

95 Transpiration decreased 17% and leaf psi w increased 39%

96 xylem water potentials and fewer days until transpiration decreased after watering was withheld.

97 d with increased TYLCV resistance, increased transpiration, decreased abscisic acid levels, and incre

98 sap, and in turn protecting shoot cells from transpiration-dependent delivery of excess Na.

99 of an Arabidopsis thaliana mutant displaying transpiration-dependent soil-salinity tolerance.

100 governs CO(2) uptake for photosynthesis and transpiration, determining plant productivity and water

101 movements and affected CO2 assimilation and transpiration differentially between dark and light cond

102 ine the relative magnitudes of gas-phase and transpiration-driven volatilization mechanisms.

103 s are consistent with a suppression of plant transpiration due to CO2-induced stomatal closure.

104 atered recovery period, facilitating reduced transpiration during a subsequent dehydration stress.

105 species nighttime conductance (g(night)) and transpiration (E(night)) to soil nutrient and water limi

106 milation (A), stomatal conductance (gs ) and transpiration (E) on mature leaves of R. stricta.

107 The model predicted canopy transpiration (E), canopy diffusive conductance (G), and

108 an canopy stomatal conductance (GS), keeping transpiration (EC) and, hence, runoff unaltered.

109 he control of transpirational water loss and transpiration efficiency (TE) we carried out an infrared

110 ospheric vapor pressure deficit and reducing transpiration efficiency (TE), but an increase in TE due

111 As a consequence, the enhancement of transpiration efficiency (TE)-that is, the biomass produ

112 on at elevated [CO2 ] that outpaced gains in transpiration efficiency (TE).

113 o of assimilation to transpiration is called transpiration efficiency (TE).

114 ical changes resulted in reduced whole-plant transpiration efficiency and reduced fitness under water

115 Both had higher transpiration efficiency because of their lower stomatal

116 ive association between Thick(leaf) and leaf transpiration efficiency.

117 lics and of the effects of PWS and nocturnal transpiration (Fe,night) on hydraulic redistribution (HR

118 entalized pools of water supply either plant transpiration fluxes or the combined fluxes of groundwat

119 We report the only study of forest transpiration following a long-term (>10 year) experimen

120 ings at both growing temperatures, increased transpiration for seedlings grown at 30 degrees C by 40%

121 ower law for the probability distribution of transpiration from a randomly chosen subbasin.

122 Global-scale estimates of transpiration from climate models are poorly constrained

123 Transpiration from the Amazon rainforest generates an es

124 during 1981-2012, and its three components: transpiration from vegetation (Et), direct evaporation f

125 ssing ABA sensitivity, which then aggravates transpiration further.

126 nd plants must balance CO2 assimilation with transpiration in order to minimize drought stress and ma

127 hetic 'tree' captures the main attributes of transpiration in plants: transduction of subsaturation i

128 st under drought, and the reduced post-pulse transpiration in the droughted trees that died was attri

129 ctance (Gst) measurements revealed that leaf transpiration in the sextuple pyr/pyl mutant was higher

130 minant concentrations increased rapidly with transpiration in the spring and decreased in the fall, r

131 l reaching the soil and directly recycled as transpiration increased to 100%.

132 ubled carbon dioxide concentrations on plant transpiration increases simulated global mean runoff by

133 Globally, transpiration is 64 +/- 13% (mean +/- 1 standard deviati

134 Stomatal transpiration is at the center of a crisis in water avai

135 f transpiration and evaporation to show that transpiration is by far the largest water flux from Eart

136 The ratio of assimilation to transpiration is called transpiration efficiency (TE).

137 Stomatal control of transpiration is critical for maintaining important proc

138 mponent of the water cycle, yet only daytime transpiration is currently considered in Earth system an

139 The water used for dry season transpiration is from the deep storage layers in the soi

140 tional contribution to the total terrestrial transpiration is limited.

141 stomatal conductance, and as a consequence, transpiration is reduced.

142 ree with conclusions from previous work that transpiration is the main driver for volatilization of V

143 ation-based WUE (WUEt , the ratio of GPP and transpiration), is analyzed from 0.5 degrees gridded fie

144 take by terrestrial vegetation by connecting transpiration losses to carbon assimilation using water-

145 e rate of water loss after stomatal closure (transpiration(min)), water deficit (% below turgid satur

146 ving greater drought-resistance (i.e., lower transpiration(min), water deficit and SLA), but these tr

147 Meanwhile, the transpiration of key-stone tree species decreased, indic

148 ugh its physiological effect (i.e., reducing transpiration of land plants).

149 Higher initial transpiration of seedlings in the 33 degrees C growing t

150 Transpiration of the leaf and canopy, by contrast, is de

151 guard cell to define the water relations and transpiration of the leaf.

152 Stomatal opening and the rise in stomatal transpiration of the mutant was delayed in the light and

153 nt tolerance to toluene, and to decrease the transpiration of toluene to the atmosphere.

154 ings suggest an additional mechanism through transpiration of water vapor and feedbacks from the ocea

155 surface, for photosynthetic gas exchange and transpiration of water.

156 l WH did not significantly affect the yield, transpiration or river flow on the South Africa scale.

157 odel also indicates that such an increase in transpiration over the Amazon and other drought-stressed

158 th surface and subsurface hydrology to study transpiration partitioning at the continental scale.

159 eral groundwater flow in the model increases transpiration partitioning from 47 +/- 13 to 62 +/- 12%.

160 n, stream water transit time and evaporation-transpiration partitioning.

161 rn California, shows that apparently similar transpiration patterns throughout the dry season can eme

162 erived, remarkably constant rates of average transpiration per unit area through the basin structure

163 Leaf photosynthetic rate, transpiration, plant height, leaf area index (LAI), biom

164 on contents were not based on differences in transpiration, pointing to a vacuolar function in regula

165 We measured rapid rates of perianth transpiration ranging from twice to 100 times greater th

166 ism, the guard cell Suc contents at a higher transpiration rate (60% relative humidity [RH]) were com

167 ty [RH]) were compared with those at a lower transpiration rate (90% RH) in broad bean (Vicia faba),

168 th rate (RGR), leaf water potential (psi w), transpiration rate (Tr), photosynthetic rate (Pn), and s

169 Furthermore, leaf transpiration rate also increased prior to APX2 expressi

170 inverse relationship between Thick(leaf) and transpiration rate and a significant positive associatio

171 n soil rehydration considerably quicker than transpiration rate and leaf water potential (typical hal

172 ch their model-estimated maximum sustainable transpiration rate approached zero.

173 Here, we considered the reduction in transpiration rate at night (En) as a possible strategy

174 from the mutant plants display an increased transpiration rate compared with wild-type plants.

175 Transpiration rate increased progressively with leaf tem

176 These results indicate that a high transpiration rate may result in a high guard cell apopl

177 water potentials, thus defining the maximum transpiration rate the xylem can sustain (denoted as E(m

178 In addition, transpiration rate was significantly reduced in TMV infe

179 ical traits, such as projected rosette area, transpiration rate, and rosette water content, were corr

180 nitrogen and shading on photosynthetic rate, transpiration rate, and total root length, root superfic

181 ination, smaller stomatal apertures, a lower transpiration rate, better development of primary and la

182 functional traits, net photosynthetic rate, transpiration rate, M conductance to CO(2) diffusion (g(

183 -deficient conditions, stomatal conductance, transpiration rate, plant hydraulic conductance, leaf wa

184 vars and shading for photosynthetic rate and transpiration rate.

185 dominated by low-LMA taxa with inferred high transpiration rates and short leaf lifespans, were repla

186 ontent, as well as maintaining 35-46% higher transpiration rates as compared to those of wild type (W

187 Stomatal conductance allows maximum transpiration rates despite partial cavitation in the xy

188 overed their hydraulic conductance and their transpiration rates faster than the dAS plants.

189 nts had reduced stomatal opening and reduced transpiration rates in the light or when deprived of CO(

190 boniferous plants were capable of growth and transpiration rates that approach values found in extant

191 ncrease in stomatal density, allowing higher transpiration rates that were sufficient to maintain coo

192 in plants experiencing water deficit, lower transpiration rates, and improved water use efficiency m

193 n have favoured biomass growth and increased transpiration rates, thus reducing available soil water.

194 e controlled by soil Ca2+ concentrations and transpiration rates.

195 ovides two mechanisms for responding to high transpiration rates.

196 to demand ratio, and of actual to potential transpiration ratio) simulated considerably different pa

197 of large lakes and rivers, we conclude that transpiration recycles 62,000 +/- 8,000 km(3) of water p

198 d cells and root cells, and attenuated water transpiration regulation and root growth in response to

199 iration into bare soil evaporation and plant transpiration remains a key uncertainty in the terrestri

200 rque on the radiometer was caused by thermal transpiration, researchers continued to search for ways

201 Transpiration resistances equaled 3 x 10(4) and 1.5 x 10

202 erma) woodland using mixed effects models of transpiration response to event size, antecedent soil mo

203 The role of belowground processes (transpiration, root growth and decomposition) in the ver

204 s evapotranspiration flux into interception, transpiration, soil evaporation, and surface water evapo

205 ficant effects on plant leaf photosynthesis, transpiration, soil respiration, height, and yield, but

206 These gaps are not part of the transpiration stream and result in gpx plants having few

207 Contaminants in the transpiration stream can become bound or incorporated in

208 liage/root concentration factors (FRCF), and transpiration stream concentration factors (TSCF) were c

209 maximal value, showing the robustness of the transpiration stream for conducting water.

210 vascular system against the direction of the transpiration stream has long been a puzzling phenomenon

211 We suggest that attenuation of the transpiration stream in whole plants is required for the

212 er analysis shows that carbon present in the transpiration stream may be used for photosynthesis in t

213 The transpiration stream that passes through a plant may fol

214 When the transpiration stream was attenuated by growing the plant

215 d expand when vessels are reconnected to the transpiration stream.

216 rganisms on root surfaces and emitted in the transpiration stream.

217 m leaves fed exogenous sucrose via the xylem transpiration stream.

218 to prevent its accumulation and loss to the transpiration stream.

219 This transpiration 'supply function' is used to predict a wat

220 s had to cope with the loss of water through transpiration, the inevitable result of photosynthetic C

221 e effect of radiation load on the control of transpiration, the potential for condensation on the ins

222 Plant scientists believe that transpiration-the motion of water from the soil, through

223 This could be achieved by reducing plant transpiration through a better closure of the stomatal p

224 s the question as to whether plants regulate transpiration through stomata to function near E(max).

225 drought stress at low elevations by limiting transpiration through stomatal closure, such that its dr

226 PME34 has a role in the regulation of transpiration through the control of the stomatal apertu

227 oils, and is transported to plant shoots via transpiration through xylem elements in the vascular tis

228 ack, which occurs when deforestation reduces transpiration to a point where the available atmospheric

229 trics that account for the response of plant transpiration to changing CO2, including direct use of P

230 t-related tree mortality caused total forest transpiration to decrease by 30%.

231 Based on the potential for transpiration to increase mass flow of mobile nutrients

232 synthesis and water loss from plants through transpiration to the atmosphere.

233 Surprisingly, given the importance of transpiration to the control of terrestrial water fluxes

234 Direct measurements of transpiration, together with chlorophyll-leaching assays

235 However, models of transpiration transients showed that minor vein collapse

236 Lower transpiration was associated with higher STOMATAL DENSIT

237 Ecosystem transpiration was dominated by the water use of the inva

238 By contrast, at glacial [CO2], transpiration was maintained under moderate drought via

239 ponses and to conventional wisdom, nocturnal transpiration was not affected by previous radiation loa

240 The dominance of transpiration water fluxes in continental evapotranspira

241 nductance; while net photosynthetic rate and transpiration were not affected.

242 ncreased stomatal conductance, and increased transpiration were observed.

243 nctional, associated with photosynthesis and transpiration were quantified on 24 accessions (represen

244 and between, structure, photosynthesis, and transpiration were tested.

245 (assimilation rate, stomatal conductance and transpiration) were measured from 4-yr old A. glutinosa

246 possibility of producing plants with reduced transpiration which have increased drought tolerance, wi

247 We investigated the relationship between transpiration, which can be down-regulated by abscisic a

248 We combined measurements of sap flux-scaled transpiration with measurements of tree allometry and de

249 and root water conductance, and whole-plant transpiration, with minor effects on plant development.

250 hytes plays little role in the regulation of transpiration, with stomata passively responsive to leaf

251 nd higher integrated WUE by reducing daytime transpiration without a demonstrable reduction in biomas