ライフサイエンスコーパス: transpiration

1 ke for photosynthesis and water loss through transpiration.

2 slowly when the shoot was covered to prevent transpiration.

3 leaf for photosynthesis with water loss via transpiration.

4 l homeostasis, stomatal dynamics, and foliar transpiration.

5 2ca mutants displayed a phenotype of reduced transpiration.

6 photosynthesis as well as water loss through transpiration.

7 mediate acclimation responses and to reduce transpiration.

8 ulics, whether by diffusion or mass flow via transpiration.

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

10 eric CO2 influences plant photosynthesis and transpiration.

11 s, including stomata, the organs controlling transpiration.

12 which vascular land plants regulate daytime transpiration.

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

14 plies parts of soil water recharge and plant transpiration.

15 the stem water content and sustain nocturnal transpiration.

16 t with decreases in stomatal conductance and transpiration.

17 CO(2) availability with suppressed stomatal transpiration.

18 a strict physiological regulation of forest transpiration.

19 to maximize photosynthesis while minimizing transpiration.

20 lic conductance partly counteracted those of transpiration.

21 e accompanied by mild reductions in g(c) and transpiration.

22 s, while stomata facilitate gas exchange and transpiration.

23 o changes in stomatal density that influence transpiration.

24 es to the atmosphere through evaporation and transpiration.

25 ng a watershed-scale fertilization effect on transpiration.

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

27 ke for photosynthesis and water loss through transpiration.

28 uard cells regulate plant photosynthesis and transpiration.

29 caused by lack of AtrbohF is dependent upon transpiration.

30 edistributes wax composition, and suppresses transpiration.

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

32 logical forcing as a result of reduced plant transpiration.

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

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

35 assimilation while minimizing water loss via transpiration.

36 tosynthesis and restricting water efflux via transpiration.

37 ing the trade-off between photosynthesis and transpiration.

38 as compared with the wild type due to higher transpiration.

39 herefore, gatekeepers for photosynthesis and transpiration.

40 ritical for modulation of CO(2) fixation and transpiration.

41 sed with increasing xylem [(13) CO(2) *] and transpiration.

42 CO(2) that is assimilated, vs simply lost to transpiration.

43 es stomatal closure to prevent water loss by transpiration.

44 sis and by reducing stomatal conductance and transpiration.

45 Species that caused an increase in leaf transpiration (+182%), thus cooling the leaf, had a lowe

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

47 thermal limit than those that decreased leaf transpiration (-75%), causing the leaf to warm up.

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

49 lated to a larger extent than predicted from transpiration alone, and we suggest the possibility that

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

51 is developed to reveal two distinct modes of transpiration: an evaporation-limited regime and a flow-

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

53 ted CO(2) increased with increasing rates of transpiration and [(13) CO(2) *]; however, rates of (13)

54 reduced with little grass/forb cover, while transpiration and annual productivity increase.

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

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

57 ircadian clock contributes to the control of transpiration and biomass accumulation.

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

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

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

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

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

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

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

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

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

67 ic limitation as an additional constraint to transpiration and evaluate its impacts on stomatal optim

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

69 Transpiration and evapotranspiration show spatially simi

70 operties and composition affect tomato fruit transpiration and firmness and are influenced by environ

71 lationship between fruit cuticle properties, transpiration and firmness, and provides insights into t

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

73 Transpiration and gas exchange occur through stomata.

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

75 ter and nitrogen growing field conditions on transpiration and how this effect influenced the perform

76 genetic screen for mutants with altered leaf transpiration and identified an uncharacterized protein,

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

78 oisture decreases both evaporation and plant transpiration and increases local temperature.

79 results demonstrate the relationship between transpiration and leaf delta(13) C in the field and the

80 a play a critical role in photosynthesis and transpiration and overall plant productivity.

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

82 Variation in K(S) has implications for plant transpiration and photosynthesis, growth and survival, a

83 for water vapor and gas exchange involved in transpiration and photosynthesis, the apoplast also accu

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

85 itatively linked to the partitioning between transpiration and soil evaporation (R(2) = 0.43).

86 Decreasing transpiration and soil moisture are associated with decr

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

88 ng significantly reduced CO(2) assimilation, transpiration and stomatal conductance, but did not affe

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

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

91 Recalibration of the transpiration and volatilisation parameters improved the

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

93 elevated abscisic acid levels, reduced host transpiration and water loss, enhanced spread of bacteri

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

95 quantities link carbon (C) assimilation with transpiration, and along with photosynthetic capacities

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

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

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

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

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

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

102 ke for photosynthesis and water loss through transpiration, and therefore play a key role in plant pr

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

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

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

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

107 onse of gross primary productivity (GPP) and transpiration at the global scale.

108 array of large diameter conduits, to enable transpiration at the same macroscopic scale as natural t

109 timate that the contribution by FU to annual transpiration at this site has a median value of 8.2% (1

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

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

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

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

114 the intracuticular wax was important for the transpiration barrier.

115 r waxes contributed equally to the cuticular transpiration barrier.

116 Furthermore, we tested a simple transpiration-based accumulation model and found that tr

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

118 Control of transpiration became possible through the development of

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

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

121 ratio of cost factors for carboxylation and transpiration (beta) expected from the theory to explain

122 13) C(leaf) were found and co-localized with transpiration, biomass accumulation, and WUE(plant) .

123 elta(2)H was not only affected by changes in transpiration but also by photosynthetic reactions, prob

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

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

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

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

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

129 odel plants show that partial restriction of transpiration can occur without a reduction in CO(2) upt

130 th high photosynthetic capacity require high transpiration capacity.

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

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

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

134 The transpiration cycle in trees is powered by a negative wa

135 Synthetic trees can mimic this transpiration cycle, but have been confined to pumping w

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

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

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

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

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

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

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

143 Specifically, p-ath773 shows how transpiration drives water flow through the plant and ho

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

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

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

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

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

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

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

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

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

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

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

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

156 Both had higher transpiration efficiency because of their lower stomatal

157 C and reveal its usefulness as a measure of transpiration efficiency under well-watered conditions r

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

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

160 Without needing to maintain high rates of transpiration, flowers rely on other hydraulic traits, s

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

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

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

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

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

166 Transpiration from the Amazon rainforest generates an es

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

168 ssing ABA sensitivity, which then aggravates transpiration further.

169 , which in turn affect genotypic rankings of transpiration in a time-dependent manner.

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

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

172 ial role in leaf function, controlling water transpiration in response to environmental stresses and

173 revealed that 37% of these species increased transpiration in the absence of increased carbon uptake.

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

175 therefore be used to "pay" for some morning transpiration in the dry season.

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

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

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

179 atal conductance declines under high VPD and transpiration increases in most species up until a given

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

181 d the consequences of these changes in plant transpiration induced by plant-insect feedbacks for spec

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

183 tion-based accumulation model and found that transpiration is a strong predictor for accumulation of

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

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

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

187 Stomatal control of transpiration is critical for maintaining important proc

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

189 tional contribution to the total terrestrial transpiration is limited.

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

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

192 as the loss of water through evaporation and transpiration is the most important factor in predicting

193 ribution of mineral nutrients to TB with low transpiration is unknown.

194 hotosynthesis per unit of water lost through transpiration) is a tracer of the plant physiological co

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

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

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

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

199 s, and showed lower stomatal conductance and transpiration, narrower xylem vessels, smaller leaves an

200 All four hypotheses assume that finite transpiration occurs, providing a further constraint on

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

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

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

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

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

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

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

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

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

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

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

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

213 asing salinity, the model captures different transpiration patterns observed in halophytes (nonmonoto

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

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

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

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

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

219 %), stomatal conductance (g(s) , +7.5%), and transpiration rate (E, +10.5%).

220 Reductions in transpiration rate (TR) and leaf area were greatest with

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

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

223 y temperature (CT) is an indirect measure of transpiration rate and stomatal conductance and may be v

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

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

226 Transpiration rate in abi1 increased linearly with VPD,

227 hile reducing cuticle permeability and fruit transpiration rate in AC and M82, but not in dfd fruit.

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

229 d type showed a steady or slightly declining transpiration rate up to VPD of nearly 7 kPa, and fully

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

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

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

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

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

235 vars and shading for photosynthetic rate and transpiration rate.

236 r pressure before the precipitous decline in transpiration rate.

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

238 trees emit soil gases during the night when transpiration rates are negligible, suggesting that axia

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

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

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

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

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

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

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

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

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

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

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

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

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

252 te genes with biological function related to transpiration, root development, and signal transduction

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

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

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

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

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

258 , however, a fundamental error was made: the transpiration stream consists of resistances in series (

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

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

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

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

263 applicable methods for estimating ecosystem transpiration (T) from eddy covariance (EC) data across

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

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

266 (4-h period) and resultant modulating plant transpiration, the SWaP enables quantification of the co

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

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

269 plates levitate due to light-induced thermal transpiration through microchannels within the plates, e

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

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

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

273 Nonstomatal water loss by transpiration through the hydrophobic cuticle is ubiquit

274 (10-200 Pa), the increased speed of thermal transpiration through the plate's channels creates an ai

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

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

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

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

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

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

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

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

283 Reduced transpiration upon seawater exposure may contribute to c

284 Lower transpiration was associated with higher STOMATAL DENSIT

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

286 Above this, sharply declining transpiration was followed by leaf death.

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

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

289 The dominance of transpiration water fluxes in continental evapotranspira

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

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

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

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

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

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

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

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

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

299 Strategies for reducing transpiration without incurring a cost for photosynthesi

300 whole-plant water use efficiency (yield per transpiration; WUE(plant) ) in any crop-breeding program