ライフサイエンスコーパス: arid

1 d marine aerosols to 5 ppm sulfur dioxide at arid (23 +/- 1% relative humidity, RH) and marine (98 +/

2 and Opuntia, for biomass production on semi-arid, abandoned, marginal, or degraded agricultural land

3 s did increases in the relative abundance of arid-adapted bovids, and in bovid body mass.

4 biota, however, it remains paradigmatic that arid-adapted species contracted to refugia at GM.

5 r than glaciation, it could be expected that arid-adapted species might have had expanded ranges at G

6 y shape current species richness of Africa's arid-adapted taxa.

7 The gum arabic tree (Acacia senegal) is an arid-adapted, morphologically diverse species native to

8 ns in Hwange National Park, Zimbabwe, a semi-arid African savanna structured by artificial waterholes

9 nd climate change in arid Central Asia, cold arid alpine QTP, and mesophytic East Asia.

10 able of growth under extremely oligotrophic, arid and cold conditions.

11 bration in desiccated versus humid contexts, arid and cold ecologies should be less amenable, when co

12 e that the 21st century will be increasingly arid and droughts more severe and prolonged.

13 Metagenomic analyses of hyper-arid and extreme hyper-arid soils in this desert reveale

14 Arid and humid biomes are both affected by drought, and

15 reeding bird and small mammal communities in arid and mesic grasslands changed in response to increas

16 ibes and is distributed predominantly across arid and montane regions of Asia.

17 we demonstrate that internal deletion of the ARID and PHD1 domains has a negligible effect on in vitr

18 conditions, by contrast, are cold, extremely arid and seemingly inhospitable.

19 The arid and semi-arid drylands of the world are increasingl

20 Many arid and semi-arid landscapes around the world are affec

21 dy points out that intensive cropping in the arid and semi-arid regions leads to an increase in both

22 ple food for more than 90 million farmers in arid and semi-arid regions of sub-Saharan Africa, India

23 icant changes are occurring in the extensive arid and semi-arid regions, and we suggest that the repo

24 The management of water resources in arid and semiarid areas has long been a challenge, from

25 survival of genomes of N2FP, particularly in arid and semiarid climates.

26 storical adaptation of sorghum production to arid and semiarid conditions has provided promise regard

27 bon sequestration, although the responses of arid and semiarid ecosystems may be highly variable.

28 2 uptake using eddy-covariance techniques in arid and semiarid ecosystems.

29 ow water and N availability influence ECE in arid and semiarid grasslands is still uncertain.

30 Water drives the functioning of Earth's arid and semiarid lands.

31 anza, and Coast provinces, as well as remote arid and semiarid regions and refugee camps.

32 tivars that must be widespread cultivated in arid and semiarid regions as KSA accompanying with estab

33 Sustainably managing and using water in arid and semiarid regions such as the southwestern Unite

34 sal of modern humans required the transit of arid and semiarid regions where the distribution of pota

35 As a primary limiting factor in arid and semiarid regions, precipitation strongly influe

36 itation in regulating ecosystem C cycling in arid and semiarid regions.

37 otential mechanisms of abiotic CO2 uptake in arid and semiarid soils: atmospheric pressure pumping, c

38 d of the Pliocene, did the broad patterns of arid and semiarid subtropical regions become fully devel

39 rtage, through either increased WUE or ci in arid and wet environments, respectively.

40 the majority of C4 plants occupy disturbed, arid, and nutrient-poor habitats, some grow in high-nutr

41 the existing repertoire of genes involved in ARID, and provide new insights into the molecular mechan

42 arim River is the longest inland river at an arid area in China.

43 sed as storage for paraphernalia in the semi-arid area of the Judean desert and the dry conditions pr

44 tainable management of water resources in an arid area.

45 sensitive to increased precipitation in more arid areas and more responsive to decreased precipitatio

46 cles (salt rocks) collected in several hyper-arid areas of the desert.

47 ity of the final product, especially in semi-arid areas where irrigation water is scarce and/or of lo

48 est increases in Rs and Q10 were observed in arid areas, and the stimulation rates decreased with inc

49 In arid areas, people living in the proximity of irrigation

50 y increased nocturnal flight activity in the arid aseasonal ecosystem, but not in the mesic seasonal

51 D4A and ARID4B are homologous members of the ARID (AT-rich interaction domain) gene family.

52 The wild relatives are endemic to the hot, arid Australian savannah.

53 arison Project Phase 5 (CMIP5) models to the arid basin (the Tarim River Basin, TRB) and humid basin

54 By setting WDI to the highest value in (semi)arid basins, absolute freshwater shortage is taken into

55 igher turnover rates of carbon pools in semi-arid biomes are an increasingly important driver of glob

56 We found that arid biomes respond to drought at short time-scales; tha

57 eficits, but they lack the rapid response of arid biomes to drought.

58 anisms likely differ from those operating in arid biomes, as plants usually have a poor adaptability

59 ction model for Australia's dry woodland and arid biota.

60 articipating in a case-control study in Semi-Arid Brazil, we identified key differences with potentia

61 N and P cycling and storage in semiarid and arid, but not in humid and dry-subhumid, environments.

62 nts, invertebrates and vertebrates in a semi-arid California grassland.

63 floristics, vegetation and climate change in arid Central Asia, cold arid alpine QTP, and mesophytic

64 UHI is 0.7+/-0.3 K (mean+/-1 s.e.) for semi-arid cities, which is stronger than that in the humid cl

65 mainly had humid to subhumid summers and no arid climate has been conclusively detected, indicating

66 cement of the equatorward MED margins by the arid climate type.

67 e climate of Laurasia, but distinct from the arid climate zone that covered extensive areas of Gondwa

68 ver the claimed amount of liquid water in an arid climate.

69 s equatorial regions require a predominantly arid climate.

70 ures for high levels of CA may be limited to arid climates where stomatal closure reduces CO2 availab

71 ific populations originating from relatively arid climates will be better adapted to cope with the ex

72 P in nitrogen per leaf area (Narea), even in arid climates, despite diazotrophy being sensitive to dr

73 cultivation was not economically feasible in arid climates.

74 worldwide at interfaces between semiarid and arid climates.

75 s (CFs) for a groundwater-fed wetland at the arid coast of Peru are developed for groundwater and sur

76 y effloresce, even when exposed to extremely arid conditions (<1% RH).

77 ies' vulnerability in Kenya, as well as more arid conditions and larger amounts of water consumed.

78 its of central China support the presence of arid conditions and modern atmospheric pathways for the

79 f tree genotypes that will thrive under more arid conditions has grown.

80 The convergence of prolonged warming and arid conditions suggests the mid-12th century may serve

81 edicted to increase productivity in warm and arid conditions.

82 d substantially increase crop yields in hot, arid conditions.

83 t confers higher productivity under warm and arid conditions.

84 ly reported from C4 plants that grow in more arid conditions.

85 ecies typify hot, sunny environments only in arid conditions; small leaves are also found in high lat

86 e, well-watered routes into the semiarid and arid continental interior were available throughout the

87 d driest deserts in the world, and its hyper-arid core is described as 'the most barren region imagin

88 els revealed that time-limited dispersal via arid corridors is a key predictor to explain macro-scale

89 y 1.5 to 147 times, particularly in the more arid countries of Turkmenistan and Uzbekistan.

90 amendments enhances PIC accumulation in the arid cropland of northwestern China.

91 om a warmer, wetter early state to the cold, arid current state.

92 ry roles of ICP0 and E2FBP1 are linked in an ARID-dependent fashion.

93 g winter and post-monsoon, especially in the arid desert and warm-temperate grasslands, the DTR decre

94 The C3 plant Rhazya stricta is native to arid desert environment zones, where it experiences dail

95 Further, arid deserts and warm-temperate grasslands exhibit negat

96 abit water-limited environments such as semi-arid deserts or seasonally dry forests.

97 is believed to grow as a soil saprophyte in arid deserts.

98 chromatin-remodeling complex incorporates an ARID DNA binding domain-containing subunit.

99 re is an atypical insertion of a DNA-binding ARID domain and a histone-binding PHD domain into the Ju

100 We found that the JumonjiC (JmjC) and ARID domain-containing histone lysine demethylase 1a (JA

101 ctly regulates THBS1 promoter activity in an ARID domain-dependent manner.

102 Depletion of ARID domain-dependent, BAF-A associations at THROMBOSPON

103 The arid and semi-arid drylands of the world are increasingly recognized f

104 ggested broadening the definition to include arid, "Dune" planets on the inner edge and planets with

105 drier environments as Australia became more arid during the late Cenozoic.

106 is paper, we examined the response of a semi-arid ecological community to a fivefold change in precip

107 ic pathway not only enables the balancing of arid ecosystem nitrogen budgets, but also changes our vi

108 st that natural coherent variability in semi-arid ecosystem productivity responded to ENSO in opposit

109 ay imply potential prediction of global semi-arid ecosystem variability, particularly based on variab

110 elevated [CO2] on plant communities in this arid ecosystem.

111 The linkages between dynamics of semi-arid ecosystems and climate at the hemispheric scale how

112 Semi-arid ecosystems are key contributors to the global carbo

113 Recent evidence shows that warm semi-arid ecosystems are playing a disproportionate role in t

114 Recent evidence shows that warm semi-arid ecosystems are playing a disproportionate role in t

115 a global hot spot for variability, with semi-arid ecosystems in that country exhibiting increased car

116 Avian communities of arid ecosystems may be particularly vulnerable to global

117 hibits stronger and faster responses of semi-arid ecosystems to ENSO than the Northern Hemisphere.

118 ariability of the sink are dominated by semi-arid ecosystems whose carbon balance is strongly associa

119 lobal carbon fluxes may be dominated by semi-arid ecosystems, but the underlying mechanisms of this h

120 In semi-arid ecosystems, herbivore distribution is generally mor

121 In arid ecosystems, herbivore presence tended to reduce mic

122 In many arid ecosystems, however, termite nests impart substrate

123 e the impacts of ENSO on variability of semi-arid ecosystems, using the Ensemble Empirical Mode Decom

124 dge of anthrax ecology is largely limited to arid ecosystems, where outbreaks are most commonly repor

125 water across a temperature range typical of arid ecosystems.

126 cooler months in moderately hot (China) and arid (Egypt) regions.

127 There is an increased risk of extremely arid environment and large deserts developed progressive

128 The long-term exposure of vegetation to this arid environment has favoured a resilient flora capable

129 goats and sheep that are indigenous to a hot arid environment in Egypt's Coastal Zone of the Western

130 orthern Africa) evolved from a predominantly arid environment with high-frequency variability to gene

131 fically for homeostasis-related genes in the arid environment-adapted saker.

132 of evolving in a low nutrient and seasonally arid environment.

133 Comparison with C3 trees from arid environments (Pinus longaeva and Pinus edulis in th

134 Desert wetlands are keystone ecosystems in arid environments and are preserved in the geologic reco

135 A global expansion of arid environments during this time could have provided n

136 Our observations reveal that eucalypts in arid environments have thick amphistomatous leaves with

137 ts differing responses based on environment; arid environments in New Mexico see increased intrinsic

138 d angiosperms, we hypothesize that plants in arid environments may reduce dx:dy below unity owing to

139 Venice Lagoon to unvegetated systems in the arid environments of the Gulf of California and Yemen.

140 support conditions similar to what occurs in arid environments on Earth.

141 ted to be substantial for species inhabiting arid environments which incur large variations in daily

142 30 years) that is adapted to survive in semi-arid environments with varying levels of parasite exposu

143 exacerbate plant water stress in marginally arid environments, providing preadapted succulent plants

144 species' ecologies, including adaptation to arid environments, reproductive output and maternal body

145 ctly influenced traits for adaptation to hot arid environments, such as thermo-tolerance (melanogenes

146 athway, which permits CAM plants to adapt to arid environments.

147 choice for CTBTO on-site inspections even in arid environments.

148 ter photosynthetic performance than C3/C4 in arid environments.

149 patobiliary tumorigenesis, including that of ARID family proteins, which have recently been reported

150 , a DNA-binding A/T-rich interaction domain (ARID) family transcription factor, is expressed ubiquito

151 e (Oryza sativa) AT-rich Interaction Domain (ARID) family, is required for SAM development.

152 eases to nematode communities at all but the arid grassland ecosystem; mites showed no responses at a

153 nder eCO(2) and warming treatments in a semi-arid grassland field experiment.

154 Here we show in a semi-arid grassland that elevated CO(2) can completely revers

155 influence invasive species success in a semi-arid grassland, as a result of both direct and water-med

156 During a 7-year experiment in a semi-arid grassland, the response of plant biomass to eCO2 an

157 ons on a water-availability gradient in semi-arid grassland.

158 individual ecosystem types (mesic, xeric and arid grasslands and a polar desert) located in the weste

159 hed world, both SWC and productivity in semi-arid grasslands may be higher than previously expected.

160 continent-specific environmental conditions (arid grasslands versus ash-laden forests) triggered conv

161 Vegetation gap patterns in arid grasslands, such as the "fairy circles" of Namibia,

162 The now arid Great Basin of western North America hosted expansi

163 The arid-grown species Setaria italica (C4) and Brachypodium

164 esting their adaptive radiation into a novel arid habitat.

165 urnover indicative of more open and probably arid habitats than those reconstructed earlier in this r

166 s colonized the region and when they invaded arid habitats within the region (typically 4-14 million

167 h America, where it has evolved to thrive in arid habitats.

168 Succulent plants dominate certain semi-arid habitats.

169 o date, dark pigmentation is associated with arid habitats; however, in D. americana, the darkest fli

170 mutations that cause autosomal recessive ID (ARID) has lagged behind, predominantly due to non-availa

171 old over a wide range of climate conditions (arid-humid) and limiting factors (soil moisture, leaf ar

172 thigenic calcite indicate a centennial-scale arid interval between 500 CE and 1150 CE, overlaid on a

173 biotic Acacia ants) animal species in a semi-arid Kenyan savanna.

174 , a replicated set of LMH exclosures in semi-arid Kenyan savanna.

175 of desert grasses, and provide insight into arid land carbon flow.

176 ing reads from the rhizospheres (RHZ) of two arid land grasses.

177 nobacterium Microcoleus vaginatusis found in arid land soils worldwide.

178 phosphorus-SRP) along a approximately 300-km arid-land river (Rio Grande, NM) and generated nutrient

179 ose strategies for closing nutrient loops in arid-land rivers.

180 In arid lands, plant productivity is limited by water and N

181 SIC) exceeds organic carbon (SOC) greatly in arid lands, thus may be important for carbon sequestrati

182 h anthropogenic pressures on biodiversity in arid lands.

183 major component of biological soil crusts in arid lands.

184 e of shrubs has increased throughout Earth's arid lands.

185 nexplained high rates of litter mass loss in arid lands; however, the global significance of this pro

186 tal to the development of human societies in arid landscapes and for long-distance trade across hosti

187 Many arid and semi-arid landscapes around the world are affected by a shift

188 conditions for crop species in semiarid and arid landscapes.

189 The climate shifted from the cold, arid Last Glacial Maximum to the warm, mesic Holocene in

190 slow constant dripping, in a temperate semi-arid location (Wellington, NSW, Australia), exhibit drip

191 Africa and South America, which represent an arid, lower-latitude biome.

192 enologically distinct invasive plant in semi-arid mixed-grass prairie.

193 differed substantially from the cold, hyper-arid modern environment to permit aqueous flows across s

194 ert of northern Chile is the oldest and most arid nonpolar environment on Earth.

195 s of soil crust microbial communities across arid North America, we observed a latitudinal replacemen

196 However, the arid north and northwest regions have much larger water

197 ion had a considerable influence in relative arid north China.

198 ionship emerged with hunter-gatherers in the arid north, while the more intensive, later one evolved

199 t mangroves and halophyte scrubs in Mexico's arid northwest, with less than 1% of the terrestrial are

200 sotope data from a passive-tectonic and semi-arid ocean margin (South Africa), which reveals a smalle

201 inant mechanism of toxic metal dispersion in arid or semiarid landscapes.

202 f the land area subjected to this warming is arid or semiarid with ecosystems that are highly vulnera

203 Results indicate that Caragana is of arid origin from the Junggar steppe.

204 define and track these transitions in other arid parts of the world subjected to similar tradeoffs.

205 However, by 1050 CE, this extended arid period, possibly combined with regional political c

206 ion and its abandonment occurred during this arid period.

207 Valley and adjacent desert drainages of the arid Peruvian coast.

208 r elevated [CO2], but the response of intact arid plant communities to elevated [CO2 ] is largely unk

209 Antarctic Dry Valleys are locked in a hyper-arid, polar climate that enables the East Antarctic Ice

210 inverted karyotype present in northern, more arid populations and an almost complete absence of the i

211 chemical weathering is preserved, indicating arid, possibly cold, paleoclimates and rapid erosion and

212 colorectal cancer cells lacking one or both ARID proteins.

213 yrah grape by-products, produced in the semi-arid region in Brazil, was optimized by a Central Compos

214 auAERONET) for the years 2009-2012 over semi-arid region Jaipur, northwestern India.

215 hece (Rhodophyta) in a small river in a semi-arid region of south-east Spain it became clear that mos

216 for dry years and to >150% for wet years in arid regions (MAP<500 mm).

217 inhibitory activities of honeys produced in arid regions and compare them with well-recognized honey

218 roportion of nocturnal species is highest in arid regions and lowest at extreme high altitudes.

219 the production of solar thermochemical fuels arid regions are best-suited, and for biofuels regions o

220 Many arid regions are introducing regulations disallowing dum

221 showed that one or more types of honey from arid regions contained higher levels of phenolic compoun

222 We show that semi-arid regions contribute to 57% of the detrended IAV of g

223 ed to evaluate the quality of 11 honeys from arid regions for first time, and compare it with 5 diffe

224 More arid regions from 5-20 degrees N preserve procolophonid-

225 may be due to the fact that plant species of arid regions have mechanisms allowing them to rapidly ad

226 This higher GPP IAV in semi-arid regions is co-limited by supply (precipitation)-ind

227 that intensive cropping in the arid and semi-arid regions leads to an increase in both SOC and PIC.

228 s of Agave, which are native to semiarid and arid regions of Central and North America and are emergi

229 ndemic to the southwestern United States and arid regions of Central and South America.

230 ore than 90 million farmers in arid and semi-arid regions of sub-Saharan Africa, India and South Asia

231 rbia (plants) and Liolaemus (animal) invaded arid regions of the Atacama-Sechura Desert in the last 1

232 ) are the most significant perennial crop in arid regions of the Middle East and North Africa.

233 to anthropogenic climate change in the semi-arid regions of the southwestern United States (US) is a

234 gation is becoming increasingly prevalent in arid regions of the world, due to growing demand and dec

235 r results demonstrate the importance of semi-arid regions to the global terrestrial carbon cycle and

236 d water use in seasonally dry, semiarid, and arid regions where precipitation and evapotranspiration

237 tence in wastewater treatment, especially in arid regions where treated municipal wastewater is exten

238 nd early-domesticated dromedary samples from arid regions with nuclear microsatellite and mitochondri

239 which are widely distributed in semiarid to arid regions worldwide.

240 turnover of dead organic matter in soils of arid regions), reduce human exposure to mycotoxins in bu

241 are occurring in the extensive arid and semi-arid regions, and we suggest that the reported increased

242 lmost exclusively on sources in low-latitude arid regions, but here we show that there are substantia

243 Since jatropha oil is nonedible and grows in arid regions, JME may help to avoid conflicts with the f

244 cause attractive production locations are in arid regions, the water footprint and the land requireme

245 Although few species extend into arid regions, those that do occupy larger ranges and thu

246 e the atmospheric lifetime of oxalic acid in arid regions, where its removal via wet deposition is in

247 Especially in arid regions, where scarcity is high, these models provi

248 s most clearly in the observations over semi-arid regions, where surface fluxes are sensitive to soil

249 es in contributing to budgets of GHGs in the arid regions, whereas their global importance would be e

250 ta) is a legume species widely grown in semi-arid regions, which has high potential to provide stable

251 re them with well-recognized honeys from non-arid regions.

252 compare it with 5 different honeys from non-arid regions.

253 predict faster carbon turnover in many semi-arid regions.

254 compared with the evaluated honeys from non-arid regions.

255 i is thought to be mineral dust aerosol from arid regions.

256 being a minor component of dust emitted from arid regions.

257 d and ecosystems, especially in semiarid and arid regions.

258 come a critical problem in many semiarid and arid regions.

259 tween supply and demand for potable water in arid regions.

260 ergy harvesting and passive refrigeration in arid regions.

261 and hematite showed increased solubility at arid RH, but no difference (p > 0.05) was observed betwe

262 CO2 on the cyanobacteria in biocrusts of an arid shrubland were examined at a large manipulated expe

263 st, tree plantations increased SOC stocks in arid sites but decreased them in humid ones.

264 stressful mesic areas than in more stressful arid sites.

265 mic analyses of hyper-arid and extreme hyper-arid soils in this desert revealed a remarkable degree o

266 with AOB higher in the more weathered, semi-arid soils of Western Australia.

267 In general, arid soils show the richest observed biosynthetic divers

268 nobacteria typically colonize the surface of arid soils, building biological soil crust (biocrusts) t

269 ame mechanisms control CH4 oxidation in more arid soils.

270 the coastal Northwest, and is less so in the arid Southwest.

271 unt and distribution of precipitation in the arid southwestern United States.

272 ce consequences as large regions become more arid, starting with water-limited, low-productivity gras

273 e trade-offs as soils transition toward more arid states is, therefore, critical to estimating global

274 Our results showed that the semi-arid steppe in north China was resistant to both daytime

275 rom regions with relatively cool winters and arid summers may be most adapted to cope with drought co

276 In the arid system, grassland and shrubland plant and breeding

277 with elevated oxidative enzyme activities in arid systems have not been well characterized.

278 widely promoted potential energy source from arid systems.

279 the century to millennial timescales in the arid to semiarid areas of the Middle East.

280 for sedentary and nomad populations in these arid to semiarid landscapes is understood, but the mille

281 d zones, indicating that climate change from arid to temperate dominance may have set the stage for t

282 polar North Atlantic Islands and four in the arid-to-semiarid deserts of the US Southwest.

283 sizes support a model of GM expansion in the arid-tolerant Grey Butcherbird that resulted in secondar

284 uction into environments once considered too arid, too variable, and too harsh to cultivate.

285 A warm season crop originating from the semi-arid tropics, sorghum is relatively susceptible to both

286 rior ganglion where it collaborates with the ARID-type transcription factor cfi-1 to determine the ch

287 mations of NO3- during storms from 10 nested arid urban watersheds that varied in stormwater infrastr

288 on sink anomaly was driven by growth of semi-arid vegetation in the Southern Hemisphere, with almost

289 We show that the responses of semi-arid vegetation to ENSO occur in opposite directions, re

290 -term changes in atmospheric wet deposition (arid vs humid periods).

291 Air temperatures in the arid western United States are predicted to increase ove

292 ave suffered declines and extinctions in the arid zone coincident with Aboriginal depopulation.

293 a highly cooperative bird of the Australian arid zone.

294 are biologically relevant and widespread in arid-zone anurans.

295 How arid-zone birds will be affected by rapid increases in a

296 ily activity, and geographic distribution of arid-zone birds.

297 water-fed wetlands generally occur in hyper-arid zones and smallest in humid zones, highlighting the

298 Previous studies in arid zones have demonstrated functional importance of th

299 a prominent feature among plants adapted to arid zones, but we know little about how succulence evol

300 stralia largely resulted in the expansion of arid zones, rather than glaciation, it could be expected