ライフサイエンスコーパス: arid

1 by targeting the AT-rich interacting domain (ARID)-3B complex.

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

3 as male-driven, suggesting that selection of arid-adapted zebu bulls enhanced herd survival.

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

5 eas, through 1.6% (9.9 trees per hectare) in arid and 5.6% (30.1 trees per hectare) in semi-arid zone

6 pacts on agricultural sustainability in semi-arid and arid climates.

7 the occupancy of epiphytic, epilithic, semi-arid and arid environments.

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

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

10 Within semi-arid and mesic grassland ecosystems, PPT gradient experi

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

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

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

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

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

16 Our findings indicate that arid and semi-arid ecosystems may not be sensitive to CO

17 ts but had variable effects on herb roots in arid and semi-arid ecosystems.

18 change factors control soil C persistence in arid and semi-arid grasslands.

19 Scarcity of fresh water in arid and semi-arid regions means that we must use more s

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

21 rtant fruit bearing tree grown widely in the arid and semi-arid regions of the world.

22 ce soil fertility and crop production in the arid and semi-arid regions stressed with water scarcity

23 ter salinization has been identified in many arid and semi-arid regions where groundwater is increasi

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

25 Being cultivated in arid and semi-arid regions, the crop often encounters in

26 hance terrestrial carbon sink, especially in arid and semi-arid regions.

27 s (P) deficiency, remains a challenge in the arid and semi-arid regions.

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

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

30 2 uptake using eddy-covariance techniques in arid and semiarid ecosystems.

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

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

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

34 is problem limits the water supply in inland arid and semiarid regions.

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

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

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

38 In semi-arid and temperate grasslands, ecosystem respiration (Re

39 entrated in rural rainfed systems throughout arid and temperate land across Eurasia, Africa and North

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

41 pattern of deteriorating environments (cool, arid, and anoxic conditions) and climate fluctuations ac

42 uced conversions among sub-humid, semi-arid, arid, and hyper-arid subtypes will lead to substantial c

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

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

45 frequently aseasonal, such as the tropical, arid, and semi-arid ecosystems that cover vast areas.

46 omogenization between the populations of the arid Andes is not only due to migrations during the Inca

47 f positive natural selection in the high and arid Andes vs. the low Amazon tropical forest: in the An

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

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

50 tainable management of water resources in an arid area.

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

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

53 n the mechanism of runoff generation in semi-arid areas while further experiments should be undertake

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

55 s from 0.1% (0.7 trees per hectare) in hyper-arid areas, through 1.6% (9.9 trees per hectare) in arid

56 te-induced conversions among sub-humid, semi-arid, arid, and hyper-arid subtypes will lead to substan

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

58 spora strains isolated from an extreme hyper arid Atacama Desert soil were determined.

59 tal conditions that prevail in extreme hyper-arid Atacama Desert soils.

60 Semi-arid Australia has a highly variable rainfall pattern, m

61 t the dynamic carbon-water relations in semi-arid Australian ecosystems.

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

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

64 ectives that are improving forecasts of semi-arid biome shifts.

65 tives will rapidly improve forecasts of semi-arid biome shifts.

66 imated tree restoration potential across all arid biomes by 33%-45% (316-440 Mha).

67 tree restoration potential across a third of arid biomes by between 7% and 20% (55-166 million hectar

68 s, however, emphasized dryland regions, with arid biomes making up 36%-42% of potential restoration a

69 rupt shifts in forest carbon capture in semi-arid biomes remain poorly understood.

70 with mycorrhizal fungi)-are most abundant in arid biomes with alkaline soils and high maximum tempera

71 South America (2,025 inventories from wet to arid biomes), and a new, large-scale phylogenetic hypoth

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

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

74 in total profile SOC within a 1.8 km(2) semi-arid catchment in Idaho, U.S.A. can be explained as a fu

75 as sampled in 188 farm tubewells in the semi-arid catchment of Berambadi and in 5 piezometers in the

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

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

78 High ocean water alkalinity due to an arid climate and low fluvial runoff therefore seems to b

79 developing Li brines with the combination of arid climate and the presence of landlocked extensional

80 hill slope scale as well as in arid or semi-arid climate conditions remain unclear.

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

82 areas with humid climate was higher than the arid climate.

83 fering in phenology, plants originating from arid climates bolted up to 48 d earlier than plants from

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

85 waves threaten agricultural productivity in arid climates, our findings will facilitate identificati

86 agricultural sustainability in semi-arid and arid climates.

87 cultivation was not economically feasible in arid climates.

88 s and unpredictable precipitation regimes in arid climates.

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

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

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

92 ndicate that these sediments developed under arid conditions in which high marine alkalinity favoured

93 The onset of warmer, more arid conditions likely contributed to the extinction of

94 can domesticates into northern Mexico, where arid conditions promote PD.

95 antibiotic resistance and virulence in more arid conditions suggests reduced intensity of biotic int

96 In terms of specific functions, more extreme arid conditions were also associated with increased rela

97 es that the secretion does not dry out under arid conditions, not melt at 50 degrees C, and not chang

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

99 edicted to increase productivity in warm and arid conditions.

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

101 t source of groundwater salinization in semi-arid context, and stress that identifying dominant drive

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

103 f endorheic lakes and wetlands when crossing arid continental interiors.

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

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

106 eficial and pathogenic fungi in increasingly arid crop soils and, secondly, through promotion of phos

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

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

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

110 icrobial communities are ubiquitous in hyper-arid deserts around the world and the last resort for li

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

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

113 l forests, montane grasslands and tundra) or arid (e.g., deserts) landscapes.

114 nity of large mammalian herbivores in a semi-arid East African savanna.

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

116 in cultivated bacteria isolated from hot and arid ecological niches.

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

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

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

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

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

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

123 ncroachment in arctic, alpine, and arid/semi-arid ecosystems around the world, yet our understanding

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

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

126 Our findings indicate that arid and semi-arid ecosystems may not be sensitive to CO(2) enrichment

127 asonal, such as the tropical, arid, and semi-arid ecosystems that cover vast areas.

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

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

130 needed access to drinkable water to survive arid ecosystems, but were simultaneously constrained by

131 ers in underrepresented regions such as semi-arid ecosystems, forests in the tropics and subtropics,

132 In arid ecosystems, herbivore presence tended to reduce mic

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

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

135 primary determinant of plant growth in semi-arid ecosystems, yet it remains difficult to forecast la

136 s were larger in cold than temperate or semi-arid ecosystems.

137 iable effects on herb roots in arid and semi-arid ecosystems.

138 33-year-long dataset spanning a 1,267-m semi-arid elevational gradient in the southwestern United Sta

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

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

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

142 re influence vital rates and viability of an arid environment specialist, the Kalahari meerkat, throu

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

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

145 supports important ecosystems in this mostly arid environment.

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

147 ct a range of traits including adaptation to arid environments and defence against pathogens and toxi

148 rassulacean acid metabolism (CAM) evolved in arid environments as a water-saving alternative to C(3)

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

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

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

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

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

154 30 years) that is adapted to survive in semi-arid environments with varying levels of parasite exposu

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

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

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

158 pancy of epiphytic, epilithic, semi-arid and arid environments.

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

160 and rivers with catchments across a humid to arid gradient covering >1,800,000 km(2) of continental e

161 nges of net ecosystem productivity in a semi-arid grassland despite whether temperature, precipitatio

162 a 4 year manipulation experiment with a semi-arid grassland on China's Loess Plateau.

163 that increased winter snowfall may stabilize arid grassland systems by reducing resource competition,

164 ent-specific community composition in a semi-arid grassland under long-term simulation of six differe

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

166 similarity on community assembly in the semi-arid grassland.

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

168 historic periods of sand deposition in semi-arid grasslands and external climatic conditions, land u

169 ignificantly across cold, temperate and semi-arid grasslands, in that responses for most C fluxes wer

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

171 control soil C persistence in arid and semi-arid grasslands.

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

173 northern India, diversifying into new, more arid habitats after environmental conditions stabilized.

174 ce of these proteins in strains from hot and arid habitats was not reported previously.

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

176 ition from the wetter glacial period to more arid Holocene accompanies a surface warming of 6.2 +/- 0

177 initions of grazed livestock agroecosystems (arid, humid, and temperate), and groups of animal produc

178 climate sensitivity occurred across the semi-arid interior.

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

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

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

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

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

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 rmed by unique features of the Mediterranean arid landscape, such as the dramatic ecological contrast

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

188 Most large herbivores in arid landscapes need to drink which constrains their mov

189 were widespread and abundant throughout the arid landscapes of Central Asia and Mongolia, but have u

190 Wetlands in arid landscapes provide critical habitat for millions of

191 es positive apparent priming effects in more arid locations with low SOC contents.

192 s to develop crops resilient to increasingly arid, low nutrient soils.

193 local coast and possess limited richness in arid (< 5% moisture) and at high elevation sites, known

194 arid Rwanda, hot subhumid Ghana and hot semi-arid Mali and Benin using an ensemble of 25 maize models

195 monsoonal alluvial plains into an extremely arid margin.

196 an be propagated from tropical areas to semi-arid Mediterranean biomes through atmospheric wave train

197 cadal shifts in forest carbon uptake in semi-arid Mediterranean pine forests in Spain over 1950-2012.

198 , and, as a result of its development in the arid Middle East, the ability to thrive in a hot, dry en

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

200 spatial range covering tropical, temperate, arid, montane and coastal environments from 9.25oS to 43

201 This study was conducted in the semi-arid mountainous region of northern China in Haihe Basin

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

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

204 tant adaptation for early farmers in China's arid north, and that management practices like these lik

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

206 the plot and hill slope scale as well as in arid or semi-arid climate conditions remain unclear.

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

208 Upper Gila Mountains and South-Central Semi-arid Prairies, and decreases in the north, particularly

209 tions of the Temperate and West-Central Semi-arid Prairies.

210 colorectal cancer cells lacking one or both ARID proteins.

211 astewater irrigated soil and crops in a semi-arid region Faisalabad, Pakistan.

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

213 River Valley (SFRV) is a wine-producing semi-arid region in Brazil.

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

215 tic betaproteobacterium isolated from a semi-arid region of southern Tunisia, forms both rods and cys

216 seven cladodes of cacti native from the semi-arid region of the Brazil were investigated.

217 E, large settlements were established in the arid region of the Negev Desert, Israel, but it remains

218 ) drive(s) the grassland restoration in semi-arid region, we investigated the relationships between p

219 h the attractiveness of rivers increasing in arid regions and decreasing in humid areas.

220 Birds inhabiting hot, arid regions are among the terrestrial organisms most vu

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

222 Many arid regions are introducing regulations disallowing dum

223 hat, relative to local conventional tillage, arid regions can benefit the most from conservation agri

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

225 ent attempts to map restoration potential in arid regions have been hindered by underlying errors in

226 trend towards increasing winter snow in semi-arid regions in China.

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

228 Scarcity of fresh water in arid and semi-arid regions means that we must use more saline waters f

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

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

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

232 bution and frequency of change within highly arid regions of the continental flyway increased their v

233 dactylifera) are an important fruit crop of arid regions of the Middle East and North Africa.

234 aring tree grown widely in the arid and semi-arid regions of the world.

235 ity and crop production in the arid and semi-arid regions stressed with water scarcity and natural re

236 nix dactylifera L.) is a major fruit crop of arid regions that were domesticated ~7,000 y ago in the

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

238 on has been identified in many arid and semi-arid regions where groundwater is increasingly used for

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

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

241 lts support that LSTs in semi-humid and semi-arid regions with little vegetation will be more sensiti

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

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

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

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

246 nter-annual variability was observed in semi-arid regions, but croplands in China and India also show

247 In arid regions, higher irrigation quota for conventional f

248 Being cultivated in arid and semi-arid regions, the crop often encounters intermittent wat

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

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

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

252 ial carbon sink, especially in arid and semi-arid regions.

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

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

255 ergy harvesting and passive refrigeration in arid regions.

256 on growth have increased demand for water in arid regions.

257 fluctuations of mean solar radiation in hot arid regions.

258 cy, remains a challenge in the arid and semi-arid regions.

259 e significantly (p < 0.05) with OM2, even in arid regions.

260 d to counteract increasing water scarcity in arid regions.

261 ific leaf area (SLA) shrubs with low K(s) in arid relative to tall large-leaved high-SLA trees with h

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

263 ers, with the exception of the water-limited arid river basins.

264 including cool subhumid Ethiopia, cool semi-arid Rwanda, hot subhumid Ghana and hot semi-arid Mali a

265 dy plant encroachment in arctic, alpine, and arid/semi-arid ecosystems around the world, yet our unde

266 ason precipitation for 2 y in field plots at arid, semiarid, and mesic grasslands to investigate temp

267 xture (sand, loam, clay), and climatic zone (arid, semiarid, dry subhumid) were nuanced.

268 mammal, fish, reptile, and plant families in arid, semiarid, dry temperate, and Mediterranean ecosyst

269 This effect was strongest at more arid sites, where water unit-costs are presumably higher

270 stressful mesic areas than in more stressful arid sites.

271 (T) and LB41, isolated from an extreme hyper-arid soil collected from one of the driest regions of th

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

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

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

275 le north, where altitudes are lower, and the arid south, where the Andes are higher, acting as a gene

276 alkaline lake fed by hot springs in the semi-arid southern Kenya Rift Valley.

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

278 inform paleoclimatic reconstructions for the arid southwestern US but are not typically preserved in

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

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

281 among sub-humid, semi-arid, arid, and hyper-arid subtypes will lead to substantial changes in region

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

283 of terrestrial ecosystems and decreases from arid to humid ecosystems.

284 ong-term MAP along the spatial gradient from arid to mesic grasslands.

285 nd affect populations of soil organisms from arid to moist environments remains unknown.

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

287 rom successive harvests were studied in semi-arid tropical viticulture.

288 ires have caused large-scale changes in semi-arid vegetation over the past 50 years.

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 e grassland types (cold, temperate, and semi-arid), warming methods, and short (<=3 years) and longer

292 Similarly, in the arid western US warming does not result in significant g

293 Wheat Screening Nurseries (IBWSNs) and Semi-Arid Wheat Screening Nurseries (SAWSNs).

294 s in avian diversity in the southern African arid zone by the end of the century.

295 ual in the region although they exist in the arid zone of Eurasia (steppes and semi-deserts).

296 The opposite pattern was found in the arid zone.

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

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

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

300 id and 5.6% (30.1 trees per hectare) in semi-arid zones, to 13.3% (47 trees per hectare) in sub-humid