ライフサイエンスコーパス: subtropical

1 but net nitrification rates are often low in subtropical acid soils.

2 ociation exists among HIV-infected people in subtropical Africa.

3 photosynthetic activity across tropical and subtropical Amazonia.

4 n rapidly spread throughout the tropical and subtropical Americas.

5 on on cropland and pasture, and in tropical, subtropical and boreal zones.

6 ellowfin, and skipjack tunas in the northern subtropical and eastern tropical Pacific Ocean, the Arab

7 ion, through circulation changes between the subtropical and subpolar gyres--the intergyre region.

8 Our results also indicate that subtropical and temperate forest biomes provide the high

9 sing data from a global network of tropical, subtropical and temperate forest plots.

10 tality has been widely detected in tropical, subtropical and temperate forests, with soil pathogens a

11 up to 400 million people and are endemic to subtropical and tropical areas of the world.

12 ual but offers a unique insight into ancient subtropical and tropical ecosystems.

13 resistant, and the larvae develop rapidly in subtropical and tropical environments.

14 Subtropical and tropical forests are biodiversity hotspo

15 he relatively weak seasonality of the stable subtropical and tropical oceans in the global model enab

16 rbon and nitrogen cycles in the oligotrophic subtropical and tropical oceans.

17 ve been reported in some developing areas in subtropical and tropical regions known to be destination

18 However, in subtropical and tropical regions, influenza epidemics ca

19 can be made at least 3 weeks in advance for subtropical and tropical regions.

20 s, particularly with reference to introduced subtropical and tropical species and predictions of both

21 s and is especially unconstrained for warmer subtropical and tropical systems which account for a lar

22 brates, corals, and fishes characteristic of subtropical and tropical waters.

23 rred in 3 (7%) of 43 temperate, 1 (17%) of 6 subtropical, and 11 (37%) of 30 tropical countries with

24 measurement periods throughout the tropical, subtropical, and boreal environments studied.

25 gesting different trajectories for tropical, subtropical, and temperate drylands.

26 whether the consumption of total, temperate, subtropical, and tropical fruit is associated with T2DM

27 cation and poleward expansion of the Pacific subtropical anticyclone culminating in A.D. 1140-1260 op

28 ing in the Agulhas Current and shifts of the subtropical anticyclones.

29 spiratory surveillance sites in tropical and subtropical areas (Bangladesh, China, Egypt, Guatemala,

30 cherry and blueberry fruits produced in the subtropical areas of Brazil and to verify that the chemi

31 poorly understood, especially in tropical or subtropical areas of Southeast Asia.

32 Carica papaya L.) production in tropical and subtropical areas throughout the world.

33 common globally, especially in tropical and subtropical areas.

34 d solar radiation on rice yields in tropical/subtropical Asia.

35 arrival of Saharan dust in the Caribbean and subtropical Atlantic coincided with high levels of disso

36 xpedition which covered all the tropical and subtropical Atlantic, Pacific and Indian oceans.

37 hase samples collected from the tropical and subtropical Atlantic, Pacific, and Indian Oceans during

38 red, for the first time, in the tropical and subtropical Atlantic, Pacific, and Indian Oceans.

39 t time in the atmosphere of the tropical and subtropical Atlantic, Pacific, and Indian oceans.

40 reviously published data from the Arctic and subtropical Atlantic, show that surface Atlantic meridio

41 n many locations across the globe, including subtropical Australia.

42 Eucalyptus stand on highly weathered soil in subtropical Australia; AmazonFACE in a highly diverse, p

43 socosm CO2 perturbation study in a eutrophic subtropical bay during summer by investigating the effec

44 include: (i) persistently positive tropical/subtropical biases in Rn using the NCEP/NCAR, and gradua

45 fer little compensation in many tropical and subtropical biomes.

46 nd with empirical data for forest-inhabiting subtropical birds that the species-fragmented area relat

47 long the northern Gulf of Mexico coast, USA, subtropical black mangrove (Avicennia germinans) at the

48 ) collected from six surface water bodies in subtropical Brisbane, Australia, prior to and after stor

49 The SAR for lakes in the East Plain of subtropical China (1.05 +/- 0.28 mm yr(-1) ) was higher

50 have occurred across the whole soil depth in subtropical China and the magnitudes of the changes in s

51 s of naturally colonized decomposing wood in subtropical China and, for the first time, compared them

52 l changes in soil C-N-P stoichiometry across subtropical China, where soils are P-impoverished, with

53 italization associated with influenza in the subtropical city of Hong Kong.

54 oniferous and broadleaved forests across the subtropical climate gradient; however, this difference d

55 n Ningbo, a southern China city with typical subtropical climate.

56 -1), respectively) than in Mediterranean and subtropical climates (13.0 and 9.7 g m(-2) day(-1), resp

57 ed with increased mortality in temperate and subtropical climates.

58 coniferous and broadleaved forests across a subtropical climatic gradient.

59 ominant invertebrates (n = 900) in a diverse subtropical coastal marine community (50 families, 72 ge

60 status and skin cancer risk in an Australian subtropical community.

61 t in mountainous biomes such as tropical and subtropical coniferous forests (0.08 km yr(-1)), tempera

62 100 in Taihe County in southern China, where subtropical coniferous plantations dominate.

63 suggest that growth rates in this species of subtropical coral have been tolerant to recent climatic

64 calcification master chronologies from seven subtropical corals (Montastraea faveolata) located in th

65 cucurbit seed crop production in tropical or subtropical countries explains its recent rapid dispersi

66 itratus Stapf is widely used in tropical and subtropical countries in cooking, as a herbal tea, and i

67 lderness and protected areas in tropical and subtropical countries with adverse consequences for thei

68 creasing at an alarming rate in tropical and subtropical countries, underlying the need for a dengue

69 ing at an alarming rate in many tropical and subtropical countries, where epidemics can put health ca

70 f death and disease across many tropical and subtropical countries.

71 itic disease endemic in several tropical and subtropical countries.

72 ned today is less than in the recent past in subtropical countries.

73 rn North Pacific, which is owing to enhanced subtropical deep convection and favorable dynamic condit

74 3.5-year field experiment was conducted in a subtropical degraded shrubland to assess how a nurse pla

75 fferent tree species in the reforestation of subtropical degraded shrublands.

76 this hypothesis were tested in two types of subtropical, depressional-basin wetland: forested swamps

77 ng storm tracks and the size and location of subtropical deserts.

78 The South Atlantic Subtropical Dipole index (SASD) is based on the distribu

79 ruses, viruses that often cause tropical and subtropical diseases.

80 In view of the large scale, tropical and subtropical distribution of the taxon, the possibility i

81 y in response to a poleward migration of the subtropical dry zone.

82 oleward displacement of the storm tracks and subtropical dry zones and to a widening of the tropical

83 is thus identified whereby the intensity of subtropical dry zones in models associated with the bore

84 the subtropics and poleward expansion of the subtropical dry zones.

85 Uncertainty in the future of tropical and subtropical drylands is well constrained, whereas soil m

86 contract by a third, primarily converting to subtropical drylands, and that deep soil layers could be

87 edictability and highlight the importance of subtropical dynamics in understanding monsoon and TS pre

88 Most of the essential elements of the subtropical EBLFs appear to have originated around the O

89 ation reconstructions have revealed that the subtropical EBLFs existed in Southwest China during the

90 e facilitated the historical assembly of the subtropical EBLFs in East Asia.

91 Data from other characteristic components of subtropical EBLFs, including Fagaceae, Lauraceae and Mag

92 Theaceae), a characteristic component of the subtropical EBLFs, to gain new insights into the assembl

93 redation plays a key role in structuring the subtropical ecosystem.

94 Subtropical ecosystems are often characterized by high N

95 ay, Western Australia--a relatively pristine subtropical embayment whose dominant, canopy-forming sea

96 l radiation of birds that originated in wet, subtropical environments, but subsequently spread to dri

97 S-transferases (GSTs) occurs in tropical and subtropical environments.

98 d data from 270 stations in 29 temperate and subtropical estuaries and lagoons show transient accumul

99 ght, both of which had profound impacts on a subtropical estuarine fish community.

100 mporal variability of ciliate community in a subtropical estuary by rRNA and rDNA-based high throughp

101 semivolatile organic chemicals (SVOCs) from subtropical eucalypt forest and tropical savannah fires

102 (e.g., permethrin) were determined from the subtropical eucalypt forest fire.

103 Subtropical evergreen broad-leaved forest (EBLF) is one

104 Subtropical evergreen broadleaved forests (EBLFs) inhabi

105 off-equatorial monsoon circulation than the subtropical-extratropical volcanoes do.

106 tation regenerating from fire disturbance in subtropical Florida was exposed to experimentally elevat

107 thropods and microorganisms-in a mountainous subtropical forest are highly nonlinear across spatial s

108 tional, and phylogenetic beta diversity in a subtropical forest chronosequence in Southeastern China.

109 on operator13 PAHs) were determined from the subtropical forest fire (7,000 +/- 170) compared to the

110 sts growing on abandoned pastures in the wet subtropical forest life zone of Puerto Rico.

111 The response of this subtropical forest to strong typhoons suggests that incr

112 2016 on seedling survival over 9 years in a subtropical forest; and (ii) how spatial heterogeneity i

113 ation could decrease soil CH4 consumption in subtropical forests and potentially contribute to increa

114 variant community composition in contrasting subtropical forests and provides a new perspective on th

115 oduction of long-lived trees in tropical and subtropical forests are also being impacted by changes i

116 esses in structuring the beta diversities of subtropical forests in human disturbed landscapes is sti

117 al physiological responses of trees in three subtropical forests representing an urban-to-rural gradi

118 Intensive forestry practiced within subtropical forests resulted in the highest rates of for

119 ximately 1.39 trillion exist in tropical and subtropical forests, with 0.74 trillion in boreal region

120 characteristics of bacterial communities in subtropical forests.

121 ly unpredictable and difficult to control in subtropical forests.

122 tionary history in disturbed and undisturbed subtropical forests.

123 ry factor for controlling CH4 consumption in subtropical forests.

124 g diversity across a gradient from boreal to subtropical forests.

125 n is under-studied in phosphorus (P)-limited subtropical forests.

126 l climbing perch (Anabantidae) and a diverse subtropical fossil flora from the Chattian (late Oligoce

127 O) and iodine oxide (IO) in the tropical and subtropical free troposphere (10 degrees N to 40 degrees

128 and diffusive fluxes were estimated in three subtropical freshwater reservoirs (Little Nerang Dam (LN

129 he highest reported thus far indicating that subtropical freshwater reservoirs could be significant a

130 across the polar front and subduction at the subtropical front.

131 mango by-products come from the tropical or subtropical fruit processing industries.

132 Sapindaceae), known as Chinese Cherry, is a subtropical fruit tree originating from southern China.

133 cold and with those previously known in the subtropical grass rice (Ehrhartoideae).

134 Pollen allergens restricted to subtropical grasses (groups 22-24) were also present wit

135 st (5.4 million km(2)) and across 80% of the subtropical grasslands (3.3 million km(2)).

136 C(4) grasses dominate tropical and subtropical grasslands and savannas, and C(3) grasses do

137 The North Pacific subtropical gyre (NPSG) plays a major part in the export

138 C) as well as the oligotrophic North Pacific Subtropical Gyre (NPSG).

139 extended throughout the entire North Pacific Subtropical Gyre (NPSG).

140 sphaera over eight days in the North Pacific Subtropical Gyre (NPSG).

141 atellite observations from the North Pacific Subtropical Gyre and a simple ecosystem model, we show t

142 nitrogen and phosphorus in the North Pacific Subtropical Gyre and iron in the equatorial Pacific.

143 e tetraether lipid pool in the North Pacific Subtropical Gyre at shallow to intermediate depths.

144 f samples collected from the North Artlantic subtropical gyre during the sea campaign Expedition seve

145 ater nutrient injection in the North Pacific Subtropical Gyre provides an aperiodic yet significant s

146 an ventilation and suggest that the interior subtropical gyre should not be ignored when considering

147 , 130 to 180 degrees W) in the North Pacific subtropical gyre that closely corresponds to centers of

148 n the permanently oligotrophic North Pacific Subtropical Gyre that document a large, rapid, and predi

149 Outside the North Pacific subtropical gyre the median plastic concentration was 0

150 signatures of lipids from the North Pacific Subtropical Gyre to show that in the surface ocean, lipi

151 lle Thomson Overflow Water (WTOW) mixes with subtropical gyre waters and the second at 1500-1600 m wh

152 Lawrence Valley advects into the subtropical gyre ~3,000 km south of the North Atlantic d

153 mimic nutrient loading in the North Pacific Subtropical Gyre, and the transcriptional responses of p

154 buoyant microplastics in the North Atlantic subtropical gyre, from 0 to 5 m depth.

155 ic Time-series Station in the North Atlantic Subtropical Gyre, while assessing seasonal shifts in sta

156 te-poor surface waters of the North Atlantic subtropical gyre.

157 g the eastern boundary of the North Atlantic subtropical gyre.

158 ps was a stable feature in the North Pacific Subtropical Gyre.

159 ean Time-series station in the North Pacific subtropical gyre.

160 s) of debris collected in the North Atlantic subtropical gyre.

161 evidence from the surface mixed layer of the subtropical gyres and adjacent equatorial and temperate

162 biting surface waters of the North and South subtropical gyres and the Equatorial Region of the Atlan

163 Oligotrophic subtropical gyres are the largest oceanic ecosystems, co

164 in the convergence zones of each of the five subtropical gyres with comparable density.

165 ing the distance to coastal regions, oceanic subtropical gyres, currents and biogeochemical processes

166 genome amplification of prokaryotes from two subtropical gyres, we obtained genomic DNA from 738 cell

167 igh latitudes and low ( approximately 5%) in subtropical gyres, with intermediate values in the tropi

168 over a broad geographic area, from boreal to subtropical habitats.

169 Feeding assays identified two key tropical/subtropical herbivores that consumed transplanted kelp w

170 The western Pacific Subtropical High (WPSH) is a prime circulation system af

171 s a precarious balance between the expanding subtropical high from the south and the south-eastward e

172 st Asian summer monsoon and the West Pacific Subtropical High.

173 position and intensity of the South Atlantic Subtropical High.

174 on (ENSO) and the variability in the Pacific subtropical highs (PSHs) have major impacts on social an

175 most prominent feature in most tropical and subtropical hydroclimate proxies.

176 This tropical to subtropical hydrologic phenomenon is likely to be an ini

177 ight the importance of polar regions for the subtropical hydrological cycle.

178 ws that tropospheric ozone concentration and subtropical intrusions account 65% of the co- variabili

179 o ENSO and that the barotropic nature of the subtropical intrusions restricts the tracers within the

180 ction of these super El Nino events with the subtropical jet annual cycle.

181 A poleward shift of the subtropical jet over South America and an increase of lo

182 opause folding, linked to variability in the subtropical jet stream.

183 4), concordant with the strengthening of the subtropical jet system and the East Asia winter monsoon.

184 er tropospheric equatorial westerly wind and subtropical jets during boreal winter to spring.

185 from stronger equatorial westerly ducts and subtropical jets during La-Nina and weaker during El-Nin

186 centration of plastic debris was observed in subtropical latitudes and associated with the observed l

187 uggests that mountain ranges in tropical and subtropical latitudes play an important role in the spec

188 lower limb of the AMOC, between subpolar and subtropical latitudes, consumes 72% of the DOC exported

189 g a temperate location [Virginia (VA)] and a subtropical location [Florida (FL)].

190 hrough growth-rate assays, we found that the subtropical Louisiana population has a higher fitness at

191 cal Caribbean basin and the other endemic to subtropical Louisiana.

192 Expression analysis of earleaf samples in a subtropical maize recombinant inbred line population (CM

193 n of anomalies has increased the subpolar to subtropical meridional gradient in SSTs, which are not r

194 o its abundance and ubiquity in the tropical/subtropical mixed layer, has been the workhorse of paleo

195 In both climate models and observations, the subtropical moistening is linked to a poleward shift of

196 lags, supporting the view that the tropical-subtropical monsoon variability is driven directly by pr

197 ibuted in northern temperate and tropical to subtropical mountainous regions.

198 ng-term chronosequence during which areas of subtropical native forest were replaced by Chinese fir,

199 rymnesiophytes sorted by flow cytometry from subtropical North Atlantic waters.

200 ) reported for the mesopelagic waters of the subtropical North Atlantic.

201 d associated anomalous anticyclones over the subtropical North Pacific and Atlantic has a deeper root

202 ming, the surface winds converge towards the subtropical North Pacific from the tropics, leading to a

203 The wind changes induce a subtropical North Pacific SST warming through wind-evapo

204 Pacific, which weakens the Aleutian low and subtropical North Pacific westerlies.

205 the tropics, with secondary increases in the subtropical Northern Hemisphere.

206 trongly associated with carbon export in the subtropical, nutrient-depleted, oligotrophic ocean.

207 ts of new nitrogen to oligotrophic, tropical/subtropical ocean surface waters.

208 vity of Trichodesmium throughout much of the subtropical ocean.

209 on of primary production in the tropical and subtropical ocean.

210 and air-sea exchanges over the tropical and subtropical oceans based on the data collected along the

211 isplay a pronounced peak in the oligotrophic subtropical oceans, where DOC accounts for roughly half

212 cur throughout the oligotrophic tropical and subtropical oceans, where they can dominate the diazotro

213 gle oceanic expedition covering tropical and subtropical oceans.

214 role in the productivity of the tropical and subtropical oligotrophic oceans.

215 e consumption of temperate fruit, but not of subtropical or tropical fruit, was associated with lower

216 ncreased influence of nutrient-poor water of subtropical origin.

217 A size-based ecosystem model for the subtropical Pacific captures this pattern well as a resp

218 nchronized to the day/night cycle across the subtropical Pacific Ocean.

219 Plankton samples from the tropical and subtropical Pacific, Atlantic and Indian Oceans were col

220 ects of warming rate on the decomposition of subtropical peats, by applying either a large single-ste

221 nducted a manipulative field experiment in a subtropical plant community in the subsiding Mississippi

222 Furthermore, the observed patterns of subtropical precipitation change, from 1979 to 2000, are

223 depletion, have substantially contributed to subtropical precipitation changes.

224 web changes with elevation in an Australian subtropical rain forest.

225 ogical variables, on ecosystem dynamics in a subtropical rainforest.

226 64 patients with grass pollen allergy from a subtropical region.

227 widely distributed in the humid tropical and subtropical regions and are generally characterized with

228 nt for patients with grass pollen allergy in subtropical regions and reduce the burden of allergic re

229 Individuals originating from tropical and subtropical regions are most at risk.

230 did the broad patterns of arid and semiarid subtropical regions become fully developed.

231 de regions are expected to become wetter and subtropical regions drier.

232 g the warm Miocene and Pliocene Epochs, vast subtropical regions had enough precipitation to support

233 c disease that is widespread in tropical and subtropical regions of Africa, Asia, and the Americas an

234 y species is an important forest tree in the subtropical regions of China and could have a major role

235 d human parasitic infections in tropical and subtropical regions of the world such as Africa, South A

236 to ecological niches throughout tropical and subtropical regions of the world, though medfly infestat

237 and -4, are endemic throughout tropical and subtropical regions of the world, with an estimated 390

238 hock syndrome and is endemic to tropical and subtropical regions of the world.

239 calis dust mite is prevalent in tropical and subtropical regions of the world.

240 bidity and mortality throughout tropical and subtropical regions of the world.

241 e of morbidity and mortality in tropical and subtropical regions of the world.

242 by mosquito vectors throughout tropical and subtropical regions of the world.

243 rough 4, are endemic throughout tropical and subtropical regions of the world.

244 (DENV) are endemic pathogens of tropical and subtropical regions that cause significant morbidity and

245 endemically circulates in many tropical and subtropical regions worldwide.

246 and A. albopictus mosquitoes in tropical and subtropical regions worldwide.

247 a major public health issue in tropical and subtropical regions worldwide.

248 e and threaten public health in tropical and subtropical regions worldwide.

249 by Aedes aegypti mosquitoes in tropical and subtropical regions, but the potential exists for furthe

250 intensification of dry conditions over these subtropical regions, rather than the return to a wetter

251 ocated in cold temperate, warm temperate and subtropical regions, respectively.

252 otrophs compete with high N:P communities in subtropical regions, the ocean nitrogen inventory rises

253 rgens of a grass with clinical importance in subtropical regions, where an increasing proportion of t

254 meters per second), and it occurs mainly in subtropical regions, where the background flows are weak

255 h by causing major outbreaks in tropical and subtropical regions, with no available direct-acting ant

256 nd is major cause of disease in tropical and subtropical regions.

257 underreported, particularly in tropical and subtropical regions.

258 th problem that mainly afflicts tropical and subtropical regions.

259 vers, and on average across wet tropical and subtropical regions.

260 e extinctions in nine important tropical and subtropical regions.

261 t in more than 120 countries in tropical and subtropical regions.

262 er--has been discovered in some tropical and subtropical regions.

263 easing public health problem in tropical and subtropical regions.

264 to human health, especially in tropical and subtropical regions.

265 , indicating the strategy could be useful in subtropical regions.

266 allergic asthma and rhinitis in tropical and subtropical regions.

267 ) infects millions of people in tropical and subtropical regions.

268 gher order auditory forebrain regions of the subtropical resident Indian weaverbirds (Ploceus philipp

269 hat phytoplankton in the phosphorus-depleted subtropical Sargasso Sea were enriched in the biochemica

270 temperature and humidity on these levels in subtropical school settings.

271 lts initially point to the importance of the subtropical South Indian Ocean, where physically coheren

272 presence and reseeding of this fauna in the subtropical southeast Atlantic was driven by interocean

273 ng 40 years of study of reforestation in the subtropical southeastern USA, repeated observations of a

274 sh first sightings appear to be tropical and subtropical species moving towards high latitudes, as wo

275 For instance, Chinese and Brazilian subtropical speleothem (cave formations such as stalacti

276 CFC-12 data reveals a decrease in the age of subtropical subantarctic mode waters and an increase in

277 cal, i.e. made dryer via pole-ward expanding subtropical subsidence.

278 010) of (90)Sr concentration measurements in subtropical surface waters of the western North Pacific

279 NTA SST triggering the following ENSO via a subtropical teleconnection mechanism) processes alternat

280 530.4, 513.2, and 336.7 kg/ha for tropical, subtropical, temperate, and boreal forests, respectively

281 udies encompassing 22 species from tropical, subtropical, temperate, boreal and mediterranean ecosyst

282 ven changes in the depth of the tropical and subtropical thermocline that have multiplicative effects

283 rical hyphal length) across 14 coexisting AM subtropical tree species following root pruning and nutr

284 esign with leaf litter inputs of four native subtropical tree species in a Pinus massoniana plantatio

285 ng contrasts in abundance between sites of a subtropical tree species, Ormosia glaberrima, to demonst

286 Our analysis shows that subtropical waters are a dominant component in the forma

287 f a deep divergence among N. phocaenoides in subtropical waters compared with N. asiaeorientalis in t

288 vidence suggests that an anomalous inflow of subtropical waters driven by atmospheric changes, multid

289 plained by the northward expansion of cooler subtropical waters due to a weakening of the South Pacif

290 values), with individuals feeding in warmer subtropical waters having lower concentrations of pestic

291 ted high transfer of mercury to predators in subtropical waters, which merits further investigation.

292 on a temperate spring phytoplankton bloom in subtropical waters.

293 These subtropical wave breaking events lead to the intrusion o

294 ngth (r = -0.92), the total TS days over the subtropical western North Pacific (r = -0.81), and the t

295 es on iodine speciation and mobility in this subtropical wetland environment, groundwater was collect

296 Tropical and subtropical wetlands estimates reach 4.7 million km(2) (

297 We examined C and N budgets of a subtropical woodland after 11 yr of exposure to elevated

298 F(a) or EF(b) for global, temperate zone and subtropical zone datasets, a power function of DIN yield

299 The soil N stock increased in the subtropical zone.

300 ease continues to expand beyond tropical and subtropical zones, a growing need exists to better under