ライフサイエンスコーパス: basin

1 diment grain size and lithology in the Ganga Basin.

2 tte Centrale depression in the central Congo Basin.

3 ion in sea-ice cover in the eastern Eurasian Basin.

4 populations throughout the Mississippi River Basin.

5 e photic-zone impacted the slope belt of the basin.

6 ver these years in upper portions of the Eel basin.

7 from 13 locations across the central Amazon basin.

8 of natural hydrocarbon seepage in the Uinta Basin.

9 y to extended but shallow peat in the Amazon Basin.

10 community in the Amazon is the entire Amazon basin.

11 ally similar to that of the western Eurasian Basin.

12 resources and kinematics study in the Tarim Basin.

13 netic break towards the southern part of the basin.

14 sh species richness across the North Pacific basin.

15 dimentary covers in the neighbouring Sichuan Basin.

16 ge proglacial lake in the Southern North Sea basin.

17 rgence between Eastern Tibet and the Sichuan Basin.

18 rom the oil and gas industry in Utah's Uinta Basin.

19 etween Eastern Tibet Plateau and the Sichuan Basin.

20 fossils in upper Eocene strata of the Gerze Basin.

21 h the total nitrogen loads in streams in the basin.

22 during the wet season in the central Amazon basin.

23 nflow of water, respectively, to the central basin.

24 rom the Arctic continental shelf to deep-sea basin.

25 nsive emerged coastal deposits of the Aurora Basin.

26 the current as it extends into the interior basin.

27 streams and rivers of the Upper Mississippi Basin.

28 of the tropical forests of the entire Congo Basin.

29 ed near Alaer City in the northwestern Tarim Basin.

30 ean climate established in the Mediterranean Basin.

31 (GZWs) on the outer shelf of the Whales Deep Basin.

32 current and potential impacts of dams in the basin.

33 mobility among communities in the same micro-basin.

34 in Borneo, the central Amazon and the Congo Basin.

35 ked strongly to hydrothermal activity in the basin.

36 le of the densely developed Denver-Julesburg basin.

37 ter inputs to the upper Indus and Aral river basins.

38 ing populations and hydro-economies of these basins.

39 nfall datasets with streamflow from 89 river basins.

40 hcp metals, or systems with similar trapping basins.

41 y climate patterns over watersheds and ocean basins.

42 ver of DOC distributions across the Atlantic basins.

43 climate variability over land and over ocean basins.

44 in the mid-oceanic ridges and abyssal ocean basins.

45 teroid Vesta would require at least 6-7 such basins.

46 redictions are consistent across three ocean basins.

47 anoxic or euxinic lakes, estuaries and ocean basins.

48 energy landscape that have relatively narrow basins.

49 move between the Pacific and Atlantic Ocean basins.

50 ecipitation to external changes over typical basins.

51 , and Apalachicola-Chattahoochee-Flint (ACF) basins.

52 th were observed in the Makarov and Amundsen basins.

53 water to underutilized stormwater spreading basins.

54 frastructures extend across four major river basins, 12,500 stream km, and contribute to 100 local ex

55 ere greater in the Dry Basin than in the Wet Basin, 2.16 vs 0.75 g N m(-2) yr(-1), respectively.

56 er-gatherers and farmers in the Lower Danube basin, a geographically intermediate area that is charac

57 r-surface heating of sediment in the Guaymas Basin, a young extensional depression, causes mass produ

58 indicator bacteria (FIB) isolated from catch basins, a constructed wetland, and feces from a beef cat

59 ce data from a 2012 study in the Great Lakes Basin along with the ToxCast effects database were used

60 ggest that the low-latitude closure of ocean basins along east-west trending plate boundaries may als

61 landichthys multifasciatus) from a system of basins along the Atlantic coast of Brazil we test for th

62 PFU min(-1), respectively, for the aeration basin and 79 PFU min(-1) and 0.3 PFU min(-1) for the sew

63 upstream nutrient loading in the Mississippi Basin and are broadly applicable to other coupled human-

64 iting stronger correlations with the El Nino basin and are warmer/cooler during El Nino/La Nina perio

65 eismicity is concentrated in the central sub-basin and decreases to both the north and south.

66 s clearly identified the sentinel lymph node basin and delineated the lymphatic drainage.

67 hemispheres, particularly over the Caribbean basin and East Coast of North America.

68 quid unloadings (a routine operation in this basin and elsewhere) could explain approximately 1/3 of

69 lipped nodes reflect the status of the nodal basin and if targeted axillary dissection (TAD), which i

70 ies of domesticated pea in the Mediterranean Basin and in the Fertile Crescent in relation to the pas

71 are noted along the edge of the Upper Tarim Basin and indicate a decreasing gradient from northeast

72 as been greatest adjacent to the central sub-basin and like the seismicity decreases to the north and

73 r dams have already been built in the Amazon basin and numerous proposals for further dam constructio

74 In the Basin and Range extensional province of the western Unit

75 ing in the Sevier Desert, located in eastern Basin and Range of central Utah, and how this faulting r

76 vely, in the chambers enclosing the aeration basin and sewer models.

77 quamocin in batches from Asia, the Caribbean Basin and the Indian Ocean.

78 e ranching have already affected ~20% of the Basin and up to ~50% of riparian forests in some regions

79 f nutrient inputs from the Mississippi River Basin and water column stratification.

80 sing stress trends were observed in all five basins and annual consumptive use exceeded 100% availabi

81 Holocene in Kivu's deep northern and eastern basins and identifies conditions enabling deposition.

82 hat involves engaging water users within the basins and the development of participatory processes.

83 ments from each basin, varied widely between basins and was (95% CI): 0.09% (0.05-0.15%) in FV, 0.18%

84 While enterococci densities in the catch basins and wetland were similar under wet and drought co

85 ater basins, two often saturated sites ("Wet Basins") and two quick draining sites ("Dry Basins"), we

86 s: toilets, a lab-scale model of an aeration basin, and a lab-scale model of converging sewer pipes.

87 es have been located on the periphery of the basin, and because interpretations can be complicated by

88 strial climate indicators in the Omo-Turkana Basin, and no relationship between paleoaridity and herb

89 entomofaunas from Kyrgyzstan and the Junggar Basin, and provides a Carnian age constraint on the lowe

90 oxic sediments, such as ore deposits, marine basins, and contaminated aquifers.

91 The peatlands occupy large interfluvial basins, and seem to be largely rain-fed and ombrotrophic

92 e lower correlations obtained with the whole basin apparently reflected variable losses of MeHg expor

93 er of the Arctic shelf seas and the interior basin are presented.

94 tained using 100 km buffers instead of whole basin areas.

95 Using the anoxic Cariaco Basin as a natural laboratory, particle association of b

96 a major role in the ventilation of the deep basins as a consequence of shelf-basin exchange.

97 The temperature history of the Malawi basin, at least for the past 500,000 years, strongly res

98 ion began at 61.8 Ma in the eastern Central Basin based on a sediment accumulation rate of 71.6 +/-

99 - 5.6 teragrams of CH4 a year for the Amazon basin, based on regular vertical lower-troposphere CH4 p

100 stantial ice volume in the Aurora subglacial basin before continental-scale ice sheets were establish

101 flow along the boundaries of the three ocean basins, before spiraling southeastward and upward throug

102 drainage projects and individual components (basin, bioswale, culvert, grass swale, storm sewer, and

103 rrestrial transport crossing the major river basin borders is also confirmed by historical sources.

104 sin subalpine species, limber pine and Great Basin bristlecone pine.

105 s from a specific well pad in the Horn River Basin, British Columbia, where there is sufficient avail

106 orly drained soils that are abundant in this basin but not consistently flooded.

107 Desert comprises 64% of the land use in the Basin, but the desert-oasis ecotone plays a prominent ro

108 vasions of freshwater systems on continental basins by multiple lineages.

109 to Pliocene warmth in the Aurora subglacial basin catchment.

110 both regions to streamflow anomalies, river basin characteristics, species traits, and non-native sp

111 nterpret these lags as indicating that Great Basin climate is sensitive to and indirectly forced by c

112 wild specimens captured in the Lambro river basin (Como, Northern Italy) were investigated in order

113 e how delivering recycled water to spreading basins could be optimally implemented.

114 g hunter-gatherers and farmers in the Danube basin, demonstrating that in some regions, demic and cul

115 erved in intra-shelf basin, slope, and slope basin deposits of the Yangtze Sea to assess the ocean re

116 e the need for more mechanistic attention to basin design because the reductions calculated by compar

117 Identification of the sub-basins driving the Fraser River's most significant chang

118 00% availability twice in the Lower Colorado basin during 2003-2015.

119 ha Islands in the South China Sea (SCS) deep basin during the period from August 2012 to January 2014

120 position in lawns, street gutters, and catch basins during two winters.

121 e to flash gas, observed frequencies in most basins exceed those expected if emissions were effective

122 of the deep basins as a consequence of shelf-basin exchange.

123 stitial sites, with analytical solutions for basin exiting time and probability.

124 Sub-basin extirpations in the Southeast (ACT n = 46, ACF n =

125 Sub-basin extirpations in the Southwest (n = 95 Upper CR, n

126 ian biostratigraphy that refine the onset of basin fill to approximately 25.5 Myr and reveal that sed

127 ord and efficiency of sediment bypass to the basin floor.

128 ad to greater efficiency in the Lower Mekong Basin food system.

129 veness and diversity (deserts, fertile river basins, foothills and plains) had no strong influence on

130 The timing of basin formation is broadly coeval with depositional chan

131 placing regular KMC jumps in trapping energy basins formed by neighboring tetrahedral interstitial si

132 raints on the sizes of the Imbrium and other basin-forming impactors markedly increase estimates for

133 cavernosa is a common coral in the Caribbean basin found in several color morphs.

134 r, while the major terrestrial source, Ganga basin (GB) contributes to the latter.

135 erved in high-elevation forests of the Great Basin (GB) region, North America.

136 Wet Basins had higher proportions of denitrification genes a

137 60s, large-scale deforestation in the Amazon Basin has contributed to rising global CO2 concentration

138 Subsequent research in the Indian Ocean basin has identified prehistoric tsunamis, but the timin

139 The southern basin has lower physical connectivity than elsewhere, ag

140 exchange, and recent droughts in the Amazon Basin have contributed to short-term declines in terrest

141 Atlantic Water layer in the eastern Eurasian Basin have increased winter ventilation in the ocean int

142 Water management institutions in each of the basins have evolved during the last 10-20 years from a r

143 Over the Mediterranean Basin, however, losses from decreasing frequency of low-

144 lmon varied among regions in the Great Lakes basin (i.e., Lake Huron, Lake Michigan, or Lake Superior

145 xisting policies are inconsistent across the Basin, ignore cumulative effects, and overlook the hydro

146 ng organic compounds (EOCs) in two catchment basins impacted by wastewater discharges.

147 maximum possible area reported for the Congo Basin in a recent synthesis of pantropical peat extent.

148 ay to the geogenic chemical signature of the basin in both dissolved and suspended loads.

149 web in the Koobi Fora region of the Turkana Basin in Kenya.

150 nct sediment facies recovered from a bedrock basin in Pine Island Bay indicates deposition within a l

151 cies over 18 years in a large, dryland river basin in southwestern United States.

152 The formation of the Central Basin in Spitsbergen is inherently linked to changes in

153 iisotope pedothem record from the Wind River Basin in Wyoming confirms a previously hypothesized peri

154 Samples from four distant basins in Chile were genotyped for 13 microsatellite loc

155 below sea level within the Aurora subglacial basin, indicating that this catchment, which drains ice

156 The Dry Basin infiltrated a much larger volume of water and thus

157 d destruction (at subduction zones) of ocean basins influences the diversity dynamics of marine inver

158 s and following their route from the central basin interior to the east (toward the Tyrrhenian) and t

159 The Permian Basin is being transformed by the "shale revolution" fro

160 Note that the Tarim River Basin is more vulnerable to the impact of emissions, esp

161 , France) edges of the Western Mediterranean basin is presented.

162 The Tarim Basin is regarded as one of the most highly erodible are

163 Multiring basins, large impact craters characterized by multiple c

164 ed (Lepidothrix iris) manakins of the Amazon basin, leading to the formation of the hybrid species, t

165 se and water stress at both the national and basin level.

166 sulted in only a single enlarged cusp in the basin-like heel (talonid in lower molars, talon in upper

167 udy, at three sites across the Mediterranean Basin, litter CO2 efflux was largely explained by litter

168 on of fungi in five permanently covered lake basins located in the Taylor and Miers Valleys of Antarc

169 0.06% of the 54,000 oil and gas wells in the basin (lower estimate) to 0.15% of the 20,700 wells in t

170 Consequently, at the watershed scale the Wet Basin may have better overall DIN treatment.

171 Himalayan uplift and changes in the Jilong basin may have contributed to these divergences, but upl

172 ropical North Atlantic, which would make the basin more suitable for hurricane formation and growth.

173 ation method and gravimetric method at Great Basin National Park, NV.

174 late Early Eocene Arshanto Formation, Erlian Basin, Nei Mongol, China.

175 The in-situ stress state in the Tarim Basin, Northwest China, down to 7 km depth is constraine

176 The Eridania basin occurs within some of the most ancient terrain on

177 tion of cells repopulated the whole original basin of attraction within days to weeks.

178 e Pleistocene site of Mata Menge in the So'a Basin of central Flores, Indonesia, have yielded hominin

179 ith newly sampled wells in the Yangtze River Basin of China.

180 uality characteristics in the northern Raton Basin of Colorado and documented the response of the Poi

181 trics for eight sites located in the western basin of Lake Erie, including a station proximal to the

182 canus [12] (260 mya) [13, 14] from the Karoo Basin of South Africa, indicates the initiation of rib b

183 mescale from the Cretaceous Western Interior Basin of what is now North America.

184 resilience, fold-bifurcations, and alternate basins of attraction.

185 y almost-invariant attracting sets and their basins of attraction.

186 tuations as these systems move between local basins of inherent structure.

187 orus reductions from 1 to 10% in major river basins of the Upper Mississippi region.

188 been difficult, particularly for the Amazon basin-one of Earth's major centres of deep atmospheric c

189 rifying 58% of incoming DIN, whereas the Dry Basin only denitrified 1%.

190 s model can inform decisions about spreading basin operation policies and the development of new wate

191 five sites in the North American Great Lakes basin over the period of March 2012 to December 2014, in

192 ng Bakken and oil-producing regions of mixed basins (p < 0.0001, chi(2) test).

193 Although Great Basin paleoclimate history has been examined for more th

194 alagmite delta(18)O time series - that Great Basin paleoclimate is linearly related to, but lagged, t

195 age of the basal conglomerate in the Qaidam basin place this event in Paleocene-Eocene.

196 an method (EPA's OTM 33a) in four major U.S. basins/plays: Upper Green River (UGR, Wyoming), Denver-J

197 the three water masses of the Central Arctic Basin (PML, intermediate Atlantic Water Layer, and the A

198 Lithospheric storage of OC in peripheral SCS basins potentially exceeded 4,000 Gt (equivalent to 2,00

199 concentrations was not observed in the Negro Basin probably due to the variable export of MeHg from p

200 g of the chronostratigraphy and evolution of basin processes.

201 rmal faulting stress regime within the Tarim Basin rather than in the compressional tectonic stress r

202 ii-like) dominated the colonies in all ocean basins regardless of morphology, although the Trichodesm

203 gment groundwater recharge through spreading basins represent cost-effective opportunities to diversi

204 ncroaching "atlantification" of the Eurasian Basin represents an essential step toward a new Arctic c

205 emission estimates in a major U.S. shale gas basin resolved from west to east show (i) similar spatia

206 Here we show that rainfall in the basin responds closely to changes in glacial boundary co

207 Moreover, research into the attractors' basins reveals the origin of stochasticity, hysteresis a

208 otprint methodology, to the Upper Rio Grande Basin (RGB) in south central Colorado.

209 sparate hypersaline sapropels (Transylvanian Basin, Romania) in relation to geochemical milieu and po

210 tic disturbances that will affect the Amazon basin's floodplains, estuary and sediment plume.

211 ally builds up soil moisture and reduces the basin's infiltration capacity, thereby elevating the ris

212 f the transient crater that would reveal the basin's maximum volume, but its diameter may now be infe

213 tidal and rotational torques can explain the basin's present-day location, but requires the feature t

214 new light on the interpretation of previous basin scale aircraft studies, and provides an improved m

215 atial and behavioral differences on an ocean-basin scale by measuring puffins' among-colony differenc

216 ource management and governance at the river basin scale is critical for the sustainable development

217 departure "expected" streamflow) at the sub-basin scale over the past half-century.

218 hancing stakeholder cooperation at the major basin scale towards preventing further degradation of fr

219 mates of nitrate storage are validated using basin-scale and national-scale estimates and observed gr

220 ated sediments and compare them with Pacific basin-scale and regional indices of ocean climate variab

221 ow conditions that amplified the 2 degrees C basin-scale anomaly.

222 ies compositions that are more influenced by basin-scale climatic fluctuations than others.

223 Evidence of regional- to basin-scale controls on domoic acid has not previously b

224 community persistence relative to local and basin-scale environmental fluctuations.

225 Here we provide the first basin-scale investigation of IME.

226 However, to understand basin-scale patterns in ecosystem and climate dynamics,

227 different datasets are inconsistent at river basin scales, and the magnitude of index differences is

228 ere also observed downstream at larger river basin scales.

229 lture panel (BCP) multiplex PCR assay (Great Basin Scientific, Salt Lake City, UT) for the rapid and

230 or-solid deposition process of ZnO, a unique basin-shaped crown was formed on the tip of each nanowir

231 ity, display predominantly subsidence of the basin side (fault hanging wall), with comparatively litt

232 bstantially higher during high-water in both basins since elevated MeHg concentrations and discharge

233 The San Juan Basin (SJB) is one of the largest coal-bed methane produ

234 n-Cambrian boundary preserved in intra-shelf basin, slope, and slope basin deposits of the Yangtze Se

235 avily populated and polluted South Coast Air Basin (SoCAB).

236 Moho are observed in the lower crust of the basins south of Qilian, which we interpret as the top of

237 mate change that includes the western Amazon basin, south-western Kenya, north-eastern Tanzania, nort

238 The sedimentary record in the Guadix-Baza Basin (southern Spain) has proved to be a great source o

239 Of the two MPXV clades, the Congo Basin strain is associated with severe disease, increase

240 ional range shift for the two dominant Great Basin subalpine species, limber pine and Great Basin bri

241 was conducted in June 2014 in the Eagle Ford basin, Texas, to examine spatiotemporal variability of m

242 nflow minus outflow) were greater in the Dry Basin than in the Wet Basin, 2.16 vs 0.75 g N m(-2) yr(-

243 ipitation anomaly over the lower Mississippi basin that gradually builds up soil moisture and reduces

244 2.5 aerosols concentration in the Owens Lake basin that might limit the impact of mineral dust aeroso

245 ental shelf seaward of the Aurora subglacial basin, that marine-terminating glaciers existed at the S

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

247 basin (the Tarim River Basin, TRB) and humid basin (the Yangtze River Basin, YRB) were evaluated, det

248 a choke point separating the sea in two main basins, the Eastern Mediterranean Sea and the Western Me

249 Among wet basins, TNMA emissions had a strong negative correlation

250 We used sediment from a reef and a boat basin to mimic natural sediment (coarse) and anthropogen

251 boxy-terminus reduces the extent of the main basin to more extended configurations of Htt17 with lowe

252 s of AGB with climate data across the Amazon Basin to reconstruct annual maps of potential AGB during

253 reveals that the lithosphere of the Junggar Basin to the north became uncoupled along the Moho, and

254 r pollutant emission rates from two Colorado basins to create a spatiotemporal industrial activity mo

255 the central Gulf is greater than in the sub-basins to the north and south.

256 ological sources are a small fraction of the basin total (0.02-0.12 Tgyr(-1)) and cannot explain basi

257 emission estimates between aircraft studies (basin total for a midday window) and emissions inventori

258 served in carbonate rocks across bathymetric basin transects from nine localities of the Nama Group,

259 to streamflow alteration in the Tarim River Basin (TRB) using the double mass curve method (DMC) and

260 5) models to the arid basin (the Tarim River Basin, TRB) and humid basin (the Yangtze River Basin, YR

261 We found that the Great Basin treeline for these species is expanding upslope wi

262 ogen (N) cycling dynamics of four stormwater basins, two often saturated sites ("Wet Basins") and two

263 Aquifers in the Upper Colorado River Basin (UCRB) exhibit persistent uranium (U) groundwater

264 Overall, wet-gas basins (UGR, DJ, Uintah) had higher TNMA emissions than

265 l dataset performance across multiple areal (basin) units.

266 ined by bootstrapping measurements from each basin, varied widely between basins and was (95% CI): 0.

267 The Wet Basin was capable of denitrifying 58% of incoming DIN, w

268 e Niobrara Formation in the Denver-Julesburg Basin was completed.

269 Once the basin was established, ice would naturally have accumula

270 For example, whether the Amazon basin was substantially drier or remained wet during gla

271 MeHg dynamics in both basins was contrasted to provide insight into the factor

272 replicated at the two extremes of the Amazon basin, we reciprocally transplanted 4638 tree seedlings

273 In 215 patients, 279 nodal basins were identified.

274 Basins") and two quick draining sites ("Dry Basins"), were monitored over a approximately 1-year per

275 city, they must find their way to the Tidal Basin where the Japanese trees grow.

276 ll distances and brief time periods, even in basins where water may be relatively abundant overall.

277 ces are available from patients in the Congo Basin, where HIV-1 expanded early in the global pandemic

278 ress regime as in the periphery of the Tarim Basin, which explains the presence of the normal faults

279 In the Piceance Basin, which had not experienced substantial prior O&G d

280 ing absolute time constraints in sedimentary basins, which improves our understanding of the chronost

281 owever, that conditions conducive to greater basin-wide Atlantic hurricane activity occur together wi

282 Across the four models, basin-wide average AGB is similar to the mean of the obs

283 We use a 60-year ocean basin-wide data set comprising >148,000 samples to revea

284 native fish species losses, irrespective of basin-wide differences in native or non-native species r

285 d that the occurrence of an unusually strong basin-wide easterly wind burst (EWB) in June was a key f

286 s stalled as a result of an unusually strong basin-wide easterly wind burst in June, which led to the

287 These data were used to generate a basin-wide ecophysiological fingerprint of Lake Erie Mic

288 act in concert to either enhance or inhibit basin-wide hurricane activity.

289 ed States coast during periods of heightened basin-wide hurricane activity.

290 e establishment of a coordinated and dynamic basin-wide management scheme; if appropriate, this may i

291 Conversely, during the most-recent period of basin-wide quiescence, hurricanes (and particularly majo

292 n heat content during this phase can lead to basin-wide uniform warm conditions in the equatorial Pac

293 ts is a common process at contaminated sites basin-wide, to constrain accumulated U(IV) speciation, a

294 connection of the Pacific and Atlantic Ocean basins will present both challenges to marine ecosystem

295 of the sampling site in the Solimoes/Amazon Basin with the best correlation obtained using 100 km bu

296 ty, and 90% of global catch comes from river basins with above-average stress levels.

297 climate variability across the Pacific Ocean basin, with influence on the global climate.

298 er in the U.S., the Ganges-Brahmaputra-Mehta Basin within Bangladesh, and the Mekong Delta in Cambodi

299 veral enormous igneous plateaus in the ocean basins worldwide.

300 pecies found in the Amazon and Orinoco river basins, yet few resources for genetic studies and the ge

301 sin, TRB) and humid basin (the Yangtze River Basin, YRB) were evaluated, determining the response of