ライフサイエンスコーパス: basin

1 ropagating mesoscale eddies from the Pacific basin.

2 ularly in countries around the Mediterranean basin.

3 of tectonic propagation in the southern Lau basin.

4 towards the deepest part of the Los Angeles Basin.

5 a injection in the Orange County Groundwater Basin.

6 pper Mississippi River and Western Lake Erie Basin.

7 lices are free to swap locally in the native basin.

8 ted watersheds such as the Mississippi River Basin.

9 rm, dry Mojave into the cooler, wetter Great Basin.

10 urring in coastal areas of the Mediterranean basin.

11 low, independent of the area of the drainage basin.

12 not compensate for the fast formation in the basin.

13 t trade winds in the tropical South Atlantic Basin.

14 rturning and its variability in the subpolar basin.

15 der control on the evolution of the drainage basin.

16 nd ~700 km along the western boundary of the basin.

17 ra-elongated shell was found in the Chindwin Basin.

18 ial, and municipal pumping within the Tulare basin.

19 in the Adriatic Sea, and the anoxic Cariaco Basin.

20 between sub-thermocline layers in the Panama Basin.

21 in the world, frequent in the Mediterranean basin.

22 entina and the Northwest Andes to the Amazon Basin.

23 le the effect of tree size varies across the basin.

24 ply explain the available data for the Laxmi Basin.

25 n the steep northern flank of the Hirondelle Basin.

26 cene pre-Columbian populations in the Amazon basin.

27 the Subtropical South Atlantic and Irminger Basin.

28 reducing future potential diversity in some basins.

29 conduits of microplastics to lake and ocean basins.

30 on on the soil water budget of salt-affected basins.

31 ous provinces into volatile-rich sedimentary basins.

32 to the gradual ventilation of the Nama Group basins.

33 buting to subsidence of flanking sedimentary basins.

34 d accelerated anthropogenic drought in these basins.

35 r from the western boundary into the eastern basins.

36 ate, largely limited to the Amazon and Congo basins.

37 ck Sea and the Adriatic Sea, but also within basins.

38 he upper Indus, Aral and Chu/Issyk-Kul river basins.

39 he exception of the water-limited arid river basins.

40 ns of the Arctic and of the Amazon and Congo basins.

41 n TNMEs ranging from 0.0093% to 0.38% across basins.

42 generation and expulsion in uplifted onshore basins.

43 s in the Pacific, Atlantic, and Indian Ocean basins.

44 estral benthic lineages in all major oceanic basins.

45 with meteorological drought indices in both basins.

46 ification has been documented in all oceanic basins.

47 sions, which are coeval with supradetachment basins.

48 use cyclone effects do differ across oceanic basins.

49 d to the variability of TC activity in these basins.

50 rom surface to depth, across different ocean basins.

51 he Amazon, Niger, Congo, Salween, and Mekong basins.

52 f and slope region with the eastern subpolar basins.

53 een rainfall, runoff and erosion in drainage basins(1-4).

54 n the east coast after leaving the Amazonian basin ~2,000 y before present; however, there is no cons

55 s triangulated upper cusps and lower talonid basin(3-5).

56 When analyzed by lymph node basin, 3302 basins were evaluated, and 38 were true posi

57 face warming throughout much of the Atlantic basin(9,12,17).

58 The Mojave, a warm desert, and the Great Basin, a cold desert, have distinct assemblages and meet

59 In the Los Angeles basin, a megacity that has pursued cleaner air for decad

60 Within basins, a random pattern of genetic patchiness was obser

61 ning groundwaters from the Upper Appalachian Basin (AB).

62 (n = 22) were assessed in the Arctic Central Basin (ACB).

63 to the decadal-scale variance of the Pacific basin, accounting for the largest fraction of the TPDV (

64 9 countries addressed 93 unique hydrological basins, accounting for 82.1% of global inland fish catch

65 Acoustic data from the Canada Basin Acoustic Propagation Experiment are discussed.

66 ature of the mantle beneath the southern Lau basin, adding new constraints on the displacement proces

67 still evident in the megabenthos of the Peru Basin after 26 years.

68 or towards the central Labrador and Irminger basins after flowing through the Charlie-Gibbs Fracture

69 Focusing on three representative river basins along the West Coast, we show that, while the dec

70 In the Congo Basin, an expansive network of streams and rivers transp

71 ructions for gages across the upper Missouri basin and an independent reconstruction of warm-season r

72 tization is not limited to the Mediterranean basin and can present diverse clinical phenotypes.

73 Continuation of this trend would deplete the basin and cause significant socio-economic challenges.

74 l and Moho topography map for the Tyrrhenian basin and its margins using ambient noise cross-correlat

75 impacts every year in the Ganges-Brahmaputra basin and Markazi basins is almost equal to an abnormall

76 nvironmental events across the Mediterranean Basin and Near East.

77 proposed right-lateral shear in the Northern Basin and Range adjacent to the Yellowstone hotspot.

78 ps the system stochastically escape from one basin and reach another to make transitions.

79 ically transforming the view that the Amazon basin and surrounding areas witnessed limited societal d

80 mal stratification patterns in a semi-closed basin and the assumed influence of isotopically depleted

81 na catchment area, including the Besos River basin and the Barcelona coast, and in the Ebro River Del

82 In the lower Mississippi river basin and the Cascades, the fraction can be as large as

83 .(4) Moreover, ancient genomes from the Yana basin and the Taimyr peninsula provided evidence of at l

84 the glacial meltwater recharging the closed-basin and well-sealed Lake Untersee largely determines t

85 in the marine Si budget like in the Cascadia Basin and which has to be considered in future investiga

86 esocosm experiments with those from 14 river basins and 22 cross-basin studies in Europe, producing 1

87 ecies undertake long migrations across ocean basins and remain in oceanic habitats for several years.

88 s for groundwater recharge through spreading basins and, with additional modification, other potable

89 boundary between orogenic (Natron and Magadi basins) and cratonic (Balangida and Manyara basins) lith

90 respect to sills bounding this semi-isolated basin, and reveal substantial corresponding changes in t

91 and tropical-extratropical stirring in that basin, and the resultant changes in the tropical atmosph

92 station and conversion to agriculture in the Basin are altering the current regime of terrestrial-to-

93 imates of natural climate variability in the basin are limited by the short observational record.

94 and Marcellus Shale Plays in the Appalachian Basin are the fourth and first largest natural gas produ

95 The Nordlinger Ries and the Steinheim Basin are widely perceived as a Middle Miocene impact cr

96 d landscapes, in which extensive valleys and basins are covered by ubiquitous fluvial plains.

97 although cleaning interactions in both ocean basins are ecologically analogous and result in parasite

98 to the natural gas supply chain, across all basins are ~4.8 times higher than those inferred from th

99 Based on datasets from 66 large rivers (basin area > 100,000 km(2)) worldwide, we identify 34 GI

100 nct from all other hominins from the Turkana Basin area as well as from the co-existing Theropithecus

101 nins and co-existing primates in the Turkana Basin area, circa 4 to 2 Ma.

102 Our approach can be applied to diverse basins around the world to reveal distribution patterns

103 F(ST) = 0.377), identifying the Indian Ocean basin as a barrier to dispersal.

104 ain Himalayan Thrust (MHT) into the foreland basin as an outer frontal thrust, and provide a modern s

105 t role in the carbon (C) cycle of the Amazon basin, as it transports and processes a significant frac

106 o elsewhere in the Ischigualasto-Villa Union Basin, as well as to the Parana Basin in Brazil.

107 vestigate the thermal history of sedimentary basins, as well as tectonic uplift and denudation rates.

108 aset to represent ice loss within the Wilkes Basin at MIS11.

109 ower planning, identification of species and basins at risk, and prioritization of restoration measur

110 ions from Andean, Himalayan, and New Guinean basins, avulsion style correlates with channel morpholog

111 entury, but the Mojave dried while the Great Basin became wetter.

112 ne (CH(4)) enters waters in hydrocarbon-rich basins because of natural processes and problems related

113 ecology is biased towards the North Atlantic Basin, because cyclone effects do differ across oceanic

114 of the Fundy, Deerfield, Hartford and Newark basins, both above and below the oldest CAMP flows in th

115 tana, to better understand the kinematics of basin bounding faults and their role in accommodating pr

116 dramatically affect the C cycle in the Congo Basin by reducing the downstream flux of stable, vascula

117 Joao de Castro seamount in the basin center indicating episodic volcanic activity along

118 e importance of atmospheric forcing of intra-basin circulation in determining the salinity of the sub

119 in the Nordic Seas via its regulation of the basin circulation plays a key role in activating an unre

120 vers the Amur Basin, rivers east of the Lena Basin, coastal basins of the Japan Sea, and the North Pa

121 and snowmelt peaks in the South Platte River Basin, Colorado, for three Salicaceae species that domin

122 om less urbanized environments in the Amazon basin compared to Araguaia.

123 c makes the TC activity indices over the two basins compensate each other, rendering the global TC ac

124 In the mid-latitude Baltoscandian Basin, conodonts displaying low delta(18)O values, which

125 essment using ArcGIS was conducted for river basins considering minimum and mean average discharge co

126 were observed over the deepest parts of the basin, consistent with the accumulation of emissions und

127 nd financial support, particularly if Amazon Basin countries are to achieve their commitments under t

128 oil and gas well pads in the western Permian Basin (Delaware Basin), using a mobile laboratory and an

129 d seismite horizons in North Alpine Foreland Basin deposits potentially related to both impacts.

130 lanted in a diseased field plot in the Great Basin Desert of Utah.

131 late the grounding line ice discharge of 176 basins draining the Antarctic Ice Sheet from 1979 to 201

132 and by the historical connection among river basins during Quaternary low-sea-level periods.

133 re-altered sagebrush ecosystems of the Great Basin ecoregion, western United States.

134 ontrolled directivity, and three-dimensional basin effects whereby energy was channeled towards the d

135 nt, more than one-third of terrestrial river basins (estimate based on the Food and Agriculture Organ

136 d at six sites in the Laurentian Great Lakes basin every 12 days from January to December 2017 (inclu

137 ribute that reflects the history of drainage basin evolution, so its form should be diagnostic of the

138 arger scale channel-morphology and long-term basin evolution, vital for understanding the past Martia

139 rface temperature increases across all ocean basins except the polar oceans.

140 he Indian Ocean by 2100, whereas polar ocean basins experienced a 20%-80% (+/-35%-200%) increase.

141 nce for the northeast migration of the Hadar Basin, extending the record of this lacustrine basin to

142 d flowback samples from the Denver-Julesberg Basin, finding that additions of oxidant enhanced haloge

143 tween flow and catch in a major Lower Mekong Basin fishery to propose a flow regime that they claim w

144 n riparian zones of the Lower Savannah River Basin, followed by cultivated crops and pasture/hay.

145 n Sea Polynya (ASP) serves as a natural test basin for assessing the fate of deep-DOC when it is supp

146 The Himalayan foreland basin formed by flexure of the Indian Plate below the ad

147 data show that the glendonites of the Danish Basin formed in waters below 5 degrees C, at water depth

148 until ~1.8 Ga, or ~2 Gyrs after the Caloris basin formed.

149 (~4.1 to ~3.94 Ga) when most Martian impact basins formed.

150 um coastal zone (BCZ) and the anoxic Gotland basin (GB).

151 nd associated low-flow conditions across the basin has increased substantially over the 20th and 21st

152 3 separate communities in Thailand's Salween basin have markedly increased fish richness, density, an

153 le chaotic terrains with no antipodal impact basins; hence a new geological explanation is needed.

154 ss fish deaths in Australia's Murray-Darling Basin highlight the need for improved conservation metho

155 6000 MTA target and help reduce its central basin hypoxia.

156 ta fallout produced by the antipodal Caloris basin impact.

157 We propose that basin-impact-generated hurricane-force winds created sed

158 -Villa Union Basin, as well as to the Parana Basin in Brazil.

159 The Salton Sea Basin in California suffers from poor air quality, and a

160 The Aral Sea basin in Central Asia and its major rivers, the Amu Dary

161 stosomiasis epidemic-the Lower Senegal River Basin in Senegal-intensive sampling revealed positive re

162 m the western boundary of Russia to the Lena Basin in Siberia.

163 In the Permian Basin in Texas and New Mexico, methane columns showed ma

164 subsequently accumulated in the northwestern basin in the absence of intense deep convective winters

165 urces for the Alabama-Coosa-Tallapoosa River Basin in the southeastern United States.

166 mide concentrations in the Monongahela River Basin in the water year (WY) 1998 (during a nationwide s

167 In the Uintah Basin in Utah, TROPOMI methane columns correlated with i

168 ogene of Tasmania; Late Cretaceous Gippsland Basin in Victoria; Paleocene and late middle Eocene of V

169 jectory space between high- and low-mobility basins in a set of model polymer freestanding films.

170 the Ganges-Brahmaputra in India and Markazi basins in Iran.

171 Basins in North America, and the La Plata and Nile River

172 ffusion is shown to arise from extended flat basins in the energy landscape and collective hopping be

173 tural gas liquid unloading activities for 18 basins in the United States in 2016.

174 e and the presence of landlocked extensional basins in thickened orogenic settings.

175 rbital-timescale changes in rate and type of basin infill will likely influence early rift sedimentar

176 TOAE from oxygenated habitats in the Iberian Basin, integrated with geochemical proxy data (delta(13)

177 and faults down to ~1200 m, showing that the basin is a half-graben with a southern depocenter driven

178 The (234)U accumulation within the Wilkes Basin is also observed in the McMurdo Dry Valleys brines

179 A strong TUTT in a basin is associated with enhanced RWB and tropical-extra

180 The Amazon Basin is experiencing climate change, altered hydrologic

181 The Amazon basin is home to numerous arthropod-borne viral pathogen

182 the Main Frontal Thrust (MFT), the foreland basin is typically portrayed as undeformed.

183 in the Ganges-Brahmaputra basin and Markazi basins is almost equal to an abnormally dry condition an

184 t move southward in the Irminger and Iceland basins is largely responsible for overturning and its va

185 an previous observations of methane in other basins, it is more prominent than that predicted by the

186 Kane Basin (KB) is one of the world's most northerly polar be

187 s Jinju Formation (Sindong Group, Gyeongsang Basin) Korea is the largest yet reported from the Cretac

188 d fishery pressures in June and July 2020 to basin-level inland fishery experts (i.e., identified by

189 The average delta(13)C(CH4) weighted by US basin-level measured emissions in 2015 was -41.8 per mil

190 ty data reported to the GHGRP, including 319 basin-level reports, covering 15,895 reported compressor

191 s of Rhuddanian black shales from the Murzuq Basin, Libya.

192 basins) and cratonic (Balangida and Manyara basins) lithosphere from north to south.

193 ed light on the interplay between tectonics, basin migration and faunal change on the one hand and th

194 e of shallow-marine sediments from Whanganui Basin, New Zealand.

195 Thus, results suggest that the Cariaco Basin nitrogen cycle is influenced by autotrophic carbon

196 tewater characteristics sampled at the inlet basin of a sewage treatment plant (STP).

197 dwater wells located in the Denver-Julesburg Basin of Colorado, a rapidly urbanizing area with active

198 mass predictor in the portion of the western basin of Lake Erie represented by these sampling station

199 o small agricultural streams in the drainage basin of Lake Erie, a large, eutrophic lake experiencing

200 aknesses, and long-term dynamics in terms of basins of attraction and sink components.

201 s throughout the water column from the major basins of each lake in spring and summer over 2 years.

202 ggest ancient connections between freshwater basins of East Asia and Europe near the Cretaceous-Paleo

203 of the global pandemic and 2) identify that basins of higher provisioning value are perceived to exp

204 2008 levels entering the western and central basins of Lake Erie to achieve a 6000 MTA target and hel

205 were identified in the densely populated air basins of San Francisco Bay Area, San Joaquin Valley, an

206 asin, rivers east of the Lena Basin, coastal basins of the Japan Sea, and the North Pacific Islands.

207 18-year hydrochemical dataset for eight sub-basins of the Panama Canal Watershed of high-temporal fr

208 ofile implies that the 35 km-wide Hirondelle Basin opened after this time along normal faults.

209 bed waters (for example, the Central Pacific Basin) or in cold waters subject to high human pressures

210 h include this epoch's most extensive circum-basin outcrops.

211 ime of soil carbon in the Ganges-Brahmaputra basin over the past 18,000 years.

212 occurred across this highly productive ocean basin over the past two centuries.

213 ft show 10s-100s of kyr cyclic variations in basin paleoenvironment as eustatic sea level fluctuated

214 face temperatures, globally and by ocean sub-basins, particularly between the tropical Atlantic tempe

215 chinochloa crus-galli from the Yangtze River basin phenotypically and by genome resequencing, and we

216 source of almost 50% of Lake Erie's Western Basin phosphorus load.

217 n age and that the purported turnover in the basin preceded the end-Permian marine event by over 300

218 in poorly characterised offshore sedimentary basins prior to exploratory drilling.

219 The Amazon river basin receives ~2000 mm of precipitation annually and co

220 al pedogenic carbonates preserved in Neogene basins record a general increase of delta(18)O and delta

221 wn earthquake within the central Los Angeles Basin region.

222 to climate change vary greatly between ocean basins, regions and species, there is compelling evidenc

223 netary scale and the typical extent of ocean basins, respectively.

224 glacials, the ice sheet margin at the Wilkes Basin retreated to near the precipitate location, about

225 k grape varieties grown in the Mediterranean basin reveal an insufficient accumulation of anthocyanin

226 ccession at Izola mensa within the NW Hellas Basin rim.

227 nd subregion with 10 species covers the Amur Basin, rivers east of the Lena Basin, coastal basins of

228 Our examination of the Caloris basin's antipodal chaotic terrain reveals multi-kilomete

229 80 km depth affecting much of the Tyrrhenian basin's uppermost mantle structure and its extension mim

230 ineral deposits can yield a new paradigm for basin scale hydrocarbon exploration.

231 n level and vegetation salt tolerance at the basin scale, which would be difficult to assess through

232 have so far not been determined at the ocean-basin scale.

233 cal index values reflect different states of basin-scale climate over time.

234 Ultimately, basin-scale dam planning that considers GHG emissions al

235 surements, we introduce a method that infers basin-scale deep-ocean temperature changes from the trav

236 This acts in opposition to decreasing basin-scale wind stress and has a potentially important

237 ity in observed sea level on both global and basin scales, which we reconstruct from tide-gauge recor

238 es County that is within the South Coast Air Basin (SCLA).

239 Locomotor modes are attracted to landscape basins separated by potential energy barriers.

240 central TRBs since 1951, while the southern basins show an insignificant trend.

241 vents by decreasing runoff efficiency in the basin since the late 20th century (1980s) onward.

242 reased globally (0.4% per year) and by ocean basins since 1948.

243 , respectively) biogeochemistry in the Congo Basin, six lowland streams that drain catchments of vary

244 the Lystrosaurus Assemblage Zone (AZ; Karoo Basin, South Africa) is time equivalent with the marine

245 Chinook salmon populations in the Cook Inlet basin, southcentral Alaska, using a hierarchical Bayesia

246 dual power plants; oil and gas emissions are basin-specific.

247 s for all land-falling or near-land Atlantic basin storms, covering 1996-2011 for all metrics and up

248 minated facies commonly observed in foreland basin stratigraphy.

249 with those from 14 river basins and 22 cross-basin studies in Europe, producing 174 combinations of p

250 work and demonstrate its use for the Cariaco Basin subeuphotic zone, one of the largest anoxic marine

251 Within the Wilkes Basin, subglacial chemical precipitates of opal and calc

252 e neighbouring uplands were not uplifting or basins subsiding, alluvial fans are absent, but in these

253 uce both methane and VOCs in oil and wet gas basins, such as the Eagle Ford.

254 e calculations, constrained by modern anoxic basins, suggest that deep-water phosphate concentrations

255 yclone intensification rates in the Atlantic basin that are highly unusual compared to model-based es

256 uptions in the highest reaches of the Amazon Basin that were caused by a weakening of the SASM during

257 ves & gastropods) isotope data from 25 river basins that have stream water isotope values, water temp

258 els also suggested upstream gene flow within basins that likely occurred through anemophilous and ent

259 CA3 of aged rats may create weaker attractor basins that promote abnormal, bistable representations u

260 is the highest, and also are found in river basins that were historically connected.

261 ove and below the oldest CAMP flows in these basins, that demonstrate that these anomalies are more c

262 on of genetic diversity within a major ocean basin (the Atlantic), a regional rookery (Cabo Verde Arc

263 Across the Upper Missouri River Basin, the recent drought of 2000 to 2010, known as the

264 sin, extending the record of this lacustrine basin to Mille-Logya.

265 rd of TWS for nine major transboundary river basins (TRBs) in Africa.

266 ployed in a field campaign in the Eagle Ford basin, TX.

267 he North China Type, the Lower Yangtze River Basin Type, the Southwest Type, the Plateau Type, and th

268 Devonian Marcellus Shale in the Appalachian Basin, USA, contain high levels of total dissolved solid

269 nd G. robusta) endemic to the Colorado River Basin using ddRAD sequencing of 368 individuals.

270 pads in the western Permian Basin (Delaware Basin), using a mobile laboratory and an inverse Gaussia

271 marine ecosystems from the Iberian Atlantic basin, using cetaceans as bioindicators.

272 ne, suboxic, and anoxic zones of the Cariaco Basin, Venezuela.

273 We propose the oldest lineage entered the basin via the isthmus of Panama and sequentially establi

274 anbedr (Mochras Farm) borehole, Cardigan Bay Basin, Wales, United Kingdom.

275 During glacials, the basin was isolated from the ocean, and sedimentation rat

276 In two study sub-regions in the Los Angeles Basin, we examined the effect of outdoor residential wat

277 Per river basin, we quantified a connectivity index (CI) for each

278 al otolith (ear stone) growth from two ocean basins, we tested whether parrotfish growth was enhanced

279 otopic dates over this interval in the Karoo Basin were limited to one high resolution ash-fall depos

280 When analyzed by lymph node basin, 3302 basins were evaluated, and 38 were true positive (1.2%).

281 llectively, climate-induced changes in Great Basin wetlands suggest a major shift in freshwater ecosy

282 er from those observed elsewhere in the same basin, where environmental controls on the underlying av

283 ansmission pockets persist across the Amazon Basin, where Plasmodium vivax is the predominant infecti

284 nhabit preferentially lowland areas of river basins, where hydrological connectivity is the highest,

285 erranean resembled modern, highly stratified basins, whereas no modern analog exists for OAEs.

286 hat these channel floors occur within a vast basin, which separates the downstream reaches of numerou

287 s with regional sea-surface temperatures and basin-wide gyre circulation strength over recent decades

288 The Chesapeake Basin-wide Index of Biotic Integrity, a benthic macroinv

289 Basin-wide methane emission rates were estimated for the

290 ow that, in addition to the reduction of the basin-wide model biases by the assimilation of the clima

291 ical monthly mean Argo data to constrain the basin-wide model biases.

292 e opposing impacts on fire, including higher basin-wide precipitation and increased drought frequency

293 ross the deglaciation period, a depletion of basin-wide soil carbon stocks was triggered by increasin

294 itate jaguar dispersal from and to Cockscomb Basin Wildlife Sanctuary.

295 otopes that have been documented in an ocean basin (with (206)Pb/(204)Pb ratios of 19.9-21.7) using h

296 hotic zone, one of the largest anoxic marine basins worldwide.

297 ophic surface ocean conditions in restricted basins would prompt shoaling of anaerobic ammonium oxida

298 from O&G facilities in the Upper Green River Basin, Wyoming.

299 d deforestation and settlement in the Amazon basin, yet evidence of a deforestation-driven increase i

300 riculture in the snow-dependent Yakima River Basin (YRB) in the Pacific Northwest United States.