ライフサイエンスコーパス: riverine

1 ilica, respectively, which are comparable to riverine and atmospheric inputs.

2 ly driven by differences in productivity and riverine and coastal influence.

3 ecological phase involves a transition from riverine and deltaic environments to marine ones, concom

4 ated in situ sensors deployed in contrasting riverine and estuarine environments.

5 frequently ingested, and appear to have both riverine and estuarine inputs, since they were ingested

6 sk in the Amazonian human population, mainly riverine and indigenous communities.

7 ation change experiment, and also applied to riverine and marine DOC.

8 radiogenic (Delta(14) C) isotopes that trace riverine and marine organic matter sources as they are p

9 onriverine sites was high in comparison with riverine and mixed geomorphic settings, with sites close

10 ological system, with major implications for riverine and near-shore marine environments.

11 atively high variation in OC storage between riverine and nonriverine geomorphic settings indicates t

12 lements (e.g., Al, Fe, Ti) far exceed global riverine and open ocean mean values and highlight the im

13 Direct comparison of riverine and reservoir reaches, where sedimentation in t

14 Also, wetlands experiencing more (riverine and tidal) hydrologic exchange recovered more r

15 lerae, an autochthonous member of estuarine, riverine, and marine habitats and the causative agent of

16 ling a significant mid-20th-century surge in riverine barium levels, and a gradual lag within records

17 s and small mammals indicate that a putative riverine barrier (the Jurua River) does not relate to pr

18 Wallace's (1854) Riverine Barrier hypothesis is one of the earliest expla

19 ocene marine incursion, Pliocene/Pleistocene riverine barriers and Pleistocene refugia.

20 has systematically evaluated the impact that riverine barriers might have on structuring whole Amazon

21 and well-dispersed Amazon tree is impeded by riverine barriers, though this has not yet resulted in s

22 rovides early and rare evidence of intensive riverine-based foraging aided by the likely adoption of

23 The riverine bicarbonate flux originates mainly from the dis

24 y of this marine reserve network paradigm to riverine biodiversity and inland fisheries remains large

25 -native species should be managed to protect riverine biodiversity and maintain the provision of ecos

26 es are a key, but understudied, component of riverine biogeochemical function.

27 Riverine biological processes could potentially be respo

28 apanese macaques hunt fish and collect these riverine biota by extensively observing their behavior,

29 thesis of climate- and LU-induced effects on riverine biota with respect to changes in species therma

30 cessible for Japanese macaques to search for riverine biota.

31 Riverine bluff areas also appeared less heavily occupied

32 f some elements contributed significantly to riverine budgets (e.g., 24% for Zn, 50% for P, and 83% f

33 termediate reservoir, then the importance of riverine carbon in the ocean carbon cycle has been under

34 alter the timing and spatial distribution of riverine carbon sequestration and greenhouse gas emissio

35 Our estimates of riverine carbon storage represent a previously undocumen

36 Riverine CH(4) emissions are not strongly temperature de

37 the implications of temporal changes in the riverine chemical weathering flux for oceanic geochemica

38 ogeographical evidence suggesting that these riverine cichlids are products of a recent adaptive radi

39 flows and fragmented habitats often simplify riverine communities and favor non-native fishes, but th

40 conducted between May and July 2015 in four riverine communities in Mazan district.

41 lian population, including urban, rural, and riverine communities representing diverse ethnic backgro

42 support a "nodal" or heterogeneous model of riverine community organization across a particularly ex

43 in carbon storage; and historical changes in riverine complexity have likely reduced carbon storage.

44 Riverine concentrations of dissolved and particulate org

45 he majority of the reservoir area maintained riverine conditions, the lateral valleys formed upon bac

46 By applying a new method to quantify riverine connectivity and map FFRs, we provide a foundat

47 ics, which is reflected in the delta(15)N of riverine consumer tissues.

48 algae are a more nutritional food source for riverine consumers than leaf litter.

49 This isotopic discrepancy indicates most riverine DBC is sequestered and/or rapidly degraded befo

50 allenge in constraining the flux and fate of riverine DBC is to develop targeted and accurate quantif

51 delivery from major rivers(8,9), sinking of riverine deltas(8,10), increased coastal erosion and sea

52 ne deposition rate is overestimated, whereas riverine deposition is underestimated by at least an ord

53 fluents made only a moderate contribution to riverine discharge (21% for PFOA, 6% for PFOS), while at

54 mples from the Mackenzie River plume suggest riverine discharge as an OPE source to the Canadian Arct

55 ivity maxima and increased precipitation and riverine discharge from northern South America are close

56 d polyfluoroalkyl substances (PFASs) through riverine discharge into coastal waters.

57 Global riverine discharge of organic matter represents a substa

58 Inputs (from riverine discharge, atmospheric deposition, coastal wast

59 be equal or larger by a factor of 16 to the riverine discharge.

60 estrial and marine net primary productivity, riverine dissolved and suspended matter fluxes to the oc

61 Riverine dissolved carbon (DC) plays a crucial role in g

62 ssolved carbon and nitrogen, indicating that riverine dissolved components could be used to scale GHG

63 ived from on-ground soil flux (n = 1558) and riverine dissolved gas concentration (n = 332) measureme

64 uch low N(2)O fluxes are associated with low riverine dissolved inorganic N (DIN) after terrestrial p

65 comparable to, or higher (~2-fold) than, the riverine dissolved input.

66 Riverine dissolved organic carbon (DOC) contains charcoa

67 Our study indicates that riverine dissolved P input and marine P biological utili

68 te weathering fluxes are calculated based on riverine dissolved sodium (Na(+)) from silicate minerals

69 Riverine dissolved sulfate (SO4(2-)) flux and sulfur sta

70 ue can be successfully applied to marine and riverine DOC without further sample pretreatment.

71 ic input will drive substantial variation in riverine DOM and, thus, estuarine optics and photochemis

72 Determining the molecular composition of riverine DOM is essential for understanding its source,

73 in APPI resolved subtle differences between riverine DOM that was absent from ESI.

74 including a fragmentation study of THF-doped riverine DOM using infrared multiple photon dissociation

75 MS spectra and assessed its robustness using riverine DOM.

76 at the genetic structure would correspond to riverine drainage basins.

77 historic as well as present-day patterns of riverine drainages.

78 underappreciated interannual variability of riverine DSi fluxes.

79 zone biogeochemistry and its influence over riverine ecosystem function.

80 has been found to have an adverse effect on riverine ecosystem health, and the livelihoods of the co

81 edictions of the effects of global change on riverine ecosystem processes.

82 ion people that live in drylands and rely on riverine ecosystem services.

83 regional development, GIWs exploitation, and riverine ecosystem, we reveal the global diversity and e

84 ers (Lontra canadensis) are top predators in riverine ecosystems and are vulnerable to per- and polyf

85 Riverine ecosystems have adapted to natural discharge va

86 genes (ARGs) in the Ganges relative to other riverine ecosystems in Europe, North and South America.

87 though the importance of these subsidies for riverine ecosystems is increasingly recognized, little i

88 Global models of riverine ecosystems need to better represent ammonia-der

89 onal forest ecosystems and here in dendritic riverine ecosystems suggests the possible application of

90 ironmental consequences of deploying VATs in riverine ecosystems to meet current and future energy ne

91 namic way to create spatial heterogeneity in riverine ecosystems, and provides a means to detect spat

92 eshwater mussels (Unionidae) are integral to riverine ecosystems, playing a pivotal role in aquatic f

93 avigation without compromising the health of riverine ecosystems.

94 ge estimates indicated continued substantial riverine emissions of long chain (C7-C12) PFCAs in the p

95 Incorporated with riverine emissions, this study indicates that N(2)O emis

96 Past shifts in connectivity in riverine environments (for example, sea-level changes) a

97 focus on denitrification in groundwater and riverine environments as a dominant source of riverine N

98 In general, rotifers were more abundant in riverine environments than lakes and reservoirs.

99 Riverine environments, such as streams and rivers, have

100 semiaquatic and lived in freshwater swamp or riverine environments, where they grazed on freshwater v

101 atterns of fish distributions in schools and riverine environments.

102 at modifying the supply of organic matter to riverine, estuarine, and coastal food webs need to incor

103 lerae, has been shown to be autochthonous to riverine, estuarine, and coastal waters along with its h

104 g achieves reliability in predicting extreme riverine events in ungauged watersheds at up to a five-d

105 that, including particulate BC fluxes, total riverine export amounts to 43 +/- 15 Tg BC year(-1) (12

106 Riverine export of particulate organic carbon (POC) to t

107 ogenic activities are subject to hydrologic (riverine) export, causing water quality problems in down

108 Atmospheric mercury (Hg(0), Hg(II)) and riverine exported Hg (Hg(II)) are proposed as important

109 cation has resulted in increased base-cation riverine exports (Ca(2+), Mg(2+), Na(+), K(+)) correlate

110 lthough local and basin-scale differences in riverine fish diversity have been analysed as functions

111 ts that connectivity is the key component of riverine fish geographic range sizes, independent of any

112 re, we linked a multicontinental database of riverine fish population abundance time series collected

113 Riverine fish showed elevated heavy metal levels as comp

114 the spatial distribution and richness of 131 riverine fish species were investigated at 1481 sites in

115 ns may provide suitable habitats for several riverine fish species.

116 ow and water temperature extremes to ~11,500 riverine fish species.

117 (scales) and highest 321.83 mg/kg (Liver) in Riverine Fish, whereas in farms fish As ranged lowest fr

118 nce among spatially separated populations of riverine fish.

119 Here, we derive a gridded global map of riverine fisheries and assess its implications for biodi

120 Here we analyze a case-study of riverine flood risk management using a multi-objective r

121 ent, which commonly occurs as contaminant in riverine floodplains and associated wetlands affected by

122 Riverine floodplains exhibit high floral and faunal dive

123 ersity to environmental gradients across ten riverine floodplains with differing degrees of flow alte

124 ated by an increase in the Fe:S ratio of the riverine flux after Sturtian glacial removal of a long-l

125 We contend that the riverine flux obtained from observations of modern river

126 n tons per year, which is ~10% of the global riverine flux of dissolved organic carbon (DOC).

127 nto account during the interpretation of the riverine flux of Fe isotopes to the ocean or tracing wea

128 gical pump efficiency and silicate-carbonate riverine flux).

129 we quantify the global impact of dams on the riverine fluxes and speciation of the limiting nutrient

130 solute fluxes represent, at a minimum, 5% of riverine fluxes for Li, Mg, Ca, Sr, and Ba.

131 consideration of the temporal variability in riverine fluxes largely ameliorates long-standing proble

132 Riverine fluxes of carbon and inorganic nutrients are in

133 long been assumed static and subordinate to riverine fluxes, if not neglected entirely, in marine is

134 TMF values of the parent compound only in a riverine food web.

135 tes of terrestrial organic C, which supports riverine food webs and is a source of CO2, are lacking.

136 ncorporation of allochthonous subsidies into riverine food webs.

137 ks, our framework facilitates predictions of riverine [Formula: see text] emissions globally using wi

138 f concentrations contributing 45-100% of the riverine fraction to the southern and outer estuary.

139 can thus be utilized to determine changes in riverine fresh water discharge.

140 (EEA), reveal centennial-scale variations of riverine freshwater input that are synchronous with nort

141 e show that allometric scaling of cumulative riverine function with watershed area ranges from linear

142 tion within nonriverine settings, but not in riverine geomorphic settings.

143 rofound implications for water resources and riverine habitats.

144 Here, we analyze riverine heat wave events by training one single deep le

145 Riverine heat wave events have increased at double to qu

146 Riverine heat wave trends are driven predominantly by cl

147 Analysis of riverine heat waves has been hindered by fragmented data

148 Rising riverine heat waves have outpaced those of air heat wave

149 lish a contemporary (2012-2017) benchmark of riverine Hg export.

150 M(1.) Concentrations peaked near a turbulent riverine hotspot, particularly at night when intensified

151 the stability constants previously found for riverine HS in temperate estuaries and HS standard mater

152 has been well characterized, ASGM impacts on riverine hydrological properties are less understood.

153 Predicted increases in riverine hypoxia via eutrophication and increased temper

154 es, whether they be atmospheric, oceanic, or riverine in origin.

155 erine settings along with those with reduced riverine influence located on tide-dominated sand island

156 ments were ingested in habitats with greater riverine influence, the opposite was observed for shorte

157 In particular, our results enable changes in riverine input along geological to perennial time scales

158 The riverine input of fine particles played an important rol

159 ming, decline in sea ice extent, increase in riverine input, ocean acidification and changes in prima

160 mercury observed in atmospheric deposition, riverine input, seawater, freshwater lakes, and freshwat

161 sea ice-modified atmospheric deposition and riverine input.

162 spheric deposition while CH is influenced by riverine input.

163 Riverine inputs of Hg to the North Atlantic have decreas

164 is, values on the same order of magnitude as riverine inputs of P and N to the MS.

165 e observed in coastal waters receiving major riverine inputs of terrestrial CDOM (0.06-0.5 m(3) (mol

166 hese clones were from sites far removed from riverine inputs, suggesting a wide diffusion of pathogen

167 astal and shelf areas that are influenced by riverine inputs.

168 duction, biological activity, transport, and riverine inputs.

169 on freshwater biota, including brown trout, riverine insects and molluscs, in Chubu Sangaku National

170 ractions between hydrological hazards (e.g., riverine inundation during periods of heavy rainfall), e

171 cosystems, our results clearly indicate that riverine iron fluxes need to be accounted for as the vol

172 ogical patterns in realistic terrestrial and riverine landscapes.

173 fringe mangroves in the Coral Triangle, and riverine mangroves in the Strait of Malacca, between the

174 tspot of diversity of onchidiid slugs in the riverine mangroves of the Strait of Malacca indicates th

175 ) and ~4 times higher than major non-glacial riverine means (~500 Sigma*meq(+) m(-2) year(-)(1)).

176 mates of global silicate fluxes derived from riverine measurements.

177 Results show a projected 10-fold increase in riverine MeHg levels and a 2.6-fold increase in estuarin

178 Yet estimates of Arctic riverine mercury (Hg) export constrained from direct Hg

179 Human activities have elevated riverine mercury budgets by two to three times in the pr

180 Riverine mercury export to AO is estimated at 50 Mg yr(-

181 Establishing a baseline riverine mercury level, our findings reveal rapid respon

182 d could be used to inform targets for global riverine mercury restoration.

183 evel, our findings reveal rapid responses of riverine mercury to human perturbations and could be use

184 Russian rivers are the predominant source of riverine mercury to the Arctic Ocean, where methylmercur

185 ems, including individual trees and forests, riverine metabolism, and river network organization.

186 the modelled contribution of terrestrial and riverine microplastic to the world's oceans.

187 between large-scale wastewater discharge and riverine microplastics (p < 0.05).

188 (3) The alloy exhibits an unusual riverine microstructure of martensite not seen in other

189 Rather, the shift from alongshore sandy to riverine muddy sediment supply was the key driver.

190 During summer flow recession, riverine N concentrations wane and Cladophora becomes de

191 U.S. watersheds and tested against available riverine N flux estimates.

192 connectivity in observations and modeling of riverine N(2)O emissions may result in significant under

193 Current models of riverine N(2)O emissions place a strong focus on denitri

194 ays for accurately estimating and predicting riverine N(2)O emissions.

195 ctivity, control the sources and dynamics of riverine N(2)O in a mesoscale river network within the U

196 iverine environments as a dominant source of riverine N(2)O, but do not explicitly consider direct N(

197 Riverine N2 O emission estimates will be further enhance

198 Previous studies may overestimate global riverine N2 O emission rates (300-2100 Gg N2 O-N yr(-1)

199 de the best fit between modeled and observed riverine N2 O emission rates (EF(a): R(2) = 0.92 for bot

200 from published literature to estimate global riverine N2 O emission rates and emission factors.

201 Global riverine N2 O emission rates are forecasted to increase

202 ads for 6400 rivers, models estimated global riverine N2 O emission rates of 29.6-35.3 (mean = 32.2)

203 Riverine N2 O flux was significantly correlated with NH4

204 ture of [Formula: see text] production along riverine networks, our framework facilitates predictions

205 tions of [Formula: see text] emissions along riverine networks.

206 allows examination of the impact of imposing riverine nitrate-N load limits on the biofuel production

207 a in the northern Gulf of Mexico by reducing riverine nitrate-N loads represent two such cases that o

208 l agricultural activities strongly influence riverine nitrogen (N) dynamics, which is reflected in th

209 icultural intensification have led to raised riverine nitrogen (N) loads, widespread oxygen depletion

210 ANI has been shown to be a good predictor of riverine nitrogen export.

211 Long-term records of riverine nitrogen fluxes are nonexistent and drivers of

212 r networks and improving estimates of global riverine nitrogen loads.

213 Global riverine nitrous oxide (N(2)O) emissions have increased

214 Estimates of global riverine nitrous oxide (N2 O) emissions contain great un

215 trations on the shelf in response to varying riverine nutrient and organic carbon loads, boundary flu

216 Sea surface warming and reduced riverine nutrient inputs are found to be likely contribu

217 dsummer hypoxic areas were most sensitive to riverine nutrient loads and sediment oxygen demand from

218 them to settle and thrive along the shifting riverine oases of the Taklamakan Desert.

219 kes up much of the DOC and particulate OC of riverine OC (along with soil OC), why do we not see more

220 ted at least two ecotypes-coastal marine and riverine-of Antillean manatees.

221 enzymatic processes in the mineralization of riverine OM: (i) the role of phenol oxidase activity in

222 For example, riverine organic matter assimilation by the glacier-nest

223 r runoff, but the influence of the influx of riverine organic matter on the trophodynamics of coastal

224 issues of marine consumers, estimates of the riverine organic matter source contribution to upper tro

225 We quantified the ecological impact of riverine organic matter subsidies to glacier-marine habi

226 Riverine organic matter supports of the order of one-fif

227 found in the open lake is not simply diluted riverine organic matter.

228 ed geomorphic settings, with sites closer to riverine outflow from the east and south of Moreton Bay

229 to calculate PFAA atmospheric inputs to and riverine outputs from the catchments.

230 lly depending on the type of flooding (e.g., riverine, overbank, coastal).

231 ering of newly P-rich crust led to increased riverine P fluxes to the ocean.

232 ogeneity in controlling processes, including riverine particulate material loads, historically changi

233 bon (delta(13) C-DIC; 1977-2014), marine and riverine particulate organic carbon (delta(13) C-POC; 19

234 tional genes also showed clear backwater and riverine patterns.

235 ted using sedimentation traps from different riverine points in Germany.

236 This riverine population of approximately 5000 individuals is

237 netic structure and demographic processes in riverine population of fishes.

238 To predict thermal impacts on migratory riverine populations, we first expanded a spatial stream

239 However, contributions of riverine processing are poorly constrained at continenta

240 understanding of basal resources supporting riverine productivity.

241 thin paleodrainages can be explained by past riverine properties (i.e., area and number of rivers in

242 Our findings extend the influence of current riverine properties on genetic diversity to those associ

243 ict differences in ecological benefits among riverine reserves.

244 the order of hours, days, and a week for the riverine, river-impacted, and open lake waters, respecti

245 based on their absorbance properties (a300): riverine, river-impacted, or open lake sites.

246 Ca and (87)Sr/(86)Sr to serve as proxies for riverine runoff and highlights the spatiotemporal comple

247 Atmospheric deposition and riverine runoff have been traditionally considered the m

248 t worldwide coastal eutrophication fueled by riverine runoff of fertilizers and the burning of fossil

249 identify the spatiotemporal distribution of riverine runoff.

250 Suspended particulate matter (SPM) from 13 riverine sampling sites of the German Environmental Spec

251 with around 5.7 times increase in the total riverine sediment flux sustained over that time.

252 However, riverine sediment fluxes after earthquakes remain poorly

253 Shanghai and Jiangsu areas, which differ in riverine sediment supply and tidal flat management patte

254 s worldwide suggest that roughly half of the riverine sediment supply is delivered to terrain that un

255 bility of coral Ba/Ca records as proxies for riverine sediment, we extend these records to the late n

256 t geomorphological settings (wetlands within riverine settings along with those with reduced riverine

257 near sediment-water interfaces in marine and riverine settings are known to act as a sediment trap fo

258 indicators of N loading might be accurate in riverine settings, but could be inaccurate when consider

259 By leveraging data for 13,069 riverine sites from temperate, subtropical, and boreal c

260 ) groups involved in nitrogen cycling in the riverine sites, suggesting a higher level of bacterial a

261 functionally different between backwater and riverine sites, which represent communities with and wit

262 horhynchus sp. from differently contaminated riverine sites.

263 pristine preindustrial natural baselines of riverine SO4(2-) flux and delta(34)S cannot be directly

264 e white-throated dipper (Cinclus cinclus), a riverine songbird, modulates both acoustic and visual si

265 lable dissolved organic carbon from external riverine sources supports a large component of ecosystem

266 MeHg in two riparian spiders is derived from riverine sources while approximately 45% of MeHg origina

267 , Lake Victoria), and Astatotilapia burtoni (riverine species around Lake Tanganyika).

268 palis gambiensis (Diptera: Glossinidae) is a riverine species that is still present as an isolated me

269 fy coastal evacuations by otherwise resident riverine striped bass in the Hudson River Estuary, New Y

270 Riverine sul1 correlated with upstream capacities of ani

271 Afterwards, a substantial accumulation of riverine suspended OM (>=50% of the channel's volume) bo

272 In a riverine system, microplastics can enter from different

273 in the flushing of soil assemblages into the riverine system.

274 However, the direction of range shifts in riverine systems is less clear.

275 Cores collected from large-scale riverine systems with many wastewater sources recorded i

276 rities of environmental variation regimes in riverine systems, and reveal a strong human fingerprint

277 hin grid cells and the potential C export to riverine systems, in a way to be conservative in a mass

278 eltwaters compared with seawater and typical riverine systems, together with the likely sensitivity t

279 Riverine systems, where groundwater mixes with surface w

280 large-scale spatial biodiversity patterns in riverine systems.

281 lity and availability of aquatic habitats in riverine systems.

282 nments, except for substantial enrichment in riverine systems.

283 lop a global model to simulate preindustrial riverine total mercury and assess human perturbations by

284 t societal choices will substantially impact riverine total nitrogen loading (+54% to -7%) for the co

285 one will substantially increase (19 +/- 14%) riverine total nitrogen loading within the continental U

286 Riverine transport of iron (Fe) and arsenic (As) is affe

287 ion, is the main driver behind PAC input and riverine transport, as supported by (i) discrepancies in

288 e focused on Glossina palpalis gambiensis, a riverine tsetse species representing the main vector of

289 , and appeared similar to small terrigenous (riverine) UDOM even in marine water.

290 t shrublands, which may indicate that global riverine uptake of carbon dioxide is higher than hypothe

291 rates were relatively high when compared to riverine uptake, especially during the spring and summer

292 and plant CO2 fertilization to increases in riverine water and carbon export from this large region

293 sis of certified reference materials (SLRS-4 Riverine water and NIST SRM 1515 Apple leaves).

294 ngs highlight the degree to which changes in riverine water and sediment discharge can be related wit

295 Moreover, microplastic concentrations in riverine water column remain underexplored.

296 first 6 weeks after the flooding, inflowing riverine water dominated the emissions over in-channel c

297 h-to-north advection and dilution with fresh riverine water enroute, and/or lower production in the n

298 ts suggest that the addition of aerosols and riverine water stimulate the biological utilization of D

299 entified as a biological component linked to riverine water, and temperature seasonality.

300 ention, boosting carbon sequestration across riverine wetlands.