ライフサイエンスコーパス: estuary

1 tal Shelf, Sao Sebastiao Channel, and Santos Estuary).

2 ulation in fishes from the San Francisco Bay Estuary.

3 as the numerous other sources of PCBs to the estuary.

4 g the bioaccumulation at another site in the estuary.

5 ronmental variation in the San Francisco Bay Estuary.

6 times higher than in the saline mouth of the estuary.

7 tions in a wetland-influenced region of this estuary.

8 pected of impacting the water quality of its estuary.

9 009 to the East China Sea off the Changjiang Estuary.

10 d test was conducted in the Delaware Bay and Estuary.

11 level of sewage contamination in the Santos Estuary.

12 ced population densities in the contaminated estuary.

13 ounted for up to 20% of the MeHg flux to the estuary.

14 sh restorations throughout the San Francisco Estuary.

15 s (Callinectes sapidus) in the Passaic River estuary.

16 s from the coastal ocean to the subterranean estuary.

17 nitrogen attenuation within the subterranean estuary.

18 from killifish subpopulations throughout the estuary.

19 es through a case study in the Yangtze River estuary.

20 ucers in this relatively long residence-time estuary.

21 t the cycling of PCBs in a typical urbanized estuary.

22 mixing in the shallow, eutrophic Peel-Harvey Estuary.

23 nt to a tidal creek of a Spartina -dominated estuary.

24 s of this highly macrotidal sediment starved estuary.

25 ores collected from the northern side of the Estuary.

26 ture from sediments of the San Francisco Bay estuary.

27 ses was low (~10-30 %) throughout the entire estuary.

28 es dominated higher salinity sections of the estuary.

29 er quality objectives for the Chesapeake Bay estuary.

30 of a substantial load of trace metals to the estuary.

31 genically labeled sediments elsewhere in the estuary.

32 ast water exchanges that dissipate along the estuary.

33 an, with one ecotype confined near the river estuaries.

34 wind wave growth in fetch and depth limited estuaries.

35 tin photodegradation during transport within estuaries.

36 e progress toward improving water quality in estuaries.

37 ydrodynamically complex environments such as estuaries.

38 lly lethal levels of pollution in four urban estuaries.

39 in the Ajkwa Estuary compared to neighboring estuaries.

40 ux and 49% of the fluvial MeHg flux into GOM estuaries.

41 ver of biotic communities in river-dominated estuaries.

42 y correlated with the growth of juveniles in estuaries.

43 ed nitrous oxide (N2O) comes from rivers and estuaries.

44 from marsh habitats to deep-water refugia in estuaries.

45 sure pathways in five Northeast coast (U.S.) estuaries.

46 offshore transport across different types of estuaries.

47 tial changes such as peatlands, marshes, and estuaries.

48 ons on the methylation rates across multiple estuaries.

49 tamination along the Gulf coast in sensitive estuaries.

50 atter does not hinder mercury methylation in estuaries.

51 atchments to larger river systems, lakes and estuaries.

52 for aquatic toxicities in urban streams and estuaries.

53 time scales that are relevant to rivers and estuaries.

54 ological connectivity between watersheds and estuaries.

55 nd denitrification in rivers, reservoirs and estuaries.

56 5 years in the Salish Sea and two NE Pacific estuaries.

57 gy coasts to calmer environments in bays and estuaries.

58 ation dominates production in reservoirs and estuaries.

59 tal contamination is a major problem in many estuaries.

60 and ecosystem function of karst subterranean estuaries.

61 the approach is transferable to other urban estuaries.

62 stability to salinity-induced aggregation in estuaries.

63 and provide an unexpected source to northern estuaries.

64 012) and freshwater inflows records into the estuary (1955-2012), we determined that the cold front w

65 ifers, groundwater transits the subterranean estuary, a region of sharp gradients in redox conditions

66 direct pathways, a consistent result in most estuaries across the northeast Pacific.

67 ods were applied in sediments from the Loire Estuary after different treatments and allowed to precis

68 omic datasets from seven connected lakes and estuaries along the Chattahoochee River (Southeastern US

69 was more important in the marine part of the estuary, although the presence of multiple carbon source

70 g retained within the benthic compartment of estuaries and also the absolute quantity of CO(2) outgas

71 he trophic webs and biogeochemical cycles of estuaries and coastal areas by freshwater loadings, and

72 on 19 chemicals in 10 Northwestern European estuaries and coastal areas.

73 om rivers are significant sources of MeHg to estuaries and coastal regions of the northern GOM.

74 Eutrophication of estuaries and coastal seas is accelerating, increasing l

75 om different sources on copper speciation in estuaries and concludes that DOC is not necessarily an a

76 tal data from four North American west coast estuaries and find heterogeneous environmental signals t

77 Fall 2012 to estimate fluxes from rivers to estuaries and from estuaries to coastal waters.

78 reviously found for riverine HS in temperate estuaries and HS standard material.

79 tuary is one of the world's largest alluvial estuaries and is adjacent to the most developed economic

80 270 stations in 29 temperate and subtropical estuaries and lagoons show transient accumulation of nit

81 inuous greenhouse gas data in lakes, rivers, estuaries and marine waters with less effort than conven

82 constructing pH, in anoxic or euxinic lakes, estuaries and ocean basins.

83 e future trajectory of biotic communities in estuaries and other transitional habitats.

84 lent in DOM of nutrient-impacted streams and estuaries and produced in phytoplankton cultures, was en

85 sediment from, for example, saltmarsh ponds, estuaries and the deep ocean than in the overlying seawa

86 is a substantial source of organic matter to estuaries and therefore has the potential to support the

87 intermediates and is especially important in estuaries and wastewater impacted aquatic systems.

88 a ratio of 0.58 in the water off Changjiang Estuary and 0.19 in the open ocean.

89 lesterol were more predominant in the Santos Estuary and Antarctica samples, respectively.

90 iver spring Chinook salmon is reduced in the estuary and coastal ocean relative to a downstream, hatc

91 tial 750-km, 1-mo-long migration through the estuary and coastal ocean, we found no evidence of diffe

92 climate-mediated oceanic variability in this estuary and discovered that the response patterns vary w

93 quilibration device during a survey along an estuary and during a 40 h time series in a mangrove cree

94 oximately 13.7 km in river length within the estuary and from a nearby reference site.

95 ropical coastal ecosystem of the Pearl River Estuary and in soil microcosm experiments.

96 UDOM) and fulvic acids from the St. Lawrence Estuary and its tributaries.

97 collected during summer and winter from the estuary and lagoon complex of the municipality of Barra

98 of water, nutrients and sediment between an estuary and marshes.

99 will affect the Amazon basin's floodplains, estuary and sediment plume.

100 mprising new environmental sequences from an estuary and the open ocean generated with high throughpu

101 MTB-associated iron flux in the investigated estuary and the pyritic-Fe flux in the Black Sea suggest

102 ffinis densities in the contaminated Scheldt estuary and the relatively uncontaminated Darss-Zingst e

103 ts (Hexagenia mayflies) from the James River Estuary and their consumers (Tetragnathidae spiders and

104 y structural and functional features of each estuary and their watersheds, including morphology, wate

105 ms that complete their life cycle within the estuary and those that spent portions of their life hist

106 t represented a spectrum of salinities in an estuary and were each amended with different forms of me

107 ) genomes were obtained from White Oak River estuary and Yellowstone National Park hot spring sedimen

108 f carbon dioxide to lakes, wetlands, rivers, estuaries, and coastal waters.

109 her patterns, decreased sink of sediments in estuaries, and increased coastal erosion.

110 ems can include drinking water, groundwater, estuaries, and lakes.

111 the sediment organic matter across multiple estuaries, and while organic matter and S are interchang

112 Estuaries are a major transport pathway for land-derived

113 Estuaries are an important source of greenhouse gases to

114 valuate PAOs in a natural system, given that estuaries are characterized by dynamic dissolved oxygen

115 Estuaries are connected to both land and ocean so their

116 Estuaries are crucial biogeochemical filters at the land

117 Estuaries are dynamic environments at the land-sea inter

118 Estuaries are transitional habitats characterized by com

119 and urban non-point-source pollution, micro-estuaries are under a dynamic risk regime, consequently

120 Sediments of the White Oak River (WOR) estuary are situated on the coast of North Carolina harb

121 micro-estuary ecosystems, like the Alexander estuary, are continuously exposed to pharmaceuticals and

122 Estuaries around the world are in a state of decline fol

123 d, gold core nanoparticles in a model marine estuary as a function of time.

124 Using the Yangtze Estuary as a study region, we developed an automatic alg

125 ream of the estuary (i.e. not "in the Severn Estuary" as stated by the authors).

126 merata in a study of oysters being farmed in estuaries at aquaculture leases differing in environment

127 om each of three tidal freshwater marshes in estuaries at three latitudes (north, middle, south) on t

128 three peripheral bays of the Columbia River estuary at abundances rivalling those observed in conven

129 m of sediment in a saline tidal creek in the estuary at Murrell's Inlet, South Carolina and character

130 ass meadows can be highly variable within an estuary, attributed largely to accumulation of fine sedi

131 line along a salt wedge estuary (Yarra River estuary, Australia).

132 decades from measurements across the world's estuaries, bays, lagoons, inland seas and shelf waters i

133 ng the uncultured archaeal groups in the WOR estuary, biogeochemical profiles as well as archaeal 16S

134 d at the sea floor of an urbanised temperate estuary bordered by an LED lit city.

135 on will increase methylmercury inputs to the estuary by 25-200%, overwhelming climate-driven changes

136 bility of ciliate community in a subtropical estuary by rRNA and rDNA-based high throughput sequencin

137 The San Francisco Estuary, California, contains mercury (Hg) contamination

138 g the salinity gradient in the San Francisco Estuary, California, USA.

139 obacteria (e.g., Microcystis aeruginosa), to estuaries can adversely affect estuarine and coastal eco

140 at the final stage of wave growth in shallow estuaries can be presented by a product of water depth a

141 Lucie Estuary can result in lower bloom intensities.

142 y, Narragansett Bay, and the Cape Fear River Estuary (CFRE), United States.

143 per thousand) previously observed in lakes, estuaries, coastal oceans, and forests.

144 4 +/- 13 kg ha(-1) d(-1)) mangrove-dominated estuaries compared to the southeastern region, highlight

145 ificantly (p < 0.05) higher SPM in the Ajkwa Estuary compared to neighboring estuaries.

146 ixture of contaminants frequently present in estuaries complicates their assessment by routine chemic

147 The anoxic sediments of the White Oak River estuary comprise a distinctive sulfate-methane transitio

148 implications for managing nutrient inputs to estuaries connected to upwelling systems, and for assess

149 The estuary contains surface sediments that are strongly red

150 used the dramatic decline of the Pearl River estuary coral communities reported from 1980 to 2000.

151 by wave erosion, an ubiquitous process along estuaries, could affect vegetation dynamics in ways that

152 Estuaries cover <1% of marine habitats, but the carbon d

153 increasingly pervasive in the San Francisco Estuary Delta (USA) since the early 2000s and their rise

154 Human land cover can degrade estuaries directly through habitat loss and fragmentatio

155 ther than Type II, despite the fact that the estuary does not have particularly high nutrient concent

156 We examined temperature variation across the estuary during cold disturbances with different degrees

157 a mandated discharges from the lake into the estuary during high rainfall periods.

158 nger residence times within the subterranean estuary during the winter, which would result from reduc

159 ations between the exit of the ditch and the estuary, during three different months showed that tempo

160 The current work highlights that micro-estuary ecosystems, like the Alexander estuary, are cont

161 cted killifish subpopulations throughout the estuary, even in sites with lower levels of PAHs.

162 Striped bass moved out of the estuary, exhibiting novel migration behaviours, that may

163 Subterranean estuaries extend inland into density-stratified coastal

164 ommon Snook, within Everglades National Park estuaries (FL US).

165 in each estuary (limited migration) or among estuaries from different latitudes in each continent (co

166 Ocean-atmosphere processes propagate into estuaries from the sea, and atmospheric processes over l

167 mospheric processes over land propagate into estuaries from watersheds.

168 We found a strong spatial pattern within the estuary, from 52.16 mg C(org) cm(-3) in seagrass meadows

169 substances (PFASs) in a temperate macrotidal estuary (Gironde, SW France).

170 strongly influence phytoplankton dynamics in estuaries globally.

171 A more recent anthropogenic input to the estuary has been technogenic tritium (specifically organ

172 The total area of tidal flats in the Yangtze Estuary has decreased by 36% over the past three decades

173 increased temperature and drought, bar-built estuaries have transitioned from lotic (flowing-water) t

174 In dynamic estuaries, HOCs can be taken up from sediments, porewate

175 er (UK), approximately 50 km upstream of the estuary (i.e. not "in the Severn Estuary" as stated by t

176 that is consistent with the footprint of an estuary identified in pre-development maps.

177 es in sediment of 4 biogeochemically diverse estuaries in the Northeast U.S.

178 serious water-quality problem in most of the estuaries in the United States, especially those downstr

179 y, USA, one of the largest and most valuable estuaries in the world, with an unparalleled history of

180 ere all collected from a Massachusetts (USA) estuary in 2007, phylogenetic reconstructions allowed us

181 A field deployment in the most urbanized estuary in Australia (Sydney Harbour) showed trace level

182 itions in Elkhorn Slough, a highly eutrophic estuary in central California (United States), which als

183 an Deep-Water Harbour near the Yangtze River estuary in China and identified more than 4,500 distinct

184 to coastal waters from a mangrove-dominated estuary in Everglades National Park (Florida, USA).

185 eutical contamination in the Alexander micro-estuary in Israel.

186 abundances were observed at the mouth of the estuary in mesohaline sediments in the spring and summer

187 totanus) overwintering on an industrialised estuary in Northern Europe.

188 d the relatively uncontaminated Darss-Zingst estuary in relation to temperature, salinity, chlorophyl

189 sapeake Bay, the largest and most productive estuary in the U.S., suffers from varying degrees of wat

190 nknown or not well-resolved in several large estuaries including the semi-lagoonal Neuse River Estuar

191 ers (Ostreidae), ecosystem engineers in many estuaries, influence water quality, construct habitat, a

192 reat to coral communities in the Pearl River estuary; instead, nitrogen (N) inputs dominated impacts.

193 We divided the Yangtze Estuary into Shanghai and Jiangsu areas, which differ in

194 demonstrate that wave growth rate in shallow estuaries is a function of wind fetch to water depth rat

195 lative importance as N sources to particular estuaries is not.

196 eral bay sediments, and hypothesized that an estuary is an ideal setting to evaluate PAOs in a natura

197 The Yangtze Estuary is one of the world's largest alluvial estuaries

198 Karst subterranean estuaries (KSEs) occur globally on carbonate islands and

199 ost of coastal cholera foci are located near estuaries, lagoons, mangrove forests, and on islands.

200 , soil samples were mixed either within each estuary (limited migration) or among estuaries from diff

201 ons in the river to be impounded, downstream estuary, locally harvested fish, birds and seals, and th

202 Using samples from a large temperate estuary (Long Island Sound, USA), we gained three major

203 our salt marshes in Waquoit Bay and adjacent estuary, Massachusetts, USA were utilized to evaluate th

204 orical Pb input phases, and highlight within-estuary mixing and supply of reworked, secondary contami

205 mg C(org) cm(-3) in seagrass meadows at the estuary mouth, despite a general gradient of increasing

206 nducted during July 2008 on the Hudson River estuary near the Tappan Zee Bridge, which is the site of

207 nt riverine striped bass in the Hudson River Estuary, New York, USA, caused by an intense period of t

208 were conducted in the N-limited Neuse River Estuary, North Carolina from 2014 to 2015.

209 ries including the semi-lagoonal Neuse River Estuary (NRE), a tributary of the second largest estuary

210 M) organic matter quality in the Neuse River Estuary (NRE), North Carolina, before and after passage

211 community composition within the Neuse River Estuary (NRE), North Carolina.

212 mercial mussel raft in the urban Bronx River Estuary, NY, in waters closed to shellfish harvest due t

213 changes reflect a slow biological process of estuary-ocean connectivity operating through the immigra

214 f sedimentary organic matter along the river-estuary-ocean continuum.

215 ortant species native to coastal regions and estuaries of the Gulf of Mexico - habitats that routinel

216 lism in diatoms that cooccur regularly in an estuary on the east coast of the United States (Narragan

217 scale bioreactor model that closely mimicked estuary or brackish sediment conditions.

218 t are likely to aggregate under salty (e.g., estuaries) or acidic (e.g., acid rain droplets) aquatic

219 But tau is highly variable in estuaries, owing to constant changes in river inflows, t

220 approaching extinction in the San Francisco Estuary, placing it in the crossfire between human and e

221 yster Crassostrea hongkongensis in a dynamic estuary polluted by metals using a 48 day transplant exp

222 (Hg) in surface sediments of the Pearl River Estuary (PRE) and the South China Sea (SCS) were analyze

223 anthropogenic impacts, while the Pearl River Estuary (PRE) in south China has been highly impacted by

224 and in free-living forms in the Pearl River Estuary (PRE) over a 10-month period.

225 of domestic sewage entered directly into the estuary, preventing removal by natural denitrification h

226 Estuaries provide critical hunting and fishing territory

227 ration of wetland ecosystems in many shallow estuaries raises concerns about the contributing erosive

228 e highest nifH expression at the head of the estuary, regardless of season.

229 Whereas across all estuaries, regression analyses showed that S alone drive

230 The framework and methods are shown using an estuary restoration case from Puget Sound, United States

231 d mussel ( Mytilus galloprovincialis) of the estuary Ria de Arousa, Spain (42.5 degrees N, 8.9 degree

232 e effects of OUT propagated further down the estuary salinity gradient than the effects of NPGO that

233 n the effects of NPGO that propagated up the estuary salinity gradient, exemplifying the role of vari

234 cate two sources of Pt and Os into the Tagus Estuary salt marshes: a regional input associated with i

235 ad uncultured benthic Archaea recovered from estuary sediments at 48% to 95% completeness.

236 enrichment culture derived from Besos river estuary sediments stoichiometrically dechlorinated 1,2-d

237 s may play an important role in P cycling in estuary sediments.

238 Wetland dominated estuaries serve as one of the most productive natural ec

239 The estuary serves as an important nursery ground for Englis

240 ytemora affinis) common in the San Francisco Estuary (SFE), an estuary with relatively low phytoplank

241 present survey was conducted in the Gironde estuary (southwestern France) where PFASs were ubiquitou

242 The macrotidal Severn Estuary (southwestern UK) has received a broad range of

243 ighly migratory, moving long distances among estuaries, spawning rivers, and distant coastal regions.

244 Subterranean estuaries (STEs) are of major importance for land-ocean

245 hurricanes, El Nino and HABs in two Florida estuaries subject to repeated intense ecosystem disrupti

246 pe components that determine the function of estuaries, successful restoration strategies require kno

247 ning the freshwater to marine regions of the estuary suggested the existence of five estuarine salini

248 the GOM were less than those from rivers to estuaries, suggesting an overall estuarine sink.

249 environmental signals that characterize each estuary, suggesting that the potential stressor exposure

250 cores and interstitial waters from the Tagus Estuary (SW Europe) affected by different traffic pressu

251 he principal sedimentary sinks of the Severn Estuary system reflects the particular dynamics of this

252 ary (NRE), a tributary of the second largest estuary-system in the lower USA, the Pamlico-Albemarle S

253 high water discharges into the Hudson River Estuary that increased the water level and reduced the w

254 ish subpopulations from sites throughout the estuary that varied significantly in PAH contamination l

255 rse environments encompassing lakes, rivers, estuaries, the open ocean and forested and non-forested

256 ate mineral dissolution in the USA's largest estuary.The potential contribution of redox reactions to

257 such as nitrate and oxygen) propagates into estuaries through fast water exchanges that dissipate al

258 incides with periods of low pH occurrence in estuaries, thus we investigated effects of moderate (pH

259 Fluxes of total Hg from the estuaries to coastal waters of the northern GOM are appr

260 ate fluxes from rivers to estuaries and from estuaries to coastal waters.

261 latitudinal gradient in California bar-built estuaries to examine their evolution in response to chan

262 +/- 3.1 Tg C yr(-1), while CO(2) efflux from estuaries to the atmosphere, removed the majority of riv

263 ol y(-1)) and MeHg (~120 mol y(-1)) from the estuaries to the GOM were less than those from rivers to

264 intensive coring study within a sub-tropical estuary to assess the spatial variability in sedimentary

265 esults illustrate the complex response of an estuary to environmental change because of interacting p

266 m from inland streams to the Milwaukee River estuary to Lake Michigan and vertically from the water s

267 sources from land to the mouth of a coastal estuary to the Chesapeake Bay.

268 marine and estuarine samples from the Colne Estuary, UK, was investigated using DNA-Stable Isotope P

269 res from a mudflat at the mouth of the Colne Estuary, UK.

270 ation, consistent with the rapid Pearl River estuary urbanization as the main cause for this eutrophi

271 es during the early phase of the Pearl River estuary urbanization.

272 ected from a tidal tributary of the Delaware Estuary using an Infiltrex sampling system equipped with

273 done in the Lake Superior-Saint Louis River estuary using SourceTracker, a program that calculates t

274 d unprecedented data set on PCBs in an urban estuary using state of the art, high-resolution high mas

275 Fluxes of total Hg and MeHg from rivers to estuaries varied as much as 100-fold among rivers.

276 Silver nanoparticles (AgNPs) enter estuaries via wastewater treatment effluents, where they

277 Lucie Estuary via mandated discharges from the lake into the e

278 also seems to be distributed throughout the estuary via the atmosphere.

279 lement existing management measures in urban estuaries was examined in Long Island Sound, Connecticut

280 lux of filter-passing (0.45 mum) MeHg toward estuary was 10 +/- 5 ng m(-2) day(-1) during a single 12

281 al impact of the tritium discharges into the Estuary was small, public concern motivated the company

282 lear an average 1.2 x 10(7) L of Bronx River Estuary water daily, removing 160 kg of particulate matt

283 mance is validated using ground, stream, and estuary waters.

284 The San Francisco Bay-Delta Estuary watershed is a major source of freshwater for Ca

285 While some estuaries were sources of Hg, the combined estimated flu

286 rs from more tidally influenced areas of the estuary were higher around high water than around low wa

287 ecal bacterial inputs into the Lake Superior estuary were primarily attributed to wastewater effluent

288 s, OCPs) in aquatic species from the Scheldt estuary were related with factors (body size, lipids, tr

289 s to nitrification, especially in polyhaline estuaries where ammonia-oxidation is largely driven by A

290 ics of this process, especially in urbanized estuaries, where the adjacent upland is likely to be a m

291 h demonstrated exploratory trips back to the estuary, which may have been to assess the conditions be

292 or of atmospheric radiative forcing from the estuary, while N2O contributed <2%.

293 d oysters can be grown at the surface of the estuary, while wild oysters typically grow at the bottom

294 e residence time over single tidal cycles in estuaries will be useful for evaluating and further unde

295 ), and SiO(2)) in an area of the Tagus River estuary with a range of about 350 m.

296 acts of an oil spill in an urbanized coastal estuary with an overlapping backdrop of atmospheric, ves

297 ommon in the San Francisco Estuary (SFE), an estuary with relatively low phytoplankton primary produc

298 l P (TP) inputs were highest at the mouth of estuaries, with P concentration double that of underlyin

299 has recently become widespread in temperate estuaries worldwide.

300 and below the pycnocline along a salt wedge estuary (Yarra River estuary, Australia).