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1 tal Shelf, Sao Sebastiao Channel, and Santos Estuary).
2 009 to the East China Sea off the Changjiang Estuary.
3 d test was conducted in the Delaware Bay and Estuary.
4  level of sewage contamination in the Santos Estuary.
5 ced population densities in the contaminated estuary.
6 ounted for up to 20% of the MeHg flux to the estuary.
7 sh restorations throughout the San Francisco Estuary.
8 s (Callinectes sapidus) in the Passaic River estuary.
9 s from the coastal ocean to the subterranean estuary.
10 nitrogen attenuation within the subterranean estuary.
11 from killifish subpopulations throughout the estuary.
12 t the cycling of PCBs in a typical urbanized estuary.
13 mixing in the shallow, eutrophic Peel-Harvey Estuary.
14 nt to a tidal creek of a Spartina -dominated estuary.
15 s of this highly macrotidal sediment starved estuary.
16 ores collected from the northern side of the Estuary.
17 ture from sediments of the San Francisco Bay estuary.
18 ast water exchanges that dissipate along the estuary.
19 -salinity sediments of the San Francisco Bay estuary.
20 verse effects on larval striped bass in this estuary.
21 ulation in fishes from the San Francisco Bay Estuary.
22 genically labeled sediments elsewhere in the estuary.
23 as the numerous other sources of PCBs to the estuary.
24 g the bioaccumulation at another site in the estuary.
25 ronmental variation in the San Francisco Bay Estuary.
26 times higher than in the saline mouth of the estuary.
27 tions in a wetland-influenced region of this estuary.
28 pected of impacting the water quality of its estuary.
29 ux and 49% of the fluvial MeHg flux into GOM estuaries.
30 ver of biotic communities in river-dominated estuaries.
31 y correlated with the growth of juveniles in estuaries.
32 and ecosystem function of karst subterranean estuaries.
33 ed nitrous oxide (N2O) comes from rivers and estuaries.
34 from marsh habitats to deep-water refugia in estuaries.
35 sure pathways in five Northeast coast (U.S.) estuaries.
36 offshore transport across different types of estuaries.
37 tial changes such as peatlands, marshes, and estuaries.
38 ons on the methylation rates across multiple estuaries.
39 tamination along the Gulf coast in sensitive estuaries.
40 atter does not hinder mercury methylation in estuaries.
41  the approach is transferable to other urban estuaries.
42 atchments to larger river systems, lakes and estuaries.
43 stability to salinity-induced aggregation in estuaries.
44  for aquatic toxicities in urban streams and estuaries.
45  time scales that are relevant to rivers and estuaries.
46 ological connectivity between watersheds and estuaries.
47 thonous quality of DOM in shallow microtidal estuaries.
48 imilar to vitamin concentrations reported in estuaries.
49 found role for infectious processes in these estuaries.
50 tion of raw oysters gathered from warm-water estuaries.
51 ducing their impact on downstream rivers and estuaries.
52  kills and human disease in mid-Atlantic USA estuaries.
53  over nutrient exports to rivers, lakes, and estuaries.
54 ts into the cycling of anthropogenic lead in estuaries.
55 and provide an unexpected source to northern estuaries.
56 an, with one ecotype confined near the river estuaries.
57  wind wave growth in fetch and depth limited estuaries.
58 tin photodegradation during transport within estuaries.
59 e progress toward improving water quality in estuaries.
60 ydrodynamically complex environments such as estuaries.
61 tal contamination is a major problem in many estuaries.
62 lly lethal levels of pollution in four urban estuaries.
63 in the Ajkwa Estuary compared to neighboring estuaries.
64 012) and freshwater inflows records into the estuary (1955-2012), we determined that the cold front w
65  stages of striped bass in the San Francisco Estuary, a population in continual decline since its ini
66 ifers, groundwater transits the subterranean estuary, a region of sharp gradients in redox conditions
67 direct pathways, a consistent result in most estuaries across the northeast Pacific.
68 ods were applied in sediments from the Loire Estuary after different treatments and allowed to precis
69 nsion and collapse of oyster fisheries in 28 estuaries along three continental margins through the an
70 al oceanic regime changes can propagate into estuaries, altering their community structure and effici
71 was more important in the marine part of the estuary, although the presence of multiple carbon source
72 g retained within the benthic compartment of estuaries and also the absolute quantity of CO(2) outgas
73 he trophic webs and biogeochemical cycles of estuaries and coastal areas by freshwater loadings, and
74  on 19 chemicals in 10 Northwestern European estuaries and coastal areas.
75 livery of biologically available nitrogen to estuaries and coastal oceans in recent decades has been
76 om rivers are significant sources of MeHg to estuaries and coastal regions of the northern GOM.
77                            Eutrophication of estuaries and coastal seas is accelerating, increasing l
78 ing encysted zoonotic protozoan parasites to estuaries and coastal waters.
79 om different sources on copper speciation in estuaries and concludes that DOC is not necessarily an a
80 tal data from four North American west coast estuaries and find heterogeneous environmental signals t
81  Fall 2012 to estimate fluxes from rivers to estuaries and from estuaries to coastal waters.
82 tuary is one of the world's largest alluvial estuaries and is adjacent to the most developed economic
83 ical analysis of 73 molluscan data sets from estuaries and lagoons reveals significantly poorer avera
84 270 stations in 29 temperate and subtropical estuaries and lagoons show transient accumulation of nit
85 inuous greenhouse gas data in lakes, rivers, estuaries and marine waters with less effort than conven
86 constructing pH, in anoxic or euxinic lakes, estuaries and ocean basins.
87 e future trajectory of biotic communities in estuaries and other transitional habitats.
88 lent in DOM of nutrient-impacted streams and estuaries and produced in phytoplankton cultures, was en
89 sed the frequency and severity of hypoxia in estuaries and semi-enclosed seas, the occurrence of hypo
90 flux of nitrogen from land and atmosphere to estuaries and the coastal ocean has increased substantia
91 moved by denitrification in the sediments of estuaries and the continental shelf, leading to a reduct
92 intermediates and is especially important in estuaries and wastewater impacted aquatic systems.
93  a ratio of 0.58 in the water off Changjiang Estuary and 0.19 in the open ocean.
94 lesterol were more predominant in the Santos Estuary and Antarctica samples, respectively.
95 iver spring Chinook salmon is reduced in the estuary and coastal ocean relative to a downstream, hatc
96 tial 750-km, 1-mo-long migration through the estuary and coastal ocean, we found no evidence of diffe
97 climate-mediated oceanic variability in this estuary and discovered that the response patterns vary w
98 quilibration device during a survey along an estuary and during a 40 h time series in a mangrove cree
99 oximately 13.7 km in river length within the estuary and from a nearby reference site.
100 UDOM) and fulvic acids from the St. Lawrence Estuary and its tributaries.
101  collected during summer and winter from the estuary and lagoon complex of the municipality of Barra
102  of water, nutrients and sediment between an estuary and marshes.
103  will affect the Amazon basin's floodplains, estuary and sediment plume.
104 mprising new environmental sequences from an estuary and the open ocean generated with high throughpu
105 MTB-associated iron flux in the investigated estuary and the pyritic-Fe flux in the Black Sea suggest
106 ffinis densities in the contaminated Scheldt estuary and the relatively uncontaminated Darss-Zingst e
107 ts (Hexagenia mayflies) from the James River Estuary and their consumers (Tetragnathidae spiders and
108 ms that complete their life cycle within the estuary and those that spent portions of their life hist
109 t represented a spectrum of salinities in an estuary and were each amended with different forms of me
110 ) genomes were obtained from White Oak River estuary and Yellowstone National Park hot spring sedimen
111 f carbon dioxide to lakes, wetlands, rivers, estuaries, and coastal waters.
112 he composition of juvenile fish stocks using estuaries, and for the appropriate conservation of estua
113 her patterns, decreased sink of sediments in estuaries, and increased coastal erosion.
114 ems can include drinking water, groundwater, estuaries, and lakes.
115 g water, acidifies rain, eutrophies bays and estuaries, and stresses ecosystems.
116  the sediment organic matter across multiple estuaries, and while organic matter and S are interchang
117 sks, the key phytoplankton consumers in this estuary, and record high abundances of several bivalve p
118  web patterns between Tuesday Lake and Ythan Estuary, and similarities of Tuesday Lake in 1984 and 19
119 d organic matter supply in a river-dominated estuary, Apalachicola Bay, Florida.
120                                              Estuaries are an important source of greenhouse gases to
121                                              Estuaries are connected to both land and ocean so their
122 ble juveniles during estuarine residency, as estuaries are critical juvenile nursery or over-winterin
123                                              Estuaries are crucial biogeochemical filters at the land
124                                              Estuaries are dynamic environments at the land-sea inter
125                                              Estuaries are transitional habitats characterized by com
126       Sediments of the White Oak River (WOR) estuary are situated on the coast of North Carolina harb
127                                              Estuaries around the world are in a state of decline fol
128 d, gold core nanoparticles in a model marine estuary as a function of time.
129                            Using the Yangtze Estuary as a study region, we developed an automatic alg
130                                     Lawrence estuary as tracers of freshwater sources to further eval
131 ream of the estuary (i.e. not "in the Severn Estuary" as stated by the authors).
132 om each of three tidal freshwater marshes in estuaries at three latitudes (north, middle, south) on t
133 m of sediment in a saline tidal creek in the estuary at Murrell's Inlet, South Carolina and character
134 line along a salt wedge estuary (Yarra River estuary, Australia).
135 decades from measurements across the world's estuaries, bays, lagoons, inland seas and shelf waters i
136 ng the uncultured archaeal groups in the WOR estuary, biogeochemical profiles as well as archaeal 16S
137 on will increase methylmercury inputs to the estuary by 25-200%, overwhelming climate-driven changes
138 bility of ciliate community in a subtropical estuary by rRNA and rDNA-based high throughput sequencin
139                            The San Francisco Estuary, California, contains mercury (Hg) contamination
140 g the salinity gradient in the San Francisco Estuary, California, USA.
141 obacteria (e.g., Microcystis aeruginosa), to estuaries can adversely affect estuarine and coastal eco
142 at the final stage of wave growth in shallow estuaries can be presented by a product of water depth a
143  per thousand) previously observed in lakes, estuaries, coastal oceans, and forests.
144 ificantly (p < 0.05) higher SPM in the Ajkwa Estuary compared to neighboring estuaries.
145 ixture of contaminants frequently present in estuaries complicates their assessment by routine chemic
146  The anoxic sediments of the White Oak River estuary comprise a distinctive sulfate-methane transitio
147 implications for managing nutrient inputs to estuaries connected to upwelling systems, and for assess
148 a previously unrecognized mechanism of ocean-estuary connectivity.
149                                          The estuary contains surface sediments that are strongly red
150                                              Estuaries cover <1% of marine habitats, but the carbon d
151  increasingly pervasive in the San Francisco Estuary Delta (USA) since the early 2000s and their rise
152                 Human land cover can degrade estuaries directly through habitat loss and fragmentatio
153 We examined temperature variation across the estuary during cold disturbances with different degrees
154 nger residence times within the subterranean estuary during the winter, which would result from reduc
155 ations between the exit of the ditch and the estuary, during three different months showed that tempo
156 cted killifish subpopulations throughout the estuary, even in sites with lower levels of PAHs.
157                Striped bass moved out of the estuary, exhibiting novel migration behaviours, that may
158                                 Subterranean estuaries extend inland into density-stratified coastal
159 ommon Snook, within Everglades National Park estuaries (FL US).
160 he data support the premise that, in shallow estuaries frequently disturbed by hurricanes, there can
161 in each estuary (limited migration) or among estuaries from different latitudes in each continent (co
162    Ocean-atmosphere processes propagate into estuaries from the sea, and atmospheric processes over l
163 mospheric processes over land propagate into estuaries from watersheds.
164 substances (PFASs) in a temperate macrotidal estuary (Gironde, SW France).
165 strongly influence phytoplankton dynamics in estuaries globally.
166  along each coastline until the most distant estuary had been reached and overfished.
167 grass), often exist as discontinuous beds in estuaries, harbors, and bays where they can reproduce se
168     A more recent anthropogenic input to the estuary has been technogenic tritium (specifically organ
169 The total area of tidal flats in the Yangtze Estuary has decreased by 36% over the past three decades
170  1970s but rates of change within individual estuaries have varied from zero to sixfold increases.
171                                   In dynamic estuaries, HOCs can be taken up from sediments, porewate
172 er (UK), approximately 50 km upstream of the estuary (i.e. not "in the Severn Estuary" as stated by t
173  that is consistent with the footprint of an estuary identified in pre-development maps.
174 es in sediment of 4 biogeochemically diverse estuaries in the Northeast U.S.
175 serious water-quality problem in most of the estuaries in the United States, especially those downstr
176 y, USA, one of the largest and most valuable estuaries in the world, with an unparalleled history of
177 ere all collected from a Massachusetts (USA) estuary in 2007, phylogenetic reconstructions allowed us
178     A field deployment in the most urbanized estuary in Australia (Sydney Harbour) showed trace level
179 itions in Elkhorn Slough, a highly eutrophic estuary in central California (United States), which als
180  to coastal waters from a mangrove-dominated estuary in Everglades National Park (Florida, USA).
181  totanus) overwintering on an industrialised estuary in Northern Europe.
182 d the relatively uncontaminated Darss-Zingst estuary in relation to temperature, salinity, chlorophyl
183 tant determinant of nitrogen delivery to the estuary in the Mississippi basin, and possibly also in o
184 sapeake Bay, the largest and most productive estuary in the U.S., suffers from varying degrees of wat
185 ars after the storms in the largest lagoonal estuary in the U.S., the Albemarle-Pamlico Estuarine Sys
186 d of the Pamlico Sound, the largest lagoonal estuary in the United States and a key West Atlantic fis
187 rs suggest that this may be the most invaded estuary in the world.
188 o the guiding paradigm that algal biomass in estuaries increases in proportion to nutrient inputs fro
189 ers (Ostreidae), ecosystem engineers in many estuaries, influence water quality, construct habitat, a
190                       We divided the Yangtze Estuary into Shanghai and Jiangsu areas, which differ in
191 demonstrate that wave growth rate in shallow estuaries is a function of wind fetch to water depth rat
192      We now show that larval emigration from estuaries is favored even over minimizing visibility to
193 lative importance as N sources to particular estuaries is not.
194  and magnitude of oyster-reef degradation in estuaries is poorly quantified.
195                                  The Yangtze Estuary is one of the world's largest alluvial estuaries
196 ost of coastal cholera foci are located near estuaries, lagoons, mangrove forests, and on islands.
197                      Large-river delta-front estuaries (LDE) are important interfaces between contine
198 , soil samples were mixed either within each estuary (limited migration) or among estuaries from diff
199 ons in the river to be impounded, downstream estuary, locally harvested fish, birds and seals, and th
200         Using samples from a large temperate estuary (Long Island Sound, USA), we gained three major
201                Our results suggest that some estuaries may no longer remove nitrogen from the water c
202 orical Pb input phases, and highlight within-estuary mixing and supply of reworked, secondary contami
203      A. ornata is an annelid, which inhabits estuary mudflats with other polychaetes that secrete a r
204  fished and transported to restock exploited estuaries near the original urban center.
205 uckerton, New Jersey, and in the Yaquina Bay Estuary near Newport, Oregon.
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  loadings to a major artery, the Neuse River Estuary (NRE), and to estimate mean annual versus storm-
210 M) organic matter quality in the Neuse River Estuary (NRE), North Carolina, before and after passage
211 mercial mussel raft in the urban Bronx River Estuary, NY, in waters closed to shellfish harvest due t
212 changes reflect a slow biological process of estuary-ocean connectivity operating through the immigra
213 ortant species native to coastal regions and estuaries of the Gulf of Mexico - habitats that routinel
214 f free-living and parasitic species in three estuaries on the Pacific coast of California and Baja Ca
215 lism in diatoms that cooccur regularly in an estuary on the east coast of the United States (Narragan
216 scale bioreactor model that closely mimicked estuary or brackish sediment conditions.
217 t are likely to aggregate under salty (e.g., estuaries) or acidic (e.g., acid rain droplets) aquatic
218                But tau is highly variable in estuaries, owing to constant changes in river inflows, t
219 yster Crassostrea hongkongensis in a dynamic estuary polluted by metals using a 48 day transplant exp
220 (Hg) in surface sediments of the Pearl River Estuary (PRE) and the South China Sea (SCS) were analyze
221 anthropogenic impacts, while the Pearl River Estuary (PRE) in south China has been highly impacted by
222  and in free-living forms in the Pearl River Estuary (PRE) over a 10-month period.
223 remained for 3 years before returning to the estuary, presumably to spawn and die.
224                                              Estuaries provide critical hunting and fishing territory
225 sapeake Bay, a seasonally variable temperate estuary, provides a natural laboratory for examining the
226 ration of wetland ecosystems in many shallow estuaries raises concerns about the contributing erosive
227 e highest nifH expression at the head of the estuary, regardless of season.
228                           Whereas across all estuaries, regression analyses showed that S alone drive
229 The framework and methods are shown using an estuary restoration case from Puget Sound, United States
230 holerae lives as an autochthonous microbe in estuaries, rivers and coastal waters.
231 rologic inputs over 2 years in San Francisco Estuary's Sacramento-San Joaquin River Delta.
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  Lake, Michigan, in 1984 and 1986, and Ythan Estuary, Scotland.
236 ad uncultured benthic Archaea recovered from estuary sediments at 48% to 95% completeness.
237  enrichment culture derived from Besos river estuary sediments stoichiometrically dechlorinated 1,2-d
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  present survey was conducted in the Gironde estuary (southwestern France) where PFASs were ubiquitou
241                        The macrotidal Severn Estuary (southwestern UK) has received a broad range of
242 ighly migratory, moving long distances among estuaries, spawning rivers, and distant coastal regions.
243                                 Subterranean estuaries (STEs) are of major importance for land-ocean
244 pe components that determine the function of estuaries, successful restoration strategies require kno
245 ning the freshwater to marine regions of the estuary suggested the existence of five estuarine salini
246  the GOM were less than those from rivers to estuaries, suggesting an overall estuarine sink.
247 environmental signals that characterize each estuary, suggesting that the potential stressor exposure
248 cores and interstitial waters from the Tagus Estuary (SW Europe) affected by different traffic pressu
249 he principal sedimentary sinks of the Severn Estuary system reflects the particular dynamics of this
250                Fishery collapse began in the estuaries that were nearest to a developing urban center
251  high water discharges into the Hudson River Estuary that increased the water level and reduced the w
252 ish subpopulations from sites throughout the estuary that varied significantly in PAH contamination l
253 rse environments encompassing lakes, rivers, estuaries, the open ocean and forested and non-forested
254 ate mineral dissolution in the USA's largest estuary.The potential contribution of redox reactions to
255  such as nitrate and oxygen) propagates into estuaries through fast water exchanges that dissipate al
256 itats located in spatially discrete bays and estuaries throughout the northern Gulf.
257 incides with periods of low pH occurrence in estuaries, thus we investigated effects of moderate (pH
258  beds of oysters in Chesapeake Bay and other estuaries to a few percent of pristine abundances and pr
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 ol y(-1)) and MeHg (~120 mol y(-1)) from the estuaries to the GOM were less than those from rivers to
262 esults illustrate the complex response of an estuary to environmental change because of interacting p
263 s toxic dinoflagellates, were displaced down-estuary to habitats less conducive for growth.
264  marine and estuarine samples from the Colne Estuary, UK, was investigated using DNA-Stable Isotope P
265 res from a mudflat at the mouth of the Colne Estuary, UK.
266 ected from a tidal tributary of the Delaware Estuary using an Infiltrex sampling system equipped with
267  done in the Lake Superior-Saint Louis River estuary using SourceTracker, a program that calculates t
268 d unprecedented data set on PCBs in an urban estuary using state of the art, high-resolution high mas
269   Fluxes of total Hg and MeHg from rivers to estuaries varied as much as 100-fold among rivers.
270           Silver nanoparticles (AgNPs) enter estuaries via wastewater treatment effluents, where they
271  also seems to be distributed throughout the estuary via the atmosphere.
272 lement existing management measures in urban estuaries was examined in Long Island Sound, Connecticut
273 lux of filter-passing (0.45 mum) MeHg toward estuary was 10 +/- 5 ng m(-2) day(-1) during a single 12
274 al impact of the tritium discharges into the Estuary was small, public concern motivated the company
275 lear an average 1.2 x 10(7) L of Bronx River Estuary water daily, removing 160 kg of particulate matt
276 mance is validated using ground, stream, and estuary waters.
277                  The San Francisco Bay-Delta Estuary watershed is a major source of freshwater for Ca
278 fishery collapsed, oysters from more distant estuaries were fished and transported to restock exploit
279                                   While some estuaries were sources of Hg, the combined estimated flu
280 rs from more tidally influenced areas of the estuary were higher around high water than around low wa
281 ecal bacterial inputs into the Lake Superior estuary were primarily attributed to wastewater effluent
282 s, OCPs) in aquatic species from the Scheldt estuary were related with factors (body size, lipids, tr
283 Sound via a major tributary (the Neuse River Estuary) were at least 2-fold higher than concentrations
284 s to nitrification, especially in polyhaline estuaries where ammonia-oxidation is largely driven by A
285 on of juvenile flatfish and crustaceans into estuaries where they feed and develop.
286 ics of this process, especially in urbanized estuaries, where the adjacent upland is likely to be a m
287 h demonstrated exploratory trips back to the estuary, which may have been to assess the conditions be
288 or of atmospheric radiative forcing from the estuary, while N2O contributed <2%.
289 e residence time over single tidal cycles in estuaries will be useful for evaluating and further unde
290 ns outcompeted co-occurring phytoplankton in estuaries with elevated levels of dissolved organic matt
291 fer effect, rates of increase are greater on estuaries with low initial numbers, and godwits on these
292 acts of an oil spill in an urbanized coastal estuary with an overlapping backdrop of atmospheric, ves
293  has recently become widespread in temperate estuaries worldwide.
294  and below the pycnocline along a salt wedge estuary (Yarra River estuary, Australia).

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