ライフサイエンスコーパス: offshore

1 ve systems (MCSs) propagating from inland to offshore.

2 he ocean during low tide transported mercury offshore.

3 ed through the dispersal system and recorded offshore.

4 d secure storage reservoirs both onshore and offshore.

5 ated the 6-km-deep Peru-Chile trench, 150 km offshore.

6 blooms nearshore, but spatially over 100 km offshore.

7 is dominated by eddies that transport water offshore.

8 a wastewater outlet pipe and pump it a mile offshore.

9 han cyclones of the same amplitude generated offshore.

10 tiple cameras optimised for different ranges offshore.

11 vealed consistent whale densities up to 3 km offshore.

12 ed water along the coast and transporting it offshore.

13 pic results suggest that prehistoric NFS fed offshore across their entire range, that California popu

14 Assumptions on lifetimes, work times for offshore activities and implementation of NOx abatement

15 nes-termed polar lows-constitute a threat to offshore activities such as shipping or oil and gas expl

16 with cascading effects on recruitment to the offshore adult population and fishery, indicating that h

17 The thorium-232 data suggest that offshore advection of particulate material from the shel

18 at the coast and Cyanobium-related sequences offshore, although it remains unclear whether these came

19 Upon hatching, young turtles migrate offshore and are rarely observed until they return to co

20 om peak levels (38 +/- 11% and 81 +/- 12% in offshore and coastal areas, respectively) reflect domest

21 A general trend was observed for the offshore and coastal reference sites with substantial in

22 eastern regions of the Mediterranean and for offshore and deep sea habitats.

23 g thought to record low-energy conditions of offshore and deeper water environments, our results call

24 dominant ASVs at the pier were found further offshore and in the California Current, but we did obser

25 lcidicum and Pachyseris rugosa found in both offshore and inshore habitats.

26 of participants being granted visas through offshore and onshore humanitarian programmes, respective

27 easing water temperatures cause them to move offshore and southwards.

28 three different seawater sources (nearshore, offshore, and near the outlet of a "brown water" stream)

29 orders) tend to originate onshore, diversify offshore, and retreat into deep-water environments.

30 arby and distant locations, both inshore and offshore, and tested them for their ability to induce se

31 Offshore Antarctic polynyas-large openings in the winter

32 ean promotes nearshore AO, while suppressing offshore AO.

33 ore contrasting with multi-decadal decreases offshore (approx. 75% lower decadal mean abundance), urg

34 Although fisheries reforms and advances in offshore aquaculture (hereafter 'mariculture') could inc

35 een the modern onshore hydrologic system and offshore aquifers.

36 f large amounts of wastewater discharge into offshore areas have helped in the understanding of pollu

37 overall peak year for PCDD/Fs in Baltic Sea offshore areas was estimated (using spline-fit modeling)

38 simulation of complex transport processes in offshore areas, and the results from such modeling syste

39 PCDD/Fs in sediment cores collected from six offshore areas, eight coastal sites impacted by industri

40 rs occurring 1-2 decades earlier compared to offshore areas.

41 e simulation of produced water discharges in offshore areas.

42 s (fishing capital) that can be used further offshore as a means to improve incomes and relieve fishi

43 e diapycnal nutrient fluxes declined rapidly offshore as a result of decreasing vertical gradients of

44 mapped and unmapped faults before continuing offshore at the island's northeastern extent.

45 s will be compensated by storm tracks moving offshore at the latitude of New York City.

46 e focused on the onshore deposits, while the offshore backwash deposits, crucial for a better underst

47 erall half-life and reductions of PCDD/Fs in offshore Baltic Sea sediment correspond well to both PCD

48 and mean currents simulated both onshore and offshore bar migration observed over a 45-day period.

49 to higher water temperature as compared with offshore barrier reefs.

50 e along a 4192-sensor ocean-bottom DAS array offshore Belgium.

51 Cretaceous: (i) decline in anoxia/dysoxia in offshore benthic environments; (ii) extinction of faunas

52 , indicating the influence of river water on offshore biological production.

53 ions yield maximal biomass near shore, while offshore biomass is positively correlated with subsurfac

54 f the East African Rift System, including an offshore branch in the western Indian Ocean, resulting i

55 le communities exhibit increasing extinction offshore but that genera within individual taxonomic cla

56 t downwind of the Coal Oil Point seep field, offshore California found methane, CH(4), concentrations

57 ely operated underwater vehicles, a dumpsite offshore California was surveyed and sampled.

58 were observed within one minute following an offshore call in almost half of the instances (43.18%).

59 In contrast to their terrestrial call, the offshore call of penguins during their foraging trips ha

60 ths and shorter durations after producing an offshore call than those before producing an offshore ca

61 offshore call than those before producing an offshore call.

62 From the video recordings, we collected 598 offshore calls from 10 individuals in two breeding seaso

63 The offshore calls varied in their dominant frequency and le

64 ng the location and geometry of a well-known offshore capable fault.

65 9 m) of the NEMO Phase 2 prototype, deployed offshore Capo Passero (Sicily) at the KM3NeT-Italia site

66 Satellite imagery and offshore chlorophyll-a samples are consistent with the p

67 ns are already developing CCS projects using offshore CO(2) storage resources, most geographic region

68 Here, we examine whether offshore CO2EOR can store more CO2 than onshore projects

69 fter oil production has been optimized, then offshore CO2EOR has the potential to be carbon negative-

70 and were higher than MeHg concentrations in offshore-collected seston.

71 r to be fueled by natural iron enrichment of offshore communities as they are transported toward the

72 urprisingly, none of the plastics exposed to offshore conditions displayed the typical signature of a

73 arine gradient from the estuarine head to an offshore continental shelf site.

74 e onshore regions such as the Middle East to offshore continental shelves.

75 We suggest that this boundary represents the offshore continuation of the Median Tectonic Line, which

76 In contrast, offshore corals harbored specific species of Cladocopium

77 Es, including shallow up-dip events that lie offshore, could lead to accurate forecasts of earthquake

78 nse was consistently muted relative to their offshore counterparts, high physiological variability in

79 zone were significantly higher in MeHg than offshore counterparts.

80 ed by a combination of the northward flowing offshore current and endogenous incompatibilities restri

81 meters) variation in the interaction between offshore currents and winds and continental shelf bathym

82 ereas the studied rhodoliths originated from offshore deep bank pinnacles in the northwestern Gulf of

83 We reveal 18 continental-shelf and 12 offshore deep-sea realms, reflecting the wider ranges of

84 Deepwater Horizon (DWH) blowout, we surveyed offshore demersal fishes in the northern Gulf of Mexico

85 istory influenced early life history traits: offshore developers initially grew slowly but compensate

86 New York Wind Energy Area (NY WEA), a future offshore development site.

87 icial light at night (ALAN) from coastal and offshore developments threatens coral reef health by mas

88 se is published for use in future studies of offshore dispersion.

89 cted as symbiotic, corroborating the onshore-offshore diversification trend recorded in marine taxa.

90 flourish in platelet ice is reflected by an offshore downward gradient in diene II concentration in

91 ore than 11,000 water samples were collected offshore during more than 100 cruises and were measured

92 e dismissed as the sources, as no concurrent offshore earthquakes or landslides were detected.

93 impact of the Deepwater Horizon oil spill on offshore ecosystems, 11 sites hosting deep-water coral c

94 is key to divergence, here we show that the offshore ecotype has higher environmental tolerance and

95 compounds in the coastal ecotype versus the offshore ecotype.

96 by the positive SLP anomalies caused strong offshore Ekman transport along the coast of NE Pacific,

97 ch, we find that the largest contribution to offshore emissions is from flaring or venting of reprodu

98 where threats from shipping, oil spills, and offshore energy development remain.

99 p to validate multiscale flow physics around offshore energy platforms that have thus far only been s

100 accelerated reproduction at small size in an offshore environment.

101 gative delta(82/78)Se values are observed in offshore environments, only a single formation, evidentl

102 lect lower dissolved organic carbon (DOC) in offshore environments, which is known to affect both the

103 scaped local extinction by diversifying into offshore environments.

104 h the expansion of deep burrowing forms into offshore environments; and (iv) offshore expansion of br

105 g forms into offshore environments; and (iv) offshore expansion of bryozoan diversity.

106 detailed evaluation of TAG:PL ratio in adult offshore-farmed gilthead sea bream.

107 An offshore field demonstration of the method was conducted

108 a "hook-type" formation process, in which an offshore filament from the southern flank of the Gulf St

109 ty hot spot and critical nursery grounds for offshore fisheries in a broader region.

110 an land use activities can indirectly affect offshore fisheries.

111 use measurements of hydraulic gradients and offshore fluxes taken at Waquoit Bay, Massachusetts, tog

112 Although offshore freshened groundwater (OFG) systems have been d

113 ts have been mapped that extend for 1,500 km offshore from northwest Africa.

114 (129)I in seawater depth profiles collected offshore Fukushima in June 2011.

115 e from the accident was deposited in the sea offshore Fukushima.

116 f 2.2 x 10(-9) in the surface seawater 40 km offshore Fukushima.

117 er depth in the carbon budget of the Panarea offshore gas release system.

118 For nations with large-scale emissions, offshore geologic CO(2) storage provides an attractive a

119 Offshore geological repositories have received relativel

120 c CO2 using a combination of air capture and offshore geological storage can address technical and po

121 also contribute to shelf-sea exchange and to offshore gradation of benthic community structure in sha

122 Likewise, inshore-offshore gradients in dinoflagellate trends, with contem

123 Mechanisms for emplacing offshore groundwater include glacial processes that drov

124 data provide more continuous constraints on offshore groundwater than previous models and present ev

125 predictable transitions between coastal and offshore habitat were associated with long-term environm

126 w these sharks to exploit multiple shelf and offshore habitats.

127 nd increased utilization of deeper waters in offshore habitats.

128 ey primarily forage on pinnipeds, to oceanic offshore habitats.

129 occasionally for extended periods of time in offshore habitats.

130 residual variability is forced by localized offshore high sea level pressure variability.

131 anism which inhabits marine ecosystems where offshore hydraulic fracturing activity is intensifying.

132 cal methane emissions, including onshore and offshore hydrocarbon seepage from subsurface hydrocarbon

133 offshore immigration detention [Nauru], and offshore immigration detention [Manus Island]).

134 ty detention, onshore immigration detention, offshore immigration detention [Nauru], and offshore imm

135 est in near-shore habitats, but also extends offshore in Lakes Erie, Ontario, and Michigan.

136 ngoing glacial erosion on land and deposited offshore in the marine sedimentary record.

137 genus during these blooms as well as further offshore in the Southern California coastal ecosystem (C

138 Offshore installation and maintenance activities cause 2

139 showed evidence of clonal expansion, and one offshore island population had exceptionally high levels

140 , yet today they breed almost exclusively on offshore islands at high latitudes.

141 e lowest concentrations observed in the most offshore Lake Erie samples.

142 AH concentrations ranged from 2.4 ng/L at an offshore Lake Erie site to 30.4 ng/L in Sheffield Lake (

143 ure on the seafloor, both at a harbor and an offshore location in the Belgian part of the North Sea.

144 as marine refugia for pelagic fauna, whereas offshore locations are potentially more climatically sen

145 ned by colonies originating from inshore and offshore locations.

146 taffing support to U.S. medical centers from offshore locations.

147 Within offshore, low-P regions of the western basin of Lake Eri

148 s for discerning OA pollution sources in the offshore marine atmosphere, where continental and marine

149 rget, developing countries must set up large offshore Marine protected areas.

150 iver of Hg reactivity and bioavailability in offshore marine waters.

151 t (Greece), the unique record of onshore and offshore markers of Pleistocene ~100-ka climate cycles p

152 nse of bottlenose dolphins to intense storms offshore Maryland, USA between 2015 and 2017.

153 lys gigantea and Astrochelys radiata, to two offshore Mauritian islands, and the costs and success of

154 as PFOS and PFOA, a comparison of inland and offshore measurements from the same year (2014) suggests

155 ng potential (CSTP) in the Texas coastal and offshore Miocene interval, comprising lower, middle, and

156 torically has been associated with extensive offshore mixing and greater primary productivity at the

157 cal analyses of the 2016 M(w) 6.4 earthquake offshore Morocco - the largest event ever recorded in th

158 context, we propose that the protection and offshore nature of Jardines de la Reina may preserve the

159 ase, a 6-year study of migrating birds to an offshore New England island was conducted during 1989-19

160 aterally continuous aquifers extending 90 km offshore New Jersey and Martha's Vineyard, Massachusetts

161 deployed at the Hikurangi subduction margin offshore New Zealand.

162 i Plateau beneath the southern Kermadec arc, offshore New Zealand.

163 A good example is the Queensland Plateau offshore northeast Australia next to the threatened Grea

164 structure of the overthrusting (upper) plate offshore northeast Japan.

165 400-kilometer strip of the Sunda megathrust, offshore northern Sumatra, in March 2005.

166 am Expedition 362 sampled incoming sediments offshore northern Sumatra, revealing recent release of f

167 species promote long-distance migrations to offshore nursery grounds.

168 Isla Mocha, a volcanic island 35 km offshore of Central-South Chile, is an example of such a

169 for 40 interplate thrust earthquakes located offshore of Honshu between 1989 and 1995.

170 ake and the subsequent tsunami that occurred offshore of Japan resulted in an important loss of life

171 ds on a 20 km section of a fiber optic cable offshore of Moss Landing, CA, in Monterey Bay, we extrac

172 the Cocos plate at the Middle America trench offshore of Nicaragua.

173 600-kilometer segment of the plate boundary offshore of northwestern Sumatra and the southern Nicoba

174 ng the northern rim of the Mediterranean and offshore of some rapidly developing tropical countries,

175 t cores, we resolve the record of glaciation offshore of South Georgia through the transition from th

176 concentrations in open ocean waters (1200 km offshore of the American Coast, at the location of the A

177 concentrations recorded in surface seawater offshore of the damaged Fukushima Dai-ichi nuclear power

178 Shipboard measurements of offshore oil and gas facilities were conducted in the Gu

179 ircraft measurements of CH(4) emissions from offshore oil and gas platforms collected over the U.S. G

180 Offshore oil exploration, oil spill contingency planning

181 Several offshore oil fields off the Mumbai-Gujarat coast, and re

182 c components of the produced water (PW) from offshore oil platforms discharged into the marine enviro

183 s in PW samples from six different Norwegian offshore oil platforms.

184 2010 the BP-operated Deepwater Horizon (DWH) offshore oil rig exploded, releasing an estimated 760 mi

185 The Deepwater Horizon blowout is the largest offshore oil spill in history.

186 originating from oil exploration activities offshore, oil sands exploitation onshore, and use of ref

187 Relative to offshore open waters, interstitial waters within decayin

188 es have underestimated the impacts caused by offshore operations and (though less important) exchange

189 offset additional emissions produced through offshore operations and incremental oil production.

190 microbial metal utilization in methane seeps offshore Oregon and California, USA, and report dissolve

191 However, offshore-origin recruits still grew significantly less u

192 counts for surface displacements on land and offshore outside the rupture area.

193 logy became earlier were characterized by an offshore, pelagic distribution, whereas species with del

194 With the expansion of offshore petroleum extraction, validated models are need

195 ature of crustal deformation measurements at offshore plate boundaries.

196 ere studied, including shallow and deepwater offshore platforms and drillships.

197 Offshore plumes were spatially narrower than expectation

198 ting coastal water offshore, resulting in an offshore POC enrichment of 20.9 +/- 11 Gg year(-1).

199 n to be more tolerant to thermal stress than offshore populations, but it is unclear whether this dif

200 e continental slope), whereas the (cyclonic) offshore portion rests on the density interface of the s

201 E striking aseismic zone of high attenuation offshore Pozzuoli.

202 Omegaaragonite that are partly controlled by offshore processes.

203 Offshore production for economic competitiveness can int

204 Minho and Galicia, respectively) and the new offshore production site of Armona (Algarve, south Portu

205 ogeochemical processes that may be linked to offshore productivity and ultimately controlled by large

206 nt of such events corresponding to increased offshore productivity.

207 ospholipids) rearrangements in the muscle of offshore-raised gilthead sea bream was carried out as a

208 ankton biomass along the coast and over 300% offshore, raises the possibility that the current warmin

209 ater from the highly protected 'crown jewel' offshore reefs in Jardines de la Reina, Cuba had low con

210 h extensive deforestation, and after 1960 on offshore reefs.

211 modeled low-salinity water transport to the offshore region and the observed chlorophyll-a in the of

212 supply, wind resources distributed along the offshore region of five coastal provinces in China (Shan

213 region and the observed chlorophyll-a in the offshore region was also observed, indicating the influe

214 conventional oil and gas (UOG) activities in offshore regions are nonexistent.

215 c cod (Boreogadus saida) were collected from offshore regions of the Beaufort Sea to determine the co

216 ctuations, variations of global RI events in offshore regions remain uncertain.

217 Due to low nitrate concentrations in offshore regions, anammox bacteria likely dominated N(2)

218 i below the western United States and nearby offshore regions.

219 The rapid development of the offshore renewable energy sector has led to an increased

220 nology and inherent difficulty of conducting offshore research, make identification and assessment of

221 fact trapping and transporting coastal water offshore, resulting in an offshore POC enrichment of 20.

222 nce coastal ocean ecosystems and delivery of offshore, river-influenced water may influence estuarine

223 ed for monitoring marine organisms; however, offshore sampling and time lag from sampling to results

224 ource rock intervals in poorly characterised offshore sedimentary basins prior to exploratory drillin

225 ermine when petroleum generation occurred in offshore sedimentary basins.

226 The half-life of PCDD/Fs in Baltic Sea offshore sediments was estimated to be approximately 2 a

227 We integrate this onshore dataset with offshore seismic data to provide a synoptic view of the

228 nt a tomographic model, derived from on- and offshore seismic experiments, that reveals a strong low-

229 ined by the orientation and intensity of the offshore seismic line source and subsequently by the tra

230 We find that delta(82/78)Se values in offshore shales show a positive excursion from 2.32 Ga u

231 at developed in waters depleted in Pb (i.e., offshore signature), potentially dispersing from upstrea

232 ight coastal, one coastal reference, and six offshore sites covering the northern to the southern Bal

233 of this syndrome (15%) were recorded at two offshore sites in the Great Barrier Reef Marine Park (GB

234 zation studies of these reservoirs, although offshore sites may offer larger potential capacity and a

235 from the coastline (i.e. lowest densities at offshore sites).

236 the greatest differences between inshore and offshore sites.

237 while relatively low diversity was found at offshore sites.

238 r in the 3' UTR, gene bodies, CpG shores or 'offshore' sites, and both positive and negative correlat

239 loor deformation observations made during an offshore slow-slip event (SSE) in September and October

240 d between ecotypes, suggesting more abundant offshore sources of these compounds.

241 we present a continuous 150,000-year record offshore south-western Australia and identify the timing

242 Africa from the Red Sea to the Indian Ocean offshore southern Mozambique.

243 the low-altitude basement landforms on- and offshore southwestern Scandinavia are a rejuvenated geom

244 maturity to enable the global deployment of offshore storage for facilitating 2DS.

245 raction (SMORE) which pairs with an existing offshore structure.

246 e the cause of damage to ships at sea and to offshore structures.

247 ues in the design and operation of ships and offshore structures: how high can rogues be and how freq

248 Shallow slip offshore Sumatra appears driven by diagenetic strengthen

249 nsient fish and invertebrate species rely on offshore surface waters for egg and larval transport bef

250 eir life history in potentially contaminated offshore surface waters prior to their recruitment to ne

251 arine sediments, we collected sediments from offshore Svalbard that represent geochemical horizons wh

252 Using geophysical observations from offshore Svalbard to constrain a coupled ice sheet/gas h

253 ticles have recently reported on gas seepage offshore Svalbard, because the gas emission from these A

254 tly more abundant at sampling stations 300 m offshore than close to the shore.

255 ntrasts with adjacent areas to the south and offshore that have lower species richness, and higher te

256 coastal water to show that cyclones located offshore that were generated near the coast contain high

257 coast, the central Pacific Ocean, and waters offshore the Antarctica Peninsula.

258 earthquake that occurred on 27 February 2010 offshore the Maule region of central Chile triggered a d

259 Once offshore, the pressure anomalies generated shallow water

260 lumbia River plume from the mid-shelf, 20 km offshore, to the coast and eventually into Yaquina Bay (

261 (-), a relationship that held along a 550 km offshore transect in the North Pacific.

262 n station, whereas variability along onshore-offshore transects was driven by oxygen concentration in

263 ntrations in Asian rivers and variability in offshore transport across different types of estuaries.

264 play a quantitatively important role in the offshore transport of coastal water, substantially widen

265 on supplies voluminous clastic debris to the offshore trench, and vast quantities are subducted.

266 The offshore trend at the community level results from a con

267 patterns for marine AO across a wide onshore/offshore trophic gradient.

268 nd, over 50 GW will be required from shallow offshore turbines.

269 undiscovered oil may be found there, mostly offshore under less than 500 meters of water.

270 s occurring in the northwestern Adriatic Sea offshore Venice at 17-24 m depth.

271 ated water is the largest contributor to the offshore waste stream.

272 the intersection of iron-poor, nitrate-rich offshore waters and iron-rich, nitrate-poor coastal wate

273 bution within ice moderates iron delivery to offshore waters and likely also affects the subsequent o

274 parameters and guiding threat assessments in offshore waters and represent an important initial step

275 at fecal indicator microbe concentrations in offshore waters from Lake Pontchartrain returned to preh

276 dual and combined data sets from coastal and offshore waters impacted by the DwH spill further reveal

277 ply of larvae is limiting, and events in the offshore waters, such as wind-driven upwelling, explain

278 Offshore, we find evidence for efficient terrestrial org

279 ane emission measurements at three abandoned offshore wells in the Central North Sea (CNS) were condu

280 Oil spill simulations for 19 existing offshore wells were carried out based on novel and high

281 t while the eastern limit extends several km offshore, where it is defined seismically by a ~40-45 de

282 ability of detection decreased beyond 2.1 km offshore, whereas visual sightings revealed consistent w

283 trations in their muscle than specimens from offshore, which confirms mineral dissolution in their gu

284 e day tends to displace and deposit material offshore, which partially sets up the system by the earl

285 Tagging studies suggest that while offshore, white sharks may forage at depth on mesopelagi

286 available technologies, few of them consider offshore wind and wave energy as contenders in future ze

287 sk--can greatly enhance the probability that offshore wind can help to meet the United States' electr

288 ramework to assess potential conflicts among offshore wind energy, commercial fishing, and whale-watc

289 ssess life cycle inventories of a conceptual offshore wind farm using a hybrid life cycle assessment

290 that would be destroyed by hurricanes in an offshore wind farm.

291 on underwater marine organisms, particularly offshore wind farms and marine energy converters (e.g.,

292 ns with other anthropogenic pressures, using offshore wind farms and the Taiwanese white dolphin (Sou

293 We apply this model to estimate the risk to offshore wind farms in four representative locations in

294 Imminent development of offshore wind farms on the outer continental shelf of th

295 results of the three tidal stream devices to offshore wind power plants (without considering water de

296 had on average 3.5 times higher impacts than offshore wind power.

297 pacity credits that should be recognized for offshore wind resources supplying power demands for Jian

298 ckling has been observed in typhoons, but no offshore wind turbines have yet been built in the United

299 e Continuous Plankton Recorder (CPR) survey (offshore) with multiple long-term fixed station-based ti

300 4)Cs and (137)Cs throughout waters 30-600 km offshore, with the highest activities associated with ne