ライフサイエンスコーパス: coastal

1 n (- 0.06 +/- 0.45 mol C m(-2) year(-1)) and coastal (- 0.03 +/- 1.83 mol C m(-2) year(-1)) ocean are

2 of loss presents an immediate challenge for coastal adaptation.

3 oroalkyl substances in plasma in pelagic and coastal adult female polar bears with similar body condi

4 and anthropogenic change affecting Borneo's coastal and coral reef environments are lacking.

5 ry productivity and phytoplankton biomass in coastal and estuarine systems.

6 ted feedbacks, impeding their predictions of coastal and global responses to change.

7 major contributor to urban air pollution in coastal and inland riverside cities.

8 to monitor anthropogenic Cu contamination in coastal and marine ecosystems.

9 but are relatively understudied compared to coastal and open marine environments.

10 However, surface CO(2) in the central (coastal and open) GoM, which is influenced by Mississipp

11 s projections of future food web dynamics in coastal and shelf areas where droughts and stratificatio

12 fish and invertebrate species in the world's coastal and/or open ocean areas.

13 Seawater intrusion into coastal aquifers can increase groundwater salinity beyon

14 also arise from groundwater pumping in some coastal aquifers with water tables above sea level.

15 In addition to becoming wetter, the coastal area also experienced higher precipitation inten

16 cale with increasing trends in fall near the coastal area and in spring around the north area.

17 A total of 68% of the global coastal area flooded will be caused by tide and storm ev

18 0.05) in annual precipitation near the south coastal area of the LMRAV and only marginally increasing

19 prevalence around Madrid (>10%) and lower in coastal areas (<3%).

20 Together, this suggests that human use of coastal areas alters natural chemical cues, negatively a

21 traffic affect significantly air quality in coastal areas and the climate.

22 ry monitoring stations, primarily located in coastal areas around Ireland.

23 estern US but are not typically preserved in coastal areas due to environmental and physiological cha

24 ensive height reductions can be expected for coastal areas of France, Greece, Spain and northern Afri

25 ically suitable conditions in large parts of coastal areas throughout Latin America, Africa and South

26 have been reported in increasing numbers in coastal areas worldwide.

27 ts greater potential to fuel algal blooms in coastal areas, especially given the likelihood that thei

28 t loss of life and property upon landfall in coastal areas.

29 bined pico- and nanophytoplankton biomass in coastal areas.

30 els by 20-30% and 6-15% respectively, in the coastal areas.

31 e Amur Basin, rivers east of the Lena Basin, coastal basins of the Japan Sea, and the North Pacific I

32 rophyll levels were observed in a downstream coastal bay through remote sensing.

33 elagic bears had higher pollutant loads than coastal bears because (1) they feed on a higher proporti

34 ine ecosystems, particularly those within in coastal benthic environments.

35 te this framework with projection models for coastal birds, which are commonly depicted as vulnerable

36 two Cascade-Sierra populations than those of coastal birds.

37 maining putative representatives of the Tupi coastal branch, a small, admixed, self-reported Tupiniqu

38 50,000 years at RLB, yielding a snapshot of coastal California during Marine Isotope Stage 3.

39 ng clinical and pathological presentation in coastal cetaceans worldwide.

40 ng-term stability determines the fate of our coastal cities and cultural heritage.

41 We conclude that light pollution from coastal cities is likely having deleterious impacts on s

42 ) and Mumbai (43.08%) with less reduction in coastal cities.

43 The average annual increase in coastal CO(2) was 3.20 +/- 1.47 uatm year(-1) for the no

44 Barrier systems also protect interior coastal communities from storm surges and wave-driven er

45 11 to 2015 in a cohort of 7,491 residents of coastal communities in Iwate Prefecture directly impacte

46 t and flood-hazard-mitigation strategies for coastal communities in the Gulf of Mexico, especially th

47 In particular, our results suggest that coastal communities that are dependent on kelp forests w

48 jor risk to the safety and sustainability of coastal communities worldwide.

49 port and economic stability for East African coastal communities-a region of least developed countrie

50 ing the short-term socio-economic impacts on coastal communities.

51 ne primary production in both open-water and coastal communities.

52 rophication, respectively, on the decline of coastal coral communities following the development of t

53 emonstrate the value of mangroves as natural coastal defenses at global, national and local scales, w

54 e we show how the morphology of about 11,000 coastal deltas worldwide, ranging from small bayhead del

55 (cm yr(-1)) more than doubled after 1950 in coastal depocenters around North America.

56 Sediment is accumulating in coastal depocenters at a rate that matches or exceeds re

57 Recent work in the coastal desert plain, known as the Pampa de Mocan, chall

58 Accelerating coastal development is increasing the exposure of marine

59 Coastal dunes protect beach communities and ecosystems f

60 is driven by two current induced mechanisms: coastal "dynamic uplift" upwelling; and westward advecti

61 to achieve conservation objectives in rural coastal economies.

62 further offshore in the Southern California coastal ecosystem (CCE).

63 ation is becoming a vital tool to counteract coastal ecosystem degradation.

64 ly enhance our capacity to spatially predict coastal ecosystem function across scales based on easily

65 ation activities observed in the subtropical coastal ecosystem of the Pearl River Estuary and in soil

66 of extreme storm responses in a subtropical coastal ecosystem.

67 en assessing the influence of hypoxia on the coastal ecosystem.

68 Vegetated coastal ecosystems (VCEs; i.e., mangroves, salt marshes,

69 a pelagic predatory component of marine and coastal ecosystems alongside early penguins.

70 imary producers of cold and temperate marine coastal ecosystems and exhibit systemic defences against

71 Anthropogenic inputs into coastal ecosystems are causing more frequent environment

72 Estuarine-coastal ecosystems are rich areas of the global ocean wi

73 eplication of this approach across vegetated coastal ecosystems has the potential to support manageme

74 educes overall productivity and stability of coastal ecosystems in our oceans, but rarely are these c

75 The coastal ecosystems of temperate North America provide a

76 ostera marina are foundation species in many coastal ecosystems of the temperate northern hemisphere.

77 Between the land and ocean, diverse coastal ecosystems transform, store, and transport mater

78 As key primary producers in coastal ecosystems worldwide, any change in their iodine

79 groves are a ubiquitous component of healthy coastal ecosystems, associated with a range of habitats

80 uman activities than global average level in coastal ecosystems, which implied a strong recovery capa

81 run-off and mechanical disruption affecting coastal ecosystems.

82 n the broader conservation and management of coastal ecosystems.

83 st be considered in Blue Carbon estimates in coastal ecosystems.

84 o reduce human fishing impacts on marine and coastal ecosystems.

85 recording of carbon flows in terrestrial and coastal ecosystems.

86 otype CRD1 interestingly was most similar to coastal ecotype I in Fe physiology and Fe-related gene c

87 s after ~11 ka: eastern Pacific EN, La Nina, coastal EN (COA), and central Pacific or Modoki EN (CP).

88 y of priority and emerging contaminants in a coastal environment (Cadiz Bay, SW Spain) over the cours

89 tion to factors that are associated with the coastal environment in Peru.

90 ering tropical, temperate, arid, montane and coastal environments from 9.25oS to 43.75oS with 11 envi

91 se dynamics on the fate of bioavailable N in coastal environments susceptible to intermittent saltwat

92 primary producers in shallow freshwater and coastal environments, fulfilling important ecological fu

93 opportunities offered in the high-relief and coastal environs of La Riera may help to explain the hig

94 of delta shoreline changes show that serious coastal erosion actually started much earlier.

95 North Yorkshire, UK, to model the changes in coastal erosion within the last 7 kyr and for the first

96 d a large decline in sediment supply causing coastal erosion, following catchment disturbance through

97 ness are anticipated to lead to increases in coastal erosion.

98 role that small streams may play in driving coastal eutrophication in large water bodies.

99 cessing plant with potential consequences to coastal eutrophication.

100 viduals within a two-month period as a focal coastal event (<1 km radius).

101 uptake after its passage across the Florida Coastal Everglades in September 2017.

102 surfaces using thin-plate spline models with coastal exposure and elevation as predictors.

103 Mesoclimatic effects (cold-air drainage, coastal exposure and elevation) were determined from the

104 arity in coastal impact assessment modulates coastal exposure, reducing recent estimates of global co

105 Barrier islands are ubiquitous coastal features that create low-energy environments whe

106 ould provide a source of settlement cues for coastal fishes, drawing larvae towards shallow benthic h

107 xposure, reducing recent estimates of global coastal flood costs by ~16%, and population affected by

108 Coastal flood risks are rising rapidly.

109 So far, estimates of future coastal flooding frequency focus on endpoint scenarios,

110 Coastal flooding is increasingly common in many areas.

111 p are used to obtain projections of episodic coastal flooding over the coming century.

112 (st) century will see significant changes to coastal flooding regimes (where present-day, extreme-but

113 Here, we investigate the continuous shift in coastal flooding regimes by quantifying continuous rates

114 Given that coastal flooding will only worsen, we must reframe this

115 accelerating sea-level rise, and increasing coastal flooding.

116 In contrast to open-water communities, coastal food webs have greater interaction redundancy, w

117 cycles of iodine, including iodine levels of coastal food webs that underpin the nutrition of billion

118 ssociated fauna [1], while fishing can alter coastal food webs, reduce biodiversity, and lower ecosys

119 ntribution to SOC accumulation in a tropical coastal forest.

120 s rapidly lowers salinity, which can destroy coastal foundation species and their associated fauna [1

121 n zones: grass, transitional, and shrub in a coastal grassland.

122 o competing climate processes: Ice loss from coastal Greenland (increased surface melt), Antarctic ic

123 Here we compile and analyze ~250,000 coastal groundwater-level observations made since the ye

124 To document the scale of coastal habitat restoration projects in the two countrie

125 e set to dramatically alter available Arctic coastal habitat, with the potential loss of diversity an

126 ation is available about sharks that live in coastal habitats(3).

127 mangrove leaf litter is a predictable cue to coastal habitats, chemical information from mangrove lea

128 Large white sharks migrate seasonally from coastal habitats, where they primarily forage on pinnipe

129 abidae), introduced in 1913, rapidly invaded coastal habitats.

130 lation linkages, spatiotemporal dynamics and coastal habitats.

131 rise, deltas are increasingly vulnerable to coastal hazards as declining sediment supply and climate

132 ties of practice to better manage threatened coastal heritage.

133 captures observed latitudinal gradients and coastal hot spots of [Formula: see text]O flux and revea

134 The need to characterize and track coastal hypoxia has led to the development of geostatist

135 idespread oxygen depletion in coastal zones (coastal hypoxia)(1) and increases in the incidence of al

136 with Greenland warming, reduced sedimentary coastal ice rafted detritus contents indicate less sever

137 t coasts of the Antarctic Peninsula and even coastal ice-free areas in parts of continental Antarctic

138 we show how accounting for non-linearity in coastal impact assessment modulates coastal exposure, re

139 ring extreme storms is necessary to minimize coastal impacts.

140 global models that more robustly reflect the coastal interface.

141 LR, can complicate estimated trajectories of coastal inundation for resource management and urban pla

142 months after febrile illness in Western and coastal Kenya (1993-2016) for binding and neutralizing a

143 for Better Health [TUMIKIA]) trial, done in coastal Kenya from 2015 to 2017.

144 Over an entire single RSV season in coastal Kenya, nasal swabs were collected from members o

145 t of targeted HIV-1 prevention programmes in coastal Kenya.

146 NV) responses, which we found were common in coastal Kenya.

147 sex workers (FSW) and heterosexuals (HET) in coastal Kenya.

148 d on coarse anomaly event detection from two coastal lacustrine sediment archives.

149 cities and (b) in a field study in a shallow coastal lagoon covering a range of transfer velocities,

150 Coastal lagoon ecosystems are important natural carbon s

151 Sea level rise, coastal land subsidence, and increasing water demands wi

152 ; however, there is a threshold beyond which coastal land will be lost, and mitigation efforts should

153 ative, evergreen shrub, Morella cerifera, in coastal landscapes.

154 nuous paleo-river system or along the Tethys coastal line, which are well supported by at least three

155 emissions are localized, especially close to coastal lines, but significant emissions also exist on o

156 e species, including those of importance for coastal livelihoods.

157 f passenger species from both their original coastal location and those picked in the open ocean.

158 activity, with losses likely concentrated in coastal lowlands that are exposed to both wind and storm

159 In these coastal lowlands, the estimates show that nightlights de

160 The role of coastal mangrove wetlands in sequestering atmospheric ca

161 er past warmer climates, via flotation along coastal margins.

162 Human-driven threats to coastal marine communities could potentially affect chem

163 Antarctic shallow coastal marine communities were long thought to be isola

164 bright spots and the relative immaturity of coastal marine ecosystem restoration, it is likely to ad

165 global climate is having profound effects on coastal marine ecosystems around the world.

166 r, ongoing region-wide changes in productive coastal marine ecosystems in response to large-scale cli

167 Restoration of coastal marine ecosystems is perceived by many to be exp

168 sediments and nutrients from terrestrial to coastal marine ecosystems, and episodic but extreme rain

169 parameters which determine biomass flows in coastal marine food web: the trophic transfer efficiency

170 Examining coastal marine restoration through a historical lens sho

171 MPB and affect biogeochemical processing in coastal marine sediments.

172 ght spots clearly demonstrate restoration of coastal marine systems can be used as a nature-based sol

173 oration efforts across a suite of metrics in coastal marine systems to highlight 'bright spots'.

174 enriched in marine aerosols, particularly in coastal mid-latitude atmospheric environments, where it

175 Here, we assess existing coastal monitoring networks and regional models, existin

176 hydrologic inputs of N, blunting the rise in coastal N sources during the early phase of the Pearl Ri

177 hing and since overfishing is common in many coastal nations, we ask how MPAs can be designed specifi

178 By the end of the 18th century, the coastal native populations were declared extinct.

179 tude among tributaries, creating a mosaic of coastal nutrient inputs.

180 By combining fisheries catches in all coastal ocean areas and life-history traits of exploited

181 CIS (Wave-Current-surge Information System), Coastal Ocean Estuarine Dynamics Lab at Louisiana State

182 r, 14-71 kg of DOC, and 1-4 kg of DON to the coastal ocean per km of shoreline per day during late su

183 entennial climate variability in controlling coastal-ocean wave climate.

184 f organic matter, prior to its export to the coastal oceans.

185 an acidification impacts, but are lacking in coastal oceans.

186 l cluster in the inner area of Irpinia and a coastal one around Salerno province.

187 Reconciling Peruvian coastal paleoclimate data is critical for testing models

188 o interannual climate variation in the mesic coastal part of Douglas-fir's range; narrower rings and

189 sites (Huaca Prieta and Paredones) in north coastal Peru and document regular consumption of maize b

190 Archaeological proxies are important to the coastal Peruvian case because more commonly used paleocl

191 riant is also significantly more frequent in coastal Peruvian populations than in populations from th

192 helps to maintain cell viability in dominant coastal photoheterotrophic oligotrophs while promoting t

193 late Cretaceous to Eocene strata on the Gulf Coastal Plain (United States).

194 Ci/L occurred almost exclusively in confined Coastal Plain aquifers where old (low percent-modern car

195 stris) ecosystem (LPE) of the North American Coastal Plain is a GBH where disturbances are integral f

196 eneric diversity nor composition of the Gulf Coastal Plain molluscan communities.

197 tris Mill.) ecosystem has been lost from the Coastal Plain of the southeastern United States and only

198 conditions did not devastate the entire Gulf Coastal Plain, allowing molluscs to rapidly recolonise v

199 These threats are managed by coastal planers through the implementation of risk mitig

200 creasing concentration of wintering Scaup in coastal Poland and Germany (where lack of effective impl

201 In the Barents Sea, pelagic and coastal polar bears are facing various ecological challe

202 o suggests that continued sea level rise and coastal population growth could trigger future increases

203 at breeding birds from the relatively robust coastal population in the San Francisco Bay area wintere

204 ssible by recovering data from the Brazilian coastal population through the genomes of mestizo indivi

205 at for regional fisheries and the welfare of coastal populations dependent on the Arabian Sea for sus

206 pre-Columbian time, giving rise to the Tupi Coastal populations, and a single distinct migration sou

207 te, yet global models lack representation of coastal processes and related feedbacks, impeding their

208 sea levels and hence its role in modulating coastal protection levels, globally.

209 Results show that for the case of, no coastal protection or adaptation, and a mean RCP8.5 scen

210 of services provided to societies including coastal protection, fishing, and cultural practices.

211 LS) estimates of the volume and AGB of large coastal redwood Sequoia sempervirens trees from three si

212 nt over time, with highest prevalence in the coastal regions and low prevalence in the highlands and

213 The results show that for Europe, coastal regions are affected the most, with the United K

214 ally before 2050 for most (i.e., 70%) of the coastal regions in the United States.

215 In order to protect the coastal regions infrastructure, an accurate estimation o

216 oman times, distinct glass types produced in coastal regions of Egypt and the Levant used evaporitic

217 centrations than the West Florida Shelf, and coastal regions off Mexico and Cuba.

218 es are recurring high-energy disturbances in coastal regions that change community structure and func

219 sure to extreme events is a major concern in coastal regions where growing human populations and stre

220 move from high-copper-contaminated waters to coastal regions with low concentrations of copper.

221 ion immediately above sulfidic zones, but in coastal regions, higher nitrate concentrations probably

222 For many coastal regions, projections of global sea-level rise by

223 tionally well preserved record of Neandertal coastal resource exploitation on a comparable scale to t

224 ing new ways of working with this threatened coastal resource.

225 ects in the two countries, we identified 914 coastal restoration projects with an accumulated area of

226 ion coming from scientific papers, and 1,620 coastal restoration projects with an accumulated area of

227 anisms from dispersed to clumped can amplify coastal restoration yields as it generates self-facilita

228 nd should be preferentially investigated for coastal risk assessment.

229 reasingly important component of sustainable coastal risk management.

230 e Littorina and the topshell Gibbula) from a coastal rocky shore, we found that the capacity to predi

231 In the coastal S. denitrificans, the genes are arranged and exp

232 t uptake fluxes of carbon dioxide (CO(2)) in coastal salt marshes using dimensional analysis method f

233 d to the available transport data and longer coastal sea-level records.

234 ic nitrogen deposition on hypoxia in Chinese coastal seas.

235 Euplotes focardii, endemic of the Antarctic coastal seawater.

236 nd potential conflicts with other marine and coastal sectors in the future.

237 g nitrate-dependent sulfide oxidation to the coastal sediment isolate Sulfurimonas denitrificans.

238 py of 12 h light-dark cycle incubated marine coastal sediment.

239 n rates, underscoring the need for including coastal-sediment management in habitat-restoration proje

240 spill remediation efforts in beach sands and coastal sediments and underscore the role of uncultured

241 edulis-over 10 years (2009-2018) in a French coastal site contaminated by diffuse Cu anthropogenic so

242 Sea spray aerosol at the coastal site was frequently internally mixed with sulfat

243 re at risk from climate change; the study of coastal sites thus helps society prepare for climate cha

244 Coastal sites, clustered at the water's edge, are alread

245 of aquatic foods, including in ceramics from coastal sites, except in the Western Baltic where this t

246 ion actions, and helping enhance adaption of coastal societies to climate change in the Anthropocene.

247 in the smallest pieces (<5 mm) and far from coastal sources (>500 km).

248 nvironment though wastewater discharges from coastal sources remain largely unexplored.

249 In the US coastal southeast-where US pellet exports to the EU orig

250 open-ocean Halobates germanus and a related coastal species H. hayanus to understand mechanisms of t

251 Many (>45) 20-km coastal stretches particularly those near cities receive

252 a Meghna Delta (GBMD) is a large and complex coastal system whose channel network is vulnerable to mo

253 stimates for global organic carbon burial in coastal systems and should be considered as an impact of

254 ific, recovering sea otters are transforming coastal systems by reducing populations of benthic inver

255 e annually transported from inland waters to coastal systems making rivers a critical link between te

256 Glacial Maximum, we hypothesize that Arctic coastal systems were recolonized from many geographicall

257 for predicting CH(4) emissions in vegetated coastal systems.

258 quality of DOM exported from terrestrial to coastal systems.

259 soil nutrient gradient spanning a series of coastal terraces in Mendocino, California.

260 cantly revised if active margins, with steep coastal topographies like the Canterbury margin, are con

261 the USA) and the USA a greater proportion in coastal upland habitats (21% versus 9% in China).

262 % of which occurs in the tropics, and 20% in coastal upwelling systems that occupy less than 3% of th

263 with samples spanning an ocean gradient from coastal upwelling to the oligotrophic South Pacific Subt

264 ence of at least two new lineages within the coastal upwelling zone, revealing an unexpectedly high l

265 We observed habitat compression of coastal upwelling, changes in availability of forage spe

266 ive effects of wetlands varies widely across coastal US counties with an average value of about $1.8

267 understood in marine systems, but cues from coastal vegetation can provide sensory information guidi

268 eres associated with convergent evolution to coastal versus oceanic environments.

269 ited, port-injected natural gas engines on a coastal vessel while under normal operation.

270 For this purpose, paddy top soil from a coastal Vietnamese delta was spiked with selected freque

271 he anomalous coastal winds are forced by the coastal warming.

272 man pathogen Vibrio vulnificus inhabits warm coastal waters and asymptomatically colonizes seafood, m

273 Cable deployments in coastal waters are increasing worldwide, in capacity and

274 generalist predator endemic to the temperate coastal waters around southern Australia.

275 Trophic downgrading in coastal waters has occurred globally during recent decad

276 Shallow, coastal waters identified here should be considered prio

277 concentrations significantly before entering coastal waters in Chandler Fjord.

278 sults suggest that episodic acidification of coastal waters might limit the ability of pueruli to loc

279 Nevertheless, in the cold coastal waters of the Antarctic, these degraders seem to

280 t content event (i.e., a marine heatwave) in coastal waters of the northern Gulf of Mexico resulted f

281 have quantified groundwater inputs to Arctic coastal waters under contemporary conditions.

282 in situ lignocellulose enrichment samples in coastal waters were traced and statistically analysed.

283 stem models, we project that the mean TTE in coastal waters would decrease from 7.7% to 7.2% between

284 In open and coastal waters, drivers were identified as a biological

285 us occurred among seals along North-European coastal waters, significantly impacting seal populations

286 his vulnerable species at kilometre scale in coastal waters.

287 d temperature, sea level and salinity across coastal waters.

288 sition is an important source of nitrogen to coastal waters.

289 Our approach is transferable to other coastal watersheds pursuing nitrogen reduction goals, bo

290 Coastal wetlands dampen the impact of storm surge and st

291 creasing recognition of the critical role of coastal wetlands in mitigating climate change, sea-level

292 insights into the CO(2) uptake potential of coastal wetlands in response to changes in key environme

293 s and the persistence of mangroves and other coastal wetlands under future scenarios of climate chang

294 fset the carbon burial rates in low-salinity coastal wetlands, there is hitherto a paucity of direct

295 model experiments further show the anomalous coastal winds are forced by the coastal warming.

296 ribution in surface sediments of the Belgium coastal zone (BCZ) and the anoxic Gotland basin (GB).

297 onsidering both natural and human factors in coastal zone defense policy.

298 uency and intensity of hypoxic events in the coastal zone, which have the potential to affect marine

299 en (N) loads, widespread oxygen depletion in coastal zones (coastal hypoxia)(1) and increases in the

300 Coastal zones, the world's most densely populated region