ライフサイエンスコーパス: coastal

1 data collected from 447 mountain goats in 10 coastal Alaska, USA, populations over a 37-year time spa

2 fferent GCM/emissions scenarios relevant for coastal Alaska.

3 strumental records show a recent increase in coastal Alaskan precipitation and Aleutian Low intensifi

4 is expected to be particularly important in coastal and agricultural areas.

5 ador, vector-borne diseases are present from coastal and Amazonian regions to the Andes Mountains; ho

6 These maps integrate the biogeography of coastal and deep-sea, pelagic and benthic environments,

7 a tool to reduce nutrient over enrichment in coastal and estuarine ecosystems through the feeding act

8 Coastal and estuarine habitats experience annual pH vari

9 System from Sargasso Sea breeding grounds to coastal and freshwater habitats from North Africa to Sca

10 flooding are nearly equally divided between coastal and inland areas.

11 (10 pairs of 20 forests) that consisted of a coastal and inland forests on the same latitude to deter

12 ste management are increasing challenges for coastal and inland regions, with high-salinity brines pr

13 For coastal and inland wetlands combined, MAT and MAP explai

14 Coastal and marine environments can begin up to 100 kilo

15 itu microbial processes (up to 55 days) in a coastal Antarctic site.

16 may not only have to contend with increasing coastal anthropogenic activities, but also have to adapt

17 ognized as a major driving forcing affecting coastal aquifer system, and deterministic modeling has b

18 ng management of groundwater extraction from coastal aquifers.

19 raminifera that inhabit a thermally polluted coastal area in Israel, where they are exposed to elevat

20 rice landrace Horkuch, endemic to the saline coastal area of Bangladesh, was used in this study as th

21 While most of Earth's coastal areas are at risk, areas that will be affected f

22 multivariate statistics to show that shallow coastal areas are extremely sensitive to changing non-li

23 el rise, especially for species that rely on coastal areas for reproduction.

24 antification, the sea level rise impact over coastal areas has to be superimposed, implying that the

25 The air quality of many large coastal areas in the United States is affected by the co

26 changing climate, and reveal the impacts on coastal areas of increasing ice mass loss and the associ

27 of low quality due to high content of NaCl (coastal areas or areas where underground water is saline

28 As global climate warms and sea level rises, coastal areas will be subject to more frequent extreme f

29 any large population centers located in near-coastal areas, and increasing evidence that various nano

30 ratures remain above freezing in the oceans, coastal areas, and parts of the Tropics, but photosynthe

31 For successful remediation in coastal areas, permanent binding of mobile P in anoxic s

32 cies in the pelagic and deep-sea compared to coastal areas.

33 cause increased inundation of many low-lying coastal areas.

34 verlooked in marine systems, particularly in coastal areas.

35 Here we show a series of data from a coastal arsenic-contaminated soil exposed to sea and riv

36 spatial structure of a population complex of coastal Atlantic cod (Gadus morhua).

37 seasons significantly increased within many coastal Atlantic regions between 40 degrees N and 60 deg

38 uggested at-sea exchange did not fully flush coastal Bacteria from all tanks; there were several inst

39 findings establish that including realistic coastal baroclinic processes in forecasts of storm inten

40 show that with rising sea levels, cliffs and coastal barriers will be subject to significantly greate

41 orphological development of west Scandinavia coastal basement rocks during the Mesozoic and later, lo

42 d Bodega Bays in California and the Virginia coastal bays) represent a range of life histories (annua

43 responsible for runoff-associated inland and coastal beach closures) in stormwater biofilters (a comm

44 x values over the surface area of the lakes' coastal boundary zone suggested volatilization may be re

45 Small parts of southern coastal British Columbia become progressively suitable w

46 Thus, coastal C. ignobilis were a biological vector transporti

47 ra) and bumble bee (Bombus spp.) foragers in coastal California from 1999, when feral A. mellifera po

48 rosol particles influenced by wildfires at a coastal California site in the summers of 2013 and 2016.

49 uaries extend inland into density-stratified coastal carbonate aquifers containing a surprising diver

50 uence of prehistoric tsunami deposits from a coastal cave in Aceh, Indonesia.

51 Pteropods from the coastal CCE appear to be at or near the limit of their p

52 iring the developing economies of equatorial coastal cities and the habitability of low-lying Pacific

53 n of aerosol samples during 2015-2016 in two coastal cities at both the African (Bizerte, Tunisia) an

54 ooding only or ocean flooding only), whereas coastal cities vulnerable to SLR are at risk for floodin

55 14 PM10 samples collected in a northeastern coastal city in Brazil.

56 l spatial and temporal dynamics of Skagerrak coastal cod.

57 rican ancestry, such as individuals from the Coastal Colombian region (odds ratio, OR 2.06; 95% CI 1.

58 Nearshore coastal communities are often dependent on the habitat a

59 Coastal communities throughout the world are exposed to

60 We thus predict that tropical coastal communities will be seriously endangered as the

61 l marshes) seagrasses are thought to provide coastal defence and encourage sediment stabilisation and

62 udies, including the decline of coral reefs, coastal defences from flooding, shifting fish stocks and

63 ns on the short-term response of a resident, coastal delphinid species.

64 Well-planned coastal development near mangrove forests will be essent

65 the importance of rethinking the impacts of coastal development projects, especially regarding the h

66 stores, functions that have been degraded by coastal development, destructive fishing practices, and

67 the photodefence mechanisms developed by the coastal diatom Skeletonema marinoi were performed.

68 ange of 300 km per generation; (ii) leapfrog coastal dispersals yield the best results (quantitativel

69 arine bacteria, despite their importance for coastal ecosystem functions.

70 Seagrass meadows are the most widespread coastal ecosystem on the planet.

71 s on multiple ecosystem functions underlying coastal ecosystem services.

72 Coastal ecosystems affect human well-being in many impor

73 cation, a major nitrogen (N) loss pathway in coastal ecosystems and both a source and sink of N2 O.

74 These coastal ecosystems are also susceptible to the impacts o

75 As coastal ecosystems are especially impacted by elevated n

76 Eutrophication of coastal ecosystems is a global problem that often result

77 Seagrasses are a major component of coastal ecosystems offering important ecosystem services

78 may have profound negative implications for coastal ecosystems reliant on this keystone species.

79 These coastal ecosystems support valuable fisheries and endang

80 es will greatly reduce their availability to coastal ecosystems, our results clearly indicate that ri

81 creases in sea levels are expected to affect coastal ecosystems.

82 s may have reduced the fishery production of coastal ecosystems.

83 ntial consequences for human populations and coastal ecosystems.

84 es, especially in redox-dynamic sediments of coastal ecosystems.

85 tween bays, and comparable to those in other coastal ecosystems.

86 a substantial loss of N removal capacity in coastal ecosystems.

87 ibute substantially to primary production in coastal ecosystems.

88 riability in dengue transmission in southern coastal Ecuador.

89 ) was used to identify microorganisms from a coastal environment that assimilate nitrogen from methyl

90 ght on Hg contamination sources for biota in coastal environment.

91 vant for understanding carbon fluxes in cold coastal environments and provides valuable information f

92 Before enhanced weathering of olivine in coastal environments can be considered an option for rea

93 When implemented in coastal environments, olivine weathering is expected to

94 ffluent is a recognized source of N and P to coastal environments.

95 ntermediate, nitrite, rarely accumulating in coastal environments.

96 tes of potential land losses associated with coastal erosion and lengthening of the coastal ice-free

97 Estimated coastal erosion losses were also larger for RCP8.5.

98 ncentrations on phytoplankton communities in coastal eutrophic environments.

99 results improve the understanding of Arctic coastal evolution in a changing climate, and reveal the

100 oduction, which impacts our understanding of coastal FDOM sources and early sediment diagenesis.

101 trophic levels, potentially re-defining the coastal fish communities of the future.

102 ted, since countries with high dependency on coastal fisheries receive very little larval supply from

103 to contribute to the effective management of coastal fisheries.

104 many heavily populated regions to increased coastal flooding and erosion hazards.

105 to numerous and increasing threats, such as coastal flooding and erosion, saltwater intrusion and we

106 global-scale analysis of the main drivers of coastal flooding due to large-scale oceanographic factor

107 So far, global-scale estimates of increased coastal flooding due to sea-level rise have not consider

108 storm surge models to estimate increases in coastal flooding on a continuous global scale.

109 For catastrophic coastal flooding, when wind-driven storm surge inundates

110 pidly increase the frequency and severity of coastal flooding.

111 sea-level rise, increasing the frequency of coastal flooding.

112 tion rates of urea-derived N in samples from coastal Georgia, USA (means +/- SEM: 382 +/- 35 versus 7

113 nd DOC production and consumption within the coastal groundwater correspond with a microbial communit

114 ssential cues for understanding and managing coastal habitats and fish populations.

115 e exacerbating seasonal acidification, OA of coastal habitats could represent a significant bottlenec

116 and aids in resilience and recovery of these coastal habitats.

117 vironment as well as navigability toward old coastal Harappan and historic towns in the region.

118 As exposure to coastal hazards increases there is growing interest in n

119 looding from multiple drivers (e.g., extreme coastal high tide, storm surge, and river flow).

120 otential for spatiotemporal stability of the coastal hybrid form and providing resilience against int

121 Coastal hypoxia (dissolved oxygen </= 2 mg/L) is a growi

122 nce should incorporate the growing threat of coastal hypoxia and include support for increased detect

123 Here we show that the lack of coastal ice in the Pacific sector of Antarctica leads to

124 (WAIS) has been warm ocean water underneath coastal ice shelves, not a warmer atmosphere.

125 with coastal erosion and lengthening of the coastal ice-free season for 12 communities.

126 However, a quantitative record of coastal impacts is spatially limited and temporally rest

127 Millions of coastal inhabitants in Southeast Asia have been experien

128 sea-level rise projections to assess future coastal inundation in New York City from the preindustri

129 the Antarctic ice sheet in assessing future coastal inundation.

130 are well studied, we focus on its effects on coastal islands of freshwater forest in Florida's Big Be

131 cal mixed-layer water and the water from the coastal jet separation site.

132 s (sediment, water column and fish gut) in a coastal lagoon under anthropogenic pressure.

133 We surveyed the behavioral intentions of coastal landowners with respect to various conservation

134 s that are dynamically re-shaping the unique coastal landscape of the Big Bend.

135 of 10 bacterial strains isolated from three coastal lichens Lichina confinis, Lichina pygmaea and Ro

136 Coastal lighting may shape intertidal communities throug

137 observations of ambient SSA observed at two coastal locations.

138 Coastal Louisiana has lost about 5,000 km(2) of wetlands

139 may account for the higher vulnerability of coastal Louisiana wetlands compared to their counterpart

140 tes spanning ~430 kilometers of shoreline in coastal Louisiana, Alabama, and Mississippi, using data

141 iophysical connectivity remotely, supporting coastal management in data-limited regions.

142 toration and conservation are increasingly a coastal management priority.

143 committed to protecting 10%-20% of national coastal marine areas.

144 er recreation at urban waterways, lakes, and coastal marine beaches is responsible for costs that sho

145 Overfishing threatens the sustainability of coastal marine biodiversity, especially in tropical deve

146 of toxicity experiments on a representative coastal marine diatom species Chaetoceros curvisetus usi

147 terrestrial sediment runoff and a downstream coastal marine ecosystem and contrast the cost-effective

148 Coastal marine ecosystems can be managed by actions unde

149 potential to alter food web dynamics within coastal marine ecosystems in Alaska.

150 rol at local, regional, and global scales in coastal marine ecosystems, and the potential implication

151 oximately 15% of the primary productivity in coastal marine ecosystems, fix up to 27.4 Tg of carbon p

152 ion assessments of sea turtle populations in coastal marine ecosystems.

153 rine organic matter on the trophodynamics of coastal marine food webs is not well understood.

154 Chemical analysis of an Australian coastal marine sediment-derived fungus, Phomopsis sp. (C

155 We document 289 living Japanese coastal marine species from 16 phyla transported over 6

156 noplectus americanus and Spartina patens) in coastal marshes of North America and has potential to dr

157 tanks in an indoor mesocosm facility, and in coastal mesocosms under pCO2 levels ranging from 400 to

158 ineage that may stem from a late Pleistocene coastal migration into the Americas.

159 hese studies because of its association with coastal migration models and genetic ancestral patterns

160 permafrost distribution are likely to alter coastal morphodynamics.

161 were not oriented towards the colony though coastal navigation was unaffected.

162 These unique coastal niches may be reflected in specific evolutionary

163 ese results corroborate the observation that coastal nitrogen pollution occurred earlier than the 19t

164 Through a novel coastal OA observing network, we have uncovered a remark

165 Coastal OC increases from Bohai Sea (0.52%) to South Sea

166 A field programme in the coastal ocean using a swarm of these robots programmed w

167 lved iron and thus enhance its export to the coastal ocean.

168 ification over short time scales and that as coastal oceans continue to acidify, negative effects on

169 the phototransformation of algal products in coastal or estuarine surface waters.

170 ear the ocean margins, with implications for coastal organisms and ecosystems.

171 of species in particular environments (e.g., coastal, pelagic), without a global map of realms based

172 datasets resolved the classic Gulf-Atlantic coastal phylogeographic break, which was not significant

173 lation of MWCNTs transport in Brier Creek, a coastal plain river located in central eastern Georgia,

174 ases (methane, krypton) were injected into a coastal plain stream in North Carolina to quantify strea

175 quatic emergent plants in the Alaskan arctic coastal plain, Carex aquatilis and Arctophila fulva, to

176 trend of Arctic sedimentary coasts along the coastal plains of Alaska, Siberia and western Canada, an

177 rise elicits short- and long-term changes in coastal plant communities by altering the physical condi

178 r (MW-fractionated DOM) in the catchment and coastal plume of a small peat-draining river over a seas

179 transformed fish cells [6-8], or products of coastal pollution [9, 10].

180 ional cooking treatments used by prehistoric coastal populations for processing aquatic faunal resour

181 water sodium (DWS) on blood pressure (BP) in coastal populations in Bangladesh.

182 mmon dentex (Dentex dentex), a Mediterranean coastal predator, in relation to the oscillations of the

183 na alterniflora (Loisel.) near an engineered coastal protection defences to discover the potential in

184 Coastal protection design heights typically consider the

185 Mangroves enhance fisheries and coastal protection, and store among the highest densitie

186 e leads to improved air quality in developed coastal provinces with a net effect of 78,500 avoided de

187 ated places were distributed in southeastern coastal provinces.

188 y, whole genome sequencing revealed that the coastal region harbours a hybrid form characterised by a

189 s population and assets located in low-lying coastal regions all around the world.

190 and ecologically important species native to coastal regions and estuaries of the Gulf of Mexico - ha

191 Results show that 75% of coastal regions around the globe have the potential for

192 ntion, dominant flow and dispersal range for coastal regions at the global scale.

193 ay aerosol (SSA) impact trace gas budgets in coastal regions by acting as a reservoir for oxidized ni

194 Rapidly developing coastal regions face consequences of land use and climat

195 Wastewaters in coastal regions may contain elevated levels of bromide (

196 t to human seafood consumers and wildlife in coastal regions worldwide.

197 dence for the occurrence of AMDEs outside of coastal regions, and their importance to net Hg depositi

198 In most coastal regions, the amount of sea-level rise occurring

199 Despite being globally widespread in coastal regions, the impacts of light pollution on inter

200 ermal events, and frequent rainfalls in some coastal regions.

201 2004 Indian Ocean tsunami caught millions of coastal residents and the scientific community off-guard

202 val between the earthquake and tsunami, many coastal residents lost their lives.

203 engineering approaches intended to increase coastal resilience in a changing ocean.

204 sent an overview of the options available to coastal resource managers during a time of environmental

205 force anomalous oceanographic conditions and coastal response along the Pacific margin, exposing many

206 e we report on the oceanographic forcing and coastal response of the 2015-2016 El Nino, one of the st

207 ive processes and their roles in restraining coastal restoration efforts.

208 ectory backtracking, we identify present-day coastal retention, dominant flow and dispersal range for

209 ffered in shelf and estuarine sediments from coastal Rhode Island over a seasonal cycle.

210 ional forecasting and, consequently, greater coastal risk during hurricane events.

211 to a demic process driven by dispersal along coastal routes.

212 Considering the likely increasing trend in coastal salinity, prompt action is required.

213 ronmental records from a southern California coastal saltmarsh reveal evidence for repeated late Holo

214 Urban coastal seawater exposure increases the incidence rates

215 ion, surface snow, streams from melted snow, coastal seawater, and plankton samples were collected ov

216 mmunities, and our results thus suggest that coastal seaweed assemblages in eutrophic waters may unde

217 in regulating GHG production and exchange in coastal sediment ecosystems.

218 Coastal sediments are important GHG producers, but the c

219 Terrestrial freshwater inputs to coastal sediments were identified as the primary source

220 solved organic matter (DOM) in estuarine and coastal sediments, although its role in the production o

221 d to OC through inner-sphere complexation in coastal sediments, as much as four times more than in lo

222 es, to methane and nitrous oxide fluxes from coastal sediments.

223 e U.S. Atlantic coast and in other urbanized coastal settings.

224 s reduced the size and population density of coastal shellfish: previously it was thought that overha

225 baco Island) based on overwash deposits in a coastal sinkhole, which indicates that the ITCZ has like

226 (-3), respectively) compared to the European coastal site (1.0 and 0.08 pg m(-3), respectively).

227 ages of respective spring sea-ice melting at coastal sites in northeast Greenland and eastern Antarct

228 to impact arsenic release from contaminated coastal soils by changing redox conditions.

229 hich arsenic may be released in contaminated coastal soils due to sea level rise are unknown.

230 senic release from historically contaminated coastal soils through reductive dissolution of arsenic-b

231 ploit carbon substrates during summer in the coastal Southern Ocean.

232 ented transoceanic survival and dispersal of coastal species by rafting.

233 Coastal species might be most affected, however, by floo

234 for understanding the potential responses of coastal species to sea-level rise, especially for specie

235 Sea-level rise will affect coastal species worldwide, but models that aim to predic

236 icantly to reciprocal air temperature at the coastal station Rao and over the Baltic, but only weakly

237 Geologic evidence for extreme coastal storms during past warm periods has the potentia

238 across analyzed sectors-agriculture, crime, coastal storms, energy, human mortality, and labor-incre

239 was genetically partitioned into inland and coastal subpopulations, separated by a central region do

240 atsa (Atyidae) are restricted to specialised coastal subterranean habitats or nearby freshwaters and

241 in the Chesapeake Bay and in the many other coastal systems facing similar stressors.

242 ess the global challenge of OA in productive coastal systems.

243 uce larger quantities of potent LMW-DON into coastal systems.

244 fully assessing the risk posed to vulnerable coastal systems.

245 HOC profiles in coastal T. truncatus from Brazil and California revealed

246 sk of gastric cancer than inhabitants of the coastal town Tumaco, despite similar H. pylori prevalenc

247 on and stable isotope data from an inland-to-coastal transect show high soil Hg concentrations consis

248 e and are an important feature of marine and coastal tropical ecosystems.

249 vascular plant functional types found on the coastal tundra near Barrow, Alaska.

250 ew production and sinking particle export in coastal upwelling ecosystems.

251 stration in the California Current and other coastal upwelling ecosystems.

252 ring about sharp changes in the chemistry of coastal upwelling ecosystems.

253 ococcus maxima occurred in the North Pacific coastal upwelling for OI (36 713 +/- 1485 copies ml(-1)

254 reover, we show that a long-term increase in coastal upwelling translates via a bottom-up mechanism t

255 Virioplankton abundances at the coastal WAP show a pronounced seasonal cycle with intera

256 . vulnificus, particularly in the context of coastal warming.

257 ts for compound flooding from river flow and coastal water level, and we show that a univariate appro

258 Degradation of coastal water quality in the form of low dissolved oxyge

259 These results illustrate how variability of coastal water temperature (and associated properties suc

260 al assemblages differed from those of local, coastal water.

261 s reduced nutrient discharges; however, many coastal waterbodies remain impaired.

262 , the effects of CO2 enrichment on eutrophic coastal waters are still unclear, as are the complex mec

263 puts may lead to more rapid acidification in coastal waters compared to the open ocean.

264 to monitor the environmental suitability of coastal waters for Vibrio spp. using remotely sensed SST

265 ution of redox reactions to acidification in coastal waters is unclear.

266 a range of organisms, biota in estuarine and coastal waters may be particularly vulnerable.

267 Increased climate variability and warming coastal waters may therefore increase the frequency of t

268 This suggests that nitrite peaks in coastal waters might be explained by differences in the

269 spiracids (AZAs) are being reported from the coastal waters of an increasing number of countries on a

270 in both the lateral boundary conditions and coastal waters surrounding the continental U.S. is exami

271 dissolved organic matter (DOM) to inland and coastal waters through increases in precipitation, thawi

272 ic carbon in glacial runoff and near surface coastal waters was aged (12100-1500 years BP (14) C-age)

273 but dissolved inorganic carbon and biota in coastal waters were young (530 years BP (14) C-age to mo

274 levels of fecal indicator bacteria in urban coastal waters, but it is unknown whether exposure to se

275 trification appears to be minor in temperate coastal waters, but may represent a significant portion

276 To alleviate eutrophication in coastal waters, reducing nitrogen (N) discharge from was

277 nces (PFASs) through riverine discharge into coastal waters.

278 rtion of the nitrification flux in Antarctic coastal waters.

279 important structural components for life in coastal waters.

280 pop-up satellite tags during escapement from coastal waters.

281 ill in U.S. waters, oiling large expanses of coastal wetland shorelines.

282 ovariance data from 22 inland wetland and 21 coastal wetland sites across the globe.

283 Coastal wetlands are known for high carbon storage withi

284 Coastal wetlands are sites of rapid carbon (C) sequestra

285 to their position at the land-sea interface, coastal wetlands are vulnerable to many aspects of clima

286 To avoid submergence during sea-level rise, coastal wetlands build soil surfaces vertically through

287 nal organizations and enterprises to restore coastal wetlands for enhancing blue carbon sinks.

288 contrasting of CO2 fluxes between inland and coastal wetlands globally can improve our understanding

289 Coastal wetlands had higher annual gross primary product

290 d and loss models to quantify the impacts of coastal wetlands in the northeastern USA on (i) regional

291 At the landscape scale, the coastal wetlands of the South East Queensland catchments

292 On a per unit area basis, coastal wetlands provided large CO2 sinks, while inland

293 bility for inland wetlands and decreased for coastal wetlands with increasing latitude.

294 as 93.15 and 208.37 g C m(-2) for inland and coastal wetlands, respectively.

295 in these environments include estuarine and coastal wetlands, such as marshes and mangroves, sand be

296 determined by GPP and Re for both inland and coastal wetlands.

297 llenge of managing change is daunting in the coastal zone where diverse human pressures are concentra

298 and increase the vulnerability of the Arctic coastal zone.

299 Our findings have implications in coastal zones worldwide that are affected by this toxin

300 ion, and upwelling introduce excess CO2 into coastal zones.