ライフサイエンスコーパス: sea

1 Oligocene (33.9 to 23.0 Ma) based on TEX(86) sea surface temperature (SST) estimates from southwester

2 glacial-interglacial cycles (MIS 100 to 95), sea levels were distinctly lower than before, strongly s

3 ates that give ample chance to escape from a sea lion-sized predator, but humpback whales could captu

4 Based in part on experiments in a sea-anemone model system, we targeted the gene encoding

5 riage were travelling to Asia, swimming in a sea/ocean, and not changing the kitchen towel daily.

6 tative Concentration Pathways 8.5, suggest a sea level contribution of 9.1-14.9 mm by 2100.

7 lved enrichment in SSA were examined using a sea spray simulation chamber.

8 Our results indicate that (a) sea level rise is unlikely to decrease the SOM decay rat

9 A remarkable fact about sea-level extremes is the existence of spatial dependenc

10 ect spanning warm dry foothills (500 m above sea level) to cold wet treeline (3250 m asl) in Californ

11 ome coastal aquifers with water tables above sea level.

12 er 21, Texas, is the combination of absolute sea level rise and land subsidence.

13 We estimate a uniform absolute sea level rise rate of 1.10 mm +/- 0.19/a in the Gulf of

14 intensifying tropical cyclones, accelerating sea-level rise, and increasing coastal flooding.

15 veloped in the Nordic countries and adjacent seas but also how knowledge from these regions contribut

16 Air-sea flux estimates indicate the GoM open (- 0.06 +/- 0.4

17 ised remotely-sensed data (chlorophyll a and sea surface temperature) coupled with krill lipid data o

18 sses influence the wave characteristics, and sea surface temperature (SST).

19 cockroaches, crickets, moths, crayfish, and sea stars.

20 1-13) the ice sheet accelerates ice flow and sea-level rise(14-16).

21 e fisheries, and carbon services on land and sea).

22 ds of sea surface salinity (delta(18)Ow) and sea surface temperatures (SSTs) from the Bay of Bengal (

23 the resilience of communities to storms and sea-level rise.

24 by recording in situ bottom temperatures and sea levels observed at depths of 5 and 30 m from May 200

25 ation a far stronger part of land, water and sea management policies.

26 ks, stiff foams, fiber composites, wood, and sea ice, the effective mode I fracture energy depends st

27 cycle with clouds, rain, rivers, lakes, and seas; it is the only world known to presently have a vol

28 nhabited a mix of thick multiyear and annual sea ice year-round.

29 abundance at most breeding colonies, annual sea ice fluctuations often explained less than 10% of th

30 and annual variation of Arctic and Antarctic sea ice concentration and observe decreases in the mean

31 We suggest Antarctic sea ice and Atlantic overturning conditions favoured aby

32 ne mammals, will cope with changes in Arctic sea ice dynamics as historically ice-covered areas becom

33 The rapid decrease in Arctic sea ice is motivating development and increasing oil and

34 d by changes in the seasonal cycle of Arctic sea-ice that are forced by orbital variations and volcan

35 fluence of natural climate drivers on Arctic sea ice.

36 ne sedimentary records to reconstruct Arctic sea-ice fluctuations.

37 climate change, future loss of summer Arctic sea ice will accelerate the thawing of Siberian permafro

38 Sacoglossans are sea slugs, some of which eat algae, digesting the cells

39 ulturable state of V. cholerae in artificial sea water at 4 degrees C, whereas the mutation of hapR l

40 Ulva lactuca, commonly known as sea lettuce, is a fast growing seaweed in the North Atla

41 gical invasions in a changing world, such as sea lamprey in the Great Lakes.

42 Soft-bodied aquatic invertebrates, such as sea slugs and snails, are capable of diverse locomotion

43 We assess sea-ice changes in KB together with changes in polar bea

44 mptomatic sea stars compared to asymptomatic sea stars.

45 ebral oxygen delivery (CDO(2) ) by 12-19% at sea level and high altitude, whereas core heating by 1.5

46 health in navy sailors during deployments at sea.

47 Every year, hundreds of people die at sea because of vessel and airplane accidents.

48 summer solstice at 40 degrees N latitude at sea level on a clear day.

49 s of a naval ship on a practicing mission at sea were recruited and randomly provided with a blinded

50 fitness benefits of the migratory tactic at sea.

51 We compare at-sea whale density estimates to estimates derived from sa

52 tarily stow snagged debris; incentivizing at-sea removal may elicit further cooperation.

53 miting the validity of using GPS to infer at-sea behaviour when answering behavioural or ecological q

54 production and/or mineral sedimentation; (b) sea level fall events, predicted to double in frequency

55 reas of polar ice sheets were grounded below sea level during both glacial and interglacial periods,

56 icularly likely where water tables lie below sea level, but can also arise from groundwater pumping i

57 The mean duration between sea-ice retreat and advance increased from 109 to 160 da

58 rs prior led to increased targeting by black sea bass, resulting in decreased survival of the squid i

59 After 106 days, bleached sea anemones with anemonefish had an algal symbiont dens

60 l chlorophyll was 66% higher in the bleached sea anemones with anemonefish than the controls.

61 ast, recovery did not occur for the bleached sea anemones without anemonefish as they had 78% fewer a

62 ulnerable to morphological changes caused by sea level rise, subsidence, anthropogenic modifications,

63 ary production than in the region covered by sea ice.

64 forcing effects were predominantly driven by sea-surface temperature thresholds or inter-ocean temper

65 ed climate model simulations, were forced by sea surface temperatures (SSTs) and exacerbated through

66 by predicted global warming (+4 degrees C), sea level changes (simulated by altering of the inundati

67 astal wetlands in mitigating climate change, sea-level rise, and salinity increase, soil organic carb

68 gen deposition on hypoxia in Chinese coastal seas.

69 ting and thermoregulation for return to cold seas.

70 Greenland ice core to resolve and constrain sea ice variations during four D-O events between 32 and

71 gest cryospheric contributor to contemporary sea-level rise.

72 yndrome (SSWS), a disease that has decimated sea star populations across the West Coast of the United

73 we present the results of novel in situ deep sea plume experiments undertaken on the Tropic seamount,

74 In much of the deep sea (>200 m water depth), the export of nutrients from t

75 able against the dark background of the deep sea [5].

76 The deep sea plays a critical role in global climate regulation t

77 sly unobserved level of dynamism in the deep sea, potentially mirroring the great migrations so well

78 significantly to chemical fluxes in the deep sea, yet little is known about the microbial communities

79 planning of competing interests in the deep sea.

80 the challenges of observing them in the deep sea.

81 Deep-sea observation efforts that prioritize these variables

82 Conducting an expert elicitation (1,155 deep-sea scientists consulted and 112 respondents), our analy

83 of this unique life history trait in a deep-sea fish and fills in a gap in the larval literature for

84 Climate drivers will alter deep-sea biodiversity and associated ecosystem services, and

85 ysis indicates a wide consensus amongst deep-sea experts that monitoring should prioritize large orga

86 a(18)O record for global ice volume and deep-sea temperature variations.

87 Finally, deep-sea conservation efforts should focus primarily on vulne

88 This characterization of Galapagos deep-sea benthic invertebrate megafauna across a range of eco

89 -water coral and commercially important deep-sea fish species under present-day (1951-2000) environme

90 ce for seasonally recurring patterns in deep-sea demersal fish abundances over a 7-year period, and d

91 nderstanding life history strategies in deep-sea environments is lacking for many species of fishes.

92 he first systematic characterization of deep-sea benthic invertebrate communities of the Galapagos, a

93 sitivity, biodiversity, and dynamics of deep-sea ecosystems.

94 vity, biodiversity and distributions of deep-sea fauna, thereby compromising key ecosystem services.

95 into other novel reproductive modes of deep-sea fauna.

96 in (reflectance <0.5%) in 16 species of deep-sea fishes across seven distantly related orders.

97 minescent light organs (photophores) of deep-sea shrimp, an autogenic system in which the organism po

98 ts to deep-sea benthos, suggesting that deep-sea biodiversity hotspots are also likely to be micropla

99 known to supply oxygen and nutrients to deep-sea benthos, suggesting that deep-sea biodiversity hotsp

100 nantly anthropogenic, is transported to deep-sea trenches primarily in carrion, and then incorporated

101 p of Parablepharismea to the uncultured deep-sea class Cariacotrichea on the basis of single-gene ana

102 Here we present unprecedentedly detailed sea ice proxy evidence from two Norwegian Sea sediment c

103 l faults, and to recharge from rivers during sea level lowstands.

104 ariables characterizing North Atlantic: i.e. sea surface temperatures (SST) from the tropical cyclone

105 ody fat index was higher in years of earlier sea ice breakup with no change occurring in polar bears.

106 (ms-PAF) to a nonchemical stressor, elevated sea surface temperature.

107 Extreme sea levels are a significant threat to life, property, a

108 ted mean sea-level (MSL) changes and extreme sea-level (ESL) events.

109 rder to quantify its contribution to extreme sea levels and hence its role in modulating coastal prot

110 s stable in the presence of a metallic Fermi sea, and its universality class in the local magnetic re

111 tar-associated densovirus (SSaDV), the first sea star densovirus discovered, by documenting its bioge

112 in the Great Lakes, and the consequences for sea lamprey control efforts.

113 rounds are the most important tools used for sea lamprey population control.

114 changes in forearm vascular conductance from sea level: ACh1: -52.7+/-19.6%, ACh2: -25.4+/-38.7%, ACh

115 tent, and also perform predictions of future sea ice concentration.

116 f the sea ice behavior and to predict future sea ice behavior.

117 aureus strains carrying enterotoxin A gene (sea) causes food poisoning and cannot be distinguished f

118 arine heatwave framework to analyse a global sea surface temperature product and identify the most ex

119 omalies, and use an observation-based global sea surface temperature dataset to calculate thermal dis

120 ntarctica with large consequences for global sea level.

121 far the largest potential source for global sea-level rise under future warming conditions(1).

122 However, global sea-level change as a result of mass loss from ice sheet

123 plications for increasing the rate of global sea level rise.

124 many coastal regions, projections of global sea-level rise by the year 2100 (e.g., 0.5-2 meters) are

125 ontributed about 3 to 4 metres(13) to global sea levels.

126 o a longer-term context to understand global sea-level contributions, regional climate-glacier system

127 When global sea level rise exceeded the local rate of bank building,

128 action, a large or rapid Northern Hemisphere sea-level forcing enhances grounding-line advance and as

129 ctions, the inclusion of Northern Hemisphere sea-level forcing in our model increases the volume of t

130 f AIS grounding lines to Northern Hemisphere sea-level forcing is more complicated than previously mo

131 In the Late Holocene, sea ice expanded and regional climate became drier.

132 Marine ice (sea ice, ice shelf and glacier retreat) losses generate

133 The results obtained can be used to identify sea buckthorn cultivars, develop crops and production, a

134 Efforts to improve sea level forecasting on a warming planet have focused o

135 the climate drivers are central to improving sea level projections.

136 The bioaccumulation factor of PM(1) in sea anemones was approximately 5-7 orders of magnitude.

137 under positive selection in elapids, and in sea snakes they have undergone multiple shifts in spectr

138 This in turn leads to sustained anomalies in sea ice extent.

139 Using simulated changes in sea water temperature from three Earth system models, we

140 c abundance, distribution and composition in sea ice cores (n = 25) and waters underlying ice floes (

141 Experiments in sea cucumbers reveal how the physiological responses reg

142 Risk of S. neurona exposure in sea otters is associated with consumption of clams and s

143 t of SSWS.IMPORTANCE The primary interest in sea star densoviruses, specifically SSaDV, has been thei

144 l model for evolution of miRNA precursors in sea anemones and their relatives, revealing alternative

145 two genes encoding putative GHR and PRLR in sea lamprey (Petromyzon marinus) and Arctic lamprey (Let

146 Quantifying global trends and variability in sea surface temperature (SST) is of fundamental importan

147 that undergo significant annual variation in sea ice concentration.

148 uantitatively demonstrate that variations in sea level and organic carbon burial are the dominant con

149 e diversity and ubiquity of these viruses in sea stars confound the original hypothesis that one dens

150 eria and includes familiar animals including sea anemones, corals, hydroids, and jellyfish.

151 mplications for the Arctic region, including sea ice loss, increased geopolitical attention, and expa

152 reef-building corals to adapt to increasing sea-surface temperatures is often debated but has rarely

153 ssion electron microscopy in a drug-induced (sea anemone toxin, ATXII) Na(+) channel GOF isolated hea

154 The Cassini spacecraft discovered lakes/seas on Titan, however, it did not observe lakes/seas at

155 on Titan, however, it did not observe lakes/seas at the AO/GBT anomalously specular locations.

156 ing in the western Pacific and enhanced land-sea thermal contrast, leading to 28% more rainfall proje

157 es on surveys to monitor abundance of larval sea lamprey in Great Lakes tributaries.

158 (i.e., lamprey pesticides) to target larval sea lamprey and barriers to prevent adult lamprey from r

159 The two dominant drivers of the global mean sea level (GMSL) variability at interannual timescales a

160 iation(7), understanding why LIG global mean sea level may have been six to nine metres higher than t

161 e sheets during the LIG, causing global mean sea level to rise at least four metres above modern leve

162 ly-driven decadal variability of global mean sea surface temperature (GMSST) by using a unique datase

163 The rate of global-mean sea-level rise since 1900 has varied over time, but the

164 opagate into uncertainties in projected mean sea-level (MSL) changes and extreme sea-level (ESL) even

165 centration and observe decreases in the mean sea ice concentration from early to later periods, as we

166 t evidence to date, from naturally migrating sea turtles, for an ability to reorient in the open ocea

167 ater, resulting in a phenomenon called milky seas or sea sparkle.

168 antly from glaciers-has caused twice as much sea-level rise since 1900 as has thermal expansion.

169 ting genetic differentiation across a narrow sea strait.

170 ted effective enrichment of PFAAs in nascent sea spray aerosols (SSA), suggesting that SSA are an imp

171 1540 km and their elevations vary from near sea level to nearly 500 m.

172 ocean-atmosphere interactions in the Nordic seas, caused by the progressive decay of Northern Hemisp

173 nds and multidecadal variability in observed sea level on both global and basin scales, which we reco

174 Even in the absence of sea-level rise, deltas are increasingly vulnerable to co

175 ase in flavonols and antioxidant activity of sea buckthorn-apple juices.

176 has allowed mangroves to persist in areas of sea level rise, might result from changes in root produc

177 tered size distribution and concentration of sea spray, with consequences for tropical cyclone intens

178 d in berries and leaves of nine cultivars of sea buckthorn (Hippophae rhamnoides L.) of various ripen

179 The annual cycle of sea-ice habitat in KB shifted from a year-round ice plat

180 sition (KMD) is applied to satellite data of sea ice concentration for the Northern and Southern hemi

181 nd the overall abundance and distribution of sea lamprey in the Great Lakes.

182 nsight into spatial and temporal dynamics of sea ice concentration not apparent in traditional approa

183 omplexity of the spatio-temporal dynamics of sea ice makes it difficult to assess the temporal nature

184 reconstruct the spatio-temporal dynamics of sea surface temperature and oxygen isotopic composition

185 Here we test for the effects of sea level rise (SLR) and its interactions with elevated

186 ir contribution to the seasonal evolution of sea surface temperature, and discuss their potential imp

187 read kelp deforestation and the formation of sea urchin barrens.

188 nfrared flux and accelerates the freezing of sea ice.

189 of this study was to quantify the number of sea lice potentially exposed to sub-lethal concentration

190 chemical composition, and sensory quality of sea buckthorn-based smoothies.

191 which are in turn a function of the rate of sea level rise, sand availability, and stress of the pla

192 llennia is investigated using new records of sea surface salinity (delta(18)Ow) and sea surface tempe

193 walk on the underlying network structure of sea connections, highlighting its pivotal role in the de

194 m trends are harder to monitor than those of sea ice.

195 The apparent use of sea ice as a predator refuge also has implications for h

196 best explained by the temporal variations of sea surface temperature (SST, negative correlation) and

197 Lastly, we focus the study on sea star-associated densovirus (SSaDV), the first sea st

198 imate, air quality, and human health in open seas and coast lines.

199 but significant emissions also exist on open seas and oceans.

200 sulting in a phenomenon called milky seas or sea sparkle.

201 ing selection, more slowly than in any other sea urchin genus.

202 Overall, sea hares that developed under OW and/or OA exhibited a

203 uding indoor dust, outdoor air particulates, sea sediment, and river water.

204 ntents, both bearing information on the past sea-ice cover.

205 al substantial melting of the EAIS, and peak sea levels during MIS G7 (~2.75 Ma) and, perhaps, MIS G1

206 d central Lomonosov Ridge and that perennial sea ice remained present throughout the present intergla

207 lga Chlamydomonas sp. ICE-L thrives in polar sea ice, where it tolerates extreme low temperatures, hi

208 Predicted sea-level rise and increased storminess are anticipated

209 pared areas of habitat to areas of predicted sea level rise, development, and protected areas.

210 regulation of pigmented cells in the purple sea urchin Strongylocentrotus purpuratus, an emerging mo

211 mate deglaciation can explain the more-rapid sea-level rise compared with the last deglaciation.

212 ing with increasing temperature and receding sea-ice cover, is tightly connected to lower latitudes t

213 These overestimates are similar to recent sea-level rise projections to 2100 at some locations.

214 ent a probabilistic framework to reconstruct sea level since 1900 using independent observations and

215 In the eastern North Pacific, recovering sea otters are transforming coastal systems by reducing

216 Reduced sea ice may contribute to warming of Arctic air(4-6), wh

217 The HadCM3 simulations reveal that reduced sea ice leads to a strengthened Aleutian Low shifted wes

218 he reduction of Ekman pumping due to reduced sea ice-ocean surface stress.

219 iocidaris erythrogramma, two closely related sea urchins with highly divergent developmental gene exp

220 Relative sea level rise at tide gauge Galveston Pier 21, Texas, i

221 ntrolled by the competition between relative sea-level rise and sediment supply that drives lobe prog

222 ponse of mangroves to high rates of relative sea level rise (RSLR) is poorly understood.

223 Based on our results, sea side and land side tritium leakage monitoring system

224 stern US salt marshes now burdened by rising sea levels.

225 rbon sink functions and resistance to rising sea levels.

226 reeding, over time and in relation to rising sea surface temperature (SST) and diet composition.

227 coast were significantly attenuated by river-sea environmental dilution.

228 Sacoglossan sea slugs are able to maintain functional chloroplasts i

229 and D3 bioaccessibility in salmon, sardine, sea bass and hake.

230 readth) and environmental variables (season, sea surface temperature [SST] anomalies, El Nino occurre

231 -term satellite tracking dataset for several sea turtle species, combined with capture-mark-recapture

232 er and was formed on what was once a shallow sea.

233 ccus poor primary producers to sustain shelf sea food webs efficiently.

234 ement of carbon stocks accumulating in shelf seas could contribute towards a nation's greenhouse gas

235 xities of carbon transport and fate in shelf seas, and the geopolitical challenges of carbon accounti

236 Since sea anemones are opportunistic suspension feeders, they

237 rmed extraocular visual system, that of some sea urchins, which also possess chromatophores [1].

238 d demography of a damaging invasive species, sea lamprey (Petromyzon marinus), in the Great Lakes, an

239 mpetition (e.g. ghost shrimp, Caprella spp.; sea anemones, Actinia equina; cone snails, Conidae; male

240 ve reefs in shallow tropical and subtropical seas.

241 jections suggest the complete loss of summer sea ice by the middle of this century(1).

242 a based on its representation in symptomatic sea stars compared to asymptomatic sea stars.

243 mal Maximum, a time of elevated temperature, sea level and salinity across coastal waters.

244 have focused on determining the temperature, sea level and extent of polar ice sheets during Earth's

245 Agreement is not met, Antarctica's long-term sea-level contribution will dramatically increase and ex

246 We found that sea snakes underwent rapid adaptive diversification of t

247 Our analyses indicate that sea-level rise in recent decades has widely outpaced mar

248 Pfaller et al. report that sea turtles respond to odors from biofouled plastic debr

249 Here, we show that sea lampreys (Petromyzon marinus L.) have cutaneous papi

250 issions of previously stored Hg from thawing sea-ice, glaciers, and permafrost.

251 rs (49% and 49%, respectively) affecting the sea urchin embryogenesis activity.

252 mals, but principally those that feed at the sea surface or use the material as a habitat.

253 issions from the O(3) + I(-) reaction at the sea surface was investigated in laboratory and modeling

254 e longer wavelengths that dominate below the sea surface.

255 chnology improvements), edible food from the sea could increase by 21-44 million tonnes by 2050, a 36

256 As food from the sea represents only 17% of the current production of edi

257 ignaling proteins in sperm flagella from the sea urchin Arbacia punctulata.

258 ver the most accurate species tree given the sea of gene trees.

259 e functions of two Argonaute paralogs in the sea anemone Nematostella vectensis of the phylum Cnidari

260 s, is expressed in the nervous system in the sea anemone Nematostella vectensis, similar to its mamma

261 In the sea lamprey, GHR and PRLR displayed a differential but o

262 1) to disrupt edn, ednr and dlx genes in the sea lamprey, Petromyzon marinus.

263 nthropogenic surface-active chemicals in the sea surface microlayer.

264 of specific subgroups of N(2) fixers in the sea; these changes have implications for foodwebs and bi

265 Here, we leverage the sea urchin embryo for its well-established gene regulato

266 bolic rate of a keystone marine mollusc, the sea hare Stylocheilus striatus, a specialist grazer of t

267 Here we utilize the tentacles of the sea anemone Nematostella vectensis as an experimental pa

268 nto the temporal and spatial dynamics of the sea ice behavior and to predict future sea ice behavior.

269 response, tied to the time evolution of the sea-surface-temperature (SST) response.

270 Here, we focus on the sea surface microlayer (SML) as a vector for microplasti

271 n the Gulf of Mexico to its footprint on the sea surface.

272 e2 but not ShK-like1 is conserved throughout sea anemone phylogeny, we conclude that the two paralogs

273 Thus, sea-level rise is creating conditions within which Sesar

274 Here we apply causal discovery algorithms to sea level pressure data from a large set of climate mode

275 m and mast cells (MCs) can be traced back to sea urchins and the ascidian Styela plicata, respectivel

276 We mimic locomotion modes common to sea invertebrates using monolithic liquid crystal gels (

277 The sum of the contributions to sea-level change from thermal expansion of the ocean, ic

278 Sheet is the largest land ice contributor to sea level rise.

279 ) changing tidal regimes in mangroves due to sea level rise might attenuate increases in SOM decay ca

280 urrence of extreme water-level events due to sea-level rise.

281 nes per year) contributing 14 millimeters to sea level.

282 maintenance of barrier island resilience to sea-level rise and is used to extend hurricane records b

283 of peat soil development, and resilience to sea-level rise.

284 Cold edges shifted further and tracked sea surface and bottom temperature isotherms to a greate

285 lour score equal to the controls (unbleached sea anemones and without anemonefish), indicating recove

286 e were lower in the bleached than unbleached sea anemones, whereas total chlorophyll remained similar

287 Observational constraints using sea surface temperature patterns reduce the uncertaintie

288 ing to environmental changes, such as varied sea surface temperatures caused by storms.

289 The robustness of permafrost when sea ice is present, as well as the increased permafrost

290 the increased permafrost vulnerability when sea ice is absent, can be explained by changes in both h

291 also found that the area of the ocean where sea surface temperatures (SST) are within Trichodesmium'

292 ding a possible unifying explanation for why sea turtles interact with marine plastic.

293 ly, whereas increases were due to widespread sea ice loss during the first decade, the subsequent ris

294 es beach loss globally, will accelerate with sea level rise (SLR), causing more beach loss if managem

295 cally SSaDV, has been their association with sea star wasting syndrome (SSWS), a disease that has dec

296 Blue carbon change with sea ice and ice shelf losses has been estimated, but not

297 ollow mass extinctions and reef crises, with sea anemones and proteinaceous corals filling empty nich

298 well as their correlative relationships with sea surface temperature (SST).

299 ertical distribution of microplastics within sea ice cores.

300 Yet, sea-level values during Marine Isotope Stage (MIS) 101 (