ライフサイエンスコーパス: marine

1 accounted for the highest fraction of OA in marine (37 +/- 4%) and mixed air (31 +/- 3%), overriding

2 migration does not explain the appearance of marine adaptations in South Patagonia.

3 The marine air and continental-marine mixed air had more abu

4 roduction efficiency of OHDCA was highest in marine air, related to the presence of sulfur dioxide an

5 river inputs, and increased tidally induced marine algae and phytoplankton).

6 tigens, as well as the building block of the marine algal galactan lambda-carrageenan.

7 be made globally in germline preservation of marine algal species via germplasm banking with an overv

8 two new class-level lineages of free-living marine anaerobic ciliates, Muranotrichea, cl. nov. and P

9 Here we show that freshwater and marine anammox bacteria couple the oxidation of NH(4)(+)

10 of taxonomic groups inhabiting terrestrial, marine and freshwater habitats.

11 ause (1) they feed on a higher proportion of marine and higher trophic level prey, (2) they have high

12 very of methane (CH(4)) accumulation in oxic marine and limnic waters has redefined the role of aquat

13 Pd/Ir, Pt/Ir and Pt/Rh ratios are similar to marine and terrestrial sediments at the ETE, and very di

14 carbon isotope excursions (CIEs) recorded in marine and terrestrial sediments attest to the input of

15 TC, which responded increasingly strongly to marine animal, bird, mammal, and human faces.

16 Leveraging the microbiomes of marine animals and cutting-edge metabolomics and genomic

17 Marine animals are increasingly instrumented with enviro

18 ivities of these traits, which suggests that marine animals are under strong selection for the tolera

19 of the resulting physiological tolerances of marine animals predicts a variety of geographical niches

20 and XPS has been documented for a variety of marine animals, but principally those that feed at the s

21 mmunication in the ocean for humans and many marine animals.

22 organic carbon preservation associated with marine anoxia in Earth history.

23 44 Ma) and has been correlated with expanded marine anoxia lasting into the earliest Silurian.

24 Modelling supports the idea that widespread marine anoxia was induced by a greenhouse-driven weather

25 celled photosynthetic organisms that inhabit marine, aquatic and terrestrial ecosystems, diatoms cont

26 e fraction of natural sulfur released to the marine atmosphere.

27 ages in cultures of the dominant lineages of marine bacteria has contributed to an ongoing debate ove

28 Marine bacteria transform DMSP via two competing pathway

29 e identified several previously unrecognized marine bacterial lignin degraders.

30 sequences of lysogeny among several dominant marine bacterial lineages.

31 e evolutionary relationship to the Antarctic marine bacterium Marinomonas sp. BSw10506 and the sub an

32 we identified and characterized an AHGD from marine bacterium Vibrio variabilis JCM 19239 (VvAHGD).

33 rred from the sulfur isotopic composition of marine barite.

34 ght to have caused grounding-line retreat of marine-based sectors of the Antarctic Ice Sheet (AIS)(1-

35 n coincided with a similar transition in the marine benthic delta(18)O record for global ice volume a

36 onsequent changes in the amount of available marine benthic habitat.

37 For many marine benthic invertebrates, migration happens during r

38 In this study, samples of Antarctic marine benthic organisms were analyzed for legacy and em

39 The first synthesis of the marine benzoxepane hydroquinone cyclosiphonodictyol A an

40 tal zone, which have the potential to affect marine biodiversity and fisheries.

41 pper Kellwasser events, during which massive marine biodiversity losses occurred.

42 ghts the need to take stock of unique Arctic marine biodiversity.

43 Here, we report a reference genome for the marine biofilm-forming diatom Seminavis robusta, showing

44 The Arctic marine biome, shrinking with increasing temperature and

45 Our results suggest Arctic marine biomes persisted through cycles of glaciation, le

46 Our results show that marine bioprospecting is a dynamically growing field of

47 Proteins and peptides account for 20-75% of marine biota biomass, of which a major fraction is metab

48 c (man-made) sound has the potential to harm marine biota.

49 thylmercury (MeHg) are accumulated in Arctic marine biota.

50 al earth system models to project changes in marine biota.

51 Using the shell of the marine bivalve Atrina rigida as a model system, and thro

52 a and peptides is important in understanding marine carbon and nitrogen cycling.

53 ted, and it shows a combination of primitive marine chelicerate and derived arachnid characteristics.

54 to the 16-cell stage of the Ciona embryo, a marine chordate and performed a computational search for

55 lved some 500 million years ago in ancestral marine chordates.

56 c consortium associated to the psychrophilic marine ciliate Euplotes focardii, endemic of the Antarct

57 a transect taken from a naturally occurring marine CO(2) seep in Levante Bay of the Aeolian island o

58 key primary producers of cold and temperate marine coastal ecosystems and exhibit systemic defences

59 ctroscopy of 12 h light-dark cycle incubated marine coastal sediment.

60 in the austral summer of 2010-2011, exposing marine communities to summer seawater temperatures 2-5 d

61 Antarctic shallow coastal marine communities were long thought to be isolated from

62 ntal degradation is a threat to all tropical marine communities, but the reefs of St.

63 trate seasonal mismatches in the exposure of marine consumers to low pH and algal resource identity d

64 in the ichnological analysis of soft modern marine cores is a very informative approach.

65 We further demonstrate that this total marine dark extracellular superoxide flux is consistent

66 the deep-set sector (~250 m) suggesting that marine debris observer reporting focused in this sector

67 conservation of transboundary and migrating marine demersal species.

68 only known from trilobites preserved in open-marine deposits.

69 in DWRT; and higher total omega-3 and total marine-derived omega-3 PUFAs with less decline in DSST.

70 During herbivory, marine diatom species release oxylipins that impair graz

71 orthwest Coast, which indicated a pronounced marine diet for Tseshaht dogs and, presumably, their hum

72 onary trajectories during a time of profound marine ecological change.

73 On this basis we identified several marine ecoregions where non-native species may have the

74 , allowing us to detect the state of a given marine ecosystem based on the dynamics of its curve shap

75 Categorizing ichthyoplankton dynamics across marine ecosystem in the Northeast Pacific can help eluci

76 Marine ecosystem models predict a decline in fish produc

77 source identity during winter in a subpolar, marine ecosystem.

78 atory populations in expansive, inaccessible marine ecosystems [6].

79 blooms are important features of productive marine ecosystems and are known to support higher trophi

80 models to effectively anticipate changes in marine ecosystems and fisheries resources.

81 to determine how climate change might impact marine ecosystems and fisheries.

82 The threat posed by plastic pollution to marine ecosystems and human health is under increasing s

83 n acidification (OA) poses a major threat to marine ecosystems and shellfish aquaculture.

84 Tropical marine ecosystems are highly vulnerable to pollution and

85 limate is having profound effects on coastal marine ecosystems around the world.

86 affects how well countries with species-rich marine ecosystems can scientifically explore those resou

87 Marine ecosystems face numerous challenges from natural

88 Restoration of coastal marine ecosystems is perceived by many to be expensive a

89 al development is increasing the exposure of marine ecosystems to nighttime light pollution, but is a

90 ensure the sustainability and resilience of marine ecosystems while integrating and balancing differ

91 leads to coral death and the degradation of marine ecosystems(2).

92 can have severe and long-lasting impacts on marine ecosystems, fisheries and associated services.

93 systems, but remain poorly resolved for many marine ecosystems, particularly those within in coastal

94 y colonised a series of ecological niches in marine ecosystems, producing textbook examples of conver

95 programs for improving our understanding of marine ecosystems, with the goal of informing policy and

96 are now causing ecosystem degradation across marine ecosystems.

97 dioxide (CO(2) ) emissions, strongly impacts marine ecosystems.

98 ng the impact of ocean acidification (OA) on marine ecosystems.

99 counter the effects of extreme conditions on marine ecosystems.

100 ity among areas closed to protect vulnerable marine ecosystems.

101 e important relationships in terrestrial and marine ecosystems.

102 etecting and responding to global changes in marine ecosystems.

103 three PFAAs are ranked among the top 5% for marine ecotoxicity, when compared to 3104 chemicals in t

104 Our results indicate the PN emissions from marine engines may remain relatively high regardless of

105 a growing recognition of the dynamism of the marine environment as well as new questions about how th

106 se exploitation of a warmer, more productive marine environment by Mesolithic hunter-gatherers drove

107 s in international waters and protecting the marine environment from the harmful effects of mining.

108 s their environmental risk in the near-shore marine environment of Antarctica.

109 DGT samplers were deployed in the near-shore marine environment of East Antarctica around the operati

110 of emerging concern (CECs) in the nearshore marine environment of Puget Sound (WA).

111 of the thousands of pollutants reaching the marine environment though wastewater discharges from coa

112 nforce the need to prevent PCBs entering the marine environment to ensure that levels continue to dec

113 ics (MPs) are ubiquitous contaminants of the marine environment, and the deep seafloor is their ultim

114 , Institute for Chemistry and Biology of the Marine Environment, Oldenburg-complex molecular mixtures

115 lastics are ubiquitous pollutants within the marine environment, predominantly (>90%) accumulating in

116 role of sponge microbiomes in the Antarctic marine environment, where sponges may dominate the benth

117 ource of large-scale changes in the subpolar marine environment.

118 global estimates of oil and gas entering the marine environment.

119 and store it primarily as bicarbonate in the marine environment.

120 risk of ingesting aged microplastics in the marine environment.

121 across a spectrum of approaches, to counter marine environmental extremes, reveals a lack preparedne

122 Sheltered shallow marine environments in areas repeatedly impacted by tsun

123 ever, few of these studies were conducted in marine environments, and almost no work extended beyond

124 In cold marine environments, the obligate hydrocarbon-degrading

125 abit nutrient-rich freshwater, brackish, and marine environments.

126 sistent with concentrations of superoxide in marine environments.

127 dly colonized by microbes when released into marine environments.

128 rsion but has only recently been utilized in marine epidemiology.

129 The marine event began at 251.941 +/- 0.037 Ma, with the PTB

130 as successive extinction events reshaped the marine fauna.

131 that the policies investing capital in local marine fisheries or agricultural sectors achieve income

132 We analyzed annual range edge dynamics of marine fishes-both at the individual species level and p

133 Phytoplankton is the base of the marine food chain as well as oxygen and carbon cycles an

134 namics is key to understanding their role in marine food webs and global biogeochemical cycles.

135 vironment, from ecotoxicity and new links in marine food webs to the fate of the plastics in the wate

136 Our study suggests that mercury in the marine foodweb at ~500 m, which is predominantly anthrop

137 population feed on prey trapped inside large marine gastropod shells.

138 ross oxygen sink comprising about a third of marine gross oxygen production, and a net oxygen sink am

139 eing concentrated in particular locations by marine habitat features, ocean physical processes, and i

140 shark population monitoring in semi-enclosed marine habitats.

141 growing frequency of extreme events such as marine heat waves increases the urgency to consider miti

142 he face of human-driven stressors, including marine heat waves.

143 th long-term (2006-2016) change and a recent marine heatwave (2014-2016) associated with two atmosphe

144 r synthesis identifies commonalities between marine heatwave characteristics and seasonality, links t

145 This study applies a marine heatwave framework to analyse a global sea surfac

146 de Marine Protected Areas before and after a marine heatwave using a kelp forest fish community datas

147 show an extreme heat content event (i.e., a marine heatwave) in coastal waters of the northern Gulf

148 ccurrence of extreme climate events, such as marine heatwaves (MHWs), has resulted in substantial eco

149 steps toward improving predictions of future marine heatwaves and their impacts.

150 Marine heatwaves have been observed worldwide and are ex

151 igh-temperature extreme events in the ocean, marine heatwaves, can have severe and long-lasting impac

152 is may be especially important for calcified marine herbivores, such as the pinto abalone (Haliotis k

153 Marine ice (sea ice, ice shelf and glacier retreat) loss

154 Polar blue carbon increases with losses of marine ice over high latitude continental shelf areas.

155 ifferent habitat types (fresh, brackish, and marine) in Canada.

156 , our results demonstrate that well-designed marine infrastructure and processes used to support the

157 Marine invertebrate species are ectothermic and should b

158 Spermatozoa of marine invertebrates are attracted to their conspecific

159 Marine invertebrates dominated the list of highest risk

160 acilitates the recruitment and settlement of marine invertebrates.

161 e ocean productivity, which in turn enhances marine iron redox cycle.

162 oxyhydroxide and pyrite sinks for Neoarchean marine iron.

163 t, on average, 22% of terrestrial and 13% of marine island areas are under protection status, but tha

164 Yet, sea-level values during Marine Isotope Stage (MIS) 101 (~2.55 Ma) also signal su

165 nce of human occupancy dating to ca. 400 ka (Marine Isotope Stage 11), is one of the very few Middle

166 eamounts have been identified as hotspots of marine life in the Azores, acting as feeding stations fo

167 We applied the model to marine mammal blubber extracted with silicone.

168 ish species, as well as increased reports of marine mammal mortalities in the region.

169 ow that ID MMEs have been reported in 14% of marine mammal species (95% CI 9%-21%), with 72% (n = 36;

170 s) have not been reported ubiquitously among marine mammal species, indicating that intrinsic (host)

171 intensify with significant consequences for marine mammal survival.

172 ales, and likely other ice-associated Arctic marine mammals, will cope with changes in Arctic sea ice

173 onomic groups from phytoplankton to fish and marine mammals.

174 oniopropionate (DMSP) is a globally abundant marine metabolite and a significant source of organic ca

175 isotopically depleted carbon source, such as marine methane clathrates, is therefore not required.

176 The marine microalgae Nannochloropsis oceanica (CCMP1779) is

177 Marine microalgae sequester as much CO(2) into carbohydr

178 ut the most plausible cause is activities of marine microbes in the sediment.

179 d demonstrate its use to evaluate novelty in marine microbial and sponge extracts.

180 Viruses that infect microorganisms dominate marine microbial communities numerically, with impacts r

181 cant source of organic carbon and sulfur for marine microbial ecosystems with the potential to influe

182 ose, suggesting expansins evolved in ancient marine microorganisms long before the evolution of land

183 standing of the fate and behavior of typical marine microplastics, these findings serve as a fundamen

184 red by salmon in common domains during their marine migration.

185 The marine air and continental-marine mixed air had more abundant hydroxyl dicarboxylic

186 ng success) and metabolic rate of a keystone marine mollusc, the sea hare Stylocheilus striatus, a sp

187 lusters in the central nervous system of the marine mollusk Aplysia californica.

188 Cuttlefish, a unique group of marine mollusks, produces an internal biomineralized she

189 al, homeostasis, and complete development of marine mollusks.

190 s, even within the soft adhesive produced by marine mussels.

191 ns, have revolutionized our understanding of marine N(2) fixation and its role in the global nitrogen

192 yse empirical data from terrestrial (n = 4), marine (n = 25) and freshwater (n = 13) environments and

193 ategy is exemplified by the synthesis of the marine natural product (+)-bretonin B.

194 we investigated capacity-building in global marine natural product discovery.

195 rbia plants and regarding the discovery of a marine natural product, revealing biological insights at

196 and allowed the proposed structure of these marine natural products to be confirmed.

197 size, determine the abundances of these main marine nitrifiers.

198 g is crucial to predicting future changes in marine nitrogen biogeochemistry.

199 res, and distribution strongly influenced by marine nutrient inputs, with 60% of blooms less than 5 k

200 rameterizing models that predict the fate of marine oil spills.

201 of placebo or one of 3 doses of an enriched marine oil supplement.

202 Intake of the marine omega-3 polyunsaturated fatty acid, docosahexaeno

203 ey are an important source of nitrite across marine OMZ boundary layers.

204 Identifying marine or freshwater fossils that belong to the stem gro

205 ral scales than previously documented in any marine or terrestrial ecosystem.

206 tions play important roles in the cycling of marine organic matter.

207 try as well as of the resulting abilities of marine organisms to construct essential materials.

208 impacts of direct and indirect stressors on marine organisms, and multi-stressor studies of their co

209 A (eDNA) is increasingly used for monitoring marine organisms; however, offshore sampling and time la

210 pancy between the samples of terrestrial and marine origins was found, indicating that marine samples

211 The negative feedback of marine P cycle to terrestrial P input would keep a relat

212 However, it remains unclear how the marine P cycle would respond to the change of terrestria

213 n, South Africa) is time equivalent with the marine Permian-Triassic boundary (PTB).

214 In the nutrient-rich region surrounding marine phytoplankton cells, heterotrophic bacterioplankt

215 mentally manipulated the species richness of marine phytoplankton communities under a range of warmin

216 endent than photosynthesis across 18 diverse marine phytoplankton, resulting in universal declines in

217 jor shifts in the geographic distribution of marine plankton species.

218 ultiple natural and experimental ecosystems (marine plankton, intertidal mollusks, and deciduous fore

219 related heterotrophic protistan lineages in marine plankton, kinetoplastids and diplonemids.

220 From marine plastic debris, we enriched and isolated microbes

221 idering the transboundary nature of both the marine plastic litter problem and the ecosystem services

222 d States (US) to lead to negative impacts on marine populations and support consumption of products f

223 Here we document the recovery of marine populations, habitats and ecosystems following pa

224 xamine how the reproductive success of a top marine predator is being affected by ecosystem change.

225 ocean, which in turn might have impacted the marine primary productivity and organic carbon burial.

226 Changes in marine primary productivity are key to determine how cli

227 We identify two periods of increased marine production across trophic levels (P1 7600-7100 an

228 this growth was driven by long-term enhanced marine production conditioned by the Holocene Thermal Ma

229 kely a consequence of the overall decline in marine productivity following the last glaciation.

230 and sulfate to the ocean, or major shifts in marine productivity.

231 ted areas and ongoing efforts to establish a Marine Protected Area along the Peninsula, a key fishing

232 e driven community shifts inside and outside Marine Protected Areas before and after a marine heatwav

233 managers in many locations have established marine protected areas or seasonal closures to recover t

234 biodiversity and temperature changes in the marine realm, where species richness mostly increases wi

235 itude annually-resolved and absolutely dated marine record spanning the last millennium, and the Pale

236 s, including cartilaginous and bony fish and marine reptiles, from northern Gulf of Mexico - located

237 The applicability of this marine reserve network paradigm to riverine biodiversity

238 protected deep-water areas in the Galapagos Marine Reserve that may help preserve these unique commu

239 sted, but the groups of fish benefiting from marine reserves profoundly changed, with low trophic lev

240 These findings highlight that while marine reserves still have important roles on coral reef

241 Our results indicate that small networks of marine reserves yield previously unrecognized stabilizin

242 In response, marine resource managers in many locations have establis

243 Huaca Prieta focused on marine resources, although there are some contributions

244 y' model) and identified considerable use of marine resources.

245 crobial resistance in bacteria isolated from marine salmon farms, but much less attention has been pa

246 nd marine origins was found, indicating that marine samples are better represented by ESI than terres

247 n the consumer, packaging, construction, and marine sectors.

248 We used marine sediment organic carbon to determine the role of

249 an 40 degrees C account for roughly half the marine sediment volume, but the processes mediated by mi

250 Here, we use marine sedimentary records to reconstruct Arctic sea-ice

251 ) have been reported in both terrestrial and marine sediments associated with the end-Triassic mass e

252 Environmental DNA (eDNA) metabarcoding of marine sediments has revealed large amounts of sequences

253 shows that the planktonic eDNA preserved in marine sediments has the potential to record climatic an

254 affect biogeochemical processing in coastal marine sediments.

255 lustrating that it took place on the shallow marine shelf coevally with deeper water, below-wave base

256 t subglacial meltwater forms morainal banks (marine shoals) or ice-contact deltas that reduce water d

257 i values, which can explain anomalies in the marine Si budget like in the Cascadia Basin and which ha

258 dered in future investigations of the global marine Si cycle.

259 ificantly to marine snow formation, and that marine snow composed of elongated phytoplankton cells ca

260 We apply this formula to marine snow formation following a phytoplankton bloom.

261 ing velocity can contribute significantly to marine snow formation, and that marine snow composed of

262 study has therefore evolved current natural marine snow protocols to generate 'artificial' marine sn

263 rine snow protocols to generate 'artificial' marine snow, into which bacteria can be incorporated to

264 ichnological signature of cores from modern marine soft sediments.

265 ted positive associations between intakes of marine-sourced omega-3 fatty acids and UL risk.

266 These findings underscore prolific marine sources of reactive oxygen species and a complex

267 nnectivity is an essential consideration for marine spatial planning of competing interests in the de

268 Peruvian marine species are rich in LC-PUFAs and micro-nutrients

269 As a result, the risk of harmful non-native marine species being introduced into this critical regio

270 This is especially the case for marine species crossing multiple Exclusive Economic Zone

271 acids (LC-PUFAs), while in the center region marine species had the lowest As and Pb contents.

272 f abundance trends of 304 widely distributed marine species over the last century, across a range of

273 dentify the number of commercially exploited marine species that are shared between neighboring natio

274 poxia thus links the biogeography of diverse marine species to fundamental energetic requirements tha

275 opper and the herbicide diuron, for tropical marine species.

276 ribe unusual trace fossils found in marginal-marine, storm- and river-flood deposits from the Middle

277 se estimated microbial turnover times in the marine subsurface and nitrogen fixation rates in pelagic

278 t is challenging for microbiota that live in marine subsurface sediments or igneous basement to obtai

279 and other organically-bound species into the marine system.

280 (NPP) accident in 1986 and in freshwater and marine systems after the more recent Fukushima NPP accid

281 preindustrial N budgets for terrestrial and marine systems and their modern-day alteration by N inpu

282 bon sequestration by sediments and vegetated marine systems contributes to atmospheric carbon drawdow

283 To date, metrics of thermal stress within marine systems have focussed on coral communities, and l

284 rewiring of host metabolism, with a focus on marine systems, (ii) consider the range and nature of te

285 importance remain inadequately understood in marine systems, but cues from coastal vegetation can pro

286 Second, in marine systems, shallow subtidal and intertidal areas wi

287 In limited investigation of marine taxa at larger spatiotemporal scales, macroecolog

288 heptapeptide cyanotoxin, are one of the main marine toxins in continental aquatic ecosystems.

289 freshwater turtle (Trachemys scripta) and a marine turtle (Caretta caretta) via analysis of small bl

290 severity of gaseous embolism (GE) and DCS in marine turtles after incidental capture in trawl gear, a

291 board and post-release mortality of bycaught marine turtles that has until now been unaccounted for i

292 Twenty-eight marine turtles were examined on-board fishing vessels.

293 Thus, in the marine urochordate Styela plicata, they have been design

294 Eighty-nine marine vertebrate species, including cartilaginous and b

295 a change in tissue expression from gills, in marine vertebrates, to kidneys in terrestrial vertebrate

296 reported to be an important component of the marine viral communities.

297 bon and sulfur reflect dietary source (e.g., marine vs terrestrial) and the nitrogen trophic level.

298 ir) up to 20 times higher than that found in marine waters.

299 green seaweed hydrolysates and seawater with marine yeast Wickerhamomyces anomalus M15 produced 48.24

300 sms that influence microplastic ingestion in marine zooplankton remain poorly understood.