ライフサイエンスコーパス: marine

1 ng and the alignment of terrestrial, ice and marine (14)C and (10)Be records, the authors show that S

2 e analyzed the genomes of 119 strains of the marine actinomycete genus Salinispora, which is currentl

3 ion intensity analysis of SSA generated by a marine aerosol reference tank were compared with observa

4 uence of polluted urban and relatively clean marine airmasses, each with distinct atmospheric chemist

5 es: the analysis of lipid production for the marine alga Thalassiosira pseudonana, and an investigati

6 Using a marine algae data set, we show that quantification of fr

7 omeric pair of compounds, 4, assigned to the marine alkaloid discoipyrrole D is reported.

8 azaspirocyclization reaction, generates the marine alkaloids (-)-fasicularin 2 and a pro-forma synth

9 terrestrial life when Enterococci split from marine ancestors 400 million years ago.

10 m (1999-2015) standardized survey of pelagic marine and anadromous species off Oregon and Washington

11 additional bacterial arborinol producers in marine and freshwater environments that could expand our

12 ate change and causing acidification of both marine and freshwater environments.

13 sediment and ice cores from the terrestrial, marine and glacial realms.

14 on paradox' has been observed in oxygen-rich marine and lake waters, and viewed to significantly cont

15 rgence in food web structure between glacial-marine and oceanic sites.

16 We found that only a quarter of Europe's marine and terrestrial areas protected over the last 100

17 cles and fruit flies are two prominent model marine and terrestrial representatives of the Arthropoda

18 ssions (fossil methane vented naturally from marine and terrestrial seeps and mud volcanoes) are thou

19 ster randomised controlled trial among Royal Marines and Army personnel in the UK military after depl

20 ystem and contrast the cost-effectiveness of marine- and land-based conservation actions.

21 However, Pi uptake in streptophyte algae and marine angiosperms requires Na(+) influx, suggesting tha

22 flects arsenobetaine's release to water from marine animals associated with the euphotic zone rather

23 strongly affect movement behavior of tracked marine animals.

24 taceans, arguably the most abundant group of marine animals.

25 ciliated larvae of Platynereis dumerilii, a marine annelid.

26 egrate demographic and ecological data for a marine apex predator, the broadnose sevengill shark Noto

27 oaches to assess the environmental impact of marine aquaculture using benthic foraminifera eDNA, a gr

28 phic level, as bears and foxes consumed more marine as opposed to terrestrial food, and as the availa

29 monooxygenase (FMO), is found widespread in marine bacteria and is responsible for converting TMA to

30 The trophic linkage between marine bacteria and phytoplankton in the surface ocean i

31 relatively high salt concentration of urine, marine bacteria would be particularly well suited for bi

32 al the catalytic process of TMA oxidation by marine bacterial Tmm and first show that NADP(+) undergo

33 ic drift driving ancient genome reduction of marine bacterioplankton lineages.

34 Under oxygen-limiting conditions, the marine bacterium Dinoroseobacter shibae DFL12(T) generat

35 me analyses and phenotypic screenings of the marine bacterium Phaeobacter inhibens we found that the

36 The marine bacterium Vibrio fischeri is the monospecific sym

37 adation among closely related strains of the marine bacterium Vibrio splendidus One strain, V. splend

38 Chisholm tells us all about this powerhouse marine bacterium.

39 , in anoxic sediments, such as ore deposits, marine basins, and contaminated aquifers.

40 ation at urban waterways, lakes, and coastal marine beaches is responsible for costs that should be a

41 y by other extinct molluscivores such as the marine bear Kolponomos.

42 an-to maximise the extent of light-dependent marine benthic habitats across decadal timescales.

43 The Coral Triangle is a hotspot for marine biodiversity held in its coral reefs, seagrass me

44 d lineages to our expanding understanding of marine biodiversity.

45 SA produced by jet drops can be modulated by marine biological activity.

46 Here we investigate whether the marine biosphere can be identified as a source of Se and

47 background by at least ca. 20%, supporting a marine biosphere-climate link through sea ice melt and l

48 trend in the rate of species description for marine bivalves and find a distinct spatial bias in the

49 lta(202)Hg) data for six species of Hawaiian marine bottomfish.

50 nts likely caused by nucleation in the polar marine boundary layer was quantified annually as 18%, wi

51 ciation in marine habitats, since all extant marine clades are relatively young.

52 help drive the pattern of young, depauperate marine clades.

53 ation may have far-reaching consequences for marine community and ecosystem dynamics, but its full im

54 Marine cone snails contain a high diversity of toxins in

55 seline sources, ambient water and tissues of marine consumers, estimates of the riverine organic matt

56 Characterisation of marine copepod gut microbiome composition and its variab

57 The absence of correlation with marine cyclic solutes contradicts a control of atmospher

58 ntial source is the atmospheric oxidation of marine derived trimethylarsine.

59 s are tightly coupled to the cell cycle in a marine diatom, and that arresting cells in the G1 phase

60 ] leads to G1-phase cell cycle arrest in the marine diatom, Phaeodactylum tricornutum, by binding to

61 Here we measured the responses of a marine diatom, Thalassiosira pseudonana, to high and low

62 ould be the world's largest known example of marine ecosystem "engineering" and suggests that trade-o

63 ial sediment runoff and a downstream coastal marine ecosystem and contrast the cost-effectiveness of

64 question of how rapidly multiple drivers of marine ecosystem change develop in the future ocean.

65 ration should be prioritised if the rates of marine ecosystem decline and expansion are similar and l

66 ection should take precedence if the rate of marine ecosystem decline is high or if the adjacent catc

67 -based actions are optimal when the ratio of marine ecosystem expansion to decline is greater than 1:

68 climate-induced modifications to the Arctic marine ecosystem may increase exposure risk to certain p

69 ultiple sedimentary records and supported by marine ecosystem modeling.

70 , but also affect components of the adjacent marine ecosystem.

71 evaluate support for this theory in lake and marine ecosystems and demonstrate that ecosystem size is

72 es may be widespread in both terrestrial and marine ecosystems and present significant conservation c

73 change and ocean acidification are altering marine ecosystems and, from a human perspective, creatin

74 biomass may be especially important in many marine ecosystems because consumers, as opposed to produ

75 The distinct marine ecosystems found in these environments include es

76 ficant swaths of terrestrial, freshwater and marine ecosystems from a range of threats.

77 ns in herbivore function have shaped shallow marine ecosystems from kelp forests to coral reefs.

78 with the conservation and sustainability of marine ecosystems presents major challenges.

79 ation as gigantic apex predators of Mesozoic marine ecosystems suggests.

80 nthropogenic nitrogen (N) loads to nearshore marine ecosystems through sediment microbial processes s

81 stically altered the abundance of animals in marine ecosystems via exploitation.

82 ly among the most serious global threats for marine ecosystems, affecting a wide range of top predato

83 y 15% of the primary productivity in coastal marine ecosystems, fix up to 27.4 Tg of carbon per year,

84 Our results suggest that in marine ecosystems, pathways for bottom-up and top-down f

85 fore buffer against the impact of warming on marine ecosystems, suggesting a novel mechanism by which

86 In marine ecosystems, the role of bottom-up and top-down fo

87 s on how consumers affect the functioning of marine ecosystems.

88 ccessing the microbial behaviours that shape marine ecosystems.

89 porting Hg from freshwater environments into marine ecosystems.

90 ges are expected to have dramatic impacts on marine ecosystems.

91 rophic to hypereutrophic) typically found in marine ecosystems.

92 g future biogeography and the functioning of marine ecosystems.

93 a to obtain faster recovery of eutrophicated marine ecosystems.

94 of marine sediments, fjord geochemistry, and marine ecosystems.The reason some of the Earth's tidewat

95 -Hakra-Nara, probably sustained a productive marine environment as well as navigability toward old co

96 The marine environment has proven to be a very rich source o

97 g and managing the risks of pollution in the marine environment requires mechanistic models for toxic

98 In the marine environment, fish respond quickly to warming, cau

99 plastics are widely dispersed throughout the marine environment.

100 own about their diversity, especially in the marine environment.

101 need not be confined to the photic zones of marine environments and, as such, may have been underest

102 Coastal and marine environments can begin up to 100 kilometers inlan

103 tion and abundance of such mobile species in marine environments remain challenging, often invasive a

104 y active isoprene degraders in estuarine and marine environments using DNA-SIP and to characterise ma

105 Dinoflagellates are key species in marine environments, but they remain poorly understood i

106 ning the impacts of past human activities on marine environments.

107 s it promising for practical applications in marine environments.

108 n seawater, indicating its good stability in marine environments.

109 n is not present in these cases, meaning the marine enzymes used to degrade carrageenans must possess

110 ge, that StII, a pore-forming protein from a marine eukaryotic organism, encapsulated into Lp functio

111 data on mercury (Hg) isotope composition in marine European fish, for seven distinct populations of

112 nd seamount location play a critical role in marine evolution, mainly by intermittently providing ste

113 Simulations show that marine extinctions help drive the pattern of young, depa

114 The reliable production of marine fish larvae is one of the major bottlenecks in aq

115 Notably, 85% of marine fish species come from a single actinopterygian s

116 m half of global biological CO2 uptake, fuel marine food chains, and include diverse eukaryotic algae

117 ton primary production is at the base of the marine food web; changes in primary production have dire

118 This could alter productivity, marine food webs and carbon sequestration in the Arctic

119 y production exerts a fundamental control on marine food webs and the flux of carbon into the deep oc

120 a large influence on the future stability of marine food webs and the functioning of global biogeoche

121 anic matter on the trophodynamics of coastal marine food webs is not well understood.

122 iability provides information on function of marine food webs, biogeochemical cycles and copepod heal

123 ostly via red meat, dairy products and fatty marine foods.

124 increase in frequency of these traits among marine genera over geological time could explain observe

125 esent a significant, and as yet unaccounted, marine geohazard.

126 Here we show, using marine geological and geophysical data from the continen

127 Marine geological data show that the West Antarctic Ice

128 nce, secondary contact, and hybridization of marine groups in the northwest Pacific marginal seas.

129 tnumber all currently known phage genomes in marine habitats and include members of previously unchar

130 riverine organic matter subsidies to glacier-marine habitats by developing a multi-trophic level Baye

131 explained by limited time for speciation in marine habitats, since all extant marine clades are rela

132 tance to ecosystem structure and function of marine habitats.

133 ated ozone (O3) deposition over seawater and marine halogen chemistry accounted for in both the later

134 Following a 2011 'marine heatwave' in Western Australia, we observed high

135 these keystone species in the degradation of marine hydrocarbons.

136 Paleontological data show that older marine invasions have consistently ended in extinction.

137 Here, we use marine invertebrate communities to parameterise numerica

138 fied, including taxa previously described in marine invertebrate microbiomes with possible links to a

139 Many marine invertebrates including ctenophores are capable o

140 el for survival of well-skeletonized benthic marine invertebrates over a 100-million-year-long interv

141 the acute warming response of six Antarctic marine invertebrates: a crustacean Paraceradocus miersi,

142 appreciation of geoenvironmental dynamics of marine islands has led to advances in island biogeograph

143 vironments using DNA-SIP and to characterise marine isoprene-degrading bacteria at the physiological

144 line of Virginia and North Carolina dated to Marine Isotope Stage (MIS) 3, from 50 to 35 ka, are surp

145 geometric measurements of modern and palaeo (Marine Isotope Stage (MIS) 5e) tidal notches on Bonaire

146 a during the sea level lowstand accompanying marine isotope stage 6, rejecting earlier records of bis

147 posited in response to sea-level rise during Marine Isotopic Stage (MIS) 13.

148 ting settlement and metamorphosis of benthic marine larvae.

149 potential for adverse health effects amongst marine life and spill responders in the northern Gulf of

150 n reef-builders, besides many other forms of marine life.

151 Such is the case for NE Atlantic marine macroalgal forests, important ecosystems whose ma

152 whales have the potential to reshape Arctic marine mammal distributions and behavior.

153 rophic levels, from zooplankton organisms to marine mammals and seabirds.

154 redator activity at-sea, with some birds and marine mammals demonstrating contrasting behavioural pat

155 Because marine mammals occupy upper trophic levels in Arctic foo

156 blubber-specific markers of acute stress in marine mammals of concern for which sampling of other ti

157 cetaceans and in contrast to North American marine mammals, chlorinated MBPs and DMBPs were more abu

158 pleted oxygen in Earth's oceans resulting in marine mass extinction.

159 he promising bioactivity of the tetraarsenic marine metabolite arsenicin A, the dimethyl analogue 2 a

160 Here we report on the use of marine metatranscriptomics to probe virus-host relations

161 tognaths quickly became important members of marine metazoan communities [6].

162 Nearly every important control on marine microbial physiology is currently in flux, includ

163 these viruses infect dominant members of the marine microbiome such as Prochlorococcus and Pelagibact

164 To investigate the behaviours of marine microorganisms at spatially relevant scales, we e

165 Galloway and Lewis discuss marine microplastics and their devastating effects on oc

166 ory induction using sensory neurons from the marine mollusk Aplysia californica.

167 cation and quantification of vitellogenin in marine mussel gonads and compared the results with those

168 r cohesion exhibited by adhesion proteins of marine mussel.

169 the construction of the potent antibacterial marine natural product bromophycoic acid E scaffold.

170 Stolonidiol, a marine natural product, has been reported to potentiate

171 The rise of marine nitrate could have allowed for the rapid diversif

172 ichodesmium, is an integral component of the marine nitrogen cycle and contributes significant amount

173 nce for the emergence of a pervasive aerobic marine nitrogen cycle.

174 s correlation to global transcription in the marine nitrogen-fixing cyanobacterium Trichodesmium.

175 logy and ecology of phytoplankton, influence marine nutrient cycles, and act as vectors for horizonta

176 A significant amount of marine oil snow formed in the water column of the northe

177 lines of evidence indicating the presence of marine oil snow sedimentation and flocculent accumulatio

178 Deep marine oil spills like the Deepwater Horizon (DWH) in th

179 tocks because it is isotopically district to marine organic matter.

180 (TMAO) that stabilizes cellular proteins in marine organisms against the detrimental denaturing effe

181 e peptides were isolated from a multitude of marine organisms and were used for a large number of mol

182 However, marine organisms have received comparatively little scie

183 ophores, a phylum of carnivorous, gelatinous marine organisms, as the sister lineage.

184 , including the adhesion proteins of several marine organisms.

185 and deoxygenation, poses a serious threat to marine organisms.

186 Brown algae are photosynthetic multicellular marine organisms.

187 ore retroviruses as a whole, have an ancient marine origin and originated together with, if not befor

188 of these microorganisms could be traced to a marine origin, being transported thousands of kilometres

189 The marine osmolyte dimethylsulfoniopropionate (DMSP) is one

190 itrogen loss processes using newly available marine oxidants.

191 ecific transporters has implications for the marine phosphorus redox cycle, and might aid the use of

192 on the biological communities that carry out marine photosynthesis.

193 s sense we challenge the general belief that marine phototrophs and heterotrophs compete for the same

194 2 level will lead to a variety of effects on marine phytoplankton and ecosystems.

195 Marine phytoplankton inhabit a dynamic environment where

196 is of a 100-day co-culture between the model marine picocyanobacterium Synechococcus sp. WH7803 and t

197 Using the marine planktonic diatom Pseudo-nitzschia multistriata,

198 Here we tested if mycoviruses derived from a marine plant endophyte can replicate in plant cells.

199 Marine plastic debris is a global environmental problem.

200 A substantial fraction of marine plastic debris originates from land-based sources

201 uires an understanding and quantification of marine plastic sources, taking spatial and temporal vari

202 e is critical for the persistence of benthic marine populations.

203 ation dynamics of a long-lived, wide-ranging marine predator are associated with changes in the rate

204 Top marine predators are expected to experience a particular

205 the global carbon cycle, with almost half of marine primary production transformed by heterotrophic b

206 pacts were significantly higher within large marine protected areas than outside, refuting the critiq

207 cline and expansion are similar and low; (2) marine protection should take precedence if the rate of

208 e sedimentary sulfur isotopic composition of marine pyrite by examining a 300-m drill core of Mediter

209 elds corresponding to locations across their marine range; second, for the fields that elicited signi

210 mate event, only few include high-resolution marine records that span the YD.

211 d their properties are poorly constrained by marine records, including delta(18)O of benthic foramini

212 ed precise alignment of ice, atmospheric and marine records, making it difficult to assess relationsh

213 arth's climate history is best known through marine records, the corresponding continental climatic c

214 We find that marine red beds are a prominent feature of the sedimenta

215 emporal record of banded iron formations and marine red beds.

216 as wide continental shelves, can function as marine refugia for pelagic fauna, whereas offshore locat

217 cade trends in species richness in nine open marine regions around North America (197 region-years) w

218 istic representation of halogen processes in marine regions can improve model prediction of O3 concen

219 he relationships between first sightings and marine regions defined by patterns of local climate velo

220 i, a species previously recovered within the marine reptile 'superclade', for which we now provide a

221 A new study of Mesozoic marine reptiles shows how minute balance organs in the i

222 tat patches can help design better-connected marine reserve networks for the future with equivalent c

223 Here, we develop a framework for designing marine reserve networks that integrates graph theory and

224 ductions in PLD due to ocean warming, future marine reserve networks would require more and/or larger

225 Yet, the extent to which marine reserves are globally interconnected and able to

226 h could be reversed, however, by placing new marine reserves in areas sufficiently remote to minimize

227 se goals requires well-connected networks of marine reserves that maximize larval connectivity, thus

228 Evidence for marine reserves' potential to manage fisheries in an eco

229 rially derived carbon (C) to atmospheric and marine reservoirs.

230 Poly-metallic nodules are a marine resource considered for deep sea mining.

231 ity may be useful for adaptive management of marine resources, but their suitability for this purpose

232 nteract land- and ocean-based stressors: (1) marine restoration should be prioritised if the rates of

233 ontinental fragmentation promotes increasing marine richness, but that coalescence alone has only a s

234 sil record, including changing quantities of marine rock or time-variable sampling effort.

235 no divergence between the kauri and Atlantic marine sediment (14)C data sets, implying limited change

236 Here, using sea-floor geophysical data and marine sediment cores, we resolve the record of glaciati

237 Marine sediment records suggest that episodes of major a

238 Chemical analysis of an Australian coastal marine sediment-derived fungus, Phomopsis sp. (CMB-M0042

239 nt a compilation of phosphorus abundances in marine sedimentary rocks spanning the past 3.5 billion y

240 conodonts, occur worldwide in many Cambrian marine sediments [6, 7].

241 hells and benthic foraminifer assemblages in marine sediments indicate that enhanced CDW upwelling, c

242 mily Teredinidae (shipworms) that burrows in marine sediments rather than wood.

243 configuration may impact interpretations of marine sediments, fjord geochemistry, and marine ecosyst

244 erobic remineralization of organic matter in marine sediments, sulfate reduction coupled to fermentat

245 logical link to mid-latitude terrestrial and marine sites, and sheds light on the long-distance trans

246 bolic potential was consistent with detrital marine snow degradation.

247 olved organic matter in the ocean point to a marine source for the measured OVOCs.

248 For two key marine species (kelp and sea urchins), we use oceanograp

249 hown for other glue-producing terrestrial or marine species and thus represent a unique glue system.

250 We document 289 living Japanese coastal marine species from 16 phyla transported over 6 years on

251 e most invasive terrestrial, freshwater, and marine species in Europe.

252 dy investigates whether 'first sightings' of marine species outside their normal ranges could provide

253 To test how marine species respond to climate variability, we analyz

254 s oceans threatens the ability of vocalizing marine species to communicate.

255 bal meta-dataset of observed range shifts of marine species, we show that incorporating directional a

256 Here, we document marine sponge presenting associated with visual and acou

257 ivated bacteria that exist as symbionts in a marine sponge.

258 Only adult males presented marine sponges, typically doing so in the presence of se

259 Here, we provide evidence that the marine streptomycete strain CNQ-525 can reduce MnO2 via

260 Marine sub-cluster 5.1A isolates with higher phycouribil

261 al is far shorter than the residence time of marine sulfate, any change in the sulfur isotopic record

262 ctive force for influencing diversity within marine Synechococcus populations.

263 genomic analyses, cobalamin biosynthesis in marine systems has been inferred in three main groups: s

264 le of Hg speciation on Hg bioavailability in marine systems has not been teased apart from that of io

265 management strategies on invasion success in marine systems is still unclear.

266 Mercury (Hg) bioavailability to bacteria in marine systems is the first step toward its bioamplifica

267 Despite promises that 'healthy' marine systems show increased resilience, the effects of

268 rning specific case studies of adaptation in marine systems, and discuss associated characteristics a

269 Within marine systems, nitrogen availability is often the limit

270 ico have the potential to drastically impact marine systems.

271 and tangible barometer of climate change in marine systems.

272 The importance of bioluminescent marine taxa is highlighted in the water column, as we sh

273 The EAIS is marine-terminating and grounded below sea level within t

274 seaward of the Aurora subglacial basin, that marine-terminating glaciers existed at the Sabrina Coast

275 results have important implications for the marine-terrestrial biodiversity gradient, and studies of

276 However, marine tests show that vanadium (V) is preferentially ex

277 e the longest-surviving group of secondarily marine tetrapods, comparable in diversity to today's cet

278 Marine Thaumarchaeota are abundant ammonia-oxidizers but

279 ly associated with postglacial adaptation of marine threespine stickleback (Gasterosteus aculeatus) t

280 oceanographic conditions and indicates that marine top predators may be more sensitive to the rate o

281 e and cost-effective methods to detect these marine toxins and protect seafood consumers' health is b

282 The marine trajectory regions include climate 'source' regio

283 back is mainly associated with a decrease in marine tropical low cloud (a more positive shortwave clo

284 Marine tufa-columns, formed by the hydrated carbonate mi

285 ating, and fatal tumor disease of endangered marine turtles.

286 pods, being restricted mostly to parrots and marine turtles.

287 udy of new environmental niches, such as the marine versus terrestrial subsurface, often expands the

288 for differential habitat use among migratory marine vertebrates, we measured the naturally occurring

289 ted ureolytic activity and its regulation in marine vibrios.

290 kely most abundant and ecologically relevant marine viral species, such as vSAG 37-F6, which were ove

291 Marine viruses are key drivers of host diversity, popula

292 While the collective impact of marine viruses has become more apparent over the last de

293 the activity and biogeochemical influence of marine viruses.

294 de catalyst (PCNx) has been synthesized from marine waste and its use demonstrated in a metal-free he

295 results indicate significant regions of open marine water and active biologic productivity throughout

296 We find that incursion of marine water beyond the crest of this ridge, forming an

297 colloids from agglomeration in high salinity marine waters by electrosteric repulsion for long time p

298 Arsenic occurs in marine waters, typically at concentrations of 1-2 mug As

299 A map of a neuronal circuit in a marine worm reveals how simple networks of neurons can c

300 m various Food and Agricultural Organisation marine zones.