ライフサイエンスコーパス: marine organism

1 demonstrated they can transfer PBDEs into a marine organism.

2 of the selected male representative of this marine organism.

3 ean acidification on carbonate deposition by marine organisms.

4 s of CO2 -driven ocean acidification (OA) on marine organisms.

5 ituent of a wide variety of invertebrate and marine organisms.

6 ttle is known about the sulfur metabolism of marine organisms.

7 cally derived from processing freshwater and marine organisms.

8 roduced in significant quantities by aerobic marine organisms.

9 n acidification can have profound impacts on marine organisms.

10 reas of the oceans and affect a diversity of marine organisms.

11 have negative consequences for a variety of marine organisms.

12 ring oyster cement to the adhesives of other marine organisms.

13 ential in reef stomatopods and probably most marine organisms.

14 ucts meridianins and variolins, derived from marine organisms.

15 s widely expected to reduce calcification by marine organisms.

16 es, such as apoptosis and cell necrosis, for marine organisms.

17 res and are among the most thermotolerant of marine organisms.

18 ectral properties afforded by FPs from other marine organisms.

19 phological clines observed across a range of marine organisms.

20 nce used for prey attraction among nonvisual marine organisms.

21 le for the controlled synthesis of silica by marine organisms.

22 rdination of reproductive activities in many marine organisms.

23 or the extensive use of coelenterazine among marine organisms.

24 important precursor for biomineralization in marine organisms.

25 s that record the activities of benthic deep-marine organisms.

26 gestion as a source of chemical pollution in marine organisms.

27 gen concentrations that are lethal for other marine organisms.

28 cycling and act as barriers to dispersal for marine organisms.

29 ogically and economically important group of marine organisms.

30 model from the limited geographical range of marine organisms.

31 e warming can work synergistically to stress marine organisms.

32 nd population dynamics of mollusks and other marine organisms.

33 ythms are a well-known phenomenon in coastal marine organisms.

34 ude) events had equivalent lethal effects on marine organisms.

35 Zinc (Zn) is vital to marine organisms.

36 ne center of animals and the apical organ of marine organisms.

37 ctions, but such estimates remain scarce for marine organisms.

38 tuent of the skeletons and shells of various marine organisms.

39 e types of hybrid nanoparticles on nontarget marine organisms.

40 , including the adhesion proteins of several marine organisms.

41 Brown algae are photosynthetic multicellular marine organisms.

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

43 e expected to have negative consequences for marine organisms.

44 scavenging by organic compounds derived from marine organisms.

45 ding the extensive accumulation of V in some marine organisms.

46 idized by the rumenal microbiota and certain marine organisms.

47 ens capable of causing disease in humans and marine organisms.

48 astics has been shown for a great variety of marine organisms.

49 cence has been reported for many animals and marine organisms.

50 e biosynthesized by prokaryote and eukaryote marine organisms.

51 able recruitment has been debated widely for marine organisms.

52 between primary producers and higher trophic marine organisms.

53 known about the accumulation of parabens in marine organisms.

54 be further metabolized to form AB in higher marine organisms.

55 he formation of arsenobetaine (AB) in higher marine organisms.

56 ansport and survival of planktonic larvae of marine organisms.

57 ely to impact the calcification potential of marine organisms.

58 of acidification derived from CO2 leakage on marine organisms.

59 educe their adverse environmental impacts on marine organisms.

60 umulate in the sea and have toxic effects on marine organisms.

61 s a vector for the assimilation of POPs into marine organisms.

62 ich demonstrates that Hg within near-surface marine organisms (0-150 m) originates from a combination

63 llied to physiological thermal tolerances in marine organisms [2], it may therefore be expected that

64 Inspired by the grooved skin textures of marine organisms, a hydrogel is assembled to present com

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

66 encing of trace DNA fragments left behind by marine organisms; an approach known as 'environmental DN

67 , calcium and iron, two ions pertinent for a marine organism and pathogen, play a signaling role with

68 en accelerated by the chemical uniqueness of marine organisms and by the need to develop drugs for co

69 dy the interactions between oil droplets and marine organisms and could significantly improve our und

70 redicted to have detrimental effects on many marine organisms and ecological processes.

71 nontoxic, degradable polysaccharide found in marine organisms and hence is a promising sustainable po

72 nvironment, and evidence of their impacts on marine organisms and human health has been highlighted.

73 MPs exposure on marine organisms and humans has been documented, but inf

74 astics may cause negative effects on benthic marine organisms and increase bioaccumulation of persist

75 an acidification affects a wide diversity of marine organisms and is of particular concern for vulner

76 h capability has been reported in many other marine organisms and is typically used as a close-range

77 s the potential ecological impacts of DPs on marine organisms and propose mitigating measures to redu

78 ith ramifications for acoustically sensitive marine organisms and the functioning of marine ecosystem

79 sses that appears to be appropriate for some marine organisms and use a sample of genetic data from a

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

81 rease in algal biomass, displacement of many marine organisms, and a rise in fish disease.

82 These pellets are a source of food for marine organisms, and contribute to the oceanic vertical

83 uctures are found in nature, particularly in marine organisms, and may be important for the pigments

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

85 These nanoplastics may profoundly affect marine organisms, and our results can provide critical i

86 Shallow-water marine organisms are among the first to suffer from comb

87 s, and changes in distribution and health of marine organisms are among the most significant processe

88 Populations of most marine organisms are connected by the dispersal of larva

89 Antimicrobial defenses of marine organisms are largely uncharacterized, although f

90 The growth rates and ages of many benthic marine organisms are poorly understood, complicating our

91 al, physiological and behavioural effects on marine organisms are potentially widespread, but our und

92 Sessile marine organisms are prolific sources of biologically ac

93 Many fish and marine organisms are responding to our planet's changing

94 event fouling due to proteins, bacteria, and marine organisms are reviewed.

95 Marine organisms are simultaneously exposed to anthropog

96 Marine organisms are threatened by the presence of pesti

97 owever, most blue carbon sinks (that held by marine organisms) are shrinking, which is important as t

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

99 It is less suitable for marine organisms because it is readily excreted.

100 tives to elucidate timekeeping mechanisms in marine organisms belonging to a major, but under-investi

101 In many marine organisms, biomineralization-the crystallization

102 t environmental cue for vertically migrating marine organisms but the physiological mechanisms of res

103 se for the Late Devonian mass extinctions of marine organisms, but detailed spatiotemporal records of

104 ffect the physiology of important calcifying marine organisms, but the nature and magnitude of change

105 ominent plastic type reported in the guts of marine organisms, but their effects once ingested are un

106 cipate tides is critical for a wide range of marine organisms, but this task is complicated by the di

107 lity may improve performance and survival in marine organisms by encouraging completion of their life

108 e then analyzed fossilized trails of benthic marine organisms by using a novel path analysis techniqu

109 Close associations between single-celled marine organisms can have a central role in biogeochemic

110 The pelagic larvae of many marine organisms can potentially disperse across hundred

111 in particle modelling of larval dispersal in marine organisms, can deliver powerful new insights to s

112 euroendocrine organs freshly isolated from a marine organism Cancer borealis.

113 Scleractinian corals thus join the group of marine organisms capable of forming bimineralic structur

114 Climate change affects marine organisms, causing migrations, biomass reduction

115 l and connectivity among populations of many marine organisms, changes to boundary currents may have

116 se outbreaks, posing a significant threat to marine organisms, communities, and ecosystems.

117 the CblC of Trichoplax adhaerens (TaCblC), a marine organism considered to be one of the earliest evo

118 of calcium carbonate (CaCO(3)) generated by marine organisms constitute the largest and oldest carbo

119 Vertical migrations by marine organisms contribute to carbon export by consumpt

120 to quantify the effects of climate change on marine organisms, decipher the details of paleoclimate r

121 We screened a chemical library of marine organism-derived extracts and identified waixenic

122 eterogeneity among subpopulations of certain marine organisms despite substantial gene flow.

123 Most marine organisms disperse via ocean currents as larvae,

124 sex determination and reproductive output of marine organisms, disrupting the population structure an

125 Biomineral production in marine organisms employs transient phases of amorphous c

126 the future effects of ocean acidification on marine organisms, especially for skeletal calcification,

127 gymnospermous forests and fern fields, while marine organisms experienced mass extinction.

128 heatwaves (MHWs) can cause thermal stress in marine organisms, experienced as extreme 'pulses' agains

129 mportant component of the stress response in marine organisms exposed to a variety of insults as a re

130 e survival of reef-building corals and other marine organisms exposed to high-solar irradiance.

131 Marine organisms, for instance, use liquid-liquid phase

132 ihood analyses of 1176 fossil assemblages of marine organisms from Phanerozoic (i.e., Cambrian to Rec

133 e data from the literature encompassing >750 marine organisms from seven phyla with oceanographic dat

134 ion years, posing an ecological challenge to marine organisms globally.

135 h PLTX-like compounds present in aerosols or marine organisms has been associated with adverse effect

136 pplying structurally complex drug leads from marine organisms has sometimes slowed their development.

137 Marine organisms have a variety of means for acquiring i

138 A variety of secreted luciferases from marine organisms have been described that harbor an N-te

139 Marine organisms have been increasingly regarded as good

140 sis of microplastics in sediment samples and marine organisms have been published, no methods have be

141 Many marine organisms have coevolved symbiotic relationships

142 rse conditions of acidification on sensitive marine organisms have led to the investigation of biorem

143 However, marine organisms have received comparatively little scie

144 Terrestrial and marine organisms have shown changes in populations and d

145 A range of marine organisms have the capacity to ingest microplasti

146 ing may have increased the MeHg exposure for marine organisms, highlighting the importance of CDW upw

147 s remain on the impacts of climate change on marine organisms, hindering our capacity to predict the

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

149 ttempts to assess the speciation in a living marine organism in vivo.

150 We used fucoid seaweeds to examine whether marine organisms in intertidal and subtidal habitats mig

151 could be useful to understand the motion of marine organisms in ocean or be leveraged to sort or org

152 and 6 Ma and corresponding events separating marine organisms in the Atlantic and Pacific oceans at c

153 idification is a global challenge that faces marine organisms in the near future with a predicted rap

154 cate for more widespread use of wearables on marine organisms in the wild and in aquaculture.

155 The increase in marine organisms in this aquatic corridor may represent

156 f halogenated natural products isolated from marine organisms, including indoles and terpenes, of whi

157 The geographic ranges of marine organisms, including planktonic foraminifera(1),

158 A wide range of marine organisms ingest plastic, and its impacts are of

159 Understanding NP uptake and depuration in marine organisms intended for human consumption is imper

160 Hydrocarbons derived from ancient marine organisms interacting with geologically younger t

161 Pelagic dispersal of most benthic marine organisms is a fundamental driver of population d

162 ng anthropogenic CO2 emissions on calcifying marine organisms is complex, owing to the synergy betwee

163 Our understanding of the impact of ALAN on marine organisms is lagging behind that of terrestrial o

164 arsenic-containing lipids (arsenolipids) in marine organisms is now well established, the possible r

165 between nutrients and disease epizootics in marine organisms is often tenuous and supported only by

166 nse to acidification when the broad range of marine organisms is pooled together.

167 The distribution of marine organisms is shaped by geographic distance and oc

168 are well understood, knowledge of clocks in marine organisms is still very limited [2-5].

169 ining biocrystals found in a wide variety of marine organisms is well established.

170 mbled holdfast proteins in mussels and other marine organisms, is generally thought to involve more t

171 ive marine waters, and those internalized by marine organisms, is of growing importance.

172 ged that these contaminants bioaccumulate in marine organisms, it is still controversial whether they

173 is has important implications as to how some marine organisms may respond to future ocean change and

174 Marine organisms may thus play an indirect but important

175 Bioluminescence of a variety of marine organisms, mostly cnidarians and ctenophores, is

176 bioaccumulation and speciation of AgNPs in a marine organism (N. virens).

177 al-dependent beta-lactamases (MBLs) from the marine organisms Novosphingobium pentaromativorans and S

178 Here I investigate the colonization by marine organisms of drift debris deposited on the shores

179 toxin secreted by Gymnodinium breve Davis, a marine organism often associated with harmful algal bloo

180 rring fluorescent proteins (FPs) cloned from marine organisms often suffer from many drawbacks for ce

181 ing the diversity and dispersal potential of marine organisms on plastic debris.

182 increased solar UVB may result in damage to marine organisms other than primary producers in Antarct

183 ough effects of plastic debris on individual marine organisms, particularly mammals and birds, have b

184 uences sex determination and reproduction of marine organisms, particularly mollusks.

185 newable energy devices (MREDs) on underwater marine organisms, particularly offshore wind farms and m

186 a unique family of natural products seen in marine organisms, plants, and bacteria.

187 Marine organisms produce biological materials through th

188 Many benthic marine organisms produce calcium carbonate (CaCO3) struc

189 Coelenterazine is widely distributed among marine organisms, producing bioluminescence by calcium-i

190 key Ediacara taxa and support that they are marine organisms rather than terrestrial lichens or micr

191 During their lifecycle, many marine organisms rely on natural adhesives to attach to

192 in underwater imaging, most of the ocean and marine organisms remain unobserved and undiscovered.

193 cult but is fundamental to understanding how marine organisms reproduce and disperse.

194 How coastal marine organisms respond to natural pCO(2) x DO variabil

195 Marine organisms seem to bioaccumulate TTX from their fo

196 ng pCO2 may alter the bacterial community of marine organisms, significantly affecting the health sta

197 iable signalling environments, especially in marine organisms so profoundly understudied relative to

198 This may hamper calcification in marine organisms such as corals and echinoderms, as show

199 ipids (arsenolipids) are natural products of marine organisms such as fish, invertebrates, and algae,

200 sider the natural production of CHBr(3) from marine organisms such as macroalgae and phytoplankton.

201 'Marine biofouling', the undesired growth of marine organisms such as microorganisms, barnacles and s

202 However, their impact on past marine organisms, such as crinoids, is hard to infer in

203 s a framework to study regional responses of marine organisms, such as planktic foraminifera.

204 s (NPs; <1 mum) have greater availability to marine organisms than microplastics (1-5000 mum).

205 Likewise, marine organisms that are vulnerable to plastic ingestio

206 rmation in foraminifera, unicellular, mainly marine organisms that can build shells by successive add

207 Colonial tunicates are marine organisms that possess multiple brains simultaneo

208 alter the growth, survival, and diversity of marine organisms that synthesize CaCO(3) shells, the eff

209 irst structure of a pheromone protein from a marine organism, that of attractin (58 residues) from Ap

210 ine bacterial genus, associated with various marine organisms, that contributes to host health, nutri

211 Whether or not marine organisms thriving in this cold stenothermal envi

212 Jurassic and Cretaceous, as known for other marine organisms through most of the Mesozoic and Cenozo

213 t-tolerant inserts was demonstrated with the marine organism, Tigriopus californicus.

214 A shift in depth range enables marine organisms to adapt to marine heatwaves (MHWs).

215 the potential exists for copper toxicity to marine organisms to also increase.

216 and upwelling; and (4) adaptive responses of marine organisms to climate-driven ocean change.

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

218 ds, the fundamental biological rationale for marine organisms to produce OH-BDEs remains elusive.

219 cular adaptations that occur in cold-adapted marine organisms to sustain cellular function in their h

220 Understanding the response of marine organisms to temperature is crucial for predictin

221 rom the Deepwater Horizon disaster, exposing marine organisms to this environmental contaminant.

222 les derived from plants, microorganisms, and marine organisms to which CCRCC cells are sensitive.

223 Marine organisms trigger inspiration to expand the parad

224 r to mimic the adhesion performance of these marine organisms, two main biological adhesives are pres

225 Active sequences were uncovered in several marine organisms, two nematodes, an arthropod, a bacteri

226 Calcified marine organisms typically experience increased oxidativ

227 Our study highlights a heightened threat to marine organisms under global warming, as the increased

228 A number of marine organisms use muscle-controlled surface structure

229 rticles (NPs) (AgNP-citrate and AgNP-PVP) in marine organisms via marine sediment exposure was invest

230 the impacts of hydropower on freshwater and marine organisms, we focus this review on the impacts of

231 er drugs in chemical libraries isolated from marine organisms, we identified the lipopeptide somocyst

232 Colonies of representative marine organisms were isolated in pure culture.

233 each contain an oxalyl group rarely found in marine organisms, were determined by spectroscopic analy

234 e found in an unaccountably diverse array of marine organisms, where their functions are largely unkn

235 stion of microplastics has been described in marine organisms, whereby particles may enter the food c

236 ll act to increase the toxicity of copper to marine organisms, which has clear implications for coast

237 ver, artificial light may attract or repulse marine organisms, which results in biased measurements.

238 iobanking and biopreserving corals and other marine organisms whose habitats have been compromised by

239 As the ocean undergoes acidification, marine organisms will become increasingly exposed to red

240 ution will have a major influence on the way marine organisms will respond, and this gives managers a

241 new settlers and their origins in a benthic marine organism with one of the longest pelagic larval p

242 Ocean stands out as a repository for extant marine organisms with ancient traits.

243 For marine organisms with complex life cycles, experiences d

244 n, behavior, and evolution within a clade of marine organisms with growing ecological and economic im

245 er overlap in the Hg isotopic composition of marine organisms with marine particles than with total g

246 Although corals are among the marine organisms with the greatest diversity of secondar