ライフサイエンスコーパス: marine organism

1 of the selected male representative of this marine organism.

2 demonstrated they can transfer PBDEs into a marine organism.

3 , including the adhesion proteins of several marine organisms.

4 Brown algae are photosynthetic multicellular marine organisms.

5 scavenging by organic compounds derived from marine organisms.

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

7 ential in reef stomatopods and probably most marine organisms.

8 ucts meridianins and variolins, derived from marine organisms.

9 s widely expected to reduce calcification by marine organisms.

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

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

12 ectral properties afforded by FPs from other marine organisms.

13 phological clines observed across a range of marine organisms.

14 nce used for prey attraction among nonvisual marine organisms.

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

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

17 rdination of reproductive activities in many marine organisms.

18 idized by the rumenal microbiota and certain marine organisms.

19 or the extensive use of coelenterazine among marine organisms.

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

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

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

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

24 e biosynthesized by prokaryote and eukaryote marine organisms.

25 able recruitment has been debated widely for marine organisms.

26 between primary producers and higher trophic marine organisms.

27 known about the accumulation of parabens in marine organisms.

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

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

30 ansport and survival of planktonic larvae of marine organisms.

31 ely to impact the calcification potential of marine organisms.

32 of acidification derived from CO2 leakage on marine organisms.

33 educe their adverse environmental impacts on marine organisms.

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

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

36 ean acidification on carbonate deposition by marine organisms.

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

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

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

40 cally derived from processing freshwater and marine organisms.

41 roduced in significant quantities by aerobic marine organisms.

42 n acidification can have profound impacts on marine organisms.

43 e expected to have negative consequences for marine organisms.

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

45 have negative consequences for a variety of marine organisms.

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

63 Sessile marine organisms are prolific sources of biologically ac

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

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

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

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

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

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

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

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

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

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

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

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

76 Most marine organisms disperse via ocean currents as larvae,

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

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

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

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

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

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

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

84 Marine organisms have a variety of means for acquiring i

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

86 Marine organisms have been increasingly regarded as good

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

88 Many marine organisms have coevolved symbiotic relationships

89 However, marine organisms have received comparatively little scie

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

105 Marine organisms may thus play an indirect but important

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

129 Calcified marine organisms typically experience increased oxidativ

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

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

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

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

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

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

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

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

138 For marine organisms with complex life cycles, experiences d

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