ライフサイエンスコーパス: bacterioplankton

1 likely again mediated through changes in the bacterioplankton.

2 enomic analyses of naturally occuring marine bacterioplankton.

3 d estimating the genome complexity of marine bacterioplankton.

4 d substrate utilization capability of marine bacterioplankton.

5 ria, can constitute large proportions of the bacterioplankton.

6 by dictating the substrates available to the bacterioplankton.

7 g Vibrionaceae strains coexisting in coastal bacterioplankton.

8 hate indirectly, possibly through feeding on bacterioplankton.

9 ate reductase constituted <1% of the sampled bacterioplankton.

10 ly 10-20% of coastal and oceanic mixed-layer bacterioplankton.

11 Bacterioplankton abundance is the most influential drivi

12 Bloom bacterioplankton also transcribed more copies of genes f

13 OC incorporation across diverse oligotrophic bacterioplankton and discuss implications for the ecolog

14 nature of these DNA photoproducts in marine bacterioplankton and eukaryotes, a study was performed d

15 Studied samples were bacterioplankton and eukaryotic fractions isolated from

16 are widely distributed, especially in marine bacterioplankton and nitrogen-fixing plant symbionts.

17 ould successfully compete with heterotrophic bacterioplankton and phytoplankton.

18 chlorococcus, low nucleic acid (LNA) content bacterioplankton and small plastidic protists inhabiting

19 n of ascidian symbionts compared to seawater bacterioplankton, and distinct microbial communities inh

20 Transect cruises on consecutive years, that bacterioplankton are fed on by plastidic and aplastidic

21 Bacterioplankton are major biogeochemical agents respons

22 Bacterioplankton are the primary trophic conduit for dis

23 opsin is the membrane protein used by marine bacterioplankton as a light-driven proton pump.

24 es (SAGs) was constructed from Gulf of Maine bacterioplankton as proof of concept.

25 plankton, and actively expressed in neritic bacterioplankton assemblages, indicating that the newly

26 31.6 C:1N), which was quickly metabolized by bacterioplankton at uptake rates two to six times that o

27 orus (P) content of marine phytoplankton and bacterioplankton can vary according to cell requirements

28 d homologs were found to be common in marine bacterioplankton cells.

29 . open waters, the Southern and Arctic Ocean bacterioplankton communities consistently clustered sepa

30 Most information about the composition of bacterioplankton communities has come from studies along

31 on the taxonomic and functional diversity of bacterioplankton communities in lotic ecosystems are lim

32 patterns with a 3-year, circumpolar study of bacterioplankton communities in the six largest rivers o

33 nmental characteristics, confirming that the bacterioplankton communities in the Xiangxi River were r

34 poral variability in the structure of stream bacterioplankton communities remains understudied.

35 mponent of the carbon cycle, as it may drive bacterioplankton communities toward less diverse and pot

36 The temporal dynamics of bacterioplankton communities were analysed throughout th

37 Our results indicated that bacterioplankton communities were both taxonomically and

38 Natural bacterioplankton communities were dosed with carboxy-fun

39 e succession in the composition of big river bacterioplankton communities.

40 ntitative spatiotemporal characterization of bacterioplankton community changes, including both direc

41 Both bacterioplankton community composition and metabolic rat

42 Understanding bacterioplankton community dynamics in coastal hypoxic e

43 ployed to study the impact of damming on the bacterioplankton community in the Xiangxi River.

44 These temporal shifts in bacterioplankton community structure were not seasonal;

45 as been found in nearly every pelagic marine bacterioplankton community studied by these methods.

46 ic and derived taxonomic change in a natural bacterioplankton community when subjected to feeding pre

47 ribosomal RNA clone libraries from a coastal bacterioplankton community.

48 Bacterioplankton consume a large proportion of photosynt

49 hat the global distribution of surface ocean bacterioplankton correlates with temperature and latitud

50 nalysis revealed that community variation of bacterioplankton could be explained by the distinct cond

51 es, also may contribute to the difficulty in bacterioplankton cultivation.

52 resent a comprehensive dataset detailing the bacterioplankton diversity along the midstream of the Da

53 ere, we report a comprehensive comparison of bacterioplankton diversity between polar oceans, using s

54 The bacterioplankton diversity in large rivers has thus far

55 e foundation for a unified concept for river bacterioplankton diversity.

56 t into the ecology of the diverse uncultured bacterioplankton dominating the oligotrophic oceans.

57 he specific partner Vibrio fischeri from the bacterioplankton during symbiosis onset and, (ii) modula

58 ting in a magnified effect of viral lysis on bacterioplankton during times of reduced productivity.

59 a more comprehensive understanding of marine bacterioplankton evolutionary history.

60 Data on whether icebergs affect bacterioplankton function and composition are scarce, ho

61 ty and annual dynamics of a group of coastal bacterioplankton (greater than 99% 16S ribosomal RNA ide

62 nexpectedly, several different heterotrophic bacterioplankton groups also displayed diel cycling in m

63 Studying heterotrophic bacterioplankton has been challenging, however, as most

64 ssential components of the oceanic food web, bacterioplankton have been acknowledged as catalysts of

65 t unicellular diazotrophic cyanobacteria and bacterioplankton have recently been found in the picopla

66 at, compared with existing cultures, natural bacterioplankton have smaller genomes, fewer gene duplic

67 ture and metabolic activities of free-living bacterioplankton in different blooming phases of a dinof

68 Bacterioplankton in freshwater streams play a critical r

69 dicates that the pathway is widespread among bacterioplankton in the ocean surface waters, making it

70 carbon-fixing protists as well as control of bacterioplankton in the ocean.

71 with DMSP methyltransferase activity, marine bacterioplankton in the Roseobacter and SAR11 taxa were

72 counts for up to 22% of the active North Sea bacterioplankton in the summer.

73 e, an abundant taxon of heterotrophic marine bacterioplankton in the world's oceans.

74 PAs may be common DON substrates for marine bacterioplankton, in line with the hypothesis that bacte

75 of dissolved organic carbon (DOC) by marine bacterioplankton is a major process in the ocean carbon

76 proteobacteria suggest that some free-living bacterioplankton lineages evolved from patch-associated

77 t driving ancient genome reduction of marine bacterioplankton lineages.

78 These results suggest that marine bacterioplankton may actively accumulate DMSP to osmotic

79 Surface bacterioplankton may be subjected to more short-term, va

80 nt decomposition of MPn by phosphate-starved bacterioplankton may partially explain the excess methan

81 athways, yet the links between jellyfish and bacterioplankton metabolism and community structure are

82 are involved in PA transformations, coastal bacterioplankton microcosms were amended with a single P

83 of 171 operational taxonomic units of marine bacterioplankton over 4.5 years at our Microbial Observa

84 ses [V-type H(+)-translocating; hppA]; bloom bacterioplankton participated less in this metabolic ene

85 etically conserved habitat preferences among bacterioplankton, particularly for particle-associated (

86 ed by the greatest diversity of oligotrophic bacterioplankton populations in surface waters, includin

87 e we show that two recently speciated marine bacterioplankton populations pursue different behavioral

88 t the growth rates of both phytoplankton and bacterioplankton populations were significantly reduced

89 n their prey, specifically phytoplankton and bacterioplankton populations.

90 Ps rapidly but temporarily inhibited natural bacterioplankton production.

91 Marine bacterioplankton regulate sulfur flux by converting the

92 To better understand how bacterioplankton respond to eddies, we examined depth-re

93 ynechococcus (up to 65%), were attributed to bacterioplankton shifts in the water column, and copepod

94 structures in the distributions of specific bacterioplankton species are largely unexplored, with th

95 owth, distribution, and activity of abundant bacterioplankton species can be studied regardless of th

96 servoir region, but how these changes affect bacterioplankton structure and function is unknown.

97 acteria and prasinophytes, and heterotrophic bacterioplankton, such as SAR11 and SAR116, dominated th

98 member of the abundant OM43 clade of coastal bacterioplankton, suggested it is an obligate methylotro

99 f horizontal gene transfer from other marine bacterioplankton taxa or viruses, including pyrophosphat

100 r pyruvate) revealed contrasting capacity of bacterioplankton to utilize specific carbon substrates i

101 Bloom bacterioplankton transcribed more copies of genes predic

102 sin (PR) is present in half of surface ocean bacterioplankton, where its light-driven proton pumping

103 revalent features among diverse, free-living bacterioplankton, whereas existing laboratory cultures c

104 s metabolic energy scavenging than non-bloom bacterioplankton, with possible implications for differe

105 mary production transformed by heterotrophic bacterioplankton within hours to weeks of fixation.