戻る
「早戻しボタン」を押すと検索画面に戻ります。 [閉じる]

コーパス検索結果 (１語後でソート)

通し番号をクリックするとPubMedの該当ページを表示します
1 ly 10-20% of coastal and oceanic mixed-layer bacterioplankton.
2 enomic analyses of naturally occuring marine bacterioplankton.
3 d estimating the genome complexity of marine bacterioplankton.
4 e highly activated in both cyanobacteria and bacterioplankton.
5 otes with polymorphic life cycles as well as bacterioplankton.
6 by dictating the substrates available to the bacterioplankton.
7 likely again mediated through changes in the bacterioplankton.
8 d substrate utilization capability of marine bacterioplankton.
9 ria, can constitute large proportions of the bacterioplankton.
10 g Vibrionaceae strains coexisting in coastal bacterioplankton.
11 hate indirectly, possibly through feeding on bacterioplankton.
12 ate reductase constituted <1% of the sampled bacterioplankton.
13 racer experiments, it takes the sheath-water bacterioplankton 1.5 years to double their concentration
14                                              Bacterioplankton abundance is the most influential drivi
15                                        Bloom bacterioplankton also transcribed more copies of genes f
16 OC incorporation across diverse oligotrophic bacterioplankton and discuss implications for the ecolog
17  nature of these DNA photoproducts in marine bacterioplankton and eukaryotes, a study was performed d
18                         Studied samples were bacterioplankton and eukaryotic fractions isolated from
19 tial impact on biogeochemistry, we collected bacterioplankton and measured stream physicochemistry du
20 are widely distributed, especially in marine bacterioplankton and nitrogen-fixing plant symbionts.
21 ould successfully compete with heterotrophic bacterioplankton and phytoplankton.
22 chlorococcus, low nucleic acid (LNA) content bacterioplankton and small plastidic protists inhabiting
23 n of ascidian symbionts compared to seawater bacterioplankton, and distinct microbial communities inh
24                        In Arctic catchments, bacterioplankton are dispersed through soils and streams
25  Transect cruises on consecutive years, that bacterioplankton are fed on by plastidic and aplastidic
26                                              Bacterioplankton are major biogeochemical agents respons
27                                              Bacterioplankton are the primary trophic conduit for dis
28 opsin is the membrane protein used by marine bacterioplankton as a light-driven proton pump.
29 es (SAGs) was constructed from Gulf of Maine bacterioplankton as proof of concept.
30 polysaccharide particles immersed in natural bacterioplankton assemblages [1, 5], we showed that succ
31  plankton, and actively expressed in neritic bacterioplankton assemblages, indicating that the newly
32 31.6 C:1N), which was quickly metabolized by bacterioplankton at uptake rates two to six times that o
33   Sponge VOC removal rates exceeded those of bacterioplankton by orders of magnitude.
34 orus (P) content of marine phytoplankton and bacterioplankton can vary according to cell requirements
35 d homologs were found to be common in marine bacterioplankton cells.
36 etabarcoding to comprehensively characterise bacterioplankton communities associated with pelagic par
37 . open waters, the Southern and Arctic Ocean bacterioplankton communities consistently clustered sepa
38    Most information about the composition of bacterioplankton communities has come from studies along
39 on the taxonomic and functional diversity of bacterioplankton communities in lotic ecosystems are lim
40 patterns with a 3-year, circumpolar study of bacterioplankton communities in the six largest rivers o
41 nmental characteristics, confirming that the bacterioplankton communities in the Xiangxi River were r
42 actors governing pelagic particle-associated bacterioplankton communities in this basin.
43 freshwater lake in Hungary, exhibits diverse bacterioplankton communities influenced by various envir
44 g seawater temperature influences the marine bacterioplankton communities is elusive.
45 poral variability in the structure of stream bacterioplankton communities remains understudied.
46 mponent of the carbon cycle, as it may drive bacterioplankton communities toward less diverse and pot
47                     The temporal dynamics of bacterioplankton communities were analysed throughout th
48                   Our results indicated that bacterioplankton communities were both taxonomically and
49                                      Natural bacterioplankton communities were dosed with carboxy-fun
50 trations affected naturally occurring marine bacterioplankton communities' structure and metabolic fu
51 Alphaproteobacteria dominates marine surface bacterioplankton communities, where it plays a key role
52 e succession in the composition of big river bacterioplankton communities.
53 ntitative spatiotemporal characterization of bacterioplankton community changes, including both direc
54                                         Both bacterioplankton community composition and metabolic rat
55                                          The bacterioplankton community differences between control (
56                                Understanding bacterioplankton community dynamics in coastal hypoxic e
57 ployed to study the impact of damming on the bacterioplankton community in the Xiangxi River.
58                     These temporal shifts in bacterioplankton community structure were not seasonal;
59 as been found in nearly every pelagic marine bacterioplankton community studied by these methods.
60 ic and derived taxonomic change in a natural bacterioplankton community when subjected to feeding pre
61 s) yield LMW products available to the wider bacterioplankton community.
62 ribosomal RNA clone libraries from a coastal bacterioplankton community.
63                                              Bacterioplankton consume a large proportion of photosynt
64 hat the global distribution of surface ocean bacterioplankton correlates with temperature and latitud
65 nalysis revealed that community variation of bacterioplankton could be explained by the distinct cond
66 es, also may contribute to the difficulty in bacterioplankton cultivation.
67  the tested seawater samples and Tara Oceans bacterioplankton datasets, but were much more abundant i
68 resent a comprehensive dataset detailing the bacterioplankton diversity along the midstream of the Da
69 ere, we report a comprehensive comparison of bacterioplankton diversity between polar oceans, using s
70                                          The bacterioplankton diversity in large rivers has thus far
71 e foundation for a unified concept for river bacterioplankton diversity.
72      Conversely, transcripts associated with bacterioplankton-dominated pathways like denitrification
73 t into the ecology of the diverse uncultured bacterioplankton dominating the oligotrophic oceans.
74 ent response in cyanobacteria and coexisting bacterioplankton during nutrient-deprived periods at var
75 he specific partner Vibrio fischeri from the bacterioplankton during symbiosis onset and, (ii) modula
76 ting in a magnified effect of viral lysis on bacterioplankton during times of reduced productivity.
77 ndirect evidence that DOM may participate in bacterioplankton EET.
78 a more comprehensive understanding of marine bacterioplankton evolutionary history.
79                                       Marine bacterioplankton face stiff competition for limited nutr
80 of the Pho regulon in both cyanobacteria and bacterioplankton, facilitating inorganic and organic P u
81  space might enable them to outcompete other bacterioplankton for nutrients.
82              Data on whether icebergs affect bacterioplankton function and composition are scarce, ho
83 ty and annual dynamics of a group of coastal bacterioplankton (greater than 99% 16S ribosomal RNA ide
84 nexpectedly, several different heterotrophic bacterioplankton groups also displayed diel cycling in m
85 xing of the seamount sheath-water stimulates bacterioplankton growth by increasing cell encounter rat
86                       Studying heterotrophic bacterioplankton has been challenging, however, as most
87 ssential components of the oceanic food web, bacterioplankton have been acknowledged as catalysts of
88 t unicellular diazotrophic cyanobacteria and bacterioplankton have recently been found in the picopla
89 at, compared with existing cultures, natural bacterioplankton have smaller genomes, fewer gene duplic
90 ated morphologies are prevalent among motile bacterioplankton in aquatic systems.
91 ture and metabolic activities of free-living bacterioplankton in different blooming phases of a dinof
92 des insights into the ecological dynamics of bacterioplankton in freshwater lakes.
93                                              Bacterioplankton in freshwater streams play a critical r
94 nteractions are of ecologically important to bacterioplankton in small boreal lakes, and that EET, pa
95 dicates that the pathway is widespread among bacterioplankton in the ocean surface waters, making it
96 carbon-fixing protists as well as control of bacterioplankton in the ocean.
97 with DMSP methyltransferase activity, marine bacterioplankton in the Roseobacter and SAR11 taxa were
98 counts for up to 22% of the active North Sea bacterioplankton in the summer.
99                Here, we show that 15% of all bacterioplankton in the surface ocean have genes phospho
100                    Our findings suggest that bacterioplankton in the Weddell Sea, which respond to or
101 e, an abundant taxon of heterotrophic marine bacterioplankton in the world's oceans.
102  PAs may be common DON substrates for marine bacterioplankton, in line with the hypothesis that bacte
103  of dissolved organic carbon (DOC) by marine bacterioplankton is a major process in the ocean carbon
104 proteobacteria suggest that some free-living bacterioplankton lineages evolved from patch-associated
105 t driving ancient genome reduction of marine bacterioplankton lineages.
106            These results suggest that marine bacterioplankton may actively accumulate DMSP to osmotic
107                                      Surface bacterioplankton may be subjected to more short-term, va
108 nt decomposition of MPn by phosphate-starved bacterioplankton may partially explain the excess methan
109 athways, yet the links between jellyfish and bacterioplankton metabolism and community structure are
110  are involved in PA transformations, coastal bacterioplankton microcosms were amended with a single P
111 er catchments to receiving catchments, where bacterioplankton-mineral relations stabilized communitie
112 zed communities in free-flowing reaches, but bacterioplankton-nutrient relations stabilized those pun
113 of 171 operational taxonomic units of marine bacterioplankton over 4.5 years at our Microbial Observa
114 ses [V-type H(+)-translocating; hppA]; bloom bacterioplankton participated less in this metabolic ene
115 etically conserved habitat preferences among bacterioplankton, particularly for particle-associated (
116                  Pelagic particle-associated bacterioplankton play crucial roles in marine ecosystems
117 ed by the greatest diversity of oligotrophic bacterioplankton populations in surface waters, includin
118 e we show that two recently speciated marine bacterioplankton populations pursue different behavioral
119 t the growth rates of both phytoplankton and bacterioplankton populations were significantly reduced
120 n their prey, specifically phytoplankton and bacterioplankton populations.
121 Ps rapidly but temporarily inhibited natural bacterioplankton production.
122                                       Marine bacterioplankton regulate sulfur flux by converting the
123                     To better understand how bacterioplankton respond to eddies, we examined depth-re
124  temperature has a profound impact on marine bacterioplankton richness, community composition, and in
125 ynechococcus (up to 65%), were attributed to bacterioplankton shifts in the water column, and copepod
126  structures in the distributions of specific bacterioplankton species are largely unexplored, with th
127 owth, distribution, and activity of abundant bacterioplankton species can be studied regardless of th
128 ated in the genomes of dominant co-occurring bacterioplankton species.
129 servoir region, but how these changes affect bacterioplankton structure and function is unknown.
130 acteria and prasinophytes, and heterotrophic bacterioplankton, such as SAR11 and SAR116, dominated th
131 member of the abundant OM43 clade of coastal bacterioplankton, suggested it is an obligate methylotro
132 f horizontal gene transfer from other marine bacterioplankton taxa or viruses, including pyrophosphat
133                                              Bacterioplankton taxonomic diversity and richness were e
134 studies have shown that rhodopsin-containing bacterioplankton thrive in the most severely nutrient-de
135 ocean water for 1.8 years for the deep-ocean bacterioplankton to grow to the 2.4x higher concentratio
136 nd matter transfer between phytoplankton and bacterioplankton to higher trophic levels and play an im
137 r pyruvate) revealed contrasting capacity of bacterioplankton to utilize specific carbon substrates i
138 ation and dissimilatory nitrate reduction in bacterioplankton toward N(2)-fixing and assimilatory nit
139                                        Bloom bacterioplankton transcribed more copies of genes predic
140 ng marine phytoplankton cells, heterotrophic bacterioplankton transform a major fraction of recently
141 high prevalence of EET genes in a bog lake's bacterioplankton, we hypothesized that the redox capacit
142 sin (PR) is present in half of surface ocean bacterioplankton, where its light-driven proton pumping
143 revalent features among diverse, free-living bacterioplankton, whereas existing laboratory cultures c
144 s metabolic energy scavenging than non-bloom bacterioplankton, with possible implications for differe
145 mary production transformed by heterotrophic bacterioplankton within hours to weeks of fixation.

 
Page Top