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1 flagellates (Ostreopsis), and cyanobacteria (Trichodesmium).
2 nonheterocystous cyanobacteria of the genus Trichodesmium.
3 osphorus-specific nitrogen fixation rates in Trichodesmium.
4 ion and activity in PCD induced mortality in Trichodesmium.
5 y observed to increase with PCD induction in Trichodesmium.
6 c signatures of potential gene regulation in Trichodesmium.
7 in the marine nitrogen-fixing cyanobacterium Trichodesmium.
8 ced by amino acids in individual colonies of Trichodesmium.
9 ize regulation, suggesting a similar role in Trichodesmium.
10 effect of OA on growth and N(2) fixation of Trichodesmium.
11 ng a more diverse array of iron sources than Trichodesmium.
12 elevated CO2 to that reported previously for Trichodesmium.
13 s and deeper in subsurface ocean waters than Trichodesmium.
14 also have a role in metabolic segregation in Trichodesmium.
15 mainly by filamentous cyanobacteria such as Trichodesmium.
17 hesis and nitrogen fixation to determine how Trichodesmium allocates resources to these processes.
18 licon sequencing to examine the diversity of Trichodesmium and associated epibionts across different
21 lation as a potentially adaptive response of Trichodesmium and importantly elucidate underlying metab
22 h they may share the same micro-environment, Trichodesmium and its colony-associated microbial cohort
23 these dynamics are key to the resilience of Trichodesmium and other colony formers in our changing e
24 Large colonial cyanobacteria in the genus Trichodesmium and the heterocystous endosymbiont Richeli
27 ghly correlated to the phosphorus content of Trichodesmium and was enhanced at higher irradiance.
28 ting mechanism under OA has little impact on Trichodesmium, and the energy demand of anti-stress resp
29 aneous nitrogen fixation and photosynthesis, Trichodesmium appears to be a conspicuous consumer of ir
30 nial diazotrophic cyanobacteria of the genus Trichodesmium are thought to play a significant role in
31 cuss the ecological advantages of DOM use by Trichodesmium as an alternative to autotrophic nutrition
32 n sources, implying that naturally occurring Trichodesmium-associated bacteria may be capable of util
33 ome-sequenced strains of bacteria typical of Trichodesmium-associated microbes to develop an understa
34 ltured the globally important cyanobacterium Trichodesmium at both low and high CO2 for 4.5 y, follow
35 ear, of which we calculate up to 84% is from Trichodesmium based on previous measurements of nifH gen
36 specialized metabolite composition of these Trichodesmium blooms and colonies in the Gulf of Mexico
37 uld reduce global N(2) fixation potential of Trichodesmium by 27% in this century, with the largest d
41 mid-Atlantic Ocean and Red Sea implying that Trichodesmium colonies are potential sites of nitrous ox
48 data collected in this study, a theoretical Trichodesmium colony was designed to model whole colony
49 asins regardless of morphology, although the Trichodesmium community structure significantly varied b
51 es of the nitrogen (N)-fixing cyanobacterium Trichodesmium create microscale nutrient-rich oases.
52 N2-fixation of the ubiquitous cyanobacterium Trichodesmium decreased under acidified conditions, notw
54 of how these specialized metabolites affect Trichodesmium ecophysiology, symbioses with marine inver
55 N-TMA DNA stable isotope probing (SIP) of a Trichodesmium enrichment was employed to further investi
56 free-living cyanobacteria, only 63.8% of the Trichodesmium erythraeum (strain IMS101) genome is predi
58 ion, by phosphorus stress, of genes from the Trichodesmium erythraeum IMS101 genome that are predicte
59 ddition, a related cluster was identified in Trichodesmium erythraeum IMS101, an important bloom-form
60 tegy remains enigmatic because the genome of Trichodesmium erythraeum strain IMS101 lacks all genes f
61 study, we used MiMoSA to model the growth of Trichodesmium erythraeum, a filamentous diazotrophic cya
62 t homologs are present in the cyanobacterium Trichodesmium erythraeum, the ciliate Tetrahymena thermo
65 , we grew the nitrogen-fixing cyanobacterium Trichodesmium for 1 year under Fe/P co-limitation follow
66 emporal distribution and growth potential of Trichodesmium for the last glacial maximum (LGM), the pr
68 atory cultures and oceanic surface blooms of Trichodesmium from the South Pacific Ocean triggered PCD
71 ent pCO(2) levels do not significantly limit Trichodesmium growth and thus, the potential for enhance
72 this century (2100) by mapping our model of Trichodesmium growth onto inferred global surface ocean
77 fixation rates of marine diazotrophs such as Trichodesmium have been intensively studied because of t
79 microbial interactions occurring within the Trichodesmium holobiont, especially between Trichodesmiu
80 rize metabolic uptake patterns in individual Trichodesmium IMS-101 cells by quantitatively imaging (1
82 oteomes of cultured and field populations of Trichodesmium in comparison with the marine diazotroph C
83 ed a protein profile similar to iron-starved Trichodesmium in culture, suggestive of acclimation towa
84 tation may help to explain the prevalence of Trichodesmium in low phosphate, oligotrophic systems.
85 eochemically important marine cyanobacterium Trichodesmium increase under high carbon dioxide (CO2) l
87 the free-living, cyanobacterial, diazotroph Trichodesmium is of great importance because of its crit
88 the prominent nitrogen-fixing cyanobacterium Trichodesmium is often limited by phosphorus availabilit
89 itions, the beneficial effect of high CO2 on Trichodesmium is overwhelmed by the deleterious effect o
90 at segregation of CO(2) and N(2) fixation in Trichodesmium is regulated in part by temporal factors.
92 gests that, relative to other phytoplankton, Trichodesmium is uniquely adapted for scavenging phospho
94 and highlight conserved motifs across three Trichodesmium isolates and two Trichodesmium metagenomes
95 conserved across spatiotemporally separated Trichodesmium isolates, thereby elucidating biogeographi
96 How nitrogen fixation by phosphorus-limited Trichodesmium may respond to ocean acidification remains
98 across three Trichodesmium isolates and two Trichodesmium metagenomes, thereby identifying highly co
99 These motifs were also highly conserved in Trichodesmium metagenomic samples from natural populatio
100 orming cells within the cyanobacterial genus Trichodesmium might account for nearly half of nitrogen
105 ated microbiota can affect the physiology of Trichodesmium, often in ways that have been predicted to
106 ggest that DOM could be directly taken up by Trichodesmium or primarily consumed by heterotrophic epi
109 Nitrogen-fixing cyanobacteria in the genus Trichodesmium play a critical role in the productivity o
110 rgenic regions in spatiotemporally separated Trichodesmium populations suggests possible genus-wide s
112 titatively analyzed experimental data on how Trichodesmium reallocated intracellular iron and energy
113 ic evidence is consistent with the idea that Trichodesmium reduces the need to produce glycogen by su
114 aerobactin were not readily bioavailable to Trichodesmium, relative to ferric chloride or citrate-as
116 sorbed phosphorus pools, suggesting that our Trichodesmium results are generally applicable to all ph
117 affected by colony formation, we claim that Trichodesmium's ecological success is tightly linked to
118 decreasing sinking velocity, thus supporting Trichodesmium's niche as a buoyant, high-light-adapted c
120 re sea surface temperatures (SST) are within Trichodesmium's thermal niche increased by 32% from the
121 chemically significant marine cyanobacterium Trichodesmium showing increased growth and nitrogen fixa
122 photosystem II and psaA of photosystem I, in Trichodesmium sp. IMS 101 using the 3 criteria for an en
123 filamentous nonheterocystous cyanobacterium Trichodesmium sp. is controlled by a circadian rhythm.
125 evaluated the rhythm of nitrogen fixation in Trichodesmium sp. strain IMS 101 by using the three crit
126 enomics, here we reveal that nondiazotrophic Trichodesmium species not only exist but also are abunda
128 ation of this compatible solute explains how Trichodesmium spp. can thrive in the marine system at va
131 ixation and the distribution of diazotrophic Trichodesmium spp. indicate that movement in the region
132 filamentous nonheterocystous cyanobacterium Trichodesmium spp. is controlled by a circadian rhythm.
134 cial benefit of daytime nitrogen fixation in Trichodesmium spp. that may counteract these costs.
135 tial distributions that differ from those of Trichodesmium, the N2-fixing cyanobacterium previously c
137 e in restricting the biomass and activity of Trichodesmium throughout much of the subtropical ocean.
138 e determined that protein level responses of Trichodesmium to iron-starvation involve down-regulation
139 arine dinitrogen (N(2))-fixing cyanobacteria Trichodesmium to ocean acidification (OA) is critical to
141 atios in natural populations and cultures of Trichodesmium were close to Redfield values and not sign
143 g, possible regulatory elements predicted in Trichodesmium, when normalized per intergenic kilobase,
144 ganisms and the higher apparent densities of Trichodesmium where aeolian iron inputs are plentiful.
145 is carried out by the marine cyanobacterium Trichodesmium, which supplies more than half of the new
146 forming, N(2) -fixing, marine cyanobacterium Trichodesmium, which undergoes PCD under low iron and hi
147 pound, inhibits N(2) fixation in cultures of Trichodesmium without impairing growth rate, suggesting