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1 increase carbon flux and redirect it towards carbon fixation.
2  increasing the photosynthetic efficiency of carbon fixation.
3 nce, and thus water loss, declined more than carbon fixation.
4 onia oxidation (nitrification) and inorganic carbon fixation.
5  the reducing power of ferrous iron to drive carbon fixation.
6 harvested via phage proteins is not used for carbon fixation.
7  fully utilize the light energy absorbed for carbon fixation.
8 cesses to drive oxygenic water-splitting and carbon fixation.
9 mes and to optimize the metabolic process of carbon fixation.
10  to that provided by (13)C about pathways of carbon fixation.
11 rganelle by sequestering enzymes involved in carbon fixation.
12 p in the Wood-Ljungdahl pathway of anaerobic carbon fixation.
13 phic bacteria that are thought to facilitate carbon fixation.
14 hosphate carboxylase/oxygenase (Rubisco) for carbon fixation.
15 process necessary for Rubisco activation and carbon fixation.
16  responsible for approximately 20% of global carbon fixation.
17  cofactor generations) more prominently than carbon fixation.
18 to accumulate CO2 to increase photosynthetic carbon fixation.
19  processes, ranging from iron homeostasis to carbon fixation.
20  algal CCM, a key process that drives global carbon fixation.
21 pendent photosynthesis and light-independent carbon fixation.
22 y without substantial cost to photosynthetic carbon fixation.
23 ydroxylation, a reaction not associated with carbon fixation.
24  and is greater in environments with greater carbon fixation.
25 s constrained through a mechanistic model of carbon fixation.
26 osynthetic reducing power and the demands of carbon fixation.
27 CO2 concentrating mechanism (CCM), enhancing carbon fixation.
28 ammonia at extremely low concentrations with carbon fixation.
29 ce, and only later evolved a central role in carbon fixation.
30 eability of carboxysome shell) for efficient carbon fixation.
31 asing light intensity, thereby enhancing the carbon fixation activity of the cell.
32 gregation during cell division, and impaired carbon fixation after disparate partitioning.
33 nthesis and growth of plants conducting C(3) carbon fixation after long exposures (days to years) to
34  thus been developed for enhanced biological carbon fixation (also referred to as CO(2) mitigation),
35 colysis-related pathways (pentose phosphate, carbon fixation, aminoacyl-tRNA biosynthesis, one-carbon
36            In the most common C4 pathway for carbon fixation, an NADP-malic enzyme (NADP-ME) decarbox
37         Removal of native regulation enables carbon fixation and 2,3-butanediol production in the abs
38 upply from the C3 products of photosynthetic carbon fixation and colleagues suggesting the utilizatio
39  it may account for a significant portion of carbon fixation and export in the ocean, and would expla
40 trogen versus phosphorus limitation but also carbon fixation and export stoichiometry and hence biolo
41  the plastid, and is mandatory for optimized carbon fixation and growth.
42 ght propagation, influencing rates of global carbon fixation and how we estimate these rates via remo
43 eobacteria is predicted to support inorganic carbon fixation and intense nitrogen loss via anaerobic
44 for the maize leaf was created to capture C4 carbon fixation and investigate nitrogen (N) assimilatio
45  D. oligosanthes utilizes the C3 pathway for carbon fixation and lacks Kranz anatomy.
46 ing enzymes for chlorophyll biosynthesis and carbon fixation and metabolism.
47 h is utilized in reductive reactions such as carbon fixation and nitrogen assimilation.
48 ocesses such as respiration, photosynthesis, carbon fixation and nitrogen fixation.
49  IA UW-2, CAP IB HKU-1 carried the genes for carbon fixation and nitrogen fixation.
50  photosynthetic electron flow is invested in carbon fixation and only 30% is retained as net carbon a
51 higher levels of transcripts associated with carbon fixation and photosynthesis, as well as slightly
52 xygenase (Rubisco), simultaneously enhancing carbon fixation and suppressing photorespiration.
53 iscussed with respect to the evolution of C4 carbon fixation and the mechanisms required for the cell
54 e/oxygenase (RuBisCO) is a crucial enzyme in carbon fixation and the most abundant protein on earth.
55 ropaea proteome revealed increased levels of carbon fixation and transport proteins and decreased lev
56 hat they play a vital role in the balance of carbon fixation and water loss.
57 bacteria perform roughly a quarter of global carbon fixation, and cyanophages that infect them libera
58 better nitrogen and phosphorus use, enhanced carbon fixation, and environmental remediation and to un
59 ments in the optimization of photosynthesis, carbon fixation, and metabolic pathways for the synthesi
60 -including genes involved in photosynthesis, carbon fixation, and nitrogen acquisition-and a number o
61 ved in SCN(-) degradation, sulfur oxidation, carbon fixation, and nitrogen removal.
62 atty acid metabolism, amino acid metabolism, carbon fixation, and the biosynthesis of plant hormones.
63 for supporting microbial life through either carbon fixation, and/or moderating pH stress.
64 timizing light capture, energy transfer, and carbon fixation are essential, as the efficiencies of th
65 lings is critical for the seedlings to start carbon fixation as well as for maintenance of abscisic a
66                              BMCs facilitate carbon fixation as well as the aerobic and anaerobic cat
67 - and total carbon dioxide (TCO2 )-dependent carbon fixation, as well as inorganic carbon species pre
68 , morphology, Rubisco content, and efficient carbon fixation at low CO2 We explain the central role o
69 se-oxygenase (RuBisCO) has a crucial role in carbon fixation but a slow catalytic rate, a problem ove
70  has been implicated in sulfur oxidation and carbon fixation, but also contains genomic signatures of
71                                              Carbon fixation by chemoautotrophic microorganisms in th
72 are bacterial microcompartments that enhance carbon fixation by concentrating ribulose-1,5-bisphospha
73                        Indirect estimates of carbon fixation by Crocosphaera were equivalent to 11% o
74 The role of a C(4) pathway in photosynthetic carbon fixation by marine diatoms is presently debated.
75    In the contemporary ocean, photosynthetic carbon fixation by marine phytoplankton leads to formati
76            We also show that, for most N2FP, carbon fixation by photosynthesis (Asat) and stomatal co
77 tly younger 'diet age', the time lag between carbon fixation by photosynthesis and its use by the con
78 in to affect carbon cycling through enhanced carbon fixation by plants.
79 re it converts HCO(3)(-) to CO(2) for use in carbon fixation by ribulose-bisphosphate carboxylase/oxy
80  the efficiency of the rate-limiting step in carbon fixation by sequestering reaction substrates.
81 s the CO2-fixing enzyme Rubisco and enhances carbon fixation by supplying Rubisco with a high concent
82 ating mechanism into crop plants to increase carbon fixation by supplying the central carbon-fixing e
83 viously reported, but also in the control of carbon fixation by the leaves mediated by a similar mech
84                    As a metabolic module for carbon fixation, carboxysomes could be transferred to eu
85 t common form for deep-branching autotrophic carbon-fixation combines two disconnected sub-networks,
86 is the key enzyme involved in photosynthetic carbon fixation, converting atmospheric CO2 to organic c
87 heterologous expression of five genes of the carbon fixation cycle of the archaeon Metallosphaera sed
88       A13 and A20 exhibited similar rates of carbon fixation despite cellular concentrations of Rubis
89 hotrophs, also use proton gradients to power carbon fixation directly.
90 ith nitrate or ammonium, tracking planktonic carbon fixation, DOM production, DOM composition and mic
91 (AEFs) in the reactivation of photosynthetic carbon fixation during a shift from dark anoxia to light
92 ation were recovered by 10 to 25 d of canopy carbon fixation during summer, thereby explaining the pr
93 2 and H2O, thus resembling plant behavior of carbon fixation during the photosynthesis cycle.
94 ering a pyrenoid into crops to enhance their carbon fixation efficiency.
95 al proteinaceous shell encapsulating the key carbon fixation enzyme, Rubisco, in the interior.
96     Carbon limitation led to a lower rate of carbon fixation, especially towards the end of the Preca
97 llate, Noctiluca scintillans, which combines carbon fixation from its chlorophyll-containing endosymb
98 rocompartment that sequesters the enzymes of carbon fixation from the cytoplasm.
99                                    Improving carbon fixation has mostly focused on enhancing the CO2
100 y of seawater for CO2, whilst photosynthetic carbon fixation has the opposite effect.
101 hey generated more transcripts per liter for carbon fixation, heterotrophy, nitrogen and phosphorus u
102  HCO3 - was found to support the majority of carbon fixation in both phylotypes.
103                We observed rapid shutdown of carbon fixation in chloroplasts after SIPK/Ntf4/WIPK act
104 oncentrating mechanism that greatly enhances carbon fixation in cyanobacteria and some chemoautotroph
105                                              Carbon fixation in cyanobacteria makes a major contribut
106 carboxysome is a protein-based organelle for carbon fixation in cyanobacteria, keystone organisms in
107 ygenase and carbonic anhydrase to facilitate carbon fixation in cyanobacteria.
108 nt in carbon accumulation and photosynthetic carbon fixation in diatoms at low (atmospheric) CO(2).
109 l inform efforts to engineer improvements in carbon fixation in economically valuable grass crops.
110                              We suggest that carbon fixation in microbial mats was not carbon-limited
111 lankton can account for 20 per cent of total carbon fixation in some systems.
112 ical role in sustaining life by catalysis of carbon fixation in the Calvin-Benson pathway.
113 dle sheath and mesophyll cells cooperate for carbon fixation in the leaves of C4 plants.
114  estimated 20-40% of chlorophyll biomass and carbon fixation in the oceans.
115         The rates of gross O2 production and carbon fixation in the SCM were found to be similar to t
116 at the microbially mediated CBB cycle drives carbon fixation in the Spathi Bay sediments that are cha
117 gical factors associated with photosynthetic carbon fixation in this layer should lead to a relations
118 inants required for hydrogen utilization and carbon fixation, including the uptake hydrogenase system
119 ess genes associated with photosynthesis and carbon fixation, indicating that some carbon destined fo
120 ore represents a key pathway for anaplerotic carbon fixation into nitrogenous compounds that are esse
121                                   Biological carbon fixation is a key step in the global carbon cycle
122                               Cyanobacterial carbon fixation is a major component of the global carbo
123                                   Biological carbon fixation is an important part of global carbon cy
124 ient stromatolites, we show that the rate of carbon fixation is higher at the greater levels of atmos
125       This finding suggests that even though carbon fixation is impeded, the available carbon resourc
126                                   Biological carbon fixation is limited by the supply of Fe in vast r
127 xation pathway, but exactly how they enhance carbon fixation is unclear.
128 cialized for carrying out photosynthesis and carbon fixation, it relies on the heterotroph to reminer
129 d its lack of metabolic pathways involved in carbon fixation may confer no benefit under elevated CO2
130 t an operon encoding three genes involved in carbon fixation may have been laterally transferred from
131 ductive and functional attributes, including carbon fixation, mycelial growth and nutrient utilizatio
132            Approximately one-third of global carbon fixation occurs in an overlooked algal organelle
133 responsible for approximately 25% of organic carbon fixation on the Earth.
134 volved in photosynthetic electron transport, carbon fixation, oxidative stress protection (superoxide
135  carbon mineralization in reservoirs exceeds carbon fixation (P<R); the global P/R ratio, however, va
136 capture evolved CO2 using the Wood-Ljungdahl carbon fixation pathway (WLP) in a process called anaero
137  study reports a comprehensive comparison of carbon fixation pathway genes across different photosynt
138 by changes at the transcription level of key carbon fixation pathway genes.
139 irmed to be branched, and the Wood-Ljungdahl carbon fixation pathway is shown to not be functionally
140             Similarly, results show that the carbon fixation pathway that defines this clade-the 3-hy
141  of a genetic system, and discovery of a new carbon fixation pathway, have been facilitated by the av
142                        In the Wood-Ljungdahl carbon fixation pathway, protein-protein interactions be
143 existence of FLS enables the design of a new carbon fixation pathway, the formolase pathway, consisti
144 its importance in the development of a novel carbon fixation pathway.
145 ng 13 gene families involved in the complete carbon fixation pathway.
146                  Nitrification and inorganic carbon fixation pathways affiliated with Thaumarchaeota
147 trification, sulfur oxidation, and inorganic carbon fixation pathways affiliated with the SUP05 group
148                                  Analyses of carbon fixation pathways in all studied organisms reveal
149 ddition, RegB/RegA also control nitrogen and carbon fixation pathways that utilize reducing equivalen
150                       Key genes of all known carbon fixation pathways were absent, as were genes for
151 cks genes that code for known photosynthetic carbon fixation pathways, and most notably missing are g
152 nctional roles with respect to the C3 and C4 carbon fixation pathways, we have investigated the expre
153  it appears to lack any of the known natural carbon fixation pathways.
154 simony that traces the evolution of complete carbon-fixation pathways, and has a clear structure down
155 ic processes, including the light reactions, carbon fixation, pigment synthesis, and other primary me
156 ing (NPQ) and maximum chlorophyll a-specific carbon fixation (Pmax ), but transcripts for archetypica
157 owth, increased levels of photosynthetic and carbon fixation proteins, and increased cyclic electron
158  necessitated by slow enzyme rates, and that carbon fixation rates in the WAP are near a theoretical
159 ly active and near CO2 saturation to achieve carbon fixation rates observed in the WAP.
160 pigment content, photoautotrophic growth and carbon fixation rates, and sulfur metabolism.
161 chnology will realize its advantages of high carbon fixation rates, inexpensive and simple feedstock
162                                  We measured carbon fixation rates, protein content and Rubisco abund
163       Here we show that the calcification to carbon fixation ratio determines whether coccolith calci
164                The kinetic constants for the carbon fixation reaction confirmed the importance of a f
165 arboxysome, a protein shell for sequestering carbon fixation reactions.
166 ete early evolutionary history of biological carbon-fixation, relating all modern pathways to a singl
167 lysis and catalyze one of the final steps in carbon fixation, respectively.
168 that are responsible for about 20% of global carbon fixation, respond rapidly to influxes of nitrate
169                                   Attenuated carbon fixation resulted in imbalances in both redox and
170                The enzyme responsible for C3 carbon fixation, ribulose-1,5-bisphosphate carboxylase (
171                      The strain has multiple carbon fixation routes (Wood-Ljungdahl pathway, pyruvate
172 f nitrogen-transforming bacteria will affect carbon fixation, storage, and release mediated by plants
173  is a metabolic adaptation of photosynthetic carbon fixation that improves water use efficiency by sh
174 he CO(2) concentration necessary to saturate carbon fixation, the CO(2) is most likely concentrated w
175 e variety of biochemical pathways, including carbon fixation, the shikimate pathway, substrate-level
176 mation exists on what pathway of autotrophic carbon fixation these bacteria might use.
177 ducing bacteria, all of which are capable of carbon fixation, thus providing the host with multiple s
178 e forests were predicted to allocate ~50% of carbon fixation to biomass maintenance and growth, despi
179 ria and impact processes ranging from global carbon fixation to enteric pathogenesis.
180 ave important and diverse roles ranging from carbon fixation to enteric pathogenesis.
181  feedback sensor that couples photosynthetic carbon fixation to lipid biosynthesis and is regulated b
182 ndance of SUP05 proteins mediating inorganic carbon fixation under anoxic conditions suggests that SU
183 ments contain abundant genes for autotrophic carbon fixation used in the Calvin-Benson-Bassham (CBB)
184 rease in pyruvate carboxylase-mediated [14C] carbon fixation was associated with a reduction in fluor
185 on (anammox), denitrification, and inorganic carbon fixation were differentially expressed across the
186 onally, only minor changes in photosynthetic carbon fixation were observed.
187                  We find that innovations in carbon-fixation were the foundation for most major early
188 r the oxygen-evolving photosystem II and for carbon fixation, which has implications for oceanic carb
189         Coordination of shoot photosynthetic carbon fixation with root inorganic nitrogen uptake opti
190        Rubisco enzymes play central roles in carbon fixation, with potential importance in biotechnol
191 pairing growth or by boosting photosynthetic carbon fixation, with the latter resulting in higher oil
192 lankton perform approximately half of global carbon fixation, with their blooms contributing dispropo
193  with the carboxylase activity necessary for carbon fixation, yet hypotheses regarding the selective

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