ライフサイエンスコーパス: heterotrophic

1 Y-derived DOC may make the water column more heterotrophic.

2 Pyrinomonas methylaliphatogenes, an aerobic heterotrophic acidobacterium isolated from New Zealand v

3 e results confirmed the potential of using a heterotrophic acidophile to facilitate the rapid commiss

4 microbial communities enriched for versatile heterotrophic Alpha- and Gammaproteobacteria.

5 roduct of an ancient endosymbiosis between a heterotrophic and a photosynthetic protist.

6 omes inferring that these Archaea are organo-heterotrophic and autotrophic acetogens.

7 rous studies to measure the contributions of heterotrophic and autotrophic N2-producing metabolisms (

8 Heterotrophic and autotrophic production data together w

9 ls active), which is inconsistent with known heterotrophic and autotrophic thaumarchaeal lifestyles.

10 etween habitats but also as a bridge between heterotrophic and chemoautotrophic symbiosis for the gia

11 argue that competition, for example between heterotrophic and fermentative bacteria, can occur in th

12 he NDH complex occurs prior to becoming holo-heterotrophic and it shows that the pattern of gene loss

13 d sand content and the presence of microbial heterotrophic and nitrifying communities partially expla

14 phy metabolism classifies these strains into heterotrophic and obligately or facultatively autotrophi

15 s Rhodobacter sphaeroides can switch between heterotrophic and photosynthetic growth.

16 or a range of biosynthetic processes in both heterotrophic and photosynthetic tissues.

17 own metabolic behaviour of tomato leaf under heterotrophic and phototrophic conditions.

18 erences in the metabolic state of the North (heterotrophic) and South (autotrophic) Atlantic oligotro

19 ating significant plasticity in autotrophic, heterotrophic, and diazotrophic strategies supporting mi

20 predicts phenotypes under photoautotrophic, heterotrophic, and mixotrophic conditions.

21 luxes predicted from a flux balance model of heterotrophic Arabidopsis cells in culture, irrespective

22 used to define the metabolic phenotype of a heterotrophic Arabidopsis thaliana cell culture grown in

23 used to define the metabolic phenotype of a heterotrophic Arabidopsis thaliana cell culture grown on

24 Heterotrophic Bacillus amyloliquefaciens associated with

25 data showed also a significant reduction of heterotrophic bacteria (36 degrees C) in 6/11 (55%) site

26 f monochloramine disinfection on Legionella, heterotrophic bacteria (36 degrees C), Pseudomonas aerug

27 cystis sp. PCC 6803) in a mixed culture with heterotrophic bacteria (i.e., Escherichia coli).

28 9), but here we demonstrate that many marine heterotrophic bacteria also produce DMSP, probably using

29 However, diel cycles in naturally occurring heterotrophic bacteria and archaea have rarely been obse

30 onally, the strength of correlations between heterotrophic bacteria and diatoms varied along a hydrol

31 ivities and interactions between anammox and heterotrophic bacteria and offer the first transcription

32 We investigated the relative role of heterotrophic bacteria and phytoplankton in P cycling by

33 uptake rates of individual microbial groups (heterotrophic bacteria and the phytoplankton groups Syne

34 o examine the gene expression of anammox and heterotrophic bacteria and to identify their potential i

35 Some heterotrophic bacteria are able to oxidize sulfide (H2 S

36 Many heterotrophic bacteria are known to release extracellula

37 Heterotrophic bacteria are the primary biotic force regu

38 Finally, our data indicate that heterotrophic bacteria can feed on the exoproteome of Sy

39 lipid production was significantly higher in heterotrophic bacteria compared with cyanobacterial phyt

40 ion in the hygroscopicity of SSA occurred as heterotrophic bacteria concentrations increased, whereas

41 seawater, using controlled phytoplankton and heterotrophic bacteria concentrations, which showed SSA

42 Many heterotrophic bacteria contain sulfide:quinone oxidoredu

43 CO2, may perturb iron uptake in many marine heterotrophic bacteria due to a decrease in oceanic bora

44 Heterotrophic bacteria exploit diverse microhabitats in

45 s to recover 17 draft genomes of anammox and heterotrophic bacteria from a laboratory-scale anammox b

46 e identified in ~50 phylogenetically diverse heterotrophic bacteria from aquatic and soil environment

47 that taxonomically and ecologically diverse heterotrophic bacteria from aquatic and terrestrial envi

48 ditions, lactic acid bacteria and endogenous heterotrophic bacteria grew better.

49 rocesses can occur through biodegradation by heterotrophic bacteria growing on other organic wastewat

50 tory, a direct interaction between algae and heterotrophic bacteria has been shown, with bacteria sup

51 These findings indicate that heterotrophic bacteria have a uniquely P-oriented physio

52 the more studied set-up, the anode contains heterotrophic bacteria in anaerobic conditions, capable

53 Heterotrophic bacteria in pelagic marine environments ar

54 Heterotrophic bacteria inactivation mirrored the trend i

55 and/or lower (BZ) degradation pathways, and heterotrophic bacteria involved indirectly in processing

56 Heterotrophic bacteria likely experience C-limitation wh

57 , we describe the growth of eight strains of heterotrophic bacteria on a variety of soluble and insol

58 ce ocean is a result of de novo synthesis by heterotrophic bacteria or via modification of closely re

59 Biovolume normalized heterotrophic bacteria P uptake rate per cell (amol P mu

60 r, little is known about the functional role heterotrophic bacteria play in anammox granules.

61 showed that marine Thaumarchaeota and select heterotrophic bacteria produce cobalamin.

62 ustering of carotenoid biosynthetic genes in heterotrophic bacteria show that a non-clustered genome

63 emolithoautotrophic life support a 'belt' of heterotrophic bacteria significantly different from the

64 es, is cycled into the environment by marine heterotrophic bacteria using largely uncharacterized mec

65 greater than phytoplankton uptake rates, and heterotrophic bacteria were responsible for generally gr

66 We found that heterotrophic bacteria were the dominant consumers of P

67 The data demonstrated that heterotrophic bacteria with SQR and PDO can rapidly oxid

68 sulfite, providing the foundation for using heterotrophic bacteria with SQR and PDO for sulfide bior

69 ies and the communities of cyanobacteria and heterotrophic bacteria, and co-occurrence analysis ident

70 involved phytoplankton, particle-associated heterotrophic bacteria, and NADH-oxidizing enzymes.

71 Other groups, such as heterotrophic bacteria, may be relatively resilient to c

72 is the remineralization of algae biomass by heterotrophic bacteria, most notably during massive mari

73 t nutrient for ecologically important marine heterotrophic bacteria, particularly the SAR11 clade and

74 s of all tested organism groups except total heterotrophic bacteria, the BWE plus BWT strategy signif

75 om marine macroalgae and nutrient source for heterotrophic bacteria.

76 e response in cyanobacteria as starvation in heterotrophic bacteria.

77 titute an important energy source for marine heterotrophic bacteria.

78 compounds that fuel secondary production by heterotrophic bacteria.

79 promoting function in type IV pili-producing heterotrophic bacteria.

80 idetes but modified in other phyla of marine heterotrophic bacteria.

81 eria and well-studied type IV pili-producing heterotrophic bacteria.

82 N2 fixation and heterotrophic bacterial activity increased up-to tenfold

83 The soil surface also harboured distinct heterotrophic bacterial and fungal communities in the pr

84 iver of variation in the C : N : P ratios of heterotrophic bacterial biomass and that the potential i

85 Furthermore, heterotrophic bacterial clades common to both ecosystems

86 both increased tailings pH and neutrophilic heterotrophic bacterial counts were observed.

87 orococcus vesicles can support the growth of heterotrophic bacterial cultures, which implicates these

88 obiont, especially between Trichodesmium and heterotrophic bacterial epibionts.

89 Furthermore, diel oscillations in different heterotrophic bacterial groups suggested population-spec

90 lication cycles in both photoautotrophic and heterotrophic bacterial hosts.

91 phosphorus lipids is well documented in some heterotrophic bacterial lineages, phosphorus-free lipid

92 ata from approximately 100 13C-MFA papers on heterotrophic bacterial metabolisms.

93 s may affect the function and composition of heterotrophic bacterial populations.

94 Unexpectedly, several different heterotrophic bacterioplankton groups also displayed die

95 of marine primary production transformed by heterotrophic bacterioplankton within hours to weeks of

96 hat is, cyanobacteria and prasinophytes, and heterotrophic bacterioplankton, such as SAR11 and SAR116

97 cently described acidophilic, iron-oxidizing heterotrophic bacterium Acidithrix ferrooxidans grown in

98 d adriaticol, produced by the aerobic marine heterotrophic bacterium Eudoraea adriatica Phylogenetic

99 odel system and found that the presence of a heterotrophic bacterium induced a potential recognition

100 Prochlorococcus and the dominant cooccurring heterotrophic bacterium SAR11 form a coevolved mutualism

101 saccharides of red macroalgae, in the marine heterotrophic bacterium Zobellia galactanivorans.

102 eveal that Ruegeria pomeroyi, a model marine heterotrophic bacterium, can oxidize DMS to DMSO using t

103 ivity of two extracellular enzymes of intact heterotrophic biofilms, beta-glucosidase (carbon-cycling

104 indicates that the environmental impacts of heterotrophic biological treatment are 2-5 times more se

105 of this subgroup are also found in numerous heterotrophic BMC-associated gene clusters encoding func

106 The oligotrophic ocean is neither auto- nor heterotrophic, but functionally diverse.

107 er, these results indicate the potential for heterotrophic carbon metabolism in the reduced sediments

108 uantified the lymphatic flow index following heterotrophic cardiac transplantation in a murine model

109 The genome describes a motile, photo-heterotrophic cell focused on degradation of protein and

110 o oceanic BNF rates based on our analysis of heterotrophic cell-specific N2 fixation rates required t

111 but plays a fundamental role in roots and in heterotrophic cells of the AP.

112 ipid renovation is a common strategy used by heterotrophic cells to reduce their requirement for phos

113 dehydrogenase (GAPCp) in photosynthetic and heterotrophic cells.

114 cay thus cannot make accurate projections of heterotrophic CO2 losses from diverse organic matter res

115 Microbial carbon oxidation by heterotrophic communities is likely to play an important

116 Therefore, phytoplankton and heterotrophic community dynamics are important in modell

117 dynamics, it can more directly constrain the heterotrophic component of Rs, but global-scale models t

118 ends on the responses of its autotrophic and heterotrophic components.

119 nine different autotrophic, mixotrophic, and heterotrophic conditions during nutrient-replete growth

120 of algae under autotrophic, mixotrophic, and heterotrophic conditions using metabolic flux analysis a

121 Under heterotrophic conditions, carbohydrate oxidation inside

122 e and succinate dehydrogenase is small under heterotrophic conditions, indicating that the newly disc

123 phase organic carbon oxidation indicate that heterotrophic consumption of oxidants could maintain the

124 dies that did not control for the effects of heterotrophic consumption.

125 itu, nonchemical UV treatment to disinfect a heterotrophic contaminant in a compact photobioreactor.

126 ethod is a repetitive procedure for one-week heterotrophic cultivation, staining intracellular lipids

127 Heterotrophic cultures accumulated TAG and starch during

128 f the symbiotically competent, facultatively heterotrophic cyanobacterium Nostoc punctiforme were con

129 d interpreted as components of a saprophytic heterotrophic, decomposing community.

130 respiration, associated with production, and heterotrophic decomposition.

131 climate change if permafrost thaw increases heterotrophic decomposition.

132 rticular, notable differences emerged in the heterotrophic degrader communities in our microcosms; on

133 ulfide in sewage could alter the activity of heterotrophic denitrification and lead to N2O accumulati

134 d nitrification-coupled denitrification) and heterotrophic denitrification in six soils (alkaline vs.

135 The experiments showed that heterotrophic denitrification was a negligible source of

136 In acid soils, however, heterotrophic denitrification was the main source for N2

137 for nitrogen was in the range determined for heterotrophic denitrification, with only the absence of

138 the breakdown of sinking organic matter via heterotrophic denitrification.

139 ed metabolic pathways for N2O productions by heterotrophic denitrifiers and ammonia-oxidizing bacteri

140 se (Nar), which is generally prevalent among heterotrophic denitrifiers and is considered as the domi

141 pathways) and the N2O production pathway by heterotrophic denitrifiers to describe and provide insig

142 Predation rates by the heterotrophic dinoflagellate Oxyrrhis marina on mutants

143 octiluca) is a cosmopolitan red tide forming heterotrophic dinoflagellate.

144 100% of dispersed oil in surface waters when heterotrophic dinoflagellates are abundant or bloom.

145 on of faecal pellets containing crude oil by heterotrophic dinoflagellates could contribute to the si

146 study indicates that crude oil ingestion by heterotrophic dinoflagellates is a noteworthy route by w

147 found after an oil spill (1 muL L(-1)), the heterotrophic dinoflagellates Noctiluca scintillans and

148 crude oil droplets (1-86 mum in diameter) by heterotrophic dinoflagellates, major components of marin

149 to chemical cues from copepods, ciliates and heterotrophic dinoflagellates, respectively, under nutri

150 up by Trichodesmium or primarily consumed by heterotrophic epibiont bacteria that ultimately transfer

151 biont hypothesis, over a billion years ago a heterotrophic eukaryote entered into a symbiotic relatio

152 Thus, the heterotrophic eukaryotic communities of Highborne stroma

153 on is sedimentation because it impedes coral heterotrophic feeding and their ability to photosynthesi

154 , showing definitively that these widespread heterotrophic fungi can acclimate to temperature.

155 by mycorrhizal partners during the initially heterotrophic gametophyte and early sporophyte stages of

156 n, and sulfur-cycling metabolisms, including heterotrophic genera Halolactibacillus, Vibrio, Marinoba

157 trophic planktonic growth to light-activated heterotrophic growth and biofilm initiation, knockout of

158 f the DeltandbC mutant under light-activated heterotrophic growth conditions but not under mixotrophy

159 calculated for autotrophic, mixotrophic and heterotrophic growth conditions, as well as knockout con

160 echanism in this bacterium under aerobic and heterotrophic growth conditions.

161 )C-labeled fructose and glucose and tests of heterotrophic growth with these sugars enabled the ident

162 yanobacteria capable of both autotrophic and heterotrophic growth, with support from structural three

163 the medium for photoautotrophic and 13% for heterotrophic growth.

164 from autotrophic respiration in wet years to heterotrophic in dry years.

165 icrobial metabolic pathways or dilution with heterotrophic isotope signals.

166 y of transition from a photoautotrophic to a heterotrophic life history.

167 Metabolic modelling predicted an aerobic heterotrophic lifestyle for the chlamydia, which were fo

168 Metabolic reconstruction indicates a heterotrophic lifestyle with conspicuous nutritional def

169 e range and controls on the stoichiometry of heterotrophic marine bacteria will help improve understa

170 nderlying biochemical allocation patterns of heterotrophic marine bacteria.

171 tegy and elemental composition among taxa of heterotrophic marine bacteria.

172 a salt solution before and after addition of heterotrophic marine bacteria.

173 mass that is successfully turned over by the heterotrophic marine bacteria.

174 the Roseobacter clade, an abundant taxon of heterotrophic marine bacterioplankton in the world's oce

175 ollow the 1:1 relationship characteristic of heterotrophic, marine denitrification.

176 Leaves are derived from heterotrophic meristem tissue that, at some point, must

177 psulate critical segments of autotrophic and heterotrophic metabolic pathways; they are functionally

178 When cells that were adapted to heterotrophic metabolism are shifted back to light condi

179 the maintenance of FeSOD in the plastid and heterotrophic metabolism in acetate-grown cells at the e

180 plastoquinone reduction confirm an impaired heterotrophic metabolism in the cph2 knockout.

181 cient to predict realistic fluxes in central heterotrophic metabolism of plant cells because of the m

182 and is degraded at night by BAM3 to support heterotrophic metabolism.

183 ntribution of the phosphoketolase pathway to heterotrophic metabolism.

184 organelles involved in both autotrophic and heterotrophic metabolism.

185 delta(13)C signatures locally attenuated by heterotrophic metabolism.

186 These methanogens are heterotrophic methyl-reducers that use C1-methylated com

187 he euphotic zone, it has been suggested that heterotrophic microbes rely largely on solubilized parti

188 osm experiments, dispersants did not enhance heterotrophic microbial activity or hydrocarbon oxidatio

189 Heterotrophic microbial communities cycle nearly half of

190 We tested directly the capabilities of heterotrophic microbial communities in surface ocean wat

191 the range of complex substrates available to heterotrophic microbial communities, paralleling the glo

192 The phylogenetic composition of the heterotrophic microbial community is depth stratified in

193 eractions; turf algae and macroalgae promote heterotrophic microbial overgrowth of coral, macroalgae

194 Heterotrophic microorganisms are commonly thought to be

195 This difference and the dominance of heterotrophic microorganisms implies that younger, surfa

196 sting of an assemblage of photosynthetic and heterotrophic microorganisms.

197 focusing on distribution and capabilities of heterotrophic microorganisms.

198 ydomonas reinhardtii, we study the impact of heterotrophic/mixotrophic acetate feeding on chloroplast

199 ntatives from mixotrophic Pyroleae and fully heterotrophic Monotropeae and Pterosporeae.

200 at this time, to support the hypothesis that heterotrophic N2 fixation contributes significantly to o

201 as transparent exopolymer particles, enhance heterotrophic N2 fixation, by forming microenvironments

202 -mixed microbial community comprised of four heterotrophic natural isolates, experimentally quantifyi

203 d direct inhibition by nitrite produced from heterotrophic nitrate reduction were the most important

204 Secondary (i.e., heterotrophic or animal) production is a main pathway of

205 e number of cytochrome c oxidase operons and heterotrophic or diazotrophic capabilities.

206 s predicted distinct proteome demands during heterotrophic or photoautotrophic growth.

207 g carbon is converted into carbon dioxide by heterotrophic organisms at depth is important in control

208 ulating, glycogen-accumulating, and ordinary heterotrophic organisms).

209 involved in the control of hexose uptake in heterotrophic organs, as we have previously reported, bu

210 consequences of oxalate down-regulation in a heterotrophic, oxalic acid-accumulating fruit, we genera

211 c, chemolithoautotrophic methanogen into the heterotrophic, oxygen-respiring, and bacteriorhodopsin-p

212 direct interspecies electron transfer from a heterotrophic partner bacterium, Geobacter sulfurreducen

213 efit from enrichment at the expense of their heterotrophic partners.

214 This analysis suggested that competition by heterotrophic perchlorate reducers and direct inhibition

215 tic (Rubisco small subunit RBCS2B [RBCS]) or heterotrophic (phosphate transporter PHT1.2 [PHT]) cell-

216 different trophic modes, i.e., autotrophic, heterotrophic, photoheterotrophic, and mixotrophic modes

217 Instead, heterotrophic picoplankton populations exhibited cross-s

218 t of 660 photoautotrophic plants and all the heterotrophic plants are missing plastid-encoded cp-ndh

219 f temperature, oxygen and pH changes through heterotrophic plasticity.

220 ng to the modified protein turnover rates in heterotrophic plastids.

221 The results show that HPC (heterotrophic plate counts), representing microbiologica

222 with AS bioselector processes can affect the heterotrophic population composition in AS.

223 Leptospira exoproteins primarily function in heterotrophic processes (the processes by which organism

224 Extensive heterotrophic processing of plant and soil-derived DOM r

225 This shift from an autotrophic to a heterotrophic profile occurred concurrently with decreas

226 lankton production is ultimately consumed by heterotrophic prokaryotes(2).

227 on of solute transporters indicates that the heterotrophic prokaryotic community is geared toward the

228 Heterotrophic Proteobacteria and Actinobacteria were iso

229 ed that both heterocystous cyanobacteria and heterotrophic proteobacteria had the genetic potential f

230 s been inferred in three main groups: select heterotrophic Proteobacteria, chemoautotrophic Thaumarch

231 expressing nifH was primarily represented by heterotrophic Proteobacteria.

232 for molecular biology and genomics in novel heterotrophic protist species.

233 eukaryotic plankton biodiversity belonged to heterotrophic protistan groups, particularly those known

234 factors that structure microbial eukaryotes (heterotrophic protists and fungi) are poorly characteriz

235 Cultures of heterotrophic protists often require co-culturing with b

236 , distributed across categories expected for heterotrophic protists.

237 cating that it plays a role predominantly in heterotrophic rather than autotrophic tissues, at least

238 itional barium and sulfate ions derived from heterotrophic remineralization of organic matter.

239 s does not offset the loss of soil C through heterotrophic respiration (RH ) on an annual basis.

240 on ecosystem net primary productivity (NPP), heterotrophic respiration (Rh) and net ecosystem product

241 tributed mainly by the additive responses of heterotrophic respiration (Rh) and net primary productio

242 Heterotrophic respiration (Rh) was measured inside deep

243 otal soil respiration, trenched chambers for heterotrophic respiration (Rh), and warmed trenched cham

244 wed that these high ratios resulted from low heterotrophic respiration and very low daylight autotrop

245 -2005), but at a lower rate due to increased heterotrophic respiration as well as lower productivity

246 g different seasons affected autotrophic and heterotrophic respiration in a bryophyte-dominated peatl

247 ng season fluxes of autotrophic and old soil heterotrophic respiration increased as permafrost thaw d

248 use a positive feedback to climate change if heterotrophic respiration increases without correspondin

249 roduction (NPP), autotrophic respiration and heterotrophic respiration is measured separately, to dev

250 2061 because the effects of warming increase heterotrophic respiration less than they increase carbon

251 e.g., 2040-2060) as committed emissions from heterotrophic respiration of beetle-killed biomass are b

252 nces in the partitioning of autotrophic from heterotrophic respiration processes in soils in conjunct

253 Old soil heterotrophic respiration ranged from 6 to 18% of Reco a

254 s about the timing and magnitude of seasonal heterotrophic respiration rates, again reflecting struct

255 How autotrophic and heterotrophic respiration sources respond to climate cha

256 em respiration and larger contributions from heterotrophic respiration than the Healy tundra, both sy

257 cessity to simulate the seasonal patterns of heterotrophic respiration to accurately simulate the net

258 e quantified the response of autotrophic and heterotrophic respiration to permafrost thaw across the

259 rbon is slowly emitted to the atmosphere via heterotrophic respiration which subsequently feeds back

260 th increasing precipitation, suggesting that heterotrophic respiration will be more sensitive than au

261 osystem root respiration (and to some extent heterotrophic respiration) at within-season time-scales.

262 P, the balance of net primary production and heterotrophic respiration) by integrating information fr

263 ater mixing in the hyporheic zone stimulates heterotrophic respiration, alters organic carbon composi

264 s such as enhanced photosynthesis, increased heterotrophic respiration, and expansion of woody vegeta

265 adiation and a similar magnitude decrease in heterotrophic respiration, in response to drying soils.

266 tion, and increased ratios of autotrophic to heterotrophic respiration.

267 nic matrices and how this ultimately affects heterotrophic respiration.

268 soil respiration (RS) and its components of heterotrophic (RH) and rhizospheric (RR) respiration dur

269 ts components, that is, autotrophic (Ra) and heterotrophic (Rh) respiration.

270 s two components [i.e., autotrophic (Ra) and heterotrophic (Rh) respiration] to single global change

271 The persistent but less abundant heterotrophic Rhizobiales bacteria possibly contributed

272 bacterial community predominantly carried a heterotrophic signal.

273 time dependency of As(III) oxidation by two heterotrophic soil bacteria (Agrobacterium tumefaciens a

274 ong-term warming were observed regarding the heterotrophic soil CO2 efflux (R10 warmed: 2.31 +/- 0.15

275 icrobes, the existence of this phenomenon in heterotrophic soil microbes remains controversial.

276 plore why a similar core model structure for heterotrophic soil respiration remains elusive and how a

277 on and a larger fractional contribution from heterotrophic sources.

278 the environmental responses among different heterotrophic species seemed synchronous, the specific m

279 which sustain the growth of autotrophic and heterotrophic species whose activities may have conseque

280 cts of phosphorus emissions to freshwater on heterotrophic species.

281 are major suppliers of carbon and energy in heterotrophic species.

282 sistent with the definition of an endogenous heterotrophic succession.

283 d by complete oxidation to carbon dioxide by heterotrophic sulfate-reducing bacteria, which closes th

284 We show that heterotrophic sycamore (Acer pseudoplatanus L.) cells in

285 biosis arose by displacement of an ancestral heterotrophic symbiosis and a report of pure culture of

286 rbon dioxide (CO(2)) effluxes from these net heterotrophic systems contribute significantly to the gl

287 , consistent with the proliferation of known heterotrophic taxa (e.g., Pseudomonadaceae, Burkholderia

288 eukaryotic communities, especially regarding heterotrophic taxa.

289 may increase sink strength in proliferating heterotrophic tissues by indicating low sugar availabili

290 SUS) is a key enzyme of carbon metabolism in heterotrophic tissues of plants.

291 lopmentally regulated starch turnover within heterotrophic tissues other than dedicated storage organ

292 rns in various tissues as well as individual heterotrophic tissues.

293 it is present in plastids of autotrophic and heterotrophic tissues.

294 microbiomes as well as seasonal shifts from heterotrophic to autotrophic microorganisms associated w

295 rming instead causes a persistent shift from heterotrophic to more autotrophic control of the growing

296 represents one of the largest and most rapid heterotrophic transformations of organic matter in the e

297 ediments host a large population of diverse, heterotrophic, uncultured microorganisms with unknown ph

298 as used to build an in silico model to study heterotrophic utilisation of autotroph biomass using ele

299 trated increased total carbon recovery above heterotrophic values associated to mixotrophic assimilat

300 - and belowground plant structures) and two heterotrophic (young and old soil).