ライフサイエンスコーパス: chlorophyll

1 SI-LHCI supercomplex contains 10 LHCIs (~240 chlorophylls).

2 rphological traits respond to a reduction in chlorophyll.

3 cause it is a major component of RuBisCO and chlorophyll.

4 e motions, including the phytol tails of two chlorophylls.

5 th molecular orbitals delocalized over the P chlorophylls.

6 noids and the pathways of energy transfer to chlorophylls.

7 l (11.6-21.0), beta-carotene (0.49-0.65) and chlorophyll (44.3-54.0), and unsaponifiable matter (2.48

8 thod shows good applicability in mixtures of chlorophyll a (Chl a) and chlorophyll b (Chl b) with con

9 employed to analyze the relationship between chlorophyll a (Chl-a) and the explanatory variables in t

10 re prepared to mimic varying compositions of chlorophyll a and b in nature for the application in foo

11 nd quantify two main chlorophyll components (chlorophyll a and b) present in their mixtures.

12 ished based on correlation coefficients with chlorophyll a and often shared molecular features (eleme

13 Our study utilised remotely-sensed data (chlorophyll a and sea surface temperature) coupled with

14 relations of FT-ICR-MS peak intensities with chlorophyll a and solar irradiation were used to define

15 oefficient (mu(s)) of the coral skeleton and chlorophyll a concentration of live coral tissue.

16 time, we explored patterns in phosphorus and chlorophyll a data from 2008 to 2018 collected in wester

17 In this study, chlorophyll a fluorescence light response curves and gas

18 Using chlorophyll a fluorescence measurements, we found photos

19 Leaf gas exchange, water potential, and chlorophyll a fluorescence were monitored during the ecl

20 its it, supporting a gating function for the chlorophyll a involved in redox sensing.

21 Chlorophyll a levels were positively related to krill li

22 asing sea surface temperature and increasing chlorophyll a levels.

23 Two conformations of the chlorophyll a phytyl tail were resolved, one that preven

24 n growth, resulting in an extensive plume of chlorophyll a that was detectable by satellite.

25 d biochemical profiles (lipid production and chlorophyll a) comparable to the untreated control, cult

26 gmentation (11 times the cellular content of chlorophyll a) enables glacier algae to tolerate extreme

27 tions in standing stocks of total carbon and chlorophyll a, and a shift towards smaller phytoplankton

28 ntration and the relationship between TP and chlorophyll a, and these indicate that spring phosphorus

29 Lake TP was a strong predictor of chlorophyll a, but the relationship was weaker at sites

30 (photosynthetic efficiency, coral whitening, chlorophyll a, host protein, algal symbiont counts, and

31 dation site (Q(p)) adjacent to haem b(p) and chlorophyll a.

32 ra of the complexes closely resemble that of chlorophyll a.

33 ts, FeCh possesses a conserved transmembrane chlorophyll a/b binding (CAB) domain that resembles the

34 Chlorophyll a/b ratios and the functional absorption cro

35 Amino acid residues of the light-harvesting chlorophyll a/b-binding proteins involved in pigment bin

36 A 75% decrease of the main fucoxanthin-chlorophyll a/c-binding proteins was identified in the a

37 To enhance the stability of chlorophyll, a polymer encapsulation method was proposed

38 iations of fisheries yield parallel those of chlorophyll-a (an index of phytoplankton biomass).

39 trophication has been expressed as increased chlorophyll-a (chl-a) driven by accelerated nutrient loa

40 Often Chlorophyll-a (Chl-a) is used to track changes in phytop

41 Here, we use satellite-derived surface chlorophyll-a (Chl-a) observations, in conjunction with

42 Chlorella is a green microalga and contains chlorophyll-a (chl-a), which is the major light harvesti

43 highly eutrophic status [99 +/- 289 ug.L(-1) chlorophyll-a (Chl-a)].

44 a FR-chlorophyll and the secondary donor is chlorophyll-a (P(D1) of the central chlorophyll pair).

45 hic vs. hypertrophic) on total phytoplankton chlorophyll-a and cyanobacterial abundance and compositi

46 lation between genetic variation and surface chlorophyll-a and salinity, suggesting an important role

47 xplanations based on the correlation between chlorophyll-a concentration (Chl-a) and climatic indices

48 treme events tended to coincide with reduced chlorophyll-a concentration at low and mid-latitudes.

49 ophyll Maxima (DCMs) are subsurface peaks in chlorophyll-a concentration that may coincide with peaks

50 st correlated to phosphorus availability and chlorophyll-a concentration.

51 cess were also strongly influenced by winter chlorophyll-a concentrations and sea-surface height anom

52 nd declines in coral cover, and (ii) maximum chlorophyll-a concentrations, which were associated with

53 While chlorophyll-a content (CHL) is commonly described as a p

54 ment was detected for both cyanobacteria and chlorophyll-a demonstrating that ecological surprises ca

55 -order rate constant for the demetalation of chlorophyll-a to pheophytin-a was experimentally determi

56 w a rapid subpicosecond energy transfer from chlorophyll-a to the long-wavelength chlorophylls-f/d Th

57 y observable and separated from that of bulk chlorophyll-a We present an ultrafast transient absorpti

58 o cyanobacteria than other pigments, such as chlorophyll-a, and to present an excellent linear correl

59 Comparison of satellite-derived chlorophyll-a, backscatter, absorption and remote sensin

60 (i.e., El Nino) was associated with peaks in chlorophyll-a.

61 duce experimentally observed shifts in known chlorophyll absorption bands, demonstrating the predicti

62 orophyll rings (CRs) are defined as elevated chlorophyll along eddy peripheries and have been observe

63 Low energy chlorophylls (also known as red chlorophylls) residing i

64 uted to an electrochromic blue shift of a FR-chlorophyll among the reaction center pigments.

65 tions were determined by ion chromatography, chlorophyll and ascorbate concentrations, and hydrophili

66 Green LED increased the chlorophyll and ascorbic acid content; white, red and ye

67 tent, activities of catalase and peroxidase, chlorophyll and capsaicin content gradually decreased fo

68 cant genotypic variation was demonstrated in chlorophyll and carotenoid concentrations.

69 tants were characterized by an extremely low chlorophyll and carotenoid content, as well as poorly de

70 ex (OSI), Maillard reaction products (MRPs), chlorophyll and carotenoid contents were increased while

71 The highest chlorophyll and carotenoid pigment contents in cotyledon

72 ich helps to ensure adequate availability of chlorophyll and heme.

73 The observed correlation between chlorophyll and laminarin suggests an annual production

74 ecosystems can be anticipated from predicted chlorophyll and sea surface temperature anomalies.

75 in which the primary electron donor is a FR-chlorophyll and the secondary donor is chlorophyll-a (P(

76 Detection of metal exchange in pigments (chlorophylls and bacteriochlorophylls) was based on reve

77 Arabidopsis (Arabidopsis thaliana) OHPs with chlorophylls and carotenoids and show that pigment bindi

78 re, mutant lines exhibited reduced levels of chlorophylls and nitrate, increased levels of sucrose, m

79 to follow the combined effect of pro-oxidant chlorophylls and the protective light filtering material

80 ygen (DO) and associated variables (nitrite, chlorophyll, and ammonium) with depth and between statio

81 peroxide dismutase, soluble protein, lignin, chlorophyll, and electric conductivity.

82 actone (PCL) was employed to encapsulate the chlorophyll, and the particles size of the composites wa

83 In leaves, carotenoids, chlorophylls, and phenolic compounds were higher compare

84 ucosinolate breakdown products, carotenoids, chlorophylls, and phenolic compounds.

85 Far-red absorbing chlorophylls are constitutively present as chlorophyll (

86 ity in mixtures of chlorophyll a (Chl a) and chlorophyll b (Chl b) with concentrations ranging from 4

87 t line it was possible to continuously alter chlorophyll b levels and correspondingly light-harvestin

88 t-harvesting antenna by selectively reducing chlorophyll b levels and peripheral light-harvesting com

89 sting antenna sizes achieved by reduction in chlorophyll b levels, we have determined that there is a

90 d 15, determines the carotenoid-to-(bacterio)chlorophyll [(B)Chl] energy transfer efficiency.

91 rbohydrates) and micronutrient (fatty acids, chlorophylls, beta-carotene, alpha-tocopherol and ascorb

92 est yield as well as the smallest amounts of chlorophylls, beta-carotene, lutein and neoxanthin in fr

93 The highest concentrations of chlorophylls, beta-carotene, lutein, neoxanthin and viol

94 ry matter, total polyphenols, ascorbic acid, chlorophylls, beta-carotene, lutein, neoxanthin and viol

95 mplex chlorophyll-binding motif required for chlorophyll binding were mutated.

96 hen residues of the light-harvesting complex chlorophyll-binding motif required for chlorophyll bindi

97 usion, the FeCh CAB domain with a functional chlorophyll-binding motif was retained in all currently

98 x of light-harvesting complexes, including a chlorophyll-binding motif.

99 margin domain, and specifically depleted of chlorophyll-binding protein complexes.

100 l for the biogenesis of the light harvesting chlorophyll-binding proteins (LHCP), the most abundant m

101 insufficient GGPP substrate availability for chlorophyll biosynthesis achieved through GGPP flux redi

102 least in part, transcriptional regulation of chlorophyll biosynthesis and catabolism genes.

103 n translation by chloroplastic ribosomes and chlorophyll biosynthesis in two developmental contexts o

104 g from the downregulation of light-dependent chlorophyll biosynthesis induced by PSII deficiency.

105 The first committed step of chlorophyll biosynthesis is catalyzed by a multimeric en

106 llide oxidoreductase (POR) genes involved in chlorophyll biosynthesis is noteworthy.

107 se (POR) catalyses a light-dependent step in chlorophyll biosynthesis that is essential to photosynth

108 ase subunits (rbcL and RbcS), and enzymes of chlorophyll biosynthesis were down-regulated in the yell

109 eed germination, hypocotyl gravitropism, and chlorophyll biosynthesis, by physically interacting with

110 iogenesis provokes a high demand for de novo chlorophyll biosynthesis.

111 Our work challenges the assumption that chlorophyll breakdown is merely a result of senescence,

112 aturated fatty acids, total carotenoids, and chlorophylls, but the lowest oxidative stability.

113 pounds, flavonoids, tannins, carotenoids and chlorophylls) by spectrophotometry and the individual co

114 the oil has low acidity, value of peroxide, chlorophyll, carotenoids, beta-carotene and high concent

115 nt increase (p < 0.05) was observed in total chlorophylls, carotenoids and phenolic contents in the e

116 The level of ascorbic acid, chlorophylls, carotenoids, phenolic compounds and solubl

117 res resulted in coordinated up-regulation of chlorophyll catabolic genes, impairment of chloroplast b

118 he upregulation by heat of genes involved in chlorophyll catabolism and chloroplast protein turnover

119 , highlighting the importance of considering chlorophyll changes at a regional level.

120 g chlorophylls are constitutively present as chlorophyll (Chl) d in the cyanobacterium Acaryochloris

121 Chlorophyll (Chl) f and d are the most recently discover

122 igated whether coral optics affects variable chlorophyll (Chl) fluorescence measurements and derived

123 The study revealed decreases in chlorophyll (Chl) ingestion rate, egg production rate an

124 ixed vibronic Q(y)-Q(x) states, arising from chlorophyll (Chl)-Chl interactions, although almost noth

125 Here, to investigate chlorophyll (Chl)-zeaxanthin (Zea) excitation energy tra

126 e composition of different commercial copper chlorophyll colorants for the first time.

127 veloped to distinguish and quantify two main chlorophyll components (chlorophyll a and b) present in

128 feces showing almost no absorption of copper-chlorophylls compounds.

129 fluorescence microscopy to estimate relative chlorophyll concentration as a function of mesophyll dep

130 ions of sea level anomalies and near-surface chlorophyll concentration in the North Pacific Ocean bet

131 rovides insights into the variation of N and chlorophyll concentration, photosynthesis rates, and N(2

132 etic energy level and an increase in surface chlorophyll concentration.

133 SICE is shown to enhance chlorophyll concentrations by up to 56% relative to ocea

134 algorithms in operational use for retrieving chlorophyll concentrations from ocean color remote sensi

135 amiding favorable alleles for improved N and chlorophyll concentrations, photosynthesis rates, and N(

136 s, correlating with reductions in leaf N and chlorophyll concentrations.

137 which subsequently affect spring and summer chlorophyll concentrations.

138 Temperature and chlorophyll conditions varied markedly due to observed E

139 al photosynthesis can be divided between the chlorophyll-containing plants, algae and cyanobacteria t

140 on dark-adapted and illuminated leaves) and chlorophyll content (Chl) were significantly different a

141 r conditions was mainly due a decline in the chlorophyll content (non-stomatal limitation), whereas t

142 data including canopy temperature (CT), SPAD chlorophyll content (SPAD), membrane thermostability (MT

143 The total phenolic, flavonoid, chlorophyll content (TCC) and antioxidant activity varie

144 OOs of Koroneiki cultivar differing in total chlorophyll content (~12-46 mg/kg) were exposed in paral

145 en communities were protein-rich, had a high chlorophyll content and contained many metabolites assoc

146 rk aimed at examining the combined effect of chlorophyll content and light filtering packaging materi

147 This phenomenon may lead to a higher chlorophyll content and photosynthesis in indica than in

148 Chlorophyll content and the overall acceptance were high

149 SPAD readings showed higher chlorophyll content in 5113-treated stressed seedlings.

150 Chloroplast development and chlorophyll content in the immature fruit has a major im

151 trait loci (QTLs), pc1 and pc10 that affect chlorophyll content in the pepper fruit by modulation of

152 tion of the orthologous genes in controlling chlorophyll content in the Solanaceae.

153 In the typical leaf, chlorophyll content increased gradually as a function of

154 tionships with proxies such as leaf nitrogen/chlorophyll content or hyperspectral reflectance, or on

155 was found to be associated with variation in chlorophyll content primarily in C. chinense.

156 asonal variation in canopy structure, needle chlorophyll content, and absorbed light.

157 mass fraction, fine root mass fraction, and chlorophyll content, as well as leaf sodium and potassiu

158 reflecting a direct effect of soil N on leaf chlorophyll content, but not on litterfall rates.

159 Phenotypic trait data (canopy temperature, chlorophyll content, hyperspectral reflectance, leaf are

160 er frequently studied green algae: decreased chlorophyll content, increased free carotenoid content,

161 There were increases in dry weight, chlorophyll content, lipids, and catalase content when c

162 ore evident in the VOO with the lowest total chlorophyll content.

163 ot lengths, reduced leaf area, and decreased chlorophyll content.

164 and total tocopherol content but the lowest chlorophyll content.

165 A range of chlorophyll contents and net CO(2) assimilation rates ca

166 We demonstrate that the effects of reduced chlorophyll contents on plant growth and development are

167 SA, a* value, browning index, carotenoid and chlorophyll contents while decreased the L* and b* value

168 SA-treated plants displayed higher biomass, chlorophyll contents, relative leaf water and better roo

169 l yield, chemical properties, carotenoid and chlorophyll contents, total phenolic content (TPC), radi

170 mples for Cd binding to soybean proteins and chlorophyll, Cr binding to Arabidopsis thaliana proteins

171 Using a decade of satellite chlorophyll data, we report substantial long-term chloro

172 n a point mutation in the psaA gene mediates chlorophyll deficiency.

173 gradation, has been suggested as a result of chlorophyll deficiency.

174 Chlorophyll deficit suppressed tillering in multiple mai

175 a, the last intact porphyrin intermediate of chlorophyll degradation and a unique pathway "bottleneck

176 cence and chlorotic stress lead to lipid and chlorophyll degradation and the deposition of acyl and p

177 JA-induced anthocyanin accumulation and chlorophyll degradation are enhanced and stomatal immuni

178 clear transcriptome and controls the pace of chlorophyll degradation in senescing leaves.

179 Chlorophyll degradation is one of the most visible signs

180 Genes in the chlorophyll degradation pathway showed differential expr

181 nd phytotoxic catabolite over-buildup in the chlorophyll degradation pathway.

182 time and plant biomass combined with delayed chlorophyll degradation suggests that this stress-escape

183 Chlorophyll degradation was observed, leading to pheophy

184 in winter, more accumulation of anthocyanin, chlorophyll degradation, closure/degradation of photosys

185 lier flowering, smaller flowers, and delayed chlorophyll degradation.

186 in the Stay-Green (OsSGR) gene encoding the chlorophyll-degrading Mg(++)-dechelatase were found to t

187 We examined 56 years of data representing chlorophyll density in 26 areas in British seas monitore

188 1% of long-timescale (> 4yrs) synchrony in a chlorophyll density index, but only 3% of observed short

189 ing the ingestion of copper chlorophylls, no chlorophyll derivative was present in serum nor urine ex

190 We present chlorophyll distribution data and model equations for ma

191 Yet, spatially resolved leaf chlorophyll distribution data are limited.

192 Chlorophyll distribution for the typical leaf from our d

193 This chlorophyll distribution pattern is likely coupled to ad

194 roline in leaves and effective protection of chlorophyll during periods of water limitation.

195 Despite the daily consumption of copper chlorophylls (E-141i), the green food colorants in foods

196 hl) f and d are the most recently discovered chlorophylls, enabling cyanobacteria to harvest near-inf

197 Additionally, the chlorophyll-encapsulated PCL particles exhibited conside

198 The composites (chlorophyll-encapsulated PCL particles) were characteriz

199 ersial explanation suggests seamount-induced chlorophyll enhancements (SICE) subsidize seamount ecosy

200 ophyll data, we report substantial long-term chlorophyll enhancements around 17% of Pacific seamounts

201 We propose that the lack of chlorophyll exerts growth control via energy balance sen

202 The recently discovered, chlorophyll-f-containing, far-red photosystem II (FR-PSI

203 er from chlorophyll-a to the long-wavelength chlorophylls-f/d The data demonstrate the decay of an ~7

204 sing selective excitation of long-wavelength chlorophylls-f/d, and the localization of the excited st

205 ct satellite-derived seasonal to multiannual chlorophyll fluctuations in many regions.

206 rice plants through visual (stay-green) and chlorophyll fluorescence ( PSII) approaches.

207 nitored by respiratory quotient (DCA-RQ) and chlorophyll fluorescence (DCA-CF) on anaerobic metabolis

208 ncurrent satellite retrievals of Sun-induced chlorophyll fluorescence (SIF) and atmospheric CO(2), we

209 sensing allow the detection of solar-induced chlorophyll fluorescence (SIF) emission from vegetation,

210 Effective use of solar-induced chlorophyll fluorescence (SIF) to estimate and monitor g

211 Solar-induced chlorophyll fluorescence (SIF), which is emitted by chlo

212 stem I subunits, acting upstream of the high-chlorophyll fluorescence 101 (HCF101) protein.

213 and photosynthetic analysis by gas exchange, chlorophyll fluorescence and P700 absorption spectroscop

214 As the emitted (bacterio)chlorophyll fluorescence competes with the photochemical

215 senescence responses using a high-throughput chlorophyll fluorescence imaging system.

216 Chlorophyll fluorescence induction experiments indicated

217 Chlorophyll fluorescence kinetic analysis has become an

218 NPQ was dissected into its components, and chlorophyll fluorescence lifetime imaging microscopy (FL

219 ergy-dependent component (qE) and stable (1) chlorophyll fluorescence lifetime; (2) amplitude of the

220 We monitored photoinhibition using the chlorophyll fluorescence parameter of photochemical quen

221 However, chlorophyll fluorescence parameters (as determined on da

222 d single-photon counting, we found that both chlorophyll fluorescence quantum yields and fluorescence

223 obic metabolism in comparison with DCA - CF (chlorophyll fluorescence) and controlled atmosphere (CA)

224 by monitoring multi-year changes in weather, chlorophyll fluorescence, chloroplast ultrastructure, an

225 For chlorophyll fluorescence, F(v)/ F(m) was the most sensit

226 Phenotypic parameters (chlorophyll fluorescence, photosynthetic pigment content

227 of new leaf production, but track changes in chlorophyll fluorescence, the photochemical reflectance

228 been made to this end via visual scoring and chlorophyll fluorescence; however, these approaches dema

229 The scaffold protein HIGH CHLOROPHYLL FLUORESCENCE244 (HCF244) is tethered to the

230 on remained localized on the long-wavelength chlorophyll forms within 0.1-20 ps and revealed little o

231 hyll fluorescence (SIF), which is emitted by chlorophyll, has a strong positive linear relationship w

232 The different modified tetrapyrroles include chlorophylls, hemes, siroheme, corrins (including vitami

233 e world's oceans including high-nutrient low-chlorophyll (HNLC) regions.

234 lular airspaces, the spatial distribution of chlorophyll in laminar leaves was remarkably well conser

235 ratures, cpn60alpha2 mutants accumulate less chlorophyll in newly produced tissues, thus allowing the

236 Photosystem I coordinates more than 90 chlorophylls in its core antenna while achieving near pe

237 te the functionality of the antenna rings of chlorophylls in light-harvesting complexes (LHCs).

238 Singlet oxygen produced from triplet excited chlorophylls in photosynthesis is a signal molecule that

239 d from 243.8 to 234.2 ng/mg cell protein for chlorophylls in the acetone and [C(4)mim]Cl extracts, re

240 tal processes are characterized by a surface chlorophyll increase and secondary ageostrophic upwellin

241 r time scales are more effective in inducing chlorophyll increase than the unbalanced shorter time-sc

242 Chlorophyll is a tetrapyrrole metabolite essential for p

243 Chlorophyll is a valuable bioactive compound, which is u

244 During senescence, chlorophyll is degraded in the multistep pheophorbide a

245 Whether the FeCh CAB domain also binds chlorophyll is unknown.

246 However, chlorophyll is unstable when it comes to retaining its a

247 the inflorescence decline with a decrease in chlorophyll level.

248 was lower in the impacted creek, and higher chlorophyll levels were observed in a downstream coastal

249 plant height showed a nonlinear response to chlorophyll levels.

250 Deep Chlorophyll Maxima (DCMs) are subsurface peaks in chloro

251 Cyanophages at the oxic primary chlorophyll maximum encoded genes related to light and p

252 where Prochlorococcus dominates a secondary chlorophyll maximum within the ODZ.

253 g two cruises, spanning depths near the deep chlorophyll maximum, where the abundance of PPEs was hig

254 ey were overrepresented in the porphyrin and chlorophyll metabolism pathways.

255 urbations first occur at the special pair of chlorophyll molecules of the photosynthetic reaction cen

256 hocystis PCC 6803 leads to overproduction of chlorophyll molecules that accumulate in the thylakoid m

257 During the ingestion of copper chlorophylls, no chlorophyll derivative was present in s

258 electronic properties of tetrapyrroles like chlorophyll or heme.

259 ots and nonsignificant variances in biomass, chlorophyll (p > 0.19), and peroxidase between BPA-treat

260 1 and D2 core polypeptides and comprise four chlorophyll (P(D1), P(D2), Chl(D1), Chl(D2)) and two phe

261 Even if no variation was detected for chlorophylls (p > 0.05), total carotenoids were increase

262 donor is chlorophyll-a (P(D1) of the central chlorophyll pair).

263 nt with concurrently observed stimulation of chlorophyll production upon additions of manganese or ir

264 plant functional types (defined according to chlorophyll profile similarity, clade, and leaf thicknes

265 These proteins are arranged in fucoxanthin-chlorophyll protein (FCP) complexes.

266 of PGPR and PGRs significantly enhanced the chlorophyll, protein, and sugar contents compared to irr

267 latter of which are also called fucoxanthin-chlorophyll proteins (FCP).

268 was used to analyse the dynamics of excited chlorophyll relaxation in isoprene-emitting and nonemitt

269 than unbleached sea anemones, whereas total chlorophyll remained similar.

270 Ethanolic guava leaf extract (EGLE) without chlorophyll removal (GLE-C) and those with chlorophyll r

271 t chlorophyll removal (GLE-C) and those with chlorophyll removal using sedimentation process (GLE-S)

272 Low energy chlorophylls (also known as red chlorophylls) residing in the antenna are important for

273 s primarily from successfully simulating the chlorophyll response to the El Nino-Southern Oscillation

274 rotenoid pigments at high irradiance or more chlorophyll, resulting in corresponding differences in p

275 Chlorophyll rings (CRs) are defined as elevated chloroph

276 A major component is thermal dissipation of chlorophyll singlet excited states and is called nonphot

277 and In(OTf)(3) at 80 degrees C afforded the chlorophyll skeleton as the chloroindium(III) chelate; t

278 The chlorophyll skeleton contains a chlorin macrocycle and a

279 The Cu N(x) is formed by intercalation of chlorophyll sodium copper salt into a melamine-based sup

280 L particles exhibited considerably prolonged chlorophyll stability.

281 h the participation of higher-lying vibronic chlorophyll states and assign observed oscillatory featu

282 ies correspond to known vibrational modes of chlorophyll, suggesting that electronic-vibrational mixi

283 The dominant source of long-timescale chlorophyll synchrony was closely related to sea surface

284 magnesium chelatase, an enzyme necessary for chlorophyll synthesis.

285 , phenols, sterols, fatty acids, phthalides, chlorophylls, tannins and flavonoids were detected in di

286 by energy transfer from the long-wavelength chlorophyll to P(700).

287 one of which is a previously uncharacterized chlorophyll-to-carotenoid energy transfer.

288 or the synthesis of key isoprenoids, such as chlorophylls, tocopherols, phylloquinone, gibberellins,

289 Regional chlorophyll trends are found to be significantly differe

290 We produce estimates of ocean surface chlorophyll trends, by using Coupled Model Intercomparis

291 theses of members of the family of (bacterio)chlorophylls, two routes to 2-iodo-3-methyl-4-(3-methoxy

292 exclusively responsible for both transverse (chlorophylls versus pheophytins) and lateral (D1 versus

293 Furthermore, total chlorophyll was 66% higher in the bleached sea anemones

294 total carotenoids and 45.9% and 68.7% of the chlorophylls were bioaccessible from the acetone and [C(

295 cellular uptakes of carotenoids, esters and chlorophylls were evaluated, since the influence of este

296 nolic compounds, tocopherol, carotenoids and chlorophylls when EVOO was evaluated by UV-Vis spectrosc

297 changes in algal symbiont density and total chlorophyll, which increased by 103% and 264%, respectiv

298 t the lutein 2 S1 state does not transfer to chlorophylls, while lutein 1 is the only carotenoid whos

299 lor sensors provide coverage of global ocean chlorophyll with a combined record length of ~ 20 years.

300 ing and modeling the spatial distribution of chlorophyll within the leaf is critical for understandin