植物中的光敏色素

光敏色素是植物体内的光受体。本介绍了光敏色素的结构、特征及由光敏色素引发的昼夜节律生物钟,着重介绍了在信号转导和昼夜节律系统中的光敏色素作用因子。     

Interactive Effects of Ocean Acidification and Nitrogen-Limitation on the Diatom Phaeodactylum tricornutum

Climate change is expected to bring about alterations in the marine physical and chemical environment that will induce changes in the concentration of dissolved CO₂ and in nutrient availability. These in turn are expected to affect the physiological performance of phytoplankton. In order to learn how phytoplankton respond to the predicted scenario of increased CO₂ and decreased nitrogen in the surface mixed layer, we investigated the diatom Phaeodactylum tricornutum as a model organism. The cells were cultured in both low CO₂ (390 μatm) and high CO₂ (1000 μatm) conditions at limiting (10 μmol L⁻¹) or enriched (110 μmol L⁻¹) nitrate concentrations. Our study shows that nitrogen limitation resulted in significant decreases in cell size, pigmentation, growth rate and effective quantum yield of Phaeodactylum tricornutum, but these parameters were not affected by enhanced dissolved CO₂ and lowered pH. However, increased CO₂ concentration induced higher rETR_max and higher dark respiration rates and decreased the CO₂ or dissolved inorganic carbon (DIC) affinity for electron transfer (shown by higher values for K_{1/2 DIC} or K_{1/2 CO2}). Furthermore, the elemental stoichiometry (carbon to nitrogen ratio) was raised under high CO₂ conditions in both nitrogen limited and nitrogen replete conditions, with the ratio in the high CO₂ and low nitrate grown cells being higher by 45% compared to that in the low CO₂ and nitrate replete grown ones. Our results suggest that while nitrogen limitation had a greater effect than ocean acidification, the combined effects of both factors could act synergistically to affect marine diatoms and related biogeochemical cycles in future oceans.     

Diatom distribution and paleoceanographic reconstruction in the Southern Ocean — Present and last glacial maximum

Diatom assemblage and preservational data are used to reconstruct paleoceanographic conditions at the last glacial maximum (18,000 yrs BP) in the Southern Ocean. From these data, the following points can be made about the last glacial maximum in this region. (1) Contraction and slight northern shift of the belt of well preserved diatoms appears to be related to the northward shift of late spring/early summer sea ice cover. (2) Presence of open-ocean, though poorly preserved, diatom assemblages to the south of this belt strongly suggest that, during many summers, large areas of the Southern Ocean were ice-free. (3) The distribution of theNitzschia kerguelensis factor, both in surface sediments and at the last glacial maximum, indicates that the gyre systems, particularly the Weddell Gyre, were intensified during glacial times. (4) Although data are sparse in the higher-latitude South Atlantic, there is an indication that the Weddell Polynya also existed during glacial times, although it was shifted a few degrees northward.     

Interspecific Chromosome-Wide Transcription Profiles Reveal the Existence of Mammalian-Specific and Species-Specific Chromosome Domains

A long-range exploration of expression levels through wide chromosome territories was carried out in three species (pig, cattle, and chicken) by aligning EST counts against the human genome. This strategy made it possible to produce expression profiles that were very similar between pig and cattle and that were significantly correlated with chicken levels of expression. In parallel with these alignments, we developed a statistical approach enabling us to screen genomic regions for both underexpression and overexpression at the chromosome level within a given species, as well as interspecifically. The observed correlations are indicative of the existence of interspecifically conserved domains of gene expression, not only for housekeeping genes (which are highly expressed), but also for regions where genes are significantly underexpressed. Furthermore, our strategy made it possible to point out regions that are differentially regulated between species. These expression data were crossed with available comparative mapping information for pigs and cattle, suggesting that coregulated regions are syntenic in various mammals.     

Light-Modulated Responses of Growth and Photosynthetic Performance to Ocean Acidification in the Model Diatom Phaeodactylum tricornutum

Ocean acidification (OA) due to atmospheric CO₂ rise is expected to influence marine primary productivity. In order to investigate the interactive effects of OA and light changes on diatoms, we grew Phaeodactylum tricornutum, under ambient (390 ppmv; LC) and elevated CO₂ (1000 ppmv; HC) conditions for 80 generations, and measured its physiological performance under different light levels (60 µmol m⁻² s⁻¹, LL; 200 µmol m⁻² s⁻¹, ML; 460 µmol m⁻² s⁻¹, HL) for another 25 generations. The specific growth rate of the HC-grown cells was higher (about 12–18%) than that of the LC-grown ones, with the highest under the ML level. With increasing light levels, the effective photochemical yield of PSII (F_v′/F_m′) decreased, but was enhanced by the elevated CO₂, especially under the HL level. The cells acclimated to the HC condition showed a higher recovery rate of their photochemical yield of PSII compared to the LC-grown cells. For the HC-grown cells, dissolved inorganic carbon or CO₂ levels for half saturation of photosynthesis (K_1/2 DIC or K_1/2 CO₂) increased by 11, 55 and 32%, under the LL, ML and HL levels, reflecting a light dependent down-regulation of carbon concentrating mechanisms (CCMs). The linkage between higher level of the CCMs down-regulation and higher growth rate at ML under OA supports the theory that the saved energy from CCMs down-regulation adds on to enhance the growth of the diatom.     

Bathy Phytochromes in Rhizobial Soil Bacteria

Phytochromes are biliprotein photoreceptors that are found in plants, bacteria, and fungi. Prototypical phytochromes have a Pr ground state that absorbs in the red spectral range and is converted by light into the Pfr form, which absorbs longer-wavelength, far-red light. Recently, some bacterial phytochromes have been described that undergo dark conversion of Pr to Pfr and thus have a Pfr ground state. We show here that such so-called bathy phytochromes are widely distributed among bacteria that belong to the order Rhizobiales. We measured in vivo spectral properties and the direction of dark conversion for species which have either one or two phytochrome genes. Agrobacterium tumefaciens C58 contains one bathy phytochrome and a second phytochrome which undergoes dark conversion of Pfr to Pr in vivo. The related species Agrobacterium vitis S4 contains also one bathy phytochrome and another phytochrome with novel spectral properties. Rhizobium leguminosarum 3841, Rhizobium etli CIAT652, and Azorhizobium caulinodans ORS571 contain a single phytochrome of the bathy type, whereas Xanthobacter autotrophicus Py2 contains a single phytochrome with dark conversion of Pfr to Pr. We propose that bathy phytochromes are adaptations to the light regime in the soil. Most bacterial phytochromes are light-regulated histidine kinases, some of which have a C-terminal response regulator subunit on the same protein. According to our phylogenetic studies, the group of phytochromes with this domain arrangement has evolved from a bathy phytochrome progenitor.Phytochromes are biological photoreceptors that were discovered in plants, where they control development throughout the life cycle in manifold ways (21, 33). Today, a large number of homologs are known also from cyanobacteria, other bacteria, and fungi, which are termed cyanobacterial phytochromes (Cphs), bacteriophytochromes (BphPs), and fungal phytochromes (Fphs), respectively (20, 24). The chromophore is autocatalytically assembled within the N-terminal part of the protein, the photosensory core module (PCM), which contains the PAS, GAF, and PHY domains (30). Typically, phytochromes are converted by light between two spectrally different forms, the red-absorbing Pr and the far-red-absorbing Pfr forms. Photoconversion is initiated by an isomerization of the covalently bound bilin chromophore (32).Plant and cyanobacterial phytochromes incorporate phytochromobilin (PΦB) and phycocyanobilin (PCB) as natural chromophores, respectively, which are covalently bound to Cys residues in the GAF domains. All characterized phytochromes that belong to these groups have a Pr ground state. Plant phytochromes can undergo dark conversion of Pfr to Pr (5), whereas the Pfr form of typical cyanobacterial phytochromes is stable in darkness (26).Bacteriophytochromes utilize biliverdin (BV) instead as a natural chromophore (1), which is covalently attached to a Cys residue in the N terminus of the PAS domain (26). Since the conjugated system of BV is longer than that of PΦB or PCB, the absorption maxima of bacteriophytochromes are found at higher wavelengths than those of cyanobacterial or plant homologs.With the discovery of a bacterial phytochrome from Bradyrhizobium sp. strain ORS278, termed BrBphP1, the first phytochrome with a Pfr ground state and dark conversion from Pr to Pfr was found (10). Thereafter, five more phytochromes with dark conversion of Pr to Pfr were described: Rhodopseudomonas palustris BphP1 (RpBphP1) from strain CEA001, RpBphP5, and RpBphP6 from strain CGA009 (11); Agrobacterium tumefaciens Agp2 (or AtBphP2) from strain C58 (18); and Pseudomonas aeruginosa BphP1 (PaBphP1) (40). These phytochromes are now termed bathy phytochromes because the absorption maxima of their ground states are bathochromically (to longer wavelengths) shifted compared to those of all other phytochromes.Moreover, some other bacterial phytochromes with unusual properties have been described. In the Ppr from Rhodospirillum centenum, a photoactive yellow protein (PYP) domain is fused to the N terminus of a phytochrome homolog. The phytochrome part of Ppr assembles with BV to form a Pr adduct. However, irradiation does not result in the formation of Pfr but in a bleaching of the Pr spectrum (23). The BV adduct of RpBphP3 from R. palustris, which has a Pr ground state, photoconverts to the so-called Pnr form with a blue-shifted absorption maximum (12). RpBphP4 from R. palustris strains Ha2 and BisB5 and Bradyrhizobium BphP3 (BrBphP3) from Bradyrhizobium BTAi1, both with a Pr ground state, photoconvert into a long-lived MetaR form (8, 42). MetaRa and MetaRc are intermediates in the photoconversion from Pr to Pfr of prototypical phytochromes (3). BphP3 from the Bradyrhizobium strain ORS 278 is an exception among bacteriophytochromes as it binds PCB as a natural chromophore. This phytochrome adopts a so-called Po (P-orange) ground state with an absorbance maximum in the orange range (11, 15). Upon irradiation, this phytochrome converts into the Pr form. RpBphP4 from R. palustris CGA009 lacks the biliverdin binding cysteine and does not bind a chromophore (42).With the rapidly growing number of bacterial genome sequences, many new bacterial phytochromes are being discovered. Thus, a large and increasing number of newly identified phytochromes remain spectroscopically uncharacterized. We established an in vivo photometry approach which allowed the rapid acquisition of spectral information about phytochromes from intact bacterial cells. In the beginning period of plant phytochrome research, in vivo photometry was extensively applied (4, 6, 29, 34). This method, in fact, allowed the identification of phytochromes for the first time in plant tissues (6), which led to the purification of phytochromes from plant extracts (37). Here, we apply in vivo photometry for the first time to organisms outside the plant kingdom. This method is especially useful for studying species with single phytochrome genes. The approach is also helpful for comparing properties of native phytochromes in vivo and of their recombinant proteins in vitro.In the present study, we concentrate on nonphotosynthetic species of the order Rhizobiales which belongs to the Alphaproteobacteria. The family Rhizobiaceae comprises plant-interacting soil bacteria. A. tumefaciens and Agrobacterium vitis can transfer genes into plants to induce plant tumors, whereas many other Rhizobiaceae can live as plant symbionts in nodules of stems or roots in which they assimilate molecular nitrogen to produce NH₄⁺, which is used by the plant for synthesis of amino acids and other nitrogen-containing molecules. A. tumefaciens C58 contains two phytochromes, termed Agp1 (or AtBphP1) and Agp2 (or AtBphP2), that have been characterized as recombinant proteins (14, 18, 26, 35) and whose spectral activities have been measured in extracts of wild-type and knockout mutants (31). A large number of phytochromes from photosynthetic Bradyrhizobium and Rhodopseudomonas species, which also belong to the order Rhizobiales, have been characterized as recombinant proteins (11), some of which have already been noted above.It turned out that most of our analyzed phytochromes undergo dark conversion of Pr to Pfr and thus belong to the group of bathy phytochromes. Such phytochromes, which absorb at around 750 nm, clearly dominate among Rhizobiales. We propose that this specific property reflects an adaptation to the light regime in the soil. Our studies also suggest that bacterial phytochromes with a C-terminal response regulator have evolved from a bathy phytochrome progenitor.     

Adaptive Evolution in the GAF Domain of Phytochromes in Gymnosperms

The GAF domain of phytochrome is essential for photoconversion and signal transduction. In gymnosperms, it exists in all members of the phytochrome family that experience gene duplication. Maximum-likelihood models of codon substitution can provide a framework for constructing likelihood ratio tests of changes in selective pressure and make clear predictions about patterns of genetic change following gene duplication. In this study, 68 gymnosperm GAF sequences were analyzed to identify lineages and sites under positive selection. Our results indicate that (1) positive selection at a few sites (3.6%), rather than relaxation of selective constraints, has played a major role in the evolution of the gymnosperm GAF domain; (2) strong positive selective pressure tends to occur in the recent PHYP lineages of cogeneric species, but is absent in old lineages consisting of distantly related species; and (3) the selective pressure indicated by the ω ratio varies greatly among lineages and sites in the GAF domain.     

Diatom assemblages in tsunami deposits associated with the 2004 Indian Ocean tsunami at Phra Thong Island, Thailand

Diatom assemblages in sandy deposits of the 2004 tsunami at Phra Thong Island, Thailand may provide clues to flow conditions during the tsunami. The tsunami deposits contain one or more beds that fine upward, commonly from medium sand to silty very fine sand. Diatom assemblages of the lowermost portion of the deposit predominantly comprise unbroken beach and subtidal species that live attached to sand grains. The dominant taxa shift to marine plankton species in the middle of the bed and to a mix of freshwater, brackish, and marine species near the top. These trends are consistent with expected changes in current velocities of tsunami through time. During high current velocities, medium sand is deposited; only beach and subtidal benthic diatoms attached to sediment can be incorporated into the tsunami deposit. High shear velocity keeps finer material, including planktonic diatoms in suspension. With decreasing current velocities, finer material including marine plankton can be deposited. Finally, during the lull between tsunami waves, the entrained freshwater, brackish, and marine species settle out with mud and plant trash. Low numbers of broken diatoms in the lower medium sand implies rapid entrainment and deposition, whilst selective breakage of marine plankton (Thalassionema nitzschioides, and Thalassiosira and Coscinodiscus spp.) in the middle portion of the deposit probably results from abrasion in the turbulent current before deposition.     

Whisker Movements Reveal Spatial Attention: A Unified Computational Model of Active Sensing Control in the Rat

Spatial attention is most often investigated in the visual modality through measurement of eye movements, with primates, including humans, a widely-studied model. Its study in laboratory rodents, such as mice and rats, requires different techniques, owing to the lack of a visual fovea and the particular ethological relevance of orienting movements of the snout and the whiskers in these animals. In recent years, several reliable relationships have been observed between environmental and behavioural variables and movements of the whiskers, but the function of these responses, as well as how they integrate, remains unclear. Here, we propose a unifying abstract model of whisker movement control that has as its key variable the region of space that is the animal''s current focus of attention, and demonstrate, using computer-simulated behavioral experiments, that the model is consistent with a broad range of experimental observations. A core hypothesis is that the rat explicitly decodes the location in space of whisker contacts and that this representation is used to regulate whisker drive signals. This proposition stands in contrast to earlier proposals that the modulation of whisker movement during exploration is mediated primarily by reflex loops. We go on to argue that the superior colliculus is a candidate neural substrate for the siting of a head-centred map guiding whisker movement, in analogy to current models of visual attention. The proposed model has the potential to offer a more complete understanding of whisker control as well as to highlight the potential of the rodent and its whiskers as a tool for the study of mammalian attention.     

Evolutionary Studies Illuminate the Structural-Functional Model of Plant Phytochromes

A synthesis of insights from functional and evolutionary studies reveals how the phytochrome photoreceptor system has evolved to impart both stability and flexibility. Phytochromes in seed plants diverged into three major forms, phyA, phyB, and phyC, very early in the history of seed plants. Two additional forms, phyE and phyD, are restricted to flowering plants and Brassicaceae, respectively. While phyC, D, and E are absent from at least some taxa, phyA and phyB are present in all sampled seed plants and are the principal mediators of red/far-red–induced responses. Conversely, phyC-E apparently function in concert with phyB and, where present, expand the repertoire of phyB activities. Despite major advances, aspects of the structural-functional models for these photoreceptors remain elusive. Comparative sequence analyses expand the array of locus-specific mutant alleles for analysis by revealing historic mutations that occurred during gene lineage splitting and divergence. With insights from crystallographic data, a subset of these mutants can be chosen for functional studies to test their importance and determine the molecular mechanism by which they might impact light perception and signaling. In the case of gene families, where redundancy hinders isolation of some proportion of the relevant mutants, the approach may be particularly useful.     

植物光敏色素入核机理的研究进展

光敏色素是植物感受外界环境变化的重要光受体,它对植物的生长发育具有重要的调控作用。在介绍植物光敏色素分子结构的基础上,对不同光敏色素的入核机理以及核内定位进行了综述,并根据最新研究进展对光敏色素入核机理进行了展望。     

Spatially Explicit Estimates of Prey Consumption Reveal a New Krill Predator in the Southern Ocean

Development in foraging behaviour and dietary intake of many vertebrates are age-structured. Differences in feeding ecology may correlate with ontogenetic shifts in dispersal patterns, and therefore affect foraging habitat and resource utilization. Such life-history traits have important implications in interpreting tropho-dynamic linkages. Stable isotope ratios in the whiskers of sub-yearling southern elephant seals (Mirounga leonina; n = 12) were used, in conjunction with satellite telemetry and environmental data, to examine their foraging habitat and diet during their first foraging migration. The trophic position of seals from Macquarie Island (54°30′S, 158°57′E) was estimated using stable carbon (δ^{1 3}C) and nitrogen (δ¹⁵N) ratios along the length of the whisker, which provided a temporal record of prey intake. Satellite-relayed data loggers provided details on seal movement patterns, which were related to isotopic concentrations along the whisker. Animals fed in waters south of the Polar Front (>60°S) or within Commission for the Conservation of Antarctic Marine Living Resources (CCAMLR) Statistical Subareas 88.1 and 88.2, as indicated by both their depleted δ^{1 3}C (<−20‰) values, and tracking data. They predominantly exploited varying proportions of mesopelagic fish and squid, and crustaceans, such as euphausiids, which have not been reported as a prey item for this species. Comparison of isotopic data between sub-yearlings, and 1, 2 and 3 yr olds indicated that sub-yearlings, limited by their size, dive capabilities and prey capture skills to feeding higher in the water column, fed at a lower trophic level than older seals. This is consistent with the consumption of euphausiids and most probably, Antarctic krill (Euphausia superba), which constitute an abundant, easily accessible source of prey in water masses used by this age class of seals. Isotopic assessment and concurrent tracking of seals are successfully used here to identify ontogenetic shifts in broad-scale foraging habitat use and diet preferences in a highly migratory predator.     

Phytochromes influence stomatal conductance plasticity in Arabidopsis thaliana

The ability to sense and respond effectively to drought stress can be important for plant fitness. Here, phytochrome loss-of-function mutants were grown in dry and moist conditions to examine the role of three photoreceptors (phyA, phyB, and phyE) in stomatal conductance (g _ST) and abscisic acid (ABA) concentration. Overall, drought treatment plants had lower g _ST than moist treatment plants. However, the wild-type Landsberg erecta line had a less pronounced conductance response to drought treatment than the phytochrome mutants, suggesting a role for phytochrome in suppressing drought tolerance. Phytochrome gene effects were potentially additive for g _ST; however, PHYB and PHYE effects were nonadditive for ABA concentration.     

Structure of the Biliverdin Cofactor in the Pfr State of Bathy and Prototypical Phytochromes

Phytochromes act as photoswitches between the red- and far-red absorbing parent states of phytochromes (Pr and Pfr). Plant phytochromes display an additional thermal conversion route from the physiologically active Pfr to Pr. The same reaction pattern is found in prototypical biliverdin-binding bacteriophytochromes in contrast to the reverse thermal transformation in bathy bacteriophytochromes. However, the molecular origin of the different thermal stabilities of the Pfr states in prototypical and bathy bacteriophytochromes is not known. We analyzed the structures of the chromophore binding pockets in the Pfr states of various bathy and prototypical biliverdin-binding phytochromes using a combined spectroscopic-theoretical approach. For the Pfr state of the bathy phytochrome from Pseudomonas aeruginosa, the very good agreement between calculated and experimental Raman spectra of the biliverdin cofactor is in line with important conclusions of previous crystallographic analyses, particularly the ZZEssa configuration of the chromophore and its mode of covalent attachment to the protein. The highly homogeneous chromophore conformation seems to be a unique property of the Pfr states of bathy phytochromes. This is in sharp contrast to the Pfr states of prototypical phytochromes that display conformational equilibria between two sub-states exhibiting small structural differences at the terminal methine bridges A-B and C-D. These differences may mainly root in the interactions of the cofactor with the highly conserved Asp-194 that occur via its carboxylate function in bathy phytochromes. The weaker interactions via the carbonyl function in prototypical phytochromes may lead to a higher structural flexibility of the chromophore pocket opening a reaction channel for the thermal (ZZE → ZZZ) Pfr to Pr back-conversion.     

Carbon and Nitrogen Isotopes from Top Predator Amino Acids Reveal Rapidly Shifting Ocean Biochemistry in the Outer California Current

Climatic variation alters biochemical and ecological processes, but it is difficult both to quantify the magnitude of such changes, and to differentiate long-term shifts from inter-annual variability. Here, we simultaneously quantify decade-scale isotopic variability at the lowest and highest trophic positions in the offshore California Current System (CCS) by measuring δ¹⁵N and δ¹³C values of amino acids in a top predator, the sperm whale (Physeter macrocephalus). Using a time series of skin tissue samples as a biological archive, isotopic records from individual amino acids (AAs) can reveal the proximate factors driving a temporal decline we observed in bulk isotope values (a decline of ≥1 ‰) by decoupling changes in primary producer isotope values from those linked to the trophic position of this toothed whale. A continuous decline in baseline (i.e., primary producer) δ¹⁵N and δ¹³C values was observed from 1993 to 2005 (a decrease of ∼4‰ for δ¹⁵N source-AAs and 3‰ for δ¹³C essential-AAs), while the trophic position of whales was variable over time and it did not exhibit directional trends. The baseline δ¹⁵N and δ¹³C shifts suggest rapid ongoing changes in the carbon and nitrogen biogeochemical cycling in the offshore CCS, potentially occurring at faster rates than long-term shifts observed elsewhere in the Pacific. While the mechanisms forcing these biogeochemical shifts remain to be determined, our data suggest possible links to natural climate variability, and also corresponding shifts in surface nutrient availability. Our study demonstrates that isotopic analysis of individual amino acids from a top marine mammal predator can be a powerful new approach to reconstructing temporal variation in both biochemical cycling and trophic structure.     

A New Appraisal of the Prokaryotic Origin of Eukaryotic Phytochromes

The evolutionary origin of the phytochromes of eukaryotes is controversial. Three cyanobacterial proteins have been described as ``phytochrome-like' and have been suggested to be potential ancestors of these essential photoreceptors: Cph1 from Synechocystis PCC 6803, showing homology to phytochromes along its entire length and known to attach a chromophore; and PlpA from Synechocystis PCC 6803 and RcaE from Fremyella diplosiphon, both showing homology to phytochromes most strongly only in the C-terminal region and not known to bind a chromophore. We have reexamined the evolution of the photoreceptors using for PCR amplification a highly conserved region encoding the chromophore-binding domain in both Cph1 and phytochromes of plants and have identified genes for phytochrome-like proteins (PLP) in 11 very diverse cyanobacteria. The predicted gene products contain either a Cys, Arg, Ile, or Leu residue at the putative chromophore binding site. In 10 of the strains examined only a single gene was found, but in Calothrix PCC 7601 two genes (cphA and cphB) were identified. Phylogenetic analysis revealed that genes encoding PLP are homologues that share a common ancestor with the phytochromes of eukaryotes and diverged before the latter. In contrast, the putative sensory/regulatory proteins, including PlpA and RcaE, that lack a part of the chromophore lyase domain essential for chromophore attachment on the apophytochrome, are only distantly related to phytochromes. The Ppr protein of the anoxygenic photosynthetic bacterium Rhodospirillum centenum and the bacterial phytochrome-like proteins (BphP) of Deinococcus radiodurans and Pseudomonas aeruginosa fall within the cluster of cyanobacterial phytochromes. Received: 9 December 1999 / Accepted: 10 May 2000     

Phytochromes A and B mediate red-light-induced positive phototropism in roots

The interaction of tropisms is important in determining the final growth form of the plant body. In roots, gravitropism is the predominant tropistic response, but phototropism also plays a role in the oriented growth of roots in flowering plants. In blue or white light, roots exhibit negative phototropism that is mediated by the phototropin family of photoreceptors. In contrast, red light induces a positive phototropism in Arabidopsis roots. Because this red-light-induced response is weak relative to both gravitropism and negative phototropism, we used a novel device to study phototropism without the complications of a counteracting gravitational stimulus. This device is based on a computer-controlled system using real-time image analysis of root growth and a feedback-regulated rotatable stage. Our data show that this system is useful to study root phototropism in response to red light, because in wild-type roots, the maximal curvature detected with this apparatus is 30 degrees to 40 degrees, compared with 5 degrees to 10 degrees without the feedback system. In positive root phototropism, sensing of red light occurs in the root itself and is not dependent on shoot-derived signals resulting from light perception. Phytochrome (Phy)A and phyB were severely impaired in red-light-induced phototropism, whereas the phyD and phyE mutants were normal in this response. Thus, PHYA and PHYB play a key role in mediating red-light-dependent positive phototropism in roots. Although phytochrome has been shown to mediate phototropism in some lower plant groups, this is one of the few reports indicating a phytochrome-dependent phototropism in flowering plants.