Photosynthesis
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Light-Induced Psba Translation in Plants Is Triggered by Photosystem II Damage Via an Assembly-Linked Autoregulatory Circuit
Light-induced psbA translation in plants is triggered by photosystem II damage via an assembly-linked autoregulatory circuit Prakitchai Chotewutmontria and Alice Barkana,1 aInstitute of Molecular Biology, University of Oregon, Eugene, OR 97403 Edited by Krishna K. Niyogi, University of California, Berkeley, CA, and approved July 22, 2020 (received for review April 26, 2020) The D1 reaction center protein of photosystem II (PSII) is subject to mRNA to provide D1 for PSII repair remain obscure (13, 14). light-induced damage. Degradation of damaged D1 and its re- The consensus view in recent years has been that psbA transla- placement by nascent D1 are at the heart of a PSII repair cycle, tion for PSII repair is regulated at the elongation step (7, 15–17), without which photosynthesis is inhibited. In mature plant chloro- a view that arises primarily from experiments with the green alga plasts, light stimulates the recruitment of ribosomes specifically to Chlamydomonas reinhardtii (Chlamydomonas) (18). However, we psbA mRNA to provide nascent D1 for PSII repair and also triggers showed recently that regulated translation initiation makes a a global increase in translation elongation rate. The light-induced large contribution in plants (19). These experiments used ribo- signals that initiate these responses are unclear. We present action some profiling (ribo-seq) to monitor ribosome occupancy on spectrum and genetic data indicating that the light-induced re- cruitment of ribosomes to psbA mRNA is triggered by D1 photo- chloroplast open reading frames (ORFs) in maize and Arabi- damage, whereas the global stimulation of translation elongation dopsis upon shifting seedlings harboring mature chloroplasts is triggered by photosynthetic electron transport. -
7.014 Handout PRODUCTIVITY: the “METABOLISM” of ECOSYSTEMS
7.014 Handout PRODUCTIVITY: THE “METABOLISM” OF ECOSYSTEMS Ecologists use the term “productivity” to refer to the process through which an assemblage of organisms (e.g. a trophic level or ecosystem assimilates carbon. Primary producers (autotrophs) do this through photosynthesis; Secondary producers (heterotrophs) do it through the assimilation of the organic carbon in their food. Remember that all organic carbon in the food web is ultimately derived from primary production. DEFINITIONS Primary Productivity: Rate of conversion of CO2 to organic carbon (photosynthesis) per unit surface area of the earth, expressed either in terns of weight of carbon, or the equivalent calories e.g., g C m-2 year-1 Kcal m-2 year-1 Primary Production: Same as primary productivity, but usually expressed for a whole ecosystem e.g., tons year-1 for a lake, cornfield, forest, etc. NET vs. GROSS: For plants: Some of the organic carbon generated in plants through photosynthesis (using solar energy) is oxidized back to CO2 (releasing energy) through the respiration of the plants – RA. Gross Primary Production: (GPP) = Total amount of CO2 reduced to organic carbon by the plants per unit time Autotrophic Respiration: (RA) = Total amount of organic carbon that is respired (oxidized to CO2) by plants per unit time Net Primary Production (NPP) = GPP – RA The amount of organic carbon produced by plants that is not consumed by their own respiration. It is the increase in the plant biomass in the absence of herbivores. For an entire ecosystem: Some of the NPP of the plants is consumed (and respired) by herbivores and decomposers and oxidized back to CO2 (RH). -
Lecture 29 Spring 2007
Geol. 656 Isotope Geochemistry Lecture 29 Spring 2007 ISOTOPE FRACTIONATION IN THE BIOSPHERE INTRODUCTION As we noted, biological processes often involve large isotopic fractionations. Indeed, biological proc- esses are the most important cause of variations in the isotope composition of carbon, nitrogen, and sul- fur. For the most part, the largest fractionations occur during the initial production of organic matter by the so-called primary producers, or autotrophs. These include all plants and many kinds of bacteria. The most important means of production of organic matter is photosynthesis, but organic matter may also be produced by chemosynthesis, for example at mid-ocean ridge hydrothermal vents. Large frac- tions of both carbon and nitrogen occur during primary production. Additional fractionations also oc- cur in subsequent reactions and up through the food chain as hetrotrophs consume primary producers, but these are generally smaller. CARBON ISOTOPE FRACTIONATION DURING PHOTOSYNTHESIS The most important of process producing isotopic fractionation of carbon is photosynthesis. As we earlier noted, photosynthetic fractionation of carbon isotopes is primarily kinetic. The early work of Park and Epstein (1960) suggested fractionation occurred in several steps. Subsequent work has eluci- dated the fractionations involved in these steps, which we will consider in more detail here. For terrestrial plants (those utilizing atmospheric CO2), the first step is diffusion of CO2 into the boundary layer surrounding the leaf, through the stomata, and internally in the leaf. The average δ13C of various species of plants has been correlated with the stomatal conductance (Delucia et al., 1988), in- dicating that diffusion into the plant is indeed important in fractionating carbon isotopes. -
Evolution of Photochemical Reaction Centres
bioRxiv preprint doi: https://doi.org/10.1101/502450; this version posted December 20, 2018. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY 4.0 International license. 1 Evolution of photochemical reaction 2 centres: more twists? 3 4 Tanai Cardona, A. William Rutherford 5 Department of Life Sciences, Imperial College London, London, UK 6 Correspondence to: [email protected] 7 8 Abstract 9 The earliest event recorded in the molecular evolution of photosynthesis is the structural and 10 functional specialisation of Type I (ferredoxin-reducing) and Type II (quinone-reducing) reaction 11 centres. Here we point out that the homodimeric Type I reaction centre of Heliobacteria has a Ca2+- 12 binding site with a number of striking parallels to the Mn4CaO5 cluster of cyanobacterial 13 Photosystem II. This structural parallels indicate that water oxidation chemistry originated at the 14 divergence of Type I and Type II reaction centres. We suggests that this divergence was triggered by 15 a structural rearrangement of a core transmembrane helix resulting in a shift of the redox potential 16 of the electron donor side and electron acceptor side at the same time and in the same redox direction. 17 18 Keywords 19 Photosynthesis, Photosystem, Water oxidation, Oxygenic, Anoxygenic, Reaction centre 20 21 Evolution of Photosystem II 22 There is no consensus on when and how oxygenic photosynthesis originated. Both the timing and the 23 evolutionary mechanism are disputed. -
The Electron Transport Chain in Anaerobically Functioning Eukaryotes
rl BIOCHIMICA ET BIOPHYSICA ACTA II BBt ELSEVIER Biochimica et Biophysica Acta, 1365 (1998) 71-78 The electron transport chain in anaerobically functioning eukaryotes Aloysius G.M. Tielens*, Jaap J. Van Hellemond Laboratory of Veterinary Biochemistry and Institute for Biomembranes, Utrecht University, P.O. Box 80176, 3508 TD Utrecht, The Netherlands Received 27 January 1998; received in revised form 26 February 1998; accepted 2 March 1998 Abstract Many lower eukaryotes can survive anaerobic conditions via a fermentation pathway that involves the use of the reduction of endogenously produced fumarate as electron sink. This fumarate reduction is linked to electron transport in an especially adapted, anaerobically functioning electron-transport chain. An aerobic energy metabolism with Krebs cycle activity is accompanied by electron transfer from succinate to ubiquinone via complex II of the respiratory chain. On the other hand, in an anaerobic metabolism, where fumarate functions as terminal electron acceptor, electrons are transferred from rhodoquinone to fumarate, which is the reversed direction. Ubiquinone cannot replace rhodoquinone in the process of fumarate reduction in vivo, as ubiquinone can only accept electrons from complex II and cannot donate them to fumarate. Rhodoquinone, with its lower redox potential than ubiquinone, is capable of donating electrons to fumarate. Eukaryotic fumarate reductases were shown to interact with rhodoquinone (a benzoquinone), whereas most prokaryotic fumarate reductases interact with the naphtoquinones mena- quinone and demethylmenaquinone. Fumarate reductase, the enzyme essential for the anaerobic functioning of many eukaryotes, is structurally very similar to succinate dehydrogenase, the Krebs cycle enzyme catalysing the reverse reaction. In prokaryotes these enzymes are differentially expressed depending on the external conditions. -
Photosynthetic Phosphorylation Above and Below 00C by David 0
VOL. 48, 1962 BIOCHEMISTRY: HALL AND ARNON 833 10 De Robertis, E., J. Biophy8. Biochem. Cytol., 2, 319 (1956). 11 Eakin, R. M., and J. A. Westfall, ibid., 8, 483 (1960). 12 Eakin, R. M., these PROCEEDINGS, 47, 1084 (1961). 13 Wolken, J. J., in The Structure of the Eye, ed. G. K. Smelser (New York: Academic Press, 1961). 14 Wald, G., ibid. 16 Eakin, R. M., and J. A. Westfall, Embryologia, 6, 84 (1961). 16 Sj6strand, F. S., in The Structure of the Eye, ed. G. K. Smelser (New York: Academic Press, 1961). 17 Miller, W. H., in The Cell, ed. J. Brachet and A. E. Mirsky (New York: Academic Press, 1960), part IV. 18 Miller, W. H., J. Biophys. Biochem. Cytol., 4, 227 (1958). 19 Hesse, R., Z. wiss. Zool., 61, 393 (1896). 20 Bradke, D. L., personal communication. 21 Wolken, J. J., Ann. N. Y. Acad. Sci., 74, 164 (1958). 22 Rohlich, P., and L. J. Torok, Z. wiss. Zool., 54, 362 (1961). 28 Eakin, R. M., and J. A. Westfall, J. Ultrastr. Res. (in press). 24 Franz, V., Jena. Z. Naturwiss., 59, 401 (1923). PHOTOSYNTHETIC PHOSPHORYLATION ABOVE AND BELOW 00C BY DAVID 0. HALL* AND DANIEL I. ARNONt DEPARTMENT OF CELL PHYSIOLOGY, UNIVERSITY OF CALIFORNIA, BERKELEY Read before the Academy, April 25, 1962 CO2 assimilation in photosynthesis consists of a series of dark enzymatic reactions that are driven solely by adenosine triphosphate and reduced pyridine nucleotide. 1-4 The same reactions are now known to operate in nonphotosynthetic cells.5-"3 It follows, therefore, that the distinction between carbon assimilation in photosyn- thetic and nonphotosynthetic cells lies in the manner in which ATP14 and PNH214 are formed. -
Thermophilic Lithotrophy and Phototrophy in an Intertidal, Iron-Rich, Geothermal Spring 2 3 Lewis M
bioRxiv preprint doi: https://doi.org/10.1101/428698; this version posted September 27, 2018. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY-NC-ND 4.0 International license. 1 Thermophilic Lithotrophy and Phototrophy in an Intertidal, Iron-rich, Geothermal Spring 2 3 Lewis M. Ward1,2,3*, Airi Idei4, Mayuko Nakagawa2,5, Yuichiro Ueno2,5,6, Woodward W. 4 Fischer3, Shawn E. McGlynn2* 5 6 1. Department of Earth and Planetary Sciences, Harvard University, Cambridge, MA 02138 USA 7 2. Earth-Life Science Institute, Tokyo Institute of Technology, Meguro, Tokyo, 152-8550, Japan 8 3. Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 9 91125 USA 10 4. Department of Biological Sciences, Tokyo Metropolitan University, Hachioji, Tokyo 192-0397, 11 Japan 12 5. Department of Earth and Planetary Sciences, Tokyo Institute of Technology, Meguro, Tokyo, 13 152-8551, Japan 14 6. Department of Subsurface Geobiological Analysis and Research, Japan Agency for Marine-Earth 15 Science and Technology, Natsushima-cho, Yokosuka 237-0061, Japan 16 Correspondence: [email protected] or [email protected] 17 18 Abstract 19 Hydrothermal systems, including terrestrial hot springs, contain diverse and systematic 20 arrays of geochemical conditions that vary over short spatial scales due to progressive interaction 21 between the reducing hydrothermal fluids, the oxygenated atmosphere, and in some cases 22 seawater. At Jinata Onsen, on Shikinejima Island, Japan, an intertidal, anoxic, iron- and 23 hydrogen-rich hot spring mixes with the oxygenated atmosphere and sulfate-rich seawater over 24 short spatial scales, creating an enormous range of redox environments over a distance ~10 m. -
Chapter 3 the Title and Subtitle of This Chapter Convey a Dual Meaning
3.1. Introduction Chapter 3 The title and subtitle of this chapter convey a dual meaning. At first reading, the subtitle Photosynthetic Reaction might seem to indicate that the topic of the structure, function and organization of Centers: photosynthetic reaction centers is So little time, so much to do exceedingly complex and that there is simply insufficient time or space in this brief article to cover the details. While this is John H. Golbeck certainly the case, the subtitle is Department of Biochemistry additionally meant to convey the idea that there is precious little time after the and absorption of a photon to accomplish the Molecular Biology task of preserving the energy in the form of The Pennsylvania State University stable charge separation. University Park, PA 16802 USA The difficulty is there exists a fundamental physical limitation in the amount of time available so that a photochemically induced excited state can be utilized before the energy is invariably wasted. Indeed, the entire design philosophy of biological reaction centers is centered on overcoming this physical, rather than chemical or biological, limitation. In this chapter, I will outline the problem of conserving the free energy of light-induced charge separation by focusing on the following topics: 3.2. Definition of the problem: the need to stabilize a charge-separated state. 3.3. The bacterial reaction center: how the cofactors and proteins cope with this problem in a model system. 3.4. Review of Marcus theory: what governs the rate of electron transfer in proteins? 3.5. Photosystem II: a variation on a theme of the bacterial reaction center. -
Lecture 7 - the Calvin Cycle and the Pentose Phosphate Pathway
Lecture 7 - The Calvin Cycle and the Pentose Phosphate Pathway Chem 454: Regulatory Mechanisms in Biochemistry University of Wisconsin-Eau Claire 1 Introduction The Calvin cycle Text The dark reactions of photosynthesis in green plants Reduces carbon from CO2 to hexose (C6H12O6) Requires ATP for free energy and NADPH as a reducing agent. 2 2 Introduction NADH versus Text NADPH 3 3 Introduction The Pentose Phosphate Pathway Used in all organisms Glucose is oxidized and decarboxylated to produce reduced NADPH Used for the synthesis and degradation of pentoses Shares reactions with the Calvin cycle 4 4 1. The Calvin Cycle Source of carbon is CO2 Text Takes place in the stroma of the chloroplasts Comprises three stages Fixation of CO2 by ribulose 1,5-bisphosphate to form two 3-phosphoglycerate molecules Reduction of 3-phosphoglycerate to produce hexose sugars Regeneration of ribulose 1,5-bisphosphate 5 5 1. Calvin Cycle Three stages 6 6 1.1 Stage I: Fixation Incorporation of CO2 into 3-phosphoglycerate 7 7 1.1 Stage I: Fixation Rubisco: Ribulose 1,5- bisphosphate carboxylase/ oxygenase 8 8 1.1 Stage I: Fixation Active site contains a divalent metal ion 9 9 1.2 Rubisco Oxygenase Activity Rubisco also catalyzes a wasteful oxygenase reaction: 10 10 1.3 State II: Formation of Hexoses Reactions similar to those of gluconeogenesis But they take place in the chloroplasts And use NADPH instead of NADH 11 11 1.3 State III: Regeneration of Ribulose 1,5-Bisphosphosphate Involves a sequence of transketolase and aldolase reactions. 12 12 1.3 State III: -
Biol 1020: Photosynthesis
Chapter 10: Photosynthesis Energy and Carbon Sources Electromagnetic Spectrum and Light Chloroplasts Photosynthesis Overview Light Reactions C3 Cycle Photorespiration Supplemental Carbon Fixation: C4 and CAM pathways . • List and differentiate the 4 possible groups of organisms based on how they obtain energy and useful carbon. Classification by Energy and Carbon Sources energy source chemotrophs can only get energy directly from chemical compounds phototrophs can get energy directly from light (these organisms can use chemical compounds as energy sources as well) . Classification by Energy and Carbon Sources carbon source autotrophs can fix carbon dioxide, thus they can use CO2 as a carbon source heterotrophs cannot fix CO2; they use organic molecules from other organisms as a carbon source . Classification by Energy and Carbon Sources combined, these leads to 4 possible groups: photoautotrophs – carry out photosynthesis use light energy to fix CO2 store energy in chemical bonds of organic molecules includes green plants, algae, and some bacteria photoheterotrophs – use light energy but cannot fix CO2; some nonsulfur purple bacteria chemoautotrophs – obtain energy from reduced inorganic molecules and use some of it to fix CO2; some bacteria chemoheterotrophs – use organic molecules as both carbon and energy sources dependent completely on other organisms for energy capture and carbon fixation includes all animals, all fungi, most protists, and most bacteria . • List and differentiate the 4 possible groups of -
Do Leaves Need Chlorophyll for Growth?
Do Leaves Need Chlorophyll for Growth? by Kranti Patil, Gurinder Singh and Karen Haydock Homi Bhabha Centre for Science Education VN Purav Marg, Mankhurd Mumbai 400088 India [email protected] Students may read or hear the following sorts of statements in their classrooms: Plants make their food by photosynthesis. Leaves are green because they contain green pigment (chlorophyll). Without chlorophyll photosynthesis cannot occur. If we assume these statements are true, then what do we think if we see a white leaf? We may assume that a white leaf does not contain chlorophyll, and that therefore it cannot make food. So then ... How does a white leaf survive? Students may raise this question when they see a plant such as this variegated variety of bhendi (Talipariti tiliaceum), an ornamental shrub which has some green leaves, some leaves with asymmetric green and white areas, and some leaves which are completely white. A variegated bhendi (Talipariti tiliaceum) shrub - about 2.5 metres high. 1 An activity which is sometimes done in school in order “to prove that chlorophyll is required for photosynthesis” is to take a variegated leaf, remove its green pigment by dissolving it in alcohol, and then show that only the areas which were formerly green test positive for starch. However, this is a rather tedious procedure, and it actually does not prove that chlorophyll is required for photosynthesis, or even that photosynthesis is occurring. It merely indicates that only the green areas contain starch. It may even lead students to ask a question like, “Then why does a potato - which is not green - also contain starch?” Is the potato also doing photosynthesis? We can question whether starch is an indicator of photosynthesis. -
The Summary Equation of Cellular Respiration. the Difference Between
The summary equation of cellular respiration. The difference between fermentation and cellular respiration. The role of glycolysis in oxidizing glucose to two molecules of pyruvate. The process that brings pyruvate from the cytosol into the mitochondria and introduces it into the citric acid cycle. How the process of chemiosmosis utilizes the electrons from NADH and FADH2 to produce ATP. E flows into ecosystem as Sunlight Autotrophs transform it into chemical E O2 released as byproduct Cells use some of chemical E in organic molecules to make ATP E leaves as heat Catabolic Pathway Complex organic Simpler waste molecules products with less E Some E used to do work and dissipated as heat Introduction Respiration (15 min) Respiration: exergonic (releases E) C6H12O6 + 6O2 6H2O + 6CO2 + ATP (+ heat) Fermentation exergonic (releases E) C6H12O6 2-3 C products + ATP (small amounts) Photosynthesis: endergonic (requires E) 6H2O + 6CO2 + Light C6H12O6 + 6O2 oxidation (donor) lose e- Xe- + Y X + Ye- reduction (acceptor) gain e- Oxidation = lose e- OiLRiG or LeoGer Reduction = gain e- oxidation C6H12O6 + 6O2 6H2O + 6CO2 + ATP reduction Energy is released as electrons “fall” from organic molecules to O2 Broken down into steps: Food (Glucose) NADH ETC O2 . Coenzyme NAD+ = electron acceptor . NAD+ picks up 2e- and 2H+ NADH (stores E) . NADH carries electrons to the electron transport chain (ETC) - . ETC: transfers e to O2 to make H2O ; releases energy Generate small amount of ATP Phosphorylation: enzyme transfers a phosphate to other