Plant Respiration Under Low Oxygen
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Comparing Aerobic Vs. Anaerobic Respiration
Comparing Aerobic vs. Anaerobic Respiration Objective: Students will compare the two types of cellular respiration: aerobic respiration and anaerobic respiration (fermentation). Students will note similarities and differences between the two processes including when, where, and how each process occurs. Students will develop a concept map using Inspiration indicating the criteria for aerobic and anaerobic respiration. This concept map will indicate: Three similarities between the two processes. Two types of cells that perform each process. Location in the cell where each process occurs. Oxygen requirements for each process. Reactants and products for each process. Energy output for each process. Two different types of anaerobic respiration. Reactants and products for each. Types of cells that perform each process. Introduction: This activity will follow a fermentation (anaerobic respiration) lab using yeast. This lab will address the process of alcoholic fermentation. Students will perform push-ups to experience lactic acid build-up in muscle cells. These activities will gain interest in the process of anaerobic respiration. Students will have already studied the detailed process of aerobic cellular respiration. Procedure: Students will work in pairs or trios to answer questions (as seen in benchmarks) on aerobic and anaerobic respiration. Students will use previous notes and lab activities to summarize main ideas for aerobic and anaerobic respiration. Individually, students will create a concept map using Inspiration to further integrate and separate the two processes. Accommodations: Instructions will be provided in written format as well as read orally. Instructions will also be on an overhead. One example will be provided for students on how to summarize data. -
Glycolysis/Embden-Meyerhof-Parnas Pathway (EMP Pathway)
Reaspiration iving cells require a continuous supply of energy for maintaining various life activities. This energy is obtained by oxidizing the organic compounds (carbohydrates, proteins, and lipids) Lin the cells. This process of harvesting chemical energy for metabolic activities in the form of ATP by oxidising the food molecules is called ‘respiration’. The most common substrate used in respiration for oxidation is glucose. Factor affecting the respiration (1) Oxygen Content of the Atmosphere: The percentage of oxygen in the surrounding atmosphere greatly influence the rate of respiration. But reduction of the oxygen content of the air, however, causes no significant lowering in the respiratory rate until the percentage drops to about 10%. With the increase of oxygen concentration in the atmosphere, the rate of respiration also increases, but this effect is not as accelerating as might be expected. In certain plants, like rice, on removal of oxygen the rate of respiration in terms of total carbon dioxide produced actually increases. This indicates that anaerobic respiration comes into action when oxygen is no longer available and that the plant, if it has to make up for the relative inefficiency of this system, has to respire faster. (2) Effect of Temperature: Like most chemical reactions, the rate of respiration is greatly influenced by temperature. If the rise is at a much higher starting temperature, say between 20° and 30°C, then the Q 10 may fall below 2. In certain cases the rate of respiration increases at lower temperature. increase in the rate of respiration is primarily due to increase in the quantity of respirable materials (such as soluble carbohydrates) which tend to accumulate in Irish potato at temperature slightly above 0°C. -
Acclimation of Photosynthesis and Respiration to Elevated Atmospheric CO2 in Two Scrub Oaks
Global Change Biology (2002) 8, 317±328 Acclimation of photosynthesis and respiration to elevated atmospheric CO2 in two Scrub Oaks GRAHAM J. HYMUS, TOM G. SNEAD, DAVID P. JOHNSON, BRUCE A. HUNGATE* and BERT G.DRAKE Smithsonian Environmental Research Center, Mailcode DYN-2, Kennedy Space Center, FL 32899, USA, *Department of Biological Sciences and Merriam-Powell Center for Environmental Research, Box 5640, Northern Arizona University, Flagstaff, AZ 86011- 5640, USA Abstract For two species of oak, we determined whether increasing atmospheric CO2 concen- tration (Ca)would decrease leaf mitochondrial respiration (R)directly, or indirectly owing to their growth in elevated Ca , or both. In particular, we tested whether acclima- tory decreases in leaf-Rubisco content in elevated Ca would decrease R associated with its maintenance. This hypothesis was tested in summer 2000 on sun and shade leaves of Quercus myrtifolia Willd. and Quercus geminata Small. We also measured R on five occasions between summer 1999 and 2000 on leaves of Q. myrtifolia. The oaks were grown in the field for 4 years, in either current ambient or elevated (current À1 ambient 350 mmol mol ) Ca , in open-top chambers (OTCs). For Q. myrtifolia,an À1 increase in Ca from 360 to 710 mmol mol had no direct effect on R at any time during the year. In April 1999, R in young Q. myrtifolia leaves was significantly higher in elevated CaÐthe only evidence for an indirect effect of growth in elevated Ca. Leaf R was significantly correlated with leaf nitrogen (N)concentration for the sun and shade leaves of both the species of oak. -
Exchange Velocity Approach and Obt Formation in Plants During the Daytime
EXCHANGE VELOCITY APPROACH AND OBT FORMATION IN PLANTS DURING THE DAYTIME Anca Melintescu PhD “Horia Hulubei” National Institute of Physics and Nuclear Engineering, Bucharest - Magurele, ROMANIA [email protected], [email protected] Third Technical Meeting of the EMRAS II, Working Group 7, “Tritium” Accidents, Vienna, Austria, 24 - 28 January 2011 THE DRIVING EQUATIONS FOR TRITIUM TRANSFER IN ATMOSPHERE - SOIL- PLANT CONTINUUM Driving equation for the HTO transfer from atmosphere to leaves: C – HTO concentration in plant water (Bq/kg); 3 depends on canopy resistance Cair – HTO concentration in air (Bq/m ); Cs - HTO concentration in the sap water (Bq/kg); 3 s - saturated air humidity at vegetation temp. (kg/m ); dC Vexc Vexc - air humidity at reference level (kg/m3); 2 (Cair 0.91 sC) (s )Cs Mw – water mass in plant on a unit soil surface (kg/m ); dt M w M w Vexc – exchange velocity from atmosphere to canopy (m/s) the transpiration flux - used for all canopy, ignoring the transfer of air HTO to steam, because the exchange velocity is smaller with one order of magnitude; - Ignores the initial diffusion of leaf water to steams The tritium dynamics at soil surface: depends on soil resistance dCsw,1 Vex,s C - HTO concentration in the first soil layer at the (Bq/kg); (Cair 0.91sat (Ts )Csw,1 ) DF sw,1 Vex,s - exchange velocity from atmosphere to soil (m/s); dt M 3 ws sat(Ts) - saturated air humidity at soil surface temp. (kg/m ); Mws – water mass in the surface soil layer; DF - HTO net flux at the bottom interface of the first soil -
Detailed Temporal Modelling of Carbon and Water Fluxes from Pastures in New Zealand
Copyright is owned by the Author of the thesis. Permission is given for a copy to be downloaded by an individual for the purpose of research and private study only. The thesis may not be reproduced elsewhere without the permission of the Author. Detailed temporal modelling of carbon and water fluxes from pastures in New Zealand: Case study of an experimental dairy farm in the Waikato region A thesis presented in partial fulfilment of the Requirements for the degree of Doctor of Philosophy In Soil Science Massey University, Palmerston North, New Zealand Nicolas Puche 2017 i ii ABSTRACT The terrestrial biosphere is an important pool of carbon, with its size governed by the opposing processes of CO2 uptake through photosynthesis and release through respiration. It is therefore critically important to understand and reliably and accurately model these processes and predict changes in carbon exchange in response to key drivers. Pasture-based livestock production is particularly important for the New Zealand’s economy but it is also a main contributor to NZ’s greenhouse gas budget. My Ph.D. work used half-hourly eddy-covariance (EC) data, previously collected over 2 consecutive years from a grazed pasture in the Waikato region. The main aims of this study were to assess whether there was any bias in gap-filled eddy covariance measurements, to assess whether incomplete capture of cow respiration during grazing events could have led to biased observations, and to quantify the resulting difference on the net carbon budget of the farm. I approached the work by developing a new process-based model, CenW_HH, running at a half-hourly time step, to predict the energy and CO2 exchange of grazed pastures. -
Acute Stimulation of White Adipocyte Respiration by PKA-Induced Lipolysis Einav Yehuda-Shnaidman,1 Ben Buehrer,2 Jingbo Pi,1 Naresh Kumar,3 and Sheila Collins1,4
ORIGINAL ARTICLE Acute Stimulation of White Adipocyte Respiration by PKA-Induced Lipolysis Einav Yehuda-Shnaidman,1 Ben Buehrer,2 Jingbo Pi,1 Naresh Kumar,3 and Sheila Collins1,4 OBJECTIVE—We examined the effect of -adrenergic receptor BAT and WAT is different. Brown adipocytes possess a (AR) activation and cAMP-elevating agents on respiration and rich complement of mitochondria and are the only cell mitochondrial uncoupling in human adipocytes and probed the type to express uncoupling protein (UCP1). After cate- underlying molecular mechanisms. cholamine stimulation of the -adrenergic receptors  RESEARCH DESIGN AND METHODS—Oxygen consumption ( ARs), UCP1 activation (by the released FAs) increases rate (OCR, aerobic respiration) and extracellular acidification the proton conductance of the inner mitochondrial mem- rate (ECAR, anaerobic respiration) were examined in response brane (IMM) and dissipates the electrochemical proton to isoproterenol (ISO), forskolin (FSK), and dibutyryl-cAMP gradient that is the driving force for ATP synthesis in a (DB), coupled with measurements of mitochondrial depolariza- process termed “mitochondrial uncoupling” (rev. in 1,2). tion, lipolysis, kinase activities, and gene targeting or knock- Catecholamine stimulation also increases Ucp1 gene ex- down approaches. pression and mitochondrial mass, altogether resulting in RESULTS—ISO, FSK, or DB rapidly increased oxidative and robust oxidation of FAs for heat production and energy glycolytic respiration together with mitochondrial depolarization expenditure. White adipocytes have fewer mitochondria in human and mouse white adipocytes. The increase in OCR was and negligible amounts of UCP1. Upon AR stimulation of oligomycin-insensitive and contingent on cAMP-dependent pro- WAT, FAs liberated by lipolysis are mostly released into tein kinase A (PKA)-induced lipolysis. -
Anaerobic Respiration - Fermentation
Anaerobic Respiration - Fermentation ! "Be ready to discuss •" Why do we need oxygen? Anaerobic Respiration - Fermentation KEY CONCEPT Fermentation allows the production of a small amount of ATP without oxygen. Anaerobic Respiration - Fermentation •" If no oxygen is available, cells can obtain energy through the process of anaerobic respiration. •" A common anaerobic process is fermentation. •" Fermentation is not an efficient process and results in the formation of far fewer ATP molecules than aerobic respiration. There are two primary fermentation processes: 1." Lactic Acid Fermentation 2." Alcohol Fermentation Anaerobic Respiration - Fermentation Lactic acid fermentation occurs when oxygen is not available. For example, in muscle tissues during rapid and vigorous exercise, muscle cells may be depleted of oxygen. They then switch from respiration to fermentation. Anaerobic Respiration - Fermentation The pyruvic acid formed during glycolysis is broken down to lactic acid and energy is released (which is used to form ATP). Glucose → Pyruvic acid → Lactic acid + energy Anaerobic Respiration - Fermentation •"The process of lactic acid fermentation replaces the process of aerobic respiration so that the cell can have a continual source of energy, even in the absence of oxygen. •"However this shift is only temporary and cells need oxygen for sustained activity. Anaerobic Respiration - Fermentation •"Lactic acid that builds up in the tissue causes a burning, painful sensation. Anaerobic Respiration - Fermentation Alcohol fermentation occurs in yeasts and some bacteria. Pyruvic acid formed during glycolysis is broken down to produce alcohol and carbon dioxide and is released (which is used to form ATP). Anaerobic Respiration - Fermentation Glucose → Pyruvic acid → alcohol + carbon dioxide + energy Anaerobic Respiration - Fermentation •" Fermentation is used in food production. -
Thermal Acclimation of Leaf and Root Respiration: an Investigation Comparing Inherently Fast- and Slow- Growing Plant Species
Global Change Biology (2003) 9, 895±910 Thermal acclimation of leaf and root respiration: an investigation comparing inherently fast- and slow- growing plant species B. R. LOVEYS1 ,L. J. ATKINSON,D. J. SHERLOCK,R. L. ROBERTS,A. H. FITTER and O. K. ATKIN Department of Biology, The University of York, PO Box 373, York, YO10 5YWUK Abstract We investigated the extent to which leaf and root respiration (R) differ in their response to short- and long-term changes in temperature in several contrasting plant species (herbs, grasses, shrubs and trees) that differ in inherent relative growth rate (RGR, increase in mass per unit starting mass and time). Two experiments were conducted using hydroponically grown plants. In the long-term (LT) acclimation experiment, 16 species were grown at constant 18, 23 and 28 ÊC. In the short-term (ST) acclimation experi- ment, 9 of those species were grown at 25/20 ÊC (day/night) and then shifted to a 15/10 ÊC for 7 days. Short-term Q10 values (proportional change in R per 10 ÊC) and the degree of acclimation to longer-term changes in temperature were compared. The effect of growth temperature on root and leaf soluble sugar and nitrogen concentrations was examined. Light-saturated photosynthesis (Asat) was also measured in the LT acclimation experi- ment. Our results show that Q10 values and the degree of acclimation are highly variable amongst species and that roots exhibit lower Q10 values than leaves over the 15±25 ÊC measurement temperature range. Differences in RGR or concentrations of soluble sugars/nitrogen could not account for the inter-specific differences in the Q10 or degree of acclimation. -
GROWTH and MAINTENANCE RESPIRATION of PERENNIAL ROOT SYSTEMS in a DRY GRASSLAND DOMINATED by AGROPYRON DASYSTACHYUM (Yiooll,) SCRIBN
New Phytol (1987) 105, 595-603 595 GROWTH AND MAINTENANCE RESPIRATION OF PERENNIAL ROOT SYSTEMS IN A DRY GRASSLAND DOMINATED BY AGROPYRON DASYSTACHYUM (YiOOlL,) SCRIBN. BY E. G. REEKIE AND R. E. REDMANN Department of Crop Science and Plant Ecology, University of Saskatchewan, Saskatoon, Saskatchewan S7N OWO, Canada {Accepted 17 November 1986) SUMMARY Respiration coefficients were determined for laboratory-grown root systems of Agropyron dasystachyum (Hook.) Scribn. (northern wheatgrass). The growth respiration coefficient (0-85 g g~^) was similar to published rates for species from mesic sites. The maintenance coefficient (0-037 g g"^ d~i) was relatively low, suggesting that plants growing in semi-arid habitats have inherently low maintenance costs per unit of biomass. The proportion of total root biomass requiring maintenance (degradable fraction) was determined by measuring the non- structural root biomass. The degradable fraction (0-13) was substantially lower than published measurements of functional (or 'live') biomass, because the latter include structural biomass, which has no maintenance requirement. Respiration parameters, root growth, degradable root fraction, soil temperature and soil moisture were used to construct a model of root respiration in field-grown roots. The maintenance coefficient was adjusted downward during periods of water stress and low temperature when roots probably were dormant. Parameters in the model, particularly the degradable biomass fraction, explained much of the discrepancy between respiration rates of laboratory-grown and field-grown root systems. Maintenance respiration represents a substantial outlay in the carbon budgets of dry grasslands but is lower than expected considering the large root biomass in these systems. Key words: Agropyron dasystachyum (Hook.) Scribn., carbon budget, grassland ecosystem, growth and maintenance respiration, roots. -
Substrate Utilization and Respiration in Relation to Growth and Maintenance Inhighe R Plants
«}] substrate utilization and respiration in relation to growth and maintenance inhighe r plants F.W.T. PENNING DE VRIES N08201.571 substrate utilization and respiration in relation to growth and maintenance inhighe r plants F.W.T. PENNING DE VRIES SUBSTRATEUTILIZATIO NAN DRESPIRATIO N INRELATIO N TOGROWT HAN DMAINTENANC E INHIGHE RPLANT S F.W.T.Pennin gd eVrie s PROEFSCHRIFT TERVERKRIJGIN GVA ND EGRAA D VANDOCTO RI ND ELANDBOUWWETENSCHAPPEN , OPGEZA GVA ND ERECTO RMAGNIFICUS , PROF.DR.IR.H.A . LENIGER, INHE TOPENBAA RT EVERDEDIGE NO P VRIJDAG 21DECEMBE R 1973DE SNAMIDDAG SO MVIE RUU R IND EAUL AVA ND ELANDBOUWHOGESCHOO LT EWAGENINGE N STbLUNJiJt - I - leerboeken iter plantenfyaiologie beaehrijven p.cvoonlijk bet begrip "fotoajmthete" te eng alt tie venting van koolhydraten uit kooleuur en water ottder invioed van lichl. liet ia beter "fatoeynlheae" ce defi- nieren *U de too van alle ayntheaeproceaeen die onder onvloed van lichc in de groene plant gebeuren, en dan de verachillende onderdeien, te weten de reductieve koolcuuraaaiedlatie, de nitraatreductie en bijbehorende proceaaen, en de ayrtthese van diverae polyeeren, afsoo- derlijk aan te duiden. (dit proefschrift) - 2 - Bijbe t bestuderen van adesrtalinp,va n planten behoort invee l grolerc •ate dan tot nu toe §c«vo«m ia,nadru k tewordc n geleed ophaa r func- tionele karakter. (dit prf^eCachrIft ) - %- De anelheid van haterotrofc groel van een plant of orgaan Van eenvou- dig en noo deatructiaf worden afgeteid uit stttingen van de adrchalinpa- snelheid. (dit proc(achrift) - 4 - Met isnie t aogelijk raasetiva n de belangrijkste landbouwgewaaaen te kveken die hun aasiailaten efficienter benutten voorbioaynthea e dan dehuidig e rassen.He t iawe l xinvol te zoeken naar planten die lagere onderhoudakoetenhebbe n dan debeataand e planten,o f te proberen een verlaplng van dexe kosten tebewerkstelligen . -
Ocean Life, Bioenergetics and Metabolism
Ocean life, bioenergetics and metabolism Biological Oceanography (OCN 621) Matthew Church (MSB 612) Ecosystems are hierarchically organized • Atoms → Molecules → Cells → Organisms→ Populations→ Communities • This organizational system dictates the pathways that energy and material travel through a system. • Cells are the lowest level of structure capable of performing ALL the functions of life. Classification of life Two primary cellular forms • Prokaryotes: lack internal membrane-bound organelles. Genetic information is not separated from other cell functions. Bacteria and Archaea are prokaryotes. Note however this does not imply these divisions of life are closely related. • Eukaryotes: membrane-bound organelles (nucleus, mitochrondrion, etc .). Compartmentalization (organization) of different cellular functions allows sequential intracellular activities In the ocean, microscopic organisms account for >50% of the living biomass. Controls on types of organisms, abundances, distributions • Habitat: The physical/chemical setting or characteristics of a particular environment, e.g., light vs. dark, cold vs. warm, high vs. low pressure • Each marine habitat supports a somewhat predictable assemblage of organisms that collectively make up the community, e.g., rocky intertidal community, coral reef community, abyssobenthic community • The structure and function of the individuals/populations in these communities arise from evolution and selective adaptations in response to the habitat characteristics • Niche: The role of a particular organism in an integrated community •The ocean is not homogenous: spatial and temporal variability in habitats Clearly distinguishable ocean habitats with elevated “plant” biomass in regions where nutrients are elevated The ocean is stirred more than mixed Sea Surface Temperature Chl a (°C) (mg m-3) Spatial discontinuities at various scales (basin, mesoscale, microscale) in ocean habitats play important roles in controlling plankton growth and distributions. -
Understanding the Role of Anaerobic Respiration in Burkholderia Thailandensis and B
1 Understanding the role of anaerobic respiration in Burkholderia thailandensis and B. pseudomallei survival and virulence Submitted by Clio Alexandra Martin Andreae to the University of Exeter as a thesis for the degree of Doctor of Philosophy in Biological Science May 2014 This thesis is available for Library use on the understanding that it is copyright material and that no quotation from the thesis may be published without proper acknowledgement. I certify that all material in this thesis which is not my own work has been identified and that no material has previously been submitted and approved for the award of a degree by this or any other University. Signature………………………………………………………………………………… 2 Abstract Burkholderia pseudomallei is the causative agent of melioidosis, a disease endemic in Northern Australia and Southeast Asia. Melioidosis can present with acute, chronic and latent infections and can relapse several months or years after initial presentation. Currently not much is known about the ways in which B. pseudomallei can persist within the host, although it has been speculated that the ability to survive within an anaerobic environment will play some role. B. pseudomallei is able to survive anaerobically for extended periods of time but little is known about the molecular basis of anaerobic respiration in this pathogenic species. Bioinformatic analysis was used to determine the respiratory flexibility of both B. pseudomallei and B. thailandensis, identifying multiple genes required for aerobic and anaerobic respiration, and molybdopterin biosynthesis. Using B. thailandensis as a model organism a transposon mutant library was created in order to identify genes required for anaerobic respiration.