Interactions Between Photosynthesis and Respiration in an Aquatic Ecosystem
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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). -
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 The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity.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. -
Analysis of Habitat Fragmentation and Ecosystem Connectivity Within the Castle Parks, Alberta, Canada by Breanna Beaver Submit
Analysis of Habitat Fragmentation and Ecosystem Connectivity within The Castle Parks, Alberta, Canada by Breanna Beaver Submitted in Partial Fulfillment of the Requirements for the Degree of Master of Science in the Environmental Science Program YOUNGSTOWN STATE UNIVERSITY December, 2017 Analysis of Habitat Fragmentation and Ecosystem Connectivity within The Castle Parks, Alberta, Canada Breanna Beaver I hereby release this thesis to the public. I understand that this thesis will be made available from the OhioLINK ETD Center and the Maag Library Circulation Desk for public access. I also authorize the University or other individuals to make copies of this thesis as needed for scholarly research. Signature: Breanna Beaver, Student Date Approvals: Dawna Cerney, Thesis Advisor Date Peter Kimosop, Committee Member Date Felicia Armstrong, Committee Member Date Clayton Whitesides, Committee Member Date Dr. Salvatore A. Sanders, Dean of Graduate Studies Date Abstract Habitat fragmentation is an important subject of research needed by park management planners, particularly for conservation management. The Castle Parks, in southwest Alberta, Canada, exhibit extensive habitat fragmentation from recreational and resource use activities. Umbrella and keystone species within The Castle Parks include grizzly bears, wolverines, cougars, and elk which are important animals used for conservation agendas to help protect the matrix of the ecosystem. This study identified and analyzed the nature of habitat fragmentation within The Castle Parks for these species, and has identified geographic areas of habitat fragmentation concern. This was accomplished using remote sensing, ArcGIS, and statistical analyses, to develop models of fragmentation for ecosystem cover type and Digital Elevation Models of slope, which acted as proxies for species habitat suitability. -
Ecological Systems of the United States a Working Classification of U.S
ECOLOGICAL SYSTEMS OF THE UNITED STATES A WORKING CLASSIFICATION OF U.S. TERRESTRIAL SYSTEMS NatureServe is a non-profit organization dedicated to providing the scientific knowledge that forms the basis for effective conservation action. Citation: Comer, P., D. Faber-Langendoen, R. Evans, S. Gawler, C. Josse, G. Kittel, S. Menard, M. Pyne, M. Reid, K. Schulz, K. Snow, and J. Teague. 2003. Ecological Systems of the United States: A Working Classification of U.S. Terrestrial Systems. NatureServe, Arlington, Virginia. © NatureServe 2003 Ecological Systems of the United States is a component of NatureServe’s International Terrestrial Ecological Systems Classification. Á Funding for this report was provided by a grant from The Nature Conservancy. Front cover: Maroon Bells Wilderness, Colorado. Photo © Patrick Comer NatureServe 1101 Wilson Boulevard, 15th Floor Arlington, VA 22209 (703) 908-1800 www.natureserve.org ECOLOGICAL SYSTEMS OF THE UNITED STATES A WORKING CLASSIFICATION OF U.S. TERRESTRIAL SYSTEMS Á Á Á Á Á Patrick Comer Don Faber-Langendoen Rob Evans Sue Gawler Carmen Josse Gwen Kittel Shannon Menard Milo Pyne Marion Reid Keith Schulz Kristin Snow Judy Teague June 2003 Acknowledgements We wish to acknowledge the generous support provided by The Nature Conservancy for this effort to classify and characterize the ecological systems of the United States. We are particularly grateful to the late John Sawhill, past President of The Nature Conservancy, who was an early supporter of this concept, and who made this funding possible through an allocation from the President’s Discretionary Fund. Many of the concepts and approaches for defining and applying ecological systems have greatly benefited from collaborations with Conservancy staff, and the classification has been refined during its application in Conservancy-sponsored conservation assessments. -
Photosynthesis and Respiration
HIGH SCHOOL LIFE SCIENCE: PHOTOSYNTHESIS AND RESPIRATION Standards Bundle Standards are listed within the bundle. Bundles are created with potential instructional use in mind, based upon potential for related phenomena that can be used throughout a unit. HS-LS1-5 Use a model to illustrate how photosynthesis transforms light energy into stored chemical energy. (SEP: 2; DCI: LS1.C; CCC: Systems, Energy/Matter) [Clarification Statement: Emphasis is on illustrating inputs and outputs of matter and the transfer and transformation of energy in photosynthesis by plants and other photosynthesizing organisms. Examples of models could include diagrams, chemical equations, and conceptual models.] [Assessment Boundary: Assessment does not include specific biochemical steps.] HS-LS1-7 Use a model of the major inputs and outputs of cellular respiration (aerobic and anaerobic) to exemplify the chemical process in which the bonds of food molecules are broken, the bonds of new compounds are formed, and a net transfer of energy results. (SEP: 2; DCI: LS1.C; CCC: Energy/Matter)[Clarification Statement: Emphasis is on the conceptual understanding of the inputs and outputs of the process of cellular respiration.] [Assessment Boundary: Assessment should not include identification of the steps or specific processes involved in cellular respiration.] HS-LS2-5 Develop a model to illustrate the role of photosynthesis and cellular respiration in the cycling of carbon among the biosphere, atmosphere, hydrosphere, and geosphere. (SEP: 2; DCI: LS2.B, PS3.D; CCC: Systems) [Clarification Statement: Examples of models could include simulations and mathematical models.] [Assessment Boundary: Assessment does not include the specific chemical steps of photosynthesis and respiration.] Content Overview This section provides a generic overview of the content or disciplinary core ideas as an entry point to the standards. -
Biodiversity Implications Is Biogeography: For
FEATURE BIODIVERSITY IS BIOGEOGRAPHY: IMPLICATIONS FOR CONSERVATION By G. Carleton Ray THREE THEMES DOMINATEthis review. The first is similarities, as is apparent within the coastal zone, that biodiversity is biogeography. Or, as Nelson the biodiversity of which depends on land-sea in- and Ladiges (1990) put it: "Indeed, what beyond teractions. biogeography is "biodiversity' about?" Second, "Characteristic Biodiversity"--a Static View watershed and seashed patterns and their scale-re- A complete species inventory for any biogeo- lated dynamics are major modifiers of biogeo- graphic province on Earth is virtually impossible. graphic pattern. And, third, concepts of biodiver- In fact, species lists, absent a biogeographic frame sity and biogeography are essential guides for of reference, can be ecologically meaningless, be- conservation and management of coastal-marine cause such lists say little about the dynamics of systems, especially for MACPAs (MArine and environmental change. To address such dynamics, Coastal Protected Areas). biodiversity is best expressed at a hierarchy of Conservation and conservation bioecology have scales, which this discussion follows. entered into an era of self-awareness of their suc- cesses. Proponents of "biodiversity" have achieved Global Patterns worldwide recognition. Nevertheless: "Like so Hayden el al. (1984) attempted a summary of the many buzz words, biodiversity has many shades of state-of-the-art of global, coastal-marine biogeogra- • . the coastal zone, meaning and is often used to express vague and phy at the behest of UNESCO's Man and the Bios- which is the most bio- ill-thought-out concepts" (Angel, 1991), as phere Programme (MAB) and the International reflected by various biodiversity "strategies" Union for the Conservation of Nature (IUCN). -
Forest Production Ecology • Objectives – Overview of Forest Production Ecology • C Cycling – Primary Productivity of Trees and Forest Ecosystems
Forest Production Ecology • Objectives – Overview of forest production ecology • C cycling – Primary productivity of trees and forest ecosystems … ecologists and ecosystem managers are unlikely to achieve desired management objectives unless they are familiar with the distribution and movements of energy that are responsible for the character and productivity of ecosystems under their management. (Kimmins 2004) – First: questions, take-home points, things you learned, etc. from reading assignment 1 Forest Production Ecology • Why should you care about C cycling? – C is the energy currency of all ecosystems • Plant (autotrophic) production is the base of almost all food/energy pyramids • Underlies all ecosystem goods & services – Plant C cycling, to a large extent, controls atmospheric CO2 concentrations (i.e., climate) • 3-4x as much C in terrestrial ecosystems as the atmosphere • Forests account for ~80% of global plant biomass and ~50% of global terrestrial productivity – C is fundamental to soil processes (i.e., SOM) • Belowground resources are a primary control over all ecosystem processes 2 Forest Production Ecology •Global Carbon Cycle ≈ “Breathing” of Earth 3 Forest Production Ecology • C enters via photosynthesis The C Bank Account 1. Gross Primary Production (GPP) •Total C input via photosynthesis 2. Accumulates in ecosystems (C pools/storage) as: (a) plant biomass; (b) SOM & microbial biomass; or (c) animal biomass 3. Returned to the atmosphere via: (a) respiration (R; auto- or hetero-trophic); (b) VOC emissions; or (c) disturbance Chapin et al. (2011) 4. Leached from or transferred laterally to another ecosystem Forest Production Ecology • Keys to understanding biological C cycling 1. Pools (storage) vs. fluxes (flows) of C • Live and dead (detrital) biomass • Above- and belowground 2. -
Microbial Lithification in Marine Stromatolites and Hypersaline Mats
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by RERO DOC Digital Library Published in Trends in Microbiology 13,9 : 429-438, 2005, 1 which should be used for any reference to this work Microbial lithification in marine stromatolites and hypersaline mats Christophe Dupraz1 and Pieter T. Visscher2 1Institut de Ge´ ologie, Universite´ de Neuchaˆ tel, Rue Emile-Argand 11, CP 2, CH-2007 Neuchaˆ tel, Switzerland 2Center for Integrative Geosciences, Department of Marine Sciences, University of Connecticut, 1080 Shennecossett Road, Groton, Connecticut, 06340, USA Lithification in microbial ecosystems occurs when pre- crucial role in regulating sedimentation and global bio- cipitation of minerals outweighs dissolution. Although geochemical cycles. the formation of various minerals can result from After the decline of stromatolites in the late Proterozoic microbial metabolism, carbonate precipitation is pos- (ca. 543 million years before present), microbially induced sibly the most important process that impacts global and/or controlled precipitation continued throughout the carbon cycling. Recent investigations have produced geological record as an active and essential player in most models for stromatolite formation in open marine aquatic ecosystems [9,10]. Although less abundant than in environments and lithification in shallow hypersaline the Precambrian, microbial precipitation is observed in a lakes, which could be highly relevant for interpreting the multitude of semi-confined (physically or chemically) -
Chloroplasts Are the Food Producers of the Cell. the Organelles Are Only Found in Plant Cells and Some Protists Such As Algae
Name: ___________________________ Cell #2 H.W. due September 22nd, 2016 Period: _________ Chloroplasts are the food producers of the cell. The organelles are only found in plant cells and some protists such as algae. Animal cells do not have chloroplasts. Chloroplasts work to convert light energy of the Sun into sugars that can be used by cells. It is like a solar panel that changes sunlight energy into electric energy. The entire process is called photosynthesis and it all depends on the little green chlorophyll molecules in each chloroplast. In the process of photosynthesis, plants create sugars and release oxygen (O2). The oxygen released by the chloroplasts is the same oxygen you breathe every day. Chloroplasts are found in plant cells, but not in animal cells. The purpose of the chloroplast is to make sugars that feed the cell’s machinery. Photosynthesis is the process of a plant taking energy from the Sun and creating sugars. When the energy from the Sun hits a chloroplast and the chlorophyll molecules, light energy is converted into the chemical energy. Plants use water, carbon dioxide, and sunlight to make sugar and oxygen. During photosynthesis radiant energy or solar energy or light energy is transferred into chemical energy in the form of sugar (glucose). You already know that during photosynthesis plants make their own food. The food that the plant makes is in the form of sugar that is used to provide energy for the plant. The extra sugar that the plant does not use is stored as starch for later use. Mitochondria are known as the powerhouses of the cell. -
Chemical Energy And
Unit 6: Energy! From Food to Forces Chemical Energy and LESSON 1 LESSON FOOD CHAIN Unit 6: Energy! From Food to Forces Chemical Energy and LESSON 1 LESSON FOOD CHAIN Food chains and webs show the flow of chemical energy through an ecosystem. From the sun to tertiary consumers. students learn about the transfer of chemical energy and how producers and consumers depend on each other. They also learn scientists classifiy living things based on what they eat. Table of Contents 4 Launch! Sun. Chemical energy passing through the food chain starts with the sun. 6 Chemical Collisions A1: Chemical Energy. Hydrogen and helium are the chemical elements in the sun. 12 Productive Primary Producers A2: Producers. Producers use energy from the sun during photosynthesis. 18 Primary Producer Eaters A3: Primary Consumers. Primary consumers get energy by eating producers. 26 Consuming Critters A4: Secondary Consumers. Secondary consumers get energy by eating primary consumers. 34 Web of Life A5: Food Chains and Webs. Food chains and webs show the transfer of chemical energy in an ecosystem. 50 Tropical Trophic Tiers A6: Energy Pyramid. Scientists show energy transfers from the sun to producers to consumers with trophic levels. Launch! (Sun) SUN! where does chemical energy begin in a food chain? Chemical energy passing through the food chain starts with the sun. Unit 6: Chemical Energy and Food Chain Ready? Materials Nothing to prepare. Sticky notes Pencil Set? • Unit 4-Lesson 1-All Activities: Sun • Unit 6-Lesson 1-Activity 1: Chemical Collisions (Chemical Energy) • Unit 6-Lesson 1-Activity 2: Productive Primary Producers (Producers) • Unit 6-Lesson 1-Activity 3: Primary Producer Eaters (Primary Consumers) • Unit 6-Lesson 1-Activity 4: Consuming Critters (Secondary Consumers) • Unit 6-Lesson 1-Activity 5: Web of Life (Food Chains and Webs) • Unit 6-Lesson 1-Activity 6: Tropical Trophic Tiers (Energy Pyramid) Hawaii Standards Go! SC.K.3.1 Develop Know-Wonder-Learn chart with students. -
Productivity Significant Ideas
2.3 Flows of Energy & Matter - Productivity Significant Ideas • Ecosystems are linked together by energy and matter flow • The Sun’s energy drives these flows and humans are impacting the flows of energy and matter both locally and globally Knowledge & Understandings • As solar radiation (insolation) enters the Earth’s atmosphere some energy becomes unavailable for ecosystems as the energy absorbed by inorganic matter or reflected back into the atmosphere. • Pathways of radiation through the atmosphere involve the loss of radiation through reflection and absorption • Pathways of energy through an ecosystem include: • Conversion of light to chemical energy • Transfer of chemical energy from one trophic level to another with varying efficiencies • Overall conversion of UB and visible light to heat energy by the ecosystem • Re-radiation of heat energy to the atmosphere. Knowledge & Understandings • The conversion of energy into biomass for a given period of time is measured by productivity • Net primary productivity (NPP) is calculated by subtracting respiratory losses (R) from gross primary productivity (GPP) NPP = GPP – R • Gross secondary productivity (GSP) is the total energy/biomass assimulated by consumers and is calculated by subtracting the mass of fecal loss from the mass of food eaten. GSP = food eaten – fecal loss • Net secondary productivity (NSP) is calculated by subtracting the respiratory losses (R) from GSP. NSP=GSP - R Applications and Skills • Analyze quantitative models of flows of energy and matter • Construct quantitative -
7.014 Lectures 16 &17: the Biosphere & Carbon and Energy Metabolism
MIT Department of Biology 7.014 Introductory Biology, Spring 2005 7.014 Lectures 16 &17: The Biosphere & Carbon and Energy Metabolism Simplified Summary of Microbial Metabolism The metabolism of different types of organisms drives the biogeochemical cycles of the biosphere. Balanced oxidation and reduction reactions keep the system from “running down”. All living organisms can be ordered into two groups1, autotrophs and heterotrophs, according to what they use as their carbon source. Within these groups the metabolism of organisms can be further classified according to their source of energy and electrons. Autotrophs: Those organisms get their energy from light (photoautotrophs) or reduced inorganic compounds (chemoautotrophs), and their carbon from CO2 through one of the following processes: Photosynthesis (aerobic) — Light energy used to reduce CO2 to organic carbon using H2O as a source of electrons. O2 evolved from splitting H2O. (Plants, algae, cyanobacteria) Bacterial Photosynthesis (anaerobic) — Light energy used to reduce CO2 to organic carbon (same as photosynthesis). H2S is used as the electron donor instead of H2O. (e.g. purple sulfur bacteria) Chemosynthesis (aerobic) — Energy from the oxidation of inorganic molecules is used to reduce CO2 to organic carbon (bacteria only). -2 e.g. sulfur oxidizing bacteria H2S → S → SO4 + - • nitrifying bacteria NH4 → NO2 → NO3 iron oxidizing bacteria Fe+2 → Fe+3 methane oxidizing bacteria (methanotrophs) CH4 → CO2 Heterotrophs: These organisms get their energy and carbon from organic compounds (supplied by autotrophs through the food web) through one or more of the following processes: Aerobic Respiration (aerobic) ⎯ Oxidation of organic compounds to CO2 and H2O, yielding energy for biological work.