NUTRIENT CYCLES (How Are Nutrients Recycled Through Ecosystems?)
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Does Dietary Fiber Affect the Levels of Nutritional Components After Feed Formulation?
fibers Article Does Dietary Fiber Affect the Levels of Nutritional Components after Feed Formulation? Seidu Adams 1 ID , Cornelius Tlotliso Sello 2, Gui-Xin Qin 1,3,4, Dongsheng Che 1,3,4,* and Rui Han 1,3,4 1 College of Animal Science and Technology, Jilin Agricultural University, Changchun 130118, China; [email protected] (S.A.); [email protected] (G.-X.Q.); [email protected] (R.H.) 2 College of Animal Science and Technology, Department of Animal Genetics, Breeding and Reproduction, Jilin Agricultural University, Changchun 130118, China; [email protected] 3 Key Laboratory of Animal Production, Product Quality and Security, Jilin Agricultural University, Ministry of Education, Changchun 130118, China 4 Jilin Provincial Key Laboratory of Animal Nutrition and Feed Science, Jilin Agricultural University, Changchun 130118, China * Correspondence: [email protected]; Tel.: +86-136-4431-9554 Received: 12 January 2018; Accepted: 25 April 2018; Published: 7 May 2018 Abstract: Studies on dietary fiber and nutrient bioavailability have gained an increasing interest in both human and animal nutrition. Questions are increasingly being asked regarding the faith of nutrient components such as proteins, minerals, vitamins, and lipids after feed formulation. The aim of this review is to evaluate the evidence with the perspective of fiber usage in feed formulation. The consumption of dietary fiber may affect the absorption of nutrients in different ways. The physicochemical factors of dietary fiber, such as fermentation, bulking ability, binding ability, viscosity and gel formation, water-holding capacity and solubility affect nutrient absorption. The dietary fiber intake influences the different methods in which nutrients are absorbed. -
The Water Cycle
Natural Resource Management Basic concepts and strategies 1 This publication was co-financed by the Catholic Relief Services (CRS) and the generous support of the American people through the United States Agency of International Development (USAID) Office of Acquisition and Assistance under the terms of Leader with Associates Cooperative Agreement No. AID-OAA-L-10-00003 with the University of Illinois at Urbana Champaign for the Modernizing Extension and Advisory Services (MEAS) Project. MEAS aims at promoting and assisting in the modernization of rural extension and advisory services worldwide through various outputs and services. The services benefit a wide audience of users, including developing country policymakers and technical specialists, development practitioners from NGOs, other donors, and consultants, and USAID staff and projects. Catholic Relief Services (CRS) serves the poor and disadvantaged overseas. CRS provides emergency relief in the wake of natural and man-made disasters and promotes the subsequent recovery of communities through integrated development interventions, without regard to race, creed or nationality. CRS’ programs and resources respond to the U.S. Bishops’ call to live in solidarity – as one human family – across borders, over oceans, and through differences in language, culture and economic condition. CRS provided co-financing for this publication. Catholic Relief Services 228 West Lexington Street Baltimore, MD 21201-3413 USA Illustrations: Jorge Enrique Gutiérrez Printed in the United States of America. ISBN x-xxxxxx-xx-x Download this publication and related material at http://crsprogramquality.org/ or at http://www.meas-extension.org/meas-offers/training © 20[nn] Catholic Relief Services – United States Conference of Catholic Bishops and MEAS project This work is licensed under a Creative Commons Attribution 3.0 Unported License. -
Terrestrial Decomposition
Terrestrial Decomposition • Objectives – Controls over decomposition • Litter breakdown • Soil organic matter formation and dynamics – Carbon balance of ecosystems • Soil carbon storage 1 Overview • In terrestrial ecosystems, soils (organic horizon + mineral soil) > C than in vegetation and atmosphere combined 2 Overview • Decomposition is: 1. Major pathway for C loss from ecosystems 2. Central to ecosystem C loss and storage 3 Overview 4 Incorporation 1 year later Overview • Predominant controls on litter decomposition are fairly well constrained 1. Temperature and moisture 2. Litter quality • N availability • Lignin concentration • Lignin:N • Mechanisms for soil organic matter stabilization: 1. Recalcitrance (refers to chemistry) 2. Physical protection • Within soil aggregates • Organo-mineral associations 3. Substrate supply regulation (energetic limitation) 5 Overview • Disturbance can override millenia in a matter of days or years: 1. Land use change 2. Invasive species 3. Climate change • Understanding the mechanistic drivers of decomposition, soil organic matter formation, and carbon stabilization help us make management decisions, take mitigation steps, and protect resources. 6 Overview Native Ōhiʻa - Koa forest Conversion to Reforestation in grass-dominated pasture (80 yr) Eucalyptus plantation (10 yr) Conventional sugar cane harvest. 20° C 18° C 16° C 14° C 7 Sustainable ratoon harvest. Decomposition • Decomposition is the biological, physical and chemical breakdown of organic material – Provides energy for microbial growth -
Macronutrients and Human Health for the 21St Century
nutrients Editorial Macronutrients and Human Health for the 21st Century Bernard J. Venn Department of Human Nutrition, University of Otago, Dunedin 9054, New Zealand; [email protected] Received: 30 July 2020; Accepted: 4 August 2020; Published: 7 August 2020 Abstract: Fat, protein and carbohydrate are essential macronutrients. Various organisations have made recommendations as to the energy contribution that each of these components makes to our overall diet. The extent of food refining and the ability of food systems to support future populations may also impact on how macronutrients contribute to our diet. In this Special Issue, we are calling for manuscripts from all disciplines to provide a broad-ranging discussion on macronutrients and health from personal, public and planetary perspectives. Keywords: macronutrient; fat; protein; carbohydrate; acceptable macronutrient distribution range; starch; sustainability The macronutrients, fat, protein and carbohydrate provide energy and essential components to sustain life. Fat is composed of glycerol and fatty acids; protein is an agglomeration of amino acids; and carbohydrate is simple sugars occurring either as monosaccharides or chains of connected monosaccharides (e.g., starch) whose bonds are either hydrolysed in the human small intestine to monosaccharides or are resistant to hydrolysis (dietary fibre). To maintain longevity and health, a combination of these macronutrients is required in our diet. It is elusive as to whether there is a combination of macronutrients that provides optimal health. When expressed as a percentage of energy to the diet, human populations have historically survived on diets with greatly differing proportions of these macronutrients. For example, the animal-based diet of an Alaskan Inuit group was found to comprise 33% protein, 41% fat and 26% carbohydrate [1]. -
Ecological Principles and Function of Natural Ecosystems by Professor Michel RICARD
Intensive Programme on Education for sustainable development in Protected Areas Amfissa, Greece, July 2014 ------------------------------------------------------------------------ Ecological principles and function of natural ecosystems By Professor Michel RICARD Summary 1. Hierarchy of living world 2. What is Ecology 3. The Biosphere - Lithosphere - Hydrosphere - Atmosphere 4. What is an ecosystem - Ecozone - Biome - Ecosystem - Ecological community - Habitat/biotope - Ecotone - Niche 5. Biological classification 6. Ecosystem processes - Radiation: heat, temperature and light - Primary production - Secondary production - Food web and trophic levels - Trophic cascade and ecology flow 7. Population ecology and population dynamics 8. Disturbance and resilience - Human impacts on resilience 9. Nutrient cycle, decomposition and mineralization - Nutrient cycle - Decomposition 10. Ecological amplitude 11. Ecology, environmental influences, biological interactions 12. Biodiversity 13. Environmental degradation - Water resources degradation - Climate change - Nutrient pollution - Eutrophication - Other examples of environmental degradation M. Ricard: Summer courses, Amfissa July 2014 1 1. Hierarchy of living world The larger objective of ecology is to understand the nature of environmental influences on individual organisms, populations, communities and ultimately at the level of the biosphere. If ecologists can achieve an understanding of these relationships, they will be well placed to contribute to the development of systems by which humans -
Learning the Water, Carbon and Nitrogen Cycles Through the Effects of Intensive Farming Techniques
Learning the Water, Carbon and Nitrogen Cycles through the Effects of Intensive Farming Techniques Winnie Chan Furness High School Overview Rationale Objectives Strategies Classroom Activities Annotated Bibliography/Resources Appendices/Content Standards Overview Elements of natural substances are constantly cycling through Earth. Water, carbon, and nitrogen move through Earth’s many ecosystems in closed paths called the biogeochemical cycles. In this unit, students will learn about these cycles by understanding modern farming techniques used to produce enough food to feed a world population of 7.8 billion. Students will plan and carry out experiments, analyze and interpret data, and communicate the information learned. This curriculum unit is intended for Biology students in Grades 9 and 10. The lessons are meant to be incorporated into “Unit 10: Ecology” of the School District of Philadelphia’s Core Curriculum for Biology, which is typically taught at the end of the year (May/June). Rationale The biogeochemical cycles operate on a fixed amount of matter on Earth. While the total amounts of water, carbon and nitrogen do not change, these substances exist in many different forms. Water is found on Earth as solid ice, liquid water or gaseous vapor. Carbon and nitrogen both exist as in the atmosphere as carbon dioxide gas and nitrogen gas, respectively, or as an integrated part of living and non-living substances. The hydrologic or water cycle describes the constant movement of water through Earth and its atmosphere. Major processes of -
Biogeochemical Cycles
Biogeochemical Cycles Essential Knowledge Objectives 2.A.3 (a) Biogeochemical Cycles • Cycle inorganic and organic nutrients between organisms and the environment – Carbon cycle – Nitrogen cycle – Phosphorus cycle – Water cycle (also known as the hydrological cycle) Cycling of Matter • Organisms must exchange matter with the environment to grow, reproduce and maintain organization • Molecules and atoms from the environment are necessary to build new molecules Molecules Essential for Life • Carbohydrates – composed of C, H, and O, monomer is a monosaccharide • Lipids – composed of C, H, and O, monomers are fatty acids and glycerol • Proteins – composed of C, H, O, N, and S in trace amounts, monomers are amino acids • Nucleic Acids – composed of C, H, O, N and P, monomers are nucleotides Carbon • Carbon moves from the environment to organisms where it is used to build the essential organic molecules • Carbon is used in storage compounds and cell formation in all organisms Carbon in the Environment • Carbon found in something non-living is called inorganic carbon • Inorganic carbon is found in rocks (limestone), shells, the atmosphere and the oceans • Living organisms must “fix” inorganic carbon into organic carbon to build the organic compounds necessary for life Carbon Cycle Nitrogen and Phosphorus • Nitrogen moves from the environment to organisms where it is used to build proteins and nucleic acids • Phosphorus moves from the environment to organisms where it is used to build nucleic acids, certain lipids, and ATP (cell energy) Nitrogen -
Human Alteration of the Global Nitrogen Cycle
What is Nitrogen? Human Alteration of the Nitrogen is the most abundant element in Global Nitrogen Cycle the Earth’s atmosphere. Nitrogen makes up 78% of the troposphere. Nitrogen cannot be absorbed directly by the plants and animals until it is converted into compounds they can use. This process is called the Nitrogen Cycle. Heather McGraw, Mandy Williams, Suzanne Heinzel, and Cristen Whorl, Give SIUE Permission to Put Our Presentation on E-reserve at Lovejoy Library. The Nitrogen Cycle How does the nitrogen cycle work? Step 1- Nitrogen Fixation- Special bacteria convert the nitrogen gas (N2 ) to ammonia (NH3) which the plants can use. Step 2- Nitrification- Nitrification is the process which converts the ammonia into nitrite ions which the plants can take in as nutrients. Step 3- Ammonification- After all of the living organisms have used the nitrogen, decomposer bacteria convert the nitrogen-rich waste compounds into simpler ones. Step 4- Denitrification- Denitrification is the final step in which other bacteria convert the simple nitrogen compounds back into nitrogen gas (N2 ), which is then released back into the atmosphere to begin the cycle again. How does human intervention affect the nitrogen cycle? Nitric Oxide (NO) is released into the atmosphere when any type of fuel is burned. This includes byproducts of internal combustion engines. Production and Use of Nitrous Oxide (N2O) is released into the atmosphere through Nitrogen Fertilizers bacteria in livestock waste and commercial fertilizers applied to the soil. Removing nitrogen from the Earth’s crust and soil when we mine nitrogen-rich mineral deposits. Discharge of municipal sewage adds nitrogen compounds to aquatic ecosystems which disrupts the ecosystem and kills fish. -
The Science and Scope of Nutrition
The Science and Scope 1 of Nutrition LEARNING OBJECTIVES Define the scope and science of nutrition ( Infographic 1.1 ) Explain the connection between nutrition and chronic disease ( Infographic 1.2 ) Define and identify the major macronutrients and micronutrients ( Infographic 1.3 and Infographic 1.4 ) Summarize the purpose of the Dietary Reference Intake (DRI) values ( Infographic 1.5 ) Distinguish between the different types of DRI values and what each represents ( Infographic 1.6 and Infographic 1.7 ) Understand/explain the basis of the scientific method and how it is CHAPTER used in nutrition research ( Infographic 1.8 ) Describe three types of experimental design and the primary advantages of each ( Infographic 1.9 ) Describe reliable sources of nutrition information ( Infographic 1.10 ) t was the final months of World War II, and the Dutch people were starving. As a last-ditch effort to hold on to the Netherlands, the Germans had blocked the transport of food SPL/Science Source SPL/Science Ifrom the Netherlands eastern rural areas to its west- Exploring the ern cities. As a result, people were eating only a few hundred calories per day, typically a couple of small Science of slices of bread and potatoes. Some people used paper to thicken soup. This period, now known as the Dutch Hunger Winter, lasted from October 1944 Nutrition until the Netherlands was liberated in May 1945. 1 Copyright © W. H. Freeman and Company. Distributed by W. H. Freeman and Company strictly for use with its products. Not for redistribution. 02_POP_14867_ch01_001_023.indd 1 10/30/18 10:27 AM 1 THE SCIENCE AND SCOPE OF NUTRITION Thirty years later, a husband and wife it appeared as if a woman’s diet during preg- team of scientists at Columbia University nancy could have a strong influence on the decided to investigate whether these extreme weight of her child. -
Nitrogen Metabolism in Phytoplankton - Y
MARINE ECOLOGY – Nitrogen Metabolism in Phytoplankton - Y. Collos, J. A. Berges NITROGEN METABOLISM IN PHYTOPLANKTON Y. Collos Laboratoire d'Hydrobiologie CNRS, Université Montpellier II, France J. A. Berges School of Biology and Biochemistry, Queen's University of Belfast, UK Keywords: uptake, reduction, excretion, proteases, chlorophyllases, cell death. Contents 1. Introduction 2. Availability and use of different forms of nitrogen 2.1 Nitrate 2.2. Nitrite 2.3. Ammonium 2.4. Molecular N2 2.5. Dissolved organic N (DON) 2.6. Particulate nitrogen (PN) 3. Assimilation pathways 4. Accumulation and storage 4.1. Inorganic compounds 4.2. Organic compounds 5. Nutrient classification and preferences 6. Plasticity in cell composition 7. Overflow mechanisms: excretion and release processes 8. Recycling of N within the cell 9. Degradation pathways 9.1. Requirements for and roles of degradation 9.2. How is degradation accomplished? 9.3. Variation in degradation 9.4. Pathogenesis and Cell Death 10. From uptake to growth: time-lag phenomena 11. Relationships with carbon metabolism 12. Future directions AcknowledgementsUNESCO – EOLSS Glossary Bibliography SAMPLE CHAPTERS Biographical Sketches Summary Phytoplankton use a large variety of nitrogen compounds and are extremely well adapted to fluctuating environmental conditions by a high capacity to change their chemical composition.Degradation and turnover of nitrogen within phytoplankton is essential for many processes including normal cell maintenance, acclimations to changes in light, salinity, and nutrients, and cell defence against pathogens. The ©Encyclopedia of Life Support Systems (EOLSS) MARINE ECOLOGY – Nitrogen Metabolism in Phytoplankton - Y. Collos, J. A. Berges pathways by which N degradation is accomplished are very poorly understood, but based on work in higher plant species, protein degradation is likely to be of central importance. -
Plant Species Effects on Nutrient Cycling: Revisiting Litter Feedbacks
Review Plant species effects on nutrient cycling: revisiting litter feedbacks Sarah E. Hobbie Department of Ecology, Evolution and Behavior, University of Minnesota, St. Paul, MN 55108, USA In a review published over two decades ago I asserted reinforce those gradients and patterns of NPP, focusing that, along soil fertility gradients, plant traits change in on feedbacks operating through plant litter decomposition. ways that reinforce patterns of soil fertility and net Specifically, I evaluate two key assumptions underlying primary productivity (NPP). I reevaluate this assertion the plant litter feedback idea: (i) plant litter traits vary in light of recent research, focusing on feedbacks to NPP predictably along fertility gradients, and (ii) such variation operating through litter decomposition. I conclude that reinforces soil fertility gradients through effects on decom- mechanisms emerging since my previous review might position and litter N release. Given the number of synthetic weaken these positive feedbacks, such as negative cross-site analyses of plant traits and their consequences effects of nitrogen on decomposition, while others for nutrient cycling over the past two decades, the time is might strengthen them, such as slower decomposition ripe for revisiting my original assertions. Indeed, I show of roots compared to leaf litter. I further conclude that that my original assertion is more nuanced and complex predictive understanding of plant species effects on than originally claimed. In particular, I discuss the need to nutrient cycling will require developing new frameworks consider leaf litter decomposition more carefully and move that are broadened beyond litter decomposition to con- beyond consideration of leaf litter feedbacks to a more sider the full litter–soil organic matter (SOM) continuum. -
Vitamin and Mineral Requirements in Human Nutrition
P000i-00xx 3/12/05 8:54 PM Page i Vitamin and mineral requirements in human nutrition Second edition VITPR 3/12/05 16:50 Page ii WHO Library Cataloguing-in-Publication Data Joint FAO/WHO Expert Consultation on Human Vitamin and Mineral Requirements (1998 : Bangkok, Thailand). Vitamin and mineral requirements in human nutrition : report of a joint FAO/WHO expert consultation, Bangkok, Thailand, 21–30 September 1998. 1.Vitamins — standards 2.Micronutrients — standards 3.Trace elements — standards 4.Deficiency diseases — diet therapy 5.Nutritional requirements I.Title. ISBN 92 4 154612 3 (LC/NLM Classification: QU 145) © World Health Organization and Food and Agriculture Organization of the United Nations 2004 All rights reserved. Publications of the World Health Organization can be obtained from Market- ing and Dissemination, World Health Organization, 20 Avenue Appia, 1211 Geneva 27, Switzerland (tel: +41 22 791 2476; fax: +41 22 791 4857; e-mail: [email protected]). Requests for permis- sion to reproduce or translate WHO publications — whether for sale or for noncommercial distri- bution — should be addressed to Publications, at the above address (fax: +41 22 791 4806; e-mail: [email protected]), or to Chief, Publishing and Multimedia Service, Information Division, Food and Agriculture Organization of the United Nations, 00100 Rome, Italy. The designations employed and the presentation of the material in this publication do not imply the expression of any opinion whatsoever on the part of the World Health Organization and the Food and Agriculture Organization of the United Nations concerning the legal status of any country, territory, city or area or of its authorities, or concerning the delimitation of its frontiers or boundaries.