Micro-Food Web Structure Shapes Rhizosphere Microbial Communities and Growth in Oak
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Freshwater Ecosystems and Biodiversity
Network of Conservation Educators & Practitioners Freshwater Ecosystems and Biodiversity Author(s): Nathaniel P. Hitt, Lisa K. Bonneau, Kunjuraman V. Jayachandran, and Michael P. Marchetti Source: Lessons in Conservation, Vol. 5, pp. 5-16 Published by: Network of Conservation Educators and Practitioners, Center for Biodiversity and Conservation, American Museum of Natural History Stable URL: ncep.amnh.org/linc/ This article is featured in Lessons in Conservation, the official journal of the Network of Conservation Educators and Practitioners (NCEP). NCEP is a collaborative project of the American Museum of Natural History’s Center for Biodiversity and Conservation (CBC) and a number of institutions and individuals around the world. Lessons in Conservation is designed to introduce NCEP teaching and learning resources (or “modules”) to a broad audience. NCEP modules are designed for undergraduate and professional level education. These modules—and many more on a variety of conservation topics—are available for free download at our website, ncep.amnh.org. To learn more about NCEP, visit our website: ncep.amnh.org. All reproduction or distribution must provide full citation of the original work and provide a copyright notice as follows: “Copyright 2015, by the authors of the material and the Center for Biodiversity and Conservation of the American Museum of Natural History. All rights reserved.” Illustrations obtained from the American Museum of Natural History’s library: images.library.amnh.org/digital/ SYNTHESIS 5 Freshwater Ecosystems and Biodiversity Nathaniel P. Hitt1, Lisa K. Bonneau2, Kunjuraman V. Jayachandran3, and Michael P. Marchetti4 1U.S. Geological Survey, Leetown Science Center, USA, 2Metropolitan Community College-Blue River, USA, 3Kerala Agricultural University, India, 4School of Science, St. -
The Importance of Herbivore Density and Management As Determinants
1 The importance of herbivore density and management as 2 determinants of the distribution of rare plant species 3 James D. M. Speed* & Gunnar Austrheim 4 NTNU University Museum 5 Norwegian University of Science and Technology 6 NO-7491 Trondheim 7 Norway 8 *Correspondence: 9 +47 73592251 10 [email protected] 11 12 Speed, J.D.M. & Austrheim, G. (2017) The importance of herbivore density and management as 13 determinants of the distribution of rare plant species. Biological Conservation, 205, 77-84. 14 Post-print: Final version available here http://dx.doi.org/10.1016/j.biocon.2016.11.030 15 16 Abstract 17 Herbivores are often drivers of ecosystem states and dynamics and in many situations are managed 18 either as livestock or through controlled or exploitative hunting of wild populations. Changes in 19 herbivore density can affect the composition of plant communities. Management of herbivore 20 densities could therefore be regulated to benefit plant species of conservation concern. In this study 21 we use a unique spatial dataset of large herbivores in Norway to test whether herbivore density 22 affects the distribution of rare red-listed plant species in tundra ecosystems, and to identify regions 23 where herbivore density is the most important factor in determining the habitat suitability for the 24 plant species. For all selected species a climatic variable was the most important determinant of the 25 distribution, but herbivore density was an important determinant of some species notably Primula 26 scandinavica. Herbivore density was the most important factor determining habitat suitability for this 27 species in 13% of mainland Norway. -
Species-Habitat Associations
Species-Habitat associations Spatial Data • Predictive Models • Ecological Insights Jason Matthiopoulos • John Fieberg • Geert Aarts 2 Suggested Citation: Matthiopoulos, Jason; Fieberg, John; Aarts, Geert. (2020). Species-Habitat Associations: Spatial data, predictive models, and ecological insights. University of Minnesota Libraries Publishing. Retrieved from the University of Minnesota Digital Conservancy, http://hdl.handle.net/11299/217469. Related Works: A copy of the book, which we plan to continuously update (with new versions in the future) can be accessed in gitbook format at: https://bookdown.org/jfieberg/SHABook/. Cover photograph: Guanacos, a camelid native to South America, grazing in Torres del Paine National Park in the Pantagonia region of Chile. ©Gary R. Jensen, www.GaryRobertPhotography.com. License: This work, other than the cover photo, is licensed under a Creative Commons Attribution 4.0 International License. ISBN: 978-1-946135-68-1 Edition 1 Contents 5 About the Authors 6 Jason Matthiopoulos . .6 John Fieberg . .6 Geert Aarts . .6 Acknowledgments 7 Abbreviations 8 Glossary 9 Notation 15 Preface 16 0.1 A “live” project . 16 0.2 Audience . 16 0.3 Objectives . 17 0.4 Why is this book unique? . 17 0.5 Why model species habitat associations? . 18 I Fundamental concepts and methods 20 1 The ecology behind species-habitat-association models 21 1.1 Objectives . 21 1.2 How do living beings “see” the world around them? . 21 1.3 What is a habitat? . 23 1.4 What is a species-habitat association? . 24 1.5 What mechanisms drive habitat-mediated changes in species densities? . 26 1.6 When is species density a reliable reflection of habitat suitability? . -
Bacterial Production and Respiration
Organic matter production % 0 Dissolved Particulate 5 > Organic Organic Matter Matter Heterotrophic Bacterial Grazing Growth ~1-10% of net organic DOM does not matter What happens to the 90-99% of sink, but can be production is physically exported to organic matter production that does deep sea not get exported as particles? transported Export •Labile DOC turnover over time scales of hours to days. •Semi-labile DOC turnover on time scales of weeks to months. •Refractory DOC cycles over on time scales ranging from decadal to multi- decadal…perhaps longer •So what consumes labile and semi-labile DOC? How much carbon passes through the microbial loop? Phytoplankton Heterotrophic bacteria ?? Dissolved organic Herbivores ?? matter Higher trophic levels Protozoa (zooplankton, fish, etc.) ?? • Very difficult to directly measure the flux of carbon from primary producers into the microbial loop. – The microbial loop is mostly run on labile (recently produced organic matter) - - very low concentrations (nM) turning over rapidly against a high background pool (µM). – Unclear exactly which types of organic compounds support bacterial growth. Bacterial Production •Step 1: Determine how much carbon is consumed by bacteria for production of new biomass. •Bacterial production (BP) is the rate that bacterial biomass is created. It represents the amount of Heterotrophic material that is transformed from a nonliving pool bacteria (DOC) to a living pool (bacterial biomass). •Mathematically P = µB ?? µ = specific growth rate (time-1) B = bacterial biomass (mg C L-1) P= bacterial production (mg C L-1 d-1) Dissolved organic •Note that µ = P/B matter •Thus, P has units of mg C L-1 d-1 Bacterial production provides one measurement of carbon flow into the microbial loop How doe we measure bacterial production? Production (∆ biomass/time) (mg C L-1 d-1) • 3H-thymidine • 3H or 14C-leucine Note: these are NOT direct measures of biomass production (i.e. -
Microbial Loop' in Stratified Systems
MARINE ECOLOGY PROGRESS SERIES Vol. 59: 1-17, 1990 Published January 11 Mar. Ecol. Prog. Ser. 1 A steady-state analysis of the 'microbial loop' in stratified systems Arnold H. Taylor, Ian Joint Plymouth Marine Laboratory, Prospect Place, West Hoe, Plymouth PLl 3DH, United Kingdom ABSTRACT. Steady state solutions are presented for a simple model of the surface mixed layer, which contains the components of the 'microbial loop', namely phytoplankton, picophytoplankton, bacterio- plankton, microzooplankton, dissolved organic carbon, detritus, nitrate and ammonia. This system is assumed to be in equilibrium with the larger grazers present at any time, which are represented as an external mortality function. The model also allows for dissolved organic nitrogen consumption by bacteria, and self-grazing and mixotrophy of the microzooplankton. The model steady states are always stable. The solution shows a number of general properties; for example, biomass of each individual component depends only on total nitrogen concentration below the mixed layer, not whether the nitrogen is in the form of nitrate or ammonia. Standing stocks and production rates from the model are compared with summer observations from the Celtic Sea and Porcupine Sea Bight. The agreement is good and suggests that the system is often not far from equilibrium. A sensitivity analysis of the model is included. The effect of varying the mixing across the pycnocline is investigated; more intense mixing results in the large phytoplankton population increasing at the expense of picophytoplankton, micro- zooplankton and DOC. The change from phytoplankton to picophytoplankton dominance at low mixing occurs even though the same physiological parameters are used for both size fractions. -
Ecological Importance of Soil Bacterivores for Ecosystem Functions Jean Trap, Michael Bonkowski, Claude Plassard, Cécile Villenave, Eric Blanchart
Ecological importance of soil bacterivores for ecosystem functions Jean Trap, Michael Bonkowski, Claude Plassard, Cécile Villenave, Eric Blanchart To cite this version: Jean Trap, Michael Bonkowski, Claude Plassard, Cécile Villenave, Eric Blanchart. Ecological impor- tance of soil bacterivores for ecosystem functions. Plant and Soil, Springer Verlag, 2015, 398 (1-2), pp.1-24. 10.1007/s11104-015-2671-6. hal-01214705 HAL Id: hal-01214705 https://hal.archives-ouvertes.fr/hal-01214705 Submitted on 12 Oct 2015 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Manuscript Click here to download Manuscript: manuscrit.doc Click here to view linked References 1 Number of words (main text): 8583 2 Number of words (abstract): 157 3 Number of figures: 7 4 Number of tables: 1 5 Number of appendix: 1 6 7 Title 8 Ecological importance of soil bacterivores on ecosystem functions 9 10 Authors 11 Jean Trap1, Michael Bonkowski2, Claude Plassard3, Cécile Villenave4, Eric Blanchart1 12 13 Affiliations 14 15 1Institut de Recherche pour le Développement – UMR Eco&Sols, 2 Place Viala, 34060, Version postprint 16 Montpellier, France 17 2Dept. of Terrestrial Ecology, Institut of Zoology, University of Cologne, D-50674 Köln, 18 Germany 19 3Institut National de Recherche Agronomique – UMR Eco&Sols, 2 Place Viala, 34060, 20 Montpellier, France 21 4ELISOL environnement, 10 avenue du Midi, 30111 Congenies, France 22 23 1 Comment citer ce document : Trap, J., Bonkowski, M., Plassard, C., Villenave, C., Blanchart, E. -
The Soil Food Web
THE SOIL FOOD WEB HEALTHY SOIL HEALTHY ENVIRONMENT The Soil Food Web Alan Sundermeier Extension Educator and Program Leader, Wood County Extension, The Ohio State University. Vinayak Shedekar Postdoctural Researcher, The Ohio State University. A healthy soil depends on the interaction of many organisms that make up the soil food web. These organisms live all or part of their life cycle in the soil and are respon- sible for converting energy as one organism consumes another. Source: Soil Biology Primer The phospholipid fatty acid (PLFA) test can be used to measure the activity of the soil food web. The following chart shows that mi-crobial activity peaks in early summer when soil is warm and moisture is adequate. Soil sampling for detecting soil microbes should follow this timetable to better capture soil microbe activity. The soil food web begins with the ener- gy from the sun, which triggers photo- synthesis in plants. Photosynthesis re- sults in plants using the sun’s energy to fix carbon dioxide from the atmosphere. This process creates the carbon and organic compounds contained in plant material. This is the first trophic level. Then begins building of soil organic matter, which contains both long-last- ing humus, and active organic matter. Active organic matter contains readily available energy, which can be used by simple soil organisms in the second trophic level of the soil food web. Source: Soil Biology Primer SOILHEALTH.OSU.EDU THE SOIL FOOD WEB - PAGE 2 The second trophic level contains simple soil organisms, which Agriculture can enhance the soil food web to create more decompose plant material. -
Unit 2.3, Soil Biology and Ecology
2.3 Soil Biology and Ecology Introduction 85 Lecture 1: Soil Biology and Ecology 87 Demonstration 1: Organic Matter Decomposition in Litter Bags Instructor’s Demonstration Outline 101 Step-by-Step Instructions for Students 103 Demonstration 2: Soil Respiration Instructor’s Demonstration Outline 105 Step-by-Step Instructions for Students 107 Demonstration 3: Assessing Earthworm Populations as Indicators of Soil Quality Instructor’s Demonstration Outline 111 Step-by-Step Instructions for Students 113 Demonstration 4: Soil Arthropods Instructor’s Demonstration Outline 115 Assessment Questions and Key 117 Resources 119 Appendices 1. Major Organic Components of Typical Decomposer 121 Food Sources 2. Litter Bag Data Sheet 122 3. Litter Bag Data Sheet Example 123 4. Soil Respiration Data Sheet 124 5. Earthworm Data Sheet 125 6. Arthropod Data Sheet 126 Part 2 – 84 | Unit 2.3 Soil Biology & Ecology Introduction: Soil Biology & Ecology UNIT OVERVIEW MODES OF INSTRUCTION This unit introduces students to the > LECTURE (1 LECTURE, 1.5 HOURS) biological properties and ecosystem The lecture covers the basic biology and ecosystem pro- processes of agricultural soils. cesses of soils, focusing on ways to improve soil quality for organic farming and gardening systems. The lecture reviews the constituents of soils > DEMONSTRATION 1: ORGANIC MATTER DECOMPOSITION and the physical characteristics and soil (1.5 HOURS) ecosystem processes that can be managed to In Demonstration 1, students will learn how to assess the improve soil quality. Demonstrations and capacity of different soils to decompose organic matter. exercises introduce students to techniques Discussion questions ask students to reflect on what envi- used to assess the biological properties of ronmental and management factors might have influenced soils. -
Supplement A: Assumptions and Equations in Ecopath with Ecosim Governing Equations
Transactions of the American Fisheries Society 145:136–162, 2016 © American Fisheries Society 2016 DOI: 10.1080/00028487.2015.1069211 Supplement A: Assumptions and Equations in Ecopath with Ecosim Governing Equations The Ecopath module of EwE is a static, mass-balance ecosystem model that uses two governing equations for each species and age group (Christensen and Walters 2004). The first governing equation describes each species group’s production for a time period, i.e., production (P) is the sum of fishery catch (F), predation (M2), net migration (immigration, I, and emigration, E), biomass accumulation (BA), and mortality from other sources (‘other mortality’, M0): P = F + M2 + (I - E) + BA - M0 The second governing equation is based on the principle of conservation of matter within a group, and is designed to balance the energy flows of a biomass pool, i.e., consumption (C) equals the sum of production (P), respiration (R), and unassimilated food (U): C = P + R + U At a minimum, Ecopath requires inputs of diet composition (DCi,j, where i is predator and j is prey), fishery catch (Yi), and three of the following four parameters for each model group (i): biomass (Bi), production-to-biomass ratio (Pi/Bi), consumption-to-biomass ratio (Qi/Bi), and the ecotrophic efficiency (EEi, the fraction of the production that is used in the system and does not move directly to the detritus pool). Mass-balance principles are then used to estimate the fourth parameter. P/B is the annual production rate of the population in Ecopath. Under equilibrium conditions, the P/B ratio of fish is equivalent to its total annual instantaneous mortality (Z) (Allen 1971). -
Towards an Integrative Understanding of Soil Biodiversity
Towards an integrative understanding of soil biodiversity Madhav Thakur, Helen Phillips, Ulrich Brose, Franciska de Vries, Patrick Lavelle, Michel Loreau, Jérôme Mathieu, Christian Mulder, Wim van der Putten, Matthias Rillig, et al. To cite this version: Madhav Thakur, Helen Phillips, Ulrich Brose, Franciska de Vries, Patrick Lavelle, et al.. Towards an integrative understanding of soil biodiversity. Biological Reviews, Wiley, 2020, 95, pp.350 - 364. 10.1111/brv.12567. hal-02499460 HAL Id: hal-02499460 https://hal.archives-ouvertes.fr/hal-02499460 Submitted on 5 Mar 2020 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Biol. Rev. (2020), 95, pp. 350–364. 350 doi: 10.1111/brv.12567 Towards an integrative understanding of soil biodiversity Madhav P. Thakur1,2,3∗ , Helen R. P. Phillips2, Ulrich Brose2,4, Franciska T. De Vries5, Patrick Lavelle6, Michel Loreau7, Jerome Mathieu6, Christian Mulder8,WimH.Van der Putten1,9,MatthiasC.Rillig10,11, David A. Wardle12, Elizabeth M. Bach13, Marie L. C. Bartz14,15, Joanne M. Bennett2,16, Maria J. I. Briones17, George Brown18, Thibaud Decaens¨ 19, Nico Eisenhauer2,3, Olga Ferlian2,3, Carlos Antonio´ Guerra2,20, Birgitta Konig-Ries¨ 2,21, Alberto Orgiazzi22, Kelly S. -
Assessing the Potential Distribution of Invasive Alien Species Amorpha
A peer-reviewed open-access journal Nature ConservationAssessing 30: 41–67the potential (2018) distribution of invasive alien species Amorpha fruticosa... 41 doi: 10.3897/natureconservation.30.27627 RESEARCH ARTICLE http://natureconservation.pensoft.net Launched to accelerate biodiversity conservation Assessing the potential distribution of invasive alien species Amorpha fruticosa (Mill.) in the Mureş Floodplain Natural Park (Romania) using GIS and logistic regression Gheorghe Kucsicsa1, Ines Grigorescu1, Monica Dumitraşcu1, Mihai Doroftei2, Mihaela Năstase3, Gabriel Herlo4 1 Institute of Geography, Romanian Academy, 12 D. Racoviţă Street, sect. 2, 023993, Bucharest, Romania 2 Danube Delta National Institute, 165 Babadag Street, 820112, Tulcea, Romania 3 National Forest Ad- ministration, Protected Areas Department, 9A Petricani Street, sect. 2, Bucharest, Romania 4 National Forest Administration, Mureş Floodplain Natural Park Administration, Pădurea Ceala FN, Arad, Romania Corresponding author: Monica Dumitraşcu ([email protected]) Academic editor: Maurizio Pinna | Received 19 June 2018 | Accepted 2 October 2018 | Published 24 October 2018 http://zoobank.org/EF484149-F35A-4B0F-9F8B-4F8164BFF94F Citation: Kucsicsa G, Grigorescu I, Dumitraşcu M, Doroftei M, Năstase M, Herlo G (2018) Assessing the potential distribution of invasive alien species Amorpha fruticosa (Mill.) in the Mureş Floodplain Natural Park (Romania) using GIS and logistic regression. Nature Conservation 30: 41–67. https://doi.org/10.3897/natureconservation.30.27627 -
Short Term Shifts in Soil Nematode Food Web Structure and Nutrient Cycling Following Sustainable Soil Management in a California Vineyard
SHORT TERM SHIFTS IN SOIL NEMATODE FOOD WEB STRUCTURE AND NUTRIENT CYCLING FOLLOWING SUSTAINABLE SOIL MANAGEMENT IN A CALIFORNIA VINEYARD A Thesis presented to the Faculty of California Polytechnic State University, San Luis Obispo In Partial Fulfillment of the Requirements for the Degree Master of Science in Agriculture with a Specialization in Soil Science by Holly M. H. Deniston-Sheets April 2019 © 2019 Holly M. H. Deniston-Sheets ALL RIGHTS RESERVED ii COMMITTEE MEMBERSHIP TITLE: Short Term Shifts in Soil Nematode Food Feb Structure and Nutrient Cycling Following Sustainable Soil Management in a California Vineyard AUTHOR: Holly M. H. Deniston-Sheets DATE SUBMITTED: April 2019 COMMITTEE CHAIR: Cristina Lazcano, Ph.D. Assistant Professor of Natural Resources & Environmental Sciences COMMITTEE MEMBER: Bwalya Malama, Ph.D. Associate Professor of Natural Resources & Environmental Sciences COMMITTEE MEMBER: Katherine Watts, Ph.D Assistant Professor of Chemistry and Biochemistry iii ABSTRACT Short term shifts in soil nematode food web structure and nutrient cycling following sustainable soil management in a California vineyard Holly M. H. Deniston-Sheets Evaluating soil health using bioindicator organisms has been suggested as a method of analyzing the long-term sustainability of agricultural management practices. The main objective of this study was to determine the effects of vineyard management strategies on soil food web structure and function, using nematodes as bioindicators by calculating established nematode ecological indices. Three field trials were conducted in a commercial Pinot Noir vineyard in San Luis Obispo, California; the effects of (i) fertilizer type (organic and inorganic), (ii) weed management (herbicide and tillage), and (iii) cover crops (high or low water requirements) on nematode community structure, soil nutrient content, and crop quality and yield were analyzed.