Supplement A: Assumptions and Equations in Ecopath with Ecosim Governing Equations
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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. -
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. -
New York Ocean Action Plan 2016 – 2026
NEW YORK OCEAN ACTION PLAN 2016 – 2026 In collaboration with state and federal agencies, municipalities, tribal partners, academic institutions, non- profits, and ocean-based industry and tourism groups. Acknowledgments The preparation of the content within this document was developed by Debra Abercrombie and Karen Chytalo from the New York State Department of Environmental Conservation and in cooperation and coordination with staff from the New York State Department of State. Funding was provided by the New York State Environmental Protection Fund’s Ocean & Great Lakes Program. Other New York state agencies, federal agencies, estuary programs, the New York Ocean and Great Lakes Coalition, the Shinnecock Indian Nation and ocean-based industry and user groups provided numerous revisions to draft versions of this document which were invaluable. The New York Marine Sciences Consortium provided vital recommendations concerning data and research needs, as well as detailed revisions to earlier drafts. Thank you to all of the members of the public and who participated in the stakeholder focal groups and for also providing comments and revisions. For more information, please contact: Karen Chytalo New York State Department of Environmental Conservation [email protected] 631-444-0430 Cover Page Photo credits, Top row: E. Burke, SBU SoMAS, M. Gove; Bottom row: Wolcott Henry- 2005/Marine Photo Bank, Eleanor Partridge/Marine Photo Bank, Brandon Puckett/Marine Photo Bank. NEW YORK OCEAN ACTION PLAN | 2016 – 2026 i MESSAGE FROM COMMISSIONER AND SECRETARY The ocean and its significant resources have been at the heart of New York’s richness and economic vitality, since our founding in the 17th Century and continues today. -
Evidence for Ecosystem-Level Trophic Cascade Effects Involving Gulf Menhaden (Brevoortia Patronus) Triggered by the Deepwater Horizon Blowout
Journal of Marine Science and Engineering Article Evidence for Ecosystem-Level Trophic Cascade Effects Involving Gulf Menhaden (Brevoortia patronus) Triggered by the Deepwater Horizon Blowout Jeffrey W. Short 1,*, Christine M. Voss 2, Maria L. Vozzo 2,3 , Vincent Guillory 4, Harold J. Geiger 5, James C. Haney 6 and Charles H. Peterson 2 1 JWS Consulting LLC, 19315 Glacier Highway, Juneau, AK 99801, USA 2 Institute of Marine Sciences, University of North Carolina at Chapel Hill, 3431 Arendell Street, Morehead City, NC 28557, USA; [email protected] (C.M.V.); [email protected] (M.L.V.); [email protected] (C.H.P.) 3 Sydney Institute of Marine Science, Mosman, NSW 2088, Australia 4 Independent Researcher, 296 Levillage Drive, Larose, LA 70373, USA; [email protected] 5 St. Hubert Research Group, 222 Seward, Suite 205, Juneau, AK 99801, USA; [email protected] 6 Terra Mar Applied Sciences LLC, 123 W. Nye Lane, Suite 129, Carson City, NV 89706, USA; [email protected] * Correspondence: [email protected]; Tel.: +1-907-209-3321 Abstract: Unprecedented recruitment of Gulf menhaden (Brevoortia patronus) followed the 2010 Deepwater Horizon blowout (DWH). The foregone consumption of Gulf menhaden, after their many predator species were killed by oiling, increased competition among menhaden for food, resulting in poor physiological conditions and low lipid content during 2011 and 2012. Menhaden sampled Citation: Short, J.W.; Voss, C.M.; for length and weight measurements, beginning in 2011, exhibited the poorest condition around Vozzo, M.L.; Guillory, V.; Geiger, H.J.; Barataria Bay, west of the Mississippi River, where recruitment of the 2010 year class was highest. -
Using Ecopath with Ecosim to Explore Nekton Community Response to Freshwater Diversion Into a Louisiana Estuary
Marine and Coastal Fisheries: Dynamics, Management, and Ecosystem 4:104-116, Science 2012 © American Fisheries Society 2012 ISSN: 1942-5120 online DOI: 10.1080/19425120.2012.672366 ARTICLE Using Ecopath with Ecosim to Explore Nekton Community Response to Freshwater Diversion into a Louisiana Estuary Kim de Mutsert*^ and James H. Cowan Jr. Department of Oceanography and Coastal Sciences, Louisiana State University, Baton Rouge, Louisiana 70803, USA Carl J, Walters Fisheries Centre, University of British Columbia, 2202 Main Mali, Vancouver, British Columbia V6TIZ4, Canada C5 ,=3 Abstract Current methods to restore I.ouisiana’s estuaries include the reintroduction of Mississippi River water through freshwater diversions to wetlands that are hydrologically isolated from the main channel. The reduced salinities associated with freshwater input arc likely affecting estuarine nekton, but these effects are poorly described. Ecopath with Ecosim was used to simulate the effects of salinity changes caused by the Caernarvon freshwater diversion on species biomass distributions of estuarine nekton. A base model was first created in Ecopath from 5 years of monitoring data collected prior to the opening of the diversion (1986-1990). The effects of freshwater discharge on food web dynamics and community composition were simulated using a novel application of Ecosim that allows the input of salinity as a forcing function coupled with user-specified salinity tolerance ranges for each biomass pool. The salinity function in Ecosim not only reveals the direct effects of salinity (i.e., increases in species biomass at their optimum salinity and decreases outside the optimal range) but also the indirect effects resulting from trophic interactions. -
CHAPTER 5 Ecopath with Ecosim: Linking Fisheries and Ecology
CHAPTER 5 Ecopath with Ecosim: linking fi sheries and ecology V. Christensen Fisheries Centre, University of British Columbia, Canada. 1 Why ecosystem modeling in fi sheries? Fifty years ago, fi sheries science emerged as a quantitative discipline with the publication of Ray Beverton and Sidney Holt’s [1] seminal volume On the Dynamics of Exploited Fish Populations. This book provided the foundation for how to manage fi sheries and was based on detailed, mathe- matical analyses of the dynamics of individual fi sh populations, of how they grow and how they are affected by fi shing. Fisheries science has developed and matured since then, and remarkably much of what has been achieved are modifi cations and further developments of what Beverton and Holt introduced. Given then that fi sheries science has developed to become one of the most data-rich, quantita- tive fi elds in ecology [2], how well has it fared? We often see fi sheries issues in the headlines and usually in a negative context and there are indeed many threats to the sustainability of ocean resources [3]. Many, judging not the least from newspaper headlines, consider fi sheries manage- ment a usual suspect in connection with fi sheries collapses. This may lead one to suspect that there is a problem with the science, but I hold this to be an erroneous conclusion. It should be stressed that the main problem is not to be found in the computational aspects of the science, but rather in how management advice actually is implemented in praxis [4]. The major force in fi sh- eries throughout the world is excessive fi shing capacity; the days with unexploited resources and untapped oceans are over [5], and the fi shing industry is now relying heavily on subsidies to keep the machinery going [6]. -
Micro-Food Web Structure Shapes Rhizosphere Microbial Communities and Growth in Oak
diversity Article Micro-Food Web Structure Shapes Rhizosphere Microbial Communities and Growth in Oak Hazel R. Maboreke ID , Veronika Bartel, René Seiml-Buchinger and Liliane Ruess * ID Institute of Biology, Ecology Group, Humboldt-Universität zu Berlin, Philippstraße 13, 10115 Berlin, Germany; [email protected] (H.R.M.); [email protected] (V.B.); [email protected] (R.S.-B.) * Correspondence: [email protected]; Tel.: +49-302-0934-9722 Received: 1 January 2018; Accepted: 11 March 2018; Published: 13 March 2018 Abstract: The multitrophic interactions in the rhizosphere impose significant impacts on microbial community structure and function, affecting nutrient mineralisation and consequently plant performance. However, particularly for long-lived plants such as forest trees, the mechanisms by which trophic structure of the micro-food web governs rhizosphere microorganisms are still poorly understood. This study addresses the role of nematodes, as a major component of the soil micro-food web, in influencing the microbial abundance and community structure as well as tree growth. In a greenhouse experiment with Pedunculate Oak seedlings were grown in soil, where the nematode trophic structure was manipulated by altering the proportion of functional groups (i.e., bacterial, fungal, and plant feeders) in a full factorial design. The influence on the rhizosphere microbial community, the ectomycorrhizal symbiont Piloderma croceum, and oak growth, was assessed. Soil phospholipid fatty acids were employed to determine changes in the microbial communities. Increased density of singular nematode functional groups showed minor impact by increasing the biomass of single microbial groups (e.g., plant feeders that of Gram-negative bacteria), except fungal feeders, which resulted in a decline of all microorganisms in the soil. -
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 -
Global Biogeography of Fungal and Bacterial Biomass Carbon in Topsoil
UC Davis UC Davis Previously Published Works Title Global biogeography of fungal and bacterial biomass carbon in topsoil Permalink https://escholarship.org/uc/item/1mm4s4x3 Authors He, L Mazza Rodrigues, JL Soudzilovskaia, NA et al. Publication Date 2020-12-01 DOI 10.1016/j.soilbio.2020.108024 Peer reviewed eScholarship.org Powered by the California Digital Library University of California Soil Biology and Biochemistry 151 (2020) 108024 Contents lists available at ScienceDirect Soil Biology and Biochemistry journal homepage: http://www.elsevier.com/locate/soilbio Global biogeography of fungal and bacterial biomass carbon in topsoil Liyuan He a, Jorge L. Mazza Rodrigues b, Nadejda A. Soudzilovskaia c, Milagros Barcelo´ c, Pål Axel Olsson d, Changchun Song e, Leho Tedersoo f, Fenghui Yuan a,g, Fengming Yuan h, David A. Lipson a, Xiaofeng Xu a,* a Biology Department, San Diego State University, San Diego, CA, 92182, USA b Department of Land, Air and Water Resources, University of California Davis, Davis, CA 95616, USA c Environmental Biology Department; Institute of Environmental Sciences, CML, Leiden University; Einsteinweg 2, 2333 CC Leiden, the Netherlands d Biodiversity, Biology Department, Lund University, SE-223 62 Lund, Sweden e Northeast Institute of Geography and Agroecology, Chinese Academy of Sciences, Changchun, 130102, China f Institute of Ecology and Earth Sciences, University of Tartu, 14a Ravila, 50411 Tartu, Estonia g Shenyang Institute of Applied Ecology, Chinese Academy of Sciences, Shenyang, 110016, China h Oak Ridge National Laboratory, Environmental Sciences Division, Oak Ridge, TN, USA ARTICLE INFO ABSTRACT Keywords: Bacteria and fungi, representing two major soil microorganism groups, play an important role in global nutrient Fungi biogeochemistry. -
Numerical and Experimental Investigation of Equivalence Ratio (ER) and Feedstock Particle Size on Birchwood Gasification
energies Article Numerical and Experimental Investigation of Equivalence Ratio (ER) and Feedstock Particle Size on Birchwood Gasification Rukshan Jayathilake ID and Souman Rudra * Department of Engineering and Sciences, University of Agder, Grimstad 4879, Norway; [email protected] * Correspondence: [email protected]; Tel.: +47-3723-3036 Received: 13 July 2017; Accepted: 15 August 2017; Published: 19 August 2017 Abstract: This paper discusses the characteristics of Birchwood gasification using the simulated results of a Computational Fluid Dynamics (CFD) model. The CFD model is developed and validated with the experimental results obtained with the fixed bed downdraft gasifier available at the University of Agder (UIA), Norway. In this work, several parameters are examined and given importance, such as producer gas yield, syngas composition, lower heating value (LHV), and cold gas efficiency (CGE) of the syngas. The behavior of the parameters mentioned above is examined by varying the biomass particle size. The diameters of the two biomass particles are 11.5 mm and 9.18 mm. All the parameters investigate within the Equivalences Ratio (ER) range from 0.2 to 0.5. In the simulations, a variable air inflow rate is used to achieve different ER values. For the different biomass particle sizes, CO, CO2, CH4, and H2 mass fractions of the syngas are analyzed along with syngas yield, LHV, and CGE. At an ER value of 0.35, 9.18 mm diameter particle shows average maximum values of 60% of CGE and 2.79 Nm3/h of syngas yield, in turn showing 3.4% and 0.09 Nm3/h improvement in the respective parameters over the 11.5 mm diameter biomass particle. -
Mapping Fisheries Onto Marine Ecosystems for Regional, Oceanic and Global Integrations
Large Marine Ecosystems of the World G. Hempel and K. Sherman (Editors) 0 2003 Elsevier B. V. All rights reserved 375 Mapping Fisheries onto Marine Ecosystems for Regional, Oceanic and Global Integrations Reg Watson, Daniel Pauly, Villy Christensen,Rainer Froese,Alan Longhurst, Trevor Platt, Shubha Sathyendranath,Kenneth Sherman,John O'Reilly, and Peter Celone ABSTRACT Research on ecosystem-based fisheries management, marine biodiversity conservation,and other marine fields requires appropriate maps of the major natural regions of the oceans,and their ecosystems.A global ocean classification system proposed by T. Platt and S. Sathyendranathand implemented by A.R. Longhurst, defined largely by physical parameters that subdivide the oceansinto four 'biomes' and 57 'biogeochemicalprovinces' (BGCPs),is merged with the systemof 64 Large Marine Ecosystems (LMEs) identified by K. Sherman and colleagues as transboundarygeographic coastaland watershedunits. This arrangementenhances each of the systems,and renders them mutually compatible. LMEs are ecologically defined to serve as a framework for the assessmentand managementof coastal fisheries and environments including watersheds,while the BGCPshave physical definitions, including borders defined by natural features, and extend over open oceanregions. The combined mapping will, for example, allow the computation of GI5-derived properties such as temperature,primary production, and their analysis in relation to fishery abundancedata for any study area in the combinedsystem. A further useful aspectof the integration is that it allows for the quantification, even within the EEZs of various countries, of the distribution of marine features (e.g. primary production, coral reef areas)so far not straightforwardly associatedwith different coastalstates. Applications to shelf,coral reef and oceanicfisheries, and to the mapping of marine biodiversity are briefly discussed.