The River Food Web
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BIG RIVER ECOSYSTEM: Program 2
BIG RIVER ECOSYSTEM: A Question of Net Worth PURPOSE To explore biodiversity at the ecosystem level. KERA CONNECTIONS to Life Science Program 2 Core Content: Structure and Function in Living Systems Academic Expectations: 2.2 Patterns, 2.3 Systems, 2.4 Models & Scale ANSWERS TO Process Skills: Observation, Modeling aFIELD NOTES OBJECTIVES 1. In a hot and hostile environment, Students should be able to: the evaporated water cannot be 1.identify five “big river” organisms incorporated into living cells (as 2.construct a diagram showing interactions between living and we know them). nonliving parts of an ecosystem 2. An extremely cold environment, 3. discuss factors that affect the level of biodiversity in their river basin. or frozen desert, does not allow cells to utilize water. VOCABULARY 3. Answers will vary but should Teachers may wish to discuss the following terms: display logical flow of water and aquatic, commercial, ecosystem, water cycle and watershed. allow for recirculation in a loop. 4. Arteries and veins. aFIELD NOTEBOOK 5. A pumping heart. Ideas for Teachers 6. Diagram A shows many different A. Develop a concept map for the water cycle. Include these items in types of ecosystems in close the concept map: clouds, groundwater, apple tree, stream, precipita- proximity. tion, condensation, evaporation, harvest mouse, snowflakes, sun and 7. Add a watering hole, plant a humans. What other cycles are needed to maintain an ecosystem? miniature forest, create a B. Biospheres, containing algae, brine shrimp and water, are often meadow of wildflowers. Most shown in advertisements. Analyze how the biosphere is self-main- importantly, break up a monocul- taining. -
Response of Marine Food Webs to Climate-Induced Changes in Temperature and Inflow of Allochthonous Organic Matter
Response of marine food webs to climate-induced changes in temperature and inflow of allochthonous organic matter Rickard Degerman Department of Ecology and Environmental Science 901 87 Umeå Umeå 2015 1 Copyright©Rickard Degerman ISBN: 978-91-7601-266-6 Front cover illustration by Mats Minnhagen Printed by: KBC Service Center, Umeå University Umeå, Sweden 2015 2 Tillägnad Maria, Emma och Isak 3 Table of Contents Abstract 5 List of papers 6 Introduction 7 Aquatic food webs – different pathways Food web efficiency – a measure of ecosystem function Top predators cause cascade effects on lower trophic levels The Baltic Sea – a semi-enclosed sea exposed to multiple stressors Varying food web structures Climate-induced changes in the marine ecosystem Food web responses to increased temperature Responses to inputs of allochthonous organic matter Objectives 14 Material and Methods 14 Paper I Paper II and III Paper IV Results and Discussion 18 Effect of temperature and nutrient availability on heterotrophic bacteria Influence of food web length and labile DOC on pelagic productivity and FWE Consequences of changes in inputs of ADOM and temperature for pelagic productivity and FWE Control of pelagic productivity, FWE and ecosystem trophic balance by colored DOC Conclusion and future perspectives 21 Author contributions 23 Acknowledgements 23 Thanks 24 References 25 4 Abstract Global records of temperature show a warming trend both in the atmosphere and in the oceans. Current climate change scenarios indicate that global temperature will continue to increase in the future. The effects will however be very different in different geographic regions. In northern Europe precipitation is projected to increase along with temperature. -
Effects of Eutrophication on Stream Ecosystems
EFFECTS OF EUTROPHICATION ON STREAM ECOSYSTEMS Lei Zheng, PhD and Michael J. Paul, PhD Tetra Tech, Inc. Abstract This paper describes the effects of nutrient enrichment on the structure and function of stream ecosystems. It starts with the currently well documented direct effects of nutrient enrichment on algal biomass and the resulting impacts on stream chemistry. The paper continues with an explanation of the less well documented indirect ecological effects of nutrient enrichment on stream structure and function, including effects of excess growth on physical habitat, and alterations to aquatic life community structure from the microbial assemblage to fish and mammals. The paper also dicusses effects on the ecosystem level including changes to productivity, respiration, decomposition, carbon and other geochemical cycles. The paper ends by discussing the significance of these direct and indirect effects of nutrient enrichment on designated uses - especially recreational, aquatic life, and drinking water. 2 1. Introduction 1.1 Stream processes Streams are all flowing natural waters, regardless of size. To understand the processes that influence the pattern and character of streams and reduce natural variation of different streams, several stream classification systems (including ecoregional, fluvial geomorphological, and stream order classification) have been adopted by state and national programs. Ecoregional classification is based on geology, soils, geomorphology, dominant land uses, and natural vegetation (Omernik 1987). Fluvial geomorphological classification explains stream and slope processes through the application of physical principles. Rosgen (1994) classified stream channels in the United States into seven major stream types based on morphological characteristics, including entrenchment, gradient, width/depth ratio, and sinuosity in various land forms. -
Ecosystem Services Generated by Fish Populations
AR-211 Ecological Economics 29 (1999) 253 –268 ANALYSIS Ecosystem services generated by fish populations Cecilia M. Holmlund *, Monica Hammer Natural Resources Management, Department of Systems Ecology, Stockholm University, S-106 91, Stockholm, Sweden Abstract In this paper, we review the role of fish populations in generating ecosystem services based on documented ecological functions and human demands of fish. The ongoing overexploitation of global fish resources concerns our societies, not only in terms of decreasing fish populations important for consumption and recreational activities. Rather, a number of ecosystem services generated by fish populations are also at risk, with consequences for biodiversity, ecosystem functioning, and ultimately human welfare. Examples are provided from marine and freshwater ecosystems, in various parts of the world, and include all life-stages of fish. Ecosystem services are here defined as fundamental services for maintaining ecosystem functioning and resilience, or demand-derived services based on human values. To secure the generation of ecosystem services from fish populations, management approaches need to address the fact that fish are embedded in ecosystems and that substitutions for declining populations and habitat losses, such as fish stocking and nature reserves, rarely replace losses of all services. © 1999 Elsevier Science B.V. All rights reserved. Keywords: Ecosystem services; Fish populations; Fisheries management; Biodiversity 1. Introduction 15 000 are marine and nearly 10 000 are freshwa ter (Nelson, 1994). Global capture fisheries har Fish constitute one of the major protein sources vested 101 million tonnes of fish including 27 for humans around the world. There are to date million tonnes of bycatch in 1995, and 11 million some 25 000 different known fish species of which tonnes were produced in aquaculture the same year (FAO, 1997). -
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. -
Developments in Aquatic Microbiology
INTERNATL MICROBIOL (2000) 3: 203–211 203 © Springer-Verlag Ibérica 2000 REVIEW ARTICLE Samuel P. Meyers Developments in aquatic Department of Oceanography and Coastal Sciences, Louisiana State University, microbiology Baton Rouge, LA, USA Received 30 August 2000 Accepted 29 September 2000 Summary Major discoveries in marine microbiology over the past 4-5 decades have resulted in the recognition of bacteria as a major biomass component of marine food webs. Such discoveries include chemosynthetic activities in deep-ocean ecosystems, survival processes in oligotrophic waters, and the role of microorganisms in food webs coupled with symbiotic relationships and energy flow. Many discoveries can be attributed to innovative methodologies, including radioisotopes, immunofluores- cent-epifluorescent analysis, and flow cytometry. The latter has shown the key role of marine viruses in marine system energetics. Studies of the components of the “microbial loop” have shown the significance of various phagotrophic processes involved in grazing by microinvertebrates. Microbial activities and dissolved organic carbon are closely coupled with the dynamics of fluctuating water masses. New biotechnological approaches and the use of molecular biology techniques still provide new and relevant information on the role of microorganisms in oceanic and estuarine environments. International interdisciplinary studies have explored ecological aspects of marine microorganisms and their significance in biocomplexity. Studies on the Correspondence to: origins of both life and ecosystems now focus on microbiological processes in the Louisiana State University Station. marine environment. This paper describes earlier and recent discoveries in marine Post Office Box 19090-A. Baton Rouge, LA 70893. USA (aquatic) microbiology and the trends for future work, emphasizing improvements Tel.: +1-225-3885180 in methodology as major catalysts for the progress of this broadly-based field. -
Linking Biological Toxicity and the Spectral Characteristics Of
Chen et al. Environ Sci Eur (2019) 31:84 https://doi.org/10.1186/s12302-019-0269-y RESEARCH Open Access Linking biological toxicity and the spectral characteristics of contamination in seriously polluted urban rivers Zhongli Chen1, Zihan Zhu1, Jiyu Song1, Ruiyan Liao1, Yufan Wang1, Xi Luo1, Dongya Nie1, Yumeng Lei1, Ying Shao1* and Wei Yang2,3 Abstract Background: Urban river pollution risks to environments and human health are emerging as a serious concern worldwide. With the aim to achieve the health of urban river ecosystem, numerous monitoring programs have been implemented to investigate the spectral characteristics of contamination. While due to the complexity of aquatic pollutants, the linkages between harmful efects and the spectral characteristics of contamination are still a major challenge for capturing main threats to urban aquatic environments. To establish these linkages, surface water (SW), sediment pore water (SDPW), and riparian soil pore water (SPW) were collected from fve sites of the seriously pol- luted Qingshui Stream, China. The water-dissolved organic carbon (DOC), total nitrogen (TN), total phosphate (TP), fuorescence excitation–emission matrix, and specifc ultraviolet absorbance were applied to analyze the spectral characteristics of urban river contamination. The Photobacterium phosphorem 502 was used to test the acute toxicity of the samples. Finally, the correlations between acute toxicity and concentrations of DOC, TN, TP, and the spectral characteristics were explored. Results: The concentrations of DOC, TN, and TP in various samples amounted from 11.41 2.31 to 3844.67 87.80 mg/L, from 1.96 0.06 to 906.23 26.01 mg/L and from 0.06 0.01 to 101.00± 8.29 mg/L, respec- tively. -
Controls and Structure of the Microbial Loop
Controls and Structure of the Microbial Loop A symposium organized by the Microbial Oceanography summer course sponsored by the Agouron Foundation Saturday, July 1, 2006 Asia Room, East-West Center, University of Hawaii Symposium Speakers: Peter J. leB Williams (University of Bangor, Wales) David L. Kirchman (University of Delaware) Daniel J. Repeta (Woods Hole Oceanographic Institute) Grieg Steward (University of Hawaii) The oceans constitute the largest ecosystems on the planet, comprising more than 70% of the surface area and nearly 99% of the livable space on Earth. Life in the oceans is dominated by microbes; these small, singled-celled organisms constitute the base of the marine food web and catalyze the transformation of energy and matter in the sea. The microbial loop describes the dynamics of microbial food webs, with bacteria consuming non-living organic matter and converting this energy and matter into living biomass. Consumption of bacteria by predation recycles organic matter back into the marine food web. The speakers of this symposium will explore the processes that control the structure and functioning of microbial food webs and address some of these fundamental questions: What aspects of microbial activity do we need to measure to constrain energy and material flow into and out of the microbial loop? Are we able to measure bacterioplankton dynamics (biomass, growth, production, respiration) well enough to edu/agouroninstitutecourse understand the contribution of the microbial loop to marine systems? What factors control the flow of material and energy into and out of the microbial loop? At what scales (space and time) do we need to measure processes controlling the growth and metabolism of microorganisms? How does our knowledge of microbial community structure and diversity influence our understanding of the function of the microbial loop? Program: 9:00 am Welcome and Introductory Remarks followed by: Peter J. -
Spatial Heterogeneity and Controls of Ecosystem Metabolism in a Great Plains River Network
Spatial heterogeneity and controls of ecosystem metabolism in a Great Plains river network Walter K. Dodds, Sophie A. Higgs, Margaret J. Spangler, James Guinnip, Jeffrey D. Scott, Skyler C. Hedden, Bryan D. Frenette, et al. Hydrobiologia The International Journal of Aquatic Sciences ISSN 0018-8158 Volume 813 Number 1 Hydrobiologia (2018) 813:85-102 DOI 10.1007/s10750-018-3516-0 1 23 Your article is protected by copyright and all rights are held exclusively by Springer International Publishing AG, part of Springer Nature. This e-offprint is for personal use only and shall not be self-archived in electronic repositories. If you wish to self-archive your article, please use the accepted manuscript version for posting on your own website. You may further deposit the accepted manuscript version in any repository, provided it is only made publicly available 12 months after official publication or later and provided acknowledgement is given to the original source of publication and a link is inserted to the published article on Springer's website. The link must be accompanied by the following text: "The final publication is available at link.springer.com”. 1 23 Author's personal copy Hydrobiologia (2018) 813:85–102 https://doi.org/10.1007/s10750-018-3516-0 PRIMARY RESEARCH PAPER Spatial heterogeneity and controls of ecosystem metabolism in a Great Plains river network Walter K. Dodds . Sophie A. Higgs . Margaret J. Spangler . James Guinnip . Jeffrey D. Scott . Skyler C. Hedden . Bryan D. Frenette . Ryland Taylor . Anne E. Schechner . David J. Hoeinghaus . Michelle A. Evans-White Received: 17 June 2017 / Revised: 14 December 2017 / Accepted: 11 January 2018 / Published online: 20 January 2018 Ó Springer International Publishing AG, part of Springer Nature 2018 Abstract Gross primary production and ecosystem limitation, and was positively related to nutrients. -
Key Restoration Methods of a Polluted River Ecosystem
Key Restoration Methods of a Polluted River Chalachew Yenew* Ecosystem: A Systematic Review Environmental Health Science, Social and Population Health (SPH) Unit, College of Medicine and Health Sciences, Debre Tabor University, Ethiopia Abstract Background: River is one of a freshwater ecosystem that plays an important role in people's living, aquatic and terrestrial living organisms, and agricultural production. Compared to other ecosystems, rivers support a disproportionately large number of *Corresponding author: plant and animal species. However, excessive human activities have busted the original Chalachew Yenew ecological balance by polluting the river ecosystem. As a result, partial or total affected the structure and functions of the river ecosystem. This review aimed to investigate the major ecological restoration methods of the polluted river ecosystem. [email protected] Methods: We have adopted the procedures from the Preferred Reporting Items for Systematic Reviews and Meta-Analyses (PRISMA) guidelines. The required data were Environmental Health Science, Social and collected via a literature search of MEDLINE/PubMed, Google Scholar, Science Direct, Population Health (SPH) Unit, College of EMBASE, HINARI, and Cochrane Library from the 9th of September, 2019 to the 5th Medicine and Health Sciences, Debre Tabor of March, 2020 using combined terms. Articles were included in our review; only if University, Ethiopia it assessed empirically and comparison and contrast between two or more different restoration methods. This review; it is mainly included published research articles, national reports, and annual reports and excluded opinion essays. Citation: Yenew C (2021) Key Restoration Results: Commonly used methods for restoration of polluted rivers around the Methods of a Polluted River Ecosystem: A globe could be categorized depending on the physical, chemical, and biological Systematic Review. -
01 Delong 2-8 6/9/05 8:58 AM Page 2
01 Delong 2-8 6/9/05 8:58 AM Page 2 INSIGHT REVIEW NATURE|Vol 437|15 September 2005|doi:10.1038/nature04157 Genomic perspectives in microbial oceanography Edward F. DeLong1 and David M. Karl2 The global ocean is an integrated living system where energy and matter transformations are governed by interdependent physical, chemical and biotic processes. Although the fundamentals of ocean physics and chemistry are well established, comprehensive approaches to describing and interpreting oceanic microbial diversity and processes are only now emerging. In particular, the application of genomics to problems in microbial oceanography is significantly expanding our understanding of marine microbial evolution, metabolism and ecology. Integration of these new genome-enabled insights into the broader framework of ocean science represents one of the great contemporary challenges for microbial oceanographers. Marine ecosystems are complex and dynamic. A mechanistic under- greatly aid in these efforts. The correlation between organism- and habi- standing of the susceptibility of marine ecosystems to global environ- tat-specific genomic features and other physical, chemical and biotic mental variability and climate change driven by greenhouse gases will variables has the potential to refine our understanding of microbial and require a comprehensive description of several factors. These include biogeochemical process in ocean systems. marine physical, chemical and biological interactions including All these advances — improved cultivation, environmental genomic thresholds, negative and positive feedback mechanisms and other approaches and in situ microbial observatories — promise to enhance nonlinear interactions. The fluxes of matter and energy, and the our understanding of the living ocean system. Below, we provide a brief microbes that mediate them, are of central importance in the ocean, recent history of marine microbiology and outline some of the recent yet remain poorly understood. -
Microbial Loop Carbon Cycling in Ocean Environments Studied Using a Simple Steady-State Model
AQUATIC MICROBIAL ECOLOGY Vol. 26: 37–49, 2001 Published October 26 Aquat Microb Ecol Microbial loop carbon cycling in ocean environments studied using a simple steady-state model Thomas R. Anderson1,*, Hugh W. Ducklow2 1Southampton Oceanography Centre, Waterfront Campus, European Way, Southampton SO14 3ZH, United Kingdom 2College of William and Mary School of Marine Science, Rte 1208, Box 1346, Gloucester Point, Virginia 23062, USA ABSTRACT: A simple steady-state model is used to examine the microbial loop as a pathway for organic C in marine systems, constrained by observed estimates of bacterial to primary production ratio (BP:PP) and bacterial growth efficiency (BGE). Carbon sources (primary production including extracellular release of dissolved organic carbon, DOC), cycling via zooplankton grazing and viral lysis, and sinks (bacterial and zooplankton respiration) are represented. Model solutions indicate that, at least under near steady-state conditions, recent estimates of BP:PP of about 0.1 to 0.15 are consistent with reasonable scenarios of C cycling (low BGE and phytoplankton extracellular release) at open ocean sites such as the Sargasso Sea and subarctic North Pacific. The finding that bacteria are a major (50%) sink for primary production is shown to be consistent with the best estimates of BGE and dissolved organic matter (DOM) production by zooplankton and phytoplankton. Zooplank- ton-related processes are predicted to provide the greatest supply of DOC for bacterial consumption. The bacterial contribution to C flow in the microbial loop, via bacterivory and viral lysis, is generally low, as a consequence of low BGE. Both BP and BGE are hard to quantify accurately.