Eutrophication in the Global Proliferation of Harmful Algal Blooms
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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. -
Geohab Core Research Project
GEOHAB CORE RESEARCH PROJECT: HABs IN STRATIFIED SYSTEMS “Advances and challenges for understanding physical-biological interactions in HABs in Strati fied Environments” A Workshop Report ISSN 1538 182X GEOHAB GLOBAL ECOLOGY AND OCEANOGRAPHY OF HARMFUL ALGAL BLOOMS GEOHAB CORE RESEARCH PROJECT: HABs IN STRATIFIED SYSTEMS AN INTERNATIONAL PROGRAMME SPONSORED BY THE SCIENTIFIC COMMITTEE ON OCEANIC RESEARCH (SCOR) AND THE INTERGOVERNMENTAL OCEANOGRAPHIC COMMISSION (IOC) OF UNESCO Workshop on “ADVANCES AND CHALLENGES FOR UNDERSTANDING PHYSICAL-BIOLOGICAL INTERACTIONS IN HABs IN STRATIFIED ENVIRONMENTS” Edited by: M.A. McManus, E. Berdalet, J. Ryan, H. Yamazaki, J. S. Jaffe, O.N. Ross, H. Burchard, I. Jenkinson, F.P. Chavez This report is based on contributions and discussions by the organizers and participants of the workshop. TABLE OF CONTENTS This report may be cited as: GEOHAB 2013. Global Ecology and Oceanography of Harmful Algal Blooms, GEOHAB Core Research Project: HABs in Stratified Systems.W orkshop on "Advances and Challenges for Understanding Physical-Biological Interactions in HABs in Stratified Environments." (Eds. M.A. McManus, E. Berdalet, J. Ryan, H. Yamazaki, J.S. Jaffe, O.N. Ross, H. Burchard and F.P. Chavez) (Contributors: G. Basterretxea, D. Rivas, M.C. Ruiz and L. Seuront) IOC and SCOR, Paris and Newark, Delaware, USA, 62 pp. This document is GEOHAB Report # 11 (GEOHAB/REP/11). Copies may be obtained from: Edward R. Urban, Jr. Henrik Enevoldsen Executive Director, SCOR Intergovernmental Oceanographic Commission of College -
Microscale Ecology Regulates Particulate Organic Matter Turnover in Model Marine Microbial Communities
ARTICLE DOI: 10.1038/s41467-018-05159-8 OPEN Microscale ecology regulates particulate organic matter turnover in model marine microbial communities Tim N. Enke1,2, Gabriel E. Leventhal 1, Matthew Metzger1, José T. Saavedra1 & Otto X. Cordero1 The degradation of particulate organic matter in the ocean is a central process in the global carbon cycle, the mode and tempo of which is determined by the bacterial communities that 1234567890():,; assemble on particle surfaces. Here, we find that the capacity of communities to degrade particles is highly dependent on community composition using a collection of marine bacteria cultured from different stages of succession on chitin microparticles. Different particle degrading taxa display characteristic particle half-lives that differ by ~170 h, comparable to the residence time of particles in the ocean’s mixed layer. Particle half-lives are in general longer in multispecies communities, where the growth of obligate cross-feeders hinders the ability of degraders to colonize and consume particles in a dose dependent manner. Our results suggest that the microscale community ecology of bacteria on particle surfaces can impact the rates of carbon turnover in the ocean. 1 Department of Civil and Environmental Engineering, Massachusetts Institute of Technology, Cambridge, MA 02139, USA. 2 Department of Environmental Systems Science, ETH Zurich, Zürich 8092, Switzerland. Correspondence and requests for materials should be addressed to O.X.C. (email: [email protected]) NATURE COMMUNICATIONS | (2018) 9:2743 | DOI: 10.1038/s41467-018-05159-8 | www.nature.com/naturecommunications 1 ARTICLE NATURE COMMUNICATIONS | DOI: 10.1038/s41467-018-05159-8 earning how the composition of ecological communities the North Pacific gyre20. -
A Thesis Entitled Diel Vertical Distribution of Microcystis And
A Thesis entitled Diel Vertical Distribution of Microcystis and Associated Environmental Factors in the Western Basin of Lake Erie by Eva L. Kramer Submitted to the Graduate Faculty as partial fulfillment of the requirements for the Master of Science Degree in Biology ___________________________________________ Dr. Thomas Bridgeman, Committee Chair ___________________________________________ Dr. Timothy Davis, Committee Member ___________________________________________ Dr. Daryl Moorhead, Committee Member ___________________________________________ Dr. Cyndee Gruden, Dean College of Graduate Studies The University of Toledo December 2018 Copyright 2018, Eva Lauren Kramer This document is copyrighted material. Under copyright law, no parts of this document may be reproduced without the expressed permission of the author. An Abstract of Diel Vertical Distribution of Microcystis and Associated Environmental Factors in the Western Basin of Lake Erie by Eva L. Kramer Submitted to the Graduate Faculty as partial fulfillment of the requirements for the Master of Science Degree in Biology The University of Toledo December 2018 Harmful algal blooms comprised of the cyanobacteria Microcystis have recently caused multiple “do not drink” advisories in Ohio communities that draw their drinking water from Lake Erie, including the city of Toledo. Microcystis colonies are able to regulate their buoyancy and have a tendency to aggregate in thick scums at the water’s surface on a diel cycle under certain conditions. The city of Toledo’s drinking water intake draws water from near the bottom of the water column, thus a concentration of the bloom near the surface would present an opportunity to minimize Microcystis biomass and microcystin toxin entering the drinking water system. To better understand the vertical distribution of Microcystis over diel cycles, five temporally intensive sampling events were conducted from 2016-2017 under calm weather conditions near the drinking water intake in the western basin of Lake Erie. -
Plankton Community Composition, Organic Carbon and Thorium-234 Particle Size Distributions, and Particle Export in the Sargasso Sea
Journal of Marine Research, 67, 845–868, 2009 Plankton community composition, organic carbon and thorium-234 particle size distributions, and particle export in the Sargasso Sea by H. S. Brew1, S. B. Moran1,2, M. W. Lomas3 and A. B. Burd4 ABSTRACT Measurements of plankton community composition (eight planktonic groups), particle size- fractionated (10, 20, 53, 70, and 100-m Nitex screens) distributions of organic carbon (OC) and 234Th, and particle export of OC and 234Th are reported over a seasonal cycle (2006–2007) from the Bermuda Atlantic Time-Series (BATS) site. Results indicate a convergence of the particle size distributions of OC and 234Th during the winter-spring bloom period (January–March, 2007). The observed convergence of these particle size distributions is directly correlated to the depth-integrated abundance of autotrophic pico-eukaryotes (r ϭ 0.97, P Ͻ 0.05) and, to a lesser extent, Synechococcus (r ϭ 0.85, P ϭ 0.14). In addition, there are positive correlations between the sediment trap flux of OC and 234Th at 150 m and the depth-integrated abundance of pico-eukaryotes (r ϭ 0.94, P ϭ 0.06 for OC, and r ϭ 0.98, P Ͻ 0.05 for 234Th) and Synechococcus (r ϭ 0.95, P ϭ 0.05 for OC, and r ϭ 0.94, P ϭ 0.06 for 234Th). An implication of these observations and recent modeling studies (Richardson and Jackson, 2007) is that, although small in size, pico-plankton may influence large particle export from the surface waters of the subtropical Atlantic. -
Biological Oceanography - Legendre, Louis and Rassoulzadegan, Fereidoun
OCEANOGRAPHY – Vol.II - Biological Oceanography - Legendre, Louis and Rassoulzadegan, Fereidoun BIOLOGICAL OCEANOGRAPHY Legendre, Louis and Rassoulzadegan, Fereidoun Laboratoire d'Océanographie de Villefranche, France. Keywords: Algae, allochthonous nutrient, aphotic zone, autochthonous nutrient, Auxotrophs, bacteria, bacterioplankton, benthos, carbon dioxide, carnivory, chelator, chemoautotrophs, ciliates, coastal eutrophication, coccolithophores, convection, crustaceans, cyanobacteria, detritus, diatoms, dinoflagellates, disphotic zone, dissolved organic carbon (DOC), dissolved organic matter (DOM), ecosystem, eukaryotes, euphotic zone, eutrophic, excretion, exoenzymes, exudation, fecal pellet, femtoplankton, fish, fish lavae, flagellates, food web, foraminifers, fungi, harmful algal blooms (HABs), herbivorous food web, herbivory, heterotrophs, holoplankton, ichthyoplankton, irradiance, labile, large planktonic microphages, lysis, macroplankton, marine snow, megaplankton, meroplankton, mesoplankton, metazoan, metazooplankton, microbial food web, microbial loop, microheterotrophs, microplankton, mixotrophs, mollusks, multivorous food web, mutualism, mycoplankton, nanoplankton, nekton, net community production (NCP), neuston, new production, nutrient limitation, nutrient (macro-, micro-, inorganic, organic), oligotrophic, omnivory, osmotrophs, particulate organic carbon (POC), particulate organic matter (POM), pelagic, phagocytosis, phagotrophs, photoautotorphs, photosynthesis, phytoplankton, phytoplankton bloom, picoplankton, plankton, -
A View of Physical Mechanisms for Transporting Harmful Algal Blooms to T Massachusetts Bay ⁎ Yu Zhanga, , Changsheng Chenb, Pengfei Xueb,1, Robert C
Marine Pollution Bulletin 154 (2020) 111048 Contents lists available at ScienceDirect Marine Pollution Bulletin journal homepage: www.elsevier.com/locate/marpolbul A view of physical mechanisms for transporting harmful algal blooms to T Massachusetts Bay ⁎ Yu Zhanga, , Changsheng Chenb, Pengfei Xueb,1, Robert C. Beardsleyc, Peter J.S. Franksd a College of Marine Sciences, Shanghai Ocean University, Shanghai 201306, PR China b School for Marine Science and Technology, University of Massachusetts-Dartmouth, New Bedford, MA 02744, USA c Department of Physical Oceanography, Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA d Integrative Oceanography Division, Scripps Institution of Oceanography, University of California San Diego, La Jolla, CA 92093, USA ARTICLE INFO ABSTRACT Keywords: Physical dynamics of Harmful Algal Blooms in Massachusetts Bay in May 2005 and 2008 were examined by the Harmful algal bloom simulated results. Reverse particle-tracking experiments suggest that the toxic phytoplankton mainly originated Massachusetts Bay from the Bay of Fundy in 2005 and the western Maine coastal region and its local rivers in 2008. Mechanism Ocean modeling studies suggest that the phytoplankton were advected by the Gulf of Maine Coastal Current (GMCC). In 2005, Lagrangian flow Nor'easters increased the cross-shelf surface elevation gradient over the northwestern shelf. This intensified the Eastern and Western MCC to form a strong along-shelf current from the Bay of Fundy to Massachusetts Bay. In 2008, both Eastern and Western MCC were established with a partial separation around Penobscot Bay before the outbreak of the bloom. The northeastward winds were too weak to cancel or reverse the cross-shelf sea surface gradient, so that the Western MCC carried the algae along the slope into Massachusetts Bay. -
Open Ocean Dead-Zones in the Tropical J I Northeast Atlantic
Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | Biogeosciences Discuss., 11, 17391–17411, 2014 www.biogeosciences-discuss.net/11/17391/2014/ doi:10.5194/bgd-11-17391-2014 BGD © Author(s) 2014. CC Attribution 3.0 License. 11, 17391–17411, 2014 This discussion paper is/has been under review for the journal Biogeosciences (BG). Open ocean Please refer to the corresponding final paper in BG if available. dead-zones Open ocean dead-zone in the tropical J. Karstensen et al. North Atlantic Ocean Title Page 1 1 1 1 1 2 J. Karstensen , B. Fiedler , F. Schütte , P. Brandt , A. Körtzinger , G. Fischer , Abstract Introduction R. Zantopp1, J. Hahn1, M. Visbeck1, and D. Wallace3 Conclusions References 1GEOMAR Helmholtz Centre for Ocean Research Kiel, Kiel, Germany Tables Figures 2Faculty of Geosciences and MARUM, University of Bremen, Bremen, Germany 3Halifax Marine Research Institute (HMRI), Halifax, Canada J I Received: 3 November 2014 – Accepted: 13 November 2014 – Published: 12 December 2014 J I Correspondence to: J. Karstensen ([email protected]) Back Close Published by Copernicus Publications on behalf of the European Geosciences Union. Full Screen / Esc Printer-friendly Version Interactive Discussion 17391 Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | Abstract BGD The intermittent appearances of low oxygen environments are a particular thread for marine ecosystems. Here we present first observations of unexpected low (< 11, 17391–17411, 2014 2 µmolkg−1) oxygen environments in the open waters of the eastern tropical North −1 5 Atlantic, a region where typically oxygen concentration does not fall below 40 µmolkg . Open ocean The low oxygen zones are created just below the mixed-layer, in the euphotic zone of dead-zones high productive cyclonic and anticyclonic-modewater eddies. -
Harmful Algal Bloom Response Program
What are HABs? • Blue-green algae are bacteria that grow in water, contain chlorophyll, and can photosynthesize. They are not a new occurrence. WHEN IN DOUBT, STAY OUT! Kansas Department of Health • When these bacteria reproduce rapidly, For additional information: and Environment it can create a Harmful Algal Bloom (HAB). Please visit • HABs can sometimes produce toxins www.kdheks.gov/algae-illness. Harmful that affect people, pets, livestock, and Or call the KDHE HAB Hotline at wildlife. The toxins can affect the skin, 785-296-1664. liver, and nervous system. Algal Bloom • People and animals may be exposed to toxins via ingestion, skin contact, or Response inhalation of contaminated water. Program • The most common human health effects from HABs can include vomiting, diarrhea, skin rashes, eye irritation, and respiratory symptoms. • Boiling water does not remove or Department of Health inactivate toxins from blue-green algae, and Environment and there is no known antidote. • Animal deaths due to HAB toxins have Department of Health been documented, so: and Environment When in doubt, stay out! To protect and improve the health and environment of all Kansans. How else is KDHE working to What causes HABs? HAB Advisory Levels prevent HABs? Blue-green algae are a natural part of water- Threshold Levels based ecosystems. They become a problem Harmful Algal Blooms thrive in the presence when nutrients (phosphorus and nitrogen) are Watch Warning Closure of excess nutrients such as nitrogen and present in concentrations above what would phosphorus. Thus, KDHE continually works to occur naturally. Under these conditions, algae blue green reduce nutrient input and improve overall can grow very quickly to extreme numbers, cell counts 80,000 250,000 10,000,000 water quality through a series of interrelated resulting in a Harmful Algal Bloom. -
Diffuse Pollution, Degraded Waters Emerging Policy Solutions
Diffuse Pollution, Degraded Waters Emerging Policy Solutions Policy HIGHLIGHTS Diffuse Pollution, Degraded Waters Emerging Policy Solutions “OECD countries have struggled to adequately address diffuse water pollution. It is much easier to regulate large, point source industrial and municipal polluters than engage with a large number of farmers and other land-users where variable factors like climate, soil and politics come into play. But the cumulative effects of diffuse water pollution can be devastating for human well-being and ecosystem health. Ultimately, they can undermine sustainable economic growth. Many countries are trying innovative policy responses with some measure of success. However, these approaches need to be replicated, adapted and massively scaled-up if they are to have an effect.” Simon Upton – OECD Environment Director POLICY H I GH LI GHT S After decades of regulation and investment to reduce point source water pollution, OECD countries still face water quality challenges (e.g. eutrophication) from diffuse agricultural and urban sources of pollution, i.e. pollution from surface runoff, soil filtration and atmospheric deposition. The relative lack of progress reflects the complexities of controlling multiple pollutants from multiple sources, their high spatial and temporal variability, the associated transactions costs, and limited political acceptability of regulatory measures. The OECD report Diffuse Pollution, Degraded Waters: Emerging Policy Solutions (OECD, 2017) outlines the water quality challenges facing OECD countries today. It presents a range of policy instruments and innovative case studies of diffuse pollution control, and concludes with an integrated policy framework to tackle this challenge. An optimal approach will likely entail a mix of policy interventions reflecting the basic OECD principles of water quality management – pollution prevention, treatment at source, the polluter pays and the beneficiary pays principles, equity, and policy coherence. -
Wetland Eutrophication: Early Warning Biogeochemical Indicators1 Alan L
SL 304 Wetland Eutrophication: Early Warning Biogeochemical Indicators1 Alan L. Wright2 Florida’s diverse wetlands provide valuable functions, The most evident results of the nutrient inputs is the including water storage, recreation, and a habitat for replacement of the primary native sawgrass vegetation with wildlife. Most famous of these wetlands is the Everglades, cattails. This in turn has altered the ecosystem considerably. a vast wetland historically encompassing most of Florida Changes include increases in soil accumulation, water south of Lake Okeechobee. Events in the last hundred years, quality, wildlife patterns, and other environmental effects. including urbanization and agriculture, have reduced the The shift from native vegetation to cattails takes many years size of the Everglades considerably, with remnants being to occur, but it may be possible to detect changes to the the heavily-managed water conservation areas (WCAs), Everglades before vegetation can respond, thus enabling stormwater treatment wetlands, and a National Refuge, corrective action to be undertaken before more irreparable Forest, and Park. damage occurs. The objective of this document is to describe effects of Many soil and microbial properties are very sensitive to nutrients in the Everglades and identify sensitive early- eutrophication, which is the process by which nutrient levels warning indicators of ecological changes. This information are increased resulting in significant ecological effects to would be of interest to water managers and the general wetlands. By identifying these sensitive factors and under- public. standing how they respond to eutrophication, we can better protect the Everglades by utilizing these factors as early The Everglades was drained to improve water control warning indicators before the more long-term ecosystem and provide land for urbanization and agriculture. -
Harmful Algal Bloom Online Resources
Harmful Algal Bloom Online Resources General Information • CDC Harmful Algal Bloom-Associated Illnesses Website • CDC Harmful Algal Blooms Feature • EPA CyanoHABs Website • EPA Harmful Algal Blooms & Cyanobacteria Research Website • NOAA Harmful Algal Bloom Website • NOAA Harmful Algal Bloom and Hypoxia Research Control Act Harmful Algal Bloom Monitoring and Tracking • EPA Cyanobacteria Assessment Network (CyAN) Project • NCCOS Harmful Algal Bloom Research Website • NOAA Harmful Algal Bloom Forecasts • USGS Summary of Cyanobacteria Monitoring and Assessments in USGS Water Science Centers • WHO Toxic Cyanobacteria in water: A guide to their public health consequences, monitoring, and management Harmful Algal Blooms and Drinking Water • AWWA Assessment of Blue-Green Algal Toxins in Raw and Finished Drinking Water • EPA Guidelines and Recommendations • EPA Harmful Algal Bloom & Drinking Water Treatment Website • EPA Algal Toxin Risk Assessment and Management Strategic Plan for Drinking Water Document • USGS Drinking Water Exposure to Chemical and Pathogenic Contaminants: Algal Toxins and Water Quality Website Open Water Resources • CDC Healthy Swimming Website - Oceans, Lakes, Rivers • EPA State Resources Website • EPA Beach Act Website • EPA Beach Advisory and Closing On-line Notification (BEACON) • USG Guidelines for Design and Sampling for Cyanobacterial Toxin and Taste-and-Odor Studies in Lakes and Reservoirs • NALMS Inland HAB Program • NOAA Illinois-Indiana and Michigan Sea Grant Beach Manager’s Manual • USGS Field and Laboratory Guide