Reassessment 2013: Assessing Progress Made Since 2008
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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. -
Hypoxia Infographic
Understanding HYP XIA Hypoxia is an environmental phenomenon where the concentration of dissolved oxygen in the water column decreases to a level that can no longer 1 support living aquatic organisms. The level is often considered to be 2 mg O2 per liter of water or lower. Hypoxic and anoxic (no oxygen) waters have existed throughout geologic time, but their occurrence in shallow coastal and estuarine areas appears to be increasing as a result of human activities. 2 What causes hypoxia? In 2015, scientists determined the Gulf of Mexico dead zone to be 6,474 square miles, which is an area about the size of Connecticut and Rhode Island combined. 3 Major events leading to the formation of hypoxia in the Gulf of Mexico include: Coastal Hypoxia and Eutrophication Sunlight Watershed Areas of anthropogenically-influenced n> In the past century, Hypoxia has become a global concern with estuarine and coastal hypoxia. 550 over 550 coastal areas identified as experiencing this issue. 4 Runoff and nutrient 1 loading of the Mississippi River. Nutrient-rich water from the Mississippi River forms 1960 a surface lens. 1970 Combined, Dead Zones 1980 cover 4x the area of the 1990 Great Lakes. % 2000 Nutrient-enhanced 4 2 primary production, Only a small fraction of the 550-plus Number of dead zones has approximately Today, there is currently about 1,148,000 km2 or eutrophication. hypoxia zones exhibited any signs doubled each decade since the 1960’s. 5 of seabed covered by Oxygen Minimum Phytoplankton growth of improvement. 5 Zones (OMZs) (<0.5 ml of O /liter) 5 is fueled by nutrients. -
Gulf of Mexico Hypoxia Monitoring Strategy
Gulf of Mexico Hypoxia Monitoring Strategy Hypoxia Zone Areal Extent (km2) Interpolation Observations Data Analysis Workshop Steering Committee Trevor Meckley, Alan Lewitus, A White Paper by the Steering Committee of the: Dave Scheurer, Dave Hilmer NOAA National Ocean Service, National 6th Annual NOAA/NGI Hypoxia Research Centers of Coastal Ocean Science Coordination Workshop: Establishing a Steve Ashby Cooperative Hypoxic Zone Monitoring Program Northern Gulf Institute convened by the NOAA National Centers for Steve DiMarco Texas A&M University Coastal Ocean Science and Northern Gulf Institute Steve Giordano on 12-13 September 2016 at the Mississippi State NOAA National Marine Fisheries Service University Science and Technology Center at Rick Greene NASA's Stennis Space Center in Mississippi. EPA Office of Research and Development Stephan Howden University of Southern Mississippi Barb Kirkpatrick Gulf of Mexico Coastal Ocean Observing System Troy Pierce EPA Gulf of Mexico Program Nancy Rabalais Louisiana Universities Marine Consortium Rick Raynie Louisiana Coastal Protection and Restoration Authority Mike Woodside USGS National Water Quality Program Abstract The Gulf of Mexico Hypoxia Monitoring Strategy is a resource to inform the proceedings of the 6th Annual NOAA/NGI Hypoxia Research Coordination Workshop: Establishing a Cooperative Hypoxic Zone Monitoring Program. It provides a framework for a cooperative hypoxia monitoring program based on programmatic and financial requirements that are designed to meet management needs. The Monitoring Strategy includes sections on management drivers, current monitoring capabilities and gaps, and projected programmatic, data, and financial requirements based on the input of multiple partners and the responses from a survey of modelers currently applying deterministic 3D time variable models to Gulf hypoxia assessment and prediction. -
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. -
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. -
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. -
Zooplankton Community Response to Seasonal Hypoxia: a Test of Three Hypotheses
diversity Article Zooplankton Community Response to Seasonal Hypoxia: A Test of Three Hypotheses Julie E. Keister *, Amanda K. Winans and BethElLee Herrmann School of Oceanography, University of Washington, Box 357940, Seattle, WA 98195, USA; [email protected] (A.K.W.); [email protected] (B.H.) * Correspondence: [email protected] Received: 7 November 2019; Accepted: 28 December 2019; Published: 1 January 2020 Abstract: Several hypotheses of how zooplankton communities respond to coastal hypoxia have been put forward in the literature over the past few decades. We explored three of those that are focused on how zooplankton composition or biomass is affected by seasonal hypoxia using data collected over two summers in Hood Canal, a seasonally-hypoxic sub-basin of Puget Sound, Washington. We conducted hydrographic profiles and zooplankton net tows at four stations, from a region in the south that annually experiences moderate hypoxia to a region in the north where oxygen remains above hypoxic levels. The specific hypotheses tested were that low oxygen leads to: (1) increased dominance of gelatinous relative to crustacean zooplankton, (2) increased dominance of cyclopoid copepods relative to calanoid copepods, and (3) overall decreased zooplankton abundance and biomass at hypoxic sites compared to where oxygen levels are high. Additionally, we examined whether the temporal stability of community structure was decreased by hypoxia. We found evidence of a shift toward more gelatinous zooplankton and lower total zooplankton abundance and biomass at hypoxic sites, but no clear increase in the dominance of cyclopoid relative to calanoid copepods. We also found the lowest variance in community structure at the most hypoxic site, in contrast to our prediction. -
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. -
Hypoxia the Gulf of Mexico’S Summertime Foe
Louisiana Coastal Wetlands Planning, Protection and Restoration News September 2004 Number 26 HYPOXIA THE GULF OF MEXICO’S SUMMERTIME FOE More Nitrogen Upstream, Fewer Filters Downstream Caernarvon: A Case Study WaterMarks Interview: John Day, LSU www.lacoast.gov September 2004 Number 26 WaterMarks is published three times a Louisiana Coastal Wetlands Planning, Protection and Restoration News year by the Louisiana Coastal Wetlands Conservation and Restoration Task Force to communicate news and issues Contents of interest related to the Coastal Wetlands Planning, Protection and Restoration Act of 1990. This legislation 3 Hypoxia: funds wetlands enhancement projects The Gulf of Mexico’s Summertime Foe nationwide, designating approximately $50 million annually for work in More Nitrogen Upstream, Louisiana. The state contributes 6 Fewer Filters Downstream 15 percent of the total cost of the project. Can Wetlands Restoration 8 Revitalize Offshore Waters? Caernarvon: 10 A Case Study What Lies Ahead 12 for the Dead Zone? Please address all questions, comments and changes of address to: WaterMarks Interview: James D. Addison 14 John Day, LSU WaterMarks Editor New Orleans District US Army Corps of Engineers P.O. Box 60267 Special thanks to Doug Daigle, Mississippi River Basin Alliance; Dugan Sabins, New Orleans, LA 70160-0267 (504) 862-2201 Louisiana State Hypoxia Committee; Ken Teague, U.S. Environmental Protection Agency; and Robert Twilley, Louisiana State University, for their assistance with e-mail: this issue of WaterMarks. [email protected] For more information about Louisiana’s coastal wetlands and the efforts planned and under way to ensure their survival, check out these sites on the web: www.lacoast.gov www.btnep.org www.saveLAwetlands.org About the Cover Blue Runners, a common Gulf Subscribe species, have the ability to escape To receive WaterMarks, e-mail [email protected] from waters with low oxygen con- For current meetings, events, and other news concerning Louisiana’s coastal tent. -
The Economics of Dead Zones: Causes, Impacts, Policy Challenges, and a Model of the Gulf of Mexico Hypoxic Zone S
58 The Economics of Dead Zones: Causes, Impacts, Policy Challenges, and a Model of the Gulf of Mexico Hypoxic Zone S. S. Rabotyagov*, C. L. Klingy, P. W. Gassmanz, N. N. Rabalais§ ô and R. E. Turner Downloaded from Introduction The BP Deepwater Horizon oil spill in the Gulf of Mexico in 2010 increased public awareness and http://reep.oxfordjournals.org/ concern about long-term damage to ecosystems, and casual readers of the news headlines may have concluded that the spill and its aftermath represented the most significant and enduring environmental threat to the region. However, the region faces other equally challenging threats including the large seasonal hypoxic, or “dead,” zone that occurs annually off the coast of Louisiana and Texas. Even more concerning is the fact that such dead zones have been appearing worldwide at proliferating rates (Conley et al. 2011; Diaz and Rosenberg 2008). Nutrient over- enrichment is the main cause of these dead zones, and nutrient-fed hypoxia is now widely at Iowa State University on January 27, 2014 considered an important threat to the health of aquatic ecosystems (Doney 2010). The rather alarming term dead zone is surprisingly appropriate: hypoxic regions exhibit oxygen levels that are too low to support many aquatic organisms including commercially desirable species. While some dead zones are naturally occurring, their number, size, and *School of Environmental and Forest Sciences, University of Washington, Seattle, Washington, USA; e-mail: [email protected] yCenter for Agricultural and Rural Development, -
Coupling and Decoupling of High Biomass Phytoplankton Production and Hypoxia in a Highly Dynamic Coastal System: the Changjiang (Yangtze River) Estuary
fmars-07-00259 May 26, 2020 Time: 17:51 # 1 ORIGINAL RESEARCH published: 28 May 2020 doi: 10.3389/fmars.2020.00259 Coupling and Decoupling of High Biomass Phytoplankton Production and Hypoxia in a Highly Dynamic Coastal System: The Changjiang (Yangtze River) Estuary Feng Zhou1,2*, Fei Chai1,3*, Daji Huang1, Mark Wells3,1, Xiao Ma1, Qicheng Meng1, Huijie Xue3,4, Jiliang Xuan1, Pengbin Wang1,5, Xiaobo Ni1, Qiang Zhao6, Chenggang Liu1,5, Jilan Su5 and Hongliang Li1 1 State Key Laboratory of Satellite Ocean Environment Dynamics, Second Institute of Oceanography, Ministry of Natural Resources, Hangzhou, China, 2 School of Oceanography, Shanghai Jiao Tong University, Shanghai, China, 3 School Edited by: of Marine Science, University of Maine, Orono, ME, United States, 4 State Key Laboratory of Tropical Oceanography, South Marta Marcos, China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou, China, 5 Key Laboratory of Marine University of the Balearic Islands, Ecosystem Dynamics, Second Institute of Oceanography, Ministry of Natural Resources, Hangzhou, China, 6 Ningbo Marine Spain Environment Monitoring Center Station, Ministry of Natural Resources, Ningbo, China Reviewed by: Sabine Schmidt, The global increase in coastal hypoxia over the past decades has resulted from a Centre National de la Recherche Scientifique (CNRS), France considerable rise in anthropogenically-derived nutrient loading. The spatial relationship Antonio Olita, between surface phytoplankton production and subsurface hypoxic zones often can Italian National Research Council (CNR), Italy be explained by considering the oceanographic conditions associated with basin size, *Correspondence: shape, or bathymetry, but that is not the case where nutrient-enriched estuarine Feng Zhou waters merge into complex coastal circulation systems. -
Scientific Assessment of Hypoxia in U.S. Coastal Waters
Scientific Assessment of Hypoxia in U.S. Coastal Waters 0 Dissolved oxygen (mg/L) 6 0 Depth (m) 80 32 Salinity 34 Interagency Working Group on Harmful Algal Blooms, Hypoxia, and Human Health September 2010 This document should be cited as follows: Committee on Environment and Natural Resources. 2010. Scientific Assessment of Hypoxia in U.S. Coastal Waters. Interagency Working Group on Harmful Algal Blooms, Hypoxia, and Human Health of the Joint Subcommittee on Ocean Science and Technology. Washington, DC. Acknowledgements: Many scientists and managers from Federal and state agencies, universities, and research institutions contributed to the knowledge base upon which this assessment depends. Many thanks to all who contributed to this report, and special thanks to John Wickham and Lynn Dancy of NOAA National Centers for Coastal Ocean Science for their editing work. Cover and Sidebar Photos: Background Cover and Sidebar: MODIS satellite image courtesy of the Ocean Biology Processing Group, NASA Goddard Space Flight Center. Cover inset photos from top: 1) CTD rosette, EPA Gulf Ecology Division; 2) CTD profile taken off the Washington coast, project funded by Bonneville Power Administration and NOAA Fisheries; Joseph Fisher, OSU, was chief scientist on the FV Frosti; data were processed and provided by Cheryl Morgan, OSU); 3) Dead fish, Christopher Deacutis, Rhode Island Department of Environmental Management; 4) Shrimp boat, EPA. Council on Environmental Quality Office of Science and Technology Policy Executive Office of the President Dear Partners and Friends in our Ocean and Coastal Community, We are pleased to transmit to you this report, Scientific Assessment ofHypoxia in u.s.