Fish in the Zone
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Coastal Processes and Causes of Shoreline Erosion and Accretion Causes of Shoreline Erosion and Accretion
Coastal Processes and Causes of Shoreline Erosion and Accretion and Accretion Erosion Causes of Shoreline Heather Weitzner, Great Lakes Coastal Processes and Hazards Specialist Photo by Brittney Rogers, New York Sea Grant York Photo by Brittney Rogers, New New York Sea Grant Waves breaking on the eastern Lake Ontario shore. Wayne County Cooperative Extension A shoreline is a dynamic environment that evolves under the effects of both natural 1581 Route 88 North and human influences. Many areas along New York’s shorelines are naturally subject Newark, NY 14513-9739 315.331.8415 to erosion. Although human actions can impact the erosion process, natural coastal processes, such as wind, waves or ice movement are constantly eroding and/or building www.nyseagrant.org up the shoreline. This constant change may seem alarming, but erosion and accretion (build up of sediment) are natural phenomena experienced by the shoreline in a sort of give and take relationship. This relationship is of particular interest due to its impact on human uses and development of the shore. This fact sheet aims to introduce these processes and causes of erosion and accretion that affect New York’s shorelines. Waves New York’s Sea Grant Extension Program Wind-driven waves are a primary source of coastal erosion along the Great provides Equal Program and Lakes shorelines. Factors affecting wave height, period and length include: Equal Employment Opportunities in 1. Fetch: the distance the wind blows over open water association with Cornell Cooperative 2. Length of time the wind blows Extension, U.S. Department 3. Speed of the wind of Agriculture and 4. -
Mechanisms Contributing to the Deep Chlorophyll Maximum in Lake Superior
Michigan Technological University Digital Commons @ Michigan Tech Dissertations, Master's Theses and Master's Dissertations, Master's Theses and Master's Reports - Open Reports 2011 Mechanisms contributing to the deep chlorophyll maximum in Lake Superior Marcel L. Dijkstra Michigan Technological University Follow this and additional works at: https://digitalcommons.mtu.edu/etds Part of the Civil and Environmental Engineering Commons Copyright 2011 Marcel L. Dijkstra Recommended Citation Dijkstra, Marcel L., "Mechanisms contributing to the deep chlorophyll maximum in Lake Superior", Master's Thesis, Michigan Technological University, 2011. https://doi.org/10.37099/mtu.dc.etds/231 Follow this and additional works at: https://digitalcommons.mtu.edu/etds Part of the Civil and Environmental Engineering Commons MECHANISMS CONTRIBUTING TO THE DEEP CHLOROPHYLL MAXIMUM IN LAKE SUPERIOR By Marcel L. Dijkstra A THESIS Submitted in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE (Environmental Engineering) MICHIGAN TECHNOLOGICAL UNIVERSITY 2011 © 2011 Marcel L. Dijkstra This thesis, “Mechanisms Contributing to the Deep Chlorophyll Maximum in Lake Superior,” is hereby approved in partial fulfillment of the requirements for the Degree of MASTER OF SCIENCE IN ENVIRONMENTAL ENGINEERING. Department of Civil and Environmental Engineering Signatures: Thesis Advisor Dr. Martin Auer Department Chair Dr. David Hand Date Contents List of Figures ...................................................................................................... -
Glossary of Terms Used in Lake Almanor Water Quality Reports
Glossary of Terms Used in Lake Almanor Water Quality Reports Algae. Algae (the plural form of alga) are one-celled plants that do not have a central vascular system for respiration and nutrient flow. Usually algae are very small, microscopic size. However, some are much larger, such a sea lettuce, but are still algae because each cell can survive on its own and there is no central vascular system. Various estimates indicate there are over 70,000 species of algae that inhabit fresh water. “Blue green algae”. These are more correctly Cyanobacteria, and not algae. The chlorophyll in each cell is spread throughout the entire cell. This contrasts with a true algae cell which has a firmer wall, like a pea, and the chlorophyll is in sacks called chloroplasts. Most of the harmful algae bloom (HAB) problems in US lakes are caused by only about 30 species of cyanobacteria. Cyanobacteria are found in many lakes and can destroy a lake's utility by producing potent toxins (cyanotoxins), taste, and odor in the lake water. The toxins can kill or harm humans that contact the lake water. Anoxic. Anoxic water has little or no measurable dissolved oxygen. Bloom. A "bloom" usually refers to excessive algal growth. Cladocera. Relatively large members of the zooplankton, such as Daphnia (water fleas), that are primarily filter feeders that eat algae and other phytoplankton. Coldwater Fishery. Waters in which the maximum mean monthly temperature generally does not exceed a certain value and, when other ecological factors are favorable, are capable of supporting year-round populations of cold water aquatic life, such as trout. -
Pond and Lake Ecosystems a Pond Or Lake Ecosystem Includes Biotic
Pond and Lake Ecosystems A pond or lake ecosystem includes biotic (living) plants, animals and micro-organisms, as well as abiotic (nonliving) physical and chemical interactions. Pond and lake ecosystems are a prime example of lentic ecosystems. Lentic refers to stationary or relatively still water, from the Latin lentus, which means sluggish. A typical lake has distinct zones of biological communities linked to the physical structure of the lake. (Figure below) The littoral zone is the near shore area where sunlight penetrates all the way to the sediment and allows aquatic plants (macrophytes) to grow. Light levels of about 1% or less of surface values usually define this depth. The 1% light level also defines the euphotic zone of the lake, which is the layer from the surface down to the depth where light levels become too low for photosynthesizers. In most lakes, the sunlit euphotic zone occurs within the epilimnion. However, in unusually transparent lakes, photosynthesis may occur well below the thermocline into the perennially cold hypolimnion. For example, in western Lake Superior near Duluth, MN, summertime algal photosynthesis and growth can persist to depths of at least 25 meters, while the mixed layer, or epilimnion, only extends down to about 10 meters. Ultra-oligotrophic Lake Tahoe, CA/NV, is so transparent that algal growth historically extended to over 100 meters, though its mixed layer only extends to about 10 meters in summer. Unfortunately, inadequate management of the Lake Tahoe basin since about 1960 has led to a significant loss of transparency due to increased algal growth and increased sediment inputs from stream and shoreline erosion. -
Estimates of Hypolimnetic Oxygen Deficits in Ponds
Aquacullure and Fisheries Management 1989, 20, 167-172 Estimates of hypolimnetic oxygen deficits in ponds W. Y. B. CHANG Center for Great Lakes and Aquatic Sciences, University of Michigan, Ann Arbor, Michigan, USA Abstract. Shallow tropical integrated culture ponds in the Pearl River Delta. China, have been found to stratify almost daily, with high organic loadings and dense algal growth. The dissolved oxygen (DO) concentration is super-saturated in the epilimnion and is under 2 mg/l in the hypolimnion (>lm). The compensation depth corresponds to twice the Secchi disk depth ranging from 50 to 80cm. As a result, little or no net oxygen is produced in the hypolimnion (> 1 m). The low DO concentration in the hypolimnion causes organic materials, such as unused organic wastes and senescent algae cells, to be incompletely oxidized, since the rate of oxygen consumption by oxidable matter in water is dependent on the dissolved oxygen concentration in water. This material becomes the source of hypolimnetic oxygen deficits (HOD) which can drive whole pond DO to a dangerously low level, should sudden destratification occur. An improved estimate of hypolimnetic oxygen deficits is introduced in this article, and the advantages of this method are discussed. Introduction Oxygen is an important parameter in fish culture, and adequate levels of dissolved oxygen (DO) are essential for maintaining optimum fish growth. Inadequate dissolved oxygen and poor water quality are frequently found in ponds receiving organic wastes and can lead to many serious problems for fish culture in ponds. Problems of low dissolved oxygen are particularly prevalent in ponds during the night and early morning when there are high densities of fish and large additions of organic wastes and feeds (Schroeder 1974; Boyd 1982; Chang 1986). -
Hydrogeology of Near-Shore Submarine Groundwater Discharge
Hydrogeology and Geochemistry of Near-shore Submarine Groundwater Discharge at Flamengo Bay, Ubatuba, Brazil June A. Oberdorfer (San Jose State University) Matthew Charette, Matthew Allen (Woods Hole Oceanographic Institution) Jonathan B. Martin (University of Florida) and Jaye E. Cable (Louisiana State University) Abstract: Near-shore discharge of fresh groundwater from the fractured granitic rock is strongly controlled by the local geology. Freshwater flows primarily through a zone of weathered granite to a distance of 24 m offshore. In the nearshore environment this weathered granite is covered by about 0.5 m of well-sorted, coarse sands with sea water salinity, with an abrupt transition to much lower salinity once the weathered granite is penetrated. Further offshore, low-permeability marine sediments contained saline porewater, marking the limit of offshore migration of freshwater. Freshwater flux rates based on tidal signal and hydraulic gradient analysis indicate a fresh submarine groundwater discharge of 0.17 to 1.6 m3/d per m of shoreline. Dissolved inorganic nitrogen and silicate were elevated in the porewater relative to seawater, and appeared to be a net source of nutrients to the overlying water column. The major ion concentrations suggest that the freshwater within the aquifer has a short residence time. Major element concentrations do not reflect alteration of the granitic rocks, possibly because the alteration occurred prior to development of the current discharge zones, or from elevated water/rock ratios. Introduction While there has been a growing interest over the last two decades in quantifying the discharge of groundwater to the coastal zone, the majority of studies have been carried out in aquifers consisting of unlithified sediments or in karst environments. -
Variability in Epilimnion Depth Estimations in Lakes Harriet L
https://doi.org/10.5194/hess-2020-222 Preprint. Discussion started: 10 June 2020 c Author(s) 2020. CC BY 4.0 License. Variability in epilimnion depth estimations in lakes Harriet L. Wilson1, Ana I. Ayala2, Ian D. Jones3, Alec Rolston4, Don Pierson2, Elvira de Eyto5, Hans- Peter Grossart6, Marie-Elodie Perga7, R. Iestyn Woolway1, Eleanor Jennings1 5 1Center for Freshwater and Environmental Studies, Dundalk Institute of Technology, Dundalk, Ireland 2Department of Ecology and Genetics, Limnology, Uppsala University, Uppsala, Sweden 3Biological and Environmental Sciences, Faculty of Natural Sciences, University of Stirling, Stirling, UK 4An Fóram Uisce, National Water Forum, Ireland 5Marine Institute, Furnace, Newport, Co. Mayo, Ireland 10 6Institute for Biochemistry and Biology, Potsdam University, Potsdam, Germany 7University of Lausanne, Faculty of Geoscience and Environment, CH 1015 Lausanne, Switzerland Correspondence to: Harriet L. Wilson ([email protected]) 15 Abstract. The “epilimnion” is the surface layer of a lake typically characterised as well-mixed and is decoupled from the “metalimnion” due to a rapid change in density. The concept of the epilimnion, and more widely, the three-layered structure of a stratified lake, is fundamental in limnology and calculating the depth of the epilimnion is essential to understanding many physical and ecological lake processes. Despite the ubiquity of the term, however, there is no objective or generic approach for defining the epilimnion and a diverse number of approaches prevail in the literature. Given the increasing 20 availability of water temperature and density profile data from lakes with a high spatio-temporal resolution, automated calculations, using such data, are particularly common, and have vast potential for use with evolving long-term, globally measured and modelled datasets. -
Lake Ecology
Fundamentals of Limnology Oxygen, Temperature and Lake Stratification Prereqs: Students should have reviewed the importance of Oxygen and Carbon Dioxide in Aquatic Systems Students should have reviewed the video tape on the calibration and use of a YSI oxygen meter. Students should have a basic knowledge of pH and how to use a pH meter. Safety: This module includes field work in boats on Raystown Lake. On average, there is a death due to drowning on Raystown Lake every two years due to careless boating activities. You will very strongly decrease the risk of accident when you obey the following rules: 1. All participants in this field exercise will wear Coast Guard certified PFDs. (No exceptions for teachers or staff). 2. There is no "horseplay" allowed on boats. This includes throwing objects, splashing others, rocking boats, erratic operation of boats or unnecessary navigational detours. 3. Obey all boating regulations, especially, no wake zone markers 4. No swimming from boats 5. Keep all hands and sampling equipment inside of boats while the boats are moving. 6. Whenever possible, hold sampling equipment inside of the boats rather than over the water. We have no desire to donate sampling gear to the bottom of the lake. 7. The program director has final say as to what is and is not appropriate safety behavior. Failure to comply with the safety guidelines and the program director's requests will result in expulsion from the program and loss of Field Station privileges. I. Introduction to Aquatic Environments Water covers 75% of the Earth's surface. We divide that water into three types based on the salinity, the concentration of dissolved salts in the water. -
Indirect Consequences of Hypolimnetic Hypoxia on Zooplankton Growth in a Large Eutrophic Lake
Vol. 16: 217–227, 2012 AQUATIC BIOLOGY Published September 5 doi: 10.3354/ab00442 Aquat Biol Indirect consequences of hypolimnetic hypoxia on zooplankton growth in a large eutrophic lake Daisuke Goto1,8,*, Kara Lindelof2,3, David L. Fanslow4, Stuart A. Ludsin4,5, Steven A. Pothoven4, James J. Roberts2,6, Henry A. Vanderploeg4, Alan E. Wilson2,7, Tomas O. Höök1,2 1Department of Forestry and Natural Resources, Purdue University, West Lafayette, Indiana 47907, USA 2Cooperative Institute for Limnology and Ecosystems Research, University of Michigan, Ann Arbor, Michigan 48108, USA 3Department of Environmental Sciences, University of Toledo, Toledo, Ohio 43606, USA 4Great Lakes Environmental Research Laboratory, National Oceanic and Atmospheric Administration, Ann Arbor, Michigan 48108, USA 5Aquatic Ecology Laboratory, Department of Evolution, Ecology and Organismal Biology, The Ohio State University, Columbus, Ohio 43212, USA 6Colorado State University, Department of Fish, Wildlife and Conservation Biology, Fort Collins, Colorado 80523, USA 7Department of Fisheries and Allied Aquacultures, Auburn University, Auburn, Alabama 36849, USA 8School of Biological Sciences, University of Nebraska Lincoln, Lincoln, Nebraska 68588, USA ABSTRACT: Diel vertical migration (DVM) of some zooplankters in eutrophic lakes is often com- pressed during peak hypoxia. To better understand the indirect consequences of seasonal hypolimnetic hypoxia, we integrated laboratory-based experimental and field-based observa- tional approaches to quantify how compressed DVM can affect growth of a cladoceran, Daphnia mendotae, in central Lake Erie, North America. To evaluate hypoxia tolerance of D. mendotae, we conducted a survivorship experiment with varying dissolved oxygen concentrations, which −1 demonstrated high sensitivity of D. mendotae to hypoxia (≤2 mg O2 l ), supporting the field obser- vations of their behavioral avoidance of the hypoxic hypolimnion. -
Freshwater Ecosystem: Part 2
Paper : 12 Principles of Ecology Module : 22 Types of Ecosystems: Aquatic Ecosystem-Fresh Water Ecosystem: Part 2 Development Team Principal Investigator : Prof. Neeta Sehgal Department of Zoology, University of Delhi Co-Principal Investigator : Prof. D.K. Singh Department of Zoology, University of Delhi Paper Coordinator : Prof. D.K. Singh Department of Zoology, University of Delhi Content Writer : Dr. Sushma Bhardwaj , Deshbandhu College, DU Ms. Harshita Mishra, Research Scholar, DU Content Reviewer : Prof. K.S. Rao Department of Botany, University of Delhi 1 Principles of Ecology ZOOLOGY Aquatic Ecosystem: Freshwater Ecosystem: Part 2 Description of Module Subject Name ZOOLOGY Paper Name Zool 12 Principles of Ecology Module Name/Title Types of Ecosystems: Aquatic Ecosystem Module Id M22: Aquatic Ecosystem: Freshwater Ecosystem: Part 2 Keywords Lentic, lotic, community, lake, temperate lake, zone, eutrophy, Langmuir circulation Contents 1. Learning Objectives 2. Introduction 3. The Lentic Aquatic System 3.1. Zonation in Lentic Systems 3.2. Characteristics of Lentic Ecosystem 3.3. Lentic Community 3.3.1. Communities of the littoral zone 3.3.2. Communities of Limnetic Zone 3.3.3. Communities of Profundal Zone 4. Lake Ecosystem 4.1. Thermal Properties of Lake 4.2. Seasonal Cycle in Temperate Lakes 4.3. Biological Oxygen Demand 4.4. Eutrophy and Oligotrophy 4.5. Langmuir Circulation and the Descent of the Thermocline 4.6. Types of Lakes 5. State of Freshwater Ecosystems in Present Scenario 5.1. Causes of Change in the properties of freshwater bodies 5.1.1. Climate Change 5.1.2. Change in Water Flow 5.1.3. Land-Use Change 5.1.4. -
Baja California Sur, Mexico)
Journal of Marine Science and Engineering Article Geomorphology of a Holocene Hurricane Deposit Eroded from Rhyolite Sea Cliffs on Ensenada Almeja (Baja California Sur, Mexico) Markes E. Johnson 1,* , Rigoberto Guardado-France 2, Erlend M. Johnson 3 and Jorge Ledesma-Vázquez 2 1 Geosciences Department, Williams College, Williamstown, MA 01267, USA 2 Facultad de Ciencias Marinas, Universidad Autónoma de Baja California, Ensenada 22800, Baja California, Mexico; [email protected] (R.G.-F.); [email protected] (J.L.-V.) 3 Anthropology Department, Tulane University, New Orleans, LA 70018, USA; [email protected] * Correspondence: [email protected]; Tel.: +1-413-597-2329 Received: 22 May 2019; Accepted: 20 June 2019; Published: 22 June 2019 Abstract: This work advances research on the role of hurricanes in degrading the rocky coastline within Mexico’s Gulf of California, most commonly formed by widespread igneous rocks. Under evaluation is a distinct coastal boulder bed (CBB) derived from banded rhyolite with boulders arrayed in a partial-ring configuration against one side of the headland on Ensenada Almeja (Clam Bay) north of Loreto. Preconditions related to the thickness of rhyolite flows and vertical fissures that intersect the flows at right angles along with the specific gravity of banded rhyolite delimit the size, shape and weight of boulders in the Almeja CBB. Mathematical formulae are applied to calculate the wave height generated by storm surge impacting the headland. The average weight of the 25 largest boulders from a transect nearest the bedrock source amounts to 1200 kg but only 30% of the sample is estimated to exceed a full metric ton in weight. -
Top-Down Trophic Cascades in Three Meromictic Lakes Tanner J
Top-down Trophic Cascades in Three Meromictic Lakes Tanner J. Kraft, Caitlin T. Newman, Michael A. Smith, Bill J. Spohr Ecology 3807, Itasca Biological Station, University of Minnesota Abstract Projections of tropic cascades from a top-down model suggest that biotic characteristics of a lake can be predicted by the presence of planktivorous fish. From the same perspective, the presence of planktivorous fish can theoretically be predicted based off of the sampled biotic factors. Under such theory, the presence of planktivorous fish contributes to low zooplankton abundances, increased zooplankton predator-avoidance techniques, and subsequent growth increases of algae. Lakes without planktivorous fish would theoretically experience zooplankton population booms and subsequent decreased algae growth. These assumptions were used to describe the tropic interactions of Arco, Deming, and Josephine Lakes; three relatively similar meromictic lakes differing primarily from their absence or presence of planktivorous fish. Due to the presence of several other physical, chemical, and environmental factors that were not sampled, these assumptions did not adequately predict the relative abundances of zooplankton and algae in a lake based solely on the fish status. However, the theory did successfully predict the depth preferences of zooplankton based on the presence or absence of fish. Introduction Trophic cascades play a major role in the ecological composition of lakes. One trophic cascade model predicts that the presence or absence of piscivorous fishes will affect the presence of planktivorous fishes, zooplankton size and abundance, algal biomass, and 1 subsequent water clarity (Fig. 1) (Carpenter et al., 1987). The trophic nature of lakes also affects animal behavior, such as the distribution patterns of zooplankton as a predator avoidance technique (Loose and Dawidowicz, 1994).