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Chapter 10 Biological Productivity in the Ocean ©2003 Jones and Bartlett Publishers Food Webs and 10-1 Trophic Dynamics An ecosystem is the totality of the environment encompassing all chemical, physical, geological and biological parts. • Ecosystems function by the exchange of matter and energy. • Material is constantly recycled in the ecosystem, but energy gradually dissipates as heat and is lost. – Energy flows downhill, materials cycle! • All ecosystems are composed of: – Autotrophs (producers) – Heterotrophs (consumers) 10-1 Autotrophs • Autotrophs use an abiotic source of energy to convert inorganic material into organic compounds for growth and reproduction. • Autotrophs produce food, and are known as “primary producers”. • Inorganic vs. organic material. – Inorganic = CO2, NH3, NO32-, PO43-, etc – Organic = living, or derived from living tissue (proteins, lipids, carbohydrates, nucleic acids, or containing C-C bonds (petroleum products). • Plants are autotrophs and the primary producers in most ecosystems. – Energy source is the Sun. • Chemosynthetic bacteria are autotrophs and primary producers in deep vent communities – Energy source is inorganic sulfur molecules, NOT SUN! Examples of Marine Autotrophs phytoplankton Seaweeds Eel grass Mangroves Salt marsh Chemosynthetic bacteria Food Webs and 10-1 Trophic Dynamics • All other organisms are heterotrophs, the consumers and decomposers in ecosystems. • Heterotrophs derive their energy from organic matter (animals, plants, detritus, dissolved organic matter) • Herbivores eat plants and carnivores eat animals. Examples of Marine Heterotrophs fish crab krill whale copepod Heterotrophic bacteria Tube worms dinoflagellate Food Webs and 10-1 Trophic Dynamics The word “trophic” refers to nutrition. • Trophic dynamics is the study of the nutritional interconnections among organisms within an ecosystem. • Trophic level is the position of an organism within the trophic structure of an ecosystem. – Autotrophs form the first trophic level. – Herbivores are the second trophic level. – Carnivores occupy the third and higher trophic levels. – Decomposers form the terminal level. Food Webs and 10-1 Trophic Dynamics • A food chain is the succession of organisms within an ecosystem based upon trophic dynamics. (Who is eaten by whom.) Food Webs and 10-1 Trophic Dynamics • A food web consists of interconnected and interdependent food chains- more realistic. Food Web Food Webs and 10-1 Trophic Dynamics • An energy pyramid is the graphic representation of a food chain in terms of the energy contained at each trophic level. • The size of each level in an energy pyramid is controlled by the size of the level immediately below. Energy Energy Pyramid Ecosystem Model: Definition • A tentative, explanatory, generalization about how ecosystem functions (i.e., a hypothesis). • Structure of model arises from observations. • Tentativeness requires that models be verified by experimentation or further observations. Ecosystem Model: Generic Ecosystem Model • Ecosystem models show: – Trophic pathways (carbon flows) – Ecological efficiency – Resilience to species loss – Biological magnification – Biogeochemical pathways (flows of other elements, Ca, Si, N, P, etc.). Phytoplankton blooms and 10-1 cell division Increased cell division causes bloom Food Webs and 10-1 Trophic Dynamics As the primary producers, plants require sunlight, nutrients, water and carbon dioxide for photosynthesis. • Photosynthesis occurs within organelles called chloroplasts, or within lamellae of prokaryotes. • The formula for photosynthesis is: Sunlight + 6 CO2 + 6 H2O C6H12O6 (sugar) + 6 O2. Food Webs and 10-1 Trophic Dynamics lamellae Diatom: Eukaryote Blue-green algae: Prokaryote 10-1 Photosynthesis 10-1 Respiration Animals must consume pre-existing organic material to survive. • Animals break down the organic compounds into their inorganic components to obtain the stored energy. • The chemical formula for respiration is: C6H12O6 (sugar) + 6 O2 6 CO2 + 6 H2O + Energy. Food Webs and 10-1 Trophic Dynamics Photosynthesis Sunlight + 6 CO2 + 6 H2O C6H12O6 (sugar) + 6 O2. Respiration C6H12O6 (sugar) + 6 O2 6 CO2 + 6 H2O + Energy. *Respiration is similar to the combustion of gasoline in your automobile. It produces energy, carbon dioxide and water. Food Webs and 10-1 Trophic Dynamics • The energy recovered during respiration is used for movement, reproduction and growth. – Respiration occurs in organelles called mitochondria – Animals and plants respire Food Webs and 10-1 Trophic Dynamics • The food consumed by most organisms is proportional to their body size. • Smaller animals eat smaller food and larger animals eat larger food, although exceptions occur. Food Webs and 10-1 Trophic Dynamics Heterotrophic dinoflagellates feeding on photosynthetic dinoflagellate Food Webs and 10-1 Trophic Dynamics Blue whale (~30 m) Krill (~0.01 m) Food Webs and 10-1 Trophic Dynamics • The basic feeding styles of animals are: – Grazing – Predation – Scavenging – filter feeding – deposit feeding feed on plants actively pursue and capture food feed on dead stuff (detritus) filter plankton or detritus from water filter food from sediment Food Webs and 10-1 Trophic Dynamics Cow grazing on grass Dinoflagellate grazing on another dinoflagellate …or any zooplankton on phytoplankton, sea urchin on algae, snail on seaweed, etc. Food Webs and 10-1 Trophic Dynamics Filter-feeder predator scavenger Food Webs and 10-1 Trophic Dynamics Deposit feeder (polychaete worm) Food Webs and 10-1 Trophic Dynamics •Population size is dependent upon food supply and grazing pressure. Food Webs and 10-1 Trophic Dynamics Bacteria are the decomposers; they break down organic material and release nutrients for recycling. Nutrient Cycling Food Webs and 10-1 Trophic Dynamics • Few bacteria are capable of completely degrading organic material into its inorganic components. Most operate in succession with other bacteria to decompose material in a series of stages. • Bacteria also serve as food for other organisms either directly or indirectly. Food Webs and 10-1 Trophic Dynamics • Bacteria can be divided into those that are aerobic or anaerobic. – Aerobic: (“with air”)- uses oxygen in air. – Anaerobic: (“without air”), in sediments. Use oxygen contained within molecules, such as sulfate SO42- 2O2 + S2- Hydrogen sulfide, H2S, then forms. “Rotten egg” smell Food Webs and 10-1 Trophic Dynamics • Bacteria can also be divided into those that are autotrophic or heterotrophic. – Autotrophic: obtains food by photosynthesis • Blue-green algae (Prochlorococcus sp. – most abundant organism on Earth?). – …or chemosynthesis - from inorganic compounds. • Volcanic vent bacteria – Heterotrophic: obtains food by eating other organic matter. • E. coli, etc. Photosynthetic vs. Chemosynthetic Food Chain Volcanic vent communities at Hydrothermal vent sites Black smoker at hydrothermal vent Volcanic vent communities at Hydrothermal vent sites Volcanic vent communities at Hydrothermal vent sites Chemosynthetic bacteria live inside worms and produce organic matter Red Riftia tube worms thrive near a sea vent. Are volcanic vent communities at Hydrothermal vents good analogs for life on other planets? Below the icy surface of Galileo’s moon Europa, heat from tectonic forces may allow liquid water to exist. Do chemosynthetic bacteria exist here as well? Food Chains and Energy Transfer Food chains transfer energy from one trophic level to another. • Biomass is the quantity of living matter per unit area or per volume of water. • With each higher trophic level, the size of organisms generally increases, but their reproductive rate, number and the total biomass decrease. Food Chains and Energy Transfer Large body size, low biomass, slow growth. Small body size, high biomass, fast growth. Food Chains and Energy Transfer • The two major food chains in the ocean are the grazing food chain and the Detritus food chain (non-living wastes form the base of the food chain). Grazing Food Chain Phytoplankton Zooplankton Detritus Deposit Feeder Detrital Food Chain Nekton Nekton •Only about 10-20% of energy is transferred between trophic levels and this produces a rapid decline in biomass at each successive trophic level. Food Chains and Energy Transfer •Only about 10-20% of energy is transferred between trophic levels and this produces a rapid decline in biomass at each successive trophic level. •Energy lost as kinetic motion and maintenance respiration. •Energy lost building nonnutritional tissue (bones, chitin exoskeleton, diatom frustules, etc.) 0.1 1 10 100 Energy Food Chains and Energy Transfer Food Chains and Energy Transfer 0.1 108 g algae 0.1 107 g krill 106 g small fish 0.1 0.1 104 g small human 105 g large fish Why not make trophic chain shorter? 104 g small human 0.1 105 g algae 0.1 0.1 105 g krill 105 g small fish General Marine Productivity Primary production is the total amount of carbon (C) in grams converted into organic material per square meter of sea surface per year (gm C/m2/yr). • Factors that limit plant growth and reduce primary production include solar radiation and nutrients as major factors and upwelling, turbulence, grazing intensity and turbidity as secondary factors. • Only 0.1 to 0.2% of the solar radiation is employed for photosynthesis and its energy stored in organic compounds. 10-2 General Marine Productivity • Macronutrients and micronutrients are chemicals needed for survival, growth and reproduction in large and small quantities, respectively. • Upwelling and turbulence return nutrients to the surface. • Overgrazing of autotrophs depletes the population and leads to a decline in productivity. • Turbidity reduces the depth of light penetration and restricts productivity even if nutrients are abundant. Wave and Tide Turbulence 10-2 General Marine Productivity Productivity varies greatly in different parts of the ocean in response to the availability of nutrients and sunlight. • In the tropics and subtropics sunlight is abundant, but it generates a strong thermocline that restricts upwelling of nutrients and results in lower productivity. • High productivity locally occurs in areas of coastal upwelling, in the tropical waters between the gyres, and in coral reefs. 10-2 General Marine Productivity • In temperate regions productivity is distinctly seasonal. • Polar waters are nutrient-rich all year but productivity is only high in the summer when light is abundant. Variations in Primary Productivity 10-3 Global Patterns of Productivity Primary productivity varies from 25 to 1250 gm C/m2/yr in the marine environment and is highest in estuaries and lowest in the open ocean. • In the open ocean primary productivity distribution resembles a “bull’s eye“ pattern with lowest productivity in the center and highest at the edge of the basin. • Water in the center of the ocean is a clear blue because it is an area of downwelling, above a strong thermocline and is almost devoid of biological activity. 10-3 Global Patterns of Productivity • Continental shelves display moderate productivity between 50 and 200 gm C/m2/yr because nutrients wash in from the land, and tide- and wave- generated turbulence recycle nutrients from the bottom water. • Polar areas have high productivity because there is no pycnocline to inhibit mixing. • Equatorial waters have high productivity because of upwelling. • Centers of circulation gyres, which occupy most of the open ocean, are biological deserts. The Sargasso Sea and Vertical Profiles 10-3 Global Patterns of Productivity It is possible to estimate plant and fish productivity in the ocean. • The size of the plankton biomass is a good indicator of the biomass of the remainder of the food web. • Annual primary production (APP) is equal to primary production rate (PPR) times the area for which the rate is applicable. APP = PPR x Area (to which applicable ) • Transfer efficiency (TE) is a measure of the amount of carbon that is passed between trophic levels and is used for growth. • Transfer efficiency varies from 10 to 20% in most food chains. 10-3 Global Patterns of Productivity • Potential production (PP) at any trophic level is equal to the annual primary production (APP) times the transfer efficiency (TE) for each step in the food chain to the trophic level of the organism under consideration. PP = APP x TE (for each step) • Although rate of productivity is very low for the open ocean compared to areas of upwelling, the open ocean has the greatest biomass productivity because of its enormous size. 10-3 Global Patterns of Productivity • In the open ocean the food chains are longer and energy transfer is low, so fish populations are small. • Most fish production is equally divided between areas of upwelling and coastal waters. • Calculations suggest that the annual fish production is about 240 million tons/yr. 10-3 Global Patterns of Productivity • Overfishing is removing fish from the ocean faster than they are replaced by reproduction and this will eventually lead to the collapse of the fish population if not regulated. Haddock Catch in North Sea Biological Productivity of 10-4 Upwelling Water Upwelling of deep, nutrient-rich water supports large populations of phytoplankton and fish. • The waters off the coast of Peru normally is an area of upwelling, supporting one of the world’s largest fisheries. • Every three to seven years warm surface waters in the Pacific displace the cold, nutrient-rich water on Peru’s shelf in a phenomenon called El Nino. • El Nino results in a major change in fauna on the shelf and a great reduction in fishes. • This can lead to mass starvation of organisms dependent upon the fish as their major food source. The Ocean Sciences: Volcanic Vent Communities • Volcanic vent communities have been discovered along sea-floor spreading ridges. • The base of the food webs in these vent communities consists of chemosynthesizing bacteria, which obtain energy to manufacture food by oxidizing hydrogen sulfide gas. • Seawater heated by magma leaches metal from the basalts and these get precipitated as sulfide and sulfate minerals that form chimneys on the sea floor. Plumbing in a Black Smoker The Ocean Sciences: What Causes El Niño? • When the trade winds are strong, cold, nutrient-rich water upwells offshore Peru, supporting high primary productivity and large populations of anchovy. • When air-pressure patterns change, the trade winds weaken and even reverse direction, dragging warm, nutrient-poor water to Peru and initiating an El Niño event. 10-1 Photosynthesis 10-1 Photosynthesis 10-1 Photosynthesis