The Aquatic Environment. Introduction Aquatic systems are those in which the primary medium inhabited by organisms is water. Aquatic systems are those.

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Presentation transcript:

The Aquatic Environment

Introduction Aquatic systems are those in which the primary medium inhabited by organisms is water. Aquatic systems are those in which the primary medium inhabited by organisms is water. 2 groups: 2 groups: Freshwater; limnologyFreshwater; limnology Marine; oceanographyMarine; oceanography

Some systems are transitional between the 2 types Some systems are transitional between the 2 types Estuaries, salt marshes, saline lakesEstuaries, salt marshes, saline lakes

Distribution Majority of the Earth’s water is found in oceans Majority of the Earth’s water is found in oceans 71% of worlds surface is covered with water 71% of worlds surface is covered with water The hydrological cycle drives the movement of water throughout the Earth The hydrological cycle drives the movement of water throughout the Earth

Oceans Oceans Largest component is the water column itself or pelagic zoneLargest component is the water column itself or pelagic zone Surface currents are generated by wind frictionSurface currents are generated by wind friction Coriolis force causes the surface layer to move at 45 o to wind directionCoriolis force causes the surface layer to move at 45 o to wind direction

Deep currents are not effected by surface currentsDeep currents are not effected by surface currents Downwelling occurs because surface waters are cooled at high latitudes, increasing their density and sinkDownwelling occurs because surface waters are cooled at high latitudes, increasing their density and sink Upwelling occurs in areas where surface water circulation patterns diverge, leaving a gap, which is filled from beneathUpwelling occurs in areas where surface water circulation patterns diverge, leaving a gap, which is filled from beneath

Benthic zone is the ocean bedBenthic zone is the ocean bed Divided into structures:Divided into structures: coastal zone where sea meets land coastal zone where sea meets land Continental shelf is part of the continental plate Continental shelf is part of the continental plate Ocean ridges occupy 33% of sea floor; site of new seafloor Ocean ridges occupy 33% of sea floor; site of new seafloor Deep sea floor covered in pelagic sediment Deep sea floor covered in pelagic sediment

Inland waters Inland waters Glacial ice at high altitudesGlacial ice at high altitudes Groundwater under most of the Earth’s surfaceGroundwater under most of the Earth’s surface Rivers, lakes, and wetlands have a high turnover of waterRivers, lakes, and wetlands have a high turnover of water

Rivers are drainage channels for the excess of precipitation and the main conduit for the return of water from land to seaRivers are drainage channels for the excess of precipitation and the main conduit for the return of water from land to sea Lakes require a basin within which to formLakes require a basin within which to form Wetlands occur where inputs of water exceed evaporation but outflow is impeded by flat topographyWetlands occur where inputs of water exceed evaporation but outflow is impeded by flat topography

Chemistry of water Dissolved substances determine the quality of water Dissolved substances determine the quality of water Salinity is the total amount of dissolved material in a sample Salinity is the total amount of dissolved material in a sample Conductivity is a measure of the ability of water to conduct electricity Conductivity is a measure of the ability of water to conduct electricity

Source of salts for the sea is the weathering or rocks by rainwater Source of salts for the sea is the weathering or rocks by rainwater Calcium carbonate is used by many marine animals as a skeletal material Calcium carbonate is used by many marine animals as a skeletal material

Dissolved gases Dissolved gases Oxygen and carbon dioxide are the most importantOxygen and carbon dioxide are the most important Physical mixing is requiredPhysical mixing is required Concentration is determined by temperature and pressureConcentration is determined by temperature and pressure

Acidity is the measure of the concentration of hydrogen ions H + Acidity is the measure of the concentration of hydrogen ions H + Alkalinity is a measure of carbonates and bicarbonates in a solution because these substances act as buffers to the acidic rainwater Alkalinity is a measure of carbonates and bicarbonates in a solution because these substances act as buffers to the acidic rainwater Sea water has a pH of 8 because it is well buffered with a high alkalinity Sea water has a pH of 8 because it is well buffered with a high alkalinity

Energy inputs Primary production is the creation of organix molecules from inorganic molecules Primary production is the creation of organix molecules from inorganic molecules Photosynthesis in plants, algae and cyanobacteriaPhotosynthesis in plants, algae and cyanobacteria Light intensity decreases with depth called attenuation Light intensity decreases with depth called attenuation

There is a relationship between photosynthesis, respiration, and depth (see figure1.7) There is a relationship between photosynthesis, respiration, and depth (see figure1.7) Photic zone is the layer of water from the surface to the compensation point Photic zone is the layer of water from the surface to the compensation point

Chemosynthesis produces organic matter without light by bacteria Chemosynthesis produces organic matter without light by bacteria most common around deep ocean ventsmost common around deep ocean vents Detritus is the dominant source of energy for many organisms; it is dead primary producers Detritus is the dominant source of energy for many organisms; it is dead primary producers

POM particulate organic matter POM particulate organic matter CPOM coarse particulate organic matter; diameter of at least 1mm CPOM coarse particulate organic matter; diameter of at least 1mm FPOM fine particulate organic matter FPOM fine particulate organic matter