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Environmental Problems, Their Causes, and Sustainability 1

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Saltwater <strong>and</strong> freshwater life zones contain four majortypes of organisms. One group consists of weaklyswimming, free-floating plankton carried by currents.There are three major types of plankton. One is phytoplankton(“FIE-toe-plank-ton,” Greek for “driftingplants”), or plant plankton. They <strong>and</strong> many types of algaeare the producers that support most aquatic foodchains <strong>and</strong> food webs. Another type is zooplankton(“ZOE-oh-plank-ton”, Greek for “drifting animals”),or animal plankton. They consist of primary consumers(herbivores) that feed on phytoplankton <strong>and</strong> secondaryconsumers that feed on other zooplankton.They range from single-celled protozoa to large invertebratessuch as jellyfish.Improved technologies for filtering <strong>and</strong> analyzingwater have revealed huge populations of much smallerplankton called ultraplankton—photosynthetic bacteriano more than 2 micrometers (40 millionths of aninch) wide. Scientists estimate that these extremelysmall plankton may be responsible for 70% of the primaryproductivity near the ocean surface.A second group of organisms consists of nekton,strongly swimming consumers such as fish, turtles,<strong>and</strong> whales. A third group, called benthos, dwells onthe bottom. Examples are barnacles <strong>and</strong> oysters thatanchor themselves to one spot, worms that burrowinto the s<strong>and</strong> or mud, <strong>and</strong> lobsters <strong>and</strong> crabs that walkabout on the bottom. A fourth group consists of decomposers(mostly bacteria) that break down the organiccompounds in the dead bodies <strong>and</strong> wastes ofaquatic organisms into simple nutrient compounds foruse by producers.How Do Aquatic Systems Differ fromTerrestrial Systems? Living withoutBoundaries <strong>and</strong> Large TemperatureFluctuationsLiving in water has its benefits <strong>and</strong> drawbacks.Living in an aquatic environment has advantages <strong>and</strong>disadvantages (Figure 7-3). Several differences betweenaquatic <strong>and</strong> terrestrial systems also hinder theability of researchers to underst<strong>and</strong> aquatic systems.One is that aquatic systems have less pronounced <strong>and</strong>fixed physical boundaries than terrestrial ecosystems.This makes it difficult to count <strong>and</strong> manage populationsof aquatic organisms.Also, food chains <strong>and</strong> webs in aquatic systems areusually more complex <strong>and</strong> longer than those in terrestrialbiomes. One reason is that the fluid medium ofwater systems <strong>and</strong> the variety of bottom habitats openup ways of getting food that are not available on l<strong>and</strong>.Another difference is that aquatic systems (especiallymarine systems) are more difficult to monitor <strong>and</strong>study than terrestrial systems because of their size <strong>and</strong>because they are largely hidden from view.AdvantagesPhysical supportfrom waterbouyancyFairly constanttemperatureNourishmentfrom dissolvednutrientsWater availabilityEasydispersementof organisms,larvae, <strong>and</strong> eggsLess exposure toharmful UVradiationDilution <strong>and</strong>dispersion ofpollutantsTrade-OffsLiving in WaterDisadvantagesCannot tolerate awide temperaturerangeExposure todissolvedpollutantsFluctuatingpopulation size formany speciesDispersionseparates manyaquatic offspringfrom parentsFigure 7-3 Trade-offs: advantages <strong>and</strong> disadvantages of livingin water.What Factors Limit Life at Different Depths inAquatic Life Zones? Living in Layered ZonesLife in aquatic systems is found in surface, middle,<strong>and</strong> bottom layers.Most aquatic life zones can be divided into three layers:surface, middle, <strong>and</strong> bottom. A number of environmentalfactors determine the types <strong>and</strong> numbers oforganisms found in these layers. Examples are temperature,access to sunlight for photosynthesis, dissolved oxygencontent, <strong>and</strong> availability of nutrients such as carbon(as dissolved CO 2 gas), nitrogen (as NO 3 ), <strong>and</strong> phosphorus(mostly as PO 4 ) for producers.3In deep aquatic systems, photosynthesis is confinedmostly to the upper layer, or euphotic zone,through which sunlight can penetrate. The depth ofthe euphotic zone in oceans <strong>and</strong> deep lakes can be reducedby excessive algal growth (algal blooms) cloudingthe water.Dissolved O 2 levels are higher near the surface becauseoxygen-producing photosynthesis takes placehttp://biology.brookscole.com/miller14129

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