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EFFECTS OF LIGHT ON LIFE IN WATER
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EARTH IS THE BLUE PLANET
BIOSPHERE—Sphere of life Comprises the area of around 8-10km above the Earth`s surface to the deepest areas of the oceans
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BIOSPHERE HYDROSPHERE LITOSPHERE ATMOSPHERE
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HYDROSPHERE-EARTH`S WATER SHELL
– 71% OF EARTH`S SURFACE IS WATER WATER ON MAINLAND 0.8% AERATED WATER 0.001% OCEANS AND SEAS 97.2% ICEBERGS 2%
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WATER ON MAINLAND ICEBERGS 73% RIVERS LAKES SPRINGS FEN MARSHES FISHPONDS 0.7% GROUNDWATER 22%
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FOR SALINITY WATER CAN BE : SALTY-3% SALT
SEAS OCEANS CORAL REEFS
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SALTY MARSHES ESTUARIES LAGOONS
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SWEET -1% SALT, CALCIUM AND CARBONATE
RUNNING WATER RIVERS WTAREFALLS STREAMS
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STAGNANT FENS LAKES FISHPONDS SWAMPS
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SUNLIGHT IS THE MAIN ENERGY SOURCE IN BIOSPHERE
LIGHT IS MADE OF WAVELENGHT SPECTRE SPEKTRA VALNIH DUŽINA ONLY VISIBLE PART OF SPECTRE IS IMPORTANT FOR PHOTOSYNTHESIS ( nm)
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RADIATION INTENSITY AND ITS VARIATIONS DUE TO GEOGRAPHIC WIDTH
MOST RADIATION IS ABSORBED IN THE ATMOSPHERE (OZONE) INFRARED RADIATION HAS LITTLE ENERGY SMALLER GEOGRAPHIC WIDTH HAS SMALLER SEASONAL CHANGES; BIGGER WIDTH HAS GREATER CHANGES
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LIGHT FEATURES MOSTLY IMPORTANT FOR LIVING BEINGS:
INTENSITY- LIGHT ENERGY DEPENDING ON GEOGRAPHIC WIDTH QUALITY – WAVELENGTH OF LIGHT RADIATION DURATION – LENGTH OF THE DAY
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WATER ABSORBS AND LETS OUT THE LIGHT
–WATER ECOSYSTEMS THE GREATEST HABITATS TWO ZONES ACCORDING TO AVAILABLE SUNLIGHT : PHOTIC-WITH ENOUGH LIGHT FOR PHOTOSYNTHESIS SEAS M LAKES – 50 M APHOTIC-NOT ENOUGH LIGHT FOR PHOTOSYNTHESIS TWILIGHT ZONE – 200 M M DARKNESS ZONE – 1000 M – 4000 M ABYSS ZONE – ISPOD 4000 M
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TWO MAIN AREAS ACCORDING TO
DISTRIBUTION OF LIVING BEINGS BENTAL – SEABED WITH SESSILE (ATTACHED) AND VAGIL (CRAWLING OR WALKING) ORGANISMS
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PELAGIC –FREE WATER WITH ORGANISMS THAT LEVITATE (PLANKTON) OR SWIM (NEKTON)
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LIGHT IS IMPORTANT FOR:
PHOTOSYNTHESIS= FOOD + OXYGEN ORGANISMS` ACTIVITY-MIGRATIONS DISTRIBUTION- LIMITATING FACTOR BIOCHEMICAL PROCESSES- ACCELERATES REPRODUCTION AND MATURATION - FASTER SPEED OF MOVEMENT-SLOWER IN THE DEPTHS SPEED OF METABOLISM-GREATER OXYGEN CONSUMPTION COLORING – FOR PROTECTION AGAINST PREDATORS PROTECTION AGAINST PREDATORS ORIENTATION, GLYCEROL PRODUCTION – AGAINST FREEZING, FEEDING –IMPOSSIBLE AT NIGHT
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LIGHT IS IMPORTANT FOR PHOTOSYNTHESIS = FOOD + OXYGEN
DIFFERENT PIGMENTS OF FITOHIDROFIT ABSORBS DIFFERENT LIGHT WAVELENGTH AND REFLECT DIFFERENT COLOURS
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CORALS LIVE ONLY IN SHALLOW, WARM SEAS THAT HAVE LIGHT AND TEMPERATURE IS ABOVE 20*C
EELS AND HERRINGS MATURE AND SPAWN FASTER AND EARLIER IN SHALLOW SEAS WITH MORE LIGHT BARRACUDAS AND TROUTS CREATE ENZYMES FOR FASTER ACTIVITY IN THE LIGHT AND DARKNESS
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URCHINS AND SEASHELLS GROW FASTER IN SUNNY SEAS WITH MORE OXYGEN
BACTERIA LOVE LIGHT BECAUSE OF PHOTOSYNTHESIS AND OCTOPUS HUNTS BETTER WHILE HIDDEN IN THE DARK OYSTER AND SOLE ARE ADJUSTED TO THE SEABED WITH COLOUR AND SHAPE
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BIOLUMINISCENCE IS IMPORTANT FOR ORGANISMS IN EUPHOTIC LAYER:
- IN RECOGNITION FOR PROCREATION FINDING AND ATTRACTING PREY CONFUSING ENEMY
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TELESCOPIC EYES CAN SERVE IN SIMILAR MANNER
ALTHOUGH IT DOES NOT HAVE TO BE IN GREAT DEPTHS
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LIGHT HAS HARMFUL EFFECT AS WELL:
- FAST VITAMIN DEGRADATION - DRAINING OF ORGANISMS IN TIDE AREA - MOVEMENT OF ORGANISMS TOWARDS DEPTH --- HUNT ONLY AT NIGHT - TRANSPARENCY
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FOR THOSE WHO WANT TO KNOW MORE …
PHOTOKINESIS – movement of organisma by light influence without specific direction . PHOTOTAXIS – movement towards the source of light. PHOTOPERIOD – seasonal influence of light on living beings (day and night/ seasons` change). HOMOKROMIJA – possibility of changing colour to resemble the seabed.
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THANK YOU FOR ATTENTION !
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