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Classification of &

OCN 201 Lecture 3 Grieg Steward can make the organic building blocks of Heterotrophs have to eat organics life starting from carbon dioxde

nucleotides

sugars

C H S H amino acids H lipids Classifying Marine by

Autotrophs - use CO to make organics • 2 • Who: All , some protista and • Can use (photo-) or chemical (chemo-) energy • Heterotrophs - Need to consume organic compounds • Who: everything that is not autotrophic • - They can do both! Autotrophy ( or )

Energy Autotrophic

6CO2 + 6H2O C6H12O6 + 6O2

Sugar

Cells are more than sugar. Other compounds are built from simple sugars plus (Nitrogen, Phosphorous) & trace metals) Respiration Reversing the reaction yields energy the cell can use

Autotrophic Cell

6CO2 + 6H2O C6H12O6 + 6O2

Energy Respiration Heterotrophs consume organics. Much is respired to get energy and some is used as building blocks to grow.

Heterotroph

6CO2 + 6H2O C6H12O6 + 6O2

Energy Heterotrophs Heterotrophs Macroalgae & Plants Photoautotrophs Photoautotrophs Heterotrophs Mixotrophs

Photoautotrophs Chemoautotrophs Bacteria and Archaea Heterotrophs Mixotrophs

3.8 bya 2 bya Today 7 Classifying Marine Organisms by • Benthic ( = bottom) • Pelagic (pelagius = of the sea)

Ocean Habitats

Intertidal PELAGIC (littoral) Classifying Marine Organisms by Lifestyle

Epifauna • Benthic (benthos = bottom) • Infauna Epifauna • Infauna • Pelagic (pelagius = of the sea) • (Drifters, weak swimmers) • Nekton (Swimmers) Pelagic Organisms 35 mm

Nekton (all are animals)

5 mm Plankton Physical Divisions of the Marine Environment

Supralittoral (splash zone) NERITIC OCEANIC

Epipelagic 200 m Sublittoral Littoral Mesopelagic (intertidal) 1000 m

Bathypelagic Bathyal

4000 m

Abyssal Abyssopelagic 6000 m Hadalpelagic Hadal Physical & Chemical Factors Affecting Life

• Temperature & Light DECREASE with Depth & Latitude • Pressure INCREASES with Depth • Salinity more variable near shore • Air exposure in the Pressure Increases with Depth

Photo courtesy Kate Achilles Deep-diving marine mammals have collapsible lungs Temperature Variations

Temperature Decreases with Depth

Temperature Decreases with Latitude

POLAR TEMPERATE

TROPICAL TEMPERATE

POLAR TOTAL light and COLOR Spectrum Vary with depth

Red Yellow Green Blue UV Euphotic zone= where photosynthesis is possible! “Good” Light Euphotic 20 to 100 m

Twilight Disphotic Disphotic zone= there is light but not enough for photosynthesis! about 600 m No Light Aphotic No light from the sun penetrates Photosynthesis Feeds The

Energy

Food The Pelagic Divisions (By Light)

Photosynthesis can only EUPHOTIC ZONE “Good” Light happen up here! 20 to 100 m

DISPHOTIC ZONE Twilight

about 600 m APHOTIC ZONE No Light

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