Biological Oceanography

46
Biological Oceanography

description

Biological Oceanography. Biologists have named about 1.8 million species. Estimates of total species range from 10 million to over 200 million. MICROBES. They make up 98% of the biomass of the world’s oceans. Supply more than half the world’s oxygen. - PowerPoint PPT Presentation

Transcript of Biological Oceanography

Page 1: Biological Oceanography

Biological Oceanography

Page 2: Biological Oceanography

Biologists have named about 1.8 million species.

Estimates of total species range from 10 million to over 200 million.

Page 3: Biological Oceanography
Page 4: Biological Oceanography

MICROBESThey make up 98% of the biomass of the world’s oceans.Supply more than half the world’s oxygen.Major processors of the world's greenhouse gases.About 1.5 million species have been named.Tens of millions of more species may exist.We know more about distant stars and planets than we do about the microbes living in our oceans.

Page 5: Biological Oceanography
Page 6: Biological Oceanography
Page 7: Biological Oceanography

The Multicellular KingdomsFungi Bodies usually made of filaments.

Absorb digested food from environment.e.g.

We won’t be talking about fungi much.

Yeah… only one percent of fungi are marine.

Page 8: Biological Oceanography

The Multicellular KingdomsPlantsMulticellular.

Photosynthetic.

Page 9: Biological Oceanography

The Multicellular KingdomsAnimals Multicellular.

Ingest food.

Page 10: Biological Oceanography

Life Zones of the

Oceans

Page 11: Biological Oceanography
Page 12: Biological Oceanography

Intertidal ZonesBetween high

and low tide levels.Alternates: wet/dry.

Many organisms attach to rocks or burrow.

Page 13: Biological Oceanography
Page 14: Biological Oceanography

Strandline – line of seaweed and debris deposited on the beach by each high tide.

Page 15: Biological Oceanography
Page 16: Biological Oceanography

Below low tide line.Coastal life zone that remains underwater.

Heavy wave impact and underwater turbulence.

Subtidal Zone

Page 17: Biological Oceanography
Page 18: Biological Oceanography

Pelagic Zone -The entire ocean of water above the sea bottom.

Page 19: Biological Oceanography

The blue stuff you’re looking at is the pelagic zone!

Page 20: Biological Oceanography

Pelagic Zone =The neritic and oceanic zones.

Page 21: Biological Oceanography

Neritic Zone – Over the continental shelf.Between low tide levels and the continental slope. ~ 200 meters at its deepest. Richest in life forms. Area of most commercial fishing.

Some areas have dense forests of seaweed.

Page 22: Biological Oceanography

Oceanic Zone – Beyond the continental shelf.

Page 23: Biological Oceanography

Photic Zone - the depth of the water with sufficient sunlight for photosynthesis to occur.

Aphotic Zone – Not enough light for photosynthesis.The majority

of “plant” life is planktonic.

Page 24: Biological Oceanography

Benthic Zone – The bottom.

Page 25: Biological Oceanography

Benthic Zone – The bottom.

Benthic organisms of the deep depend on detritus from above.

Page 26: Biological Oceanography

Detritus – Organic material “raining down” from above.

Page 27: Biological Oceanography
Page 28: Biological Oceanography

EstuariesWhere freshwater and saltwater meet.

Mixture of salt and fresh water.

Brackish -

An estuary is a semi-enclosed body of water connected to the sea.

Page 29: Biological Oceanography

Estuaries are regions of transition and sharp gradients.

Estuaries support fauna recruited mostly from the sea.

Page 30: Biological Oceanography

• Estuaries are nutrient rich – important breeding grounds.

• Calm water - protected by Barrier Beaches.

Page 31: Biological Oceanography

Estuaries –• Have more food for organisms.• But the organisms usually have to deal with large temperature and salinity changes, high silt content and pollution.

Page 32: Biological Oceanography

Why is high silt a problem for marine organisms?

Hint: How does this guy get food?

Page 33: Biological Oceanography

Many marine organisms are filter feeders so silt can be a major problem.

Page 34: Biological Oceanography

The number of species in an estuary is greatly reduced, but the number of individuals is large.

What the heck does that mean?

Page 35: Biological Oceanography

It means that if you can survive here you will find a lot of food.

But there is low biodiversity.

Page 36: Biological Oceanography

The Salt Marsh

• Controlled by tides•Marsh grasses

• The“nurseries” of the estuary.

Page 37: Biological Oceanography

Mud Flats• No grasses. Little or no aeration in the sand.• Caused by decomposing bacteria turning the

wastes in the sand into a dark mud. • Considered the “graveyards” of the estuary.

Page 38: Biological Oceanography

CHESAPEAKE BAY

Anyone know the largest estuary in the U.S.?

Page 39: Biological Oceanography

Can you name the 6 states that make up the watershed of the Chesapeake Bay?

A watershed is the drainage area for a bay.

Page 40: Biological Oceanography

VirginiaMarylandWest VirginiaDelawareNew YorkPennsylvania

Page 41: Biological Oceanography

Estuary TypesThe Chesapeake Bay is a

drowned river valley. This is the most common type of

estuary. It was formed after the last ice age some 12,000

– 18,000 years ago.

Page 42: Biological Oceanography

Bar-Built EstuariesThese are found where sand bars and barrier

islands form.The shallow water

behind these barrier islands forms low salinity estuaries.

Page 43: Biological Oceanography

Tectonic EstuariesThese

estuaries form where land sank or

subsided.e.g. San Francisco Bay.

Page 44: Biological Oceanography

Anyone know the last type of estuary?e

Hint: Think viking.

Page 45: Biological Oceanography

Fjords! Created when

retreating glaciers cut deep into the earth.

Page 46: Biological Oceanography

End point marine bio quiz 1.