EARTH SCIENCE Prentice Hall EARTH SCIENCE Tarbuck Lutgens 

Slides:



Advertisements
Similar presentations
Ocean Water and Ocean Life
Advertisements

Ocean Water and Ocean Life
15. 2 Diversity of Ocean Life & 15.3 Oceanic Productivity
Chapter 15.  Purpose – In this activity, students begin to recognize the relationship between the salinity and density of water and understand that higher.
Edward J. Tarbuck & Frederick K. Lutgens
Chapters 14, 15, 16 Oceanography Who is Stan Hatfield and Ken Pinzke.
Warm Up 2/11/09 Which of the following is NOT a process that decreases the salinity of seawater? a. icebergs melting c. runoff from land b. precipitation d.
OCEAN ZONES Chapter 13 Section 2 Ocean Zones Chapter 13 Section 3.
Ocean water & ocean life
Ocean Water and Ocean Life
The Diversity of Ocean Life
The Oceans Composition. The Oceans There are five main oceans: –Pacific, Atlantic, Indian, Arctic, Antarctic.
Earth Science: 15.1B Ocean Water and Life
OCEAN WATER.
Warm Up 2/17/09 1) 1) Which of the following is NOT a process that decreases the salinity of seawater? a. icebergs meltingc. runoff from land b. precipitationd.
The Composition of Seawater
EARTH SCIENCE Prentice Hall EARTH SCIENCE Tarbuck Lutgens 
The Composition of Seawater
Ocean Water and Ocean Life
15.1 Composition of Seawater.  The total amount of solid material dissolved in water  Mass of dissolved substances : Mass of the water sample  Shown.
Review and New Material  Now that our class has tested… its times to move on BUT…. before we do one last review.
Oceans Water, Life, Floor, Currents, & Tides. Oceanography Oceanography is comprised of many different areas of science. Oceanography is comprised of.
Ocean Zones.
D IVERSITY & PRODUCTIVITY OF O CEAN L IFE.  Classification is a way of organizing living things  Things that live in the ocean are called marine organism.
15 Chapter 15 Ocean Water and Ocean Life The Composition of Seawater  Salinity is the total amount of solid material dissolved in water.  typically.
Ocean Water Chapter 20.
1.__________ is NOT a process that decreases the salinity of seawater. a.icebergs meltingc. runoff from land b.precipitationd. evaporation 2.The ________.
CH 15 Ocean Life and Ocean Water Salinity – total amount of dissolved solids in water Expressed in parts per thousand Average salinity of is 35 ppt or.
Oceanic Zones.
Color of the water is determine by the way sunlight is – Absorbed – Reflected.
Biological Oceanography:
19 Chapter 19 Ocean Life. Life  Living things must do several processes:  Take in and use energy  Grow and develop  Respond to the environment  Excrete.
Ocean Life Zones. Starting with an activity Starting with an activity Look at the organisms around the classroom. Look at the organisms around the classroom.
Ocean Water and Ocean Life
Warm Up  What is salinity? The total amount of solid material dissolved in water The total amount of solid material dissolved in water  What is the difference.
Ocean Water and Life. Salt in the Ocean Salinity is the total amount of solid material dissolved in water. Salinity is expressed by the amount of salt.
Estuary Shoreline areas where fresh water from rivers mixes with salt water from the ocean. Question: Describe 2 reasons why estuaries are important.
Salinity Salinity is the total amount of solid material dissolved in water. Because the proportion of dissolved substances in seawater is such a small.
Chapter 15. Salinity Chemical weathering on land creates chemicals picked up by freshwater and delivered to the ocean Mainly sodium chloride Chemicals.
Starter Complete the #5-7 on page 2 of the sheet entitled, “Standardized Test Prep”. Answer all questions to the best of your ability. You may write on.
Marine Life.
Oceanic Zones.
Oceanic Zones.
Ocean Water & Ocean Life
Prentice Hall EARTH SCIENCE
15.1 The Composition of Seawater
Ocean Water California Standards: 5d, 7b
OCEAN WATER AND OCEAN LIFE
The Diversity of Ocean Life
Ocean Water Earth Science Ch. 15.
Marine Hydrology Oceanography Properties of seawater Topics:
Estuary Shoreline areas where fresh water from rivers mixes with salt water from the ocean. Question: Describe 2 reasons why estuaries are important.
15.2 – The Diversity of Ocean Life
Oceanic Zones.
Ocean Water and Ocean Life Chapter 14
The Composition of Seawater
Oceanic Zones.
Estuary Shoreline areas where fresh water from rivers mixes with salt water from the ocean. Question: Describe 2 reasons why estuaries are important.
15.1 – The Composition of Seawater
Life in the Ocean.
OCEAN ZONES Chapter 13 Section 2 Ocean Zones Chapter 13 Section 3.
The Composition of Seawater
Life in the Ocean.
OCEAN ZONES Chapter 13 Section 2 Ocean Zones Chapter 13 Section 3.
How does life change in each zone of the ocean?
The Composition of Seawater
Life in the ocean.
The Discovery of Ocean Life
OCEAN WATER & OCEAN LIFE
OCEAN ZONES Chapter 13 Section 2 Ocean Zones Chapter 13 Section 3.
Presentation transcript:

EARTH SCIENCE Prentice Hall EARTH SCIENCE Tarbuck Lutgens 

The Study of the Oceans Project Booklet Chapter 15 Ocean Water and Ocean Life –Do all Vocabulary p. 442 –Copy ALL KEYS in the Chapter and divide them up in Sections. –Draw, Color and Label p. 430 –Pp How the Earth Works Key Terms (Answer All) –Extra 10 points (Draw, Color and Label p. 438 Life in the Ocean Zones)

15 Chapter 15 Ocean Water and Ocean Life

Salinity 15.1 The Composition of Seawater  Salinity is the total amount of solid material dissolved in water.  Most of the salt in seawater is sodium chloride, common table salt.  Sources of Sea Salt Chemical weathering of rocks on the continents is one source of elements found in seawater. The second major source of elements found in seawater is from Earth’s interior.

Salinity  Processes Affecting Salinity 15.1 The Composition of Seawater Processes that decrease salinity: Processes that increase salinity: - Precipitation - Runoff from land - Icebergs melting - Sea ice melting - Evaporation - Formation of sea ice

Natural Processes Affecting Salinity

Ocean Layering  Oceanographers generally recognize a three-layered structure in most parts of the open ocean: a shallow surface mixed zone, a transition zone, and a deep zone The Composition of Seawater  Surface Zone Sun-warmed zone Zone of mixing Shallow (300 to 450 meters)

Ocean Layering  Transition Zone 15.1 The Composition of Seawater  Deep Zone Constant high-density water Temperatures are just a few degrees above freezing. Sunlight never reaches this zone. Thermocline and pycnocline Between surface layer and deep zone

Classification of Marine Organisms  Marine organisms can be classified according to where they live and how they move The Diversity of Ocean Life  Plankton Plankton include all organisms—algae, animals, and bacteria—that drift with ocean currents. Phytoplankton are algal plankton, which are the most important community of primary producers in the ocean. Zooplankton are animal plankton.

Plankton

Classification of Marine Organisms  Nekton 15.2 The Diversity of Ocean Life  Benthos Nekton include all animals capable of moving independently of the ocean currents, by swimming or other means of propulsion. Benthos describes organisms living on or in the ocean bottom.

Nekton

Benthos

Marine Life Zones  Three factors are used to divide the ocean into distinct marine life zones: the availability of sunlight, the distance from shore, and the water depth The Diversity of Ocean Life  Availability of Sunlight The photic zone is the upper part of the ocean into which sunlight penetrates.

Marine Life Zones  Distance from Shore 15.2 The Diversity of Ocean Life The intertidal zone is the strip of land where the land and ocean meet and overlap, or the zone between high and low tides. The neritic zone is the marine-life zone that extends from the low-tide line out to the shelf break. The oceanic zone is the marine-life zone beyond the continental shelf.

Marine Life Zones

 Water Depth 15.2 The Diversity of Ocean Life The pelagic zone is open zone of any depth. Animals in this zone swim or float freely. The benthic zone is the marine-life zone that includes any sea-bottom surface regardless of its distance from shore. The abyssal zone is a subdivision of the benthic zone characterized by extremely high pressures, low temperatures, low oxygen, few nutrients, and no sunlight.

Marine Life Zones  Hydrothermal Vents 15.2 The Diversity of Ocean Life Here seawater seeps into the ocean floor through cracks in the crust. At some vents, water temperatures of 100 o C or higher support communities of organisms found nowhere else in the world.

Hydrothermal Vents

Tube Worms Found Along Hydrothermal Vents