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Exploring the Oceans

Section 1 Earth’s Oceans

Section 2 The Ocean Floor

Section 3 Life in the Ocean

Section 4 Resources from the Ocean

Section 5 Ocean Pollution

Chapter 13

Preview

Concept Mapping


Section 1 Earth’s OceansChapter 13

• List the major divisions of the global ocean.

• Describe the history of Earth’s oceans.

• Identify the properties of ocean water.

• Describe the interactions between the ocean and the atmosphere.

Objectives



• The largest ocean is the Pacific Ocean.

• The other oceans, listed from largest to smallest, are: • the Atlantic Ocean• the Indian Ocean• the Arctic Ocean • the Southern Ocean

Divisions of the Global Ocean





• About 4.5 billion years ago, there were no oceans.

• Sometime before 4 billion years ago, water vapor in the atmosphere condensed and fell as rain.

• The rain filled the deeper levels of Earth’s surface and the first oceans began to form.

How Did the Oceans Form?



• The shape of the oceans has changed over time.

How Did the Oceans Form?, continued



• Dissolved Gases Nitrogen, oxygen, and carbon dioxide are the main gases dissolved in ocean water.

Characteristics of Ocean Water

• Solids Sodium chloride, or table salt, is the most abundant dissolved solid in the ocean. Other solids are also found in ocean water.



• Salinity is a measure of the amount of dissolved solids in a given amount of liquid.

• Changes in Salinity Climate and water movement affect salinity. Costal water in cool, humid places has a low salinity. Slow-moving bodies of water have higher salinity than other parts of the ocean do.

Characteristics of Ocean Water, continued





• Temperature Zones The temperature of ocean water decreases as depth increases.




• Surface Temperature Changes Surface-zone temperatures vary with latitude and the time of year.

• Surface temperatures range from 1ºC near the poles to about 24 ºC near the equator.

• The surface zone is heated more in the summer.




• The water cycle is the continuous movement of water from the ocean to the atmosphere to the land and back to the ocean.

• The ocean is an important part of the water cycle because nearly all of Earth’s water is in the ocean.

The Ocean and the Water Cycle





• The ocean regulates atmospheric temperatures.

• A Thermal Exchange The ocean absorbs and releases thermal energy much more slowly than dry land does.

• The circulation of warm water causes some coastal lands to have warmer climates than they would have with the currents.

A Global Thermostat


Section 2 The Ocean FloorChapter 13

• Describe technologies for studying the ocean floor.

• Identify the two major regions of the ocean floor.

• Classify subdivisions and features of the two major regions of the ocean floor.

Objectives



• Seeing by Sonar Scientists use sonar to determine the ocean’s depth.

• Oceanography via Satellite Scientists use images from the satellite Seasat to study ocean currents.

• Studying the Ocean with Geosat Scientists use the Geosat satellite to measure slight changes in the height of the ocean’s surface.

Studying the Ocean Floor





• Regions of the Ocean Floor The two regions of the ocean floor are the continental margin and the deep-ocean basin.

• Underwater Real Estate The continental margin and the deep-ocean basin are subdivided into different areas and have different features, as shown on the next two slides.

Revealing the Ocean Floor







• Piloted Vessels: Alvin and Deep Flight Alvin and Deep Flight are two research vessels that can reach some of the deepest parts of the ocean.

• Robotic Vessels: JASON II and Medea JASON II and Medea are a robotic team. JASON II explores the ocean floor. Medea is attached to JASON II with a tether and explores above the the sea floor.

Exploring the Ocean with Underwater Vessels


Section 3 Life in the OceanChapter 13

• Identify the three groups of marine life.

• Describe the two main ocean environments.

• Identify the ecological zones of the benthic and pelagic environments.

Objectives



• Organisms that float or drift freely near the ocean’s surface are called plankton.

• Organisms that swim actively in the open ocean are called nekton.

• Organisms that live on or in the ocean floor are called benthos.

Three Groups of Marine Life


Chapter 13 Section 3 Life in the Ocean



• The Benthic Environment is the region near the bottom of a pond, lake, or ocean.

• The benthic environment is divided into ecological zones based on where different types of benthos live.

The Benthic Environment



• The Intertidal Zone is where the ocean meets the land.

• The intertidal zone is exposed to air for part of the day. Organisms found in this zone include starfish, sea anemones, barnacles, crabs, and seaweed.

The Benthic Environment, continued



• The Sublittoral Zone The sublittoral zone begins at the low-tide limit and extends to the continental shelf, which is about 200 m below sea level.

•The temperature, water pressure, and amount of sunlight remain fairly constant in this zone. Coral is found in this zone.




• The Bathyal Zone The bathyal zone extends from the continental shelf to the abyssal zone. The depth of this zone ranges from 200 m to 4,000 m below sea level.

• Because of the lack of sunlight, few plants are found in this zone. Animals such as sea stars, sponges, and octopuses are found here.




• The Abyssal Zone The abyssal zone is the largest ecological zone of the ocean and can reach 4,000 m in depth.

• No plants live in this zone. The few animals that can be found include crabs, sponges, sea cucumbers, and worms.




• The Hadal Zone The hadal zone consists of the floor of the ocean trenches and any organisms found there. The depth can reach from 6,000 m to 7,000 m below sea level.

• The only organisms that have been found in this zone include a type of sponge, a few species of worms, and a type of clam.




• The zone near the ocean’s surface and at the middle depths is called the pelagic environment.

• The pelagic environment is above the abyssal zone and beyond the littoral zone.

•The two major zones of the pelagic environment are the neritic zone and the oceanic zone.

The Pelagic Environment



• The Neritic Zone The neritic zone is a warm, shallow zone that covers the continental shelf.

• The neritic zone contains the largest concentration of marine life.

• The neritic zone receives more sunlight than other ocean zones, allowing plankton to grow and serve as a food supply.

The Pelagic Environment, continued



• The Oceanic Zone The oceanic zone includes the volume of water that covers the entire sea floor except for the continental shelf.

• The deeper parts of the oceanic zone have colder water temperatures and much greater pressure than the neritic zone.

• Organisms are more spread out in the oceanic zone.

The Pelagic Environment, continued


Section 4 Resources from the OceanChapter 13

• List two ways of harvesting the ocean’s living resources.

• Identify three nonliving resources in the ocean.

• Describe the ocean’s energy resources.

Objectives



• Fishing the Ocean Fish are the larges group of organisms take from the ocean.

• Farming the Ocean People have begun to raise ocean fish and other organisms in fish farms to help meet the demand for seafood.

• Savory Seaweed Many types of seaweed are harvested from the ocean for use as food.

Living Resources



• Oil and Natural Gas Oil and natural gas are used for energy and are found under layers of impermeable rock.

• Searching for Oil Scientists use seismic equipment to find oil and natural gas under the ocean floor.

Nonliving Resources



• Fresh Water and Desalination Fresh water can be collected for human use by removing the salt from ocean water.

•Sea-Floor Minerals Scientists estimate that 15% of the ocean floor is covered with mineral-rich nodules. However, mining them is costly and difficult.

•Tidal Energy is energy generated from the movement of the tides.

Nonliving Resources, continued



• Wave Energy The constant motion of waves is a clean, renewable energy resource.

• Researchers have found certain areas of the world where wave energy can generate enough electrical energy to make building power plants worthwhile.

Nonliving Resources, continued


Section 5 Ocean Pollution

Objectives

Chapter 13

• Explain the difference between point-source and nonpoint-source pollution

• Identify three different types of point-source pollution.

• Describe what is being done to control ocean pollution.


Section 5 Ocean PollutionChapter 13

• Pollution that comes from many sources rather than from a single site is called nonpoint-source pollution.

• Most ocean pollution is nonpoint-source pollution and can be difficult to regulate and control.

Nonpoint-Source Pollution



• Trash Dumping Dumping trash in the deeper parts of the ocean is a common practice in many countries.

• Effects of Trash Dumping Trash thrown in the ocean can be harmful to ocean organisms.

• Sludge Dumping Sludge is the solid waste removed from raw sewage. Sludge can pollute beaches and kill marine life.

Point-Source Pollution



Point-Source Pollution, continued

• Oil Spills If not handled properly, oil transports can cause oil spills.



• Effects of Oil Spills Oil spills can harm or kill many plants and animals.

• Preventing Oil Spills New technology is being used to safeguard against oil spills. Oil tankers are now being built with two hulls instead of one.

Point-Source Pollution, continued



• Nations Take Notice Many international agreements and laws restrict ocean pollution.

• Citizens Taking Charge People have demanded that their governments work to solve ocean pollution and have begun organizing beach cleanups.

• Action in the United States The U.S. has passed laws to control local pollution.

Saving Our Ocean Resources


Exploring the Oceans

Use the terms below to complete the concept map on the next slide.

Chapter 13

Concept Mapping

ecological zones

benthos

intertidal zone

benthic zone

nentic zone

marine life

oceans

plankton

oceanic zone


Exploring the OceansChapter 13


Exploring the OceansChapter 13

Documents

< BackNext >PreviewMain Exploring the Oceans Section 1 Earth’s OceansEarth’s Oceans Section 2 The Ocean FloorThe Ocean Floor Section 3 Life in the OceanLife