Chapter 3 The Biosphere.

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Presentation transcript:

Chapter 3 The Biosphere

What is Ecology? Ecology is the scientific study of interactions among organisms and between organisms and their environment The Biosphere combines all portions of land, water, and air. Everywhere that life exists.

What is Ecology? To understand relationships within the biosphere, biologists ask questions about events and organisms, from the single individual to the entire biosphere

What is Ecology? Species- group of organisms that can interbreed and produce fertile offspring. Populations-groups of individuals, same species, live in same area Communities- assembly of different species living in an area Ecosystem-collection of organisms that live in a particular place Biome-collection of ecosystems, same climate, similar communities

Ecological Methods Ecologists use a wide range of tools and techniques Observing-1st step, observations are simple Experimenting-test hypothesis, perhaps setting up an artificial environment Modeling-make models to study complex phenomena

3–2 Energy Flow

Producers Producers Without a constant input of energy, living systems cannot function. Sunlight is the main energy source for life on Earth. Only plants, some algae, and certain bacteria can capture energy from sunlight to produce food. These organisms are called autotrophs

Producers Autotrophs use energy from the sun to make organic compounds (food/sugars) These organic molecules combine and recombine to produce living tissue. Because they make their own food, autotrophs are called producers.

Producers Energy From the Sun The best-known autotrophs harness solar energy through a process known as photosynthesis.

Producers Photosynthesis is responsible for adding oxygen to—and removing carbon dioxide from—Earth's atmosphere. Sunlight is the main energy source for life on Earth. Some types of organisms rely on the energy stored in inorganic chemical compounds. Plants use the energy from sunlight to carry out the process of photosynthesis.

Producers Plants are the main autotrophs on land. Algae are the main autotrophs in freshwater ecosystems and in the upper layers of the ocean

Consumers Consumers Many organisms cannot harness energy directly from the physical environment. Organisms that rely on other organisms for their energy and food supply are called heterotrophs. Heterotrophs are also called consumers.

Consumers There are many different types of heterotrophs. Herbivores eat plants. Carnivores eat animals. Omnivores eat both plants and animals. Detritivores feed on plant and animal remains and other dead matter. Decomposers, like bacteria and fungi, break down organic matter.

Feeding Relationships Producers and consumers are connected into feeding networks based on who eats whom.

Feeding Relationships Energy flows through an ecosystem in one direction, from the sun to autotrophs (producers) and then to various heterotrophs (consumers).

Feeding Relationships Food Chains A food chain is a series of steps in which organisms transfer energy by eating and being eaten.

Feeding Relationships In some marine food chains, the producers are microscopic algae and the top carnivore is four steps removed from the producer. Small Fish Zooplankton Squid Food chains show the one-way flow of energy in an ecosystem. In this marine food chain, energy is passed from the producers (algae) to four different groups of consumers. Shark Algae

Feeding Relationships Food Webs Ecologists describe a feeding relationship in an ecosystem that forms a network of complex interactions as a food web. A food web links all the food chains in an ecosystem together.

Feeding Relationships This food web shows some of the feeding relationships in a salt-marsh community. This illustration of a food web shows some of the feeding relationships in a salt marsh.

Feeding Relationships Trophic Levels Each step in a food chain or food web is called a trophic level. Producers make up the first trophic level. Consumers make up the second, third, or higher trophic levels. Each consumer depends on the trophic level below it for energy.

Ecological Pyramids Ecological Pyramids The amount of energy or matter in an ecosystem can be represented by an ecological pyramid. An ecological pyramid is a diagram that shows the relative amounts of energy or matter contained within each trophic level in a food chain or food web.

Ecological Pyramids Energy Pyramid: 0.1% Third-level consumers Energy Pyramid: Shows the relative amount of energy available at each trophic level. Only part of the energy that is stored in one trophic level is passed on to the next level. 1% Second-level consumers 10% First-level consumers Ecological pyramids show the decreasing amounts of energy, living tissue, or number of organisms at successive feeding levels. The pyramid is divided into sections that represent each trophic level. Because each trophic level harvests only about one tenth of the energy from the level below, it can support only about one tenth the amount of living tissue. 100% Producers

Ecological Pyramids The more levels that exist between a producer and a top-level consumer in an ecosystem, the less energy that remains from the original amount. Only about 10 percent of the energy available within one trophic level is transferred to organisms at the next trophic level. The rest of the energy is lost as heat energy

3–3 Cycles of Matter Photo Credit: ©Bruce Coleman, LTD/Natural Selection

Recycling in the Biosphere Energy and matter move through the biosphere very differently. Unlike the one-way flow of energy, matter is recycled within and between ecosystems.

Recycling in the Biosphere Elements, chemical compounds, and other forms of matter are passed from one organism to another and from one part of the biosphere to another through biogeochemical cycles. Matter can cycle because biological systems do not use up matter, they transform it. Matter is assembled into living tissue or passed out of the body as waste products.

3–3 Cycles of Matter The Water Cycle All living things require water to survive.

3–3 Cycles of Matter Water moves between the ocean, atmosphere, and land. This diagram shows the main processes involved in the water cycle. Scientists estimate that it can take a single water molecule as long as 4000 years to complete one cycle.

The Water Cycle Evaporation: Water molecules enter the atmosphere as water vapor, a gas, when they evaporate from the ocean or other bodies of water. Water can also enter the atmosphere by evaporating from the leaves of plants in the process of transpiration.

The Water Cycle Water vapor condenses into tiny droplets that form clouds. The water returns to Earth’s surface in the form of precipitation. Water enters streams or seeps into soil where it enters plants through their roots.

Nutrient Cycles Nutrient Cycles All the chemical substances that an organism needs to sustain life are its nutrients. Every living organism needs nutrients to build tissues and carry out essential life functions. nutrients are passed between organisms and the environment

Nutrient Cycles Primary producers, such as plants, usually obtain nutrients in simple inorganic forms from their environment. Consumers obtain nutrients by eating other organisms.

Nutrient Cycles The Carbon Cycle Carbon is a key ingredient of living tissue. Biological processes, such as photosynthesis, respiration, and decomposition, take up and release carbon and oxygen. Geochemical processes, such as erosion and volcanic activity, release carbon dioxide to the atmosphere and oceans.

Nutrient Cycles The burial and decomposition of dead organisms and their conversion under pressure into coal and petroleum (fossil fuels), store carbon underground. Human activities, such as mining, cutting and burning forests, and burning fossil fuels, release carbon dioxide into the atmosphere.

Nutrient Cycles CO2 in Atmosphere CO2 in Ocean Carbonate Rocks Photosynthesis Volcanic activity feeding Respiration Erosion Human activity Respiration Decomposition CO2 in Ocean Uplift Carbon is found in several large reservoirs in the biosphere. In the atmosphere, it is found as carbon dioxide gas; in the oceans as dissolved carbon dioxide; on land in organisms, rocks, and soil; and underground as coal, petroleum, and calcium carbonate rock.  Deposition Photosynthesis feeding Fossil fuel Deposition Carbonate Rocks

Nutrient Cycles The Nitrogen Cycle All organisms require nitrogen to make proteins. Although nitrogen gas is the most abundant form of nitrogen on Earth, only certain types of bacteria can use this form directly. Such bacteria live in the soil and on the roots of plants called legumes. They convert nitrogen gas into ammonia in a process known as nitrogen fixation.

NH3 N2 in Atmosphere NO3 and NO2 Synthetic fertilizer manufacturer Atmospheric nitrogen fixation Decomposition Uptake by producers Reuse by consumers Uptake by producers Reuse by consumers The atmosphere is the main reservoir of nitrogen in the biosphere. Nitrogen also cycles through the soil and through the tissues of living organisms.  Decomposition excretion Decomposition excretion Bacterial nitrogen fixation NO3 and NO2 NH3

Nutrient Cycles When organisms die, decomposers return nitrogen to the soil as ammonia. The ammonia may be taken up again by producers.

Nutrient Cycles Other soil bacteria convert nitrates into nitrogen gas in a process called denitrification.

Nutrient Cycles The Phosphorus Cycle Phosphorus is essential to organisms because it helps forms important molecules like DNA and RNA. Most phosphorus exists in the form of inorganic phosphate. Inorganic phosphate is released into the soil and water as sediments wear down.

Nutrient Cycles Organic phosphate moves through the food web and to the rest of the ecosystem. Organisms Phosphorus in the biosphere cycles among the land, ocean sediments, and living organisms. Land Ocean Sediments