Cycles of Matter In an Hour or Less!!!!. Recycling in the Biosphere  Unlike the one-way flow of energy, matter is recycled within and between ecosystems.

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Presentation transcript:

Cycles of Matter In an Hour or Less!!!!

Recycling in the Biosphere  Unlike the one-way flow of energy, matter is recycled within and between ecosystems. 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 into living tissue or passed out of the body as waste products.

The Water Cycle All living things require water to survive. The Water Cycle

Water molecules enter the atmosphere as water vapor, a gas, when they evaporate from the ocean or other bodies of water. The process by which water changes from a liquid form to an atmospheric gas is called evaporation. 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. The Water Cycle

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.  Similar to water, nutrients are passed between organisms and the environment through biogeochemical cycles.

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. Biogeochemical processes, such as 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 CO 2 in Atmosphere Photosynthesis feeding Respiration Deposition Carbonate Rocks Deposition Decomposition Fossil fuel Volcanic activity Uplift Erosion Respiration Human activity CO 2 in Ocean Photosynthesis

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.  Other bacteria in the soil convert ammonia into nitrates and nitrites.  Once these products are available, producers can use them to make proteins.  Consumers then eat the producers and reuse the nitrogen to make their own proteins.

Nutrient Cycles Bacterial nitrogen fixation N 2 in Atmosphere NH 3 Synthetic fertilizer manufacturer Uptake by producers Reuse by consumers Decomposition, excretion Atmospheric nitrogen fixation Uptake by producers Reuse by consumers Denitrification Decomposition, excretion NO 3 and NO 2

When organisms die, decomposers return nitrogen to the soil as ammonia. The ammonia may be taken up again by producers. Other soil bacteria convert nitrates into nitrogen gas in a process called denitrification. This process releases nitrogen into the atmosphere once again. Nutrient Cycles

If a nutrient is in short supply, it will limit an organism's growth. When an ecosystem is limited by a single nutrient that is scarce or cycles very slowly, this substance is called a limiting nutrient. Nutrient Limitation