By the end of section 2.2 you should be able to understand the following: Earth’s biosphere is like a sealed terrarium, where all nutrients and wastes.

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Presentation transcript:

By the end of section 2.2 you should be able to understand the following: Earth’s biosphere is like a sealed terrarium, where all nutrients and wastes are constantly recycled. The carbon cycle, nitrogen cycle and phosphorous cycle move nutrients in and out of ecosystems. Human activities such as land clearing, agriculture, industry and motorized transportation can affect nutrient cycles.

Nutrient cycles the flow of nutrients IN and OUT of the land, ocean, atmosphere and deep rock. The health of our ecosystems depends on the balance of: Carbon, Nitrogen, Phosphorous, Hydrogen and Oxygen C N P H O

NutrientFacts How it changes form Human Influence

A. Carbon Facts : Carbon is found in all living matter. Places that carbon is found are called stores or sinks Short Term StoresLong Term Stores living things in water & on land rotting tissue of plants / animals atmosphere (air) ocean (dissolved in the water) underground (oil, gas, natural gas and coal) sedimentary rock ocean floor (old shells) (limestone)

B. How Carbon Changes Form: 1. Photosynthesis (in plants, algae and cyanobacteria) CO 2 + H 2 O + sunlight  C 6 H 12 O 6 + O 2 2. Cellular respiration (in cells of all living things) C 6 H 12 O 6 + O 2  CO 2 + H 2 O + ENERGY (energy is used for growth, repair etc.) 3. Decomposition (rotting) – done by bacteria/fungi cellulose  CO 2

4.Ocean mixing: moves CO 2 around the world - CO 2 sinks in cold ocean waters  flows to the warm equator and evaporates into the air. 5.Combustion: (burning, engines, volcanoes, forest fires) fossil fuels + O 2  CO 2 + H 2 O + ENERGY (oil, gas, natural gas, coal)

1. Burning Fossil Fuels  CO 2 in atmosphere has increased 30% in past 160 years.  In the 160,000 years before that, it only increased 1- 3%.  Carbon is removed from long-term storage as we mine coal & drill for oil and gas.  C O 2 is also a greenhouse gas, (traps heat in atmosphere) 2. Removing Trees  Trees absorb C O 2, so when they are cut down, C O 2 is released into the air.  Other crops don’t remove as much C O 2

A. Nitrogen Facts  Makes up DNA & proteins (muscle function).  Help plants grow. Where Nitrogen is Found:  Atmosphere (78% is N 2 )  Oceans  Organic matter in soil  Lakes, marshes, organisms

B. How Nitrogen Changes Form: - N 2 is not usable by plants or animals, so it has to be converted to other forms. Plants can use NO 3 - (nitrate) and NH 4 + (ammonium) 1. Nitrogen Fixation Lightning changes N 2 (nitrogen gas)  NO 3 - (nitrate). Rain washes nitrate into soil. (small amount) Bacteria in soil (rhizobium) & cyanobacteria in water, change N 2 (nitrogen gas)  NH 4 + (ammonium). 2. Nitrification 2. Nitrification (done by nitrifying bacteria). NH 4 + (ammonium )  NO 2 - (nitrite)  NO 3 - (nitrate)

3. Uptake NO 3 - is sucked into plants & used for growth. Herbivores eat plants & use N for making proteins & DNA. 4. Denitrification 4. Denitrification (done by denitrifying bacteria & volcanic eruptions) NO 3 -  N 2

C. Human activities affect the nitrogen cycle. in The amount of nitrogen in the ecosystem has doubled in 50 y. due to: 1. Burning fossil fuels & sewage treatment. NO & NO 2 are byproducts 2. Land-clearing by burning. acid rain is formed which contains nitric acid (HNO 3 ). 3. Overfertilization NH 4 + & NO 3 - leach into soil & waterways. huge growth in aquatic algae = eutrophication These algal blooms use up all CO 2 & O 2, block sunlight & produce neurotoxins which poison and kill many aquatic organisms.

A. Phosphorous Facts Phosphorous is a part of the molecule that carries energy in cells ( ATP ). Phosphorous helps root growth, stem strength and seed production. In animals, phosphorous is important for strong bones. B. Where Phosphorous is Found: Not in atmosphere, but in phosphate rocks (PO 4 3–, HPO 4 2–, H 2 PO 4 ) and sediments on the ocean floor.

B. How Phosphorous Changes Form. 1. Weathering (breaking down rock into smaller pieces). a) Chemical weathering: acid rain or lichens releases phosphates (PO 4 3- ) b) Physical weathering wind, water and freezing release the phosphates. 2. Uptake : plants suck up PO 4 3-, then are eaten by animals. 3. Decomposition : Bacteria break down organic matter & phosphorous is returned to soil. 4. Geologic Uplift : when rocks under the ground are pushed up  mountains  weathering.

C. Human activities affect the Phosphorous Cycle. 1. Mining : increases Phosphorus in ecosystems quickly. 2. Slash-and-burn forest practices: turns Phosphorus into ash, which runs into waterways.

Any significant changes to any of these nutrients (C, H, O, N or P) can greatly impact biodiversity. 1. Carbon cycle changes  climate change & global warming. 2. Too much nitrogen can allow certain plant species to out-compete other species. 3. Decreased levels of phosphorous  slow growth of algae (important producers). Take the Section 2.2 Quiz