The Law of Conservation of Energy Energy CANNOT be created or destroyed, but only changes forms.
Biogeochemical Cycles Bio Life Geo Earth Chemical Elements, compounds, substances Cycle Series of events repeated in the same order
Biogeochemical Cycles Chemicals move from living things (biotic) to non-living (abiotic) things and back.
Important Elements Carbon 4 valence electrons Good at bonding Macromolecules
Important Elements Hydrogen Provides energy transfer Photosynthesis Water
Important Elements Nitrogen Important part of amino acid Builds proteins Nitrogen bases in DNA
Important Elements Oxygen Water Cellular Respiration
Important Elements Phosphorus Phospholipid Cell Membrane Sugar and Phosphate Backbone DNA ATP Adenosine Triphosphate
Water Cycle
Water Cycle Essential to ALL living organisms 97% of water is in oceans 2% in glaciers and polar ice caps 1% in lakes, rivers, and groundwater
Key Processes Evaporation of liquid water by solar energy Condensation of water vapor into clouds Precipitation Water hitting the earth Rain, snow, sleet, hail, etc. Transpiration Water evaporation through plants Surface and groundwater flow Returns water to the oceans
Runoff and groundwater Percolation through soil Evapotranspiration from land Precipitation over land Movement over land by wind Evaporation from the ocean Precipitation over the ocean
Precipitation over the ocean
Evaporation from the ocean
Movement over land by wind
Precipitation over land
Percolation through soil
Evapotranspiration from land
Runoff and groundwater
Runoff and groundwater Percolation through soil Evapotranspiration from land Precipitation over land Movement over land by wind Evaporation from the ocean Precipitation over the ocean
Carbon Cycle Carbon absorbs heat energy. Increase CO 2 in the atmosphere increases global temperature creating the Greenhouse Effect .
Biological Importance Carbon is the essential organic element that forms molecules essential to all organisms
Key Processes Photosynthesis by plants and phytoplankton Removes CO 2 from the atmosphere Cellular respiration by producers and consumers Adds CO 2 to the atmosphere Burning of fossil fuels and wood Adds LOTS of CO 2 to the atmosphere Fossil fuels include coal, oil, natural gas, organic soil Decomposition Adds CO 2 to atmosphere
CO 2 in Atmosphere Photosynthesis Consumer Decomposition Photo- synthesis Phyto -plankton Burning of fossil fuel and wood Soil Movement Cellular Respiration
CO 2 in Atmosphere
CO 2 in Atmosphere Photosynthesis Photo- synthesis Phyto -plankton
CO 2 in Atmosphere Consumer
CO 2 in Atmosphere Cellular Respiration
CO 2 in Atmosphere Decomposition
CO 2 in Atmosphere Burning of fossil fuel and wood
CO 2 in Atmosphere Soil Movement
CO 2 in Atmosphere Photosynthesis Consumer Decomposition Photo- synthesis Phyto -plankton Burning of fossil fuel and wood Soil Movement Cellular Respiration
Nitrogen Cycle
Biological Importance Nitrogen is part of amino acids, proteins, and nucleic acids and is often a limiting plant nutrient. 78% of the Earth’s Atmosphere
Nitrogen Fixation Plants cannot use nitrogen gas from the air to make organic compounds for themselves or other organisms. Nitrogen (N 2 ) must be converted to a form called nitrates (NO 3 ) by nitrogen-fixing bacteria Plants can absorb nitrates through their roots.
Nitrogen-Fixing Bacteria Live in soil and roots of legumes Peas Beans
Decomposers Break down dead plants and organisms Release nitrogen in the form of ammonium ions (NH 4 + ) Nitrifying bacteria change the ammonium into nitrates Some nitrates are changed back to nitrogen gas by denitrifying bacteria
The Role of Bacteria in the Nitrogen Cycle Nitrogen-fixing Bacteria Converts nitrogen (N 2 ) to nitrates (NO 3 ) so that it can be used by plants Decomposers Break down dead plants and organisms. Release ammonium ion (NH 4 + ) Nitrifying Bacteria Convert ammonium (NH 4 + ) to nitrates (NO 3 ) to be used by plants. Denitrifying Bacteria Convert ammonium (NH 4 + ) to nitrogen (N 2 )