Conditions For Life On Earth Flashcards
Features of earth that created suitable conditions for life
Mass
Distance from sun
Axis of rotation
Speed of rotation
Magnetic field
Early conditions on earth that allowed life to develop
Presence of liquid
Temperature range
Atmospheric gases
Solar insulation
Presence of atmosphere
- Large mass and gravitational pull which keeps the atmosphere close
- Contains important gases: CO2, N2 AND CH4
- Temperature and pressure means water is in liquid form
Solar Insulation
Suitable temperature range for enzyme action and water in liquid state
Provides energy for photosynthesis
Amount absorbed depends upon the albedo of the surface
Position in the solar system
- 3rd rock from the sun
- Temperature warm enough for enzyme action
Earth orbital behaviour
- Rotation and tilt of the earth on its axis and its orbit around the sun
- Controls daily and seasonal variations in isolation and temperatures
- Enough day length to stop temperature extremes and light for photosynthesis
Presence of the magnetosphere
Provides protection from solar radiation
Produced by the movement of earths molten core
Presence of liquid water
Solvent water
Transport within organisms
Temperature controls
Anomalous expansion on freezing (most dense at 4°C)
High specific heat capacity
Aquatic habitats
Absorption of UV radiation
Temperature range
Temperatures between 0°-35°
Atmospheric gases
Carbon dioxide for photosynthesis and the synthesis of carbohydrates, proteins and lipids
Nitrogen for protein synthesis
How life on earth caused environmental change
Atmospheric oxygen
Carbon sequestration by photosynthetic organisms
Biogeochemical
Transpiration
Limitations of early methods
• Lack of ancient historical data.
• Limited reliability of proxy data for ancient conditions.
• Limited coordination between researchers.
• Lack of sophisticated equipment for accurate measurements.
• Inability to measure many factors.
• Lack of data collection in many areas.
• Reliance on proxy data, eg dendrochronology, pollen analysis.
Improved methods
• Collection of long-term data sets.
• The use of electronic monitoring equipment.
• Gas analysis of ice cores.
• Isotope analysis of ice cores.
• Improved carriers for monitoring equipment, eg helium balloons, aircraft, satellites.