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B15 Revision - Evolution - Coggle Diagram

- - - - Animalia
      - Protoctista
      - Plantae
      - Prokaryote
      - Fungi
  - - - eubacteria
      - archaebacteria
- - - - Mud fossils
      - Amber fossils
      - Ash fossils
      - Ice fossils
      - Rock fossils
    - - Types of Formation
        
        Hard parts that do not decay easily such as teeth and bones
        
        Whole organisms preserved in ice (ice fossil)
        
        Hard parts of an organism replaced by other minerals. (most common, rock fossil)
        
        Traces of plants or animals are left behind (mud fossil)
      - Formed:
        
        Parts of organisms that have not decayed because one or more of the conditions needed for decay are absent (oxygen, temperature, moisture). When parts of the organism are replaced by minerals as they decay. As preserved traces of organisms such as footprints burrows and rootlet traces
    - - Soft tissue will never be a fossil
      - Can be destoryed
      - Need specific conditons
- - - - melting sea ice flooded the seas and ice and caused a sea temperature drop of 9 degrees which caused a mass extinction.
      - This was proved from unexpected fossils changes in Norway
      - 137 million years ago
    - - There was a crater 180km in diameter with debris flung into the sky it blocked the sun making everywhere dark causing plants to die, the animals eating the plants to die and the carnivores to die, the asteroid also caused fires, tsunamis and earthquakes when it crashed.
      - They proved this in 2010 though iridium being found in the geological records 65 million years ago
      - 65 million years ago - Chicxulub Mexico
- - - - Methicillin Resistant Staphylococcus Aureus