Theme 5C: The history of life Flashcards
What was the Earth’s early atmosphere like?
- Originally very little oxygen
- Oxygen did not exist in a molecular state
What type of energy input was used to transform some of the compounds in the earth to form the first organic compounds?
- Lightning!
- This was replicated in the Urey-Miller experiment
When was there a rapid expansion of life?
- During the Phanerozoic eon.
Where were some of the first prokaryotes found?
- Found in stromatolites due to the presence of cyanobacteria
- Stromatolites appear in fossils dating back to 2.7 billion years ago, decline in abundance by 500 million years ago
How did cyanobacteria contribute to the change in the Earth’s atmosphere?
- Cyanobacteria obtain their energy through photosynthesis, so gaseous oxygen is produced as a by-product
- Converted the Earth’s atmosphere into an oxidizing one
- Rusting of the Earth
- Led to the near-extinction of oxygen-intolerant organisms
What was the great oxygenation event?
- When free oxygen accumulated in the atmosphere about 2.5 billion years ago, with an increase about 850 million years ago
What is some of the major evidence regarding the great oxygenation event?
- Banded iron formation in different rocks
- Major changes in the number of rock types formed after this event
What could explain the long gap before oxygen was able to develop in the atmosphere?
- There was a long period of anoxygenic photosynthesis
- The oxygen that was being produced by the cyanobacteria was most likely being absorbed by the ocean, changing the chemistry of the ocean
What’s the endosymbiotic theory?
- The origin of key eukaryotic organelles result of a symbiosis between separate single-celled organisms
What’re some of the major evidence supporting the endosymbiotic theory?
- Organelles are bound by membranes
- Organelles have their own DNA
- Mitochondrial DNA sequences similar to bacteria/chloroplast DNA sequences similar to those of some cyanobacteria
What’s the Paleozoic era?
- One of the major episodes in the history of life
- When the Cambrian explosion occurred, invasion of land, the appearance of gymnosperms, major groups of tetrapods
What was the Cambrian explosion?
- Rapid appearance of many groups of organisms about 530 million years ago.
- Preceded by the appearance of small shell parts (calcium carbonate was more abundant)
- Unusually high number of sites with soft-body preservation
- Includes evidence of arthropods, echinoderms, and a large number of extinct forms
- Features of many modern groups started to apear such as mouths, heads, eyes, and legs
Why was there such an increase in oxygen in the atmosphere after the Cambrian explosion?
- Eukaryotic algae developed
Why was there such a high rate of mutations in organisms found during the Cambrian explosion?
- The organisms do not have the same proofreading capabilities that we have now, so many mutations were able to occur, creating a lot of variation among the species.
What is mass extinction?
- When the rate of extinction greatly exceeds the rate of speciation (i.e., more than 75% of known species in a geographically short interval)