Lecture Two Flashcards
What organisms followed the anaerobic autotrophs and when did this occur?
Photoautotrophs with oxygenic photosynthesis. Developed around 3.5 billion years ago.
What was the key innovation of photoautotrophs that gave them an advantage over the anaerobes?
Their use of water as the electron donor (water is split). The advantage came about because water was very plentiful. Oxygen is a by-product of this (hence the term oxygenic photosynthesis).
What were the first fossil organisms?
Cyanobacteria, occurred in stromatolites 3.5 BYA.
How are stromatolites formed?
The photosynthetic bacteria grows in mounds that are eventually covered by debris (primarily Calcium carbonate which precipitates out of the water). As the bacteria get covered they die, while new bacteria grows on top of the debris. This occurs again and again, producing a fossilized layered rock that is able to preserve.
What Canadian reserves have plenty of stromatolites?
Red Lake, Ontario.
Steep Rock Lake, Ontario.
Yellowknife, NWT.
Where do modern stromatolites grow?
Shark Bay, Western Australia. There is approximately 3 billion cyanobacteria/m2.
Where are modern stromatolites found?
Generally in hot or hyper-saline environments where they are free from grazing and burrowing animals (generally reach 1.5 metres high, while ancient ones can get up to 10 m)
Where Cyanobacteria the first life forms?
Unlikely, however they are likely the first life form that had hard parts that could fossilize.
How did oxygen appear in the atmosphere?
Ferrous iron suspended in solution was very plentiful in ancient anoxic oceans. Once oxygenic photosynthesis started with the advent of Cyanobacteria, oxygen accumulated in the atmosphere and the surface waters of the ancient seas. This resulted in the oxidation of ferrous iron to ferric iron in these surface waters.
Ferric iron, with oxygen attached, precipitated to the sediments - leaving banded iron formations. By 2 BYA the ferrous iron within the oceans had largely been precipitated to the ocean floor.
What is the iron content of the oceans like today?
Currently very low in solution because most of it has been locked up in sediments following oxidation.
Is there more oxygen in the atmosphere (currently) or in banded iron formations?
There is currently 20x more oxygen in BIFs than in the atmosphere as a result of billions of years of oxygen production by photosynthesis.
What did early biodiversity on earth consist of from 3.5 BYA to 2.2 BYA?
Only of prokaryotes.
How long have Cyanobacteria occupied the earth?
For at least 3.5 BY and had been the dominant life form for more than 1.5 BY.
What three effects did the build up of oxygen in the atmosphere have?
- A rapid expansion in the biodiversity of aerobic microorganisms (with a concurrent reduction in anaerobic prokaryotes).
- The first ice age (snowball Earth)
- Providing the atmosphere needed for the next major evolutionary step (origin of eukaryotes)
What major extinction even is not included in the major five and occured 2.2 BYA?
The Great Oxygenation Event