Lecture 4 - Origin of prokaryotes & eukaryotes Flashcards
How are fossil stromatolites (rocks) evidence for prokaryotes life?
found in rural Australia - Sharks bay - outside of rock covered in bacteria which sticks to sediment. The bacteria migrates to the outside of rock to keep photosynthesising
- only over in hyper saline (high salt) - no fish in these area - as they would eat bacteria
- aerobic bacteria on outside of rock - anaerobic bacteria onside
What is a stromatolite?
colony of bacteria
How is fossil microorganisms evidence for prokaryote life?
- identical to modern bacteria (have been preserved)
- silt stones contain grains of sand, as well as skeletons of bacteria. If sand is dissolved, the bacteria pops out (these are called acritarchs)
How can carbonaceous matter can be identified chemically as the product of ancient life?
rubisco prefers a light carbon isotope. Rubisco preferentially fixes carbon 12, as a result, high levels of carbon 12 found in fossils is a sign of life
When did RNA turn into prokaryotes?
3.5 billion years ago
Have prokaryotes changed a lot?
- prokaryotes have remained consistent
- prokaryotes remained relatively unchanged to the present day - they dominated the planet for some 2 billion years
How did oxygen content in oceans increase?
3.5 billion years ago, prokaryotes advanced into the ocean. This consisted of complex & diverse communities of stromatolite form ping communities on the floor of shallow seas & free living prokaryotes floating around in the oceans.
- both communities include Cyanobacteria that produce oxygen as a biproduct of their photosynthetic metabolism
- a lot of oxygen is left as a biproduct, as a result
Explain how early oxygen sinks?
- Volcanic gases that compromised the early atmosphere readily combine (H –> H2O)
- Dissolved iron that scavenged O2 to form BIF (banded iron formations) - this is because the oceans release rust, as oxygen reacts with iron causing rust and falling to the bottom of the oceans.
- Microorganisms carrying out aerobic respiration (O2 + organic matter = H2O + CO2 + cellular energy). Some early organisms were no doubt facultative, respiring aerobically when O2 was available, but switching back to aerobic fermentation when it was in short supply.
What is evidence for banded iron formations?
banded iron formations were present till around 2 billion years ago - this suggests that the oxygen were used up
What is evidence for pyritic conglomerate (pebbles)?
also disappeared around 2 billion years ago - when they react with oxygen they disintegrate
What is evidence for red beds?
red beds require oxygen to form and they formed around 2 billion years ago
What event happened in the atmosphere around 2 billion years ago?
The atmosphere can then be said to go from an anaerobic atmosphere to an aerobic atmosphere around 2 billion years ago.
What coincided with the change to an aerobic atmosphere 2 billion years ago?
the Huronian Ice Age caused by the elimination of atmospheric methane during the GOE
What are the 2 considerations when thinking about the origin of eukaryotes?
- when were conditions suitable for the origin of eukaryotes
- fossil evidence for eukaryotes
When could eukaryotes develop?
when the world became aerobic - as oxygen is toxic & poisonous to most eukaryotes
- 2 billion years ago - some acritarchs are large enough to suggest that they were eukaryotes
- there is fossil evidence of eukaryotes dating back 2 billion years