Lecture 3 History of life on earth Flashcards
exam
Hypothesis
Physical and chemical processes could have produced simple cells
RNa Hypoothsis 1st step
The biotic synthesis of small organic molecules
RNA Hypothesis 2nd step
Joining of these small molecules into macromolecules
RNA Hypothseis 3rd step
packaging of molecules into “protocells”
Rna hypothesis 4th step
the origin of self-replicating molecules
- first genetic material probably RNA because it can from 3d shape and can self replicate
Monomoers
single
amino acid
nucleotides
sugars
poly
Chain
proteins
carbons
nucleic acids (Dna, RNA)
Hydrothermal vents
break in earths crust, bottom of the ocean, release geothermically heated water
Vents and early life
release hot water with high pH (basic)
surrounded by cool water ( acidic)
vents are made of porous rock
ph difference gives rise to proton gradient = main source of energy
Key event in life’s history
paleozoic (542-251 mya)
Mesozoic ( 251-655 mya)
Cenozoic ( 655-today)
- First unicellular organisms
3.5 bya
Stromatolites layered rocks shows earliest prokaryotes
- Oxegen revolution
atmospheric o2 gas comes from living organisms which is a byproduct of phtosyncthesis which becomes saturated by the ocean and the ocean releases oxygen to the atmosphere.
- First eukaryotic : endosymbiosis
Some euk organelles arose when small props began living inside larger cells
- First multicellular organisms
some euks are multicellular
allows for increased diversity
descendants include plants, animals, fungi
- Cambrian explosion
many animal groups appear “suddenly”
increased predators = defensive mechanisms emerged
- Colonization of land
adaptations include :
1) prevent dehydration
2) allowing for reproduction
most succesful animals are the anthropoids
Mass extinctions
loss of large # of species due to global environment change
5 in last 500 mya
50 % of marine species wiped out
cretaceous –> 50% of plants , marine , terrestiral , dino were wiped out
6th mass extinction
100-100 x faster than usual
often coorelates with increawse in global temps
over in 100-1000 years
Consequences of mass extinctions
change course of evolution
5-10 mya for biodiversity to recover
adaptive radiation
follows mass extinctions
period of evo change during which orgs form new species filling in empty ecological roles
Features shared by all cells
prokaryote- simple , small
euk- larger , complex
contain cytoplasm
ribosome transfer rna
carry out similar types of metabolism
dna is genetic material
what make cells different
size
location of dna ( euk nuk, prok cyto)
membrane bound organelles ( euks only)
cell wall
ribosomes
cytoskeleton (euk)
evidence for endosymbiosis
circular dna
mechanisms of growth / division
compnents of inner membrane
size
Development of endosymbiosis
1) capture of bacterial cells (prokaryote) by archean cell
2) symbiotic relationship = more efficient energy production
3) bacterial cell lost ability to be free living= mitochondria + chloroplasts