History of Life Flashcards
(111 cards)
Timeline for history of life
Timeline has changed a lot BUT only push back never push forward
How long has all of this been going on
The change from sheep hoof mammals to blue whales took place over 50 million years
Before then = history of animal life on earth
- Have huge amount of time before braod scale change in mamales
END – ALL of multicellular animal life - small in history of earth
- Animals are small in history of earth
All animal life Vs. All life
All animal life = result of 600 MU of evolution BUT the history of life is 6X longer –> Evolution of biochemical pathways is longer than history of animal life as whole
How old is earth
4.85 BYO (based on radiometric dating)
How did earth form
Earth formed out of the Sun’s primordial dust/debris disk
Debris in orbit around sun (early starts as dust then collapse on own gravity and form planets)
Hadeon Eon
Start of earth – for the first few hundred million years conditions were extremley unstable
Earth started very hot and was constaly bombarded by objects in the solar system
- Earth was getting hit by lots of stuff (smashing = unstable)
- Early collison with ither small thing created the moon (part of
Creation of moon
Part of earth was knocked off to space around earth and made moon
Life during Hadean
Earth was unstable + hot = not hospitable
Everything = very volatile = not much chance for life to get started
Archean eon
Overall: Earth started to cool = get solid crust + formed continents and oceans
- Still more voltile (volcanism is active)
- Earth starts to look somewhat more recognizable
- Still a lot of bombardment from space (metiores)
When do we start to get life
Archean – start to get life
- Get life early –> within 100 MY
Stability started 4 Billion YO and by 3.7 BY get signs of biologic activity
How did we get oceans
During Archean – have commet bombardment = where you get most water –> filled oceans
First signs of biolgic actiivuty
Get signs in archean 3.7 BYO – shift in carbon isotopes = suggests biochemical processes drive isotope
NOT direct evidence but compelling indirect evidence
Fossile evidence of life
May date back further – doesn’t get to 3.7 BY but gets close
In fossils = see geologic formatting –> Interpret as microbial communities that date 3.5 BYO
- Not individual microfossils BUT overall patterns are similar to microbial communities we see today (Similar stromatotes)
- Have stromatolites in same area of the wrold
- Found arcgean rock that suggests the presence of micrbial communities 3.5BYO
Stomatolies
Early evidence for life 3.5BYO
Lay fine layers of silicae + is laminated in a stratified fashion
- Similar structure from 3.5BYO
Shows that orgin of life in complex microbial communities
Microfossils
Some oldest unambigous microfossils date to 3.5BYO
Give direct evidence of indiviual organisms going back nearly 3.5 Billon years
Evidence of life in Archean
IS SCANT – have isotopes + Starting in microbial communities + microfossils
- More recent evidence of microbes are more readily avalble
Evidence is scarce because rocks from a long tine ago are rare on the surface BUT in places where we do have them we see signs of living world
Proteozoic evidence of life
Get more evidence of microbial communities (evidence is more readily avalible)
- Found strong evidenve of thruving microbial communities for 2 BY
Vs.
Archean – solid traces of life are rare from the archean BUT know life starts
Proterozoic eon
Start to get solid traces of life (2.5 BYO)
The transition to the proteozoic marks a shift in the fossil record to forms that can unabigously tied to modern forms
- Have transition from scant to see life 2-2.5 BYO – life we can connect to life today
Example evidence in Proterozoic
Proteocoin old = very similar to modern red algea (modern microbes that we have today)
What happened during Proteozoic
The chemistry of the atompshere and the ocean became more like they are today + have organisms similar to organisms that we have today
Change = due to action of life – driven by living world itself
Example - Great oxygentaion event
Great Oxygenation event
Started in the Proteoic
Early microfossils were similar to photosynthetic microorganisms today –> the photosythetic start to proloferate = have change on earth
Photosynthesis = Energy + Water –> Glucose + O2
- Photosynthetic take CO2 out and spit out O2 = profound effect on overall earth systems as a whole
- See increase in O2 in ocean first
Length of Great oxygenation event
LONG - 2.4 - 1.8 BY = took 600 MIllion years – same amount of time as ALL animal life
Evidence of Oxygenation
Seen in ocean first – evidence = banded iron formations
- See fossil evidence of photosynthestic microbes in Proteozoic
O2 in coean increase = binds with Iron in ocean = bind all Iron out = iron sinks to sedimemnt and O2 builds again
Rocks = have layers of Iron oxide then other sediemnts building as make O2
- 600 Million years to get all Iron out of ocean – Since no Iron in ocean = O2 proliferates to atmosphere = get O2 in atmosphere
Action of living world + Atmosphere
Action of living world influenced atmosphere that plays into living world