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Overview of the key events in the history of life in the last 4.5 billion years
orign of the solar system and earth
prokaryotes
armostheric oxygen
single celled eukaryotes
musticellar eukoraytoes
animals
colonization of alnds
Humans
The fossil reocrd documents the history of life
radiometrei dating uses the decay or radiocatice isotpes as a “clock” to date them
Muletiple lines of eveidnece suggest that life arose on earth billions of years ago
earliest fosil of singel-celled life on earth date to arround 3.5 biollion years ago
eveoulitnary trees ingereed froom the DNA of living speices alsosuggests that all life shares a single celled ancestory that lived arround 3-4 billion years ago
CUrrently we hypothesize that four key processes lead to the orgin of life
abiotic sythensis of small orgnaic moleuces (acids, bases)
Abiotic sythenses of thsese small molcues into marcomolcues
packing macrmolecules into protocells
the orgin of self-replicating mocleues
Condtions on the early earth may have allowed simple organize molcules to from
many places on the early earth may have been condutive to the formation of simple molecules
Simple reactsion among ambien C O N H could have been fuled by lighting, hdrothermal vents, volcani eruptions
The miller-Urery expermient (1953) let great support to hypthesis
created constions simmilar to the earlty earth in lab
heate water, methane, ammonia, hydrogen, and applied and electral charge
oberservted the formatio of 11 of the 21 essential amino acids
Oirgin of single -celled prokaryotes
earth;s first orgnaims were single-celled prokaryotes that lived in the ocean
the earliest evidence from 3.5 billion years ago are fossiled stromatlies structres that are formed exculcey by single celled organims (still today!)
early prokaryotes were earth’s sole inhbaittnats for about 1.5 billion year
eveoultion of photosyntheseis lead to “oxygen reveoultion”
most atmoshpereic ozygen gas coems from photosythensis
when photsyhtneizing organmis similar to today’s cyanbavteria eveoled, they began to conver CO2 to O2
Dramtic increase in oxygen contetn in the atmoshpere, and condtions for celluar respiration bcome dominant
Origin of eukarotyes
Endomysis
a kinds of mcafrage didnt desotry the bacterim, used and provided portenction, stabitly coxeisted
Rise of mutleisccluar organismis
Fossile evidence and DNA sequence data seuggest that mutleucellar eukarotes merged about 1.3 biollion years ago
Mutielcelluarty allows indivudals cells to copperate and speicalize in thier functions, allow for more complez organsims
Mulitcuellary eveolved muleitpe times indiedpently
Volovciie alage most simple mulstcellar ogransims
Cmbarian eplozsion and the diverstifaction of animal life
many present day animal groups appear suddenlty in fossil formed 535-535 miillion years ago in the cmabrain preriod
this phenomen is reffered to as cmbrain explosion
Many possible cuases: increases oxygen, increases genetic complexity of organsims, climate change
Colonization of land
larger forms of life, such as fungi and plants, began to colonize land, about 500 million years ago
Arthpods were the first animals to colonize land
vertrebrated follwer later with air rbeathing and other adapations
Species extincitons
Extinction: after athrouhg sear,, no member of the speices is found alive anywhere in the world = total dispperance
Mass extienction: large number of speices, genera, and even familes become eztinct nearly simulatansely
Extion rate: rate at which speices are lost
Extiontics in the mpast
Mass ecitons are common (5 in fosssil record), family diveristy over time
Mass extinction
Paloezonic ended with thhe end=permian mass exintction
Volcanoes erupted on gran scel realses gasses
52% gamiles, 96% of speices of marine invertbreates wetn extinct
Meszozoic ended with another mass extionction
Asteriod hit earth and drasticly changed climate
mamals rose in diveristy to rpelace dinsouars