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the pre-biotic atmosphere
no life, only traces of oxygen, high methane and carbon concentrations
high methane concentrations due to…
intense volcanic activity and meteorite bombardment
high carbon concentrations due to…
emissions from volcanos
higher temperature and light penetration
carbon dioxide and methane are heat-traping greenhouse gasses ex. hot springs and hypothermal vents in oceans
the stratospheric ozone layer
currently protects us by absorbing uv would not have existed because of the lack of oxygen
vents
are commonly found near in volcanically active areas. ALong with heat energy the vents secrete a ready support of reduced inorganic.
difference between living and non-living
living things use energy to keep themselves in a highly ordered state, are self-sustaining, passing the ability to maintain a highly ordered state to offspring, can divide to produce more cells,
spontaneous generation of life
the first cells must have arisen from non-lilving material or life was transported here from elsewhere in the universe
reducing atmosphere
low oxygen, only methane, ammonia, water vapor, carbon dioxide, it favored chemical reactions that add electrons to molecules
primary energy sources on early earth that facilitated chemical reactions
solar radiation
geothermal heat from volcanic activity
electrical energy from lightning.
water
acted as a solvent for chemical, reactions, provided a medium for molecules to move and collide, helped stabilize formed compounds
simple organic molecules that could form under pre-biotic conditions
amino acids
nucleotides
simple sugars
early earths environments that facilitated chemical reactions
hydrothermal vents
tidal pools
volcanic hot springs
why spontaneus formation of organic molecules is unlikely on modern earth?
presence of oxygen, which breaks down organic molecules
ozone layer blocking uv radiation
stabilized environmental conditions
J.B.S Haldane hypothesis
variety of organic molecules are made when ultraviolet light acts on a mixture of water→ based on the assumption that the atmosphere contained water vapour, carbon dioxide and ammonia
Stanley Miller and Harold Urey experiment
they mixed methane, hydrogen and ammonia and added water vapour.Then used electrical discharges to stimulate lightning. Mixture was allowed to cool and after one week simple amino acids and complex oily hydrocarbons formed.
Vesicles
small droplets of fluid enclosed in a membrane mainly composed of phospholipids
exosomes
extracellular vesicles
phospholipid molecule
hydrophilic head- attracted to water because its polar
hydrophobic tails- attracted to non-polar substances
when they are mixed with water phospholipids naturally form spherical bilayers
amphipathic molecule
molecule with both hydrophilic and hydrophobic parts
RNA
can store information in the same way as DNA but it is self-replacing and it can act as catalyst because it can form complex three-dimensional structures that can undergo precise interactions with other molecules
ribozymes
ribonucleic acid enzymes, they have the ability to catalyze specific biochemical reactions, including RNA splicing in gene expression.
The RNA world hypothesis
suggests that RNA may have been important in the evolution of pre-biotic self replicating systems
Species using the same code
they inherited it from a common ancestor
convergent evolution
evolution of strikingly similar structures in organisms that do not have a recent common ancestor
LUCA
the last universal common ancestor
natural selection
extinction of other forms of life due to competition from LUCA or species that evolved from LUCA
Palaeontology
the scientific study of ancient life through fossils like rocks, it has provided the priceless evidence about the pathways of evolution, so it is an obvious approach for dating the first living cells and the last common universal ancestor
The Strelley Pool Formation
3.5 to 3.0 billion-year-old rock layer in Western Australia, large structures that resemble fossilized stromatolites have been discovered in these rocks
stromatolite
It forms when clusters of cyanobacteria in shallow seawater trap sediment and secrete calcium carbonate, slowly building rocky mounds over thousands of years. However, simpler life forms exist than the bacteria that form stromatolites, so we can deduce that earlier cells must have existed before 3.42 billion years ago.
why there are no rocks older than 4gya?
because tectonic processes continuously destroy them by subduction and create new rock from magma.
sedimentary rocks
when rock is ground down by erosion the hardest fragments can persist and become part of new sedimentary rocks
planet theia
first living cells existed soon after the earth is thought to have been impacted by the planet Theia. This impact would have sterilized the earth and led to formation of the moon.
bacteria and archea
groups of organisms that originated early in the history of life in which researchers have identified genes that occur widely
Luca had a gene
if an evolutionary tree is constructed for a shared gene and it matches the accepted evolutionary tree for bacteria and archea deductive reasoning tells us that a gene has been inherited from a common ancestor of bacteria and archea.
genes in LUCA
355 gene filaments needed for anaerobic metabolism and for fixing carbon dioxide and nitrogen, from this we can deduce that LUCA lived in an environment with high. concentrations of hydrogen, carbon dioxide and iron (found in hydrothermal vents)
hydrothermal vents
cracks in the earth’s surface,, characterized by gushing hot water carrying reduced inorganic chemicals such as iron sulfide.
the hydrothermal fluids
emerge at 60 to 90 degrees
contain high concentrations of hydrogen, methane, ammonia and sulfides → represent readily accessible supplies of energy which early cels would have needed to assemble carbon compounds into polymers