History Of Life Flashcards
Macroevolution
occurs over large - scale time
Origin of key biochemical processes
Emergence of the first terrestrial vertebrates
How did life originate?
Biochemical and physical processes on early earth, aided by natural selection gave rise to small simple cells
4 step process
The abiotic synthesis of small organic molecules
Organic molecules are being synthesized by abiotic sources
Miiler - Urey (1953) university of Chicago
Using means, ammonia, hydrogen, and water with lightning as an energy source
were able to incorporate carbon into organic compounds
Depended on lightning
Required a source of electrons
Juan Oro (1961) -
showed that amino acids could be made from hydrogen cyanide and ammonia in an aqueous solution
Large volume of adenine
Both experiments relied on reduction
Required a reducing atmosphere to make molecules
Small pockets of atmosphere around volcanoes and deep sea vents that were reducing
Meteorite - chondrites - 1-2% of their composition is carbon, supports existence of amino acids outside biological systems
From small molecules to macromolecules
Macromolecule: single or identical monomers
Amino acids and RNA nucleotides when dripped onto a substrate (sand, clay, or rock) spontaneously form polymers
Polymer of amino acids - polypeptide
Polymer of RNA nucleotide - polynucleotide
May be precursors of modern day proteins of RNA
Protocells
Life requires reproduction and metabolism
Self-replication molecules
Metabolism-like source of small molecules
Appeared together as protocells
Protocells will form spontaneously from organic macromolecules
Liposomes: type of vesicle that form when lipids are added to water
Montmoorilonite (soft mineral clay)
Increases rate at which vesicles form
Vesicles can reproduce and can carry out basic metabolic reactions
If they absorb RNA and other organic molecules
Origin of self-replicating molecules
RNA can carry out a # of enzymatic functions
RNA catalysts = ribozymes - complementary copies of small pieces of RNA - nucleotides available
Natural Selection can act on pieces of RNA
RNA with a particular nucleotide sequence may be:
1. more stable
2. Can replicate faster with fewer errors
More descendants that contain RNA molecules will be produced
Continued replication - mutations and errors can occur - differences in nucleotide sequence - more stable molecule
RNA - DNA
DNA is more stable than RNA - because of its double helix
Fossil Records
Document the history of life
Show changes in types of organisms that dominated life on earth
Sow that organisms of the past are quite different than today’s organisms
Show that organisms that were once common are now extinct
Show how new organisms arose from pre-existing organisms
Incomplete: doesn’t show all evolutionary change
1. Many organisms are not fossilized or preserved
2. Fossils have been destroyed due to geological processes (earthquakes/volcanic eruptions)
3. Fossils not found yet
Dating of fossil and rock
Soil sediments are layer down over time
Some organisms are fossilized and sediments are turned to rock
Can look at rock layers and determine relative age of fossils
Sequence does not tell actual/absolute age - radio metric dating - based on decay of radioactive isotopes
Parent isotopes: decay to daughter isotopes at a constant rate
Rate of decay is measured in half - lives - amount of time for 50% of the parental isotope to decay
Accumulating isotopes
Carbon 14 decays & carbon 12 doesn’t
To date fossils:
Use ratio of C 14 + C 12
Old fossils:
1. Have isotopes with short half - lives — none to measure
2. Fossils are found in sedimentary rock - can be difficult to use indirect method of dating
Indirect method of dating - use isotopes to date volcanic rock layers
Origins of new groups of organisms
Fossils show how new features arose and how long it took
Mammals gradually evolved from a group of tetrapods called synapsids
Over time mammals evolved a lower jaw consisting of one bone
Single hinge between upper and lower jaw
Differentiated teeth
Key events in earths history
3 major events:
- Origin of single - celled prokaryotes
- Development of multi-cellular organisms
- Origin of life on land
Prokaryotes
Stromatolites - certain prokaryotes link thin filaments of sediments together
3.5 billion years ago
Photosynthesis
Photosynthesis: aquatic bacteria - Cyanobacteria - 2.7 billion years ago
Oxygen dissolved in water produces iron oxides - increase
- gassed out into atmosphere- oxygen increased for 0.5 billion years
Rapid increase in oxygen in atmosphere due to evolution of eukaryotic cells that contain chloroplasts
Eukaryotes
Evidence supports serial endosymbiosis
Mitochondria and plastids (chloroplasts) were small prokaryotes that injured larger prokaryotes
Entered as:
1. Bits of in digested prey
2. Parasites
All eukaryotes contain mitochondria and only some contain chloroplasts
Mitochondria evolved before chloroplasts
The origin of multicellularity
Fossils and DNA sequencing
Common ancestor to multicellular eukaryotes lived 1.2m to 1.5 billion years ago
Larger more diverse eukaryotes do not appear until 565 million years ago
Geological evidence: series of ice ages - limited life
1. Deep sea vents & hot springs
2. Limited to open ocean water which was only found around equator.
30 million years
Cambrian explosion
Cambrian explosion
Origin of many phyla of current living animals
Prior to explosion:
1. Animals had soft bodies
2. Herbivores, filter feeders, scavengers
Cambrian explosion
1. Predators
2. Prey - defensive adaptations - sharp spikes & body armor