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The Universe
All of matter and energy that exists in space and time
It is everything that has ever existed and everything that ever will exist
Stars
Giant spheres made of super heated gas
Produce energy through nuclear fusion
Planets
Spheres made of matter that orbit stars
Black holes
Massive stars that end their lives by collapsing in on themselves
So dense and have such a strong gravitational field that light can’t escape
Nebulas
Made of hydrogen gas and dust
Slowly collapse together under the force of gravity to create stars
Leftover gas and dust forms planets (a nursery)
Galaxies
Collection of stars, stellar remnants, gas, dust and dark matter
Held together by gravity
Astronomical unit & when to use
Average distance between Earth and the Sun
Measures distances in our Solar System
Light year & when to use
Distance light travels in a year
Measures dinstances to other stars in the Milky Way
Parsec & when to use
Measures distances to other galaxies
Wurdi Youang stone arrangment
Located in Ballarat, Vic
Over 11’000 years old - oldest known astronomical site
Maps different setting positions of the sun throughout the year
Shows different seasons & what food is available
Electromagnetic waves
Form of radiation
Travels through vaccum of space at the speed of light
7 types
Main sequence
First stage after creation
Composed of 98% hydrogen and helium
Lasts 90% of Star’s life
Supergiant
Produce heavier elements like Iron through fusion
Makes them lose mass
Supernova
Outer layers are of H and He are ejected
Happens within seconds
Neutron star
Core collapses into a dense mass of neutrons
Life cycle of high mass stars
Stellar nebula
Protostar
Main sequence
Supergiant
Supernova
Black hole or Neutron star
Red giant
Star extends the outer layers by using the H in the core
Grows more than 100x their main sequence size
Planetary nebula
Outer layers are ejected
Core contracts into a white dwarf
Takes tens of thousands of years
White dwarf
Composed of carbon and oxygen
Can also be neon, magnesium and helium
Black dwarf
Theoretical phase
Occurs when the Star has cooled so much it no longer emits light
Universe’s existense is too short to prove this
Life cycle of low mass stars
Stellar nebula
Protostar
Main sequence
Red giant
Planetary nebula
White dwarf
Black dwarf
Exoplanet
Planet that orbits a star outside our solar system
Criteria of a Planet
Be spherical
Orbit a star
Big enough that its gravity clears away things in its orbital path
Criteria for life to form
Liquid water must be able to form
Only occurs in “Goldilocks zone’s”
Elliptical galaxies
Spherical/egg shaped
Lack gas and dust
Therefore cannot form new stars
Do not rotate
Spiral galaxies
Have a buldge made of stars
Rotate and therefore have “arms”
Mix of young and old stars
Bars can form if stars orbit becomes unstable - stretches out and grows as they collect new stars
Irregular galaxies
No symmetry/organised structure
Mix of young and old stars
Have pockets of gas
Steady state theory
Suggests:
Density of the universe is infinite
Universe only expands as new matter is created
Constant creation of matter keeps the universe in a steady state
In theory, properties of the universe do not change; has no beginning or end of time
The Big Bang Theory
The universe was once in a condition where density is infinite
Was very hot & expanded rapidly creating the big bang
The rapid expansion cooled and the universe became what it is today
Homogenous and uniform in all directions of space, but not time
Cosmic background radiation
Uniformly fills the universe
Supports big bang theory; provides evidence of the universe’s early hot and dense state
Creation of the Universe
Big bang
Inflation
First protons and neutrons created
First Helium and Hydrogen atoms created
Light shines for the first time
Stars and galaxies form
The Solar System forms
Earth forms
Life starts to appear on Earth
Excited state
Occurs when an atom gains energy and jumps to a higher valence shell/energy level
Unstable state
Will eventually lose energy in the form of light and moves back down to its original shell
Group numbers
Number of electrons in the valence shell
Period numbers
Number of valence shells
Metals
Lustrous
Malleable
Ductile
Good conductors of heat and electricity
1-3 valence electrons
Non-metals
Non shiny or lustrous
Poor conductors of heat and electricity
4-7 valence electrons
Metalloids
Brittle
Somewhat shiny
Semiconductors
3-6 valence electrons
Cation
Positively charged atom
Anion
Negatively charged ion
Ionic bonding
Between a metal and a nonmetal
Atoms will gain or lose electron/s to become stable
Electrostatic attraction between the atoms ionically bonds the two together
Covalent bonding
Between nonmetals
Atoms share electrons to form an intramolecular bond
Metallic bonding
Between metals
Electrons are delocalised and free to move throughout the metal lattice; creates a “sea of electrons”
Holds metals togeter
Intramolecular bond
Bond within molecules
Strong
Intermolecular bond
Bond between molecules
Weak
Amino Acids
Human body uses 20
Joined together by a chemical reaction to form polymer
50 amino acids joined together forms a protein
Proteins
Transmit messages
Build structures
Perform chemical reactions
Support the immune system
Store vital chemicals for the body like amino acids
Proteins & amino acids; link to the big question
Murchison meteorite:
Fell in Victoria in 1969
Contained amino acids such as;
Glycine
Alanine
Glutamic acid
& unidentified acids
Asteroids:
Amino acids have been found on asteroids 200 million miles from Earth
Link to BQ:
Amino acids form proteins
Proteins are building blocks of cells which can form living substances
Also perform functions that maintain life
Biological evolution
Genetic change in a population
Inherited over several generations
LUCA
Last Universal Common Ancestor
Original form of life
Most likely a prokaryotic cell
Lived near iron rich, underwater hydrothermal vents
Around 3 billion years ago LUCA evolved to photosynthesise
After this, oxygen started to accumulate in the atmosphere
Brief timeline of the evolution of Homo sapies
3.7 billion years ago - single cellular organisms exist
800 million years ago - multicellular organisms exist
4 million years ago - first humans exist
70’000 years ago - Homo sapiens exist
Biodiversity
The variety of livings things and their interactions with their environment
Changes over time as a result of evolution
Levels of Biodiversity
Species: the number of species present in an ecosystem
Genetic: genetic variation within the species
Ecosystem: the variety of habitats, ecosystems and communities
Key observations of Darwin’s Theory of Evolution
Traits are inheritable
More offspring are produced than can survive
Offspring vary in their inherited traits
Natural selection
Natural mechanism of evolution
Organisms that are better adapted to the environment through inherited traits have a better chance at survival
Therefore, these traits are passed down to the next generation
Depends on the environment
Acts on existing variation in the animal - must be variation in the species to occur
Key points of evolution
Variation: must be genetic differences in the population
Birth rate: more offspring are produced than can survive
Inheritance: the trait must be coded into the DNA for the organism to receive it
Selection: some organisms’ traits are more favorable, meaning the organisms that have are more likely to survive and pass those traits to their offspring
Time: the frequency of traits will change over time
Artificial selection
Process of humans identifying desirable traits in animals and plants
Then bred together to create a new organism
Process of artificial selection
Observivng individuals in the population
Selecting the individuals with the desirable traits
Breeding the organisms together to create a new generation
Repeating the cycle until the desirable organism is created
Negative side effects of artificial selection
Defects and less genetic diversity
New diseases
No contronl over genetic mutations
Species
A group of living organisms consisting of similar individuals that are capable of breeding
Speciation
Process of forming new and distinct species over evolutionary time
Occurs in 4 stages
Stages of speciation
Variation: must be genetic differences in the population
Isolation: an event occurs in which are part of the population is isolated
Selection: the usual process of natural selection occurs
Time: over thousands of years, the two populations have changes so much that they can no longer breed and are difference species
The fossil record
Shows history of life as documented by fossils
Incomplete due to the conditions required for fossils to form
Formation of fossils
Organism must be covered with sediment very close to time of death
The rocks the organism is covered with must be burried as well so the organism is preserved, but eroded enough so that the fossil can be found
Pertrification
Occurs through permineralisation
After the organism is burried in sediment, it may be exposed to mineral rich fluids that flow through the rocks
Rocks are filled with preserving minerals like calcium carbonate and silica
Minerals replace the organic materials and the remains are turned to stone
Compression
An imprint of the fossil is produced
Due to high pressures from the weight above
Moulds and casts
If the shell or bone dissolves, it can leave a space in the shape (mould)
Sediments fill the space to form a cast
Preserved remains
Organisms beome trapped in amber, preserving the organism
Comparative anatomy
Study of the similarities and differences in the structures of different species
Divergent evolution
Two or more species diverge from a common ancestor
Evolve seperately due to different selection pressures
Homologous structures
Similar structures in related organisms
Due to inheritance from common ancestors
Structures have differing functions
Convergent evolution
Two or more organisms evolve in similar environmet, and therefore have similar characteristics
Due to selection pressures
Analogous structures
Similar structures in unrelated organisms
Evolve to do the same job, not due to inheritance
Genome
All of an organisms DNA and the way it is stored and structured
Comparative genomics
Study of comparing genomes for similarities in the DNA sequence
The more similar, the more related
Evidence for LUCA
All living organisms have the same 4 bases in their genetic codes
Same mechanisms for turning DNA into proteins
Homologous gene
Genes that have a similar function
Passed down from a common ancestor
Ubiquitious proteins
Proteins that exist in many living things
Performs the same function in each
Number of Protons =
= atomic number
Number of electrons =
= number of protons (neutral atom)
Neutrons =
= mass number - protons
Mass number =
= protons + neutrons
Element+ =
= - electrons
Element- =
= + electrons
Neutral charge =
= same number of protons and electrons
Negative charge =
= more electrons than protons
Positive charge =
= more protons than electrons