Universal Beginnings
I. Definitions
The Universe consists of all objects and phenomenon observed or
postulated. [Encyclopedia Britannica]
Scale Of the Universe
Distance from sun to earth = 500 Light Seconds (93 Million
Miles)
Distance to nearest star (Proxima Centauri) = 4.3 Light Years
Diameter of Local Galaxy = 100,000 Light Years
Nearest Large Galaxy (Andromeda) = 2 Million Light Years
Distance to Quasi Stellar Objects =
Mythology for our purpose is a peoples attempt to explain
observed or postulated phenomenon by the best means they have
available to them
II. Ancient Mythology
To explain the origins of the world as they knew it, the ancient
people postulated creation by beings or powers greater than themselves
Types of Ancient Creation Myth
Creation by a supreme being often a sky god
All Powerful, Pre-existent
Primoral matter in chaotic state
Creation a conscious act
Judeo-Christian creation stories in Genesis
Creation through emergence
Gradual creation from chaotic situation under the
earth
Navaho Emergence Myth
Movement from lower to higher levels
Creation by world Parents
Primordial mother and father
Chaos before coming of world parents
World Parents bear lesser gods who sometimes rebel and
take over
Babylonian Myth - Enuma elish
Creation from the cosmic egg
Primoral chaos compared to an egg with the germs of
creation
Japanese and Chinese creation stories
Creation by earth divers
Cosmic waters present before creation
Animal dives into water to secure a portion of the
earth
Common Threads
Primoral matter in form of chaos
Some agent separates the chaotic matter and creates the earth
and all on it
Men and Women highest order of creation
Creation of the Earth, Sun, and Moon were the main act of
creation
Everything else was secondary
III. Modern Mythology
Steady State Universe postulated by British school in 1948
Based on astronomical knowledge of the time??
Universe has always existed as it is and will continue that
way
Observation has since indicated this may be wrong
Beginning and End of the Universe Possible Conclusion
Hubbell's Law
Postulated by Edwin Hubble
On a large scale, Galaxies appear to be moving away from one
another at a rate proportional to their distance from us
Red shift phenomenon
Tracing location of galaxies back in time Hubble concluded
that 10 to 15 Billion years ago, all matter was in the same
place packed in an incredibly dense state
Big Bang Creation
At that time everything exploded in a Big Bang which began
the expansion seen today
Evidence supported by steady, uniform microwave background
radiation detected by radio telescopes
Believed to be remains of light of primeval fireball
Measurement problem
Since objects at the extremes of the universe are so far away,
we are seeing them as they were up to billions of years ago
Requires very careful evaluation to understand state of the
universe
Future of the Universe Presently Not Known
Will expansion continue, achieve a steady expansion velocity,
or contract again??
Need to know mass of universe to answer
At present time, the total mass of the universe is not known
With what we know today, the universe will continue to expand,
but theoretical physicists are learning more all the time
Latest work I have seen indicates Neutrinos may have
mass which will significantly change estimates
Questions and doubts
Religious Objections
Present state of knowledge
mass calculations very tentative and being revised on
a regular basis
The Formation of the Stars
I First Generation Stars
Temperature of universe about a few thousand degrees C around 300,000
years after the big bang
At that point, hydrogen and helium atoms form by capture of
electrons by protons
Cosmic background radiation emitted and universe became
electrically neutral
First Stars began to form about 12 billion years ago and hydrogen
atoms fuse into helium
Elements up to iron form in the interior of stars
Elements up to uranium form in supernova explosions
The forming and explosion of this first generation of stars created
the materials from which later stars including our sun were formed
The Sun and The Solar System
I. Definition
The Solar System consists of the sun, nine known planets and their
satellites, countless asteroids and comets and the interplanetary
medium.
II Origins Of the Solar System
Observed Process
Solar system began with the gravitational collapse of an
interstellar cloud of gas and dust possibly started by density
fluctuations within the cloud
Initial shape roughly spherical
Outer edge moves slower than inner, thus as it collapses, it
begins to rotate
As cloud contracts, it flattens - more away from the center
than close to it [called solar nebula]
As the cloud condenses, it heats up as its potential energy is
eventually converted to heat
As temperatures become high enough at the center, nuclear
reactions start and a star is born
This process takes about 10 million years
In the case of our sun, this happened about 4.6 Billion Years
Ago based on lead isotope decay measurements
The Formation of Planets
Attraction and Collision in the disk forms larger objects
Collisions relatively low velocity due to rotation so gravity
often holds the colliding objects together
Dichotomy in planet growth
The Inner Planets
Planets close to the sun formed where temperatures
were above the freezing point of water and became
small rocky bodies with a density of about 3 gm/cc
Hydrogen, Helium, and some of the Water Vapor escape
back into space
Inner Planets formed in about 100 Million Years
Continued collision with large bodies caused
significant effects
retrograde rotation of Venus
loss of atmosphere on Mars
Heavy bombardment continued for about 600 Million
Years further changing planetary features
The Outer Planets
Planets forming outside the freezing point become very
large, low density objects large enough to retain
Hydrogen and Helium
Availability of Ice resulted in very large planets
At about 10 time mass of earth, they can retain
Hydrogen and Helium
Since Hydrogen and Helium are most common elements in
the universe, the outer planets can become very large
but with densities of about 1.2 gm/cc
Large planetary systems formed as minor solar systems
Some moons added by capture
Strong solar wind later cleared much of the remaining dust
out of the system
Rocky asteroids formed in gap between Mars and Jupiter
source of meteorites
Icy bodies formed outside orbit of Neptune and Pluto
(Oort Cloud)
source of comets
The Formation of the Earth
I. Age
The Earth, like the Solar System formed about 4.6 Billion Years Ago
Based on Lead Isotope measurements
II. Differentiation and Crust Formation
Energy of formation and collisions resulted in mostly molten early
earth
Heavy elements like iron and nickel sank to the center and remained
molten
Lighter elements rose toward the top and formed an early crust over
the molten interior
The lightest ones that probably formed the first atmosphere escaped
into space
A secondary atmosphere then formed by outgassing associated with
surface volcanic activity
Continued bombardment of bodies from space added more energy and
probably destroyed the earliest crust
Oldest rocks on earth date to about 3.9 Billion Years Ago
III. The Atmosphere
Assume gases emitted by early volcanoes same as today
No free oxygen in secondary atmosphere (anoxygenic)
Evolution of Free Oxygen
Ultraviolet radiation broke up water vapor
Hydrogen escaped, Oxygen stayed in atmosphere
mostly captured by iron and other elements
Once life appeared, photosynthesis became predominant
form of oxygen production
Blue-green algae known to exist about 3.5 Billion
Years ago
Early iron absorbed much of oxygen in forming ferric
iron ores
Excess iron in oceans probably cleared about 1.7 Billion
Years Ago
Oxygen levels at beginning of Precambrian period about 2.2
Billion years ago were about 1% of today's levels
Oxygen content of atmosphere at end of Precambrian period
650 Million Years ago were about 10% of today's levels
When first land plants appeared about 400 Million Years ago,
present levels had been reached and they have stayed there
IV. The Oceans
Volcanic output includes water vapor
Once the surface cooled to less than 100 degree C about 3.5 Billion
Years ago, the vapor began to condense
Oceans achieved modern chemical characteristics about 2 Billion Years
ago once deposition of iron slowed due to slowing of volcanic activity
Most of iron precipitated out about 1 Billion Years ago
During the last 570 Million years, the oceans have been essentially
steady state chemical systems
Plate Tectonics
I Theory
About 1908 a German, Alfred Wegener proposed a theory of continental
drift based on a match of the profiles of South America and Africa
Theory not generally accepted
Findings of seafloor studies after World War II
Mid Ocean Ridge
Oceanic trenches
Earthquake and Volcanism Zones identified at trenches
Seafloor spreading model
Developed about 1960 by Henry Hess
New crust formed at mid ocean ridges
Dealt only with ocean crust (basaltic)
Crust flows into the trenches where it melts and is recycled
This melt also indicated by zones of volcanoes
Total crust produced at the ridges is equal to that destroyed in
the trenches
Can show rate and direction of movement in Pacific Island Chains
Evidence to support theory in magnetic anomalies tied to earth
field polarity reversal
As crust cools, magnetic particle in it align with the earth
field
Result is stripes parallel to ridges
Produces about 140 million years of evidence in ocean crust
II. Continental Movement
Continental mass less than ocean crust, thus rides on top of it
Collision of continental masses produce mountain ranges
Effects seen today in Western Americas and North of India
Rate and direction can be inferred from locations of glacial deposits,
chalk beds, coal beds, Etc.
Projections to the past
Assumes that the plates do not deform
Present day movements and indicators show much of land
together 240 Million years ago in continent called Pangaea
Less certain projections also indicate an earlier giant
continent of Godwana about 390 million years ago
It is estimated that when the earth was hotter, there was
more movement as the ridges expanded at a higher rate
III. Effects of Plate Movement
Climactic effects due to changes in ocean currents
Less diversity of life when the continents were joined
Movement of diverse life forms when they join together
North and South America example
IV. Unanswered Question
What drives the movement?
The Beginnings of Life On Earth
I. Reducing atmosphere of early earth fostered formation of building blocks
of life
Allowed production of amino acids and other building blocks of life
Chemical process driven by ultraviolet light exposure and lightning
Over time more complex proteins developed from the early building
blocks
II. About .1 to 1.5 Billion Years ago self replicating, mutable systems
developed out of the primoral soup of the early ocean
Early life forms probably lived deep enough in the oceans to avoid
UV light
They along with other processes produced oxygen that gradually built
up in the atmosphere
As Oxygen and Ozone built up, UV exposure reduced and life forms
moved toward the surface
Vertebrate life forms appear in the fossil record beginning about 600
million years ago
Land life forms appear about 500 million years ago
They very quickly adapted and spread to all corners of the earth
Theory of Evolution
I. Definition
A theory that animals and plants have origins in earlier types and
mutate over long time spans
All plants and animals derive from bacteria-like microorganisms that
originated about 3 billion years ago
II. Darwin's Theory
"On the Origin of Species by Means of Natural Selection" Published
in 1859
Expanded to Humans in 1871
Natural selection the driving force of change as organisms move to
new environments or their environment changes
Offshoots of Darwin's theory regarding species
Herbert Spencer - survival of the fittest
rejected by Darwin
Social Darwinism of the late 19th and early 20th centuries
Marxist theories of economic/political evolution
III. Mendelian Genetics
Synthetic Theory of Evolution came from this development
Work on Peas published by Gregor Mendel in 1866
Developed principles of inheritance/heredity
Tied to Origin of Species by Theodosius Dobzhansky in 1937 publication
"Genetics and the Origin of Species"
Widely accepted by about 1950
IV. Evidence for Evolution
Comparative Studies of living organisms by Darwin and others
Fossil Remains of similar and extinct species
Shows succession of organisms through time
Bacteria - 3.5 Billion Years Ago
Soft body worms - 700 Million Years Ago
Vertebrates - 400 Million Years Ago
Mammals - 200 Million Years Ago
Hominoid Australopithecus - 3 to 4 Million Years Ago
Homo Habilis - 1.5 to 2 Million Years Ago
Homo sapiens sapiens - 100,000 Years Ago
Structural Similarities
Bone structure of vertebrates very similar
Inheritance from common ancestor makes sense
DNA Evidence
Structure DNA deduced in 1953 by James Watson and Francis Crick
Similarities in Genetic code in DNA indicate common origins
Example cytochrome c grouping of amino acids
humans and chimps have 104 amino acids in the same
order
rhesus monkeys have one different
Horses have 11 additional amino acids
Tuna fish have 21 added
Comparison shows recency of common ancestors
Hundreds of such groups have been tested with similar results
Theory resisted by fundamentalist religions as a denial of God
began very early after Darwin's publication
Liberal religious interpretation is that God acts through
natural causes
Conclusions
Beginning with the formation of the universe in the Big Bang about 13 Billion
Years ago, the universe has continued to expand.
About 4.6 Billion years ago the solar system and the earth were formed.
Life appeared on earth about 3 Billion years ago and all life on earth has
developed from those first life forms.
Hominoid life forms appeared about 4 million years ago and the Homo Sapien
sub-species about 50,000 years ago.
We will discuss the developments by homo sapiens in the period before
historical recording began in the next lesson.