Evolution – Lesson 1 – Beginning of Earth
Evolution according to Homer:
http://www.youtube.com/watch?v=faRlFsYmkeY&feature=player_detailpage
How did Life Begin?
In this study of evolution, we must first consider theories of the beginning of the Earth and all life on it.
1. Creationism
In this theory, the Earth and all living beings were created by one or more supernatural beings or gods.
An example of this is the belief found in the Book of Genesis of the Bible that God created all over 7
Days and that humans were formed in his image. Within this specific theory there are three other
theories including:
A. Young Earth Creationism – Earth about 10,000 years old
B. Omphalos Hypothesis – God created the Earth in its mature form
C. Old Earth Creationism – broken into three parts, gap, day age and progressive
creationism and accepts God as the physical creator of the universe and accepts
scientific dating.
Please remember that all of these theories come out of the one belief in the Bible. We could research
and learn so many more theories of Creationism, meaning that all was created by supernatural beings or
Gods. For instance, in Hinduism it is believed that humans are part of the natural cycle of creation and
destruction that began millions of years ago. It is also believed that humans have remained unchanged
during that time.
2. Intelligent Design
This is a relatively new theory that challenges Science to explain how all of this, the creation of the Earth
and its beings, the universe, could happen at random. It believes that all things were done for a reason
and that there is an intelligent explanation, reason, plan behind all that has happened and will continue
to happen. In many ways it is very similar to Creationism, but does not label a specific creator (like God)
within the theory.
3. Big Bang Theory
This theory states that our Universe began about 13.7 billion years ago as a very small, dense pocket of
gasses. As they met, they began a large reaction causing the small pocket to expand and become the
universe that we have today. During the expansion, other particles met and reacted causing things like
planets to form, atmospheres to develop and eventually life to form.
How are the theories different? What is the same?
How did life begin on Earth?
The following videos, each about 10 minutes long, give a quick history of the Earth and how life came to
be. Please watch the videos and create a quick time line based on the information in the videos for
yourself. We will take up the timelines in class to ensure we are all have the same basic information.
Please do not worry about the last minute of the The First Humans video, we will discuss this topic later
in much more detail.
YouTube Origin Evolution of Life
http://www.youtube.com/watch?v=8SgnnV8nV9g&feature=player_detailpage
The First Humans
http://www.youtube.com/watch?feature=player_detailpage&v=s-nLJI2BZIM
Chemical evolution is the increase in complexity of chemicals that led to the first cells.
1. Today, we say that "life only comes from life."
2. However, the first cells had to arise from an increased complexity of chemicals.
A. The Early Earth
1. The Earth came into being about 4.6 BYA (BYA).
- Early Earth's atmosphere differed from the current atmosphere, consisting of:
a. water vapor,
b. nitrogen,
c. carbon dioxide,
d. small amounts of hydrogen, methane, ammonia, hydrogen sulfide, and carbon monoxide.
2.. The early atmosphere contained little free oxygen (O2) and was probably a reducing atmosphere with
little free oxygen; a reducing atmosphere lacks free O2 and allows formation of complex organic
molecules.
3. The early Earth was so hot that H2O only existed as a vapor in dense, thick clouds.
4. As the Earth cooled, H2O vapor condensed to form liquid H2O, and rain collected in oceans.
B. Monomers Evolve
1.. Experiments performed by Miller and Urey (1953) showed experimentally that these gases (methane,
ammonia, hydrogen, water) reacted with one another to produce small organic molecules (amino acids,
organic acids).
C. Polymers Evolve
1. Newly formed organic molecules polymerized to produce larger molecules.
If a protocell was a heterotrophic fermenter living on the organic molecules in the organic soup that was
its environment, this would indicate heterotrophs preceded autotrophs.
a. A heterotroph is an organism that cannot synthesize organic compounds from inorganic substances
and therefore must take in preformed organic compounds.
b. An autotroph is an organism that makes organic molecules from inorganic nutrients.
Geologists have devised the geological timescale, which divides the history of Earth into eras, and then
periods and epochs.
Era
Period
Years Ago
4.5 billion
First living cells
Bacteria
Photosynthesis
Algae
First invertebrates
590 million
Algae
Marine Invertebrates
505 million
Arthropods
Mollusks
First fish
Fungi
Silurian
438 million
Many fish
Trilobites
Vascular Plants
Plants on Land
Arthropods on Land
Devonian
"Age of Fishes"
408 million
Lots o' fishes
First amphibians and insects
360 million
Mosses
Many amphibians
First reptiles
Permian
286 million
Mass marine extinction
Amphibian decline
Pangaea
Triassic
248 million
First mammals
Dinosaurs
Precambrian
Cambrian
Ordovician
Paleozoic
Carboniferous
Mesozoic
"Age of Reptiles"
Major Events
Pangaea begins to separate
Cenozoic
"Age of Mammals"
Jurassic
213 million
Dinosaurs dominate
First birds
Cretaceous
144 million
Flowering plants
Mass extinction
Tertiary
65 million
Birds,mammals, insects flourish
Continents in modern positions
2 million to
present
First hominids
Ice Ages
Extinction of giant mammals
(mammoth)
Quaternary
History of Life
A. Fossils Tell a Story
1. A fossil is the remains or traces of past life, usually preserved in sedimentary rock.
2. Most dead organisms are consumed by scavengers or decompose.
3. Paleontology is the study of fossils and the history of life, ancient climates, and environments.
4. Sedimentation has been going on since the Earth was formed; it is an accumulation of particles
forming a stratum, a recognizable layer in a stratigraphic sequence laid down on land or in water.
5. The sequence indicates the age of fossils; a stratum is older than the one above it and younger than
the one below it.
B. Relative Dating of Fossils
1. Strata of the same age in England and Russia may have different sediments.
2. However, geologists discovered that strata of the same age contain the same fossils, termed index
fossils.
3. Therefore, fossils can be used for the relative dating of strata.
4. A particular species of fossil ammonite is found over a wide range and for a limited time period;
therefore, all strata in the world that contain this ammonite are of the same age.
5. However, relative dating does not establish the absolute age of fossils in years.
C. Absolute Dating of Fossils
1. Absolute dating relies on radioactive dating to determine the actual age of fossils.
2. Radioactive isotopes have a half-life, the time it takes for half of a radioactive isotope to change into a
stable element.
3. Carbon 14 (14C) is a radioactive isotope contained within organic matter.
a. Half of the carbon 14 (14C) will change to nitrogen 14 (14N) every 5,730 years.
b. Comparing 14C radioactivity of a fossil to modern organic matter calculates the age of the fossil.
c. After 50,000 years, the 14C radioactivity is so low it cannot be used to measure age accurately.
4. It is possible to determine the ratio of potassium 40 (40K) and argon 40 to date rocks and infer the
age of a fossil.
What is Pangea? Continental Drift?
Plate tectonics is the study of the lithosphere, the outer portion of the earth
consisting of the crust and part of the upper mantle. The lithosphere is divided into about a dozen large plates
which move and interact with one another to create earthquakes, mountain ranges, volcanic activity, ocean
trenches and many other features. Continents and ocean basis are moved and changed in shape as a result of
these plate movements.
The sequence of maps show how
a large
supercontinent, known as Pangaea was fragmented into several pieces, each being part of a mobile
plate of the lithosphere. These pieces were to become Earth's current continents. The time sequence
show through the maps traces the paths of the continents to their current positions..
In the early 1900's Alfred Wegener proposed the idea of Continental Drift. His ideas centered around
continents moving across the face of the earth. The idea was not quite correct - compared to the plate
tectonics theory of today - but his thinking was on the proper track. In addition, a variant spelling of
Pangaea is "Pangea". It appears in some textbooks and glossaries, however, Pangaea is the current
preferred spelling.