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The Fossil RecordThe estimated age of the Earth is about 4.5 billion
years (that’s 31.5 billion in dog years).
About 1 billion years after that…some life stuff
started happening (prokaryotes…in case yer
interested).
So, for about 3-4 billion years, life has been
evolving.
3 BYA the party starts…Cyanobacteria (forms
stromatolite fossils…remember that for high school
bio)
2.7 BYA Eukaryotes show up…they bring snacks.Mr. Blacher's 7th Grade Biology
2.2 BYA we get some atmospheric O2.
This is the result of photosynthesis (from
the cyanobacteria…aka blue-green algae).
From about 2.5-1.2 BYA it’s pretty quiet.
About 1.2 BYA we get us some
metazoans…multicellular organisms.
The longest period of time in the geologic
time table is called the Precambrian Time
(technically it’s a supereon).
Ok…so how do we figure this all out?
Mr. Blacher's 7th Grade Biology
The Endosymbiont Theory
There’s a really cool theory which
postulates that mitochondria and
chloroplasts were organisms that were
food for other larger organisms.
Eventually these organisms became
interdependent and could not live without
each other…a symbiotic relationship.
Living inside the larger organisms, the
chloroplasts produced food and oxygen,
and the mitochondria used food and
oxygen to produce ATP. Mr. Blacher's 7th Grade Biology
One Way To Visualize This
Stuff
Mr. Blacher's 7th Grade Biology
Dating Fossils & Rocks
Fossils are the petrified remains of once-
living organisms. There are a few kinds:
Mineralization: the bone or tissue is
replaced by minerals (there are several
types).
Molds and Casts
Trace fossils: tracks and burrows.
Mr. Blacher's 7th Grade Biology
How Old?
There are two types of dating…relative and absolute.
Relative Dating: Sediment builds up over time…if the layers are undisturbed, the older stuff is on the bottom (this is called Superposition).
You can’t get an actual time in years this way, but you can say fossil A is older or younger than fossil B.
Mr. Blacher's 7th Grade Biology
Absolute Dating: Radioactive isotopes are used to figure out an actual age in years.
Isotopes are elements that are radioactive and unstable. They decay at a measurable rate. When this happens, they breakdown into another element.
By measuring the ratio of isotope to breakdown product, we calculate the age of the rock.
The time it takes for half of an isotope sample to break down is called…half-life.
Mr. Blacher's 7th Grade Biology
Some Isotopes Used for Absolute
Dating
Parent-------Daughter
Carbon-14>Nitrogen: half-life= 5,730 years
Potassium-40>Argon-40: HL= 1.3 bill. Yrs.
Uranium-235>Lead-207: HL= 700 mill. Yrs
That means for example that if you had 100 grams of U-235, after 700 million years had passed you’d have 50 grams left (along with 50 grams of Lead-207)
That also means…you can’t use C-14 to calculate the age of dinosaurs fossils. Why? Cuz…it breaks down too quickly! You can use other isotopes though
Mr. Blacher's 7th Grade Biology
As the amount of Parent
Decreases the amount of Daughter
Increases!
Mr. Blacher's 7th Grade Biology
Try This…
Carbon-14 has a half-life of 5,730 years.
1. If you had a 10 gram sample of C-14,
how many years would take for there to
be 2.5 grams left?
2. If you had a 20 gram sample of C-14,
how much would remain after 22,920
years?
Mr. Blacher's 7th Grade Biology