BioG 1105-1106 at Cornell University
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Unit 8: Demos

Objective 1:

Absolute vs. relative dating (1c)

Objective 2:

Continental drift (2a)
Did cracking continent trigger a deep freeze?: The break-up of a supercontinent may have caused a 'Snowball Earth'. (optional)
Extinction of the North American large mammals: Who or what killed them off? (optional)

Objective 3:

Conditions necessary for species dispersal (3 a and b)

Objective 6:

Convergent evolution (6c)
Confused by evolutionary trees? Check out Understanding Evolution.

Objective 8:

"Evolution in the Everyday World" from Scientific American (optional; see Blackboard for link)

Objective 9:

Primates (9a)
Hominoid divergence (9d)
A recent split of humans and chimps? (optional)
Unique characteristics of primates (optional)
Earliest "human footprints" found (optional)

Objective 10:

Characteristics that differ between apes and humans (10b)
Peking man older than previously thought! (optional)
"The Human Pedigree" from Scientific American (optional; see Blackboard for link)

Objective 13:

Latitudinal trends in species diversity (13e)
Life is faster in the temperate zones (optional) (New!)

Objective 14:

Lake turnover (download a .pdf file)
More lake turnover
What is a mesotrophic lake? (14b)
Beebe Lake
Change of course for ocean circulation (optional)

Objective 15:

More on biomes
Biomes slideshow

Absolute and Relative Dating Methods

Absolute vs. Relative Dating

Absolute dating methods allow a researcher to determine the age of a sample in years whereas relative dating methods only allow scientists to determine that a given sample is older or younger than a reference sample. For example, using an absolute dating method, like radiometric dating described below, you could determine that a tooth from the La Brea Tar Pits is 11,050 years old. A relative dating method, like comparing fossil sequences in sedimentary rocks from around the world, will only able to conclude that a sample is older than a particular layer of rock or another sample.

Radiometric Dating:

Naturally occurring isotopes such as radioactive carbon (14C) make possible the dating of many rocks and fossils. The ratio of the radioactive isotope 14C to the stable 12C, for instance, is relatively constant in the carbon dioxide of the atmosphere, but once a plant has captured a CO2 molecule and built it into a product like sucrose or cellulose, the decay of 14C atoms to 12C causes a ratio of 14C to 12C to decline steadily with time. The older the sample, the lower the amount of 14C and the higher the amount of 12C. Hence, the 14C:12C ratio in a sample provides a moderately accurate measure of age.


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