BIOL100 Lecture Notes - Devonian, Cambrian Explosion, Sirius Passet
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•Radioactivity- a method of dating rocks; discovered at the beginning of the twentieth century
•Half-Life- a successive time interval in which half of the remaining radioactive material of the
radioisotope decays, either changing into another element or becoming the stable isotope of the
•For 14C, production in the upper atmosphere is about equal to its natural decay.
•In an organism, the ratio of 14C to 12C stays constant during its lifetime.
•When an organism dies, it is no longer incorporating 14C from the environment.
•The 14C that was present in the body decays with no replacement and the ratio of 14C to 12C
•As soon as an organism dies, it ceases to exchange carbon compounds with its environment
•Isotopes in a sedimentary rock do not contain reliable information about the date of its formation
oSince they are transported over long distances and are deposed in another location
•But igneous rocks (e.g., lava or volcanic ash), that have intruded into layers of sedimentary rock
can be dated.
•Other radioisotopes are used to date older rocks.
•Decay of potassium-40 to argon-40 is used for the most ancient rocks.
•Radioisotope dating is combined with fossil analysis.
How have Earth’s Continents and Climates Changed over Time?
•Lithosphere- is Earth’s crust which consists of a number of solid plates each about 40 kilometers
oFloats on a fluid layer of molten rock or magma; the magma circulates because heat
produced by radioactive decay deep in Earth’s core sets up convection currents in the fluid
•The plates move because magma rises and exerts tremendous pressure
•Where plates are pushed together, either they move sideways past each other, or one plate slides
under the other, pushing up mountain ranges and carving deep rift valleys (when they occur under
water, such valleys are known as trenches)
•Where plates are pushed apart, ocean basins may form between them
•Continental Drift- movement of the lithospheric plates and the continents they contain
•Throughout Earth’s history, the plates that carry the continents have drifted apart and moved back
together numerous times.
•Plate movement has affected climate, sea level, and the distribution of organisms.
Increase of Oxygen in Atmosphere
•Increase in atmospheric oxygen have been largely unidirectional
•Oxygen first in atmosphere 3.8 bya (billion years ago)
•Oxygen concentrations began to increase significantly about 2.4 billion years ago when some
prokaryotes evolved the ability to split water as a source of hydrogen ions for photosynthesis. The
waste product is O2.
•One lineage of these oxygen-generating bacteria evolved into the cyanobacteria. These organisms
formed rocklike structures called stromatolites.
•The cyanobacteria liberated enough O2 to allow the evolution of oxidation reactions as the energy
source for the synthesis of ATP
•When oxygen first appeared in the atmosphere, it was poisonous to the anaerobic prokaryotes that
inhabited Earth at the time
•Organisms with aerobic metabolism replaced anaerobes in most of Earth’s environments
•As life continued to evolve, the physical nature of the planet was irrevocably changed.
•Living organisms added O2 to the atmosphere & removed CO2 from it.
•An atmosphere rich in O2 made possible the evolution of larger cells and more complex organisms.
•About 1,500 mya (million years ago), O2 concentrations became high enough for large eukaryotic
cells to flourish and diversify.
•By 750–700 mya, O2 had increased to levels that could support multicellular organisms.
•To the largely unidirectional change in atmospheric oxygen concentration, most physical conditions
on Earth have oscillated in response to the planet’s internal processes, such as volcanic activity,
continental drift and meteorite impacts
•Extraterrestrial events such as collisions with meteorites, have also left their mark causing mass
•Mass Extinctions- during which a large proportion of the species living at the time disappeared
Earth’s Climate Change
•For Earth to be in a cold, dry state, atmospheric CO2 levels had to have been usually low
•Weather changes rapidly; climates usually change slowly
•Most volcanic eruptions produce only local or short-lived effects, but a few very large volcanic
eruptions have had major consequences for life
•The collision of continents during the late Permian (about 275 mya) created a single, giant land mass
called Pangaea and caused massive volcanic eruptions.
•Ash from the eruptions reduced the penetration of sunlight to Earth’s surface, lowering temperatures,
reducing photosynthesis, and triggering massive glaciations
•Massive volcanic eruptions also occurred as the continents drifted apart during the late Triassic period
and at the end of the Cretaceous
•The first impact to be documented: meteorite 10 km in diameter that caused a mass extinction at the
end of the Cretaceous.
•Abnormally high concentrations of iridium in a thin layer separating the Cretaceous and Tertiary rocks