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Lecture

BIO205H5 Lecture Notes - Cambrian Explosion, Atmospheric Temperature, Radionuclide


Department
Biology
Course Code
BIO205H5
Professor
A

Page:
of 7
Chapter 21: The History of Life on Earth
21.1 How Do Scientists Date Ancient Events?
Fossils can tell us a great deal about the body form, or morphology, of
organisms that lived there long ago, as well as how and where they lived.
Earth’s history is largely recorded in its rocks. The oldest layers, or strata, lie
at the bottom, and successively higher strata are progressively younger.
Observations of fossils contained within sedimentary rocks:
oFossils of similar organisms were found in widely separated places on
Earth.
oCertain organisms were always found in younger rocks than certain
other organisms.
oOrganisms found in higher, more recent strata were more similar to
modern organisms than were those found in lower, more ancient strata.
Radioisotopes provide a way to date rocks
Half of the remaining radioactive material of the radioisotope decays
Radioisotope dating have been expanded and refined
The decay of potassium-40 to argon-40 has been used to date most of the
ancient events in the evolution of life.
Fossils in the adjacent sedimentary rock that are similar to those in other rocks
of known ages provide additional clues.
Radioisotopes dating of rocks, combined with fossil analysis, are the most
powerful method of determining geological age.
21.2 How Have Earth’s Continents and Climates Changed over Time?
Earth’s crust consists of a number of solid plates approximately 40km thick,
collectively make up the lithosphere. It floats on a fluid layer of molten rock
(magma)
Magma circulates b/c heat produced by radioactive decay deep in Earth’s core
sets up convection currents in the fluid.
The plates move b/c 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 (underwater known as trenches).
Where plates are pushed apart, ocean basins may form between them.
The movement of the lithospheric plates and the continents they contain is
known as continental drift.
Oxygen has steadily increased in Earth’s atmosphere
Increase in atmospheric oxygen has been largely unidirectional.
The atmosphere of early Earth probably contained little or no free oxygen gas.
The increase in atmospheric oxygen came in two big steps; the first step
occurred 2.4 billion years ago, when certain bacteria evolved the ability to use
water as the source of hydrogen ions for photosynthesis.
One group of oxygen-generating bacteria, cyanobacteria, formed rocklike
structures called stromatolites.
Cyanobacteria liberated enough O2 to open the way for the evolution of
oxidation reactions as the energy source for the synthesis of ATP.
When it first appeared, oxygen was poisonous to anaerobic prokaryotes that
inhabited Earth.
Those prokaryotes evolved the ability to metabolize O2 survived and gained
numerous advantages: aerobic respiration proceeds at more rapid rates and
harvests energy more efficiently.
An atmosphere rich in O2 also made possible larger cells and more complex
organisms.
In contrast to this largely unidirectional change in atmospheric O2
concentration, most physical conditions on Earth have oscillated in response to
the planet’s internal processes.
Earth’s climate has shifted between hot/humid and cold/dry conditions
Earth’s climate was considerably warmer than it is today, and temperatures
decreased more gradually towards the poles.
At other times, Earth was colder than it is today; large areas were covered with
glaciers during the end of the Precambrian and during parts of the
Carboniferous and Permian periods.
For Earth to be in a cold, dry state, atmospheric CO2 levels had to have been
unusually low.
Volcanoes have occasionally changed the history of life
A few very large volcanic eruptions have had major consequences for life.
The collision of continents during the Permian period (275 mya) to form a
single, gigantic land mass, Pangaea, caused massive volcanic eruptions.
The ash ejected by volcanoes into the atmosphere reduced the penetration of
sunlight to Earth’s surface, lowering temperatures, reducing photosynthesis,
and triggering massive glaciations.
Extraterrestrial events have triggered changes on Earth
A meteorite caused or contributed to a mass extinction at the end of the
Cretaceous period (65 mya).
oThe first clue came from abnormally high concentrations of the element
iridium in a thin layer separating rocks deposited during the Cretaceous
from those deposited during the Tertiary.
oIridium is abundant in some meteorites; rare on Earth’s surfaces.
21.3 What Are the Major Events in Life’s History?
Life first evolved on Earth about 3.8 billion years ago.
By about 1.5 billion years ago, eukaryotic organisms had evolved.
The fossil record of organisms that lived prior to 550 million year ago is
fragmentary; good enough to show that the total number of species and
individuals increased dramatically in late Precambrian times.
Several processes contribute to the paucity of fossils
Only a tiny fraction of organisms ever become fossils.
Most organisms live and die in oxygen-rich environments in which they quickly
decompose
They are not likely to become fossils unless moved to an unoxygenated region;
most fossils are destroyed by geological process that transforms rocks.
Many fossil-bearing rocks are deeply buried and inaccessible.
Number of known fossils is especially large for marine animals that had hard
skeletons.
Insects and spiders are also relatively well represented in the fossil record.
The fossil record (incomplete) is good enough to demonstrate clearly that
organisms of particular types are found in rocks of specific ages and that new
organisms appear sequentially in younger rocks.
Precambrian life was small and aquatic
Life was confined to oceans and all organisms were small.
Over the Precambrian the shallow seas slowly began to teem with life.
For most of the Precambrian, life consisted of microscopic prokaryotes
(eukaryotes evolved 2/3 of the way through the era).
Unicellular eukaryotes and small multicellular animals fed on floating
photosynthetic microorganisms.
Small floating organisms, plankton, were eaten by slightly large animals.
Other animals ingested sediments on the seafloor and digested the remains of
organisms within them.
By late Precambrian, many kinds of multicellular soft-bodied animals had
evolved.
Life expanded rapidly during the Cambrian period
Cambrian period (452-488 mya) marks the beginning of the Palaeozoic era.
The O2 concentration was approaching its current level; the continents had
come together to form several large land masses.
The largest, Gondwana.
A rapid diversification of life took place Cambrian explosion.
Most of the major groups of animals that have species living today appeared
during this period.
THE ORDOVICIAN (488-444 MYA)
oThe continents, located primarily in the S. Hemisphere, still lacked
multicellular plants.
oEvolutionary radiation of marine organisms during early stages.
oAt the end, massive glaciers formed over Gondawa, sea levels were
lowered about 50 meters, and ocean temperatures dropped.
oAbout 75% percent of the animal species became extinct, probably
because of these major environmental changes.
SILURIAN (444-416 MYA)
oNorthernmost continents coalesced, but the general positions did not
change much.
oMarine life rebounded
oAnimals able to swim and feed above the ocean bottom appeared for
the first time.
oNo new major groups of marine life evolved.
oThe tropical sea was uninterrupted by land barriers
oMost marine organisms were widely distributed.
oFirst vascular plants appeared late in Silurian period; less than 50cm tall
and lacked roots and leaves.
oFirst terrestrial arthropods appeared at about the same time.
DEVONIAN (416-359 MYA)
oRates of evolutionary change accelerated.
oThe northern land mass (Laurasia) and the southern land mass
(Gondwana) moved slowly toward each other.