25 The History of Life on Earth Flashcards
What is macroevolution?
The broad pattern of evolution above the species level.
Therefore it deals more with questions such as how did life move from the water to land.
What is the general consensus on how life emerged from abiotic components?
It is believed to have happened in 4 stages:
- The abiotic (nonliving) synthesis of small organic mol- ecules, such as amino acids and nitrogenous bases
- The joining of these small molecules into macromolecules, such as proteins and nucleic acids
- The packaging of these molecules into protocells, droplets with membranes that maintained an internal chemistry different from that of their surroundings.
- The origin of self-replicating molecules that eventually made inheritance possible
What is an example of a set of conditions where the synthesis of amino acids could occur?
Many were found during a stimulated volcanic eruption
What are the basic forms of amino acids and how do they differ? (not acidic, basic etc.)
L Isomer and D isomer forms
Life on earth uses on the L form
What does ‘L isomer’ refer to in terms of amino acids?
One of two forms (L isomer and D isomer) of amino acids
Life on earth uses only L isomer
Thus the presence of the D isomer form in meteorites shows that amino acids can be synthesised abiotically.
What were primitive cells called?
Protocells
What are protocells?
The first primitive cells.
They existed as vesicles that spontaneously formed from hydrophobic substances to form a basic lipid bilayer.
They had clumps of clay called ‘montmorillonite’ around which chemicals concentrated and thus the rate of reaction increased.
What came first: RNA or DNA?
Probably RNA
What is ‘montmorillonite’?
A soft mineral clay that was abundant when life on earn began so was likely part of the first ‘protocol.’
What are the key sources of information about the history of life on earth?
- The fossil record
- Genetic analysis
When did the first unicellular eukaryote paper?
1,500 mya
What does ‘MYA’ refer to in the context of history?
Million years ago - therefore 1000 mya is a billion years ago
When where plesiosaurs around n earth?
200 to 65.5 mya
What is a common methods to determine the age of rocks and organic samples?
Radiometric dating
What is radiometric dating?
A method of determining the age of something based on its concentration of isotopes.
It works on the assumption that when an organism dies it will take in no new carbon. Any radioactive carbon that remains inside will slowly decay into stable carbon.
What it called when the age of something is determined by looking at isotopes?
Radiometric dating
What is a common isotope looked at when performing radiometric dating?
Carbon-14 which eventually becomes carbon-12
Some specimens are so old that they have minute amounts of carbon-12 present. How are they dated?
Organisms do not accumulate the radioactive uranium-238 However the rocks around them do.
Therefore by measuring the ratio of uranium-238 to U-235 in the surrounding rocks the age of the sample can be deduced.
What is the sequence in the evolution of mammals?
Synapsid → Therapsid → Early cynodont → Later cynodont → Very late cynodont → Modern Mammals
In the evolution of mammals, when did Snapsids first appear?
300 mya
In the evolution of mammals, when did Therapsid first appear?
280 mya
In the evolution of mammals, when did Early cynodont first appear?
260 mya
In the evolution of mammals, when did Later cynodont first appear?
220 mya
In the evolution of mammals, when did Very late cynodont first appear?
195 mya
In the evolution of mammals, what are synapsids?
They have multiple bones in the lower jaw and single-pointed teeth.
The jaw hinge was formed by the articular and quadrate bones. Synapsids also had an opening called the temporal fenestra behind the eye socket. Powerful cheek muscles for closing the jaws probably passed through the temporal fenestra.
Over time, this opening enlarged and moved in front of the hinge between the lower and upper jaws, thereby increasing the power
In the evolution of mammals, therapsids?
Therapsids had large dentary bones, long faces, and the first examples of specialized teeth, large canines. These trends continued in a group of therapsids called cynodonts.
In the evolution of mammals, what are Early cynodonts?
In early cynodont therapsids, the dentary was the largest bone in the lower jaw, the temporal fenestra was large and positioned forward of the jaw hinge, and teeth with several cusps first appeared.
As in earlier synapsids, the jaw had an articular-quadrate hinge.
In the evolution of mammals, what are Later cynodonts?
Later cynodonts had teeth with complex cusp patterns and their lower and upper jaws hinged in two locations: They retained the original articular-quadrate hinge and formed a new, second hinge between the dentary and squamosal bones.
In the evolution of mammals, what are Very late cynodonts
In some very late (non-mammalian) cynodonts and early mammals, the original articular-quadrate hinge was lost, leaving the dentary-squamosal hinge as the only hinge between the lower and upper jaws, as in living mammals.
The articular and quadrate bones migrated into the ear region (not shown), where they functioned in transmitting sound. In the mammal lineage, these two bones later evolved into the familiar hammer (malleus) and anvil (incus)
What is the ’temporal fenestra’?
An opening in the skull behind the eye socket.
Powerful muscles to close the jaw pass through this “archway”
In the evolution of mammals, where did the hammer (malleus) and anvil (incus) originate?
They are derived from the ‘articular-quadrate hinge’
What is the ‘geologic record’?
The entirety of the layers of rocks on earth and thus the entirety of Earth’s history
What is the geologic record divided into?
Three eons:
These are in order from oldest to most recent: Archaean, Proterozoic and Phanerozoic.
How long did the Archaean eon last?
4 billion years
How long did the Proterozoic eon last?
4 billion years
How long did the Phanerozoic eon last?
Half a billion years
What is the ‘geologic record’?
The entirety of the layers of rocks on earth and thus the entirety of Earth’s history
What is the geologic record divided into?
Three eons:
These are in order: Archaean, Proterozoic and Phanerozoic.
How long did the Archaean eon last?
4 billion years
How long did the Proterozoic eon last?
4 billion years
How long did the Phanerozoic eon last?
Half a billion years
What is the ‘proterozoic’ eon divided into?
The ediacaran period
Other events happened within the proterozoic but outside the Ediacaran
How is the Geologic record divided?
It has 3 eons.
An eon is divided into ‘eras’ which are divided into ‘periods’ which are then divided into ‘epochs’
What happened in the Ediacaran period?
Diverse algae and soft-bodied invertebrate animals appear
When was the Ediacaran period?
542 to 635 mya
What happened in the Archaen eon?
In order form first to most recent:
- Origin of earth
- Oldest known rocks on earth’s surface
- Oldest fossils of cells appear
- Oxygen levels in the atmosphere increase
What is the Phanerozoic eon divided into?
The cenozoic, mesozoic and paleozoic eras. (in order from most recent to oldest)
What is the Paleozoic era divided into?
The permian, carboniferous, devonian, silurian, ordovician and cambrian periods. (in order from most recent to oldest)
When did the earth first originate?
4,600 mya