G10 Evidence for Evolution Flashcards
The age of fossils can be determined through different methods, and the most commonly used ones are relative dating and absolute dating.
refers to the method of determining the age of a rock layer and the fossils within based on sequences of events
Relative dating
four major laws in the field of geochronology
law of original horizontality
law of lateral continuity
law of superposition
law of crosscutting
which merely states that depositions for the layers are usually in a horizontal manner
law of original horizontality
which states that layers spread out laterally until they thin at the edges of the area, or into a different rock layer segment
law of lateral continuity
which states that the oldest rock layers are usually found under newer rock layers
law of superposition
which states that rocks and other features are younger than the layers that they intrude into
law of crosscutting
It gives a numerical estimate of the age of the object being tested
This method relies on the decay of certain elements through their half-life
The half-life of an element is the time it takes for that element to be reduced to half of its original amount
absolute dating
Absolute dating will usually involve taking the estimated age of a rock layer, or sometimes, even the fossil itself.
The most commonly used elements for absolute dating are carbon-14 with a half-life of 5,730 years, and potassium-argon dating with a half life of 1.3 billion years
fossil classification
mold fossils
trace fossils
true form fossils
cast fossils
is formed when an impression of an organism is made over a substrate. Most of the time, this creates a concave image (or a “negative”) of the organism in the substrate
mold fossil
is the fossilized remains of the traces of an organism
examples of fossils include remains of footprints, nests, and the like
trace fossil
is the fossilized remains of a part or the entire organism. Examples include dinosaur bones and insects trapped in amber
true form fossil
can be formed alongside a mold fossil
occur when a substance fills in the mold fossil, which forms a replica of the organism from the cast
cast fossil
A fossil record is derived from the discovered fossils all over the world. It shows the history of life as documented by fossils.
are fossils of organisms that are used for determining the age of surrounding rocks, and consequently, the age of the fossils within these rocks
index fossils/guide fossils
four criteria for classifying a fossil as an index fossil
abundance of the fossil
ease of identification
geographic range
temporal range of the fossil
From fossils, scientists were able to construct an evolutionary tree based on the similarities between specific structures of organisms.
Amphibians are known to have descended from fish, and the fossils of these fish have been found. Scientists based the evolutionary tree they created on the development of the different structures found, as well as the change from fins to legs.
Another example is the Pakicetus which is considered to be one of the ancestors of modern whales. They are land animals with long skulls and large carnivorous teeth, and their skulls strongly resemble those of the living whales.
are body parts of different organisms with similar forms but the functions are not necessarily the same
This implies that these structures may come from the same sources but have possibly evolved as a result of different pressures.
Homologous structures
refer to the repeating structures found within one organism
serial homology/homotopy