FossilRecords provide an actual record of Earth’s pastlifeforms.Change over time can be seen in the fossil record.
Paleontologist- scientist who studied fossils.
Biogeography is Organisms from a prior geographic region that were closely related but different species travelled into surrounding habitats and evolved in these far apart geographic regions.
DNA/ Proteinsequences are All living things share the same genetic structure (DNA & RNA)
Homologous Structures Structures found in organisms that share a common ancestry but have
since evolved for different functions.
AnalogousStructure Refers to the parts of living organisms that have different structures
but similar functions.
ANALOGOUS ANIMALS: Bat,Bird,Butterfly and Shark(Fish), Penguin(Bird), Dolphin(Mammal)
Vestigial Structure Refers to the structures that are reduced in size and function.
Non-functioning parts of living organisms.
Embryology Early on in development vertebrate embryos are strikingly similar.
Each has a tail, Pharyngeal pouches, buds
WHAT IS FOSSILS?
Evidence of organisms that lived in
the past.
they can be actual remains like
bones, teeth, shells, leaves, seeds,
spores or traces of past activities
such as animal burrows, nests, and
dinosaur footprints or even the
ripples created on a prehistoric
shore.
Unaltered preservation- small organism or past trapped in amber, hardened plant sap is observed.
Per mineralization/ Petrification- the organic contents of bone and wood are replaced by silica, calcite, forming a rock-like fossils.
Replacement- hard parts are dissolved and replace by other minerals.
Carbonization/ coalification – the other elements are ionized and only the carbon remained.
Recrystallization- the hard parts are converted into more stable minerals or small crystals turned into larger crystals.
Authigenic preservation- molds and casts are formed after most of the
organisms have been destroyed or dissolved.
MOLDS
Description: impression made in a
substrate = negative image of an
organism.
A hollow area in sediments in the
shape of an organism.
Ex. Shells.
CASTS
Description: when a mold is filled in.
Solid copy of the shape of an
organisms.
Ex. Bones and teeth
PETRIFIED
Description: Organic material is
converted into stone.
Ex. Petrified trees; coal balls
(fossilized plants and their tissues,
in round ball shape).
ORIGINALREMAINS
Description: Preserved wholly (
frozen in ice, trapped in tar pits,
dried/ dissected inside caves/
fossilized resin.
Ex. Woolly mammoth
CARBONFILM
Description: Carbon impression in
sedimentary rocks.
Ex. Leaf impression on the rocks.
TRACE/ ICHNOFOSSILS
Description: Record the
movements and behaviors of the
organism.
Ex. Trackways, toothmarks,
gizzard rocks, corpolites.
RELATIVEDATING is Based upon the study of layers of rocks.
Does not tell the exact age: only compare fossils
as older or younger, depends on their position in
rock layers.
Fossils in the uppermost rock layer/ strata are
younger while those in the lowermost deposition
are oldest.
LAW OF SUPERPOSITION:
Sedimentary layers are deposited
in a specific time- youngest rocks
on top, oldest rocks at the bottom.
LAW OF ORIGINAL
HORIZONTALITY: Deposition of
rocks happen horizontally- tilting,
folding, or breaking happened
recently,
LAW OF CROSS-CUTTING RELATIONSHIPS: If an igneous
intrusion or a fault cuts through existing rocks, the intrusion/fault is
YOUNGER than the rock it cuts through.
ABSOLUTE DATING
Determines the actual age of the fossil
Through radiometric dating, using radioactive
isotopes carbon-14 and potassium-40
Considers the half-life or the time it takes for half
of the atoms of the radioactive element to decay
The decay products of radioactive isotopes is
stable atoms.
What is Evolution?
It deals with the starting point of life and process of alteration of
simple life forms to complex.
Some organisms may change or appear, and some are lost or become
extinct.
It refers to gradual change in species eventually resulting to genetic