Given its name by Richard Owen to classify unusual reptile fossils, a group of animals that share a unique common ancestor
Clade
Hypothesized similarities and traits among common ancestors were grouped under this name
Subclade
A sub category that grouped members more closely related to each other
Synapomorphy
This particular shared, derived trait supports how to define a group (key word: derived). As an example, the number of holes in a skull distinguishes different clades
Dimetrodon
Commonly misidentified as a dinosaur, obtained traits that differentiated it from dinosaurs
Cladogram
An evolutionary tree (phylogeny) made from cladistic analyses
Oviraptor
A small theropod (meat-eating dinosaur) best known for their behavior of stealing other eggs for consumption
Empirical
Things that can be recognized by the senses (sight, touch, etc.)
Law
A generalization about some aspect of the natural world that appears to be true in all cases
Hypothesis
A proposed explanation for a set of observations about the natural world, often thought of as an "educated guess"
Theory
An explanation about some aspect of the natural world that has been repeatedly tested and confirmed, the most reliable form of scientific knowledge
Falsifiable
The act that we can test ideas and discard incorrect ideas
Progressive
Changes over time, never stays the same. There are constantly new discoveries and explanations to already discovered ideas.
Normative
The culture dictates how observations are interpreted and what questions are worth asking; such as what data we collect, what counts as "scientifically significant" and the norms for scientific research
Scientific journal
A specialized publication for evaluating and sharing scientific research between scientists
Peer review
A process used in scientific journals where multiple scientists (usually anonymously) argue for the publication or rejection of an article
Corroboration
When multiple studies / techniques support the same hypothesis, a critical part of theory building
Fossil
The preserved remains of a prehistoric organism
Body fossil
Physical remains of an organism that are typically fragmented or damaged
Trace fossil
Remains of an organism but not the organism itself that provide evidence of prehistoric organism's behavior; ex: bite marks, fossil poop
Molecular fossil
Examples of these fossils include ancient DNA, proteins, and lipids (fats)
Biostratinomy
Everything that happens to an organism between death and burial, impacts what gets preserved
Hydroxyapatite
The main mineral in bones in vertebrates
Diagenesis
Everything that happens to an organism between burial and discovery, it typically involves the loss of any remaining organic matter. Also impacts what gets preserved
Lagerstätte
A fossil deposit with exceptional preservation
Bone bed
Exceptional deposits of hundreds/thousands of bones preserved in one site, sometime all members of the same species and sometimes a mixture
Erosion
The loss of sediment by the weathering of rock by wind or water. Helps reveal the order that rock layers were deposited
Sedimentation
The accumulation of sediment, most occurs along coastal regions. The laying down of dirt and mud, eventually turning into layers of rock
Paleontology
The branch of science that deals with the discovery, collection, and preservation of fossils
Stratigraphy
The science of mapping the order of rocks
Mesozoic
The middle of the stratigraphic column, dinosaurs are usually found here
Igneous rock
Formed through the cooling and solidification of magma and lava
Sedimentary rock
Formed by the accumulation and cementation of sediment at the Earth's surface
Metamorphic
Formed by the transformation of other rocks through extensive heat and pressure
Geologic map
Ranges where patterns of sedimentation and erosion rocks from different geologic ages are exposed in different parts of the world
Deinonychus
Before the discovery of this dinosaur, dinosaurs were seen as big reptiles and evolutionary losers
Lithostratigraphy
Dating rocks based on their order and mineral composition
Law of superposition
In undeformed stratigraphic sequences, the oldest strata lie at the bottom while the youngest strata are at the top; the deeper you go (towards the bottom) the farther you go back in time