Quiz #2 Flashcards
The transformation of a single species over time
Anagenesis
Species identified from the fossil record based on PHYSICAL SIMILARITIES AND DIFFERENCES with other species along an evolutionary line (lineage)
Paleospecies
The formation of one or more species from another time
Ex: humans, chimpanzees, and gorillas
Cladogenesis
Originally proposed by Niles Eldredge and Stephen Jay Gould (1972), it proposes that most species will exhibit little net evolutionary change for most of their geological history, remaining an extended state called STASIS. When significant evolutionary change occurs it is generally restricted to rare and rapid (on a geologic time scale) events of branching speciation called cladogenesis.
Punctuated Equilibrium
Two different methods to study fossil record
Relative Dating & Chronometric Dating
- Determines which fossils are older (relative to each other)
- Does not determine exact date
Relative Dating
- Layers of earth
- Utilizes the geological process of superposition (the accumulation over time of the earth’s surface)
Stratigraphy/Strata
The older the strata (layers, singular=stratum) are on the bottom, and the younger strata are on the top
Principle of Superposition
The study of the temporal and spatial distribution of fossil organisms
Biostratigraphy
Provides an ‘exact’ date (plus or minus statistical variation)
Chronometric Dating
-Divided into two eons
Geologic Time
(4.6 billion years ago to 545 million years ago)
Precambrian Eon
-545 million years ago to present Broken into 3 geological eras: -Paleozic (545-245 mya) -Mezozoic (245-65 mya) -Cenozoic (65 mya-present)
Phanerozic Eon
- ‘Age of mammals’
- Mammals radiate to fill vacant environmental niches left by the extinction of the dinosaurs
Cenozoic
- 225 mya (plate tectonics)
- last time land was above sea level
Pangea
- Paleocene epoch
- Eocene epoch
- Oligocene epoch
Epochs