Topic 9 Flashcards
What does an entity need to be considered alive?
Organization, metabolism, response to stimuli, homeostasis, adaptation, and reproduction
Are viruses alive?
Viruses are infectious parasitic entities that span the boundary between living and non-living.
Viruses have nucleic acids that replicate, mutate, and respond to natural selection, but LACK metabolism, homeostasis, and cannot reproduce outside of the host cell
3 Eons of geologic Record
Archaean, Proterozoic, and Phanerozoic
Phanerozoic
The last half billion years encompassing multicellular eukaryotic life.
3 eras: plaeozoic, mesozoic, and cenozoic
Factors for an Organism to undergo Fossilization
Existed for a long time
Abundant and widespread
hard rather than sof-bodied
aquatic
inshore marine, not offshore
not a decomposing organism
Mold Fossils
Form when a hollow space (impression) remains after the organism decays or resolve. Ex: cast fossils creating a mold
Replacement/Petrified fossils
The original tissues of the organism are replaced by minerals, preserving the detailed structure of the organism
Trace Fossils
Provide evidence of organism’s behaviour, such as tracks, burrows, or feces
Preserved Fossils
retain much of the original organic material of the organisms, such as carbon films, amber, tar or peat, or being frozen
Sedimentary Strata
Layers (strata) revealing the relative ages of fossils but not the absolute ages.
Challenges to Relative Dating
Common to have gaps in sedimentary sequence
Sediments can be tipped or even inverted by makor land movements
Radiometric Dating
Absolute dating of fossils using radioactive decay of isotopes of various elements providing a means to an age
Plate Tectonics Theory
considers that the Earth’s crust is composed of large plates that have been slowly moving since about 3.4 billion years ago causing continental drift to impact Earth’s biodiversity and the distribution of fossils
Supercontinent name
Pangaea
250 million years ago
“Big Five” Phanerozoic mass extinctions and main 2 examples
mass extinctions where 50% of the Earth’s species became extinct.
1. Permian extinction
2. Cretaceous extinction
Permian mass exctinction
Defines the boundary between the Palaeozoic and Mesozoic eras 252 million years ago caused by volcanic activity and coincided with the formation of Pangaea
Cretaceous mass extinction
66 million years ago, separating the Mesozoic from the Cenozoic. About 20% of all families went extinct, many being terrestrial plants and animals. Lost non-avian dinos.
Coincides with worldwide geologic deposits from a meteorite impact at Chicxulub, Mexico
Holocene extinction
Probable human-caused mass extinction ongoing now as a result of human population growth and overconsumption of natural resources
Consequence of mass extinctions
Lost of biodiversity altering ecological communities and niches available for organisms. Entire lineages can be lost by mass extinctions
Adaptive radiation
The rapid evolution of diversely adapted species from an ancestral species occurring when a change in the environment makes new niches available.
Causes of Adaptive Radiation
Mass extinctions, evolution of novel characteristics, and colonization of new regions with little competition
When did the Earth form?
Approximately 4.6 billion years ago during the Hadean Eon
Early Earth Conditions (first billion years)
Unstable crust floated on molten magma as earth cooled
Early Earth Conditions (first billion years)
Unstable crust floated on molten magma as earth cooled, steaming gases formed an atmosphere without oxygen, and when temperature dropped, water vapour condensed into raid which collected in basins