25. The history of life on earth Flashcards
Key concept: Conditions on early Earth made the origin of life possible
- The abiotic (nonliving) synthesis of small organic molecules, such as amino acids and nitrogenous bases
- The joining of these small molecules into macromolecules such as proteins and nucleic acids
- The packaging of these molecules into protocells, droplets with membranes that maintained internal chemistry different from that of their surroundings
- The origin of self- replicating molecules that eventually made inheritance possible
Key concept: The fossil record documents the history of life
Fossils as a form of scientific evidence
Key concept: Key events in life’s history include the origins of unicellular and multicellular organisms and the colonization of land
Phanerozoic eon: Paleozoic, Mesozoic and Cenozoic era
Key concept: The rise and fall of groups of organisms reflect differences in speciation and extinction rates
Key concept: Major changes in body form can result from changes in the sequences and regulation of developmental genes
Key concept: Evolution is not goal oriented
How has life on earth changed over time
Continental drift, mass extinction, adaptive radiation
macroevolution
- evolutionary change above the species level
-the origin of a new group of organisms through a series of speciation events and the impact of mass extinctions on the diversity of life and its subsequent recovery
hydrothermal vents
- the hypothesis that organic compounds were first produced in deep-sea hydrothermal vents
- area on the seafloor where heated water and minerals from Earth’s interior gush into the seawater, producing a dark hot, oxygen-deficient environment
- producers in a hydrothermal vent community are chemoautotrophic prokaryotes
alkaline vent
- deep-sea hydrothermal vent that releases water that is warm rather than hot and that has a high pH (is basic)
- these vents consist of tiny pores lined with iron and other catalytic minerals that some scientists hypothesize might have been the location of the earliest abiotic synthesis or organic compounds
ribozyme
- an RNA molecule that functions as an enzyme, such as an intron that catalyzes its own removal during RNA splicing
Sedimentary rock
- most fossils are found in sedimentary rock such as this plant fossil
radiometric dating
- a method for determining the absolute age of rocks and fossils based on the half-life of radioactive isotopes
half-life
- the amount of time it takes 50% of a sample of radioactive isotope to decay
stromatolites
- layered rock that results from activities of prokaryotes that bind thin films of sediment together
endosymbiosis
- a relationship between two species in which one organism lives inside the cell or cells of another organism
endosymbiont
-a cell that lives within another cell, called the host cell.
serial endosymbiosis
- a hypothesis for the origin of eukaryotes consisting of a sequence of endosymbiotic events in which mitochondria, chloroplasts and perhaps other cellular structures were derived from small prokaryotes that had been engulfed by larger cells
Cambrian explosion
- a relatively brief time in geologic history when many present-day phyla of animals first appeared in the fossil record. This burst of evolutionary change occurred 535-525 million years ago and saw the emergence of the first large, hard-boiled animals
plate tectonics
- the theory that the continents are part of great plates of Earth’s crust that float on the hot underlying portion of the mantle. Movements in the mantle cause the continents to move slowly over time
Pangea
- the supercontinent that formed near the end of the Paleozoic era, when plate movements brought all the landmasses of Earth together
mass extinction
the elimination of a large number of species throughout Earth, the result of global environmental changes
adaptive radiation
period of evolutionary change in which groups of organisms form many new species whose adaptations allow them to fill different ecological roles in their communities
heterochrony
- evolutionary change in the timing or rate of an organisms development