Chapter 25 - History of Life on Earth Flashcards
Macroevolution -
the broad pattern of evolution above the species level
The four main stages that are hypothesized to have have produced simple cells:
- 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
Hypothesis’s by both A. I. Oparin and J. B. S. Haldane:
Earth’s early atmosphere was a reducing (electron-adding) environment, in which organic compounds could have formed from simpler molecules
Hydrothermal vents -
areas on the seafloor where heated water and minerals gush from Earth’s interior into the ocean
Black smokers -
a type of hydrothermal vent that release water so hot that organic compounds formed there may have been unstable
Alkaline vents -
a type of hydrothermal vent that release water that has a high pH (9–11) and is warm rather than hot, an environment that may have been more suitable for the origin of life
The first genetic material was most likely _____, not DNA
RNA: RNA molecules with certain nucleotide sequences may have shapes that enable them to replicate faster and with fewer errors than other sequences
the known fossil record is biased in favor of species that _______________________________________
existed for a long time, were abundant and widespread in certain kinds of environments, and had hard shells, skeletons, or other parts that facilitated their fossilization
Radiometric dating -
dating based on the decay of radioactive isotopes
Half-life -
the time required for 50% of the parent isotope to decay, which the rate of decay is expressed by
by measuring the ratio of _______ to _______ in a fossil, we can determine the fossil’s age
carbon-14; carbon-12
A geologic record -
a standard time scale that divides Earth’s history into four eons and further subdivisions
The Phanerozoic eon -
roughly the last half billion years, encompasses most of the time that animals have existed on Earth
Three era’s the Phanerozoic eon is subdivided into:
the Paleozoic, Mesozoic, and Cenozoic
Mesozoic era -
sometimes called the “age of reptiles” because of its abundance of reptilian fossils, including those of dinosaurs