exam 1 Flashcards
natural selection
Evolution that selects for differential survival and reproduction of different phenotypes in a population.
Macroevolution
generally concerned with large patterns over evolutionary time. and the large-scale deployment of species over space and time.
igneous rocks
Igneous rock, or magmatic rock, is one of the three main rock types, the others being sedimentary and metamorphic. Igneous rocks are formed through the cooling and solidification of magma or lava. The magma can be derived from partial melts of existing rocks in either a planet’s mantle or crust.
metamorphic rock
Metamorphic rocks started out as some other type of rock, but have been substantially changed from their original igneous, sedimentary, or earlier metamorphic form. Metamorphic rocks form when rocks are subjected to high heat, high pressure, hot mineral-rich fluids, or, more commonly, some combination of these factors.
sedimentary rock
Common sedimentary rocks include sandstone, limestone, and shale. These rocks often start as sediments carried in rivers and deposited in lakes and oceans. When buried, the sediments lose water and become cemented to form rock. Tuffaceous sandstones contain volcanic ash.
universe age
13.6 billion years old.
number of galaxies
2 trillion observed galaxies.
supernova
the explosive death of a star that results in all the elements of the period table.
Hadean eon
The Hadean is a geologic eon of Earth history preceding the Archean. On Earth, the Hadean began with the planet’s formation about 4.54 billion years ago. The Hadean ended, as defined by the International Commission on Stratigraphy, 4 billion years ago.
archean
The Archean Eon is the second of four geologic eons of Earth’s history and by definition representing the time from 4 to 2.5 billion years ago. The Archean was preceded by the Hadean Eon and followed by the Proterozoic.
habitability zone hypothesis
the criteria that a planet must meet in order to be habitable for life like proximity to a star, necessary materials, etc.
early tangible evidence for life on Earth
- 4.1-3.8 billion chemical clues towards the existence of life
- 3.8 billion years old microfossils in Nuvvuagittug
- 3.7 billion direct fossil evidence of life
- 3.5 billion ancient stromatolites
- 2.7-1.8 billion BIFs show evidence of 02
- 2.4-2.2 billion increased O2 concentration
- 2-2.7 billion eukaryotes evolve
Alexander Oparin
Alexander Ivanovich Oparin was a Soviet biochemist notable for his theories about the origin of life, and for his book The Origin of Life. He also studied the biochemistry of material processing by plants and enzyme reactions in plant cells.
systematics
phylogenies + taxonomy
phylogeny
the genetic history of life