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science vocab 4-2-08

Terms

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fossil
remains, imprints, or traces of prehistoric organisms that can tell when and where organisms once lived and how they lived
cyanobacteria
chlorophyl containing, photosynthetic bacteria thought to be one of the worlds earliest life forms
mesozoic era
middle era of earth's history, during which Pangaea broke apart, dinosaurs appeared, and reptiles and gymnosperms were the dominant land life forms
principle of superposition
states that older rocks are at the bottom and younger rocks are at the top
unconformity
gap in the rock layer that is due to erosion or periods without any depostion
epoch
the next smaller division of geologic time after the period; characterized by differences in life forms that might vary regionally
index fossil
remains of species that existed on earth for a reletively short period of time, they were abundant and widespread geographically, and can be used by geologists to assign the ages of rock layers
permineralized remains
fossils in which the spaces inside are filled with minerals from groundwater
cenozoic era
era of recent life that began about 65 million years ago and continues today; includes the first apperance of homo sapiens about 400 thousand years ago
precambrian time
longest pert in earth's history, lasting from 4 billion to about 544 million years ago
uniformitarianism
principle stating that earth processes occuring today are similar to those in the past
paleozoic era
era of ancient life, which began about 544 million years ago when organisms developed hard parts and ended with mass extinctions about 245 million years ago
organic evolution
change of organisms over geologic time
pangea
large, ancient landmass that was composed of all continents joined together
period
horizontal rows of elements in the periodic table whose properties change gradually and predictably
eon
longest subdevision in geologic timescale; based on the abundance of certain types of fossils and subdevided into eras, periods and epochs
trilobite
organism with a three lobed skeleton that was abundant in Paleozoic oceans and is considered to be an index fossil
species
group of organisms that reproduce only with other members of their own group
natural selection
process by which organisms that are suited to a particular environment are better to survive and reproduce than organisms that are not
half-life
the time it takes for half the atoms of radioactive isotope to decay
radioactive decay
process in which some isotopes break down into other istotopes, releasing energy and particles from the nucleus
carbon film
thin film of carbon residue produced as a fossil
radiometric dating
process used to calculate the absolute age of rock by measuring the ratio of parent isotope to daughter product in a mineral and knowing the half- life of the parent
absolute age
age of rock- determined by using properties of the atoms that make up materials
cast
a type of body fossil that forms when crystals fill a mold or sediments wash into a mold and harden into rock
geologic time scale
division of earth's history into time units based largely on the types of life forms that lived only during certain periods
mold
a type of body fossil that forms a rock when an organism with hard parts is buried, decays or dissolves, and leaves a cavity in the rock
relative age
the age of something compared with other things

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