domingo, 12 de junio de 2011

Vocabulary#2

analogous structure: Body parts that once differed in evolutionarily distant lineages but converged in structure and function as responses to similar environmental pressures.

as   asteroid: Rocky, metallic body, a few to 1,000 kilometers across, hurtling through space.
 
co  comparative morphology: Scientific study of comparable body parts of adults or embryonic stages of major lineages.
 
      derived trait: A novel feature that evolved but once and is shared only by the descendants of the ancestral species in which it evolved.
 
]--  fossil: Recognizable, physical evidence of an organism that lived in the distant past.
 
      fossilization: How fossils form. An organism or evidence of it gets buried in sediments or volcanic ash; water and dissolved inorganic compounds infiltrate it; then chemical changes and pressure from accumulating sediments above transform it to stony hardness.
 
<!   geologic time scale: Time scale for the Earth's history with major subdivisions corresponding to mass extinctions.
 
<!   Gondwana: Paleozoic supercontinent; with other land masses, it formed Pangea.
 
<]   half-life: The time it takes for half of a given quantity of any radioisotope to decay into a different, and less unstable, daughter isotope.
 
]      homologous structure: Of separate lineages, comparable body parts that show underlying similarity even when they may differ in size, shape, or function; outcome of morphological divergence from a shared ancestor.
 
       lineage: Line of descent.
 
]--   morphological convergence: Macroevolutionary pattern. In response to similar environmental pressures over time, evolutionarily distant lineages evolve in similar ways and end up being alike in appearance, functions, or both.
 
]-    morphological divergence: Macroevolutionary pattern; genetically diverging lineages undergo change from body form of a common ancestor.
 
<    Pangea: Paleozoic supercontinent upon which the first terrestrial plants and animals evolved.
 
<    plate tectonics theory: Theory that great slabs (plates) of the Earth's outer layer float on a hot, plastic mantle. All plates are slowly moving and have rafted continents to new positions over time.
<!   stratification: Stacked layers of sedimentary rock, built up by gradual deposition of volcanic ash, silt, and other materials over time.
 
]--   theory of uniformity: Early theory that the earth's surface changes in gradual, uniformly repetitive ways. Has since been replaced by plate tectonics theory.
 
<    adaptive radiation: Macroevolutionary pattern; burst of genetic divergences from a lineage that gives rise to many species.
 
       adaptive zone: Minimum amount of energy required to get a specific reaction going, with or without the help of an enzyme. Reactions differ in the amount required.
 
 
 

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