chapter 25: ap bio

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49 Terms

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how did life arise? 1

small organic molecules were synthesized (ex. amino acids and nitrogenous bases)

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how did life arise? 2

small molecules polymerized into macromolecules (ex. proteins and nucleic acids)

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how did life arise? 3

molecules packaged into protocells

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protocells

membrane-containing droplets

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how did life arise? 4

self-replicating molecules allow for inheritance (RNA)

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ribozyme

first RNA catalysts

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when did earth form?

4.6 billion years ago

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what did earth's early atmosphere contain?

water vaper and chemicals released by volcanic eruptions, such as nitrogen, nitrogen oxides, carbon dioxide, methane, ammonia, hydrogeb, hydrogen sulfide)

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oparin and haldane

hypothesized a reducing environment

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miller and urey

lab experiments proved the abiotic synthesis of organic molecules (like amino acids)

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alternative theory 1

first organic compounds were synthesized near volcanoes or deep-sea vents

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small organic molecules would polymerize when

concentrated on hot sand, clay, rock

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what can lipids do in water?

form vesicles with a lipid bilayer

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the first genetic material was?

RNA, not DNA

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ribozymes do what?

make complementary copies of short stretches of RNA

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the first living organisms have been documented

3.5 billion years ago

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3.5 bya there was no

oxygen

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when did oxygen appear?

2.7 billion years ago

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what allowed for the production of oxygen?

cyanobacteria would undergo photosynthesis

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what is strata?

layers of rock

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incomplete record

many organisms not preserved, fossils destroyed, or not yet found

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fossil record is biased towards

existed for a long time, abundant, widespread, had hard parts

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radiomentric dating

a way to find the age of fossil using the half-life

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half-life

the time required for half the parent isotope to decay

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relative dating

uses order of rock strata to determine the relative age of fossils

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each era ends and starts with

ends with major extinction and starts with adaptiove radiation

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timeline

3.5 bya - first prokaryotes

2.7 bya - oxygen in atmosphere

2.1 bya - first eukaryotes

1.2 - first multicellular eukaryotes

500 mya - colonization of land

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stromalites

the oldest fossil- rocks formed by the aaccumulation of sedimentary layers on bacterial mats

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banded iron formations

oxygen that reacted with dissolved iron and precipitated out to form

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oxygen revolution

caused the extinction of many prokaryotic groups

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endosymbiont theory

mitochondria and chloroplasts were formerly small prokaryotes living within larger host cells

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cambrian explosion

the sudden appearance of fossils resembling modern animal phyla

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plants and fungi

mutually beneficial and likely colonized land together

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the rise and fall of groups depend on

speciation and extinction rates within the group

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plate tectonics

earth's crust is composed of plates floating on earth's mantle

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interactions between plates cause

the formation of mountains and islands, and earthquakes

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the distribution of fossils and living groups reflects

the movement of continents

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mass extinction

a large extinction of species in a relatively short period of time

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factors that contribute to mass extinctions

volcanoes, glocal warming, redcued temperature gradient, reduced mixing of ocean waters

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alternative theory 2

organic molecules could have been transported to earth by a meteorite

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adaptive radiation

evolution from a common ancestor of many species adapted to diverse environments

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adaptive radiation may follow

mass extinctions, evolution of novel characteristics, colonization of new regions

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heterochrony

evolutionary change in the timing or rate of an organism's development

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heterochrony examples

human and chimpanzee skulls

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paedomorphosis

the rate of reproductive development accelerates compared with somatic development

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homeotic genes

genes that determine basic features of where a body part is

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homeotic gene example

wings on a bird

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hox genes

class of homeotic genes. changes in these genes can have a profound impact on morphology

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exaptations

structures that evolve in one context but become co-opted for another function