topic 9 Flashcards

1
Q

features that define life

A

organization (one or more cells), metabolism, response to stimuli, homeostasis, adaptation, reproduction

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2
Q

are viruses alive

A

ish. they lack metabolism/homeostasis and cannot reproduce outside of a host cell

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3
Q

eons of the geologic record

A

archaean, proterozoic, phanerozoic (precambrian = archeaen/proterozoic)

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4
Q

eras of the phanerozoic eon

A

paleozoic, mesozoic, cenozoic

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5
Q

how are boundaries between geologic definitions made

A

mass extinction events from the fossil record

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6
Q

what are fosssils

A

preserved remains/evidence of past organisms, often found in sedimentary rock

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7
Q

rock strata

A

distinct layers of rock

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8
Q

what are fossils used for

A

calibrate phylogenies, record extinct species, link evolutionary events

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9
Q

why is the fossil record biased and incomplete

A

requres burial in sediment, often only hard parts preserved, most organisms were never fossilized

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10
Q

what increases the probability of fossilization

A

existed for a long time, abundant/widespread, hard bodied, aquatic, inshore marine, absent of decomposing organism

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11
Q

mold fossils

A

hollow space/impression eft my the organism

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12
Q

cast fossil

A

minerals fill the mold –> solid replica

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13
Q

replacement/petrified fossils

A

original tissues replaced by minerals (preserves detailed structure)

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14
Q

trace fossils

A

behavioral evidence (tracks, burrows, feces)

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15
Q

preserved possils

A

carbon films/amber/tar/peat/frozen that retain a lot of organic material

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16
Q

how does relative dating work

A

sedimentary strata reveal how old they are relative to eachother

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17
Q

issues with relative dating

A

leaves gaps, sediments can move around (overcome through indicator fossils)

18
Q

absolute/radiometric dating

A

radiactive decay of isotopes provides an absolute age for the fossil, based off of its half-life

19
Q

plate tectonics theory

A

the earths crust has large plates that have been slowly moving since 3.4 ba –> continental drift

20
Q

results of continental drift

A

tectonic plates collide/slide/separate, forming mountains, islands, earthquakes

21
Q

continental druft during the phanerozoic eon

A

alterations of physical geography and climate: fomration of pangaea leading to cooler/drier/deeper, impacting biodiversity through opportunities for diversification/speciation, mass extinctions,

22
Q

gondwana

A

paleo-continent of australia, antartica, s america having similar fossi

23
Q

continental drift and biodiversity

A

diversitification when land masses are isolated, mass extinctions as climates change

24
Q

permian mass extinction

A

between paleozoic and mesozoic eras (252ma), most servere extinction event, the great dying, caused by volcanic activity (or gradual changes)

25
cretaceous mass extinction
between mesozoic and cenozoic, 66ma, coincides with meteorite deposites --> impact-cause extinciton
26
holocene extinction
sixth, human-caused extinction, rapid decrease in biodiversity
27
consequences of mass extinctions
takes a long time to recover biodiversity, changes types of organisms in communities, can wipe entire lineages, adaptive radiation
28
adaptive radiation
rapid evolution of diversely adaped species from ancestral species (new niches available)
29
causes of adaptive radiation
mass extinctions, evolution of new characteristics, colonization of new regions
30
early earth
formed 4.6bya during hadean eon, very hostile for 1st by, thin crust on unstable magma, atmosphere without oxygen, water vapour as earth cooled, atmosphere of volcanic cases
31
how did life begin
abiotic synthesis of small organic molecules, polymerization, formation of protocells, emergence of self-replicating molecules
32
abiotic synthesis of small organic molecules
formation of basic organic compounds through abiotic proesses: spontaneous terrestrial origins or extraterrestrial impacts, likely near volcanoes or deep hyrothermal vents
33
miller-urey experiments
demonstrations that organic molecules can be produced spontaneously in reducing and non-reducing environments
34
polymerization into organic polymers
small organi molecules forming larger organic molecuels, likely on hot surfaces where evaporation of water triggered spontaneous formation of organic polymers
35
formation of protocells
lipids form a hollow vesicle (faster in volcanic clay), simple reproduction/metabolism, maintain an internal chemical environment
36
emergence of self replicating molecules
molecules that can store and transmit infomration (rna, dna), self replication to pass on information
37
catalysis
some rnas (ribosomes) act like enzymes inself-replicating molecules to speed up reactions
38
prokaryotes
oldest fossil evidence of life: unicellular, uncontained dna, organelles not membrane-bound, bacteria/archaea
39
stromalolites
oldest known fossils, accumulation of sedimentary layers on prokaryote mats
40
the great oxygenation event
when oxygen began accumulated in atmosphere and oceans, oceanic photosynthetic prokaryotes (cyanobacteria) evolved to use the sun's energy, producing o2 --> ocean saturation and eventual atmospheric oxygen
41
results of the goe
extinction of many prokaryotic groups (end of archean eon) because o2 was toxic to anaerobic prokaryotes, those that surived evolved aerobic respiration