Great Oxidation Event Flashcards

1
Q

How did the early Earth form?

A

-formed after collision with mars-sized planet called Theia + continually bombarding of meteorites at 4.5 bya/Ga (proterozoic)

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2
Q

What was the early earth called and why?

A

-hadean earth
-hades (hell-like)

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3
Q

After the hadean earth, what process occured to produce our core, mantle, and crust?

A

-earth was really hot so iron and nickel melted and sank to the middle due to gravity to produce the core
-lighter silciates floated to the top = this formed mantle and crust
-this process is called differentiation

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4
Q

after the earth differentiated and cooled below 1000 C, what formed? what type of landmass?

A

-rocks formed and landmass was mostly low-lying volcanic islands like hawaii; these rocks were ultramafic lavas called komatiites

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5
Q

even with the landmass, earth was mostly covered with what? coupled to this, we were able to date which type of rocks to the hadean earth?

A

-water
-sedimentary (3.9-3.8 by)

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6
Q

what was the atmosphere of early earth like? what were the effect of these gases on the environment?

A

-it had high CO2 and methane, no atmospheric O2, not ozone layer
-high temperature reaching 90C, really hot, lack of ozone layer means that there was no protection from UV radiation
-rain was highly acidic because of richness of acids -> chemical weathering

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7
Q

origin of life: what is the organic soup model?

A

monomers where formed by reduced gases in atmosphere + UV radiation -> could form amino acids

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8
Q

origin of life: what are the two ways that meteorites are hypothesized to play a role in the development of life?

A

-shock waves from entry into atmosphere formed shock waves that make a.a monomers form gases
-panspermia: comets carry organic compounds for life or actually life

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9
Q

the meteorites and organic soup models have been rejected for what reason?

A

difficult to form polymers in ocean due to monomer disperion

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10
Q

problem with shockwave and organic soup model is what?

A

CO2 acts as greenhouse, so atmosphere is not as reducing

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11
Q

the open ocean models for origin of life was problematic and the solution proposed was what?

A

evaporation of monomers lead to polymerization

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12
Q

last and most plausible start for origin of life?

A

reduced gases emitted at hydrothermal vents reacts with oxidizing seawater to form organic compounds and minerals are the templates of polymerization

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13
Q

what is the period of late heavy bombardment?

A

-happened 4.1-3.8 bya
-weakens organic soup model cause vaporized H20 would have sterilize the planet for years

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14
Q

life likely arouse in sheltered environemtn free from bombardments like what?

A

diffuse vents, black smokers associated with mid-ocean ridges

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15
Q

the oldest organisisms that we know of are what?

A

associated with growth in hot water, thermophilic prokaryotes

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16
Q

earliest cells used which chemical materials?

A

-sulfur
-methane (methanogenic bacteria in deep sea vent)

17
Q

what are 4 evidences of archean life?

A

-microfossils
-biogenic structures (stromatolities and MISS)
-isotopes
-biomarkers

18
Q

MISS stands for what? what are them?

A

-microbially induced sedimentary structures
-structures formed by microbial mats of filamentous bacteria trapped in sediments in tidal flat settings

19
Q

how do isotopes indicate life?

A

photosyn. takes in C12 and eriches C13 in environments
C13 (+) = low C12
C13 (-) = high C12 (photosynthesis)
-20 = biological (from photosynthesis)
-40 = from methanotrophic bacteria

20
Q

type of photsynthesis

A

oxygenic and anoxygenic

21
Q

when does cyanobacteria formed?

A

3.5- 2.7 bya

22
Q

though cyanobacteria evolved earlier, GOE happened when?

A

2.5 bya

23
Q

Proxies supporting timing of GOE

A

-red beds
-pyrite
-decreasing in 33S isotope (only produced in absence of oxygen)
-manganese ore
-banded iron formation (BIF)

24
Q

what was the lomagundi event?

A

long lasting peak of C13 isotopes during GOE; photosynthesis take in C12 (environment enriched in C13)

25
Q

BIF despite forming in shallow platforms, source of iron is what? iron is oxidized by what?

A

-deep hydrothermal vents
-oxygenic or anoygenic photosynthesis (both biological)

26
Q

How did NI depletion lead to GOE?

A

early earth rick in Ni and then earth cools so [Ni] decrease= starvation of methanotrophs = lower [methane] = increase [oxygen]

27
Q

increasing landmass contribution to GOE

A

allowed for Cyanobacteria and stromalites to grow

28
Q

what is the connection between pyrite oxidation and GOE?

A

oxidation = increasing acid which dissolves Cr which becomes part of BIF

29
Q

What prevented O2 accumulation before GOE?

A

-cyanobacteria were starved (low phosphate)
-dissolved iron was toxic to cyanobacteria
-many reductants that oxygen reached with first
-not enough landmass for cyanobacteria growth

30
Q

increase in oxygen and formation of ozone had which consequences?

A

-plankton growth in ocean
-biofilms conquered land = increase weathering
-euk diversification

31
Q

life in proterozoic

A

-thrombolities
-gunflint chert (BIF which microfossils)
-algae

32
Q

euk seen in fossils record at what time?

A

1.9bya (grypania)
1.2 (red algae)

33
Q

what are acritarchs?

A

organic-walled microfossils of unknown biological affinity, but with features interpreted as eukaryotic