THE PROTEROZOIC EON OF PRECAMBRIAN TIME
2.5 b.y. - 544 m.y. Eras:
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Paleoproterozoic (2.5-1.6 b.y.)
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Mesoproterozoic (1.6-1.0 b.y.)
(Not necessary to memorize any of these)
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Neoproterozoic (1.0 b.y.-544 m.y.)
Important Topics
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Modern style orogenesis
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Glaciations
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Evolution of the atmosphere
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Proterozoic evolution of North America
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The formation of Rodinia
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Origin of eukaryotes
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Life evolution through the fossil record
MODERN STYLE OROGENY: Woopmay Orogen in the Slave Province
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magmatic arc core
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regional metamorphic rocks
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fold and thrust belt: flysch followed by molasse sediments
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Origin: collision of Woopmay Craton with volcanic arc
GLACIATIONS: First about 2.3 b.y.a.
Four between 850 & 600 m.y.a.
Varangian Glaciation: (last one) affected every continent
except Antarctica, => climate at the end of the Proterozoic extremely
cold.
Evidences: _______________, ____________________, ________________, striations.
ATMOSPHERE: Out gassed Archean atmosphere had very little oxygen,
Cyanobacteria => Photosynthesis => released O2 (late Archean)
Atm. build up not possible until oxygen sinks were filled (iron
precipitation & pyrite)
Sinks filled at about 1.9 b.y.a.
Evidences:
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Banded iron formations (BIF's) in 2 b.y.a. rocks
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Paleosoils without iron older than 1.9 b.y.a.
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Continental red beds younger than 1.9 b.y.a.
Ocean's surface O2 abundance => oxidation of N2 to nitrates
= a nutrient for the expansion of planktonic eukaryotes.
DANCE OF THE CONTINENTS & ASSEMBLY OF NORTH AMERICA
Recall: Continents grow by suturing
-
another __________________
-
a ______________________
-
a _________________ ________________
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metamorphosed cont. shelf
sediments
Continents are reduced in size by
-
_________________________ (too slow to be
relevant)
-
rifting
The North American craton grew South & East by
accretion of crustal blocks, reaching as far south as northern Mexico.
Together with Greenland they formed _______________________________.
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1.2-1.0 b.y.a. Laurentia started to rift apart but aborted. What
is the evidence?
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basaltic flows & dikes +
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continental sediments
=> Keweenawan formation
Grenville orogeny (ended 1.0 b.y.a.) along Laurentia's _____________________
margin.
Sutured it to north South America (Gondwana continents to the
E & SW)
The Grenville suture is part of the extensive suturing
that joined most of the land masses into the super continent Rodinia
(1
b.y.a)
800 m.y.a. Rodinia breaks up by the formation of the _______________
Ocean. Evidence?
The Belt Supergroup (Canada & N. USA: contains ____________________
& mud cracks filled with salt crystals)
=> shallow marine environment
=> rapidly subsiding basin
=> frequent transgressions & regressions => rifting
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Pan-African Orogeny: Migration of the rifted portions of
Laurentia brought it into collision along opposite sides of the African
craton.
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New supercontinent? Between 700 & 500 m.y.a. numerous crustal
segments added to the African craton.
-
Climatic consequence of the supercontinent? __________________________
Huge land mass prevented the continent from receiving the warming effects
from the ocean.
PROTEROZOIC LIFE
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Early Proterozoic: similar to Archean
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______________________ dominate
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First eukaryotes: Archean; First eukaryote fossils:
Proterozoic
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Gunflint Flora (Lake Superior): Paleoproterozoic, prokaryotes only
(2 b.y.)
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Stromatolites become widespread: Mesoproterozoic
Origin of the advanced eukaryote cell
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Early eukaryotes very similar to prokaryotes & unicellular
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Advanced eukaryotes needed to evolve cytoskeleton (engulfing
ability)
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One prokaryotic cell came to reside within the other (was engulfed)
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Engulfed cell became the mitochondrion
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Mitochondria helps host cell to ______________ ____________ ____
________________ (respiration)
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Mitochondrial DNA & RNA ______________________ from host cell
Similarly,
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a cyanobacterium engulfed within another cell originated the
chloroplasts
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chloroplasts are the site of photosynthesis
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chloroplasts & cyanobacteria have ___________________________
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Chloroplast's DNA & RNA__________________________from host cell
ALGAE
First advanced eukaryotes were unicellular, but first advanced
eukaryote fossils were multicellular, seaweed like algae.
Eukaryotes became more abundant after 2 b.y. (after sea ________________________________)
Acritachs: resting state of ____________________________?
(plant-like protists)
ornamentation became more elaborate through the
eon
many species extinct & replaced after Varangian
glaciation.
EVOLUTION AND RADIATION OF METAZOAN FAUNA
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First multicellular animals were ___________________ _____________________.
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Known from trace fossils, soft body prints & few skeletal parts.
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____________________________ fauna (Australia): cnidarians, annelids,
arthropods and mollusks
Explosive radiation in the eon's last 50 m.y. Reason still unknown
.
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