Formation of the great lakes part 2 precambrian and paleozoic
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Formation of the Great Lakes Part 2 Precambrian and Paleozoic. History Channel Video Chapter 2 in Grady Chapter 2 in Greenberg. Great Lakes Basin in the Precambrian. Foundation for Great Lakes Basin (GLB) was formed over 3 bya in Precambrian Canadian Shield Igneous rocks

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Formation of the Great Lakes Part 2 Precambrian and Paleozoic

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Formation of the great lakes part 2 precambrian and paleozoic
Formation of the Great LakesPart 2Precambrian and Paleozoic

History Channel Video

Chapter 2 in Grady

Chapter 2 in Greenberg


Great lakes basin in the precambrian
Great Lakes Basin in the Precambrian

  • Foundation for Great Lakes Basin (GLB) was formed over 3 bya in Precambrian

    • Canadian Shield

      • Igneous rocks

      • Exposed in northern and northwestern part of GLB

      • Extends below sedimentary rocks deposited in the southern and eastern parts of GLB during Paleozoic era



Canadian shield
Canadian Shield

  • Once Shield formed

    • Middle of continent stable geologically

      • Craton

    • Margins of continent very active

      • Volcanism creating new land

      • Orogenies


Great lakes basin
Great Lakes basin

  • Remnants of the rocks of these three provinces form the deep basement of the Great Lakes basin.

    • Smooth

    • Grey to pinkish

  • Central Lowlands Province

    • Lower midwest USA region of the GLB

    • No shield rock is visible at surface

    • Region was covered over and over again by shallow sea

      • Bedrock here is limestone

      • Lots of evidence of ancient life – good fossils

    • Basin for lower Great Lakes

      • Resources: coal, natural gas, petroleum


Precambrian
Precambrian

  • The Precambrian is actually a segment of time that includes two eras, the Proterozoic and the Archaean that span billions of years.

  • The oldest rocks on earth formed during this time, as well as the first continents, and the earliest, simplest forms of life.



Archean
Archean

  • 3800 to 2500 mya

  • The oldest rocks on earth are from this era

  • During the Archean, the cratons--the masses of rock that make up the basic, initial structure of continents--formed.

  • The crustal bodies that formed were smaller than today's continents and are referred to as protocontinents.

  • Today, Archean-aged rocks are found in areas such as the Superior Upland and the Rocky Mountains.


Archean era
Archean Era

  • Major Events:

    • The earth was pummeled with meteors.

    • Scientists believe that a huge impact tore away a large chunk of the earth and trapped it in orbit, forming the moon.

    • Seawater and an atmosphere developed.

    • The oceans became populated with algae, bacteria, and colonies of microorganisms known as stromatolites (first oxygen deposited in atmosphere).


Precambrian1
Precambrian

  • Many of the oldest rocks found on earth today are found in the Superior Upland, a part of the Canadian Shield, the broad swath Precambrian rocks that curves around Hudson Bay.

  • These rocks make up the "core" of the North American continent.


Precambrian2
Precambrian

  • Other Precambrian rocks are found throughout the continent, in places such as the Adirondack Mountains, the Rocky Mountains, the Llano Uplift, the Black Hills, the Baraboo Range, and the Grand Canyon.


Great lakes basin in the precambrian1
Great Lakes Basin in the Precambrian

  • Volcanism and sedimentary deposits were the source of the rich mineral deposits found in this region

  • Early sedimentary and volcanic rocks were folded and heated into complex structures.

  • These were later eroded and, today, appear as the gently rolling hills and small mountain remnants of the Canadian Shield, which forms the northern and northwestern portions of the Great Lakes Basin.


Great lakes basin in the late precambrian cont
Great Lakes Basin in the Late Precambrian (cont.)

  • Central North America experienced repeated transgressions and regressions of shallow, tropical seas during Paleozoic

    • large areas of tropical coral reefs

    • seas deposited layers of materials that became sedimentary rocks

      • limestone, shales, sandstone, gypsum


Two types of cells
Two Types of Cells

  • Prokaryotes – cells without a nucleus, simple cell structure

    • Bacteria and Archaea

  • Eukaryotes – cells have a nucleus which contains the DNA, also have complex structure

    • Includes protozoa, algae, plants, fungi and animals (including us)


Life in the precambrian
Life in the Precambrian

  • Archaean Era - 3800 to 2500 mya

    • Oldest sedimentary rocks (3.8 BYA)

      • Few fossils

    • First life appears ~3.6 bya

      • Chemotrophic, anaerobic, asexual

      • Oldest fossils - 3.55 BYA

    • Prokaryotes dominate

      • Eubacteria and Archaea

      • Cyanobacteria form extensive stromatolite systems

    • Primitive Eukarya appear

    • Photosynthesis appears


How old are they
How old are they? 

  • Oldest known fossil bacteria are about 2.8 billion years old

    • Look like cyanobacteria suggesting ancient origin for photosynthesis

    • Cyanobacteria fossils from stromatolites date to 2.8 to 2.5 bya (maybe older)

      • Filamentous strands of cells resembling modern species of Oscillatoria or Lyngbya

    • Stromatolites still exist as living fossils


Formation of the great lakes part 2 precambrian and paleozoic

Floating cyanobacterial mat from a hot spring

Fossilized cyanobacterial mat


Formation of the great lakes part 2 precambrian and paleozoic

Colonial chroococcalean cyanobacterium from the Bitter Springs chert of central Australia, a site dating to the Late Proterozoic, about 850 million years old.



Formation of the great lakes part 2 precambrian and paleozoic

Palaeolyngbya also from the Bitter Springs chert.

Living Lyngbya



Stromatolites
Stromatolites

  • Layered mounds of calcareous material between cyanobacterial cells.

  • Following slides show fossil stromatolites

    • Closest place to find these: Upper Peninsula of Michigan

  • FOSSIL






Stromatolite formation
Stromatolite Formation Precambrian sea

  • Many layers were produced as calcium carbonate precipitated over the growing mat of bacterial filaments.

    • Photosynthesis by the cyanobacteria depleted carbon dioxide in the surrounding water, initiating precipitation of calcium carbonate.

    • The minerals, along with grains of sediment precipitating from the water, were then trapped within the sticky layer of mucilage that surrounds the bacterial colonies, which then continued to grow upwards through the sediment to form a new layer.

    • As this process occured over and over again, the layers of sediment were created.


Stromatolite structure
Stromatolite Structure Precambrian sea


Formation of the great lakes part 2 precambrian and paleozoic


Formation of the great lakes part 2 precambrian and paleozoic

Fossil Precambrian sea Oscillatoria


Formation of the great lakes part 2 precambrian and paleozoic

Living Precambrian sea Oscillatoria



Proterozoic
Proterozoic Precambrian sea

  • The Proterozoic was a time in which multicellular algae began to appear.

  • The continents grew in size

  • Oxygen began to build up in the atmosphere (from cyanobacteria).

  • Today, Proterozoic rocks are found in features like the Superior Upland, the Black Hills and the Adirondack Mountains.


Formation of the great lakes part 2 precambrian and paleozoic

Cambrian Precambrian sea


Paleoproterozoic 2500 to 1600 mya
Paleoproterozoic Precambrian sea (2500 to 1600 mya)

  • Oxygen present in atmosphere so -

  • Metabolism began diversification

    • Earliest Proterozoic life was single-celled and anaerobic – did not use oxygen

      • Oxygen was toxic to these organisms – 1st max extinction event!

      • Various ways to breakdown glucose anaerobically

    • Later, more complex single-celled aerobic life evolved which used oxygen

      • Use oxygen for the process of respiration


Paleoproterozoic
Paleoproterozoic Precambrian sea

  • Peak of stromatolites

    • Cyanobacteria oxygenated the atmosphere

  • Oxygen caused “Rusting of the Earth”

    • Depletion of oceanic iron

      • Combined with oxygen and precipitated as “rust”

      • Precipitated iron settled to the ocean floor

    • Iron found in Banded Iron Formations


Banded iron formations
Banded Iron Formations Precambrian sea

  • Banded Iron Formations (BIFs) are another type of stromatolite

  • 1.8 to 2.5 billion years old

  • Composed of alternating layers of iron-rich material (commonly magnetite) and silica (chert)

  • Also found in Northern Michigan

  • How they were made

    • Cyanobacteria provided the source of oxygen for BIF formation.

    • FOSSIL


Banded iron formations1
Banded Iron Formations Precambrian sea

  • How they were made #1

    • Large amounts of the soluble form of iron were released from the Earth's interior into the Archaean oceans. (reduced ferric iron)

    • Oxygen in the oceans would have oxidized (rusted) this iron to form insoluble (ferrous) iron oxide which precipitated and formed layers of reddish sediment on the ocean floor.

    • The layers or banding is assumed to result from cyclic peaks in oxygen production. It is unclear whether these were seasonal or followed some other cycle.


Formation of the great lakes part 2 precambrian and paleozoic

sis Precambrian sea


Banded iron formation
Banded Iron-Formation Precambrian sea

  • Seasonal and/or biological cycles resulted in intervening periods when iron or oxygen were not as available

  • The black layers are made of chert (micro-crystalline quartz) that was laid down during these intervening periods.


Banded iron formations2
Banded Iron Formations Precambrian sea

  • How they were made #2

    • It is also thought that bacteria may have played a role in the formation of these bands of precipitated iron.

    • Certain bacteria can oxidize reduced ferric iron to insoluble ferrous iron

  • Economic significance

    • BIF’s are important sources of iron ore (mining)

    • Bacteria are capable of precipitating a number of other minerals including manganese and even gold

      • These processes are being adapted to facilitate mining of these minerals and removal of heavy metal pollutants from soils


Formation of the great lakes part 2 precambrian and paleozoic

Banded Iron Formations Precambrian sea


F09 c pg13
f09_c_pg13 Precambrian sea


Complex single celled life
Complex Single-celled Life Precambrian sea

  • Acritarchs

    • Acid-resistant, organic-walled, micro-plankton

    • Common Proterozoic eukaryote fossils

  • Represent encysted "resting stage" of organism

    • Resting cysts of algae

    • Egg cases of small metazoans

    • Others are cysts of unknown eukaryotes


F09 20 pg16
f09_20_pg16 Precambrian sea


F09 21a pg17
f09_21a_pg17 Precambrian sea


Late proterozoic ice age
Late Proterozoic Ice Age Precambrian sea

  • Occurred from 850 to 635 mya in the late Proterozoic

  • Second, and possibly most severe glaciation in earth’s history

    • Glacial deposits are so widespread at this time that geologists refer to it as “Snowball Earth".

  • May have caused extinction of Acritarchs

  • It has been suggested that the end of this cold period was responsible for the subsequent Cambrian Explosion, However, this theory is still controversial

  • Formal name Varangian glaciation

    • Named after an area in Norway


Precambrian animals 650 to 544 mya
Precambrian Animals Precambrian sea 650 to 544 mya

Ediacaran Fauna of Australia and Newfoundland, CA

Soft Bodied Invertebrates


Life in the late proterozoic
Life in the Late Proterozoic Precambrian sea

  • In the latest part of the Proterozoic (~ 600 mya), multi-cellular, complex life is recorded in the fossil record.

  • Oldest fossils within Kingdom Animalia are Vendian age 650 to 544 mya, and are found at nearly 30 locations around the world, and are most distinctive.

  • Fossils are preserved as thin impressions on bedding surfaces of fine to medium-grained sedimentary rocks.

  • Organisms were very thin, lacked any minerallized hard parts or well developed organs or organ systems, and had a quilt-like outer surface.

  • Uncertainty about what groups of animals these fossils might represent, and, if they were ancestral to the animals that appeared in the late Cambrian.



Ediacaran biota
Ediacaran Biota Precambrian sea

  • Appeared immediately after the prolonged period of global glaciations towards the end of the Precambrian

  • Extraordinary organisms:

    • Discs

    • Fronds

    • Segmented morphologies

  • Locations

    • Flinders Range (Ediacaran Hills), South Australia

    • Avalon Zone of Newfoundland

    • Nama Group in Namibia

  • Jellyfish

  • Worm Tubes


Formation of the great lakes part 2 precambrian and paleozoic

Cyclomedusa Precambrian sea a jellyfish


Formation of the great lakes part 2 precambrian and paleozoic

Charnia masoni Precambrian sea - no known living descendants


Formation of the great lakes part 2 precambrian and paleozoic

Dickinsonia costata – Precambrian sea early relative of earthworms?


F09 27 pg19
f09_27_pg19 Precambrian sea

f09_27_pg19


F09 28 pg20
f09_28_pg20 Precambrian sea

f09_28_pg20


Formation of the great lakes part 2 precambrian and paleozoic

Trace fossils Precambrian sea of primitive worms



Formation of the great lakes part 2 precambrian and paleozoic

Charnia Precambrian sea

Cloudinia

Cyclomedusa

Dickinsonia

Parvancorina

Spriggina


Paleozoic era
Paleozoic Era Precambrian sea

  • With the coming of the Paleozoic Era, most of central North America was flooded again and again by marine seas, which were inhabited by a multitude of life forms, including corals, crinoids, brachiopods and mollusks.

    • The seas deposited lime silts, clays, sand and salts, which eventually consolidated into limestone, shales, sandstone, halite and gypsum.



The paleozoic periods
The Paleozoic Periods

  • Cambrian – Cambrian Explosion!

  • Ordovician

  • Silurian

  • Devonian

  • Carboniferous – coal forests

  • Permian – ended in mass extinction event

    • Largest mass extinction until the one going on now!

    • Cause? - maybe glaciation (Snowball Earth); asteroid?

Shallow seas covered GLB


Paleozoic
Paleozoic

  • The Paleozoic era witnessed the proliferation of life in diverse forms across the planet.

    • Animals and plants began to move out of the water and populate terrestrial environments.

  • As the continents shifted around the globe, they had, by the end of the Paleozoic, combined to form the supercontinent Pangaea.











Animals diversify
Animals Diversify

The Cambrian Explosion

570-505 million years ago


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