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Precambrian Time: Vast and Puzzling

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Title: Precambrian Time: Vast and Puzzling


1
Precambrian Time Vast and Puzzling
  • Chapter 13, Section 1

2
Precambrian History
  • The Precambrian encompasses immense geological
    time, from Earths distant beginnings 4.56
    billion years ago until the start of the Cambrian
    period, over 4 billion years later
  • The Precambrian comprises about 88 of the
    geologic time scale
  • Most Precambrian rocks do not contain fossils,
    making correlating rock layers difficult
  • Many rocks are metamorphosed and deformed,
    extremely eroded, and hidden by overlaying strata

3
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4
Concept Check
  • Why are specific events in Precambrian history
    difficult to determine?
  • Most Precambrian rocks do not contain fossils,
    which makes correlating rock layers difficult.
    Many Precambrian rocks are metamorphosed and
    deformed, extremely eroded, or hidden by
    overlying strata.

5
Earth Forms
  • Scientists hypothesize that Earth formed as
    gravity pulled together dust, rock, and ice in
    space gravity increased as Earth grew and began
    pulling in more materials
  • The high velocity impacts caused the planet to
    melt and divide into specific layers based on
    density
  • Over several hundred million years, the crust and
    mantle cooled and hardened, forming rock

6
Earth Forms
7
Earths Atmosphere Evolves
  • Earths original atmosphere was made up of gases
    similar to those released in volcanic eruptions
    todaywater vapor, carbon dioxide, nitrogen, and
    several trace gases, but no oxygen
  • Torrential rains continued and slowly filled low
    areas, forming the oceans this reduced the water
    vapor and carbon dioxide in the atmosphere,
    leaving behind a nitrogen rich atmosphere
  • Primitive organisms evolved that used
    photosynthesis and released oxygen
  • Slowly, the oxygen content increased, seen in the
    banded iron formations (which took the free
    oxygen out of the atmosphere)
  • Oxygen began to accumulate in the atmosphere
    about 2.5 billion years ago

8
Evidence of Early Oxygen
9
Concept Check
  • Why did the amount of oxygen in Earths
    atmosphere increase dramatically?
  • The evolution of organisms that used
    photosynthesis caused the release of increasing
    amounts of oxygen into the atmosphere.

10
Precambrian Rocks
  • The lack of Precambrian rock illustrates the law
    of superposition, it is covered by much younger
    strata
  • Precambrian rocks do show through the surface
    where younger strata are extensively eroded, such
    as in the Grand Canyon and in some mountain
    ranges
  • Shield a large relatively flat expanse of
    ancient metamorphic rock within the stable
    continental interior
  • Much of what we know about Precambrian rocks
    comes from ores mined from shields
  • The mining of iron, nickel, gold, and other
    metals has provided Precambrian rock samples for
    study

11
Remnants of Precambrian Rocks
12
Precambrian Fossils
  • The most common Precambrian fossils are
    stromatolites
  • Stromatolite structure produced by algae
    trapping sediment and forming layered mounds of
    calcium carbonate
  • Remains of cyanobacteria have been found that
    extend the record of life back beyond 3.5 billion
    years
  • Many of these ancient fossils are preserved in
    cherta hard, dense chemical sedimentary rock
  • Plant fossils date from the middle Precambrian,
    but animal fossils date to the late Precambrian
    (many are trace fossils)

13
Precambrian Fossils
14
Assignment
  • Read Chapter 13, Section 1 (pg. 364-368)
  • Do Section 13.1 Assessment 1-8 (pg. 368)
  • Print Out Application Lab 13 Modeling the
    Geologic Time Scale
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