Fossils & Stratigraphy 5.4 Flashcards

1
Q

Uniformitarianism?

A

The self evident truth that all natural processes & scientific laws are the same throughout time & the universe.

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2
Q

Superposition?

A

The older layers are always beneath the new/younger layers

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3
Q

Stratigraphy?

A

Study of strata in rocks

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4
Q

Relative Dating?

A

Determining the age of a layer by comparing it with the above layer and below layer.

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5
Q

Fossils and how they form? (4 types)

A

Casts & Moulds

  • hard shells, bones preserved in sediments but slowly dissolve leaving a mould
  • if cavity fills it becomes cast

Carbonisation

  • Tissues of organism chemically changed to carbon-rich material like coal
  • Common for plants

Mineralisation

  • Minerals precipitate into hollow parts of fossil > hardening it e.g. petrified wood
  • Mineralisation can occur in tiny spaces (hollow cells) like plant veins > detailed fossil

Replacement
-Hard parts of organism dissolved by water chemicals & replaced by minerals

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6
Q

Index Fossils?

A

-Fossils or organism which lived in many places throughout Earth but flourished for short time
-Many are microscopic plankton with silica skeletons
-remains are widespread in sediments from a particular time & instantly recognisable
-presence of index fossils tells us where in history we’re looking at:
above it = younger
below it = older

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7
Q

What can we conclude from Index Fossils?

A

Using stratigraphy & absolute dating we find:

  • end of snowball earth =(same time) first Ediacaran fossils
  • Oxidation of sediments increased 15% - 20% FAST = perfect amount for larger animals to function well
  • Maybe global warming > more algae photosynthesis > releasing more Oxygen
  • at some point evolution of larger, oxygen dependant animals became possible: Ediacarans arise!
  • End of snowball earth = tectonic rifting and volcanic activity > releasing C02 and causing global warming
  • Rifting at MOR = concentrations of Calcium ions in oceans to rise > calcium ions essential for skeleton & shells to evolve
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8
Q

Extinction?

A
  • When 30% or more species world-wide become extinct within 2 my or less
  • Detected by counting number of types of living things found as fossils in rocks from each period in history
  • info needed from all global fossil sites
  • When types are graphed against time > mass extinctions shown as sudden large dips in graph
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9
Q

Mass Extinctions & The Geological Time Scale

A
  • 2 mass extinctions correspond to division on Phanerozoic Eon
  • Major mass extinctions are the divide between periods
  • mass extinction divided Ordovician & Silurian periods of the Palaeozoic Era
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10
Q

The End-Permian Extinction?

A

Marks division between Palaeozoic & Mesozoic Eras (95% earth species became extinct)

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11
Q

Evidence of End-Permian Extinction?

A
  • Fossil studies > 95% extinct over 2-3 phases over 1-2 mys
  • Sedimentary layers show big drop in sea levels followed by big rise
  • Volcanic lava structures in Siberia date from this time > total amount of lava could bury earth 10m deep
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12
Q

Hypothesis of End-Permian Extinction?

A
  • resulted from climate changes induced by huge volcanoes over 60 thousand years
    1. dust/ash caused cooling > ice caps > lea levels drop > Marine life in shallow seas died out
  1. so much C02 in atmosphere > greenhouse global warming occurred > ice melted, sea levels rise > oceans made anoxic by rotting of dead materials > made acidic by dissolved C02 & volcanic gases
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