Spores and pollen Flashcards

1
Q

What are spores and pollen made of?

A
  • organic walled microfossils or palynomorphs
  • Sporopollenin is a very resistant organic compound
  • 30 microns to a few hundred microns in diameter
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2
Q

Name the land plant families that produce spores:

A

Seedless plants

  • Bryophytes
  • Lycophytes
  • Pteridophytes (Ferns)
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3
Q

Whats the difference between bryopytes and pteridophytes?

A
  • Bryophyte spores are a single size

- Pteridophyte spores can be homosporous or heterosporous with larger female spores

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4
Q

What is the geological range of spores and pollen?

A

Spores: Ordovician to recent (earliest crytospores)
Pollen: L. Devonian to recent

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5
Q

Where does a spore germinate through?

A

Their laesura

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6
Q

Describe spore morphologies:

A
  • Monolete spores have a single laesura, tetragonal tetrad

- Trilete spores have a Y-shaped mark, tetrahedral tetrad

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7
Q

What did mid Silurian plants lack?

A

425Ma Trachaeophytes had no roots

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8
Q

Describe spore wall structure:

A

External surfaces may be smooth or sculptured with either positive (protrusive) or negavtive (indenting) elements

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9
Q

What microfauna do mid devonian spores also look like?

A

Acritarchs

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10
Q

Name the pollen producing plant familys

A

seed plants

  • gymnosperms (non- flowering)
  • angiosperms (flowering)
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11
Q

Describe pollen evolution:

A

Devonian: earliest pollen
Carboniferous: Large increase in diversity creating forests and gymnosperm pollen developed
Lower Cretaceous (or Upper Jurassic): Angiosperms developed

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12
Q

What are the types of gymnosperm pollen sacs?

A

They are air sacs from the expansion of the pollen wall

  • Monosaccate
  • Bisaccate
  • Trisaccate?
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13
Q

What are the types of angiosperm pollen grains?

A
  • Monads (single grains)
  • Dyads (pairs)
  • Tetrads (fours)
  • Polyads (groups of fours)
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14
Q

Spore and pollen uses:

A
  • Biostratigraphy of marine + non-marine strata (terrestrial)
  • Palaeoenvironmental analysis
  • Palaeogeography
  • Primary record for Plant taxonomy and evolution
  • Palaeoclimate reconstruction
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15
Q

What are the 3 key applications for organic walled microfossils?

A
  • In forensic application (terrestrial palynology used to place criminals at the scene)
  • Palaeoclimate/palaeoenvironmental analysis (e.g. evolution of rivers)
  • Search for hydrocarbons, where spores, pollen, dinoflagellates and acritarchs all play a huge role
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16
Q

How do plants have an environmental impact on river systems:

A

Plants bind sediment together and possible cause meandering before that most rivers were braided

  • increased meandering
  • increased mudrock proportion
  • increased sandstone maturity
  • increased bioturbated fine sediments and lateral accretion surfaces (Davies and Gibling 2012)
17
Q

Describe how you use organic microfossils to find oil:

A

Look at Arabian peninsula - Palaeozoic succession

  • Acritarch diversity reflects palaeodepth (Ordovician in China)
  • Find max flooding surface from max carbon sequitation
  • Find biostratigraphy and environment against chronostratigraphic record
  • Acritarchs = marine phytoplankton and tell us the max diversity/abundance on the palaeo open marine/ shelf environments
  • In L.Silurian finding acritarchs and chitinozoans suggest another max flooding surface and therefore oil!