Introduction Flashcards

1
Q

Name the major microfossil groups:

A
  • Prokaryotes (cyanobacteria in PreCambrian);
  • Protistants (acritarchs, radiolarians, foraminifera;
  • Plants (spores and pollen);
  • Animals (ostracods, conodonts, SSF)
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2
Q

How long does the microfossil record extend to?

A

Archean (3.5Ga) - Eubacteria, cyanobacteria

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3
Q

How can microfossils be characterised, give examples?

A

By their skeleton composition:

  • calcareous (ostracods, foraminifera, nannoplankton)
  • siliceous (diatoms, radiolarians)
  • phosphatic (conodonts, SSFs)
  • organics (chitinozoans, acritarchs, dinoflagellates, SCF)
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4
Q

What are the environmental ranges of microfossil groups:

A
  • use diagram*
  • Pollen and spores from land to marine
  • ostacods and diatoms in freshwater and marine
  • acritarchs and benthic foraminifera in marine shelf and basin
  • chitinozoans, nannoplankton, planktonic foraminifera, radiolarians in marine basin
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5
Q

State the geological history of microfauna

A
Hadean: Prebiotic world
Archean: 3.8Ga origin of life
Proterozoic: 2.5Ga Earliest cyanobacteria
1.8Ga Early eukaryotes (acritarchs)
BORING BILLION
L. Proterozoic: SSF 
E.Cambrian: Forams
L.Cam.: Possible Ostracods, conodonts 
Mid. Ord.: Ostracods, Spores 
L.Dev.: Gymnosperm Pollen 
Triassic: Dinoflagellates, nannoplankton
Jurassic: Diatoms, Angiosperm pollen
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6
Q

Why are microfossils important?

A
  • Identifying the early evolution on earth, only fossil for about 3Ga
  • Help explain some important feedback loops between early evolution of the planet and biosphere
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7
Q

Whats the other name for organic walled microfauna?

A

palynomorphs

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8
Q

name the organic walled microfauna:

A
  • Acritarchs
  • Chitinozoans
  • Dinoflagellates
  • Pollen and spores (terrestrial)
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9
Q

What was the range for dinoflagellates and what forms do they come in?

A

Cambrian?
- Triassic to recent
Photosynthetic and heterotrophic forms, it is the cyst that preserves as a fossil
- expelled from coral in dying reefs

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10
Q

Name the microfossils that contribute to the silica cycle

A
  • Diatoms
  • Radiolarians
  • Silicoflagellates
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11
Q

When do the silica based microfauna range?

A
  • Radiolarians: Cam - recent, marine photic zone to abyssal depths
  • Diatoms: Lower Jurassic - recent, Marine and freshwater
  • Silicoflagellates: Lower Cret. - recent, marine photic zone
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12
Q

How many species of diatoms are there?

A

100,000, responsible for circa 45% of primary production in the ocean - organics

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13
Q

Which microfauna are important for the carbon cycle and palaeoclimate?

A
  • Ostracods
  • Foraminifera
  • Nannoplankton
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14
Q

When do the calcareous microfauna range?

A
  • Ostracods: Ordovician - recent, abyssal planes to damp leaf litter
  • Foraminifera: Lower Cambrian - recent, freshwater to deep ocean
  • Nannoplankton: Triassic - recent, marine photic zone
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15
Q

How many living species of ostracod are there?

A

65,000, most abundant arthropods in the fossil record, reflective of ecology

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16
Q

How many species of foram are there?

A

38,151 fossil and 8981 living, providing the best record of deep time climate

17
Q

What microfauna are responsible for 45% of marine primary productivity?

A

Algae: Coccolithophores (calcareous nannoplankton) and diatoms (siliceous)