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Marine Microfossils

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Marine Microfossils Dr. J Bret Bennington Department of Geology What are marine microfossils? Fossilized remains of small organisms or tiny hardparts of larger organisms. – PowerPoint PPT presentation

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Title: Marine Microfossils


1
Marine Microfossils
2
What are marine microfossils?
  • Fossilized remains of small organisms or tiny
    hardparts of larger organisms.
  • Plankton
  • Benthic fauna
  • Many different groups representing animals,
    protists, and a variety of algae.

3
Protistan Microfossils
  • Mineralized test (shell) formed by amoeba-like
    protozoans.
  • Foraminifera - calcareous (calcium carbonate) or
    agglutinated (test composed of cemented grains of
    sand or other sediment).
  • Radiolaria - test composed of silica.

4
Foraminifera - sarcodina (amoeba)
Protistan Microfossils
5
Foraminifera - sarcodina (amoeba)
  • Benthic forams
  • live in sediments
  • relatively large
  • Planktic forams
  • live floating in the water column
  • relatively small

Protistan Microfossils
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Foraminifera - sarcodina (amoeba)
Benthic forams
Protistan Microfossils
Calcite
8
Foraminifera
Planktic forams
Calcite
Protistan Microfossils
9
Radiolarians - Spumellarians
Protistan Microfossils
Silica
10
Radiolarians - Nacellarians
Protistan Microfossils
Silica
11
Animal Microfossils
  • Mineralized shells and teeth produced by
    metazoans (multicellular animals).
  • Ostracods - calcareous (calcium carbonate) shell
    produced by tiny crustaceans.
  • Conodonts - calcium phosphate teeth produced by
    an extinct group of vermiform (worm-like)
    vertebrates.

12
Ostracods - Arthropoda
Animal Microfossils
calcite
13
Conodonts - Vertebrata
Animal Microfossils
14
Conodonts - Vertebrata
conodont apparatus
Animal Microfossils
15
Conodonts - Vertebrata
Animal Microfossils
16
Conodonts - Vertebrata
Animal Microfossils
calcium phosphate
17
Algal Microfossils
  • Mineralized tests and plates produced by a
    variety of unicellular algae.
  • Coccolithophorids - tiny algae that produce
    calcareous plates - main component of chalk.
  • Diatoms - algal cells that produce paired tests
    (called frustules) composed of silica.
  • Dinoflagellates - marine algae that produce
    organic cysts preserved in sedimentary rock.
    Also the cause of most harmful algal blooms
    (HABs).

18
Coccolithophorids - Haptophyta
calcite
Algal Microfossils
19
Chalk Cliffs, England
20
Diatoms - Chrysophyta
silica
Pennate - benthic, parasitic
Centric - planktic
Algal Microfossils
21
Diatoms - Chrysophyta
silica
Algal Microfossils
22
Diatoms - Chrysophyta
silica
Algal Microfossils
23
Dinoflagellates - Pyrrhophyta
Sporopollenin
living
fossil
Algal Microfossils
24
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Dinoflagellates - Pyrrhophyta
Living cell
Cyst
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Why are marine microfossils useful?
  • Biostratigraphy - dating rock layers using
    fossils.
  • Environmental reconstruction - identifying
    different marine environments in the past.
  • Paleothermometry - determining ocean water
    temperature in the past.
  • Paleoclimatology - reconstructing climate change
    through Earths history.

29
From Sugarman, et. al, 1995
Biostratigraphic zones - intervals of time
defined by the presence of particular fossil
species.
30
From Sugarman, et. al, 1995
31
From Sugarman, et. al, 1995
32
Deep Sea Drilling Project ship - Glomar Challenger
33
Recovering sediment cores from the deep ocean.
34
Foraminifera
  • Fossil foram species can be used to date age of
    seafloor and sediment layers.

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Stable Isotopes Oxygen
99.76
.2
CO2 H2O HCO3-1 H
2 HCO3-1 Ca CaCO3 H2CO3
  • O18 is preferentially removed from seawater
    during calcite formation.
  • This effect is sensitive to temperature.
  • Ratio of O18 / O16 in shell is temperature
    dependent.
  • Can be measured using a mass spectrometer.

38
Mass Spectrometer
39
Increasing 18O in calcite relative to water
Change in isotopic ratio in carbonate shell with
change in water temperature.
40
Modern sea-surface temperature
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d18O due to ice buildup Glaciations cause more
d18O to accumulate in seawater. This happens
because 16O evaporates preferentially and becomes
trapped on land as glacial ice.
H216O
42
Average d18O curve from 5 deep sea cores (foram
calcite). After Imbrie et al. (1984)
43
Onset of Cenozoic cooling trend - development of
cold deep ocean circulation.
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Navesink Formation, central New Jersey
46
70X
Benthic foraminifera
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70X
Benthic foraminifera
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70X
Planktic foraminifera
49
70X
Ostracod
50
70X
Ostracod valve
51
70X
Burrowing echinoid spine
52
70X
Fish denticle
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