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The fossil record 2
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The fossil record 2 What is a fossil? Where do we find fossils?
Why study fossils? Palaeobiology Geochronology Palaeoenvironments/climates How are fossils formed? Types of fossil preservation Quality of the fossil record
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Taphonomy - ‘fossilization’
The manner and cause of death Processes of decay and decomposition Transportation of fossils/potential fossils Burial of remains Diagenesis of remains
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NB text-book, p. 8-17
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Taphonomic information
life position, clustering articulation, breakage, sorting, orientation population structure - age and size frequency trace fossils sedimentology
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Types of preservation ‘Unaltered’ remains Altered remains Imprints
Soft parts - very rare Freezing Mummification amber, etc. Hard parts Altered remains Petrifaction Permineralization Recrystallization Replacement Carbonization Imprints Moulds/casts impressions Tracks, trails and burrows
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Unaltered remains - freezing
1999
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Unaltered remains - freezing
Lyuba (age 4 months, 40kya old) - discovered in 2007 in Siberian permafrost
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Unaltered remains - freezing
Dima (age 7 months, 40kya old) - discovered in 1977 by gold diggers in a lump of ice near the Kirgilyakh Creek
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Unaltered remains - amber
Oligocene (~30Ma) amber, Baltic
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Unaltered remains - amber
Oligocene (~30Ma) amber, Baltic
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Altered remains - permineralization
Triassic (~230 Ma) trees, Petrified Forest NP, Arizona
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Altered remains - recrystallization
NB. mineralogy is unchanged gastropod/snail
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Altered remains - replacement, e.g. aragonite to calcite
Peronoceras fibulatum Placenticeras meeki ammonites
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Altered remains - replacement, e.g. aragonite to pyrite
Jurassic ( Ma) ammonites
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Altered remains - carbonization
fossil fern frond (Neuropteris)
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Imprints - moulds and casts
internal mould external mould imprints
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Chemical/molecular fossils
degree of alteration may be difficult to determine
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Quality of the fossil record
Chances of fossilization Soft parts vs. hard parts Lagerstätten Biases Sedimentary environment e.g. marine vs. continental Stratigraphic bias older rocks - less exposure, tectonized Collection bias towards commonest and most accessible sedimentary facies (~environments) NB. oldest ocean crust 165 m.y.
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Chances of fossilization
~60% of marine animals are soft bodied and usually unrepresented in the fossil record (NB shell and coral carbonate is also broken down by bioerosions - up to 60% in coral reef settings) Discalioides jellyfish, Oligocene, Provence, Southern France
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Chances of fossilization
marine vs. continental environments + scavengers, decomposition
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Lagerstätten deposits of exceptional value - conservation
- concentration Solnhofen (Jurassic, S Germany) - a conservation lagerstätte Shrimp - Aeger tipularius
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Lagerstätten Solnhofen (Jurassic, S Germany) Dragonfly - Libellulium
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Lagerstätten Solnhofen (Jurassic, S Germany)
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Lagerstätten Messel (Eocene, Germany) beetle
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Lagerstätten Messel (Eocene, Germany) snake
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Lagerstätten Messel (Eocene, Germany) Fish - Cyclurus kehreri
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Lagerstätten Messel (Eocene, Germany)
Turtle - Allaeochelys crassesculptata
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Lagerstätten Messel (Eocene, Germany)
Mammal - Propalaeotherium parvulum Messel (Eocene, Germany)
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Lagerstätten Messel (Eocene, Germany) Marsupial - Leptictidium nasutum
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Lagerstätten Messel (Eocene, Germany) Bat - Archaeonycteris trigonodon
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Lagerstätten Holzmaden (Jurassic, Germany)
marine reptile - ichthyosaur Holzmaden (Jurassic, Germany)
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Quality of the fossil record
Chances of fossilization Soft parts vs. hard parts Lagerstätten Biases Sedimentary environment e.g. marine vs. continental Stratigraphic bias older rocks - less exposure, tectonized Collection bias towards commonest and most accessible sedimentary facies oldest ocean crust 165 m.y. UP TO HERE!!
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Stratigraphic bias
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Collection bias e.g. oceans vs. shelf sediments Europe vs. Asia, etc.
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Quality of the fossil record - biases but ……
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Quality of the fossil record
Palaeobiology and the Fossil Record Benton & Harper
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Quality of the fossil record
‘corrected’ for sampling biases Sepkoski data PBDB data Alroy et al. 2008, Science
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