Formation Of Fossils Flashcards

1
Q

Outline exceptional preservation in Amber

A

Tree resin that has been hardened and preserved. Flowed from trees, accumulated on trunk, animals get caught in it. Hardened by chemical reactions-tells us what was present in ancient forests

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2
Q

What type of exceptional preservation can be seen displayed in Scandinavia?

A

Amber formed by resin of extinct pine Pinus succinifera used for jewellery-gold of the north

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3
Q

Outline exceptional preservation in tar pits

A

Hydrocarbons migrate to surface to form poop of asphalt, water accumulated on top, animals lured in and become trapped

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4
Q

Outline processes of exceptional preservation in the Burgess Shales

A

Cambrian age, found in Canadian Rocky Mountains, snapshot into evolution of life on Earth, animals all extinct but soft parts preserved replaced by clay mineral. Found trilobites, crabs, velvet worms- totally soft bodies so wouldn’t have known about its existence without

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5
Q

Define Benthonic

A

Creature that lives in it on sediment substrate in sea floor

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6
Q

Define infaunal

A

Organism lives in sediment, usually in a burrow

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7
Q

Define epifaunal

A

Organism lives on sediment substrate

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8
Q

Define sessile

A

Organism does not move around on substrate, may be attached or free lying

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9
Q

Define vagrant

A

Organism moves around on sea floor, may be a scavenger it predator

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10
Q

Define pelagic

A

Organism lives in water column

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11
Q

Define Nektonic

A

Organism actively swims in the water column

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12
Q

Define pelagic

A

Floats in the water column to wherever the current will take it

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13
Q

Define mechanism of replacement

A

Original material slowly dissolved and substituted with another, most common Is aragonite to calcite- polymorphs as calcite is more stable. Typically replaced with another mineral present in the groundwater

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14
Q

Define mechanism of silicification

A

Percolating groundwater rich in SO2 moves through the rock. Minerals crystallise out I solution to full pores and voids in the rock, may be space left behind by dissolves material or in pores within mineral-often in bone or wood

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15
Q

Define mechanism of pyritisation

A

Replacement of original material by iron pyrites. In anoxic environments with only sulfur bacteria present, use sulfur to respire, reduces sulfur to bisulphate, reacts with iron to iron pyrites, then replaces the fossil material. Common in deep sea of swamps

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16
Q

Where in the world are important exceptionally preserved fossils found?

A
Burgess shales in Canada, Cambrian 
Changjiang formation in China, Cambrian 
Soom Shales in South Africa, Ordivician 
Herefordshire Lagerstatten, Silurian 
Solenhofen Limestone, Germany
17
Q

What are the types of trace fossils?

A

Tracks on bedding planes, soft sediment

Trails on soft sediment, made by whole or parts of organism

Burrows soft sediment, dwelling, locomotion or protection

Borings stuctures in wood or Rick, hard substrate
Excrement fecal pellets, covered quickly so high sedimentation

Root structures woody impression in rocks or lignite, shallow marine, terrestrial

18
Q

What are the main types of preservation?

A
Replacement 
Silicification
Pyritisation
Carbonisation 
Mould and cast formation
19
Q

How can dinosaur tracks give us information about the animal that made it?

A

Shape of soft parts
Patterns of scales on the skin
Weight, estimated by size and length and depth
Running/walking speed

20
Q

Outline mechanism of carbonisation

A

Occurs during burial, overlying rock increases temperature and pressure, squeezes out volatiles, given off as gas, increasing carbon content. Fossils left as thin layer of carbon within mudstone or shales

21
Q

Define mechanism of mould and cast formation

A

Fossils dissolved out of rock they are in, leaving void in the rock. Breaking rock open would show external mould, imprint of fossil, internal mould formed if fossil filled with sediment before burial, cast made if void filled with another material

22
Q

What is a fossil?

A

Remains of a living organism, mostly formed from hard parts, can be body fossils or trace fossils

23
Q

What factors affect the type of fossilisation

A
Original composition
Energy levels 
Transport distance
Rapidity of burial
Amount of oxygen 
Size if sediment 
Diagnosis
Composition and acidity of groundwater
24
Q

What is a derived fossil?

A

Organisms originally preserved in older sedimentary layer are eroded, transported and deposited in younger later. Rounded and broken due to transport

25
Q

How can fossil assemblages indicate paleoenvironments

A

Thick shells, ribbed, attachment mechanism, broken fragments indicate high energy
Thin shells, wise shells, complete specimens indicate low energy

26
Q

What is an assemblage?

A

More than one fossil type found in a rock

27
Q

What us a defeats assemblage and how is it recognised?

A

Accumulation of fossils after death, transported and broken then deposited, not in their living position
Broken and fragmented
Sorting of shells by size
Alignment to currents
Mixture of organisms not generally found in same environment

28
Q

What is a life assemblage and how is it recognised?

A

Fossils found in living positions eg in reef community or in burrow. Have not been transported, complete and in position they lived in

29
Q

What is exceptional preservation?

A

Fossils have fine details or soft parts preserved

30
Q

What are the ideal conditions for exceptional preservation to occur?

A
Rapid burial in soft sediment 
Burial in low energy conditions
Lack of oxygen 
pH is acidic 
No scavenging animals
31
Q

Why may fossil record be biased?

A

Generally only hard parts preseved, some fossils may be entirely soft parts, better preservation in marine conditions

32
Q

Where in Britain can exceptionally preserved fossils be found?

A

Charwood forest in Leicestershire, Cnidaria, 575Ma related to corals

33
Q

What is a trace fossil?

A

Tracks trails and burrows left behind by ancient organism, provide glimpse of nature and behaviour and help interpret paleoenvironments

34
Q

How are trace fossils formed?

A

Organism walks across fine soft substrate, leaves imprint

Footprints infilled with sediment before destroyed, may be seen on base of i filling sediment layer