Week 2 Flashcards

1
Q

Taphonomy

A

study of natural processes that occur to a dead animal (decay, erosion, potential scavenging)

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2
Q

Bloat and float

A

One of the many ways a carcass can move from where it died to a new location, caused by build up of gasses then carried by water

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3
Q

Vehicles of carcass movement

A

Flowing water, scavengers, broken part then washed away (depends on weight and shape), sunlight disintegration, losing only a bit that becomes exposed, mineral content leached away.)

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4
Q

Plastic deformation

A

The deformation of bones from pressure of rocks

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5
Q

Preferable fossilization environment

A

Wet environments (so that water can bury the carcass in silt/mud/sand)
low elevations (where silt/mud/sand are washed too)

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6
Q

Fossil probable location

A

Ancients rivers, streams, lake deposits

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7
Q

Lacustrine deposits

A

fossils found in old lakes, higher chance to fossilize hair or feathers because of little water movement and because of fine particulates like mud providing better feather fossilization chance

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8
Q

Fluvial deposits

A

Fossils found in rivers and streams

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9
Q

costal deposits

A

don’t often find fossils here but can happen by a storm washing the carcass out. Only found in the shallows

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10
Q

Aeolian deposits

A

Are also wind-based deposits, usually found the in desert. Not common at all but found in abundance in Mongolia as there was a river

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11
Q

Sedimentary rocks

A

where most fossils are found (very few exceptions), they form from particulates that accumulate and then compact together

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12
Q

Igneous rocks

A

solid magma rocks

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13
Q

metamorphic rocks

A

form when other rocks undergo changes by heat or pressure (fossils don’t survive this)

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14
Q

Different types of sedimentary rocks

A

Mudstone, from mud mostly in lakes and slow rivers
Shale, from silt mostly in lakes
Sandstone, from sand indicates former beach, river channel or ocean floor
coal, comes from compression of plant material, indicates former swamp
limestone, from shells and exoskeletons of small marine invertebrates, indicates former shallow marine environment

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15
Q

Permineralization

A

Preservation style of empty internal spaces filled with minerals, water deposits the minerals in the bone voids

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16
Q

Replacement

A

preservation style of bone gradually decaying then minerals fill in the space

17
Q

Best chance for finding fossils

A

The burial process has to be partly undone to re expose the fossil. So a place with minimal plant life is preferable to increase erosion rates

18
Q

overburden

A

Rock and earth that covers the fossil

19
Q

Bone bed

A

they location of many bones. as they are removed they are carefully mapped relative to each other `

20
Q

Long bone alignment

A

when the long bones are oriented parallel they most likely traveled down a fast flowing river

21
Q

Plaster shell

A

The fossils are delicate and unlikey to hold their own weight so they are covered in plaster to support them

22
Q

Marks on bone giving hints

A

Disarticulation can point to scavenging
long bone orientation is a point of how it was moved
abrasion from water erosion and impacts can show how far down a river it went
tooth marks indicate scavenging