Lecture 5 - Interpreting past environments Flashcards

1
Q

what frameworks are important?

A

temporal and spatial

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2
Q

what do spatial frameworks show?

A

how continents were configured/ paeleogeology

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3
Q

when did dinosaurs evolve?

A

in the triassic period - 50 million years in duration

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4
Q

what are wilson cycles?

A

repetitive cycles of continents drifting apart and then coming back together

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5
Q

what are the 5 basic ways of interpreting / reconstructing past environments?

A

1 - the nature of sediments
2 - the nature of fossil content
3 - the distribution of climatically sensitive sediments and fossils
4 - environmentally discriminating isotopes
5 - environmentally influenced characteristics of organisms
6 - modelling environments

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6
Q

how does the nature of sediments help to reconstruct past environments?

A

looks at the way physiochemical properties interact with water/ice

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7
Q

how does the nature of fossil content help to reconstruct past environments?

A

by looking at fossils you can get a clear idea of where sediment was deposited

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8
Q

examples of environmentally influenced characteristics of organisms

A

ostrochods - shell characteristics change depending on salinity levels
work out seasonality of the types of seasonality e.g. palms grow all year round and don’t have growth rings, others grow periodically = growth rings

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9
Q

early Jurassic geology

A

everything shifting northwards

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10
Q

late Jurassic geology

A

fracturing has occured e.g. N.America and S.America

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11
Q

early cretaceous geology

A

major ruptures, India split from Africa

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12
Q

biota evolve independently when?

A

continents become isolated e.g. Australia and marsupials

therefore more endemism expected in late cretaceous

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