Stratigraphy & Geologic Time Flashcards

(31 cards)

1
Q

Principle of Superposition

A

Tendency for rock layers to be chronologically stacked.

Oldest rocks from oldest deposited sediments at the BOTTOM.
Layers become increasingly younger towards the top.

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2
Q

Exceptions to the Principle of Superposition

A

Igneous rock may cut vertically through the horizontal layers.

Mountain building events may tilt, fold & flip rock layers.

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3
Q

Stratigraphy

A

Science of using the arrangement & composition of rock layers to interpret geological history.

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4
Q

Formation

A

Large uninterrupted sequence of rock that is made up of multiple layers that all share similar properties & that all formed under similar conditions.

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5
Q

How do we determine absolute age of rock layers?

A

Radiometric dating - as isotopes decay & ratio of isotopes to decay products deacreases, use mass spectrometer to measure ratio & tell how long ago it formed.

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6
Q

Isotopes

A

variant of a chemical elements that has an unusual number of neutrons.

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7
Q

Which rocks cannot be accurately dated with radiometrics?

A

Sedimentary rocks - formed of pre-existing sediments

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8
Q

Which rocks are perfect for radiometric dating?

A

Igneous rocks - formed new.

Also, volcanic ash!

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9
Q

How can we use Igneous rocks to get date range for sedimentary rocks?

A

Dating igneous above and below the sediments tells us the range

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10
Q

Geological Time Scale

A

Standardized series of chronological divisions that parses the Earth’s history into discrete named units.

Largest <—————-> Smallest

Eons Eras Periods Epochs

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11
Q

Hadeon Eon

A

4.6 - 4 billion years ago

Moon ~4.5 bil yrs ago

Large oceans covered surface

Complex organic molecules formed in oceans & were prob earliest true life forms.

Oldest dated ROCKS from here @ ~4.4 bil yrs ago.

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12
Q

Archean Eon

A

4 - 2.5 bil yrs ago

oldest known FOSSILS from here of single celled organisms

Cyanobacteria: Photosynthetic & produced large amounts of oxygen gas that became concentrated in Earth’s atmosphere.

Stromatolites: Cyanobacteria formed these structures. Best early records of life. Look like lumpy stones & when cut in half cans ee layers created as cyano secreted sticky films that trapped sediment.

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13
Q

Proterozoic Eon

A

2.5b - 541 million yrs ago

~1.7 nillion yrs ago, first multicellular organisms evolved. No bones / hard structures & were generally microscopic, so poor fossil record.

Edicarian Period: ~630 - 541 mil yrs ago, large forms of life w/ some harder parts evolved, including first animal life!

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14
Q

Phanerozoic Eon

A

541 - 0 million years ago.

3 Eras, each w/ many Periods.

Animal life rapidly evolved into a multitude of diverse forms, including dinos.

Includes Paleozoic Era (primitive invertebrates & forests w/ reptiles and whatnot), Mesozoic Era (‘Age of Dinos’) and Cenozoic Era (post-dinos to us, ‘age of mammals’).

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15
Q

Paleozoic Era

A

541 - 252 million years ago

primitive invertebrates in oceans, great forests w/ insects, amphibians and reptiles.

Includes Cambrian period, Ordovician Period, Silurian Period, Devonian Period, Carboniferous Period & Permian Period.

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16
Q

Cambrian Period

A

541 - 485 million years ago

Cambrian Explosion - Dramatic diversification of aquatic life @ beginning of Cambrian. Sponges, molluscs, worms, arthopods (trilos) evolved.

Pikaia - early relative of vertebrates. No vertebrae but many other features.

17
Q

Ordovician Period

A

485 - 443 million yrs ago

High sea levels

Oceans continued to diversify, fish increasingly becoming dominant large aquatic animals.

18
Q

Silurian Period

A

443 - 419 million years ago

Fish evolve jaws & large predatory fish evolve.

Primitive plant life began to flourish on land.

19
Q

Devonian Period

A

419 - 359 million years ago

First forests on land

Huge jawed fishes like Dunkleosteus (second strongest bite ever, behind T.Rex) & first true sharks.

Lobe finned ‘fishapods’ like Tiktalik ventured onto land & gave rise to tetrapods.

20
Q

Carboniferous Period

A

359 - 299 million yrs ago

Amphibians abundant in swamps

Reptiles (first amniotes!) evolved

Todays coal is from Carboniferous rotting swamps

21
Q

Permian Period

A

299 - 252 million yrs ago

Continents collide & form PANGAEA

Reptiles evolve 3 main lineages: Anapsids (turtles), Synapsids (mammals), & Diapsids (crocs, lizards, snakes & DINOS).

Rocks from this Period are arid, dry desert environments.

End Permian Extinction Event - single greatest mass extinction in history. All trilos dead :(

22
Q

Mesozoic Era

A

252 - 66 million years ago

Age of Dinos - dinos evolve & become dominant form of terrestrial life.

Marine reptiles, like Ichtyosaurs, Plesiosaurs & Mosasaurs evolve.

First true crocs, turtles, lizards, snakes, mammals & birds evolve.

First flowering plants evolve by end Mesozoic.

Includes Triassic, Jurassic & Cretaceous Periods.

23
Q

Cenozoic Era

A

66 - 0 million years ago

Age of mammals - extinction of dinos allowed mammals to evolve larger forms & fill those ecological roles.

Grasses abundant.

Includes Palogene period, Neogene period, Quaternary period.

24
Q

Palogene Period

A

66 - 23 mil yrs ago

global temps began to cool

mammals diversify (primates, bats, whales, etc.)

Birds Diversify.

25
Neogene Period
23 - 2.6 million years ago Global temps continue to cool First hominids evolve in Africa.
26
Quaternary Period
2.6 - 0 million years ago Earth experiences many 'ice ages' Humans evolve & civilization spreads
27
How long did non-avian dinos exist?
For 135 million years. Less time separating first humans to last dinos than the last dinos to the first dinos.
28
Triassic Period
252 - 201 million years ago Pangaea beings to break apart. First ornithiscians (Psianosaurus), Theropods (Eoraptor & Herrerasaurus), & sauropodomorphs (Panphagia) were all SMALL & BIPEDAL. Prosauropods (i.e. Plateosaurus) were first large herbivorous dinos. First Ichthyosaurs ('fish lizard' but not lizards nor fish). Reptiles whose ancestors were fully terrestrial & they found success by making evolutionary return to water. Evolved paddle-like front & hindlimbs, finned tail & shark-like dorsal fin. Long snouts w/ conical teeth - psicivores. Never evolved gills. Plesiosaurs - Large chests & torsos, broad paddle-shaped limbs & relatively short tails. Above shoulders varied tremendously. Pterosaurs - close relatives of dinosaurs, branched off of reptiles @ roughly same time as dinos. First vertebrates to fly. Have membranous wings supported by single extremely elongated finger. Early ones belonged to rhamporhynchoids.
29
Jurassic Period
201 - 145 million yrs ago Dinos diversified, peak sauropod diversity. small & medium ornithopods were common non-coelurosaurian theropods like Allosaurus were dominant terrestrial carnivores. Stegosaurs almost completely restricted to jurassic. first ankylosaurs, ornithopods & ceratopsians appear and first birds evolve (Archaeopteryx). Morrision Formation USA & Solnhofen Germany best fossil records of Jurassic. Pterodactyloids evolve from Rhamphorahynchoid pterosaurs. Have shorter tails & elongated carpals in their wrists (longer wings). Large head crests (display structures). Could be small (robin size) or over 10m wingspans (largest ever flying creatures).
30
Early Cretaceous
146 - 100 million years ago. First flowering plants New theropods (i.e. Spinosaurids & Carcharodontsaurids) evolve & coelurosaurian theropods become more diverse. Iguanodonts become larger & more abundant. Yixian Formation China, Wealden Supergroup England & Cedar Mountain Formation Utah were important early creataceous fossil units. Mosasaurs - Relatives of modern lizards and snakes. Tail fins & limbs modified into paddles, bodies & tails elongate. Some over 18m long. Seem adapted to deep-sea & big-game hunting.
31
Late Cretaceous
100 - 65 million years ago Apex of non-Avian dino diversity (most famous dinos from here). Coelurosaurians theropods (tyrannosaurids, ornithomimids, therizinosaurs, oviraptorosaurs, dromaeosaurs, troodontids) diverse in NORTHERN hemisphere. Snkylosaurs diverge into ankylosaurids (tail-clubbed) & nodosaurids (non-tail clubbed). Ceratopsians & Hadrosaurs are dominant large herbivores in norther hemisphere. Only single sauropod lineage remaining are titanosaurids, dominant herbivores in southern hemisphere. Pachycephalosaurs ONLY known from late cretaceous. End cretaceous - big meteor collides w/ earth leading to extinction of all non-avian Dinos.