Lesson 9) Statigraphy and Geologic Time Flashcards

Statisgraphic concepts and the scale of Earth History

1
Q

Principle of Superposition

A

Tendency or rock layers to be chronologically stacked.
- Sediments deposited -> gradual build up
- How things normally work, but can be exceptions:.

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2
Q

Unconformity

A

Flat surface caused by partially melted igneous intrusions that are uplifted and eroded

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3
Q

Statigraphy

A

Science of using arrangement and composition of rock layers to interpret geological history

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4
Q

Formation

A

Large uninterrupted sequence of rock that is made of multiple layers that all share similar properties (eg- composition + grain size) all formed under similar conditions

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5
Q

What is indicated when a rock changes formations?

A

Large scale change occurred in the environment where the rocks were deposited.

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6
Q

Principle of Superposition

A

Allows stratigraphies to infer relative age of rock layers (layer age vs other layer age)
- DOES NOT determine absolute age

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7
Q

Radiometric dating

A

Technique to determine rocks age.

As rock ages, isotopes decay and ratio of isotopes : decay product decreases.
Mass spectrometers can measure the isotope ratio of rock, which can tell how old it is.

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8
Q

Isotope

A

Variant of a chemicalelement that has unusual number of neutrons.
- some are unstable and undergo radioactive decay: energy release, resulting in atoms w/ different compositions (decay products)

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9
Q

What rock can’t be radiometrically dated?

A

Sedimentary
They are not new: they are made of sediments that have already formed and are undergoing radioactive decay already probably.

However: can use volvanic ash layers (within sedimentaries to estimate nearby fossil ages)

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10
Q

What can usually be radiometrically dated?

A

Igneous
Formed anew
- When igneous rock solidifies, it starts out w/ isotope ratio equal to that found in its environment

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11
Q

How can we measure fossils age, if they’re usually found in sedimentary rocks?

A

Radiometric dating + principle of superstition

IF found between two horizontally deposited igneous rock layers— can bracket age

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12
Q

Geologic Time Scale

A

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

Eons > Eras > Periods > Epochs

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13
Q

Hadean eon

A

4.4-4 billions yrs ago

Formation and earl Earth years.
- Surface partially molten and hella volcanoes
- Planet collision which formed moon

By then end, Earth had cooled and hella oceans
- organic molecules form

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14
Q

Archean Eon

A

2-2.5 billion yrs ago

  • Oldest fossils (single-celled organisms)
  • Cynanobacteria made oxygen and stromatolites
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15
Q

Stromatolites

A

Structures formed by cyanobacteria from the Archean Eon
- Lump stones that when cut in half, show layers of secreted sticky limbs trapping sediment particles.

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16
Q

Proterozoic Eon

A

2.5 billion-541 million years ago

  • FIrst multicellular organisms
  • very poor fossil record as life at this point was BONELESS
    Ediacarian period: Large forms of life (like animals) finally got here bruh
17
Q

Phanerozoic Eon

A

540-0 millions years ago

Subdivided into 3 eras
- Rapid animal evolution

18
Q

Paleozoic Era

A

541-252mil years ago

  • Primitive ocean-dwelling invertebrates (me fr)
  • Big ass forests w/ reptiles, amphibians, insects
19
Q

Cambrian Period

A

541-485 mil years ago

  • Aquatic life diversification (Cambrian explosion)
  • Anomacolaris, arthropods, SpongeBob worms etc
20
Q

Ordovician Period

A

485-443 mil years ago
- OCEAN ANIMALS RULE!!!!

21
Q

Silurian Period

A

443-419mil years ago
- predator fish get jaws #looksmaxing
- land plants start flourishing
- millipede anthropods start crawling on ocean floor

22
Q

Devonian Period

A

419-359 mil years ago
- FIrst forests EVOR!!!
- sharks
- the fishies start venturing onto land

23
Q

Carboniferous Period

A

359-299 mil years ago
- ambhipians swamps and reptiles

24
Q

Permian Period

A

299-252 mil years ago

  • PANGAEA FORMS!!!
  • Reptiles evolve into 3 linages which make up every major animal
25
Q

Mesozoic Era

A

252 - 66 mil years ago
“Age of Dinosaurs”

  • Marine reptiles evolve (first true reptiles, mammals, birds)
  • First flowering plants
26
Q

Cenozoic Era and its 3 periods

A

66-0 mil years ago
“Age of Mammals”
- Grass reveal

Periodt!!!
1. Paleocene: 66-23 mil
- Cooling temperatures, mammals + birds diversifying

2. Neogene: 23-2.6mil
- HOMINIDS IN AFRICA

3. Quaternary: 2.6-0 mil
- Ice age
- First anatomically modern humans and civilization

27
Q

Triassic Period

A

252-201 mil years ago
- Life slowly recovers from mass extinction of Permian era
- first mammals and Dino’s evolve
- Pangaea breaks apart
- Ichthyosaurs + Plesiosaurs = Pterosaurs

28
Q

Dinosaurs of the Triassic Period?

A

First Ornithischians:
- Pisanosaurus

First Theropods:
- Herrerasaurus
- Eoraptor

First sauropodomporphs:
- Panphagia

Prosaurupods:
- Plateosaurus

29
Q

Ichthyosaurs

A

“Fish Lizard” but aren’t lizards (nor fish)

Group of reptiles that took on a fish-like lifestyle and evolved a very fish body form (and returning to sea)
- Ancestors: Terrestrial reptiles
- Paddle-like front + hind limbs, fin tail, dorsal fin
- Long snout w/ conical teeth (piscovore)
- BUT: never evolved gills so they still needed to breath air

30
Q

Plesiosaurs

A

Group of reptiles that a loved secondarily aquatic lifestyle
- Large chests + torsos
- Broad, paddle iambs
- Short tails
- Vary in front

eg) elasmosaurus (keep in mind it lived in Cretaceous period)

31
Q

Pterosaurs

A

Close relatives of dinosaurs who branched off reptilian family tree at roughly the same time dinosaurs did
- FIRST FLYERS
- Membranous wings supported by elongated

32
Q

Jurassic Period

A

201-145mil years ago

Dino diversification
- Sauropods were dominant terrestrial herbivores
- small ornithopods
- theropods were dominant terrestrial carnivores
- rhamphorhynchoids and pterodactyloids
- first birds
- first ankylosaurs and ceratopsians (but not diverse yet)

33
Q

Rhamphorhynchoids

A

Early pterosaurs

eg) stegosaurus

34
Q

Pterodactyloids

A

Came from ramphorhynchoids, differing in morphology
- short tails
- elongated carpels which made wings longer
- large head crests as display
- ranged in size

eg) pteranodon

35
Q

Early Cretaceous Period

A

146-100 mil years ago

  • first flowers
  • spinosaurids and charcharodontosaurids
  • coelurosaurian theropods diversify
  • iguanodonts get big and many – sauropods decline
  • Mosasaurs
  • stegosaurs get replaced by ankylosaurs
  • primitive birds abundant (better than archaeopteryx)
36
Q

Mosasaurs

A

Relatives of modern monitor lizards and snakes
- reptiles
- tail finds and paddle limbs
- BUT bodies were longer than ichthyosaurs and plesiosaurs
- most were predatory and big

37
Q

Late Cretaceous Period

A

100-65 mil years ago
- all the famous celebrity Dino’s
- coelurosaurian theropods abundant and diverse
- ankylosaurs diverge into two: ankylosaurids and clubless nodosaurids
- Ceratopsians and hadrosaurs are dominant herbivores (northern)
- titanosaurid sauropods are dominant herbivores (southern)
- pachycephalosaurs!!!
- flower plants evolve <3
- THEN THEY ALL DIE!!!! MASS EXTINCTION!!!!!

38
Q

What were some coelurosaurian theropods that lived

A

Tyrannosaurs, oviraptorosaurs, dromaeosaurids, oviraptosaurs, therizinosaurs, troodontids

39
Q

How long ago was the Earth formed?

A

4.6 billion years ago