5a - Primate Evolution Flashcards

(29 cards)

1
Q

How are fossils formed

A
  • When animals, plants, and other organisms die, they typically decay completely. But sometimes when the conditions are just right, they’re preserved as fossilsW
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2
Q

What are fossils

A

Fossils are any remains of life preserved in rocks
- Bones, Teeth, Impressions, Footprints, Natural molds, termite nests, worm burrows, et

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3
Q

Are fossils common

A
  • Fossils are very rare: of all the life that has ever lived, we only find a very tiny percentage of it in the fossil record
  • Due to their rarity, there are many gaps in our record of life in the past
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4
Q

What needs to happen for us to find a fossil

A

Right conditions for preservation: slow decomposition, limit the access of bacteria and fungi

Fight conditions to be found: exposed at the surface somehow

An organism might get buried very quickly, ex seabed or stuck in sap

A body can get buried in an environment inhospitable to bacteria/fungi. Ex tar pit

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5
Q

What are good fossil sites

A

Geological activity can expose buried fossils to the surface

Cave sites can accumulate high fossil concentrations

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6
Q

What are bad fossil sites

A

Moist, high rate of decomposition, many bacteria/fungi/insects, very difficult to excavate

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7
Q

What is Taphonomy

A

Goal: reconstruct the original community of plants and animals and its ecology

Taphonomy: the study of factors that affect organic remains prior to and during fossilization, and during excavation

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8
Q

What Taphonomic factors impact what we see

A

Many taphonomic factors can impact what we actually see

  • Predation, Accident, Disease, and Old age affect the transition from the Original Community of Plants and Animals to Organic remains
  • Scavenging, Water transport, Trampling, Time averaging, Burial, Dissolution, and Mineralization affect the transition from Organic remains to Fossils
  • Erosion, Collection and Preparation for study affect the transition from Fossils to Fossil Collections
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9
Q

How can we date fossils

A

Relative Dating involves comparison to layers above and below

Absolute Dating products a numerical date and margin of error

Relies on knowing exactly where a fossil came from in the soil

  • Its provenance
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10
Q

What are the laws of stratigraphy

A

Laws of Superposition: Oldest on the bottom, youngest on the top

Principle of Cross-cutting Relationships: cutting strata are younger

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11
Q

How can we absolutely date something

A

Determining a precise date for the age of an organic material by comparing the amount of naturally occurring radioactive isotopes of known decay rate

Radiocarbon dating:

Carbon exists naturally in two forms, C14 and C12

C14 decays at a known rate: half of it will be gone in 5730 years

Measure ratio of C14 and C12 in a fossil (less C14) compared to its normal ratio in the atmosphere = you can date how long ago it died by how much C14 has died by how much C14 has decayed

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12
Q

When do primate fossils first appear

A

Major events in primate evolution and climate change occurred in the Cenozoic Era (65 mya to present) → when mammals first evolved

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13
Q

Describe geologic time and how primates fit in

A

Divides earth’s history into time periods based on:

  • fossils
  • climatic changes

We can precisely date these time periods

Important Epochs for Primate Evolution:

Paleocene 66 mya

Eocene 56 mya

Oligocene 34 mya

Miocene 23-5 mya

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14
Q

What were primates like in the Paleocene

A

In the Paleocene (~66-56 mya):

  • Plesiadapiforms (rare) in Europe, Asia, and North America
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15
Q

What were primates like in the Eocene

A

In the Eocene (56-34 mya):

  • Omomyids appear in Europe, Asia, and North America
  • Adapids appear in America
  • Few fragments in Africa
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16
Q

What were primates like in the Oligocene

A

In the Oligocene (34-23 mya):

  • There are early Catarrhines from Fayum in Africa
  • Almost nothing in North America
  • Primates appear for the first time in South America
17
Q

What were primates like in Miocene

A

In the Miocene (23-5 mya):

  • Prosimians, colobines (9mya) and early apes (22 mya) in Africa
  • Colobines, early apes (16 my) in Europe and Asia
  • Fossils - Early Platyrrhines? in South America
18
Q

What were primates like in the Pliocene

A

In the Pliocene (5-1.8 mya):

  • Theropithecus and Early Hominins in Africa
  • Cercopiths and Colobines in Europe and Asia.
  • Platyrrhines in South America
19
Q

What were primates like in the Pleistocene

A

In the Pleistocene (1.8mya - 12 kya)

  • Baboons and homo appear in Africa
  • Carcopiths and Colobines disappear from Europe
  • Cercopiths and Colobines present in Asia
  • Platyrrhines in South America
20
Q

What were primates like in the holocene

A

Holocene (12 kya-Present)

  • Essentially modern fauna
21
Q

Describe the Paleocene Epoch

A

66-56
Europe and North America at the time = subtropical forests

Primates probably evolved from a small, insectivorous mammal

Earliest primate-like mammals in the Paleocene:

Plesiadapiforms

22
Q

describe Plesiadapiforms

A

Plesiadapiforms

  • some features similar to modern primates, some not seen in modern primates
  • Extinct by end of Paleocene
23
Q

Describe the Eocene

A

56-34
Global warming and spread of tropical forests to northern Africa

First true primates appear and spread → adaptive radiation

  • Adapidae: lemur-like
  • Omomyidae: tarsier-like

Primate traits similar to Strepsorrhines:

  • Forward Facing eyes
  • Postorbital bar
  • Reduced snout
  • Vertical clinging and leaping
  • Insectivorous and frugivorous diets
24
Q

Describe the oligocene

A

34-23
Climate is cooler, so the world is less forested

  • Most primates disappear from northern climates and appear in equatorial regions

Earliest unambiguous Catarrhine fossils come from this time

  • 32 mya in the Fayum Depression in Egypt

Sexual dimorphism

Ape like Y-5 molar pattern

Arboreal quadruped

Earliest fossil evidence of Platyrrhine monkeys appears as well

25
describe the Miocene
The Miocene (23-5) was a time of ape adaptive radiations Extraordinary number of species and diversity Miocene deposits of Africa and Eurasia = Planet of the Apes
26
Describe the early Miocene
Early Miocene 23-17 MYA Early Miocene in East Africa was forested - This is where we see the earliest probable ancestors of modern catarrhines: 23-17 mya - This is where we see the earliest evidence for ape like suspensory locomotion: 20 mya Early hominoids: 15 species of genus Pronconsul - Western Kenya - Ape like characteristics: no tail, large brain, Y5 molar pattern, fruit diet
27
Describe the Middle Miocene
Middle Miocene 17-12 MYA The climate started to cool, and sea levels drop - land bridge to Eurasia opens Hominoid fossils from Germany, Spain, etc Time of major ape migration and dispersal into Eurasia e.g. Dryopithecus 13 MYA, France, Spain, Austria, Georgia - Dentition and brain size like modern chimpanzee - Arboreal and used suspensory locomotion
28
Describe the Late Miocene
Late Miocene 12-5 MYA Climate has cooled and dried to the point that forests decline and open grasslands expand Hominoid fossils in Ethiopia, India, Pakistan, Vietnam, China, etc Apes start moving out of Europe into Asia, and back into Africa e.g. Sivapithecus 12-8 MYA, India, and Pakistan - Ancestor of modern orangutans - arboreal quadrupedalism and suspensory adaptations
29
do we know the direct ancestors of living apes
Today, Thousands of Miocene Ape Fossils, But only 5 genera of Living Apes - Direct Ancestor still unknown Human and chimp lineage split about 7 million years ago.