Week 1: Introduction Flashcards

1
Q

Palaeoanthropoly

What sources do we have

A
  • the morphology of present day primates
  • the behaviour of present day primates
  • chemical and physical data
  • tools and cultural objects
  • contextual information
  • fossil hominins
  • other fossils
  • DNA (ancient and recent)
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2
Q

How do we find hominin fossils

A
  • excavation (retrieving fossils and artifacts)
  • survey (scouting for fossils on the surface)
  • the great rift valley
  • volcanoes
  • rock-hewn churches of lalibela
  • fiels work
  • afar triangle today
  • “the crawl”
  • sieving
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3
Q

environment and biochronology

what can fossil fauna tell us?

A
  • bovids and small mammals are in dense forests, woodland, and grassland
  • proboscidea and suids evolve fast
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4
Q

What are bovids

A
  • bovid family comprise of biological family of cloven-hoofed, ruminant mammals that includes cattle, bison, buffalo, antelopes, sheep and goats
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5
Q

what are proboscidea

A
  • a taxonomic order of afrotherian mammals containing one living family and several extinct families
  • encompasses the elephants and their close relatives
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6
Q

what are suids

A
  • refers to a member of the suidae family
  • includes pigs and wild boars
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7
Q

dating and time scales of fossils

A
  • geological time scales (what happened when?)
  • shows ice ages
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8
Q

OIS

Oxygen Isotopic Stages

A
  • the proportion of O16 and O18 in the seawater is proportional to the ice free ocean surface area, as the lighter O16 evaporated preferentially
  • by using ice cores from deep drillings in the Arctic/Antarctic you can create curves of proportions of these isotopes where δ18O approximates global temperatures ( δ18O is the difference of O18 concentration from a standard )
  • phases are numbered consecutively backward with the Holocene being OIS 1, cold periods have even numbers while warm phases have odd numbers
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9
Q

What dating methods are used

A
  • relative dating
  • absolute dating
  • direct dating
  • indirect dating
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10
Q

what is relative dating

A

estimated age relative to other finds or sites

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11
Q

what is absolute dating

numerical/chronometric

A

the exact age in years based on physical/chemical properties, there are numerous assumptions subject to statistical variation and independent of other sites or finds

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12
Q

what is direct dating

A

techniques that directly measure the age of artifacts, fossils, or other objects, rather than relying on the age of surrounding materials

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13
Q

what is indirect dating

A

determining the age of an artifact or feature by relating it to another object or matrix of known age, rather than directly dating the item itself

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14
Q

tephrostratigraphy

A

the study and dating of pyroclastic layers of volcanic ash

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15
Q

biostratigraphy

A
  • a branch of stratigraphy that uses fossils to establish the relative ages of rocks and correlate different rock layers
  • it is geographically widespread
  • rapid morphological changes
  • directional evolutionary trends
  • first appearance and extinction at the same time everywhere
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16
Q

what are important taxa

A
  • rodents
  • suids
  • elephants
  • equids
17
Q

paleomagnetism

A

the study of earth’s ancient magnetic fields as recorded in rocks and sediments

18
Q

paleomagnetism

geometric polarity time scale

A
  • a chronological framework that records the history of Earth’s magnetic field polarity reversals
  • chrons can be normal (today) or reversed
  • subchrons are short
  • it is especially important for human evolution
19
Q

absolute dating

general features of isotopic dating

A
  • radioactive delay is constant
  • they are independent of temperature, moisture, pH
  • half life of radioactive material allows age determination
20
Q

radiocarbon dating

carbon-14 dating

A
  • a method for determining the age of organic materials up to about 50,000 years old
  • works by measuring amount of carbon-14 remaining in a sample which decays at a known rate
  • C14-C12 ratio is variable
  • C14 is not likely to enter biosphere
  • C14 is not from the atmosphere
21
Q

radiocarbon dating

postdepositional process

A

natural and anthropogenic activities that occur after sediments or artifacts are laid down, altering their original state and potentially impacting their preservation and interpretation
* erosion
* flooding
* animal activity
* human disterbances

22
Q

radiocarbon dating

contamination

A
  • a significant issue
  • even small amounts of extraneous carbon can skew the results, leading to inaccurate age estimates
  • can be natural; soild or plant roots
  • or artificial; conservation chemicals or modern carbon
23
Q

carbon dating methods

A
  • conventional radiocarbon dating
  • AMS dating
24
Q

radiocarbon dating methods

conventional radiocarbon dating

A
  • counting of beta radiation through liquid scintillation detectors
  • it is cheap, inaccurate, and needs a large sample size
  • up to 30-40 ka
25
# radiocarbon dating methods AMS dating
* direct counting of C14 atoms through accelerator mass spectrometry * expensive, accurate, faster, needs smaller sample size * theoretically up to 100 ka, in practice 40-50 ka
26
potassium-argon and argon-argon dating
* radiometric techniques used to determine the age of rocks and minerals * K-Ar dating reliees on measuring the decay product of potassium-40 to argon-40; can be challenging to obtain accurate ages that have undergone significant heating/contaminated with excess argon * Ar-Ar is a derivative of K-Ar dating that involves irradiating a sample to convert potassium to argon allowing for easier and more procise age calculations
27
# dating examples Ust'-Ishim 1 | a hominin femur
* term given to the 45,000-year-old remains of one of the early modern humans to inhabit western siberia * had intact DNA which permitted complete sequencing of its genome
28
# dating examples Willendorf 2
* an upper palaeolithic site in central europe * numerous cultural horizons interspersed with loeess deposits. abundant charcoal in the cultural horizons/paleosols * earliest known sites in Europe
29
micromorphology
* the study of fine-scale structures and details, particularly in soils, sediments, and other materials * examining thin sections under a microscope to analyze the arrangement and composition of components at a microscopic level
30
# carbon dating examples Galili | a plio-pleistocene site in ethiopia
* about 150m thick succession of fluviatile and lacustrine deposits, interspersed with volcanic horizons * numerous localities with rich fossil assemblages