lecture 8 Flashcards Preview

U0 Anthropology 203 > lecture 8 > Flashcards

Flashcards in lecture 8 Deck (75)
Loading flashcards...
1
Q

There are three general phases to paleoanthropological research:

A

discovery
description
classification

2
Q

what is discovery

A

of a fossil specimen via a predictive model, and the conservation of the find

3
Q

what is description

A

that permits comparison with other fossil discoveries

4
Q

what is classification

A

and the establishing of evolutionary relationships with previously-‐ discovered fossils

5
Q

what is Fossilization

A

is the environmental or chemical alteration of the physical structure of an organism’s remains, which generally keep their original form.

6
Q

is fossilization common

A

It is a very rare process, and is almost always limited to hard, durable parts of the body: bone, shell, teeth, etc.

7
Q

what is the best preserved, typically

A

teeth are always the best preserved because of the enamel, and you can get so much DNA from it

8
Q

Two general conditions must be met for fossilization to occur:

A

rapid burial

limited exposure

9
Q

what is rapid burial

A

of the specimen and steady accumulation of soil over time (no erosion).

10
Q

what is limited exposure

A

to oxygen, heat or animal scavenging/burrowing

11
Q

The study of natural processes that lead to fossilization is called what

A

taphonomy

12
Q

true or false

The same taphonomic forces that favor fossilization generally hinder discovery of new fossils

A

true

13
Q

what is A predictive model

A

is used in the research design that will evaluate the likelihood of finding fossils in a given location

14
Q

Most primate fossils have been discovered in one of three general location types:

A

volcanic deposits and rift valleys
river or lake deposits
(as they expand and contract, there is constant movement of soil)
sheltered cave systems

15
Q

After discovery, the specimen must be described and classified as one of 2 things;

A

A member of a previously identified species
or
Representative of previously unknown species or genus

16
Q

In making these determinations, the researcher must take into account:

A

1) the physical (morphological) variation of individuals within a species
2) pathological anomalies (diseases)

17
Q

There are two general ways in which fossil specimens can be classified:

A

Phenetic classification

Phylogenetic (or cladistic) classification

18
Q

what is Phenetic classification,

A

which is based solely on the similarities of physical traits, such as size, color, general morphology

19
Q

what is Phylogenetic (or cladistic) classification,

A

which organizes organisms according to their evolutionary descent

20
Q

Phenetic Classifications…

…can be mislead by:

A

Convergent (parallel) evolution

21
Q

what is Convergent (parallel) evolution

A

the evolution of traits that are similar in function, but evolved from different structures (aka analogous traits)

22
Q

what are analogous traits.

A

Similar structure between the wings of bats and birds, but different evolutionary trajectories

23
Q

Cladistic Classifications…

… try to express evolutionary relationships between species based on what

A

homologous traits, traits are similar because of ancestry.

24
Q

what is a clade

A

Clade = a group of species that share a set of derived homologous characteristics

25
Q

Homologous Characters (Traits) can be what

A

Can either be primitive (ancestral) or derived

26
Q

what is an ancestral trait

A

The presence of 5 fingers and toes in primates is an ancestral trait.
ancestral is shared

27
Q

what is a derived trait

A

The alignment / structure of the human big toe is a derived trait
derived is different

28
Q

There are two general means of estimating the age of archaeological and paleontological specimens:

A

Absolute vs. Relative Dating

29
Q

what is Relative dating,

A

which tells us the order in which events occurred, but little else

30
Q

what is Absolute dating

A

provides an age estimate in calendar years

31
Q

what does Stratigraphy do

A

Form the basis for relative dating

32
Q

what are the principles of Stratigraphy

A

the Principle of Original Horizontality,

33
Q

what is Principle of Original Horizontality

A

which holds that strata were originally laid down horizontally, and any alterations are the result of later processes

34
Q

what is 2) the Principle of Superposition,

A

which holds that older deposits among strata are lower than younger deposits

35
Q

what is 3) The Principle of Cross-Cutting Relationships

A

states that a geological feature must exist prior to a feature cutting across or into it.

36
Q

what is 4) The Principle of Faunal Succession

A

states that fauna appear in predictable sequences in strata. Relies on the concept of an index fossil

37
Q

Relative dating techniques are derived from the geological principle of what

A

uniformitarianism and the principles of stratigraphy

38
Q

Relative dating techniques are derived from the geological principle of uniformitarianism and the principles of stratigraphy, and form two postulates:

A

1) the Principle of Superposition

2) “comparison by fossil,”

39
Q

what is “comparison by fossil,”

A

which assumes two widely-‐separated strata with similar minerals, fossils or artifacts are contemporaneous (biostratigraphy)

40
Q

chichis more reliable, absolute to relative dating and why

A

Absolute dating is much more reliable than relative dating, as it provides chronological age estimates, always with an error range.

41
Q

All but a few of the most commonly used absolute dating techniques are what

A

radiometric

42
Q

what is radiometric

A

that is, they rely on radioactive phenomena, specifically, the measurement of radioactive decay.
isotopes can be radioactive (decay) and others can be stable… this helps us determine the time of the fossil

43
Q

what are the types of absolute dating

A
Carbon-14 (Radiocarbon) Dating
Potassium-Argon (K-Ar) Dating
Argon-Argon (Ar-Ar) Dating
Thermoluminescence
Electron Spin Resonance (ESR)
Amino Acid Racemization
44
Q

what is Carbon—14 testing

A

measures the decay of 14C, which is an unstable radioactive isotope of carbon–the key element in all living things

Carbon-14 testing is based on the premise that 14C breaks down at a consistent rate; every 5,730 years, its concentration within a sample is halved; this is referred to as its half-life.
When an organism dies, it has equal parts carbon-14, which decays, and carbon-12, which does not. By measuring the ratio of 14C to 12C, we can see how much time has passed since an organism died

45
Q

what is a limitation of Carbon—14 testing

A

It can only be used to date carbon— containing organic materials (e.g., bone, wood and other vegetation, etc.).
only done on things made up of carbon

46
Q

what range does Carbon–14 testing cover

A

Its effective range of dating is between 300 years BP and 50,000 years BP

47
Q

what is BP

A

(BP— before present… 1950 is the arbitrarily set “present”)

48
Q

what is Potassium-Argon (K-Ar) Dating

A

Radioactive Potassium-40 breaks down into Argon-40 gas very slowly. The transformation half-life is 1.3 billion years! We measure the ratio of Argon- ‐40 to nonradioactive Potassium-39, which doesn’t transform or break down; the differences represent the age of the sample.

49
Q

what is K-‐Ar dating is used for

A

to date potassium-rich volcanic rock and ash

50
Q

what is the date race for K-‐Ar dating

A

Because of Potassium-40’s long half-life, the upper age limit of K-Ar dating is effectively unlimited; the lower limit, however, is around 500,000 years BP

51
Q

what is Argon-Argon (Ar-Ar) Dating

A

Argon-Argon dating is similar in principle (and date limits) to K-Ar dating, only instead of measuring the amount of Potassium-39 (which is found in minerals as a solid), then measuring the amount of Argon-40 (which is found in minerals as a gas) and comparing the ratio, it first converts non-radioactive Potassium-39 into radioactive Argon-39 and then compares the ratio of Argon-40 to Argon-39.

52
Q

is Argon-Argon (Ar-Ar) Dating very reliable

A

This technique is considered more reliable than K-Ar dating, as it requires only one sample for testing, and is testing only one variety of element (Argon).

53
Q

what is a limitation for Argon-Argon (Ar-Ar) Dating

A

where as in K-Ar there are two samples needed from the same thing and error can occur when taking one+ sample

54
Q

what is Thermoluminescence

A

measures the light emitted by electrons trapped in the lattice structure of some crystalline minerals

55
Q

how does Thermoluminescence work

A

Electrons become trapped in the crystal structure due to background radiation; the accumulation of electrons occurs at a fairly steady rate.
The electrons are freed by heat; each time a sample is heated, the “electron clock” is reset to zero

can measure the last time it was heated and that exposure to heat is the point in tie we want to know about … it releases e- when heated then absorbs more e- from the atmosphere effectively “resetting” the e- clock

56
Q

what is Thermoluminescence used for

A

this is used especially with pottery

57
Q

what is Electron Spin Resonance (ESR)

A

ESR operates on the same principle as thermoluminescence, only instead of releasing the trapped electrons, the magnetic field of the sample is measured to determine how many electron “traps” exist in the lattice

58
Q

what is the date range for Electron Spin Resonance (ESR)

A

The effective dating range is anywhere from 3,000 years to 300,000 years.

59
Q

what can Electron Spin Resonance (ESR) be used on

A

It can be used on cave deposits, fossil shells, corals and tooth enamel

60
Q

what is Amino Acid Racemization

A

Amino acid racemization measures the transformation of amino acids from one form (L) (when they are alive) to another form (D) after death of the organism. This transformation process is called racemization.

61
Q

what can Amino Acid Racemization be used for

A

The ratio of D to L amino acids increases over time, and can be measured to provide a date of death

62
Q

what is included in Earliest Primates

A

Earliest prosimians (the Strepsirrhines and tarsiers)
Earliest Haplorrhine monkeys (both Old World and New)
Earliest Haplorrhine apes (aka, hominoids)

63
Q

One thing we must remember is that our fossil knowledge of early primates is very limited, in part because:

A

arboreal 1. fossilization is an incredibly rare process
so we can never say that we are looking at the very first of a species… that is not known, but they

  1. our ability to effectively survey and excavate these fossils is limited
64
Q

The earliest primates and proto-‐ primates were entirely______

A

arboreal

65
Q

what is angiosperm

A

flowering

66
Q

when did angiosperm appear

A

The appearance of angiosperm (flowering) vegetation between 100 and 50 mya

67
Q

what did the appearance of angiosperm result in

A

The appearance of angiosperm (flowering) vegetation between 100 and 50 mya created micro-‐ ecological niche that could support these early tree-‐ dwellers

68
Q

what is K-T Exctinction

A

The Cretaceous-Tertiary (K-T) mass extinction event resulted in the extinction of three-‐quarters of the world’s reptiles, mammals and birds

69
Q

when did K-T Exctinction happen

A

approximately 65 mya

70
Q

-‐T is believed to have been caused by what

A

K-‐T is believed to have been caused by the impact and resulting fallout from a large (~6 mi- diameter) iridium- ‐rich asteroid or comet

71
Q

what played a role in surviving the K-T Exctinction

A

Diet played the largest role in survivorship; omnivores and insectivores were more likely than others to survive the event

72
Q

how are Physical geography and paleoclimates are very closely related

A

interior areas experience the harshest weather.

73
Q

what did The gradual breakup of the continents do

A

The gradual breakup of the continents exposed more land to weather-mediating bodies of water, opening up new territory to mammals worldwide

74
Q

when did The gradual breakup of the continents happen

A

65 mya, the planet was much warmer and wetter than it is today

75
Q

do Slight changes in climate can have major impacts on the evolutionary development of certain species

A

yep