Lecture 6/7 Flashcards
provenance
the original location of a fossil artifact - must be done before identifying time frame
Relative dating
method of dating that identifies fossils as being young/older of other known artifacts or objects
- doesn’t assign exact age
Stratigraphy (Strata)
method of relative dating
- study of different layers (strata) that have been deposited over time
- works well with sites that haven’t been disturbed
law of superposition: within undisturbed geological deposits, strata are laid down from oldest to most recent
- this is reversed in sites of erosion, materials that are found in the water are on top, but they are oldest
- fossils buried lower in the strata are older than those buried closer to surface
- alterations from geological process such as folding and uplifting disturb a site
Biostratigraphic dating (faunal correlation)
faunal: Animals, especially the animals of a particular region or period, considered as a group
- dating a fossil based on association of faunal remains that have been securely dated using other methods
- primate fossil found with remains of extinct species of pig known to have lived 35-40mya -> association = fall into the same range of time
Flourine dating
relative dates based on amount of fluorine in bones
- bones and teeth absorb fluorine when animals dies from surrounding ground water.
- more amount of fluorine present = older specimen
Absolute dating methods (Chronometric)
assigns a specific age and estimated error to a fossil or site
associated with dating error +/- differing from the actual day
Radioactive isotopes
unstable isotopes that decay, emitting radioactivity
decay at a constant rate into more stable forms
Radiometric dating
absolute dating method using radioactive decay of the isoptoe c14 into N14
- all living organism posses C14 from the environment
- when they doe it stops taking in C14 and turn it into 14N
- c14 has a half life of 5730 years +/- 40 years
- use to date organic materials: wood, bone, charcoal
- only usually for dating past 40,000 to 45,000 years ago
Potassium-Argon dating
absolute dating to measure decay of K40 into argon gas Ar40
K40 has a half like of 1.3 billion years
- used for dating volcanic material - and not dating fossils you are dating time of events
Atomic mass spectrometry
method of radiocarbon dating used to date very small samples
Geological Times scale
evidence of climate change, precise radiometric dating
- division of the earls geological events into time periods such as eras and epochs. Based on temporal divisions defined by features of fossilized remained of extinct organisms
Epoch
measure of geological time that partitions geological eras into smaller units, defined with regard to major climatological/environmental events
Cenozoic era
included mammals and emergence of primates
Oxygen isotope analysis
stable oxygen isotopes to reconstruct ancient climates using ice cores taken from polar icecaps and sediment cores taken from ocean floor
looking at ratio of O18 and O16
O18 is heavy so when water evaporates it gets left behind and makes sea water a high ratio
glacial period have O16 locked in, a low ratio = cold periods
ice cores with high ratio were warmer periods
Crown group
last common ancestor of a clade plus all of its descendants including living members of the clade
stem group
extinct organisms that are not part of the crown group
Paleocene
Plasidapiforms and flowering plants!
After extinction of the dinosaurs and less proliferation of gymnosperms
first epoch of the cenozoic era
warmer climate which allowed for angiosperms to proliferate
primate like mammals with a low dental formula of 3.1.4.3, large procumbent (forward-facing) incisors, long snout, laterally facing orbits, claws, no post-orbital bar
- diet of insects and fruits
Eocene
Strepsirhines and start of haplorhines
First euprimates - lemurs and lorsises
- very warm climate, tropical all over NA, africa, europe and asia
- foreword facing eyes, post-orbital bar, reduced snout
Omomyidae: tarsier like primates
- small, large eye orbits to be nocturnal, lack of tapetum, elongated calcaneus to leap branch to branch
- teilhardina asiatica found in china
Adapids
- lemur like primates
- larger than omomyids, larger snout, smaller eyes, teeth suggest leaves and fruit diet
Darwinius masillae
- small, arboreal quadruped that is debated to be either a strepsirhines or a haplorhine
Eosimias
- found in china
- looks alot like darwinius masillae
- tree-dwelling primate
- displays tarsier (omomyid) like features like the ankle bone
Tapetum:
reflective layer behind the retina that increases the light capturing capacity of the eye
- omomyids do not have this, the large eye orbit allows for the extra light to allow them to still be nocturnal
Oligocene
Anthropoids: Oligopithecidae, Parapithecids, Proliopithecis
Temperature dropped significantly - reduction in forest, extinction of many land mammals in europe
- Fossils all found in the Fayum depression in Egypt (very small area of land)
- includes haplorhines and strepsirhines
Oligiopithecidae
2.1.2.3
ancestor to catarrhines - Old world monkeys
Paralithecidae
2.1.3.3.
ancestor to platyrrhines - new world monkeys
low rounded cusps - fruit eating
small eye socket - diurnal
post cranial skeleton gives quadrupedal mode
Proliopithecidae
2.1.2.3
ancestor to catarrhines - old work monkeys
dimoprhic canines which shows variety in mating system
type: aegyptopithecus: very large 6-8kg
y-5 patterns on lower molars
sagital crest which shows lots of chewing - leaves in diety
large brain
New world monkeys
2.1.3.3.
Platyrrhines
Found in South America
Hypothesis: NWM arose from African anthropoid and spread to south america by rafting across southern atlantic on floating masses of vegetation
Oligocene had low levels of sea water so there were islands to make this possible
Morphological similarities between african and south american anthropoids to support hypothesis