bio anth

Cards (63)

  • geological time scale
    -Paleozoic Era (ancient life-trilobites): 545-245 mya
    -Mesozoic Era (middle life-dinosaurs): 244-66 mya
    -Cenozoic Era (recent life): 65 mya - now
  • cezanoic era
    -7 epochs (at least)
    *Paleocene
    *Eocene
    *Oligocene
    *Miocene
    *Pilocene
    *Holocene
    *Pleistocene
    -Primate evolution began 66 mya during Paleocene
    -Human evolution began 7 mya during Miocene
    -We are currently in Holocene
  • when did human evolution start?
    late miocene
  • when did primate evolution start?
    paleocene; 66mya
  • what period are we currently in?
    holocene
  • fossils
    remnants of organic materials that have wholly or partially been transformed into rock
  • fossilization processes
    Oxygen free environment
    Rapidly covered (soil/rocks)
    Submerged in water
    Protected from scavengers
  • dating methods
    -relative dating
    -absolute dating
    -genetic dating
  • relative dating methods
    -Stratigraphy & Steno's Law of Superposition
    -Biostratigraphy
    -Flourine Dating
  • stratigraphy
    -the study of rock layers and the sequence of events they reflect
    -oldest layers on bottom
    -youngest layers on top
  • superposition
    -used to determine the relative age of rock strata, or layers
    -a principle that states that younger rocks lie above older rocks if the layers have not been disturbed
  • fluorine dating
    -a relative (chemical) dating method that compares the accumulation of fluorine in animal and human bones from the same site
    -recently deposited bones will have had little time to absorb fluorine
    -fossils that have been in the soil longer will have absorbed greater quantities of fluorine
    -the amount of fluorine in bones at the bottom will be much greater than the bones near the top
  • absolute dating techniques
    radiometric dating:
    -uses constant measurable change in an element as a clock
    half-life:
    -amount of time for one-half of an unstable (radioactive) isotope to decay into its stable counterpart
    genetic dating:
    -molecular clock: genetic mutations accumulate over time at more or less constant rate
    -date divergences of species
  • biological species concept
    a group of actually or potentially interbreeding individuals that are reproductively isolated from other such groups
  • speciation
    -the transition from an ancestral species to a descendant species
    -evolutionary process in which populations evolve into their own distinct species
    -requires:
    *variation in environment (food, climate, predators)
    *natural selection producing differing phenotypes
    *reproductive isolation
  • disruptive selection
    -form of natural selection in which a single curve splits into two
    -occurs when individuals at the upper and lower ends of a distribution curve have higher fitness than individuals near the middle
  • reproductive isolation
    separation of a species or population so that they no longer interbreed and evolve into two separate species
  • phyletic gradualism
    -small changes accumulate over millions of years to produce new species
    -A->B->C linear
  • cladogenesis
    -branching evolution
    -A->B, A->C (V shaped)
  • adaptive radiation
    -species into many niches
    -example: Darwin's finches
  • punctuated equilibrium
    rapid speciation events followed by long periods of stasis
  • hallmarks of bipedalism
    Human-Ape (Chimpanzee) Comparison
    -Skull
    -Pelvis
    -Knee
    -Foot
    - Teeth
  • skull
    Humans: smaller
    Apes: larger, longer
  • foramen magnum
    Humans: on the bottom of the cranium
    Apes: toward the back of the cranium
  • palate shape
    Human: U-shaped; arched
    Apes: rectangle shaped; parallel posterior tooth rows
  • pelvic shape
    Human: bowl-shaped, shorter, broader
    Apes: longer, thinner, narrow
  • femur & knee
    Human: femur angles in toward the midline of the body and centers the knees under the body; valgus (medial) angle
    Apes: straight femurs and knees positioned more toward the lateral sides of their bodies; straight
  • valgus angle
    increased angle of femur allows legs to be under body and allow more efficient walking and running
  • foot
    Human: short, straight toes and nondivergent hallux (big toe); longitudal arches
    Apes: long, curved toes and a divergent hallux that is used for grasping; flat feet - no longitudal arch
  • non-divergent 1st digit
    in line (parallel) with other toes
  • longitudal arch
    -extends down the length of the foot from the base of the toes to the heel
    -helps with shock absorption as we walk
    -helps to direct our body weight and energy to create a smooth push-off while stepping forward
  • teeth
    Humans: do not have a C-P3 complex; small, non-projecting canine' no diastema
    Apes: C-P3 honing complex: the lower canine and P3 sharpen the upper canine every time the primate closes their mouth; long, projecting canine; diastema
  • african apes at the end of the Miocene and how they survived
    Gorillas: reinvade forests and become folivores
    Chimps and Bonobos: become arboreal and terrestrial; they have a more general use of their environment
    Our ancestors: bipedalism, become terrestrial and arboreal
  • why did our ancestors adapt to bipedalism? (hypotheses)
    -free hands to carry children, food, tools
    -access to arboreal food from the ground (no need to climb)
    -more energy efficient (ex: sun only hits shoulders)
    -walk between trees
    -see over high grass
  • first possible primates
    Cenozoic Era (66 mya - present)
    Paleocene (66 - 56 mya)
    -Plesiadapis
    -Carpolestes simpsoni
  • first true primates
    Eocene (56 - 34 mya)
    - lemur and tarsier like forms
    *Adapis (adapid): lemur like
    *Shonshonius (omomyid): tarsier like
  • when was evolution of the anthropoids?
    oligocene (34-23 mya)
  • when was evolution of hominoids?
    miocene (23-5.3 mya)
  • climatic change & adaptation in cenozoic (eocene, olidocene, miocene)
    -Natural cycles of warming and cooling
    Eocene:
    -temperature increase= tropical forests and tree dwelling creatures
    Oligocene:
    -temperature plunged
    -forests replaced by grasslands so primate ancestors adapt to this
    Miocene:
    -drastic reduction in sea level and temperature increase
    -possibly related to the adaptation of bipedalism
  • Early Hominins