LECTURE 6 Flashcards
1
Q
cretaceous - palogene extinction (65 mya)
K/Pg
A
the dinosaur killer
- at least 50% of all species lost
- nothing over 25kg survived on land
- larger body = needed more to survive
- one exception = crocodile/alligator = generalists - not fussy eaters and can survive without food for a while
- 80-90% of marine species
- includes marine reptiles, ammonites, mosasaurs, plesiosaurs
2
Q
K/Pg boundary
A
- mass extinctions changes in the fossil record
- rock layers deposited 65mya record the changes
- looks like a thick black band in the rock
- palogene = sandstone sediments
- cretaceous = eg mudstone
3
Q
causes of the K/Pg extinction
alvarez hypothesis
A
- thought to be impact of large asteroid
- found high iridium levels at the K/Pg contact
- iridium is rare on earth
- huge spike to 3.7ppb (20x normal concentration)
- typically 0.2ppb
- recorded globally
- iridium known to exist in higher concentrations in extra-terrestrial objects
- so thinks the object must have been at least 10km in diameter
further evidence:
- soot layers associated with iridium layers = massive global fires
- fern spores = first to colonise a fire-impacted area
- tektites = natural glass produced by melting rocks during impact = shows large impact
- shocked quartz = planar deformation/lamellae
- tsunami deposits
- the crater = drilling off coast of Yucatan Peninsula, Mexico reveals odd rocks = suevite
- suevite = rock of brecciated material (glass and rock) glass = partial melting and rapid cooling
4
Q
chicxulub impact crater
A
- geophysical surveys
- shows earths gravitational field
- gravity = proxy to rock density
- see concentric rings (like a crater structure)
Yucatan Peninsula, Mexico
- seismic refraction tomography shows density of ocean bottom layer
- shows that sediment had filled in the crater
- crater size = 180-240km diameter
- meteor size = about 10km in diameter
- large complex crater:
• concentric ringed structure
• central peak or peak ring
5
Q
impact
A
- meteor was ~10km diameter
- shallow angle of entry (20-30degrees)
- energy of impact = 6.2x107 tonnes of TNT
- 100km3 rock vaporised
- air blast >1500km radius
- ejecta deposited north west of the impact site
- winds in excess of 1000km per hour near the impact site possible
- ejecta would have been several hundred meters thick near impact
- along campeche bank, 350-600km from chicxulub, impact deposits of ~50 to ~300 meters have been logged in boreholes