Lesson 9 Flashcards
(26 cards)
Plate tectonics
The earth moves, plates shift creating movements of continents by millimetres (can move greater distances because of big events- earthquakes)
Alfred Wagner
1912 theory that continents fit together. Prevailing thought at the time was that land bridges were submerged just below sea level
Earth layers
Outermost layer = crust, 5-25 km thick
Mantle = mobile flowing layer
Outer core = iron and nickel, liquid
Inner core = solid molten, temperature of the sun
Lithosphere = crust and upper part of mantle
Aesthenosphere = part of mantle that flows like play dough
Crust and inner core are solid layers, mantle and outer core are liquid
Plate movements
Hot materials rise, cool materials sink, which creates slow moving currents. Solid crust plates sink at edges, pulling continents
Earthquakes
Earthquake fault lines occur at edges of continental plates, when two plates collide, slip under each other, overlap, ect
Lithosphere movement
Causes earthquakes, volcanoes, oceanic rifts, and mountain formations
Pangea
Triassic (240 million years ago)
Panthalassa - giant ocean that encompasses the globe
Laurasia
Asia, Europe, and NA (Jurassic 170 million years ago)
Gondwana
South America, Australia, Africa, Madagascar, India, and Antarctica
(India and Asia were originally separate, when it collided with Asian the Himalayas were born)
Broke apart in Cretaceous 100 million years ago
Dinosaurs and movement
First Dino’s appeared in Triassic 220 mya, while Pangea still existed. Therefore large mixing of Dino’s, where similar types are found all over the world
Once Laurasia and Gondwana split, we see predominant types in each.
Laurasia = tyrannosaurs, pachyceohalosaurs, and ceratopsians
Gondwana = sauropauds, abellasaurs, carcharadontasaurs
Late Cretaceous leads to breakup of continents and further break up of Dino’s, and potentially an increase in number of species
Antarctica Dino’s
Cryolophosaurus - frozen lizard - has a unique crest that looks like a snow shovel, but lived in warmer climates,
Antarctic climate was warmer due to an altered ocean circulation (transporting warm water from equator down to polar region)
70 million years ago, Antarctica was attached to Australia, and currents had to go around Australia, and warmed up there
Marine fossils on land areas
Sea level was much higher during Mesozoic era (up to 250 meters higher) this created sea ways that spanned areas that are currently covered by land
Sea level was higher because of a lack of glaciation, thermal expansion (warm water takes up more space), and sea floor spreading associated with plate techtonism (basins filling with rock and sediment)
Land area decreased
Interior NA was covered by a seaway
Nearby lakes and oceans create increased precipitation a and smooth out extremes in temperature (decreasing seasonality)
Higher temperatures and sea levels could have increased species diversity
Species diversity
Total number of species in an area
Increased due to increased water levels, increased temperatures, and decreased seasonality
Jurassic
Golden age of sauropods and long necks
Late Jurassic = thriving diplodocus, macronaroans
Macronaroans
High browser, robust, long front legs, long necks,
Spoon teeth lining entire jaw
Not pickey, crunched woody vegetation
Ecological niche
How a particular species makes its living, where it fits into the role of an ecosystem
Diplodocus
Simple peg teeth, selective nipper, reach high and prune leaves
Niche partitioning
Two competing species occupying slightly different niches, diverging to specialize
Thyreophorans
Ornithischians with body armour in Jurassic period, grazed in the shadows of sauropauds
Theropod takeover
Late Jurassic, large theropods were common, with stiff spines and long legs (ie allosaurus)
Ornitholesies - Turkey sized coelurosaur, long sacral vertebra, short, fast, small predators hunting small mammals, fish, insects, ect.
Coelurosaur
Early ancestor of birds
Titanosaura
Most robust of sauropods, like argentinosaurus, not easy prey. Largest animal to walk the earth
Preyed on by carcharadontasaurs, named for shark like teeth, had large jaws, largest was giganotosaurus.
Abellasaurs are the last of carcharadontasaurs, they had to adapt a different morphology (short muzzles and small heads, very short arms, wrinkley bone, cranial ornaments for sexual display)
At the end of the Cretaceous period, only Titanosaurs were found in both Gondwana and Laurasia
Abelisaurs = Gondwana,
Stegosaurus = became extinct long before Cretaceous began
Carcharadontasaurs = outcompeted by end of the Cretaceous
Ankylosaurs
In Laurasia, split into 2 groups
- ankylosaurids -tall clubs, backward pointing horns
- nodosaurid -large osteoderm spikes, narrow snouts, no tail club
Hadrosaurs (new iguonodon in late Cretaceous, most successful herbivorous Dino)
Sophisticated dental batteries, 2 groups, most abundant in Laurasia
Lambeosaurine - big crests, nasal passages amplifying their calls
Cranial instruments with complex ears leads to intricate calls
Hadrosaurine - crestless or lessened crested hadrosaurs, no sound amplification