1 / 28

Life of the Mesozoic

Life of the Mesozoic. Mesozoic Climates. Primary control is the balance between incoming/outgoing solar radiation Factors affecting balance: Configuration and dimensions of oceans and continents Development and location of mountain systems Changes in snow, cloud or vegetative cover

walker
Télécharger la présentation

Life of the Mesozoic

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript


  1. Life of the Mesozoic

  2. Mesozoic Climates • Primary control is the balance between incoming/outgoing solar radiation • Factors affecting balance: • Configuration and dimensions of oceans and continents • Development and location of mountain systems • Changes in snow, cloud or vegetative cover • Carbon dioxide • Location of poles • Amount of radiation aerosols • Astronomic factors – changes in earth’s orbital parameters

  3. Factors favoring cooler climates • Vast continental areas • Low sea level • Uplifting mountains • Polar position of continents • Lower CO2 levels

  4. Triassic • Relatively cool • Pangaea continents still clustered • Mountain building created many highlands • Paleo-equator: central Mexico to north Africa • Wind shadow deserts in continental interior • Red beds • Evaporites

  5. Jurassic • Relatively mild • No glacial deposits • Evidence of monsoons and aridity • Coal in many spots (including Antarctica) • Wide belts of tropical conditions • Continents at current latitudes • Atlantic continuing to opening • Tethys brought warm ocean currents inland

  6. Cretaceous • Relatively warm • Subtropical flora existed at +70o Latitude • High and low latitude coal swamps • High sea level (maximum inundation of Phanerozoic) • Continents near where they are today • Arctic Canada near north pole • Antarctica near south pole

  7. By the end of the Cretaceous • Rapid cooling • Vast regression • Major mountain building • Plankton produced CO2 shortage • Volcanic activity • Terminal Cretaceous climatic event • Tropical cyads sharply reduced • Hardy conifers and angiosperms expand • Drop in ocean temp

  8. Mesozoic invertebrates • Marine invertebrates • Permian extinction decimates brachiopods • Pelecypods bivalves take hold (mostly oysters) • Gryphaea –small oyster • Exogyra – large oyster • Rudistids (horn-like valve, with left valve acting as lid) – become major reef builder of Mesozoic • Scleractinian corals • Hermatypic (reef builders) normal salinity, less than 50 m water and 20o C (Algal symbionts)

  9. Echinoderms • Starfish, sea urchins, crinoids • Regular echinoids: five-fold symmetry spherical shell numerous in European chalks • Irregular echinoids: displaced regular echinoids during cretaceous • Crinoids: both stemmed and stemless forms.

  10. Ammonoids Cephalopods • Mesozoic also age of ammonoids • Suture pattern key to taxonomy • Variety due to environmental adaption; expansion follows sea-level rise and continental flooding. • Diversity of forms; planispiral (early cretaceous) to open spiral, straight conch, helicoids (late cretaceous) • Extinction at end of cretaceous • Nautilods: sole survivors

  11. Belemnite Cephalopods • Highly successful: Jurassic- Cretaceous • Straight pointed shell • Moved through water by jetting water • Related to modern squid and octopus

  12. Crustaceans: • barnacles, crayfish, lobsters, crabs, shrimp

  13. Terrestrial Invertebrates • Pulmonates – air breathing snails • Fresh-water clams • Centipedes, spiders, millipedes, scorpions • Insects: Several groups appeared before the end of Jurassic • Butterflies (Lepidoptera) • Ants, bees, and wasps (Hymenoptera) • Termites (isoptera) • Mantises (mantodea) • Earwigs (dermopera)

  14. Amphibians • Temnospondyls: Surviving group of tetrapods from Permian extinction • Triassic – 17 families survive • Jurassic – 2 remain • Cretaceous – 1 lineage left • Lissamphibia: oldest forms known • Oldest frog- Triadobatrachus (lower Triassic) • Oldest salamander: Karaurus (upper Jurassic) • Surviving forms of Lissamphibia- frogs, toads, salamanders, and newts

  15. New reptiles groups • First turtles (toothed turtles) • Rhynchocephalians (tuartaran lizards) • Archosaurs: crocodiles, flying reptiles, thecodonts, dinosaurs • Hesperosuchus • Small, light, agile, long tail, short limbs • Walked erect (ancestor of dinosaurs) • Caught prey with forelimbs • Forelimbs most likely evolved into wings

  16. Phytosaurs • Reverted to four legged stance, some armored • Example of genetic convergence

  17. Dinosaurs • Two orders: Sauriscia (lizard hipped) and Ornithiscia (bird hipped) • Sauriscia: triradiate pelvic bones like thecodonts • Ornithiscia: pubis parallel to ischium like birds

  18. Saurischians • First dinosaurs • Eoraptor and herrerasaur: late Triassic • Coelohysis • Ornithomimus: the bird mimic (toothless beak)

  19. Carnivorous saurischians or therapods • Large hind limbs, claws on toes, smaller forelimbs, and serrated teeth • Deinonychus and velociraptor – Cretaceous predators • Family of Allosauridae – Allosaurus (US) • Giant therapods: Tyranosaurus (13m, 4 tons, North America)

  20. Herbivorous saurischians or Sauropods • (Jurassic- Cretaceous) • Evolved from late Triassic protocerapod • Long necks, long tails, four-legged stance • Apatosaurus(formerly Brontosaurus, Jurassic Colorado) • Brachiosaurus: Longer forelimbs to reach high branches) • Supersaurus: 80 – 100 tons • Sauropods left extensive footprint record

  21. Ornithischians • (late Triassic – Cretaceous) • Characteristics: Beak for cropping plants, quadrupeds and bipeds, primitive jaw • Ornithopods: bipedal forms – Iquanadon (the thumbs up dino) Herd animal • Hadrosaurs- web-footed aquatic version (duck-billed dinosaurs)

  22. Quadropedal Ornithischians • Stegosaurus- two paired, spike tail, heavy plates • Ankylosaur – bony plates over side an back • Ceratopsians- horn on face, bony frill on back of head (triceratops)

  23. Aerial Reptiles • Adaptive radiation of Permian forms • Gliders with skin wings • Coelurosauravus (Permian - Triassic) • Icharosaurus (Triassic) • Gliders with modified ribs functioning as wings: Longisquama (Triassic)

  24. Active fliers • Pterosaurs (late Triassic – Cretaceous) • Sharovipteryx – skin membrane between elbows and knees • Sordes pilosus “Hairy devil” wing flapping reptile • Large head and eyes, long jaw, thin slanted teeth, finger bones long to support wings • Two groups evolved: rhamphophynchoids (long tails) and Pterodactyloids (no tails) • Pteranodon – 7m wingspan example of pterodactyloid

  25. Marine Reptiles • Archosaurs: only one group invaded Mesozoic oceans (Crocodiles) • Nothosaurus (paddle shaped limbs) • Appeared during Triassic • Ancestor of Plesiosaur

  26. Placodonts • Mollusk eating reptile • Paddle-shaped flipped • Pavement type teeth in jaws and palate

  27. Plesiosaurs • First appeared during Jurassic • Short broad body with flippers and small head • Long neck and short neck forms • Slender curved teeth • Loch Ness Monster?

  28. Ichthyosaurs • Reptilian counterpart of modern whales

More Related