Geology 143: History of Life

Lecture 12 Notes

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Lecture 12

Therapsids

Super continent of Pangea formed in the Permian
Overall global climatic drying trend

Therapsids ­ synapsid reptiles
Evolved from sphenacodont pelycosaurs
Inhabited mid- to high-latitudes, not the tropics
Seasonal and dry climates with abundant vegetation, inclding the famous leaf fossil Glossopteris
Seasonal temps means that sophisticated thermoregulation existed besides just behavioral

Mammals evolved from therapsids in the Late Triassic
Different from modern African carnivores in that they were larger and more numerous

Therapsid Evolution

Theriodonts ­ large canines, some approaching sabor-toothed condition
Gorgonopsians dominant carnivore of the Late Permian
Cynodonts evolved into mammals in the Late Triassic

Dicynodonts ­ large-bodied herbivores and carnivores
Interlocking canines and incissors

Dinocephalians ­ dominant worldwide herbivores of the Late Permian
Make-up 90% of known therapsid fossils
Lost nearly all teeth except for upper cannines
Weak jaw moved forward and back in shearing action
Rat-sized to cow-sized

Diapsid Reptiles

Significant evolution in diaspids as well as synapsids in the Permian and Triassic

In Triassic, diaspids replaced synapsids as dominant land vertebrates

Diapsids evolved from Petrolacosuarus

Diapsid groups
1. Turtles ­ lost the two holes in the skull during shell adapatation

2. Lepidosauromorphs ­ small, lizard-like ectothermic, terrestrial
New Zealand Sphenodon

3. Archosauromorphs (Archosauria) ­ consist of 4 groups
a. thecodonts ­ med to large aquatic, terrestrial, and amphibious carnivores
b. crocodylia ­ crocodiles and aligators
c. dinosaurian ­ prosauropods, sauropods, ornithischians, theropods) bird ancestors
d. pterosauria ­

Early diapsids with poorly understood phylogeny
1. weigeltisaurs ­ includes Coelursauravus (glider) and mesosoaurs (aquatic)
2. ichthyosaurs

Hovasaurus, aquatic carnivore, is the best preserved Late Permian diapsid
Shares traits with thecodonts

Triassic Diapsid Takeover

Early Permian ­ forests were dominated by large pelycosaurs

Middle Permian ­ therapsids replaced pelycosaurs as dominant land reptiles

Late Permian ­ dominated by therapsids, began invading cooler climates

Early Triassic ­ therapsid diversity dropped, but widespread and numerous

Middle Triassic ­ therapsids were the dominant herbivores, improved running
Abundant carnivores

Late Triassic ­ archosaurs (dinosaurs) replace thecodonts
Dominance continued through Jurassic and Cretaceous

Respiration and Locomotion

Carrier's Constraint - Sprawling vertebrates cannot run and breath at the same time due to twisting trunk

Anaerobic glycolysis helps, but detrimental effects of oxygen debt and lactic acid

Stops in running are for breathing

Amphibians and reptiles have a 3 chambered heart, mammals and birds have 4 chambers

Pelycosaurs had a synapsid mitigation of Courier's Constraint ­ stiffened background, thus not so much twisting, and "wheel barrow" propulsion

erect stance also helped, evolved diaphram, maybe required for distance running
Triassic diapsids the first to make this breakthrough?

Therapsids evolved in cooler climates, diapsids in warmer climates
Erect gait did not evolve until the Early Jurassic in synapsids

Thecodonts

Stem group of archosaurs

Mid ­ Late Triassic ­ largest carnivores were thecodonts (rauisuchians and ornithosuchians)
Up to 6 or 7 m long and 2 m high

First Dinosaurs

The first dinosaurs appeared in the Late Triassic ~ 225 MY as small, agile, bipedal carnivores


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