Quiz Flashcards
What are the challenges of terrestrial habits?
Support Locomotion Feeding and Respiration Sensory Systems Water Balance
Tiktaalik
Late Devonian
Fins and scales of a fish, mobile neck, separate pectoral girdle of a tetrapod
Not a true terrestrial tetrapod
Had aquatic lifestyle and used fins to maneuver around
Early Tetrapod Locomotion
Limbs splayed out to the side
Axial flexion of vertebral incorporated into the stride (similar to salamanders)
Body was probably not elevated off substrate during stride
Girdles attach to vertebral column
Ribs become more robust
Increase range of limb motion
Traits of Late Devonian Tetrapods
Amphibious habits
Reliant on water for reproduction
Generalized predators
Evolution of tetrapod girdles and limbs
Adaptations for Terrestrial Plants
Rigid stem/stalk
Root system to act as anchor for taller structures
Leaves to aid in collection of sunlight for photosynthesis
Vascular tissues to distribute water and nutrients throughout the organism
What is the first land plant?
Cooksonia
What are some traits of Cooksonia?
No leavs, no flowers, no seeds, no roots
Reproduction via spores
Photosynthesis
When did Cooksonia appear?
428 mya
Silurian
Traits of Plants in Early Devonian
Small vascular and non-vascular plants
Traits of Plants in Late Carboniferous
Vegetation with trees >35 m tall
Evolution of Roots
Substantial rooting systems present by Late Devonian
Evolution of Leaves
Microphylls
Megaphylls
Microphylls
Small, single vascular strand
Megaphylls
Large, complex vascular networks
The Seed
Freed plants from needing water for reproduction
Product embryo
Nourish developing embryo
Arborescent Revolution
Earliest trees appear in the middle Devonian
Until the late Carboniferous, forests were dominated by 4 groups of spore producing trees, and 2 groups of early seed producing trees
Climate Change During Devonian-Carboniferous
Climate changed from warm, humid and ice-free to cooler, drier climates with glaciation in high latitude of southern hemisphere
Several glaciations
Glaciation = lower sea levels
Amniotic Egg
Semipermeable shell that allows gas exchange with atmosphere
Allows tetrapods to become fully terrestrial
Extraembryonic Membranes
Chorian
Ammion
Allantois
Chorian
Surrounds embryo and yolk sac
Ammion
Surrounds embryo with water
Allantois
Sac for respiration and waste storage
Phylogenetic Reconstruction
All amniotes share a common feature in that they have closed the otic notch
What are the earliest amniotes?
Hylonomus and Paleothyris
Four groups of Amniotes
Anapsids
Aynapsids
Diapsids
Euryopsids
Anapsids Creatures
Turtles and early amniotes
Synapsids Creatures
Mammals and mammal like reptiles
Diapsids Creatures
Reptiles (birds, lizards, dinosaurs, crocodilians)
Euryopsids Creatures
Several convergent marine retile groups (Plesiosaurs and Ichthyosaurs)
Anapsids Skull
Lack of postorbital fenestra
Diapsids Skull
Two postorbital fenestrae framed by the parietal, postorbital, squamosal, jugal and sometimes the quadratojugal
Diversified during late Permian
Euryapsids Skull
Single postorbital fenestra bordered by the parietal, postorbital and squamosal
Synapsids Skull
Single postorbital fenestra framed by the squamosal, postorbital and jugal
Cynodonts
Show mammal like features
What are the Mammal Like Features that Cynodonts Have?
Double occipital condyle Secondary palate Increase in jaw muscle mass Limbs rotated under body Dentary makes up more than 3/4 of the lower jaw Well-developed heterodonty
Secondary Palate
Separates nasal region from oral region
Two parts: hard (up front) and soft (at back)
General Early Synapsid Trends
More upright posture
Reduction of girdle elements
Elongation of limbs
Specialization of dental battery
When is the Permo-Triassic Boundary?
252.17 mya
How many extinctions were there around the Permo-Triassic Boundary?
2 extinctions, about 5 million years apart
Causes of the P/T Extinction
Extraterrestrial
Terrestrial - Physical and Biological
Extraterrestrial Causes
Bolide impacts
Physical Terrestrial Causes
Volcanism
Climate Change
Sea Level Change/Anoxia
Biological Terrestrial Causes
Spread disease or predators
Evolution (new plant types)
Volcanism
Siberian Traps eruptions, starting before and continuing after
Mantle Plume
Upwelling of abnormally hot rock within the Earth’s mantle
Heads of mantle plumes can partially melt when they reach shallow depths
Often invoked as the cause of volcanic centers
Effects of Large Scale Volcanism
Massive input of greenhouse gases
Released aerosols could combine with H2O in atmosphere to form acid rain
Burning of large amounts of coal
These effects could lead to global warming, which may have shut down the ocean currents and lead to ocean anoxia