Extinct taxa: About 50% gone by Triassic >245 MYA
Rest during Mesozoic 245-65 MYA
Major radiations: Carboniferous 360-285 MYA; Permian 285-245 MYA
and Cretaceous 145-65 MYA for infraordinal taxa
Correlations with other major taxa
Pre Devonian 600-400 MYA- First land plants & animals;
Scorpions, Millipedes
Devonian 400-360 MYA- Seed ferns; first insects, spiders;
Eurypterids (marine)
Carboniferous 360-285 MYA- Ferns; Amphibian specialization; first
Reptiles, Pterygota: Paleoptera and Neoptera
Permian 285-245 MYA- Conifers; Reptiles diversify; Many insect
orders go extinct, modern orders appear; first Endopterygota
Mesozoic 245-65 MYA- Ginkos, Cycads, Angiosperm radiation;
Age of Reptiles; first Mammals, Birds; Neoptera dominant,
many modern insect families; Amber fossils
Tertiary 65-1 MYA- Insect fauna similar to present by mid Tertiary;
Amber fossils.
III. Amber insects and biotechnology
Age - commercial value - fakes
DNA extraction & replication - Jurassic Park
Comparisons between fossil and modern taxa
Termites & Stingless bees (40 MYA)
Weevils (120 MYA)
IV. Biogeography
Biogeographic regions
Why do insects occur where they do today?
Disjunct patterns
Evolution
Extinction
Continental Drift
Dispersal
Active
Passive
Human assisted: Accidental; Intentional
Readings in Gullan, P.J. and Cranston, P. S. (1994). The Insects: An Outline of Entomology: