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greg,
See the article by M.J. Benton, 'Diversification and Extinction in the History of Life' in the journal Science, volume 268 (7 April 1995), pages 52-58. Benton separates marine from terrestrial extinction rates, but shows that they parallel each other quite well over the Phanerozoic (or that part of it for which there WERE terrestrial animals!). Like most other investigators (Sepkoski, Raup, Boyajian, Hallam etc.) Benton recognises 5 big mass extinctions: the end Ordovician (O/S), late Devonian (F/F), end Permian (P/T), end Triassic (T/J), and end Cretaceous (K/T). Benton's maximal estimate of percent familial diversity drops for continental animals AND plants are: K/T - 10.9%, T/J - 29.2%, P/T - 64.3%, F/F - 61.9% (no terrestrial fossils at O/S). So, it's true, you see, that the K/T was a relatively modest 'big' extinction. You may feel confused because you're focused on 100% loss of the dinos, but remember that there are a great many more invertebrate families, plant families etc. that would have had at least a few species representatives in protected microenvironments: soil, leaf litter,hollow logs, caves, lakes, swamps, streams, or with protective habits: non-visual food location, detritus feeding, food storage, hibernation, estivation, resting eggs, larvae, spores, seeds, rhizomes - any of these could have made the difference between survival and extinction of a family. Benton's data show a number of lesser mass extinctions than the 'big five', so the K/T event still holds some distinction in the list of life's great catastrophes.
HTH & GOYM
Bob Hartwick
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