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Dinos and boundaries
>Only one species has been found in
>more than one stratigraphic layer (species, not taxon).
Not quite true (Leptoceratops gracilis is in both the early-mid
Maastrichtian Meeteesee Formation and the late Maastrichtian Lance,
Anchiceratops ornatus in both the late Campanian Judith River Group and the
early-mid Maastrichtian Horseshoe Canyon, some of the species of Iguanodon
may cross over the Neocomian-Gallic boundary, and Coelophysis bauri might
be in both the Carnian and Norian), but for the most part a fair statement.
>The K/T " die out
>may just be representative of changing conditions world wide, and not be the
>result of some global catastrophe.
> Second, by the systematics used in paleontology now, birds are dinosaurs.
>And Aves (or birds) had evolved by the late Cretaceous. So why didn't they
>die out with the other dinosaurs?
Indeed, they'd been around since at least the Late Jurassic.
> Third, we only know about 500 dinosaur species (correct it, but I think
>I'm in the ballpark) all thinly spread out through 100-150 million years. I
>do not think that we have anywhere near a reasonable picture of the
>diversity of life in the past. We have enough of the puzzle to learn a lot
>about vertebrate development, but not nearly enough to construct scenarios
>on mass extinction. Even the mass extinctions took millions of years to
>happen. Hardly a stunning and instantaneous loss.
However, the invertebrate, microfossil, and plant records do show pretty
well a rapid event of less than a few thousand years at the boundary,
although this was preceded by several million years of stepwise declines in
diversity.
And, welcome to the net.
Thomas R. Holtz, Jr.
tholtz@geochange.er.usgs.gov
Vertebrate Paleontologist in Exile Phone: 703-648-5280
U.S. Geological Survey FAX: 703-648-5420
Branch of Paleontology & Stratigraphy
MS 970 National Center
Reston, VA 22092
U.S.A.