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Re: the start
Just a quick comment on John Erick Schneide's post (I'll get back to
David Schwimmer when I get a chance). The "impact during the
Triassic/Jurassic" to which Schneide refers is (I believe) the impact
that created the Manicouagan crater in Canada. As I recall, recent
dates on the crater show it to be far too old to relate to the
Triassic-Jurassic boundary event. Additionally, there are plenty of
dinosaurs around already in the late Triassic (Carnian-Norian). It's
true that Michael Benton has argued for 1) a late Carnian extinction
event, and 2) a rapid dinosaur radiation after that. However, 1)
rests on shaky biostratigraphic data (the correlations largely rest
on a priori assumptions about what "early" or "late" Carnian
vertebrate faunas should look like) and has never been supported
statistically (e.g., tests for above-background extinction rates or
for the Signor-Lipps effect). Meanwhile, 2) suffers from similar
data-quality and statistical problems. In the first place, you need
to show that an evolutionary radiation is something that needs to be
explained at all. This means showing that the radiation proceeded
more quickly than would a random diversification with constant
speciation and extinction events. A statistically unusual pattern of
this kind is abundantly clear for the early Paleocene radiation of
mammals, for example, but I know of no such study for any group of
Mesozoic vertebrates. I also should point out that our knowledge of
late Triassic vertebrates is far better than out knowledge of, say,
early Triassic vertebrates, but generally not that good and far worse
than our knowledge of virtually any fossilizable group of marine
invertebrates (molluscs, trilobites, forams, graptolites, ostracods,
etc.) at any point in history. I think we should refrain from arguing
about "why" the dinosaurs radiated until we have some solid evidence
that there was anything unusual about their early history of
diversification.