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Re: Pleistocene & K/T extinctions
Whoops, accidental flame war. Okay, so my posts have been worded
strongly. That's what happens when I write first draft - on a second
draft I take out all the flame baiting. But here I'm going to shoot
straight from the hip, so go ahead and correct me when I screw up.
1) Europe. I don't know the dates off the top of my head, but I seem
to recall the Eurasian extinctions are substantially earlier than
those in North America but occur when Homo sapiens is going through
its big migration/population increase phase on that continent. The
Australasian extinctions are another case of extinctions well before
the North American extinctions, certainly much earlier than 10 kybp.
The African extinctions are earlier still. I find it implausible that
the same "climate" factors are responsible for the SELECTIVE
extinction of completely unrelated mammals in Australasia and the
rest of the world (marsupials vs. placentals). And then there's
always New Zealand... and Madagascar... and Hawaii, or any number of
other Pacific islands... and South America. The only common
denominator in any of these cases is the presence of H. sapiens.
2) "no directed human invasion" in Europe? Technically speaking this
may be right if Homo erectus is "human" or (here's a new one) if H.
erectus not only was directly ancestral to H. sapiens, but gave rise
to the latter through an agonizingly (shall we say "glacially"?)
gradualistic process. Then maybe we could say there was no human
"invasion" of Europe in the late Pleistocene. But I doubt we're going
to find many paleoanthropologists at this point who really think H.
erectus was the direct ancestor of H. sapiens; that H. sapiens was
present in Europe much before 40 - 50 kybp; or that the appearance of
H. sapiens (whatever caused it) was gradual. At some point there WAS
a human invasion of Europe, and that invasion DID shortly precede a
wave of large-mammal extinctions that is completely outside the range
of mammalian extinction rates during previous intervals of the
Pleistocene.
3) I'm sorry, but at this point it sure looks to me like "gradualists
are practicing an obsolete science" (not my phrase, but it will do).
Standard genetic models (in evolutionary debates) and standard
geophysical processes (in geological debates) all predict large
variation in rates of change. Therefore, it's actually strict
gradualism and not punctuationalism that requires extraordinary
processes. Just look at population genetic/microevolutionary theory,
where a host of processes are known that can cause a punk eke pattern
- stabilizing selection, developmental contraints, peripheral
isolates speciation, founder effects, genetic drift, you name it.
There is no sensible MICROevolutionary account of how a lineage could
evolve slowly and constantly on geological time scales, unless the
environment also changes slowly and constantly. Talk to any geologist
and you will get a quick denial that any factor of the abiotic
environment ever changes that way. The real question isn't WHETHER
evolutionary or geological rates vary greatly, but exactly how and
why.
4) U of C. Yes, I'm a recent graduate of the U of Chicago (actually,
I just defended and I graduate in August). Does that make me some
kind of a leper? Does being from the U of C make me a mindless
"product" instead of a human being? No, my advisors (Raup and
Jablonski) are not "rabid punctuationalists." They're not really
rabid about anything in particular, being more interested in figuring
out HOW to answer a question than in upholding dogma, and neither of
them really gives a damn about the punk eke debate - nor do any of
the other faculty or students here apart from a few geneticists (who
will go unnamed) who seem to think there is nothing else going on in
paleontology. The fact of the matter is that most professional
paleontologists gave up worrying about punk eke ten years ago or
more.
5) "great deal of valid counterpoint to the impact hypothesis"? This
may have rung true circa 1981 or even 1991, but at this point I think
the anti-impact people are fooling themselves. It's perfectly
reasonable that a lot of people in the scientific community who
aren't in the thick of things might think there is a reasonable
debate still going on. It's perfectly insane that certain people
could continue to oppose the impact model after attending symposium
after symposium where they are confronted directly with the evidence.
I'm sorry, but I've SEEN the anti-impact people in action at a
symposium during the last GSA meeting. Their capacity for doublethink
is amazing - just check out the recent exchange of letters between
Gerta Keller/Norm MacLeod and Richard Kerr in the 29 April issue of
Science. I'm sorry if I'm offending anyone who is in the Keller camp,
but speaking strictly from my own experience, I felt that talk after
talk in that GSA symposium exemplified desperate special pleading
against a) the impact and b) the rapid mass extinction. One of the
least impressive talks was on the 1966 core data from the Chicxulub
site, later published as the Meyerhoff et al. paper in Geology. The
data consisted of a well log describing observations on the core as
it was being drilled, and there was no documentation of the claim
that microfossils from units above the presumed base of the crater
are late Cretaceous. Furthermore, there was no discussion of the
possibility that said fossils (if they are Cretaceous) could have
been reworked from carbonates disturbed by the impact event. The
Meyerhoff paper itself summarizes two independent papers presenting
40Ar/39Ar analyses for samples from this same core that give dates
indistinguishable from K-T dates on units from across North America,
only to declare that these dates must be the result of alteration!
6) Stress below the K-T. I think everyone agrees that the world was a
very interesting place in the late Maastrichtian. Sea levels changed
rapidly, the reef-building rudist bivalves seem to have gone out well
before the boundary, and so on. I wouldn't be surprised at all if the
severity of the K-T event had a lot to do with the world being a
lousy place for organisms at the time, as Dr. Schwimmer indicates
(can I get some reprints on this? - I see from a quick check of J
Paleont that Dr. Schwimmer's earlier papers are largely on Campanian
fossils, so perhaps the data he mentions are still in preparation).
However, I think we should remember that stresses like changes in
ocean circulation patterns, onset or offset of glaciation, changes in
global temperatures, sea level changes, etc. happen ALL THE TIME and
fail to cause any detectable extinctions at all. I am speaking here
from a Tertiary perspective, where there are plenty of test-cases to
look at. I DO find the "world went to hell" hypothesis intriguing and
appealing IN COMBINATION with the impact hypothesis, and a grand
"world went to hell" hypothesis is currently popular among students
of the Permo-Triassic mass extinction.
7) "Scientific Method." I'm amazed to find myself being accused of
having no familiarity with the "Scientific Method" (whatever that is;
I challenge you to find a philosopher of science who thinks there is
any one "scientific method"), as if to say that siding with the
majority of paleontologists and geologists who agree with the impact
hypothesis disqualifies me as a scientist. I'm amazed to find myself
accused of not having an "open mind" or of believing that any
gradualist need "be a fool or ignorant." As I've outlined above, I do
think that accepting gradualist interpretation could result from not
following the literature too closely, but I do not think that mere
foolishness would explain continuing to believe in that
interpretation despite the published evidence against it. That's what
I would call not having an "open mind" and rejecting the "Scientific
Method" (again, whatever that is - if you want to argue Popper and
Kuhn, maybe we should take this elsewhere).