When all ecosystems are destroyed, normal ecology may not have to
say much... real question: why should life history be
so important?
No seed-eating species are known (though I can't speculate about
what Gobipteryx did, for example).
Were there any deserts in the Maastrichtian? Was there any such
thing as a savannah anytime before the Eocene? Were there certainly marsh-living
dinosaurs apart from some neornithine bird groups that survived? So maybe it's
enough to explain how more or less all forests worldwide were devastated. A
big impact can cause this, and there is ample evidence that gigantic wildfires
happened.
What a difference.
Is the fossil record of these groups good enough to allow any
statistics?
When "placental mammals" means the crown group Placentalia, I
disagree because no certain member of that group is known from the Mesozoic.
When "placental mammals" means Eutheria, I disagree likewise because of the
diverse Asian clade of Eutheria that is known from the Coniacian to the
Campanian or Maastrichtian but not from the Cenozoic (Zalambdalestidae
+ Asioryctitheria + Ukhaatherium + maybe Zhelestidae). Why
doesn't one known Cenozoic eutherian have epipubes?
And then there is the diverse clade
Djadochtatheria, a group of multituberculates with AFAIK the same range in time
and space as the abovementioned assemblage.
Is 70 % of... what? Species? so far from
complete?
All freshwater sharks of North America. All non-deep-sea coelacanths
worldwide.
Asia had a lot of endemic turtle clades in the Mesozoic (look for Chinese
family names and for Lindholmemydidae in www.fmnh.helsinki.fi/users/haaramo/Metazoa/Deuterostoma/Chordata/Reptilia/Parareptilia/Cryptodira.htm).
All gone, though I don't know if exactly at the boundary.
The ammonites are not going to be amused
when they read that. Hippurites? Inoceramids? Plesiosauria and
Mosasauroidea? All completely dead, with no descendants. Ammonitoidea certainly
qualifies as a "broad group", whatever that is.
Not to mention the immense
extinctions of plankton. Unfortunately I don't know anything about the internal
taxonomy of Foraminifera and Coccolithophorida. Same for Echinodermata... there
were those free-swimming crinoids like Uintacrinus before the K-T,
right?
The Antarctic Connection sounds good to me. All birds killed
off everywhere except in Antarctica, almost all birds killed off in Antarctica,
and because all Antarctic birds were Neornithes in the Maastrichtian all
survivors were Neornithes. Relies on negative evidence, though.
Maybe I can offer a
more ecological explanation. Most of the few well enough known
Enantiornithes, such as Avisauridae, were apparently arboreal, while no
other known Maastrichtian bird was. Burn down all forests, and Enantiornithes is
history. Ichthy- and Hesperornithiformes fed on fish that fed on plankton. Make
a Strangelove ocean practically without plankton, and these bird groups are
gone, too. Chicken- respectively tinamou-like birds, on the other hand, are
expected to survive -- they live off whatever lives in leaf litter, and off
seeds. They are, for maybe months, independent of primary production. Shorebirds
(in the ecological sense) can likewise feed on survivors.
Not to mention the role
of pure random once the world has crashed down and population sizes are
minimal.
BTW, as long as it isn't
completely clear on whom the burden of proof is, one must first answer the
question "why not?".
At least in North America, they didn't rise or fluctuate at
that time, but AFAIK they fell steadily through 4 million years. Any new
evidence here?
Therefore the gigantic mid-Oligocene
mass extinction which almost reached the Permian-Triassic boundary in magnitude
:-> :->
AFAIK there's no evidence for ferocious climates around
the K-T boundary, except for the very short heat wave mentioned onlist
recently that is predicted by an
impact.
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