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Re: Why did small dinos become extinct?
I thought some theories of survival/extinction allowed for plain old
luck--good luck and bad luck. Not very scientific, I know.
----- Original Message -----
From: "Philip Chalmers" <email@example.com>
Sent: Wednesday, December 12, 2007 10:56 AM
Subject: Re: Why did small dinos become extinct?
> Despite the thoroughness of David Marjanovic's response I think there
> are still some gaps:
> "Because they (small non-flying dinos), or most of them at least, did
> not have similar ecological niches. The surviving mammals and lizards
> mentioned above were for the most part granivores and insectivores; of
> the only dinosaurs in these niches, some survived -- all of them
> happened to be neornithean birds (and lithornithids, if those don't
> belong to Neornithes)."
> Why were small dinos excluded from these niches?
> Why could small dinos not survive by preying on the granivores and
> insectivores, as cats do now?
> "No flightless theropod the size of *Compsognathus* or smaller is
> currently known from the Maastrichtian, AFAIK." That's also my
> impression, but the question is why not, given that there were earlier
> very small flightless theropods?
> These two points are the central part of the question I originally
> raised. The only explanation I can think of is that small flightless
> theropods were squeezed out by the young of larger theropods and by
> small predatory mammals (successors of Repenomamus). The young of larger
> theropods were doomed because they grew to a size where they needed to
> prey on large herbivores, which were exterminated by the catastrophe(s).
> Are there better theories?
> "The Deccan traps are out of the question anyway because the main
> episode of eruptions ended 100,000 years before the boundary. It had
> made the global average temperature rise by 3 °C, and when it was over,
> the temperature came back to normal. And that was it." Some scientists
> (e.g. Chenet & Courtillot; Keller) think the geological evidence shows
> that the Deccan Traps erupted in a very period (under 100K years) in a
> series of pulses, the last of which was at the K-T boundary. So I prefer
> to regard this as an unresolved issue at present. But I wasn't asking
> about the cause(s) of the crisis, I was asking what feature(s) of dinos
> or of latest Cretaceous ecosystems made it impossible for small
> non-flying theropods to survive.
> David Marjanovic wrote:
> >> Most accounts of the K-T extinction state that no purely terrestrial
> >> animal larger than a cat survived (crocs and champsosaurs are / were
> >> semi-aquatic). Cat-/chicken-sized non-flying predatory dinos are known
> >> (most notably Compsognathus).
> > _No_ purely terrestrial animal larger than a cat survived, and _almost
no_ purely terrestrial animal smaller than a cat survived.
> >> David Marjanovic suggests the whole terrestrial ecosystem was
> >> devastated too baldly to sustain viable populations of predatory dinos.
> > We have some direct evidence for this, in the form of paleosols, the
fern spike, the fungal spike, and...
> >> But this is too simple:
> >> * Mammals survived.
> > As I just said: many mammals did _not_ survive. Let's take the
metatherian example: Before the boundary, we had "pediomyids", stagodontids,
peradectids, and maybe still deltatheridians. After, we had peradectids and
notometatherians*, which is apparently descended from some "pediomyid" -- it
is AFAIK enough to suppose that _two species_ of metatherians survived. The
eutherian example is little different: before the boundary, we had true and
false zhelestids, cimolestans, probably** asioryctitheres, *Deccanolestes*,
probably** zalambdalestids, and leptictidans. After it, we had cimolestans,
leptictids, and the clade composed of *Purgatorius*, *Protungulatum*,
*Oxyprimus*, and the (other?) placentals in the strict sense, which is the
sister-group of Leptictida; it is enough to suppose that _three species_ of
eutherians survived. I know little about multituberculate phylogeny, but not
long before the boundary there were djadochtatherian**, taeniolabidoid and
> > of which only the latter two groups are known from after the boundary,
and the known Cretaceous diversity of taeniolabidoids was very small, so it
is likely that very few species of multis survived.
> > I also remember reading a little book from 1981 (by Archibald and
someone else) that argued that 30 % of the North American lizard species
died out at the boundary. Notably, the herbivorous polyglyphanodontids bit
> > * Contains the marsupials in the strict sense and the now extinct
> > ** Known only from Mongolia, where the top of the Maastrichtian is
> >> Why could small small non-flying predatory dinos not
> >> survive in similar ecological niches?
> > Because they, or most of them at least, did not have similar ecological
niches. The surviving mammals and lizards mentioned above were for the most
part granivores and insectivores; of the only dinosaurs in these niches,
some survived -- all of them happened to be neornithean birds (and
lithornithids, if those don't belong to Neornithes).
> > Incidentally, no flightless theropod the size of *Compsognathus* or
smaller is currently known from the Maastrichtian, AFAIK.
> >> * The greatest devastation of plants was in N America, less in other
> >> parts of the N hemisphere, and even less in the S hemisphere.
> > Are you sure? New Zealand burnt down as well. That's where the fungal
spike (world going mouldy) was found for the first time.
> >> He also bases his response solely on the impact hypothesis. I've seen
> >> suggestions that the N and S hemispheres had separate wind systems, as
> >> they do now, so most of the fallout from Chixculub ( well N of the
> >> tropics) would have affected only the N hemisphere, except for the CO2
> >> emissions.
> > No. The gas emissions went all the way up to the mesosphere; the solid
ejecta exited the atmosphere and reentered all over the globe. This is
inevitable from an explosion of that size.
> >> If another factor (e.g. Deccan Traps) was responsible for most of the
> >> extinction in the S hemisphere,
> > (The Deccan traps are out of the question anyway because the main
episode of eruptions ended 100,000 years before the boundary. It had made
the global average temperature rise by 3 °C, and when it was over, the
temperature came back to normal. And that was it.)
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