Gesendet:ÂDonnerstag, 05. Dezember 2019 um 20:46 Uhr
Von:Â"Mailing" <mailinglistinformation@gmail.com>
Outcrop area is not necessarily a good proxy for predicting (terrestrial) diversity, see e.g. Dunhill (2012), Dunhill et al. (2014), Walker et al. (2017), and getting outcrop area/exposure area on a global scale is a non-trivial task (even less so the density of fossils per formation).
Well, the worst-case scenario is not that we have to use a worse proxy. The
worst-case scenario is that we simply cannot predict diversity unless we
perform a non-trivial task.
I am not so sure what you mean with "actually known fossils". The results are obviously based on what is known at the moment - but that is trivial and also holds true for the opposite interpretation of the fossil record. So, I think I misunderstand you here: What do you mean by this?
As I said: if there was a radiation going on in Africa, we're not likely to
find out anytime soon.
I'm not trying to argue that I can show there was no decline in origination
rates; I'm trying to argue nobody has shown a reason to think there was a
decline.
The shape of the curves is determined by the mathematical properties of the
involved models. For a model with constant speciation/cladogenetic rates (I will
stick to speciation since that is the commonly used term) and extinction rates
(with spec. rates > ext. rates) you expect a linear increase in the number of
speciation events in log space through time. If speciation rate decreases through
time and is ultimately surpassed by extinction rate, you expect a quadratic
relationship (also holds true for the opposite case, where speciation rate
increases through time + extinction rate remains constant).
You then fit your models to the data and assess which model performs best. That
will tell you whether non-avian dinosaurs as a whole were in decline or not (in
terms of speciational capability). You can add various covariates to account
for other effects involved (e.g., sampling bias, extrinsic controls on
speciation dynamics, etc.), but it is not necessary for the model per se.
Yes, yes. My problem with this is the long-term view all authors so far appear to have taken. Shouldn't we expect extinction rates, and probably also origination rates, to vary much faster and much more erratically than the smooth curves in the paper? Environments aren't stable, or show stable trends, over tens of millions of years, so why should origination or extinction rates do that?