Thanks Doug,
Got to really dig into this paper to make sense of the conclusion which is only 
speculative and needs 
to be further evaluated for positive confirmation bias and field and lab work 
around the world.  It was 
quite top heavy on analysis which appears well done!

The authors, or maybe it was the press, used the study's 270 kg dissolved 
sample of well-characterized 
"chronostratigraphic" sediments from a Russian deposit in the study which got 
approved for publication 
in the prestigious journal, "Nature", if I read it correctly.  

It would have been more rigorous for my taste if it had been reviewed by MAPS 
editors, or the like, where the focus
 would have been more on interpretation, than on methodology.  Just my opinion, 
as both are important.  
It is an interesting subject - do we call it paleo-meteoritics? Getting any 
paper into Nature deserves congrats
for sure but I expected to be more awed from their editorial staff choices.  
Luckily no one told that to the Alvarez'.

In the end the conclusion is that ordinary chondrites used to be a 
significantly lower proportion of finds, nearly a 
half billion years ago according to the results of their study.  Then 466 mya 
that all changed with the disruption
of an L parent body.  I didn't notice special mention of H- or L-chondrites, so 
the assumption IMO is that that another
event happened recently.  None of this seems remarkably insightful but perhaps 
the authors point of view is 
that here's a smattering of evidence that confirms the idea that the ratios of 
meteorite classes will vary throughout 
geological ages which is nice when things make sense and people begin to 
dimension it with the 'fossil' record.

Kindest wishes
Doug

-----Original Message-----
From: Doug Ross <[email protected]>
To: mexicodoug <[email protected]>
Cc: Meteorite List <[email protected]>
Sent: Wed, Jan 25, 2017 1:38 pm
Subject: Re: [meteorite-list] (no subject)

Hi Doug,

Here is a link to the original paper:

http://www.nature.com/articles/s41550-016-0035

"Our data show that the meteorite flux has varied over geological time as 
asteroid disruptions create new fragment populations that then slowly fade away 
from collisional and dynamical evolution. The current flux favours disruption 
events that are larger, younger and/or highly efficient at delivering material 
to Earth."

Cheers from the “other” Doug,

Doug Ross







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