This came in the 11th September ScienceDaily newsletter:
Oxygen theory of mass extinction questioned by new research findings
(1) How does ambient temperature influence the results? Was 20°C a wise choice? I can't recall all the climate trends of the Mesozoic off hand but I'm quite sure many modern summer nights at my latitude are warmer than that.
(2) Where are the studies that talk about these oxygen levels <12%? I'm sure they exist if they are referred to by the authors but I can't seem to find a graph that shows such a low oxygen level for any point in the Phanerozoic.
(3) I'm not sure which extinction the second of the "at least two" is (assuming one is the Permo-Triassic affair), but if it's the Late Devonian (the Devonian has an oxygen dip in the graph I'm looking at) then that has frank all to do with Mesozoic charcoals.
EDIT:
it was in the blurb, which I didn't read at first, and it's the Late Triassic extinction. Please kindly forget point (3).
(I was also wondering why paper, matches and candles? Moss and wood are kinda realistic, as would be ferns, random dry leaves/needles but I have no idea what insights a candle can give about wildfires
)
In summary... what am I to think of these findings?
Oxygen theory of mass extinction questioned by new research findings
I have a few wee questions/problems wrt this:By performing experimental burns using pine wood, moss, matches, paper and a candle at 20°C in varying ranges of oxygen concentrations and comparing these results to the occurrences of fossil charcoal throughout the Mesozoic (250-65 million years ago), we were able to identify that prolonged periods of low oxygen are unlikely to have occurred, says Dr Claire Belcher from the School of Biology and Environmental Science, University College Dublin, the lead author of the report.
Low oxygen atmospheres, less than 12%, are considered to be the primary driver of at least two of the big five mass-extinction events, explains Dr Belcher. But our research findings question that hypothesis and highlight the need for more detailed studies of fossil charcoal across these mass extinction events.
(1) How does ambient temperature influence the results? Was 20°C a wise choice? I can't recall all the climate trends of the Mesozoic off hand but I'm quite sure many modern summer nights at my latitude are warmer than that.
(2) Where are the studies that talk about these oxygen levels <12%? I'm sure they exist if they are referred to by the authors but I can't seem to find a graph that shows such a low oxygen level for any point in the Phanerozoic.
(3) I'm not sure which extinction the second of the "at least two" is (assuming one is the Permo-Triassic affair), but if it's the Late Devonian (the Devonian has an oxygen dip in the graph I'm looking at) then that has frank all to do with Mesozoic charcoals.
EDIT:
it was in the blurb, which I didn't read at first, and it's the Late Triassic extinction. Please kindly forget point (3).(I was also wondering why paper, matches and candles? Moss and wood are kinda realistic, as would be ferns, random dry leaves/needles but I have no idea what insights a candle can give about wildfires
In summary... what am I to think of these findings?
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) challenges the role of the oxygen factor.