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Old 12-25-2002, 06:19 AM   #11
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There is very good evidence that prior to the Tertiary Earth's atmosphere was richer in oxygen- the size of fossil insects indicates that there was then some way to allow them to oxygenate their tissues, which is not present today; a higher partial pressure of O2 would allow more efficient diffusion, the process which furnishes oxygen to insect tissues.
There's another graph of this in Jennifer Clack's Gaining Ground, which shows the highest oxygen levels in the earliest Permian, before the big dinosaurs. Carbon dioxide levels were comparable to today's then, and quite a bit higher in the Triassic and Jurassic.
It's odd that amber would preserve oxygen-rich air that well - I would have expected the oxygen to react with the hydrocarbons in the tree sap over that long a period. I'm sure that it would if it were modern pine-tree sap - but maybe that's why amber is preserved: it's not as reactive as turpentine.

BTW, the Clack book is pretty hard going - it reads like a text instead of a "popular treatment" - but it gives a fantastic overview of just how complicated and difficult a paleontologist's work must really be. It traces the fossil record of the transition of "fish" to land animal in wonderful detail: you'll learn all about ectopterygoid bones and how they changed over time.
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Old 12-25-2002, 08:14 AM   #12
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Oddly, I could find very little information about gas inclusions in amber. However, Berner et al's (2000) paleo O2 curve does show a major Permian-Carboniferous peak in PO2, and a smaller and more diffuse late Mesozoic peak. Gale et al (2001) cites estimates of 28kPa O2 for the end-Cretaceous, which is higher than the present atmospheric level of 21 kPa O2, but much lower than the up to ~40kPa O2 indicated for the Permian-Carboniferous by Berner et al's paper. 28 kPa O2 for the end Cretaceous is consistent with Berner's data, but is at the upper limit of the estimated error range.



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The modeling results for the Phanerozoic history of atmospheric O2 based on Eqs. 1 through 3 and the isotopic composition of sedimentary carbonates (35, 36) and sulfates (16, 37, 38) as proxies for seawater isotopic composition are shown in Fig. 2 and are compared with the results of the sediment abundance model of Berner and Canfield (15). There is surprisingly good agreement between the results of these two totally independent approaches.
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Other physiological studies suggest that elevated pO2 during the Permo-Carboniferous may help explain patterns in evolution. Flight metabolism in arthropods is enhanced at elevated O2 concentrations (44), and the sudden rise and subsequent fall of insect gigantism documented from the fossil record by, for example, giant dragonflies with wingspans of 70 cm is coincident with the Permo-Carboniferous maximum in pO2 (45, 46). Other patterns have been linked to elevated O2, such as changes in organisms with diffusion-mediated respiration and the invasion of the land by vertebrates (45, 46).
Berner et al, Isotope Fractionation and Atmospheric Oxygen: Implications for Phanerozoic O2 Evolution

Gale et al, The high oxygen atmosphere toward the end-Cretaceous; a possible contributing factor to the K/T boundary extinctions and to the emergence of C4 species

Berner, Atmospheric oxygen over Phanerozoic time.

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Old 12-25-2002, 02:18 PM   #13
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As far as I know, the biggest land mammal was Indricotherium, a hornless rhinoceros that lived during the early Miocene. A large adult would have weighed about 20 tons, which puts it in the range of the "smaller" sauropods. (Of course, the really big sauropods like Brachiosaurus would have weighed 80 tons or more, and dwarfed even something like Indricotherium.)

Angelos Economos has argued that "metabolic cost" limits the size to which land mammals can grow, and that Indricotherium was at or near the size limit for a land mammal. [Economos, A. C. 1981. "The Largest Land Mammal." Journal of Theoretical Biology, 89: 211-215.] I don't know how well his arguments have stood up over the past 20 years or so, however.

Cheers,

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Old 12-25-2002, 04:18 PM   #14
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Originally posted by pz:
Yes. Completely seriously. The guy really believes this stuff.
Wow.....

I don't know what's sadder.....

my question or your answer....
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Old 12-27-2002, 05:16 AM   #15
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I formatted all the old html (I think??) code out - then realized that might be a mistake -

Can someone tell me whether html code will always be disabled here?

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Old 12-27-2002, 07:26 AM   #16
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This problem was discussed on the dino list a while back. Basically the oxy problem is two-fold; first, the biggest land dwellers were gigantic, nigh on 100 tons, and second, they had really long necks. Take this mamenchisaurus. Note that there's no way it could breathe with a pipe that long and lungs located in the chest, it would drown in its own CO2. So it is a bit of a mystery -- air sacs in the neck? -- how it managed to inhale down a windpipe that long, and then exhale, and get fresh air. I don't know what the latest is; perhaps it is a solved problem.

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Old 12-27-2002, 07:27 AM   #17
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Last night on TLC, there was a 10,000 y.o. Mastadon skeleton. When it was alive it came in at 16 feet high and 10 tons. Not close to the sauropods, but still pretty damn big.
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Old 12-27-2002, 08:40 AM   #18
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would it be technically possible for them to live together?

I've heard Sauropods make terrible roommates.

From the discussion above, it sounds like it might not be possible for large dinosaurs to live with humans at today's oxygen levels. But of course, if you go outside for a bit you're likely to see a few small ones flying around or possibly singing you a nice song.

And while it might not be possible for large dinosaurs to co-exist with us today due to the lower oxygen levels, if the question is merely one of "technical possibility", I think it would have been "technically possible" for humans to survive 65+ million years ago at the higher oxygen levels (a point which seems to have been overlooked in the above responses).
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Old 12-27-2002, 08:52 AM   #19
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Quote:
Originally posted by Jobar
There is very good evidence that prior to the Tertiary Earth's atmosphere was richer in oxygen- the size of fossil insects indicates that there was then some way to allow them to oxygenate their tissues, which is not present today; a higher partial pressure of O2 would allow more efficient diffusion, the process which furnishes oxygen to insect tissues.
Fossils of giant insects are known from the Carboniferous (i.e., long before the time of dinosaurs). I don't believe they are found post-Permian. And the really bigt insects were dragonfly relatives, which were mostly wing anyway and long narrow bodies. I doubt the surface-to-volume ratio was much smaller than that of some present-day large insects, like some beetles and cockroaches.
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Old 12-27-2002, 09:07 AM   #20
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Quote:
Originally posted by Vorkosigan
This problem was discussed on the dino list a while back. Basically the oxy problem is two-fold; first, the biggest land dwellers were gigantic, nigh on 100 tons, and second, they had really long necks. Take this mamenchisaurus. Note that there's no way it could breathe with a pipe that long and lungs located in the chest, it would drown in its own CO2. So it is a bit of a mystery -- air sacs in the neck? -- how it managed to inhale down a windpipe that long, and then exhale, and get fresh air. I don't know what the latest is; perhaps it is a solved problem.

Vorkosigan
The problem with breathing through a tube is that the tube retains the air you just exhaled, and you just breathe it in again. This is one of the inefficiencies of our own lungs, but isn't a problem because the volume of the lungs is considerably greater than the volume of the trachea. For the same reason, breathing through a 1-foot tube is not a problem, but breathing through a 50-foot hose would be. It's possible that the dinosaurs were able to tolerate the same inefficiency (has anybody calculated the ratio of their lung to trachea volume?).

I can think of a couple of different ways to improve the design. One would be to have some kind of peristaltic contractions in the trachea, so air is forced in and out completely (i.e., no deoxygenated air is retained in the trachea). Another is to have a partitioned trachea, so the air only goes one way in each section, one breathing in, the other breathing out. Another way would be to have a separate exit from the lungs to expel air more or less directly, without having to go out the trachea.
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