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Natural Science Forum / Biology / Paleontology / January 2007



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Solution to the Big Dinosaur Paradox

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esker_phys@pcisys.net - 07 Jan 2007 07:05 GMT
Over three hundred and fifty years ago Galileo wrote about scaling
properties.  He said that as animals get bigger their bones become much
thicker and their relative muscle strength is reduced.  Because of this
the Africa elephant is the largest animal that can exist today.  While
the giraffe is the tallest animal that can exist today.  The
Brachiosaurus was over twenty times heavier than today's Africa
elephant and over three times taller that today's giraffe.

Scaling properties are fundamental to all science disciplines. But
because paleontologists have failed to solve the big dinosaur paradox,
they continue to insist that size does not matter.  Because of this,
Galileo's scaling properties are not taught in science classes and so
everyone's education suffers.

I have posted a web site www.dinosaurtheory.com where I explain the
scaling properties and the many problems presented by the large
dinosaurs and pterosaurs of the Mesozoic era.  On the web site I also
make available external links to other researchers that are presenting
similar information.  Finally, from my web site an article can be
requested that gives the solution to the big dinosaur problem.

The controversy is over.  I have solved the big dinosaur paradox and
much more.  Enjoy the article and try not to lose too much sleep
thinking about it.  I am David Esker and I will rock the science world.
don kenney - 07 Jan 2007 14:59 GMT
I can't figure out how to get to your article and I imagine others will
have similar problems.  Why not post a summary of your theory?

A couple of points:

In point of fact, land mammals significantly larger than the African
elephant are known.Indricotherium is estimated to have had about twice
the mass.  That's all I plan to say on that subject, I'm not really
equipped to evaluate at what point land animals exceed physical
possibilities.

You're correct about giraffes and the problem of getting blood to their
head.  I've long been a bit curious how they do it without a lot of
strokes and similar circulatory problems.  Note however, that there are
at least three relatively straightforward "engineering" fixes that
could have been used by the long necked sauropods.

1.  Secondary pumps (hearts) every few meters in the neck.

2.  Operate the central circulatory system at quite high pressure and
feed the smaller blood vessels through pressure reducers.

3.  Simply don't deliver (much) oxygenated blood to the brain when the
neck is elevated and apply the sort of physiological techniques that
allow air breathing mammals to function underwater.  That would mean
that the head would have to "come down for air" periodically just as a
whale or seal needs to come up for air occasionally.  It doesn't seem
like that would be enormous problem.  (I'll leave the issue of the
musculature required to raise and lower a neck that long to someone
better equipped to comment).

===

Your discussion of blood pressure seeems essentially correct.  If it
will help, here are three decidedly unscientifc diastolic blood
pressure measurements made with a wrist cuff.  Standing, arm elevated
-- 47.  Standing, wrist at heart level - 80.  Standing, arm at side --
109.

> Over three hundred and fifty years ago Galileo wrote about scaling
> properties.  He said that as animals get bigger their bones become much
[quoted text clipped - 20 lines]
> much more.  Enjoy the article and try not to lose too much sleep
> thinking about it.  I am David Esker and I will rock the science world.
John Harshman - 07 Jan 2007 16:14 GMT
> I can't figure out how to get to your article and I imagine others will
> have similar problems.  Why not post a summary of your theory?

If it has to do with the felt effect of gravity based on Saturn being
stationary over the north pole, Ted Holden is way ahead of him on that.

> A couple of points:
>
[quoted text clipped - 56 lines]
>>much more.  Enjoy the article and try not to lose too much sleep
>>thinking about it.  I am David Esker and I will rock the science world.
esker_phys@pcisys.net - 07 Jan 2007 17:16 GMT
To get to my article it is first necessary to visit my web site
'www.dinosaurtheory.com'.  Just type this in at the top of the page of
your web browser and hit enter.

I appears that you do have good questions and comments.  Your
statements about the Indricotherium, giraffes, and blood pressure are
all on target.  You will find the answers to most of your questions
either in my web site or in my article.

The article is twelve pages long and yet this is not nearly enough to
explain the theory.  It is really only a partial summary of the theory.
Twelve pages is not enough to get to issues such as your question
about Indricotherium and so that is why I am writing a book that
explains the theory.  My intention is for the book to come out in the
fall of 2007.

Thank you again for your comments.

David Esker

> I can't figure out how to get to your article and I imagine others will
> have similar problems.  Why not post a summary of your theory?
don kenney - 10 Jan 2007 15:31 GMT
***To get to my article it is first necessary to visit my web site
'www.dinosaurtheory.com'.  Just type this in at the top of the page of
your web browser and hit enter. ***

Didn't have any trouble finding or navigating the website.  Problem was
(and is) that nothing there including the 'Request Article' link took
me anyplace where I could read, download, or request said article.  I'm
using Firefox.  Could you have used some sort of wierd HTML that only
works in Internet Explorer?
esker_phys@pcisys.net - 10 Jan 2007 21:30 GMT
> ***To get to my article it is first necessary to visit my web site
> 'www.dinosaurtheory.com'.  Just type this in at the top of the page of
[quoted text clipped - 5 lines]
> using Firefox.  Could you have used some sort of wierd HTML that only
> works in Internet Explorer?

Once you click 'Request Article', you can write me a short note or not,
but then send me the e-mail.  Once you send an e-mail to me, the system
will automatically send an e-mail back to you that has an attachment
containing the article.

I am not really a computer person, but I would think that it should
work for everyone's system.  If you did not send me an e-mail, then
that would be the reason that you didn't get the article.
deowll - 13 Jan 2007 06:15 GMT
> I can't figure out how to get to your article and I imagine others will
> have similar problems.  Why not post a summary of your theory?
[quoted text clipped - 26 lines]
> musculature required to raise and lower a neck that long to someone
> better equipped to comment).

Some had what was most likely an elastic ligament in the neck. Acted like a
rubber band so not much muscle was needed.

> ===
>
[quoted text clipped - 28 lines]
>> much more.  Enjoy the article and try not to lose too much sleep
>> thinking about it.  I am David Esker and I will rock the science world.
William Wingstedt - 08 Jan 2007 18:36 GMT
>Over three hundred and fifty years ago Galileo wrote about scaling
>properties.  He said that as animals get bigger their bones become much
[quoted text clipped - 20 lines]
>much more.  Enjoy the article and try not to lose too much sleep
>thinking about it.  I am David Esker and I will rock the science world.

It seems that all that is left is to describe the mechanism
responsible for the increased atmospheric pressure and possibly, what
caused it to change towards its present value, which may have led to
the demise of the giant animals of that time. I wonder what other
record there might be of a more dense atmosphere since it does seem to
explain several observations. I had mistakenly thought atmospheric
pressure to be a function of a planets mass, but considering the
atmosphere of Venus, a generally Earth-sized planet, is 90 times as
dense, I see that is not true.
Larry Caldwell - 09 Jan 2007 05:42 GMT
> It seems that all that is left is to describe the mechanism
> responsible for the increased atmospheric pressure and possibly, what
> caused it to change towards its present value, which may have led to
> the demise of the giant animals of that time.

The largest animal ever to live on the planet is currently alive and
well, breathing the same air we breathe.

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William Wingstedt - 09 Jan 2007 13:50 GMT
>> It seems that all that is left is to describe the mechanism
>> responsible for the increased atmospheric pressure and possibly, what
[quoted text clipped - 3 lines]
>The largest animal ever to live on the planet is currently alive and
>well, breathing the same air we breathe.

True enough, though it is supported by the bouyancy provided by the
ocean. The issue here is land animals.
Larry Caldwell - 09 Jan 2007 15:38 GMT
> >> It seems that all that is left is to describe the mechanism
> >> responsible for the increased atmospheric pressure and possibly, what
[quoted text clipped - 6 lines]
> True enough, though it is supported by the bouyancy provided by the
> ocean. The issue here is land animals.

There is no issue at all.  The oxygen to the brain thing is easily
disposed of by anatomy.  Long necked sauropods didn't keep their brains
in their heads.  Instead, they had two brains, the larger of which was
located at the base of the spine.  It is also quite likely that the
circulatory system made some compensations, probably by using the
swallowing contractions to move blood up the neck. That could have
evolved into a simple 2-chambered secondary heart.  We will probably
never know, because soft tissue has not survived.

What has not changed is the atmosphere, at least since the
Carboniferous.  

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William Wingstedt - 10 Jan 2007 04:00 GMT
>> >> It seems that all that is left is to describe the mechanism
>> >> responsible for the increased atmospheric pressure and possibly, what
[quoted text clipped - 18 lines]
>What has not changed is the atmosphere, at least since the
>Carboniferous.  

That is contrary to what little study I have done (I don't plan on
making this my life's work) and I would actually be more surprised to
find there has been no change. I see that CO2 & O2 levels have
fluctuated quite a bit since then. While you have described what is
quite likely, probable and what we may never know, I was hoping to
find a smoking gun, but how is one to determine what record there is
of something so ephemeral as the atmospheric pressure, even more so
than the soft tissue we both lament. I found two techniques that may
help. One was the use of fossil stomata and their response to
pressures of CO2 to measure the altitude of the Sierra Nevadas in
ancient time. Another was the use of bubbles in lava that could
indicate what the atmospheric pressure was at the time of its
deposition, accurate to within 0.10 bar. I think that was also used to
measure altitude by assuming a standard pressure. Perhaps if one could
mask the data by using an independant measure of altitude in order to
gain an absolute measure of atmospheric pressure, we may have
something useful.
esker_phys@pcisys.net - 10 Jan 2007 07:09 GMT
Hi William,

In your first posting you said something about the larger the planets
having the thicker atmosphere.  This statement is true.  The present
Earth is unique in breaking the rule.  But during the Mesozoic era (the
age of the dinosaurs) the Earth did have the thickest atmosphere of the
four terrestrial planets.  Then the order of the thicknes of the
atmosphere was the same as the mass of the planet: Mercury, Mars,
Venus, Earth.

As far as finding a smoking gun or evidence of a previous denser
atmosphere, it may seem that this might be difficult to prove but
instead I believe that you will be amazed by all of the evidence.

Also you made a statement about the mechanism of how this change took
place.

I have solutions, along with the supporting evidence, for all of these
issues.
However I think that it would be best that I focus on completing my
book on the subject as the best way to share this information with you
and everyone else.  The bad news to this is that it will be several
months until my book is published. Sorry!

For now, I would be interested in knowing your thoughts about my
website dinosaurtheory.com and the article 'the solution to the big
dinosaur problem'.

David

>William Wingstedt wrote:
>While you have described what is
> quite likely, probable and what we may never know, I was hoping to
> find a smoking gun, but how is one to determine what record there is
> of something so ephemeral as the atmospheric pressure, even more so
> than the soft tissue we both lament. >
William Wingstedt - 10 Jan 2007 15:20 GMT
>Hi William,
>
[quoted text clipped - 19 lines]
>and everyone else.  The bad news to this is that it will be several
>months until my book is published. Sorry!

Very well, I'll be patient and look forward to seeing your book.

>For now, I would be interested in knowing your thoughts about my
>website dinosaurtheory.com and the article 'the solution to the big
>dinosaur problem'.

I approached it very skeptically, but found it to be interesting and
thought provoking. Good luck in all of your endeavors...

>David
>
[quoted text clipped - 4 lines]
>> of something so ephemeral as the atmospheric pressure, even more so
>> than the soft tissue we both lament. >
George - 10 Jan 2007 09:36 GMT
>>> >> It seems that all that is left is to describe the mechanism
>>> >> responsible for the increased atmospheric pressure and possibly,
[quoted text clipped - 37 lines]
> gain an absolute measure of atmospheric pressure, we may have
> something useful.

Atmospheric concentrations of carbon dioxide in the Early Carboniferous
Period were approximately 1500 ppm, but by the Middle Carboniferous had
declined to about 350 ppm - comparable to average CO2 concentrations today.
Earth's atmosphere today contains about 380 ppm CO2 (0.038%). Compared to
former geologic times, our present atmosphere, like the Late Carboniferous
atmosphere, is CO2- impoverished. In the last 600 million years of Earth's
history only the Carboniferous Period and our present age, the Quaternary
Period, have witnessed CO2 levels less than 400 ppm. So the issue, as I see
it, is likely one of figuring out the relative change in CO2 concentrations
over time, since it has apparently fluxiated quite a bit over time. We know
what the concrentration is now, and what the current pressure is, as well
as what it was in the early carboniferous period.  It stands to reason that
we should be able to figure out what those concentrations were during the
mesozoic (if that already hasn't been done), and thereby estimate what the
atmospheric pressure was (accounting for changes in other gas
concentrations as well, naturally).  I'm not an expert in this particular
field either, but it seems like this would be a good place to start.

Doing a web search, I find that Berners' "results show a similar overall
pattern to those for GEOCARB II: very high CO2 values during the early
Paleozoic, a large drop during the Devonian and Carbonifer- ous, high
values during the early Mesozoic, and a gradual decrease from about 170 Ma
to low values during the Cenozoic. However, the new results exhibit
considerably higher CO2 values during the Mesozoic, and their downward
trend with time agrees with the independent estimates of Ekart and others
(1999)."

So if the atmospheric pressure was high, the elevated CO2 levels may be
part of the reason.  The questions in my mind are was the pressure high
enough to account for large land animals?  Why would higher pressure
facilitate larger animals as opposed to an increase in oxygen levels?
Berner, for instance showed that O2 was higher during the mesozoic (when
these big animals were evolving) than now
(http://www.pnas.org/cgi/content-nw/full/96/20/10955/F2).  of course, it
was much higher 300 million years ago, but then, there weren't all these
critters running around on the continents then, either. And also, what
would high atmospheric CO2 concentrations do to their metabolisms?

George
 
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