Tracking Dinosaurs
The problem with tracking
dinosaurs is “what happens when you find one”?
The day that I was at the
dinosaur track site, the wind was gusting to over 40 miles per hour. As the area
is sandy desert, this amounted to being painfully sand blasted. I would really
like to return to the site to study and measure the tracks in more detail –
hopefully, it will be a day without the strong winds.
The first thing about the location
that caught my attention was the lack of controls or security for the fossils. I
suspect that there are very few dinosaur track sites where one can actually walk among the artifacts. The second thing that becomes immediately apparent is
the number of fossilized tracks; there are literally hundreds of them.
Dinosaur tracks are
considered to be “trace fossils”, also referred to as ichnites or ichnofossils.
Trace fossils are formed while the ancient animal is still alive.
As a tracker, it was exciting
to see a number of successive prints just waiting to be followed. One set of
prints I found had at least seven consecutive footfalls. In the jargon used by
the scientists, a series of two or more consecutive tracks is called a
“trackway”. While we are discussing jargon, “Paleoicnologists” is the term used
for the scientists who study these ancient trace fossils.
While checking out the stride
and straddle, it is quickly observed that the stride is quite long. According
to formulas developed by
R. M. Alexander and others (Alexander, 1989) the estimated speed of travel can
be calculated by comparing the length of the footprint to the pace distance.
Basically, if the length of the pace (distance between successive prints) is
approximately four times the length of the actual track print, it indicates
that this animal was running. Although this trackway’s prints were not quite
the four to one ratio, it is close enough to consider that this animal was
moving quickly.
Subsequent research indicates
that the tracks were made by a three toed, bipedal, meat eating Theropod from
the lower Jurassic period (between 199.6 and 175.6 million years ago). There were
a number of similar tracks of varying sizes in the area ranging from eight to fourteen
inches long with strides reaching up to about four feet. It was interesting to
see that there was not much straddle. This would indicate a fairly narrow
pelvic girdle.
The foot falls were neutrally
aligned (no toe in or out). It would be interesting to find out if a dinosaur’s
gender can be indicated by “toe-in” like with gender differentiation of ungulates
- such as deer.
With so many unanswered
questions, the field of dinosaur tracking is certainly worth investigating
further. However, it really doesn’t
matter what your specialty is in tracking.
If it is true that “trackers” track, then we should be able to study any
track and get a better understanding of what made the “sign”. You don’t have to
be a scientist to study fossilized dinosaur tracks, just a tracker.
Just imagine tracking something
that existed 200 million years ago…unbelievable. But after all…Adventure is
where you find it.
Bart Bjorkman
Northern Tracker
One of the best sites that I
found on the internet about tracking dinosaurs is by Glen J. Kuban
www.paleo.cc/paluxy/ovrdino.htm