A friend of mine introduced me to the famous Salmon Creek
coprolites a few years ago when I came home from Iraq. At the time
I did not know what a coprolite was. At first glance it looked like
dog poop. I asked what it was and he told me it was fossilzed
turtle dung. I was fasinated and wanted to find some for
myself.
A few days later we loaded up the SUV and off we went in search
of some coprolites. The desitination was Salmon Creek, not far from
Toledo, WA. Once at the site it was not long before I found my
first piece of turtle coprolite. I was hooked! At the end of the
day I had my bucket full of coprolite and very proud of my little
treasures.
I was told my coprolites are from prehistoric turtles called
Turtlesaurs. Turtlesaur Coprolites are unique fossilized dinosaur
droppings and most likely from a turtle-like dinosaur that lived in
the wetlands of western Washington state between 12 and 20 million
years ago. The dung droppings are preserved by the mineral
Siderite, a carbonate of iron. Scatologists can tell a lot about
the diet of the dinosaur from studying these coprolites. Remains of
nuts, seeds and bone may be seen in the mineralized dung.
Coprolite, meaning "dung stone" , kopros means dung and lithikos
means stone in Greek, is fossilized feces. And no, coprolite does
not smell bad - it had undergone a fossilization process. Copro
means "dung," from the Greek word kopros. The ending "-lite" is a
common ending for fossil or mineral terms, coming from the Greek
word lithos, which means stone. The term coprolite was coined
around 1830.
We can learn a lot from coprolite.
Learning About Diets: Coprolites record the diet, feeding
behavior, and habitat of prehistoric animals. Paleontologists can
study the contents of a coprolite to see what one meal of an animal
consisted of. For example, if the coprolite consists of partially
digested plant material (leaves, seeds, bark, roots), the animal in
question was probably an herbivore; if the coprolite contains bits
of animal material (crushed bits of bones, sinew, claws), the
animal in question was a carnivore.
The recognition of coprolites is aided by their structural
patterns, such as spiral or annular markings, by their content,
such as undigested food fragments and by associated fossil remains.
The smallest coprolites are often difficult to distinguish from
inorganic pellets or from eggs. Most coprolites are composed
chiefly of calcium phosphate, along with minor quantities of
organic matter. By analyzing coprolites, it is possible to infer
the diet of the animal which produced them.
Coprolites have been recorded in deposits ranging in age from
the Cambrian period to recent times and are found worldwide.
However, animal excrement is easily fragmented and destroyed, so
usually has little chance of becoming fossilized.
Now the debate. Is what I found really coprolite? A few
geologists dissagree that the coprolites in Salmon Creek are turtle
poop but instead are from decomposing trees. The geologists call
these fossils pseudocoprolites.
Pseudocoprolites are excrement-shaped masses of siderite and
limonite from clay-rich sedimentary rocks that range in age from
Late Permian to Holocene. These objects have been widely accepted
as being coprolites, but the ferruginous composition, absence of
internal inclusions, and scarcity of associated vertebrate remains
suggest that they may instead be pseudofossils created by
mechanical deformation of plastic sediment. Possible abiotic
mechanisms include coseismic liquefaction, intrusion of sediment
into hollow logs, or expulsion of sediment in response to gravity.
Alternatively, carbon stable isotope ratios indicate that sediment
extrusion may have been related to emission of biogenic methane
during early stages of diagenesis.
According to geologists, the Salmon Creek pseudocoprolites have
never been found to contain any trace of organic material. They
also exist in a wide variety of sizes and shapes which make it
impossible to attribute them to any single type of organism.
Furthermore, they are found highly concentrated in sediments that
have never yielded animal fossils that could serve to corroborate
their identity as dung. Overall there is a lack of evidence to
support the notion that they are fossilized animal droppings. But
if they are not true feces, then what exactly are they?
To begin with, their rust color indicates the presence of iron.
Their chemical composition is, in fact, solid iron carbonate—the
mineral known as siderite. How these mineral concentrations came to
have their distinctive shapes has been the topic of much
speculation, and at the moment there is no consensus. There are
four hypotheses, each with their supporters and detractors. Two
involve forces such as seismic liquefaction and gravitational
pressure. A third envisions a mechanism involving hollow logs with
holes through which the siderite could be forced.
The fourth hypothesis requires a scenario in which siderite mud
is situated in strata above a layer of decaying plant matter
undergoing methanogenesis—the production of swamp gas. In this
hypothesis, gas pockets would develop within deposits of
decomposing plant material underlying siderite mud which was itself
beneath a plastic layer of sediment. When the pressure build-up of
the gas reached a critical point, the strata had to “relieve
itself” by forcing a stream of gas up through the siderite mud and
the overlying sediment. It would be like the scene in the movie The
Labyrinth, in which the heroes must cross through the Bog of
Eternal Stench, the steamy swamp filled with black mud constantly
bubbling and erupting with the sounds and smells of flatulence.
The apertures through which the siderite mud would extrude
itself dilated as the pressurized materials squeezed through. As
the pressure decreased, the diameter of the aperture reduced in
size and created the distinctive pointed tips found on the
pseudocoprolites, while irregularities along the edges of the
aperture created the striations that can be found along the length
of the specimens.
To the left of the GPS is a piece of Coprolite I found at the
EC site. Coprolite comes in a varity of shapes and sizes.
Personally, I believe these are real coprolites, however I am
not a scientist or a geoligist, but I do know what poop looks like
and this looks like the real thing. Like my grandpa always said,
"if it looks like poop and smells like poop, its probably
poop..."
As I type this I'm looking at a coprolite I found in the creek
and chuckling to myself because it looks like a pile of dog waste
my dog left in my back yard.
When you visit this site, you be the judge. It looks real and I
hope someday the geologists can agree on one thing and that is
wether or not its real turtle poo.
Now here is the hard part, (no pun intended). The coprolite near
the bridge looks like the surrounding rocks on the bank. Look at
the attached pictures and take your time. The coprolites are all
over the banks. You may even find some very colorful agates while
here.
To get credit for this EC, post a photo of you anywhere near the
EC site in Salmon Creek and the bridge in the background (no photos
of just a hand) and please answer the following questions. Also
post some pictures of the coprolites you find.
1. What is the average size of coprolites you find?
2. Do the coprolites feel heavy or lite?
3. Do you think the fossils are really coprolites or
pseudocoprolites?
Cav Scout has earned GSA's highest
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PLEASE DO NOT POST YOUR ANSWERS IN THE LOG. ANY LOGS THAT
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Sources of
information for the EarthCache quoted from the Cumberland National
Historic Park. I have used sources available to me by using google
search to get information for this earth cache. I am by no means a
geologist.. I use books, internet, and ask questions about geology
just like 99.9 percent of the geocachers who create these great
Earth Caches. I enjoy Earth Caches and want people to get out and
see what I see every time I go and explore this great place we live
in.