I am a fossil collector.
Ever since I was a small child I have been collecting fossils. In fact, I can trace my own fascination with biology directly to my discovery that the very house in which I lived (actually a trailer back then), was set upon land literally made of these long dead and formerly ocean-dwelling ancestors and distant cousins. I’ll never forget the awe that crept into my little brain as I tried to imagine enormous oceans covering my forested Ozark mountains.
When I was very young, my Mamaw (paternal grandmother) gave me a simple large toolbox for Christmas – a toolbox with a myriad little compartments intended for the sole purpose of housing my growing “rock collection.”
For years I filled this box and a couple more with fossils, rocks, gems, shed snake skins, feathers, arrowheads, seashells, and all manner of relatively non-decomposable animal and plant remains – almost all of which I found myself.
The time came when I was not content to let my collection sit in toolboxes in a closet. Thus I built a shadowbox coffee table during graduate school (with super thick glass so my cats could leap onto it from 10 feet away without smashing my fossils…er…the glass and themselves). Now my collection fills my coffee table and almost every bookshelf in my home.
I’ve amassed a decent collection – I’m proud of it anyway, though any paleontologist or geologist would almost certainly laugh at it. Most of them are simple ocean invertebrates, as most of them came from Carboniferous Period limestone of the Ozark Mountains (the entire region is pretty much made of pure crinoids).
All of the above being said, I’m a bit ashamed to admit that I don’t know that much about many of my fossils.
Thus, I am starting this series of posts to catalog my entire collection and to see what the experts out there can teach me and all of us about some of our long lost branches of life. Please, if you can add any information whatsoever, it would be much appreciated – i.e. taxonomy, factoids, comments, conjecture, anything. And please point out if I have identified anything incorrectly – a very real possibility.
For this first installment, I am going to begin with my most recent additions – all found this weekend in Bella Vista, Arkansas where I returned for my mom’s wedding.
A hat tip goes out to my four nieces (ages 9 to 12) for helping me find them.
Location: Bella Vista, Benton County, Arkansas

Bella Vista, AR fossil site (within 30 meters). Click to go to Google Maps version. Fossils found mostly in gravel uplifted by roots at the bases of trees.
Fossils
What I know: based on my limited understanding of the region’s geology, these rocks are primarily limestone from the carboniferous period (and I believe they are towards the boundary between Pennsylvanian and Mississippian – but I could easily be wrong. I know very very little about geology).
Note: You can click on all images for higher res/quality images. These are highly compressed for bandwidth. I’ve tried to give multiple views of each fossil.
#1 – Crinoid
#2 - Productid Brachiopod – Order Strophomenida
Update: information provided by Chris Nedin, of Ediacaran: “looks like a productid brachiopod. Order Strophomenida, Suborder Productidina. They can be distinguished by being large, very rounded, with a thick, heavy shell, and along the top, a very straight hinge line, with almost nothing appearing above the hinge line. An example is here at image 408.”
#3 – Spirifid Brachiopod – Order Spiriferida
Update: information provided by Chris Nedin, of Ediacaran: “an internal mold of a spirifid brachiopod, Spiriferida, Suborder Spirifieridina. The shell has been filled with sediment and that has hardened. Then the original shell has dissolved away, leaving the sediment inside, which is what you see. The shape is caused because the shell tapers down to a point away from the centre, and curls somewhat. An example is here.”
#4 – Rhynchonellid Brachiopod
Update: information provided by Chris Nedin, of Ediacaran: “I think the brachiopod here is a rhynchonellid. Order rhynchonellidida. An example is here.”
#5 – Spirifid Brachiopod
Update: information provided by Chris Nedin, of Ediacaran: “another spirifid, this time weathered (see the spirifid link above).”
#6 – Crinoid
#7 – Possible Spirifid Brachiopod
Update: information provided by Chris Nedin, of Ediacaran: “not sure, maybe another spirifid.”
#8 – Shelly strata
I know – these aren’t exactly impressive specimens. However, I already had them unpacked and laid out so I figured I’d start with these. I definitely have some other cool ones to come in future posts.
If you know of any fossil aficionados, please send them this way, as I would really like to know at least a little bit more about my collection. If any of you end up being particular helpful, I may just send you one of my awesome limestone rocks made of pure crinoid discs (they’re much cooler than those above), assuming you don’t already have some or consider them too bland ![]()

























Sorry, I can’t help you with information on your beautiful fossils, I took a fossil identifying class and still don’t have the eye, but I just wanted to let you know I love your setup. The coffee table and everything is gorgeous, and such a nice way to show off your stuff instead of having it hidden away in a closet.
Thanks for stopping by, Alisha. Your compliments are much appreciated.
The craftsmanship of the table is not that great – but it does the job. The finish is nice and shiny at least.
Hi Daniel,
You have some nice fossils there. You should try and get some books on Ozarks fossils, I’m sure there are a number around
I can hazard a guess at some of the fossils you have.
#2 looks like a productid brachiopod. Order Strophomenida, Suborder Productidina. They can be distinguished by being large, very rounded, with a thick, heavy shell, and along the top, a very straight hinge line, with almost nothing appearing above the hinge line. An example is here at image 408.
#3 is an internal mold of a spirifid brachiopod, Spiriferida, Suborder Spirifieridina. The shell has been filled with sediment and that has hardened. Then the original shell has dissolved away, leaving the sediment inside, which is what you see. The shape is caused because the shell tapers down to a point away from the centre, and curls somewhat. An example is here
#4 I think the brachiopod here is a rhynchonellid. Order rhynchonellidida. An example is here
#5 is another spirifid, this time weathered (see the spirifid link above)
#7 not sure, maybe another spirifid.
Hope this helps.
Thank you SO much Chris! This is most definitely helpful. It’s much more satisfying to have an idea of the taxonomy of my specimens.
You realize, of course, that I will now be begging you to identify the fossils with each new post, right?
You rock!
8G7QbD comment4 ,
Irratiatus, good to see you posting again. It appears that you are in the Lower Mississippian(Carboniferous is an archaic term)Boone Formation. In the US, what the Europeans referred to as Carboniferous is Miss. for the lower units and Penn. for the upper. Now though, the International Commission on Stratigraphy recognizes the Miss. and Penn. as the appropriated nomenclature.
In the valleys around there, you can also find some Devonian(Clifty Lm and Penters Chert).
The reason for the post is that it appears that in the second photo-about middle ways a little down from center(if cartesian coordinates -2 on y axis), you have an impression from a primitive tree-like plant(lycopod).It appears to be a Lepidodendron sp… very cool! They are from the Penn period.
In your area, as with most of what was this continent, there was a time when the seas regressed the continent during the Late Miss. This led to erosion for about 5 million years until the seas again transgressed. This is when the Penn sandstones and shales were deposited in the area.