Long Pause

It's been a while since I posted anything to my blog and I apologize to my regular readers for that. This summer I was getting some work done on my house which distracted me and took away my usual backdrop for photography (the brick wall on the back of my house). It also forced me to box up all of my fossils and put them into storage since the space was needed for the contractors to work in. Additional stress came from my day job in the form of several projects that I fell behind on and had to play catch up.

The good news is that my renovations are complete and I'm caught up with the day job. In the next few weeks I will be moving my fossils into a new, larger work space and I'll be working to sort them and find new material to write about. I didn't get a summer vacation this year but hopefully I can sneak some small trips in before winter gets too cold.

In the meantime here are some pictures of finds from this spring that don't really need full blog entries:

Phacops rana molts from the Moscow Formation at the Penn Dixie site in Blasdell, NY.

The base plates and stem attachment point of an Arthrocantha sp. Crinoid from the Moscow Formation at the Penn Dixie site in Blasdell, NY.

And a small geode formed by a fossil that contains small Calcite crystals and some blades of what I think are Barite that I found in a piece of the Tichenor Limestone (bottommost layer of of the Moscow formation) along the shoreline of Lake Erie.

That's all for now, I'll hopefully be back to regular updates in the coming weeks. Thanks for stopping by!

-Dave

Inocaulis fossil from the Bertie formation of Canada

One of the odd fossils that I've found at the Ridgemont Quarry near Fort Erie, Ontario, Canada are these positive a negative specimens of an enigmatic fossil called Inocaulis plumosa. It's been something of a mystery for a number of years and has been thought to be an algae or possibly a graptolite. Well there is a new paper coming out (in Alcheringa, the Journal of the Association of Australasian Palaeontologists) that states, based on new fossils from China, that it most certainly is a graptolite (possibly a dendroid or tuboid type).

I photographed the fossils wet to better show detail.

 

Graptolites were colonial animals that lived similar lives to a coral or bryozoan in that they filtered the water for food. Most were free floating but some did attach to the substrate. They are more closely related to vertebrates than invertebrates. The fossil does show some "hairy" extensions around the periphery of the body. This is only part of what was likely a larger group of animals. The specimen was found in the Bertie formation which is Silurian (Pridoli stage) in age.

Cooksonia plant fossils from the Bertie formation of Canada

Cooksonia is one of the first recognized vascular plants. That means it had a system that allowed water and nutrients to be distributed internally. This is an important step for a plant if you are going to exist outside of a watery environment. The specimens below are individual pieces of what could be C. hemisphaerica likely before they fully produced their sporangia.

Specimen #1

Specimen #2

Specimen #3

All three specimens came from the Bertie formation (upper Silurian, Pridoli stage) in Ridgemont quarry, Fort Erie, Ontario, Canada.

Fossil Algae from the Bertie formation in Canada.

I'm a little surprised that I hadn't posted anything regarding some plant fossils I found last fall in Canada. These next few posts should rectify that starting with some humble Algae. The carbon coating on dolostone below is thought to be a fossil algae and was found in the Bertie formation at Ridgemont Quarry, Fort Erie, Canada. The Bertie formation is better known for it's Euryptid fauna but plant material is actually more rare.

This was collected last fall from the Ridgemont Quarry which is kind enough to allow collectors access to their property to prospect for fossils. The Bertie formation is late Silurian (Pridoli stage) in age and has been interpreted as a shallow lagoonal deposit.

Chonetes oklahomensis from Oklahoma

Chonetes genera brachiopods are somewhat common from the Devonian onward and they retain their Strophomenid styling. Below is a specimen of Chonetes oklahomensis from the Fayetteville shale (Carboniferous, Mississippian, Serpukhovian stage), itself a part of the Wewoka formation, of Hughes county, Oklahoma.

Pedicle valve

Anterior

Brachial valve

Posterior

Profile

Here is a group of them together.