Showing posts with label research. Show all posts
Showing posts with label research. Show all posts

Sunday, April 12, 2020

Mucrosprifier mucronatus from the Moscow formation

One of the most recognizable Brachiopod genus that can be found in the middle Devonian is Mucrospirifer. Below is a specimen of M. mucronatus from the Windom shale member of the Moscow formation. It's a wide hinged shell, often with the hinge line extending farther beyond the main body out into points. This gives the shell a wing like appearance and a friend of mine once told me his daughter called them fossil butterflies. The long hinge line is thought to provide stability for the shell on muddy surfaces where there was not as much of a hard substrate to attach to.

Mucrospirifer is so named due to it's "mucronate" appearance (mucronate is an adjective that means "ending abruptly in a short sharp point or 'mucro'").  That description is based on specimens that have the margin of the shell meeting the hinge line at an acute angle rather than a rounded appearance.The specimen below illustrates that habit well on the right side of the specimen.



There are many different Mucrospirifer species that I have collected from the middle Devonian deposits such as M. arkonensis, M. prolificus, and M. thedfordensis.

But it seems nearly all of the above species were recombined in 1964 by John Tillman ("Variation in Species of Mucrospirifer from Middle Devonian Rocks of Michigan, Ontario, and Ohio", John R. Tillman, Journal of Paleontology, Vol. 38, No. 5 (Sep., 1964), pp. 952-964) into M. mucronatus with the exception of M. thedfordensis. Tillman remarked that "M. thedfordensis (Shimer & Grabau)
differs from M. mucronatus (Conrad) in having a U-shaped to V-shaped sulcus, never with a flattened floor; a low moderately convex fold, never with flattened surface."

Finally, here is an example of M. mucronatus from the Silica shale.

This specimen was found at a borrow pit on Deep Springs Road in Madison County, NY which exposes the Windom shale member of the Moscow formation (middle Devonian in age, Givetian stage.)

Sunday, September 29, 2013

Pentamerella (?) from Alpena, Michigan

A few weeks ago I posted the photo's below on the Fossil Forum in the hopes that someone would recognize the fossil and help me name it. You see, it came into my collection as part of a lot of material that was labelled "Alpena, Michigan". That description covers a large area and several geologic formations so if I can't recognize the specimen I have to go digging for info. Here are some of the pics I took of the specimen:

Brachial valve

Anterior

Pedicle valve

Posterior

 Right profile with pedicle valve on top

 Left profile with brachial valve on top


After I posted them on the forum one member, Fossilcrazy, suggested it might be Camarotoechia pauciplicata based on David M. Linsley's "Devonian Paleontology of New York" (Pg.188 Plt. 83 Items 1-5). This seemed like a good fit except that my specimen lacks a fold and sulcus (the divot that is often seen in the middle of some brachiopods).

Another member, Plantguy, took it upon himself to reach out to some experts and came back with the following:

Dr. Lindsey Leighton, of the University of Alberta, responded:
I have collected a lot of brachs from the Devonian of the Alpena region, as well as Ontario and New York, and I have never seen that particular brachiopod. It does not look like a typical Camarotoechia, but it is possible that the species is atypical for the genus. Camarotoechia, by definition, should have a fold and sulcus present the length of the brach, and based on the photos, I don't really see a fold and sulcus at all. Similarly, I don't see any costae (ribs), which again, is part of the genus definition. But this could be that I can't see the relevant features on the photo. The combination of weak to absent fold and sulcus, and the lack of costae, is a little weird. My best guess is that it is not a rhynchonellide at all, but something in the Pentamerida, possibly some odd species of Pentamerella or Gypidula, but it doesn't quite look right for either of those two genera either. There are leiorhynchids that have a more or less naked (lacking in ornament such as ribbing) umbonal area and few plicae, so it might still be a rhynchonellide of some sort.
Dr. Leighton suggested contacting Dr. Jed Day, of Illinois State University, who subsequently reviewed the pictures and came back with this:
Your specimen appears to be crushed near the posterior end of its lateral margin and may be a juvenile specimen of one of two things I know of from eastern side of the Lower Peninsula area. The only things I know of that look like the specimen (s) you show in the photos are from the Ferron Point (Pentamerella lingua, Imbrie, 1959) and Norway Point (Pentamerella pericosta, Imbrie, 1959) formation quarry and natural exposures in Alpena County (See old Guidebook series, Ehlers and Kesling, 1970) . There are a number of other pentamerids that have been described from the west side of the LP that also resemble the specimen described in the older litherature (Imlay, etc.). There also rhynchonellids that it might be, especially Eumetabolotoechia.
Here is  specimen of P. lingua from the Ferron Point Fm. on the Michigan Basin Fossils website:
http://michiganbasinfossils.org/viewrecord/1506. They have a specimen of P. pericosta as well: http://michiganbasinfossils.org/viewrecord/1508. The former appears to be the closest match to what I have although the width of my specimen is less than those pictured. Maybe that is because part of the one side is slightly crushed or this is a juvenile specimen.

In any case this has been an interesting mystery and may not yet be solved. For now I am labeling my specimens as Pentamerella lingua.

Wednesday, March 20, 2013

500th blog post - A new method for me to find fossils

I noticed today that this will be my 500th post on the blog. That means I've been regularly posting to this blog for the last three years. Well, not a full three years since my first post was on May 22nd, 2010. This is an outlet for me to express my interest in fossils, catalog my collection and coalesce my thoughts and research into a useful medium.  Here's to the next 500 posts (and many more)!

I'm not going to wallow in self congratulatory pomp and circumstance. Instead I have some new toys to help me find fossils. It's a set of 6" diameter sieves to screen soil and eroded rock for microfossils.


There are six screens plus a bottom to catch the water/leftover residue. Each screen has a mesh with a different number of spaces per inch. They start with a #5 screen (fave holes per inch)...


... and include a #10 screen...


... a #35 screen...

... a #60 screen...

... a #120 screen...

... and a #230 screen (230 holes per inch)...

Through experimentation I have found that I don't really need the first two or last two screens for what I'm after. I generally only use the #35 and #60 screens to look for Ostracod fossils. Anything that the larger spaced screens would catch would be spotted with my naked eye while anything that fell through to the smaller screens would need a legitimate microscope to view.

I did buy a stereo microscope but it only has a 10x and 30x settings with eye pieces that can alter the magnification to 20x and 60x.



It's called a dissecting microscope and is, like the name states, more often used for examining dissected animal, plant and soil samples.

I also bought a rig and adapter so that I can use my camera to take pictures of my finds.


So expect to see more microfossils show up in my blog posts in the future. Right now I am sorting through residues from the Silica Shale, Arkona Shale & Centerfield Mbr. of the Ludlowville Fm. It is a nice activity to do in the winter when you can't go outside and collect macrofossils.

Saturday, December 10, 2011

Plectatrypa from Lockport, NY

When exploring a new rock formation and picking up fossils you often find some that are somewhat abundant but you have no idea what they are. It then follows that you spend time asking others for info or searching through books trying to find a match. The specimen below, from the Irondequoit limestone Rochester Shale near Lockport NY, is just such a troublesome fossil. While it has required some research to find information about the fossils that are found within the Irondequoit limestone Rochester Shale are well documented. This does not always cover every instance though and it took until I read through a book called "Paleocommunities—A Case Study from the Silurian and Lower Devonian", A.J. Boucot and J.D. Lawson, editors, 1999, Cambridge University Press, Cambridge. It had a chapter that described the brachiopod community that can be found within the Irondequoit limestone/Rochester Shale. In the list it has Plectatrypa sp. as a common member but I was having a hard time finding any pictures of specimens to compare mine to. Then I stumbled across this page (plates Plates XVIII & XXII) which is part of the "Paleontology of Kentucky" by Willard Rouse Jillson that was published in 1931. The examples illustrated looked similar to what I had found and were from the Silurian (as is the Irondequoit limestone Rochester Shale which is falls within the Wenlock series, Shienwoodian stage) I think I have a match.

Which brings us to the specimen that I found and am naming Plectatrypa sp.

Pedicle valve

Anterior

Brachial valve

Posterior

Profile

I think this specimen is also a Plectatrypa.
Pedicle valve

Anterior

Brachial valve

Posterior

Profile


Hopefully the research I have done resulted in the correct name being assigned to the fossil and will be helpful for others searching to examples.