Carboniferous

BPS members took a long road trip to roadcuts in Colbert County on August 25, where everyone found a good selection of blastoids, brachiopods, trilobites, and other Mississippian age fossils at two separate collecting sites.

Afterwards, we relaxed and cooled off in a creek on some propery owned by one of our members.

ANCIENT ALABAMA ANIMAL TRACKS INSPIRE AMATEUR FOSSIL COLLECTORS

TO DOCUMENT FINDS

"The handprints, which include long, curving toes with easily-distinguished pads on the tips, are nearly as big as my own," exclaimed Dr. Jim Lacefield of Tuscumbia. "This was a huge beast. Although I had read that some amphibians reached rather large size in the Pennsylvanian, in all my collecting in Coal Age rocks in Alabama I have never seen any that were anywhere nearly this large," he said.

Lacefield, a part-time biology and Earth science instructor at the University of North Alabama, and author of a recently published book on Alabama fossils, was describing remarkable fossil footprints of an ancient alligator-sized animal that he had collected at a surface coal mine in Walker County owned by the New Acton Coal Mining Company of Warrior, Alabama. Lacefield was visiting the mine on an outing early last year with members of the Birmingham Paleontological Society (BPS), an active group of local amateur fossil hunters who had received permission from the company to salvage fossils from the area.

The mine had been discovered only a few months earlier to be an unusually good source of fossil vertebrate trackways by Ashley Allen, an Oneonta High School science teacher who is also a member of the BPS. A student in Allen's class had alerted him to the site owned by his grandmother, Mrs. Dolores Reid. Fossils connected with vertebrate animal life (that is, animals with a backbone) are of great paleontological significance since they represent some of the most advanced forms of life that developed on Earth at the time and are usually very rare.

Since Allen's discovery, the Walker County mine has been the focus of an extraordinary salvaging effort by BPS members that has led to a remarkable cooperation with professional paleontologists. The trackways collected from the mine are of vertebrate as well as invertebrate animals that lived during the Late Carboniferous Period of Earth history, known to North American geologists as the Pennsylvanian Period. This Period dates back 310 million years to a time when much of the Earth (particularly North America and Europe) was covered with great tropical swamps that eventually laid down many of the vast coal reserves we use today. (In fact, the Pennsylvanian Period is also often referred to as the "Coal Age.") During the past 15 months, mainly through the efforts of the BPS, more than 800 track specimens have been salvaged from the residual rock piles left after the coal mining was discontinued.

According to Dr. Anthony J. Martin of the Department of Environmental Sciences, Emory University, the Walker County mine is "one of the best vertebrate track sites for the time period in question in the world." Martin is an ichnologist, a paleontologist who studies "trace" fossils, or traces of ancient activity. Tracks are trace fossils since they show what an animal was doing but not specifically what it looked like. Martin became involved in the study of the Walker County mine tracks through the insight of Steve Minkin, an Anniston geologist and BPS member who was very active in collecting trackways from the site. Recognizing the scientific importance of the tracks, Minkin proposed a series of meetings at which amateur collectors would bring all of their track finds from the mine to one place for photographic documentation and detailed inspection by professional paleontologists. The first of these events, jokingly dubbed a "Track Meet", was held on August 19, 2000 at the Alabama Museum of Natural History on the campus of the University of Alabama. Dr. Ed Hooks, Museum curator, fully supported the event and was instrumental to its success. The event was also sponsored by the Geological Survey of Alabama. A second meeting, called "Track Meet 2", was held at Oneonta High School on October 14, 2000 to document all finds since the first track meet. The third and final track meet, called "Track Meet 3", will be held on May 12, 2001 at the Anniston Museum of Natural History and will photographically document all tracks found since Track Meet 2 and since the final reclamation of the mine in December, 2000.

Although no fossils of the ancient animals that made the tracks have been found, the trackways record the dynamics of life on land nearly 90 million years before the first dinosaurs walked the Earth. According to Dr. Jack Pashin of the Geological Survey of Alabama, the tracks occur at the head of an area that was once a tidal mud flat much like the one seen today in Mobile Bay. The environment would have been far enough inland to be fresh water rather than salt water, but it would have been an area still dominated by one or more daily tides. At ebb tide, animals would walk or creep across the still wet mud and impress the tracks of their activities. The mud was soft and fine enough that even small creatures could leave well-defined tracks. The best-preserved tracks were probably impressed so deeply that they were buried before they had a chance to be altered in any significant way. Once buried, they were effectively removed from further disturbance for the next 310 million years.

The tidal flat was evidently near a rich forest of tall tree-like lycopods (primitive spore-bearing plants whose foliage resembled that of modern clubmosses), giant horsetails (plants roughly like reeds or bamboo), and tree-sized seed ferns, because among the tracks BPS members also found bark impressions, pith casts, fern impressions, and reproductive organs of a wide variety of ancient plants that are now extinct. It is known that these types of plants could only thrive in fresh-water swamps. Insect life was probably abundant in the forest, and it is significant that one insect fossil was found at the Walker County mine. Dr. Prescott Atkinson, a Birmingham pediatrician and BPS member, found a pair of 4-inch long wing impressions of an extinct relative of modern dragonflies. This is the only fossil found at the site that gives direct information on the actual appearance of a creature that lived in the area. Because of the high quality of many of the plant fossils found at the same site, Track Meet 3 will include a "Plant Fest", where the best plant specimens from the mine will be photographically documented and examined by professional paleobotanists (scientists who study fossil plant life).

Many of the tracks found by BPS members are of amphibians, animals whose modern relatives include frogs and salamanders. These tracks include striking five-toed patterns over a wide range of sizes from less than a centimeter to the size of an adult human hand. Other tracks are those of animals that may be transitional between amphibians and reptiles. Although we do not know precisely what these creatures looked like, they would have been some of the earliest vertebrates to be fully adapted to dwelling on dry land.

Tracks of other animals, mostly invertebrates, have also been found at the Walker County mine. Apparently, the area was very popular with horseshoe crabs, animals that are related more to scorpions and spiders than to conventional crabs. Today's horseshoe crabs are "living fossils", and the ancient ones that left the tracks probably looked very similar to modern ones. The complex pattern of legs on horseshoe crabs, and the way they walk in water, can explain a wide variety of tracks found at the Walker County mine. Horseshoe crabs in large numbers also left "resting traces", simple impressions of their leg patterns. Evidence also for early fish swimming in shallow areas has been found in the form of wavy tracks where it is thought that fins lightly touched the bottom. Numerous worm burrows have also been found.

All of the trace fossils found at the mine record valuable information on life in the Paleozoic ("ancient life") Era of Earth history. This Era runs from 570 to 245 million years ago, and it was during this time that life on Earth gained a foothold on land. From studies of the tracks brought to the various track meets, ichnologists have deduced that the Walker County mine area was a nursery for many of the animals living there. According to Dr. Andy Rindsberg, an ichnologist working for the Geological Survey of Alabama, the fact that the various tracks occur in a broad range of sizes whose shapes changed slightly as they grew larger points to this interpretation, which is similar to the way modern animals use tidal mud flats today. Rindsberg, along with Martin and his undergraduate student Nick Pyenson, is actively researching the tracks and the team presented talks about them in March to the Southeastern Section of the Geological Society of America.

For the BPS, the discovery of the beautiful trackways has made for a very exciting year. The amateur group, headed by Kathy Twieg of Vestavia Hills (near Birmingham), put a lot of time into salvaging as many tracks as possible before the mine was reclaimed in December. The generosity of the New Acton Coal Mining Company, in particular the enthusiasm of owner Mrs. Reid, was instrumental to the success of the venture. For many of the collectors, the great appeal of the tracks was not only because of their possible scientific value and great beauty, but also because they are more about life than about death. Unlike a pile of bones, tracks record what animals were doing when they were alive. They bring to life an era far removed in time from our own.

For Allen, the Walker County mine experience is part of what being a teacher is all about. "I try to convey to my science students the importance of communication in the scientific community," he says. "I want to be accurate in representing the principles that the scientific enterprise is based upon. Work done without proper communication is called a secret, not a discovery. I feel that any opportunity that I get to show them how to use problem solving skills, scientific reasoning, communication skills, and the ability to put things into a proper social and historical perspective is worth the effort."

The Track Meets themselves represent a rare collaboration between amateurs and professionals that could become a model for other similar finds. "Amateurs are often the source of new discoveries in paleontology," says Rindsberg, who notes that if the BPS had not learned about the site so soon after mining operations ended, any tracks exposed would either have weathered away or been re-buried when the site was reclaimed. He also notes that "if the BPS had not spent so much time looking and splitting open boulders, then the fossils would not have yielded up as much information as they have. Even with the nearly one thousand tracks and trackways that have been labeled so far, Tony Martin and Nick Pyenson have identified some specimens with unique features. If those single specimens had been missed, we would know less about the creatures that made them. At every step of the way, persistence and open-mindedness paid off in this case. I am certain that Alabama has many other surprises for us to find."

To see what some of the tracks look like, click on the following links:

Image 1: Tracks of an amphibian known as Cincosaurus cobbi, a common five-toed animal on the mud flat.

Image 2: Tracks of a larger amphibian, possibly a more grown C. cobbi.

Image 3: Tracks of one of the largest amphibians that walked on the mud flat, known as Attenosaurus subulensis.

Image 4: Tracks of a likely horseshoe crab.

This press release was prepared by BPS member Dr. Ron Buta, a professional astronomer at the University of Alabama. He can be contacted at 205-348-3792 or buta@sarah.astr.ua.edu.

Interested persons may contact Drs. Martin and Rindsberg at the following e-mail addresses:

Dr. Anthony J. Martin - geoam@learnlink.emory.uab

Dr. Andy Rindsberg - ARindsbert@uwa.edu

The following people are either quoted or mentioned above, and may also be contacted for information:

Dr. Jim Lacefield 

Dr. Ed Hooks - hooksge@longwood.edu

Dr. Prescott Atkinson - patkinso@uab.edu

by Ron Buta, Department of Physics and Astronomy

University of Alabama
Tuscaloosa, Alabama

The Union Chapel Mine is now known to be one of the best Lower Pennsylvanian track sites in North America. During December, the mine was in the process of reclamation, and the BPS returned one more time as a group to search for trackways among turned-over spoil piles in one of the most productive areas of the site. About 15 BPS members and several newcomers attended the field trip on a pleasant mid-December day.

Figure 1: Trackway of a likely arthropod. Each print is a small spot. When we arrived at the site, only one small area was not reclaimed. This particular area was one which had yielded many good tracks in the past and so we were all delighted to see that the mine workers had moved some of the old rock piles around, allowing us to see if any new material had been exposed. In spite of this, we all had difficulty finding any new high quality tracks. Nevertheless, there were still tracks to be found. I found the interesting specimen shown in Figure 1. It appears to be the trackway of an arthropod, where each track is a small roundish spot. In the significant collection of track photos which the BPS "track meets" have provided, I had not seen another set like this one. I also found the tracks shown in Figures 2 and 3.
Figure 2: Trackway of another likely arthropod, notable for its asymmetry and strong trail-dragging mark
Figure 3: Two tracks of an Attenosaurus subulensis, a common alligator-like amphibian from the Union Chapel site.
On the reclaimed areas and in the overturned area, one can still find nice plant fossils at this site. Figure 4 shows an especially nice set of ferns from a split rock. Most interesting is how strong the stem of these ferns is.   Figure 4: Strong fern impressions from a split rock.
Figure 5 shows brown ferns of the genus Neuropteris, which was common at this mine. Figure 5: Beautiful Neuropteris ferns defined by iron compound deposits.
Figure 6 shows a single large seed impression of a seed fern. This is how such seeds are often found. Figure 6: A seed impression, Trigonocarpus.
However, I found another rock in the overturned area having more than a dozen seed impressions. Several of these are shown in Figure 7. Figure 7: Part of a slab showing numerous seed impressions
The ferns they are associated with are shown in Figure 8. Jim Lacefield discusses the seeds of seed ferns on page 66 of his new book, "Lost Worlds in Alabama Rocks", and gives a wonderful general discussion of the Coal Age in Alabama and what happened to the seed ferns. Figure 8: Part of the same slab showing another seed impression among the ferns likely associated with the seeds

The reclamation of the Union Chapel Mine caps off a spectacular year of discovery for the BPS, and the Union Chapel experience marks the beginning of a remarkable cooperation between BPS amateur rock collectors and two professional organizations, the Geological Survey of Alabama and the Alabama Museum of Natural History on this new project. The more than 500 track specimens salvaged by BPS members and guests since January 23, 2000 are currently being researched by professional paleontologists. Hundreds of high quality plant fossils were also salvaged and will eventually be studied. We will no doubt be talking about the experience for years to come.

Department of Physics and Astronomy
University of Alabama
Tuscaloosa, Alabama

It was decided at the March meeting that the BPS should return to this mine once again as an organized field trip. As I have noted in previous reports, this is a site the BPS visited with great success just two months earlier. The site is rich in footprint fossils of Pennsylvanian amphibians and other creatures. Although the previous organized visit, on January 23, occurred on a rather bleak day, it was nothing like the one today. Rain fell hard all day across most of Alabama and never let up even for a few minutes. Because of the weather, only six people turned up for this outing.

Figure 1 Unusual tracks of one or two large creatures that must have been moving in very wet mud.

In spite of the weather, several of us still found nice tracks and other fossils. I show a few that I picked up here. One large set of tracks I found was lying at the bottom of a rock pile that had been thoroughly searched. After the tracks were cleaned of mud, it looks to me like they are amphibian tracks that were laid down in rather wet mud. The impressions are wide as the creatures' whole body probably sloshed in the mud. There are two sets of tracks on the main piece, and details of one are shown in the close-up.

Figure 2 Close-up of part of the previous specimen, showing likely toe prints flanking the broad body scrape.

Figure 3 Small tracks of one or more creatures that could be Bipedes aspodon. A much smaller set of tracks I found in a different area has small y-shaped prints in a bit of a random pattern. In Museum Paper No. 9 of the Alabama Museum of Natural History (authors Aldrich and Jones), a creature that produced similar tracks is known as Bipedes aspodon. At least two sets of tracks are also present on this piece. Bipedes aspodon is described by Aldrich and Jones as an animal with only two toes. Although Aldrich and Jones clearly considered the creature to be an amphibian, BPS members who found similar tracks felt they are more likely to be tracks of an arthropod.

Figure 4 Single print of Quadropedia prima, a modest-sized amphibian. At this layer, the track shows five clear toes as well as a pad. I found some other interesting and larger tracks on a large rock on the well-searched rock piles. I suspected tracks might be inside at a deeper level in this rock. The rock had interesting deposits or formations that covered different layers, but it was not clear what these features might be. After removing many layers of the rock, I did indeed find four footprints of a modest-sized creature which, according to Museum Paper No. 9, is an amphibian known as Quadropedia prima. Aldrich and Jones state that the creature is higher in the scale than most of the species they illustrated in their article, because it walked more like later reptiles. They point out the presence of a distinct pad, which we can see in the pictures I show here. The four prints could be detected at several different layers, and at least one of the prints was well-defined at all of the layers. The appearance of the prints seemed different at different layers, suggesting that some of the variety in the prints we have been finding at the site is due in part to the different layers that were exposed.

Figure 5 Two tracks of the same creature, the one at right being the same foot as in the previous picture, but the print looks different because it is at a different level. At this level, only three toes are seen, with a strong pad.

Other Notes on the Union Chapel Site January 23-March 19, 2000

The Union Chapel Mine was visited many times by BPS members and guests between January 23 and March 19. Ashley Allen brought to the February BPS meeting a huge rock with a set of excellent large amphibian prints. Bruce Relihan brought to the March BPS meeting a large stump cast of a likely Lepidodendron. The stump is more than a foot in diameter and tapers around the edges, as if it were near the bottom of the original trunk. Bruce related the heroic effort he put into getting the huge fossil by himself, which involved building a rock ramp to allow him to get it into his truck. Steve Minkin also brought to the last BPS meeting an excellent set of modest-sized tracks found by his wife.

All in all, the Union Chapel site elicited such great interest and finds that Steve Minkin asked Ed Hooks if the BPS could have a temporary display case at the Alabama Museum of Natural History in Tuscaloosa. Ed agreed to this and some of the new Union Chapel pieces may soon be on display for the public to see!