Great Plains’ past hidden in plain sight
By NET News
July 9th, 2014
Lincoln, NE — Happy Jack Chalk Mine is about an hour north of Grand Island on highway 11. The mine sits under a hill overlooking the Loup River. Jesslyn Weiner has been a tour guide there for five years and she takes me into the mine through a shack at the foot of the hill.[audio:https://kvnonews.com/wp-content/uploads/2014/07/Fossil-Burrows-070314-KVNO02.mp3]
â€œWe do have lights in here, but this first oneâ€™s burned out and itâ€™s not one we can fix. And these are the burrows,â€ Weiner points to a dark grey balloon-shaped rock embedded in the stark white rock of the mineâ€™s wall. Less than a foot away, there’s another one. Weiner points out another one, â€œAnd this is just one them burrows but it looks like a rabbit. Can you see its ears?â€
At the mine entrance, there are at least four I can see without turning my head. These burrows are all over the ceilings and walls in the 6000 square foot mine. It wasnâ€™t until recently that they became a regular part of the tour. In 1997, Happy Jack reopened as a privately owned tourist attraction. In 2002, the mineâ€™s owners invited University of Nebraska Lincoln geologist Matt Joeckel to visit and give tour guides some background on the mineâ€™s geology. Joeckel expected to talk about the chalky rock, called diatomite, that makes up the mine, but he got a surprise when he walked in.
â€œWhat it amounts to is the minute we walked into the mine we recognized the features on the wall as being fossil burrows. We picked them out right away,â€ Joeckel said.
According to Joeckel, rodents dug the long, nearly vertical tunnels and large chambers into the soft rock in the mine about five million years ago. Sometime later, sand washed in and filled in the burrows, helping to preserve them as fossils. Even though the burrows have always been there, Joeckel didnâ€™t know they were there until that first visit in 2002.
Since then, Joeckel and his colleague Shane Tucker, a paleontologist for the University of Nebraska Museum, have mapped out the locations of all the burrows in the mine. Which wasnâ€™t easy. Parts of the mine are cramped and narrow, and Joeckel is a little claustrophobic. Tucker remembers when they had to start photographing the ceiling. â€œSo we brought one of the museum carts and Matt lay down on his back. He had the light and was looking up,â€ Tucker said. â€œAnd I would push him.â€œ
â€œIt sounds like that would be great fun, for me, lying on my back on this little 4-wheeled cart. But it wasnâ€™t. It was more like a medieval torture chamber,â€ Joeckel said.
The first thing Tucker and Joeckel wanted to do was try and figure out what kind of animals made these burrows Tucker says they sifted through 500 pounds of sediment from the mine looking for body fossils. What they found fits into the palm of one hand.
â€œOut of the twenty-some different body fossils we got from there, six teeth were well-preserved. Soâ€¦not great,â€ Tucker said.
But the burrows themselves are just as important as body fossils to identify what made them. Tucker and Joeckel made a silicone mold of one burrow to create a plaster replica they could study back at UNL.
â€œWe have an exact carbon copy of what we saw at the diatomite mine.Â And in some portions of the wall you could see the striations, these paired grooves much more easily,â€ Tucker said.
Those grooves are evidence of ancient rodents using their top teeth to anchor into the rock and gnawing with their lower teeth to dig. Those grooves and the burrowâ€™s general shape suggest a kind of ground squirrel, like modern prairie dogs, built the burrows. Joeckel says these rodents may have started spending more time underground in response to ancient forests disappearing and open grasslands, like the Great Plains, forming.
â€œWhy would they do that? Well, open grasslands are a somewhat harsh environment. There could be prairie fires. There could be extremes in temperature. So weâ€™re seeing a snapshot of the emergence of the modern grassland environment which is no small thing,â€ Joeckel explained.
In a way, these burrows are a witness to the last great period of climate change â€“ a time of global cooling and drying, right before the most recent Ice Age. We have general idea of what the earth was like 5 million years ago, but not a good idea of specifics, like what Nebraska was like then. Joeckel says itâ€™s hard to find rocks from that specific time period in the state so these burrows can help fill in those gaps.
â€œWeâ€™re looking through a glass darkly at an emerging world. There are a lot of things we donâ€™t know.â€
For instance, we donâ€™t really know how different animals and plants responded to that cooling and drying period right before the Ice Age. The burrows are solid evidence of how one population reacted to that change.
Joeckel and Tucker are hoping the burrows can tell them about small mammal evolution on the grasslands and about the formation of the Great Plains ecosystem as we know it today.
â€œAs is usually the case with these kinds of geologicalÂ studies, probably raises more questions than it answers. I personally find that comforting,â€ Joeckel said. â€œI donâ€™t think I want to know everything. I think I want to be in the business of always trying to come up with interesting ways of approaching an understanding of the history of the planet.â€
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