Showing posts with label Colonial National Historical Park. Show all posts
Showing posts with label Colonial National Historical Park. Show all posts

Sunday, May 29, 2022

Recent Work from the National Park Service Paleontology Program

My day job is with the Paleontology Program of the National Park Service, and I thought you might like to see some of the work we've put out over the past few months. First up is the Spring 2022 issue of the Park Paleontology newsletter. For this issue, we have articles on:

Next, a couple of articles have just come out in the latest volume of the New Mexico Museum of Natural History and Science Bulletin series, both focused on Quaternary cave paleontology of specified parks in the southwest. Hodnett et al. (2022) describes previously overlooked bones from Grand Canyon National Park as specimens of the "American cheetah" Miracinonyx trumani. Meanwhile, drawing on the Carlsbad Caverns National Park paleontological inventory published a few years ago, Kottkamp et al. (2022) discusses the Pleistocene vertebrate record of the park's various caves.

Finally, public versions of our four latest park-specific paleontological inventory reports are also available to view and download. For just four parks, they feature a wide range of types of fossils, geology, and geography. They are:

References

Hodnett, J. P., R. White, M. Carpenter, J. Mead, and V. L. Santucci. 2022. Miracinonyx trumani (Carnivora; Felidae) from the Rancholabrean of the Grand Canyon, Arizona and its implications on the ecology of the “American cheetah.” New Mexico Museum of Natural History Bulletin 88:157–186.

Kottkamp, S., V. L. Santucci, J. S. Tweet, R. D. Horrocks, and G. S. Morgan. 2022. Pleistocene vertebrates from Carlsbad Caverns National Park, New Mexico. New Mexico Museum of Natural History and Science Bulletin 88:267–290.

Sunday, August 1, 2021

Practical applications of Chesapecten, early 19th century

"Fossil pectens of a large size, some of them ten inches wide, are found abundantly in the lower part of Virginia. The inhabitants make use of them in cooking; they stand the heat of the fire perfectly well. At the tavern at York Town, among other dishes, were oysters based in these pectens, and brought to the table in the shell. I wanted the company of a few scientific friends to enjoy the treat. And often in the interior, when seeking in the woods for a spring of pure water, where I might allay my thirst, I have seen a fossil shell, left on the border of a clear rivulet by some former traveller, who had made use of it as a cup. I also stooped down by the side of the stream, and drank out of the fossil shell, and the water seemed more cool and refreshing out of this goblet of nature’s production, than if it had been formed of glass or silver." (Finch 1833)

Chesapecten madisonius, not quite as famous as C. jeffersonius but still quite nice.

References

Finch, J. 1833. Travels in the United States of America and Canada. Longman, Rees, Orme, Brown, Green, and Longman, London, United Kingdom.

Sunday, March 7, 2021

Proboscidean update: the Williamsburg mammoth (or mastodon)

Leaving titanosaurs aside for the moment...

A couple of times now, I've featured inventories of National Park Service proboscidean fossils: mammoths, mastodons, and so forth. One of the records that's been stuck as questionable is an 1811 report from the area of Colonial National Historical Park. To quote from the most recent published assessment, in Mead et al. (2020):

“The Williamsburg-area mastodon was first reported in 1811 (Anonymous 1811). The details vary from report to report, but apparently the bones were found 10 km (6 mi) south (Anonymous 1811) or east (Mitchill 1818) of Williamsburg on the south bank of the York River. It is unclear where the former location would be, but the latter is potentially within COLO [Colonial National Historical Park], in the vicinity of Bellefield Plantation and the mouth of Indian Field Creek. Anonymous (1811) reported that the site was a few yards within high water near the home of Gawin Corbin. The fossils include 2 tusks, 2 vertebrae, 1 pelvis, 1 femur, and partial mandibles with 7 associated teeth (Mitchill 1818). Given the presence of molars, it is surprising that Mitchill (1818) identified the specimens as mammoth, yet Hay (1923) reported them as a mastodon (Mammut). Hay (1923) reported that the bones were probably destroyed in the 1859 fire at the College of William and Mary. Clark and Miller (1912) refer this specimen to the Pleistocene of the Talbot Formation (a now-obsolete name)."

I and others have made attempts over the past few years to determine who the Gavin Corbin in question was and where his property was located, most recently as part of the Colonial National Historical Park paleontological inventory currently being reviewed. The primary issue has been the numerous Corbins who have lived in this region, including multiple Gawin Corbins. In such a case, sometimes you have to trust in serendipity, and I can now state that I'm practically certain the answer is at hand. The man in question is Gawin Lane Corbin (1778–1821), and the property is the “Kings Creek” plantation, now within the U.S. Navy's Cheatham Annex just north of the Colonial Parkway.

This was the kind of thing where it was helpful to have some experience in genealogical research. It wasn't enough to have a good candidate for the name; there also had to be a way to track the location. In this case, "Kings Creek" has a lengthy history, beginning as "Utimaria" in 1630 and passing through various hands until being sold to Corbin's father in 1790 (Tyler 1894; Anonymous 1913). Later the area was known as Penniman, and eventually the Navy's Cheatham Annex. Importantly for us, we also know that the Ringfield and Bellefield (or Bellfield, or Belfield) plantations were active in the same time frame as the fossil discovery, on what is now the NPS side of Kings (or King’s, or King) Creek. With this knowledge, we can be certain than any mammoth or mastodon found near the home of Gawin Corbin on the York River shore was found in what would now be part of the Cheatham Annex, and therefore near but not within the historical park. (On the other hand, if anyone from the Annex is reading this, it looks like there's a mammoth or mastodon in your history.)

Presumably Corbin had some idea of the significance of the find for it to have been collected in the first place. He was certainly in a position to have been exposed to discussion of such fossils, having social standing and a college education (William & Mary alum; Anonymous 1922) at a time when fossils of mammoths and mastodons held an unusual fascination beyond their scientific value.

Near the mouth of King's Creek, looking north toward Penniman Spit.

References

Anonymous. 1811. Curious discovery [elephant bones from York River, Williamsburg, Virginia]. Philadelphia Repertory 2:87–88.

Anonymous. 1913. Notes from the records of York County. William and Mary College Quarterly Historical Magazine 22(2):73–89.

Anonymous. 1922. The Corbin Family (continued). The Virginia Magazine of History and Biography 30(4):403–407.

Clark, W. B., and B. L. Miller. 1912. The physiography and geology of the Coastal Plain province of Virginia. Virginia Geological Survey Bulletin 4:13–222.

Hay, O. P. 1923. The Pleistocene of North America and its vertebrated animals from the states east of the Mississippi River and from the Canadian provinces east of longitude 95 degrees. Carnegie Institution of Washington, Washington, D.C. Publication 322.

Mead, J. I., J. S. Tweet, V. L. Santucci, J. T. Rasic, and S. E. Holte. 2020. Proboscideans from US National Park Service lands. Eastern Paleontologist 6:1–48.

Mitchill, S. L. 1818. Observations on the geology of North America; illustrated by the description of various organic remains found in that part of the World. Pages 319–431 in G. Cuvier. Essay on the theory of the Earth, with mineralogical notes, and an account of Cuvier’s geological discoveries, by Professor Jameson. Kirk and Mercein, New York, New York.

Tyler, L. G. 1894. Notes by the editor. The William and Mary Quarterly 2(4):230–236.