From the Smithsonian Institution, here’s a passenger pigeon bone, specifically a left humerus (wing). the Smithsonian only identifies it as being from Bartow County, Georgia, but given the collector is attributed to “Lipps et al,” it is likely from Ladd’s Quarry. In the 1960s, Shorter College biology professor Emma Lewis Lipps excavated at this site and sent many fossils to the Smithsonian.
Pet cats, hunting dogs, and underwater mammoths: the journal Antiquity has assembled a group of recent zooarchaeology articles and made them freely available on their Online Collections page.
There’s no type of extinct mammalian megafauna we like better than the giant beaver. Most specimens of the giant beaver, an extinct Pleistocene rodent found throughout North America that approached the size of a black bear, are considered Castoroides ohioensis. Now, scientists have proposed a new species of giant beaver, Castoroides dilophidus, based on skulls found in Florida.
This new species lived during the Late Pleistocene and is limited, so far, to Florida and surrounding states. It is distinguished from C. ohioensis by several cranial characteristics as well as the presence of a divided lophid on two teeth, the lower fourth premolar and upper third molar (hence the species name dilophidus). An earlier named species, C. leiseyorum, thought to be restricted to the Early Pleistocene, is now also subsumed into C. dilophidus as a junior synonym.
Some interesting issues regarding the collection and curation of fossils pop up. One of the skulls used to define the new species “is housed in a private collection, but a high fidelity cast is in the UF [University of Florida] collection. Furthermore, the owner of the original specimen has agreed to make it available for study to other workers.” (Hulbert et al. 2014:29). The owner is unnamed. They also discuss in detail casts of a giant beaver skull sold by the company Bone Clones that “likely reside in a number of museum collections” (Hulbert et al. 2014:38). This specimen, which the company labels C. ohioensis, also has characteristics of C. dilophidus. It appears that the original fossil has dilophidus traits, but when the fossil was restored, missing parts were reconstructed using ohioensis (and modern beaver) as references. Hulbert and colleagues were able to solve this puzzle by speaking with the original collector and the person who did the restoration, both of whom are unnamed, but the actual fossil “is now in a private collection and not available for study.” (Hulbert et al. 2014:38). The authors have tried to make the best of an awkward situation by documenting as thoroughly as possible these mystery fossils.
Hulbert, Richard C., Jr., Andreas Kerner, and Gary S. Morgan
2014 Taxonomy of the Pleistocene Giant Beaver Castoroides (Rodentia: Castoridae) From the Southeastern United States. Bulletin of the Florida Museum of Natural History 53(2):26–43.
The first issue of PaleoAmerica, something of a successor to the discontinued Current Research in the Pleistocene, has just been released. Maney Online has made the entire first issue, which includes articles on the early peopling of North and South America, available for free (for a limited time?).
Animal bones from the last Ice Age are continually being exposed by gold mining in the Yukon. The provincial government hires two paleontologists to collect the bones, and occasionally bits of flesh or fur, from the many mining operations; they already have 25,000 specimens.
“Typically, you know you’ve found it because you smell it before you see, it,” said Duane Froese, a University of Alberta scientist who has been coming to the Klondike for 20 years. “Imagine putting something in your freezer for 40,000 years and then thawing it out.”
In fact, most placer mines are permeated by a noticeably foul smell. As Klondike silt is blasted away, it unleashes the distinctive stench of millennia-old rotting plants and animals.
“It’s like rotting ancient barnyard, and you know when you have that smell that you’re going to find a lot of ancient material,” said Mr. Zazula.
The Klondike region, along with parts of Alaska, was one of the only parts of North America not to be covered by ice sheets during the last ice age.
As a result, while soil in the rest of Canada was repeatedly smashed and churned by glaciation, the frozen Klondike ground remained as undisturbed as a graveyard. In some remote area of the northern Yukon, prospectors even talk of finding mammoth prints.