Type localities are a big deal in vertebrate paleontology. It's the location of first contact with a part of the Earth's history that has never before been seen and recognized for its importance. They are also the place where present and future researchers can visit and continue to collect information using new ideas and techniques. Also, these sites are bloody cool!
I had a great opportunity to visit the type locality of Ignotornis mcconnelli, the very first Mesozoic bird footprint ever named. Ignotornis was named by Maurice Goldsmith Mehl (1887-1966) in 1931 from a locality "one and a half miles northwest of Golden, Colorado". The specimen was found by N. H. McConnell and donated to the University of Colorado at Boulder. This specimen, the holotype specimen, is UCM 17614.
|Ignotornis mcconnelli holotype slab, figured in Lockley et al. (2009).|
"Hold up, Shaman: what's a holotype?"
A holotype is the one physical example (it can be a picture, if there is no physical specimen) of an organism (or the trace of an organism) that is being given a unique name. The type is also the specimen to which other similar-looking specimens must be compared when you name a completely new specimen. There are many different categories of types, and many, many rules governing how the different types are named and under what circumstances. This is governed by the International Code of Zoological Nomenclature. For example: did the original physical specimen go missing and you want to make a different specimen the reference? There's a rule for that!
One of the great things with science is that there is always an opportunity to clear up confusing statements. When Mehl described Ignotornis, he made reference to other track-bearing slabs, but didn't really state how they were related to the type (although they were all originally cataloged under the same number), or make specific mention of which rock layer in the outcrop these slabs came from. Lockley et al. (2009) cleared up this bit of confusion and used these other track-bearing slabs to re-examine Ignotornis mcconnelli (and provided lots of great data and images), and formally name these other slabs as additional reference (type) specimens. Lockley et al. also narrowed down exactly how old Ignotoris is by tracking down (pun completely intended) the discovery site of the original specimen, which is in the Cretaceous Dakota Group, Albian - Cenomanian (approximately 113-94 million years old) in age.
Ignotornis mcconnelli was the first footprint type attributed to a bird by a long lead: Koreanaornis hamanensis was named in 1969, and the Peace Region's own Aquatilavipes swiboldae was named in 1981. The ichnogenus Ignotornis existed for 75 years with only one ichnospecies until 2006 when Ignotornis yangi was named (Kim et al. 2006), and in 2012 Kim et al. named Ignotornis gajinensis, which has a great feeding trace associated with the trackway (both from South Korea)
I visited the rediscovered type locality of Ignotornis mcconnelli in October in the company of Martin Lockley and Rich McCrea. It is not exactly the most obvious of localities: the mountain-building processes of the region have uplifted and shifted the rock layers around quite a bit, and I had a scary moment of having to climb up and over a vertical piece of sandstone and scramble down a steep slope to get to the locality. I don't like heights (which surprises many, given the amount of vertical track work I do), but that was not going to stop me from visiting this site.
|This was the easy part of the climb. There are no pics of the scary part: I needed both my hands to keep from dying.|
|Ignotornis mcconnelli, in the flesh, er, foot!|
While we were there, we decided to document a large in-place (or in situ) set of Ignotornis trackways with photogrammetry. This way we get to take a 3D digital replica of the tracksite to our home lab with zero impact on the surface.
|Martin Lockley (left) and Rich McCrea (right) digitally documenting Ignotornis footprints.|
|Footprint #3 in this photo (numbered from left to right) is much more shallow, and only leaves a hint of something that could be a hallux. Prints #1 and #2 have deeply impressed hallices.|
|The track surfaces also contain invertebrate burrows, seen here in the upper left and center right of the picture.|
|Natural cast of a left foot of an ornithopod. The wide foot and rounded toes tell us that it is a plant-eater.|
This ends my visit to the Ignotornis type locality! We collected a lot of great images and data, and I hope this will not be my only visit to the site. As the rock layers erode, more tracks will make their appearance after being hidden for 100 million years, waiting to tell us their story.
Currie PJ. 1981. Bird footprints from the Gething Formation (Aptian, Lower Cretaceous) of northeastern British Columbia, Canada. Journal of Vertebrate Paleontology 1:257-264.
Kim, BK. 1969. A study of several sole marks in the Haman Formation. Journal
of the Geological Society of Korea 5:243-258.
Kim JY, SH Kim, KS Kim, M Lockley. 2006. The oldest record of webbed bird and pterosaur tracks from South Korea (Cretaceous Haman Formation, Changseon and Gansu Islands): more evidence of high avian diversity in East Asia. Cretaceous Research 27:56-69.
Kim JY, MG Lockley, SJ Seo, KS Kim, SH Kim, KS Baek. A paradise of Mesozoic birds: the World's richest and most diverse Cretaceous bird track assemblage from the Early Cretaceous Haman Formation of the Gajin Tracksite, Jinju, Korea. Ichnos 19:28-42.
Lockley MG, K Chin, K Houck, M Matsukawa, R Kukihara. 2009. New interpretations of Ignotornis, the first-reported Mesozoic avian footprints: implications for the paleoecology and behavior of an enigmatic Cretaceous bird. Cretaceous Research 30(4):1041–1061.
Mehl MG. 1931. Additions to the vertebrate record of the Dakota Sandstone. American Journal of Society 21:441-452.