Showing posts with label chirotherium. Show all posts
Showing posts with label chirotherium. Show all posts

Monday, March 29, 2010

Chirotherium World Tour

A team of scientists from the TU Freiberg recently unearthed well-preserved tetrapod footprints from the Triassic of the High Atlas (Morocco). Surprisingly, this ichnofauna is dominated by the ichnogenus Chirotherium, wich is suggested to present an exclusive element of North-Pangean or Laurasian localities that are nowadays associated to Europe, China and North America. Although the scientists are aware that similar trackways were reported from western Gondwana (Argentina; Peabody, 1955), it was stated by several local newspapers that the imprints represent the first occurrences of such traces from Gondwana.

Fig. 1: Pes (the big one) and manus imprint of the ichnogenus
Chirotherium
from the Triassic of Morocco (courtesy of Jan Fischer).


Extensive field work yielded several well-preserved imprints and trackways that can be assigned to the ichnospecies Chirotherium barthii (fig. 1), which is described from (watch out, confusing terms) upper Lower Triassic (Olenekian) to lower Middle Triassic (Anisian) rocks like the Moenkopi Formation of the western U.S. or the Buntsandstein of Central Europe (Klein & Haubold, 2007; and references therein).

As noted above, at least the ichnogenus seems to occur in Argentina as well but the new data from Morocco now strongly support the hypothesis of Peabody (1955) that Chirotherium is a track with a global distribution and its archosaurian producer inhabited the northern and southern hemisphere (see a reconstruction of the palaeoenvironment in fig. 2).

All specimens are currently under investigation by Hendrik Klein, Sebastian Voigt and Jörg Schneider of the TU Freiberg and I expect some interesting papers to be published in near future. For instance, the age of these findings will play an important role in unravelling the evolutionary history of archosaurs.

Fig. 2: A reconstruction of the palaeoenvironment based on the
geological context and sedimentary analysis of the track bearing interval.
Drawn by F. Spindler (taken from Sächsische Zeitung, march 20/21, 2010).



References

Peabody, F.E., 1955: Occurrence of Chirotherium in South America: Geological Society of America Bulletin, v. 66, p. 239-240.

Klein, H., Haubold, H., 2007: Archosaur footprints - potential for biochronolgy of Triassic contintal sequences. In Lucas, S.G., Spielmann, J.A., (eds): The Global Triassic. New Mexico Museum of Natural History and Science Bulletin 41.

Friday, November 14, 2008

And now all together: Chirotherium is not an Archosaur!

Actually this one is not really important and I thought about publishing this post altogether. Although it is rather a popular problem than a scientific or academic one, it still teases me. You can find it everywhere: Newspaper, blogs and wikipedia for instance. Trackways of the ichnogenus Chirotherium are constantly mistaken for an Archosaur or related creatures.

For instance, the german Wikipedia article on Chirotherium: Fossilised footprint (ichnite) of the ichnogenus Chirotherium, an archosaur of the Lower Triassic, first found 1833 in Hildburghausen (Thuringia, Germany).

This is just wrong. An archosaur cannot be an ichnogenus.

Unfortunately, Chirotherium literally means something like "hand beast" or "hand animal". However, the term Chirotherium is scientifically used for a certain type of trackway(s), which is found in Sediments with a Triassic age, ranging from Olenikian to Anisian (KLEIN & HAUBOLD, 2007). In fact, Chirotherium is the first scientifically described trackway (KAUPP, 1835) and, by the form of the pes imprints (rear leg) resembling human hands, it animated the early palaeontologists imagination for the mysterious ancient beast that once left its trackway on the wet sand of the vast Triassic plain. In a way the "hand animal" is a chimera of those early days of palaeontological research. From a modern point of (ichno)taxonomic view, the scientific name Chirotherium, however, is attributed to the trace fossil only, although the trace maker most likely was an archosaur of some sort. Yes, you are right, this is scientific quibble but still; it is not correct.
Yours Ichnogeek!


Chirotherium (pes imprint) from the Triassic of Germany.


The "Chirotherium Monument" with a reconstructed "hand beast" (Hildburghausen, Germany)


References:

Kaup, J.J., 1835: Über Thierfährten bei Hildburghausen. Neues Jahrbuch für Mineralogie, Geognosie, Geologie und Petrefaktenkunde. v. 1835, pp. 227-228.

Klein, H., Haubold, H., 2007: Archosaur footprints - potential for biochronolgy of Triassic contintal sequences. In Lucas, S.G., Spielmann, J.A., (eds): The Global Triassic. New Mexico Museum of Natural History and Science Bulletin 41.