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PRESS RELEASE - Uniquely Preserved Whale Fossil Shows Important Characters of the Transition to Water





Figure 1
DEERFIELD, ILLINOIS (November, 2011) – Decorative stone is often used in buildings for its strength and durability but is not often thought of as a hiding place for fossils. If not for an observant Italian stonecutter, a recently discovered fossil whale specimen from Egypt might have become part of the edifice of some new skyscraper rather than the focus of a scientific study. This fossil skull and partial rib cage, described in the latest issue of the Journal of Vertebrate Paleontology, show transitional features of a new species of early whale and hint at how it became a fossil in the first place.



Figure 2
Giovanni Bianucci of the Università di Pisa and Philip Gingerich of the University of Michigan collaborated to describe this unique find. “The fossil came from deep in an enormous limestone quarry in Egypt, but it was only recognized to be a fossil skeleton when it was cut into decorative facing stone in Italy. Fortunately it then found its way to the museum in Pisa where it could be studied,” said Bianucci. Working with researchers at museums and universities in Egypt and using Google Earth, Gingerich was able to find and revisit the location of the quarry where the fossil had been quarried.



Figure 3
Because the limestone had already been cut into thick slabs about 1 inch (27mm) thick, details of the specimen could be examined in a way that would normally require destruction of a fossil. The researchers were able to remove the slices of the skull and rib cage from the stone and reposition them as they had been in life.  After accomplishing this, they were able to investigate the unusual characters preserved by the fossil and recognize that it represented a new species, dubbed Aegyptocetus tarfa (ay-jip-to-SEE-tus TAR-fa).



Figure 4
Says Gingerich, “Connecting links that are intermediate in geological time, intermediate in morphological form, and intermediate in functional adaptation are the evidence for evolution, and Aegyptocetus tarfa falls right in the middle of what we know about the evolutionary transition of whales from land to sea.” Dating to around 40 million years ago, the fossil documents a transitional stage in the evolution of whales from their terrestrial ancestors to the fully aquatic species we see today. The transitional characters present in this species include a retained sense of smell (which is usually lost in aquatic mammal lineages), an enhanced ability to hear (a characteristic of later and modern whales), and the ability to still haul itself out of the water, similar to modern seals.



Figure 5
In addition to these transitional features, the fossil had some other surprises. Bite marks on its ribs may show that the whale was attacked by a shark before dying and becoming fossilized. “It is rare to find evidence of behavioral interaction in the fossil record, but here we have evidence of an early semiaquatic whale being attacked by a shark,” says Bianucci. In addition, small scars on the bones are the burrows of ancient barnacles, giving some idea about how long the carcass sat on the bottom of the ocean before being buried.


The researchers suspect there may be other fossils hidden in the limestone and are making connections with stonecutters who work with the rock from the quarry so that they can ask them to keep an eye out for other ancient treasures.


About the Society of Vertebrate Paleontology
Founded in 1940 by thirty-four paleontologists, the Society now has more than 2,300 members representing professionals, students, artists, preparators and others interested in vertebrate paleontology. It is organized exclusively for educational and scientific purposes, with the object of advancing the science of vertebrate paleontology.

Journal of Vertebrate Paleontology
The Journal of Vertebrate Paleontology (JVP) is the leading journal of professional vertebrate paleontology and the flagship publication of the Society. It was founded in 1980 by Dr. Jiri Zidek and publishes contributions on all aspects of vertebrate paleontology.

For complimentary access to the full article beginning November 9, 2011, visit http://www.tandfonline.com/toc/ujvp20/current.

The article appears in the Journal of Vertebrate Paleontology 31(6), published by Taylor and Francis.



Giovanni Bianucci
Dipartimento di Scienze della Terra
Università di Pisa
Pisa, Italy
Fax: +39-050-2215800

Phillip D. Gingerich
Museum of Paleontology and
Department of Earth and Environmental Sciences
University of Michigan
Ann Arbor, Michigan USA
Fax: +1-734-936-1380

Other Experts Not Associated with this Study

Anthony Friscia
University of California, Los Angeles
Dept. of Integrative Biology and Physiology
Los Angeles, CA USA

Mark D. Uhen
George Mason University
AOES Geology
Fairfax, VA USA
Fax: +1-703-993-1066

Ewan Fordyce
University of Otago
Dunedin, New Zealand

Figure 1. Top: the six limestone plates containing the Aegyptocetus tarfa skeleton before preparation. Plates are lettered a-f from top to bottom stratigraphically. Bottom: schematic shows oblique orientation of the skull, as preserved, relative to bedding and relative to plate surfaces. Photographs and illustration by G. Bianucci and P. D. Gingerich.

Figures 2-3. Aegyptocetus tarfa skeleton as exposed at the Natural History Museum of Pisa University (Italy). The bones are disposed in the original position on the sea floor before the burial. Photograph by G. Bianucci.

Figure 4. One of the six limestone plates containing the Aegyptocetus tarfa skeleton before preparation. Photograph by G. Bianucci.

Figure 5. Top: assembly of the skeleton of Aegyptocetus tarfa in life position. Bottom: map view of the skeleton as it was preserved in the limestone. Illustration by G. Bianucci.

Figure 6. Particular of the six limestone plates containing the Aegyptocetus tarfa skeleton before preparation. A cross-section of the skull is visible. Photograph by G. Bianucci.

Figure 7. Assembly of the skeleton in life position of Aegyptocetus tarfa showing the position of large tooth marks on ribs (dotted red line) indicating an attack by a large shark. Illustration by G. Bianucci.

Figure 8. Limestone plates containing fossil bones in a marble factory of Italy. The limestone comes from a commercial rock quarry in Egypt. Photograph by G. Bianucci.

Figure 9. Arrival at the Natural History Museum of Pisa University (Italy) of the the six limestone plates containing the Aegyptocetus tarfa skeleton before preparation. Photograph by G. Bianucci.

Figure 10. Khashm el-Raqaba quarry on the northern flank of Wadi Tarfa (Egypt) where Aegyptocetus tarfa was found. Photograph by P. D. Gingerich.

Figure 11. Map of Egypt showing the location of Wadi Tarfa and the Khashm el-Raqaba limestone quarry complex (star) where Aegyptocetus tarfa was found. Illustration by P. D. Gingerich.


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