Fossil Shark SQUALICORAX KAUPI Pathological teeth – Bulk Fossil

Eocene Fossil Shark Teeth – SQUALICORAX KAUI- Authentic Moroccan Specimens

Squalicorax kaupi pathological teeth from the Sidi Chennane Basin near Khouribga, Morocco, are particularly significant due to the rich fossil record of this area. The Sidi Chennane Basin is well-known for its phosphate deposits, which have preserved an abundance of marine fossils from the Late Cretaceous period, including a variety of shark species.

These pathological teeth, ranging in size from 0.75 inches to 1.25 inches, exhibit unusual growth patterns that are likely the result of injuries, diseases, or genetic factors affecting the sharks during their lifetime. The teeth retain the classic triangular shape and serrated edges typical of Squalicorax kaupi but are distinguished by their deformities, which might include twisted crowns, irregular serrations, or asymmetrical roots.

Fossils from the Sidi Chennane Basin are highly regarded in the paleontological community due to their excellent preservation and the diversity of species found in the region. The unique conditions of the basin have allowed for the fossilization of these teeth, providing a rare glimpse into the lives of ancient sharks in this part of the world.

SPECIES : SQUALICORAX KAUPI.
AGE : Eocene (~55 Million Years Old)
LOCATION : Sidi Chennane Basin, Morocco
FORMATION : Phosphate Deposits
SIZE : 0.75″ – 1.25″
CATEGORY : Shark Fossils

Ideal for educational purposes or as unique gifts, these fossil shark teeth offer a tangible connection to the ancient past.

Squalicorax kaupi is a species of extinct shark that lived during the Late Cretaceous period, around 100 to 66 million years ago. The genus Squalicorax, often referred to as “crow sharks,” is known for its distinctive teeth, which have a broad, triangular shape with serrated edges. These teeth are relatively small compared to other prehistoric sharks but are notable for their sharpness and efficiency in cutting.

 

Squalicorax kaupi is typically found in marine deposits that were once shallow seas, such as those in North America, Europe, and North Africa. These sharks were likely scavengers, feeding on a variety of prey including fish, marine reptiles, and possibly even dinosaur carcasses that washed into the sea.

The teeth of Squalicorax kaupi are popular among fossil collectors due to their distinct shape and the historical period they represent.

Otodus obliquus and Megalodon

The connection between Otodus obliquus and Megalodon lies in their evolutionary relationship. Researchers consider Otodus obliquus an ancestor of Megalodon, with the prevailing belief that Megalodon evolved from a lineage of Otodus species. Fossil evidence suggests a transition from Otodus-like sharks to the larger, more massive Megalodon over millions of years.