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Scientists uncover lost world beneath Egypt’s desert that rewrites its ancient past

by LJ News Opinions
August 24, 2026
in Technology
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Scientists have uncovered evidence of a lost world buried beneath Egypt’s desert for more than 70 million years.

Researchers found 14 fossilized teeth that belonged to five now-extinct shark species, including one that may never before have been found in Africa.

The discovery brings the number of shark species identified in the area to at least seven.

It reveals that one of the driest places on Earth was once submerged beneath a warm tropical sea teeming with life.

The discovery was made on Egypt’s Abu-Tartur Plateau, a remote stretch of the Western Desert rich in phosphate deposits.

The teeth varied dramatically in shape: some were thin and needle-like, others were broad and serrated, and one specimen was curved.

Those differences suggest the sharks hunted different prey and occupied separate positions within the food chain.

Together with evidence of small fish, invertebrates and predatory marine reptiles, the fossils reveal a rich ecosystem that once thrived where only deserts exists today.

The discovery was made on Egypt’s Abu-Tartur Plateau, a remote stretch of the Western Desert rich in phosphate deposits. Above is a mine in the Abu-Tartur Plateau

The team suggested that powerful ocean currents likely carried nutrient-rich water toward the surface, helping plankton and other small organisms thrive. 

That abundance of food supported an entire marine food chain, from small fish and invertebrates to medium-sized sharks and enormous predators. Marine reptiles also lived in parts of the region, according to the study published in the journal Cretaceous Research.

Some of the sharks typically lived closer to shore, while others preferred deeper waters. This suggests the fossils accumulated over time and came from several different parts of the ancient marine environment.

Overall, the findings reveal that the area was once a rich and highly productive ocean ecosystem during the Late Cretaceous period.

Abu-Tartur Plateau is a major limestone highland in the central Western Desert, located roughly 400 miles southwest of Cairo between the Kharga and Dakhla oases. 

It holds one of the region’s largest phosphate reserves, serving as a vital hub for Egypt’s mining and fertilizer industries.

The sharks lived during the Cretaceous period, between 145 and 66 million years ago, when the Earth was much hotter and more humid than it is today.

What is now Egypt was also a lush, tropical landscape, with portions of the country submerged beneath warm Tethys seawater that teemed with marine life.

Researchers recovered 14 fossilized teeth belonging to five now-extinct shark species, bringing the number known from the area to at least seven

Researchers recovered 14 fossilized teeth belonging to five now-extinct shark species, bringing the number known from the area to at least seven

By comparing the teeth with fossils found elsewhere in the world, the researchers led by Cairo University linked them to five extinct shark species: Cretalamna cf. maroccana, Scapanorhynchus cf. raphiodon, Serratolamna cf. serrata, Squalicorax bassanii and Squalicorax pristodontus.

None had previously been recorded at Abu-Tartur, while two, Serratolamna cf. serrata and Squalicorax bassanii, had never before been documented in Egypt.

But one discovery was particularly remarkable.

Scapanorhynchus cf. raphiodon, distinguished by its long, needle-like teeth, may be the first example of the species ever found in Africa.

Researchers said it could also be the youngest known specimen in the fossil record, as every other example discovered so far is significantly older.

Together, the five species reveal far more than the simple presence of sharks.

Their differently shaped teeth suggest they hunted separate prey and occupied distinct roles within a rich and complex marine ecosystem, rather than competing for the same food.

The team suggested that finding all seven species in the same phosphate-rich layer means their remains accumulated in a warm tropical or subtropical sea. 

The area was probably located along the outer continental shelf and the upper part of the slope leading into deeper water.

The sea also appeared to have been affected by active upwelling, a process in which currents carry cold, nutrient-rich water from the depths toward the surface. 

Those nutrients would have fueled the rapid growth of plankton and other tiny organisms, supporting a large and varied marine food web, according to researchers.

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Tags: dailymailearthEgyptsciencetech
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