The desert sands of Egypt have been dry for hundreds of years.
As troublesome as it’s to image now, nevertheless, a lot of that desert was as soon as submerged beneath a sea that lined a lot of the northern perimeter of the African continent.
Nor was it a useless sea – proof means that, in the course of the Cretaceous interval, it could have been a tropical wonderland, the place rising currents lifted vitamins into the water column to feed a thriving ecosystem.
Now, buried in what was as soon as the ground of that long-ago sea, on the Abu-Tartur Plateau, paleontologists have discovered proof of its lushness: the enamel of sharks that will have thrived amid the bounty of fish.
And never only one shark. The entire variety of completely different species present in that layer of the Duwi Formation now numbers no less than seven – providing a glimpse of the wealthy marine ecosystems that when flourished alongside the northern fringe of Africa.

“Collectively, this assemblage highlights a nutrient-enriched, high-productivity marine ecosystem alongside a phosphogenic shelf margin,” writes a staff led by paleontologist Tarek Yassin of Cairo College in a paper revealed in Cretaceous Research.
Through the Cretaceous interval, between about 145 to 66 million years in the past, our Earth was a really completely different place. Below a greenhouse climate pushed by tectonic exercise, the world was hotter, with little to no polar ice; higher sea levels meant that a lot of the land we inhabit at this time was underwater, together with northern Africa.
We all know this no less than partially due to phosphate. Phosphorite deposits generally type the place marine productiveness is excessive, and phosphorus is being intensively cycled and concentrated.

The intensive phosphate deposits of the Duwi Formation subsequently protect not simply the stays of this historic sea, however clues to how productive its waters as soon as have been.
In earlier analysis, Yassin and his colleagues had identified two shark species in a handful of enamel discovered within the fossil mattress – an intriguing sign, since a neighborhood able to supporting a number of massive predators requires a productive meals net beneath them.
In order that they went again to Abu-Tartur to see if they might discover out extra.
And the black and yellow layers of the Duwi phosphate ponied up the products. They discovered one other 14 shark enamel – representing one other 5 shark species, none of which had been recognized at Abu-Tartur.
When all you’ve got is enamel – and with historic sharks, that is usually the case – refined variations might be the only real metric on which a species analysis hangs.
With the Duwi enamel, the variations weren’t all the time refined.
A number of of the enamel have been lengthy and slender, like a needle. Others have been broad and serrated, most likely higher fitted to slicing than penetrating. One tooth was prominently curved like a karambit. Some had small, fang-like facet projections, known as cusplets; others didn’t.
Based mostly on different fossil data all over the world, the researchers recognized these enamel as belonging to 5 extinct species: Cretalamna cf. maroccana, Scapanorhynchus cf. raphiodon, Serratolamna cf. serrata, Squalicorax bassanii, and Squalicorax pristodontus.
All 5 are new data for Abu-Tartur.
Two have been new for Egypt solely – Serratolamna cf. serrata and Squalicorax bassanii.
One stood out as extraordinary. Scapanorhynchus cf. raphiodon – the one with the needle enamel – might characterize the primary identified prevalence in Africa. As well as, it may very well be the latest instance on the fossil file, the researchers mentioned – all different specimens are considerably older.
These identities, nevertheless, paint a way more attention-grabbing image than “a bunch of sharks”.
As their enamel may counsel, they might not have been straight competing, however occupying completely different ecological niches in a wealthy marine surroundings.
“The presence of Squalicorax might counsel an enter from nearshore/interior shelf settings, whereas the prevalence of Scapanorhynchus displays deeper-water situations on the outer shelf and slope,” the researchers write.
“Lamniform taxa corresponding to Cretalamna and Serratolamna additional help secure open-shelf situations.”
The researchers imagine that the key to this richness might have been upwelling.
Nutrient-rich waters rising from deeper within the ocean would have delivered phosphorus and different vitamins to the sunlit floor waters, driving intense major productiveness – plankton that got here to feast.
That may have supported small fish and invertebrates, then predators corresponding to Squalicorax and Cretalamna, with Cretoxyrhina and marine reptiles larger up the meals net.

However that is the place the shark “graveyard” will get attention-grabbing. There was little or no sediment accumulation in the course of the time that the sharks lived, so the phosphate mattress represents a extra condensed span of time than you may discover someplace with extra mud.
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Consequently, the enamel are a time-averaged accumulation from a number of ecological niches, not proof that seven shark species lived on the identical time and all died there collectively.
Nevertheless it does add to proof that these ecosystems have been frequent throughout the northern fringe of Africa in the course of the Late Cretaceous. Different phosphate deposits from locations corresponding to Morocco and Syria file massive numbers of shark species hanging round – suggesting the complete area was an ideal place to conduct shark enterprise.
At the moment, little stays of that shark paradise. The Tethys is gone, the seafloor has change into desert, and the predators that prowled its waters vanished hundreds of thousands of years in the past.
Like a projector from the previous, nevertheless, only a scattered handful of enamel embedded in a rock can conjure up a whole misplaced world.
The findings have been revealed in Cretaceous Research.
This text was fact-checked by Rebecca Dyer and edited by Rebecca Dyer. Whereas we pleasure ourselves on our course of, we’re solely human. For those who spot a mistake, please let us know.
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