I am fortunate to have in my
collection representative fossils of the phosphate beds of the Ouled Abdoune
Basin of Morocco: Enchodus
lybicus and Mosasaur
beaugei from the Upper Cretaceous Period near Ouled Abdoune and an
assortment of sand
shark teeth from the Paleocene Epoch of the Khouribga portion of the
phospate beds, both time periods represented in fossil bed’s stratigraphy shown
below. However much I value my Moroccan
teeth collection, I shall discuss them briefly as I have all my other specimens,
in context with the fossils within the geological stratigraphy they were
found. In the case of Ouled Abdoune and
the fossil beds found in Khouribga, the discoveries have inspired many
paleontologists and geologists to call this corner of the Sahara another Burgess Shale. This claim might seem like an exaggeration,
since most of the Moroccan species are not unique, but the phosphate beds are
considered to be one of the most important paleontological discoveries made in
Africa.
Ouled
AbdounE: Africa’s Version of the Burgess Shale
The fossils found in the Ouled Abdoune Basin have
several important features for the professional and amateur paleontologist:
they are plentiful, remarkably diversified and well preserved, and they attest
to key periods in vertebrate evolution, chronicled in logical succession in the
phosphate beds. In terms of the ICS
Time Scale, as shown in the following chart, the fossil sequence begins in
the Santonian stage of the Upper Cretaceous period, continuing through the
Maastrichtian stage and ending in the Danian stage of the Paleogene at what the
Standard Geological Scale would indicate as the demarcation point between the
end of the Cretaceous period and beginning of the Tertiary period or Paleocene
epoch. Since many scientists believe
that this time interval saw the extinction of the dinosaurs, the ICS Time
Scale’s smaller increments of time encourage paleontologists and geologists to
see in the Danian (earliest Paleocene) an almost seamless point for the KT
boundary (K=Cretaceous and T=Tertiary).
Whatever theory is recognized—comet collision, virus attack, egg-eating
mammals, etc—recent discoveries in New Mexico
indicate that not all dinosaurs became suddenly extinct when the geological
dial moved into the Danian stage. Yet
nowhere else in the world is there a site where the dinosaurs and giant
reptiles transition into the Age of Mammals in such a logical, complete
sequence. Evolution is seen clearly in
the barren Sahara rock, where primitive forms evolved into more advanced
forms—proof-positive of the principle of
faunal succession.
Stratigraphy of the Ouled
Abdoune Phosphate Beds
Creatures
of the oULED ABDOUNE Phosphate Beds
Because the setting for Ouled Abdoun’s diverse
creatures was a shallow sea that bordered dry land, the outcrops at this site
reflect both a marine and terrestrial environment. The richest vertebrate marine fauna known to science also
includes, after recent discoveries, dinosaur fossils,
along with bony fishes, crocodiles, early mammals, and birds in the
Maastrichtian stage of the Upper Cretaceous, as well as more advanced mammals,
new crocodile species, and sea birds in the Danian stage of the Paleocene
Epoch. The Ouled Abdoun Phosphate Beds
have also yielded the oldest known modern birds (Neornithes), shedding light
on the evolution of this important subclass.
One of the mammal specimens found in the Danian levels, Eritherium, who is considered by many
paleontologists to be the ancestor of elephants, is also the oldest known
placental mammal of Africa. Among the
signficant finds at Ouled Abdoun, Enchodus lybicus, a
saber-tooth relative of the modern salmon, was discovered in both the Upper
Cretaceous and succeeding Tertiary levels of the phosphate beds. Unlike the dinosaurs and marine reptiles,
this fish survived the Upper Cretaceous extinction and is found, along with
other fossil fish, throughout the beds.
Mosasaur beaugei,
which didn’t survive into the Tertiary period, probably included juvenile
Enchodus in his diet. The fact that
such giant fish as Enchodus and large crocodiles, such as Arambourgisuchus, as
well, as many land mammals and reptiles survived the KT extinction has made me
a skeptic of the theory that a comet wiped out the dinosaurs. Nevertheless, whatever it was that wiped out
the dinosaurs and marine reptiles, the transitioning layers of the phospate
beds appear to add weight to a general and sudden end. At the top portion of the Maastrichtian
stage in various outcrops there are still an assortment dinosaur and marine
reptile bones, and then, quite abruptly, in the earliest Danian, where the
Tertiary period begins and the Cenozoic Era launches the Age of Mammals, the
Age of the Dinosaur and Marine Reptiles is suddenly over. The upper levels also present advanced
species of mammals and birds and the continued existence of Enchodus in the
marine outcrops.
Note: To zoom in and out on one set of teeth, click
on one the photos below:
Mosasaur beaugei Enchodus lybicus Sand Shark