2.3" Asaphellus Trilobite With Unidentified Carpoid - Morocco

This is a reddish, 2.3" long Asaphellus trilobite from the Ordovician deposits near Zagora, Morocco. The orange coloration is due to the oxidization of iron pyrite. There is a unidentified carpoid preserved over the top of it.

Comes with an acrylic display stand.

Carpoids are an enigmatic organisms. They are early echinoderms related to starfish and sea urchins. Unlike modern echinoderms, carpoids lack the five fold radial symmetry and water vascular system. Most were asymmetric or bilaterally symmetric. LIke other echinoderms they did possess a skeleton of calcite plates. They consisted of, depending on species, one or two ambulacra (filtering appendages), a theca (“head”) and a three section stele (“tail”). It is believed that they are early ancestors of starfish and other echinoderms but it is also possible that they are an early ancestor of the Chordates. This is phylum that humans are a part of. This is a contentious theory based on the presence or absence of early gills in carpoids. Because these organisms are only known from fossils, gills are hard to identify accurately.

Carpoids evolved during the Middle Cambrian Period and disappear from the fossil record during the early Devonian Period.

Carpoids were an unconventional looking organism. The vital organs of the animal were contained in a theca. Internal organs were surrounded by calcite plates. Depending on the species of carpoid, one or two ambulacrum extended from one end of the theca. These were appendages for filtering water for food. A mouth was located at the base of the ambulacrum if there was just one or between them if there were two. From the other end of the theca, the three section stele (“tail”) extended. This was used either for locomotion or to hold the organism in place if sessile. That is fixed in one location. It is thought that carpoids grew up to about 4 inches (10cm).

Trilobites were a very diverse group of extinct marine arthropods. They first appeared in the fossil record in the Early Cambrian (521 million years ago) and went extinct during the Permian mass extinction (250 million years ago). They were one of the most successful of the early animals on our planet with over 25k described species, filling nearly every evolutionary niche. Due in large part to a hard exoskeleton (shell), they left a excellent fossil record.
Asaphellus sp. & Unidentified Carpoid
Zagora Area, Morocco
Fezouata Shale
2.3" Trilobite, 4.3 x 3.6" shale
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