Entothyreos

Entothyreos Temporal range: Middle Cambrian
Life restoration
Scientific classification
Domain:	Eukaryota
Kingdom:	Animalia
(unranked):	Panarthropoda
Phylum:	†"Lobopodia"
Family:	†Luolishaniidae
Genus:	†Entothyreos Aria & Caron, 2024
Species:	†E. synnaustrus
Binomial name
†Entothyreos synnaustrus Aria & Caron, 2024

Entothyreos is a genus of extinct panarthropod belonging to the group Lobopodia and known from the middle Cambrian Burgess Shale in British Columbia, Canada. The genus contains a single species, Entothyreos synnaustrus (meaning "convergent inner shield"), described in 2024. Entothyreos is significant for possessing a remarkable degree of sclerotization among lobopodians, comparable to that of arthropods.

Description

Entothyreos is a stout collinsovermid lobopodian, capable of reaching roughly 5 cm in length. The dorsum was protected by numerous paired sclerite spines (2 pairs per trunk segment). The spines are longest at the middle of the body. These spines are associated (although still dissociable) with subrectangular sclerotic sheets which lie just below the cuticle surface. These sclerite sheets may have increased body rigidity, allowing easier erection of the body to allow for suspension feeding from the water column. They are comparable with the sclerotic rings found in other luolishaniids, which probably evolved at first to allow for the otherwise soft body to carry numerous large spines. Additionally, the head segment bears 2 pairs of small sclerite spines (with no apparent underlying sclerotic sheet), and a pair of soft antenniform sensory structures.

Entothyreos possessed 11 pairs of lobopodous limbs, divided into two sets. The anterior set of 6 limb pairs are elongate and lined with 2 rows of large, sclerotized setae, which allowed the animal to sieve food particles from the water. These limbs were also covered in numerous shorter, fine setae on their dorsal side, and tipped with a pair of sickle-shaped claws. The posterior 5 pairs are thick and conical, each tipped with a single, large, highly developed claw. The annuli of these posterior limbs are highly sclerotized, the margins of which are lined with short setae of alternating lengths. The posterior claws have an additional branch near their base opposing the tip like a claw, unique to Entothyreos, which aided in anchoring to substrate. The final, posterior-most pair of limbs have annuli differentiated into 7 sclerotized sheets, which covered at least the dorsal surface of the limb, probably for further protection. While not truly arthropodized (they are likely not articulated with an arthrodial membrane), the degree of sclerotization present does represent a remarkable convergence with arthropods.

Ecology

Entothyreos is relatively common compared with other Burgess Shale lobopodians, being initially described from a suite of 51 fossil specimens. One slab, preserving a large amount of organisms including Anomalocaris, Peytoia, and some sponges, contains 9 different individual specimens of Entothyreos. All fossil specimens derive from the Tulip Beds locality of the Burgess Shale (found at the base of the Campsite Cliff Shale Member, making it one of the oldest Burgess Shale localities), which represents a more distal environment, further from the Cathedral Escarpment than the more famous Walcott Quarry. The Tulip Beds palaeoenvironment is dominated by sessile animals, particularly suspension feeders. Entothyreos likely used its posterior limb pairs to anchor itself to a raised substrate (e.g. sponges), and then used its frontal limb pairs to sieve food particles from the water column. The posterior portion of the body is often poorly preserved, which the authors speculate could be caused by kinetic force of burial (a mudflow) tearing apart the body, as the anchoring claws are still firmly embedded in substrate. Comparable signs of tearing are seen in other sessile Burgess Shale taxa.