Marrellomorpha
Marrellomorpha are an extinct group of arthropods known from the Cambrian to the Early Devonian. It is divided into two major groups, Marrellida and Acercostraca. They lacked mineralised hard parts, so are only known from areas of exceptional preservation, limiting their fossil distribution. The best known member is Marrella, with thousands of specimens found in the Cambrian aged Burgess Shale of Canada.
Description and ecology
The group is divided up into two major orders, Marrellida and Acercostraca. Both groups have cuticles that are not mineralised, unbranched antennae attached to the head section and a segmented trunk with a pair of biramous appendages attached to each trunk segment except the last. Marrellida is recognised by the possession of head shields with two or three pairs of elongate spine-like projections, and two or three attached pairs of uniramous head appendages, while Acercostraca have large ovoid dorsal shields that cover the entire upper half of the body, and up to five pairs of appendages attached to the head section.The trunks of marrellids are divided into numerous cylindrically-shaped segments. The endopods of the biramous trunk limbs of marrellids have six segments. The exopods of marrellids had an annulated appearance, and had numerous attached elongate lammelate setae and are thought to have functioned for respiration. The trunk limb exopods of at least some acercostracans were similar to those of marrellids.
Marrellids are either suggested to have swum close to the seafloor or have lived walking along the sea floor and to have used their hind trunk appendages to sift food particles, which were then passed forward by the limbs to the mouth. The posterior trunk appendages of at least some vachonisiid acercostracans have been suggested to have been used the same way, and are also suggested to have lived on the seafloor.
Taxonomy
Internal taxonomy
Internal taxonomy of Marrellomorpha after Moysiuk et al., 2022.- Acercostraca Lehmann, 1955
- * Skania Burgess Shale, Canada, Cambrian ? Kaili Formation, China, Cambrian
- * Primicaris Burgess Shale, Canada, Cambrian, Maotianshan Shales, China, Cambrian Stage 3
- * Vachonisiidae Tasch, 1969
- ** Xylokorys Coalbrookdale Formation, England, Silurian
- ** Vachonisia Hunsrück Slate, Germany, Lower Devonian
- ** Enosiaspis Fezouata Formation, Morocco, Early Ordovician
- Marrellida Størmer, 1959, pro Marrellina Raymond, 1920
- * Marrella Balang Formation, China, Cambrian Stage 4 Kaili Formation, China, Cambrian, Burgess Shale, Canada, Cambrian
- * Furca Letná Formation, Czech Republic, Upper Ordovician
- * "Furca mauretanica" Fezouata Formation, Morocco, Early Ordovician
- * "Mimetaster" florestaensis Floresta Formation Argentina, Lower Ordovician
- * Mimetasteridae Birenheide, 1971
- ** Tomlinsonus Kirkfield Formation, Canada, Late Ordovician
- ** Mimetaster Hunsrück Slate, Germany, Lower Devonian
Some studies have recovered Marrellomorpha as paraphyletic, with Marrellida and Acercostraca more closely related to other arthropods than they are to each other.
Relationship to other arthropods
Their phylogenetic position within arthropoda is uncertain, beyond being placed in Deuteropoda for their possession of biramous appendages. Various studies have alternatively placed them in the Arachnomorpha as relatives of Artiopoda, as related to Mandibulata, or as stem group euarthropods. The engimatic Cambrian arthropod Burgessia may be closely related to marrellomorphs. Some authors have proposed that they may be closely related to sea spiders within Chelicerata though the cladistical support for such a relationship is relatively weak. A 2025 paper found Marrellomorpha to be within total-group Mandibulata, as a paraphyletic group at the base of Artiopoda.Phylogeny
Internal phylogeny
After Legg, 2016.After Moysiuk et al., 2022.