Walliserops

Walliserops Temporal range: Upper Emsian and Lower Eifelian PreЄ Є O S D C P T J K Pg N
File:Walliserops trifurcatus, Early Devonian, Timrhanrhart Formation, Jbel Gara el Zguilma, Draa Valley, Morocco - Houston Museum of Natural Science - DSC01584.JPG
Walliserops trifurcatus
Scientific classification
Kingdom:	Animalia
Phylum:	Arthropoda
Class:	Trilobita
Order:	Phacopida
Family:	Acastidae
Genus:	Walliserops
Type species
Walliserops trifurcatus Morzadec, 2001
Species
W. trifurcatus Morzadec, 2001 W. hammii Chatterton et al., 2006 W. lindoei Chatterton & Gibb, 2010 W. tridens Chatterton et al., 2006

Walliserops (named after Prof. O. Walliser of Göttingen) is a genus of spinose phacopid trilobite, of the family Acastidae, found in Lower to Middle Devonian age rocks from the Anti-Atlas Mountains of Morocco. All species of Walliserops possess a three-pronged "trident" that protrudes from the glabella. Walliserops is most closely related to the genus Comura.

Walliserops was originally erected for a single species, W. trifurcatus. Later, two other species were assigned: W. hammii & W. tridens. All three currently described species come from the same strata near Foum Zguid in southern Morocco. Three as yet un-described species are recorded from other locations.

Early reports of "trident" trilobites and placement within the proposed new genus "Parabolops" ("parabola face") - long tridents being placed within "P. neptunis", short tridents placed within "P. hammi" - were pre-empted by the publication of the detailed analysis of Walliserops.

Departures from bilateral symmetry are an unusual feature within Walliserops species, most clearly shown by the curved occipital spine of W. hammii taking a noticeable curl to one side. The regular development of these features in multiple specimens suggest a genetically controlled feature of the genus and not mutations or pathology. Most of the exceptions to bilateral symmetry noted (and also the absence of spines on the first two thoracic segments) can be explained by adaptations allowing the trident to be held off the sea floor while walking. Between the species there are variations in the extent of departure from bilateral symmetry: W. trifurcatus, with a long trident that is curved away from the seabed, has less obvious departures from bilateral symmetry than W. hammii, with a short trident close to the seabed.

The function of the trident itself is poorly understood. With the amount of energy and nutrients expended in growing such a large adornment (probably multiple times as the trilobite shed its skin) its function was clearly important. Although a number of suggestions have been made (e.g. sensory apparatus, disguise or protection), the most satisfactory current explanation is that the trident served as "horns" similar to present day beetles.

Sexual dimorphism was an intriguing prospect (longer trident forms as jousting males) when only two species (or possible dimorphs) were known. With the description of three species from the same location, polymorphism (e.g. caste system in ants and bees) was another prospect but seemed unlikely. Although the presence of horns strongly suggests sexual dimorphism, lack of data on numerous fronts currently prevents firm conclusions from being drawn.

Sexual dimorphism in any trilobite exoskeleton has not yet been satisfactorily demonstrated and any decision to regard evidence as sexual dimorphism or as subspecific/specific difference(s) will be arbitrary.

— Whittington, 1997

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Walliserops trifurcatus

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Walliserops tridens

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Walliserops n. sp. undescribed species

External links

• Virtual tour of W. hammii, Natural History Museum
• Example of W. trifurcatus, University of Alberta
• Earliest combatants in sexual contests revealed, New Scientist
• W. trifurcatus, Fossil Mall