| Erbenochile Fossil range: Devonian | |
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| Scientific classification
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Acastidae | |
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Erbenochile | |
Erbenochile is a genus of spinose phacopid (acastid) trilobite found in Lower to Middle Devonian age rocks from Algeria and Morocco.[1][2] Originally described from an isolated pygidium,[1] the first complete articulated specimen of E. erbeni revealed the presence of extraordinarily tall eyes:
- ""Straight-sided towers of lenses... with [upto] 18 lenses in a vertical file""
- — Fortey & Chatterton (2003)[3]
Number of lenses has been estimated at 560[3] or 450[4] incomplete preservation accounting for the uncertainty. A lens count of 18 lenses per file is unusually high (twice that of closely related genus) and accounts for the height of the eye, as opposed to a noticeable increase in the size of the individual lenses.[4] A recently found undescribed species of Erbenochile has smaller eyes, with fewer files (33-35) and fewer lenses per file (15 max) than E. erbeni.[4] E. erbeni eyes allow full 360 degree coverage in the horizontal plane and were high enough to allow the trilobite to see backwards over its thorax. The presence of eye shades, blocking glare from over head, validates the suggestion that (at least some) trilobites were diurnal and not nocturnal,
- ""a detail of life habit which had previously been equivocal: Eyeshades are no use in the dark.""
- — Fortey & Chatterton (2003)[3]
Distribution[]
- E. erbeni has been found in the latest Lower Devonian of Algeria (upper Emsian strata at Ougarta) and Morocco (Timrhanrhart Formation at section Foum Zguid III).
- E. issoumourensis is known from the latest Lower Devonian or possibly earliest middle Devonian of Morocco (upper Emsian or lower Eifelian, Erbenochile bed, El Otfal Formation, Jbel Issoumour, near Alnif southeastern Morocco 30°58'14.5 N - 05°01'44.3W).
Description[]
Erbenochile is a trilobite with very large eyes, with 33–36 vertical rows of 13–19 lenses each. The lower edge of eye slightly overhangs the adjacent part of the free cheek. The most backward part of the glabella (or occipital ring), the rings of the thorax, and rings on the pygidium each have a prominent median spine. The thorax consists of 11 segments. The frontal band of each of the lateral parts of the thorax segments (in the so-called pleural region) are not adorned. The posterior bands have a row of distinct small spines. The large tailshield (or pygidium) has 11 pairs of spines along the edge, and one in the middle, and 10–11 pairs of well-defined segments. The frontal pleural bands of each segment on the pygidium is lower compared to the posterior pleural band, and lacks the small spines of the posterior pleural band. The posterior border of pygidium is longer medially than laterally.
Taxonomy[]
Gallery[]
References[]
- ^ a b Morzadec, P. (1995), "Erbenochile erbeni (Alberti), Trilobite de Dévonian inférieur d'Ougarta (Algerie).", Neues Jahrb. Geol. Paläontol. Monatsh. 10: 614-621
- ^ Alberti, G.K.B. (1981), "Beziehungen zwischen "herzynischen" Trilobitenfauna NW-Marokko und Deutschland (Unter- und Mittel-Devon)", Natur und Museum 110: 172-182
- ^ a b c Fortey, R.; Chatterton, B. (2003), "A Devonian Trilobite with an Eyeshade", Science 301: 1689
- ^ a b c Chatterton, B.; Fortey, R.; Brett, K.; Gibbs, S.; McKellar, R. (2006), "Trilobites from the Lower to Middle Devonian Timrhanrhart Formation, Jbel Gara el Zquilma, southern Morocco.", Palaeontographica Canadiana 25, ISBN 1-897095-15-5
External links[]
- Big-eye trilobite: Erbenochile - Natural History Museum (London) virtual tour
- Richard Fortey's book cover Fossils - key to the past features E. erbeni
fi:Erbenochile