Abstract

The oldest preserved visual systems are to be found in the extinct trilobites, marine euarthropods which existed between about 520 and 250 million years ago. Because they possessed a calcified cuticle, they have a good fossil record, and commonly the lens-bearing surfaces of their paired compound eyes are well preserved. The sublensar structures, however, remain unknown. Three kinds of eyes have been distinguished. Holochroal eyes, apomorphic for trilobites, typically have many contiguous small lenses, set on a kidney-shaped visual surface. Lens optics, angular range of vision, and ontogeny have been established for many compound eyes. Some pelagic trilobites have enormous eyes, subtending a panoramic field of view. Schizochroal eyes are found only in one group, the phacopids (Ordovician to Devonian). These have large lenses, separated from each other by cuticular material, and the lenses have a complex doublet or triplet internal structure, which could focus light sharply. The optics of phacopid eyes are becoming increasingly well known despite the fact that there are no direct counterparts in any living arthropods today. Schizochroal eyes are apomorphic for phacopids and were derived by paedomorphosis from a holochroal precursor. Abathochroal eyes are confined to a short-lived Cambrian group, the eodiscids (of which most representatives were blind). Less is known about them than other trilobite eyes and their origins remain obscure. Some trilobite groups had no eyes, but had other kinds of sensory organs. In Upper Devonian times several groups of trilobites independently underwent progressive eye-reduction leading to blindness, related to prevailing environmental conditions of the time. The last trilobites (of Carboniferous and Permian age), however, had normal holochroal eyes, which persisted until the final extinction of trilobites at the end of the Permian.

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