The Arandaspida, or arandaspids, are a small group of armored, fossil jawless vertebrates, which lived in the Ordovician (from -480 to -440 million years ago). They are thus among the earliest known craniates, if one excepts the controversial Euconodonta. They are regarded as belonging to the Pteraspidomorphi, because of the large, median dorsal and ventral plates of their head armor. Arandaspids were marine and are recorded only from Australia and South America (Bolivia and Argentina).
Arandaspids are characterized by:
- Frontally placed eyes, included in an anterior notch of the dorsal shield.
- long, posteriorly slanting series of about twenty diamond-shaped platelets which separate the dorsal from the ventral shield of the head armor. Between these platelets open minute external gill openings.
The head armor of arandaspids is elongated, fusiform, with a rather flat dorsal shield, and a bulging ventral shield. The eyes, surrounded by a sclerotic ring, are housed in a notch at the anterior end of the dorsal shield. The nostrils are nor clearly located, but may have been situated between the eyes. Ventrally, the ventral lip of the mouth is armed with long series of small oral plates which recall those of heterostracans. In the anterior part of the dorsal shield are two, closely-set holes, which have been thought to be a paired pineal opening, but which are more likely the external openings of the endolymphatic ducts. The gill openings are probably numerous (more than 15) and minute. They opened between the diamond-shaped platelets which separate the dorsal from the ventral shield.
The body is covered with rod-shaped scales arranged in chevrons, and the tail is probably pad-shaped and diphycercal. The dermal bones of arandaspids consist of aspidine (acellular bone) and are ornamented with oakleaf-shaped tubercles which seem to contain no dentine. The sensory-lines were housed in narrow grooves between the tubercles.
The Arandaspida comprise four monospecific genera, Arandaspis, Porophoraspis, Sacabambaspis, and Andinaspis, which occur in the Middle Ordovician of Australia, Bolivia, and Argentina, Sacabambaspis is the best known genus. Fragments of arandaspid bones are, however known from the base (Arenig; 480 million years) to the top (Ashgill; 440 million years) of the Ordovician. They are thus the earliest known undisputed craniate remains.
To date, there is no phylogeny of the Arandaspida and, considering the fragmentary state of the material of Porophoraspis and Andinaspis, the only available characteristics would be in the aspect of the dermal ornamentation. The tubercles of Arandaspis are drop-shaped and scalloped, those of Sacabambaspis and Andinaspis oakleaf-shaped, and those of Porophoraspis are perforated by large pores. Which of these types of ornamentation is primitive for the group is unknown, although one may note that the earliest known arandaspid fragments are of the Porophoraspis type.
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Gagnier, P. Y. (1993b). Sacabambaspis janvieri, Vertébré ordovicien de Bolivie. 2. Analyse phylogénétique. Annales de Paléontologie, 79, 119-166.
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Shergold, J. H. (1991). Late Proterozoic and Early Palaeozoic palaeontology and biostratigraphy of the Amadeus Basin. In Geological and Geophysical Studies in the Amadeus basin, Central Australia (ed. R. J. Korsch and J. M. Kennard). Bulletin of the Bureau of Mineral Resources, 236, 97-111.
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