Palaeobiogeographical provenance, taphonomy, and mode of life of Aturia cubaensis (Cephalopoda, Nautiloidea) from Cainozoic deposits of Chile

Abstract

The presence of Aturia cubaensis (Lea) is reported from several Cainozoic localities along the central and southern Chilean coast. The shells are very well preserved and the ultrastructure of the shell, especially of the siphuncular tube, of A. cubaensis is described and the function of the siphuncular tube discussed. A. cubaensis shows an interesting distributional pattern in Chile, becoming more frequent towards higher latitudes. It occurs in the Navidad, Ranquil, and Lacui formations of central and southern Chile and the Cameronian Stage of Tierra del Fuego, spanning a time of Eocene-Oligocene to latest Miocene, possibly even earliest Pliocene. Tierra del Fuego is the southernmost record of this species. The preservation of Aturia in all these localities is exceptionally good, no incrustation and microboring is observed in the shells. Post-mortem shell breakage is present, but usually the phramocone is not destroyed. These records contradict either the subtropical to tropical nature of the genus Aturia or existing climatic reconstructions for the southeastern Pacific during the middle to late Cainozoic. A number of southern South American names for nautiloids are synonymized with A. cubaensis: Nautilus maldonadi Philippi, Nautilus caroliameghinoi Ihering, Aturia ( Sphenaturia) brueggeni Ihering, Aturia ( Sphenaturia) felschi Ihering. Nautilus araucanus Philippi and Nautilus magellanicus Philippi are nomina nuda but presumably also synonyms of A. cubaensis.