Exoskeletal structure in the Ordovician trilobiteFlexicalymene

Abstract

Scanning Electron Microscope study of the exoskeletal ultrastructure of secondarily phosphatized material of Flexicalymene sp. from the Upper Ordovician Maquoketa Shale, Iowa, USA, shows that the exocuticle, comprising 20% of the total exoskeletal thickness, is composed of horizontal laminar units between 0.2 and 1 .mu.m thick. These units consist of primary mineralized organic fibers which form horizontal laminae interconnected by inter-laminae. The endocuticle is considerably more mineralized than the exocuticle, its original organic structure cannot be observed in untreated preparations. Etching with chromium sulfate reveals: horizontal organic laminar units, 0.2-2 .mu.m thick, and pore canals with non-twisted walls about 0.3 .mu.m in diameter. Exuvia cannot be distinguished from the exoskeletons of dead animals. The exoskeletal ultrastructure in trilobites agrees essentially with that in crustaceans.