A review of exceptional preservation in fossil ostracods (Ostracoda, Crustacea)

Abstract

Ostracods are the most abundantly preserved arthropod group in the fossil record, but they are almost entirely represented only by their calcitic carapaces. In over two hundred years of fossil ostracod research, only about 33 occurrences of fossil ostracods that include preserved appendages, or soft parts, have been reported. These range from the Ordovician through to the Holocene, and are from a wide range of paleoenvironments, including the seas, brackish inlets, lakes, caves, and the edges of ancient forests. Preservation includes silica, phosphate, goethite, pyrite or calcite mineralization replacing or coating soft parts, or direct preservation of the chitinous body and appendages, such as with amber entombment and mummification. Although rare, they have provided information on the morphology of some of the earliest ostracods, given clues about phylogenetic relationships of extinct groups, and demonstrated remarkably long periods of evolutionary stasis. Preserved sexual organs, eggs, brooded juveniles and even spermatozoa have given valuable insights into the reproduction of the group. Technological advances, such as scanning electron microscopy and more recently micro- and nanotomography, have dramatically expanded our capabilities to study these specimens, even down to the sub-cellular level. This review presents these occurrences in a historical context, from the first to the most recently reported, and highlights how these discoveries have contributed to our understanding of ostracod evolution.