title: Systematics, phylogeny, and taphonomy of ghost shrimps (Decapoda): a perspective from the fossil record.
abstract: Ghost shrimps of Callianassidae and Ctenochelidae are soft-bodied, usually heterochelous decapods representing major bioturbators of muddy and sandy (sub)marine substrates. Ghost shrimps have a robust fossil record spanning from the Early Cretaceous (~ 133 Ma) to the Holocene and their remains are present in most assemblages of Cenozoic decapod crustaceans. Their taxonomic interpretation is in flux, mainly because the generic assignment is hindered by their insufficient preservation and disagreement in the biological classification. Furthermore, numerous taxa are incorrectly classified within the catch-all taxonCallianassa. To show the historical patterns in describing fossil ghost shrimps and to evaluate taphonomic aspects influencing the attribution of ghost shrimp remains to higher level taxa, a database of all fossil species treated at some time as belonging to the group has been compiled: 250 / 274 species are considered valid ghost shrimp taxa herein. More than half of these taxa (160 species, 58.4%) are known only from distal cheliped elements, i.e., dactylus and / or propodus, due to the more calcified cuticle locally. Rarely, ghost shrimps are preservedin situin burrows or in direct association with them, and several previously unpublished occurrences are reported herein. For generic assignment, fossil material should be compared to living species because many of them have modern relatives. Heterochely, intraspecific variation, ontogenetic changes and sexual dimorphism are all factors that have to be taken into account when working with fossil ghost shrimps. Distal elements are usually more variable than proximal ones. Preliminary results suggest that the ghost shrimp clade emerged not before the Hauterivian (~ 133 Ma). The divergence of Ctenochelidae and Paracalliacinae is estimated to occur within the interval of Hauterivian to Albian (133-100 Ma). Callichirinae and Eucalliacinae likely diverged later during the Late Cretaceous (100-66 Ma), whereas Callianassinae did not appear before the Eocene (56 Ma).
authors: Geological-Paleontological Department, Natural History Museum Vienna, Burgring 7, 1010 Vienna, Austria; Matúš Hyžný [hyzny.matus@gmail.com]; Geological-Paleontological Department, Natural History Museum Vienna, Burgring 7, 1010 Vienna, Austria; Matúš Hyžný [hyzny.matus@gmail.com].
authors: Matúš
authors: M
authors: Hyžný
authors: Florida Museum of Natural History, University of Florida, 1659 Museum Road, PO Box 117800, Gainesville, FL 32611, USA; Adiël A. Klompmaker [ adielklompmaker@gmail.com ].
authors: Adiël A
authors: AA
authors: Klompmaker
keywords: Callianassidae; Crustacea; Ctenochelidae; Decapoda; burrow; fossil record; heterochely; phylogeny; taphonomy; taxonomy