Abstract

Pellornis mikkelseni is an early gruiform from the latest Paleocene-earliest Eocene Fur Formation of Denmark. At approximately 54 million years old, it is among the earliest clear records of the Gruiformes. The holotype specimen, and only material thus far recognised, was originally considered to comprise a partial postcranial skeleton. However, additional mechanical preparation of the nodule containing the holotype revealed that the skeleton is nearly complete and includes a well-preserved skull. In addition to extracting new information from the holotype, we identify and describe two additional specimens of P. mikkelseni which reveal further morphological details of the skeleton. Together, these specimens show that P. mikkelseni possessed a schizorhinal skull and shared many features with the well-known Paleogene Messelornithidae (“Messel rails”). To reassess the phylogenetic position of P. mikkelseni, we modified an existing morphological dataset by adding 20 characters, four extant gruiform taxa, six extinct gruiform taxa, and novel scorings based on the holotype and referred specimens. Phylogenetic analyses recover a clade containing P. mikkelseni, Messelornis, Songzia and crown Ralloidea, supporting P. mikkelseni as a crown gruiform. The phylogenetic position of P. mikkelseni illustrates that some recent divergence time analyses have underestimated the age of crown Gruiformes. Our results suggest a Paleocene origin for this important clade, bolstering evidence for a rapid early radiation of Neoaves following the end-Cretaceous mass extinction.

Highlights

  • Extant Gruiformes comprise six family-level clades: finfoots (Heliornithidae), flufftails (Sarothruridae), rails (Rallidae), trumpeters (Psophiidae), the monotypic limpkin (Aramidae), and cranes (Gruidae)

  • We describe numerous novel elements from the Pellornis mikkelseni holotype based on additional preparation of the holotype specimen and refer and describe two additional specimens of P. mikkelseni

  • Unconstrained parsimony heuristic analysis resulted in 34,720 most parsimonious trees (MPTs) of 326 steps. This analysis recovered a large polytomy with all relationships within Gruiformes unresolved with the exception of Gruoidea, in which Parvigrus pohli was placed as the sister-taxon of Gruidae+Aramidae (CI = 0.356, RI = 0.705, RC = 0.251, HI = 0.644)

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Summary

Introduction

Extant Gruiformes comprise six family-level clades: finfoots (Heliornithidae), flufftails (Sarothruridae), rails (Rallidae), trumpeters (Psophiidae), the monotypic limpkin (Aramidae), and cranes (Gruidae). Gruiformes is further subdivided into Ralloidea (Heliornithidae, Sarothruridae, Rallidae) and Gruoidea (Psophiidae, Aramidae, Gruidae)—a division uniformly supported across recent phylogenetic studies [1,2,3,4,5,6,7,8,9,10,11,12,13,14,15,16,17,18]. Several morphological and molecular phylogenetic studies have attempted to resolve the higher-level interrelationships of extant Gruiformes [13,14,15,16,17]. The composition and phylogenetic position of the rail-like Sarothruridae with respect to Heliornithidae and Rallidae remains controversial [12,17,18], with implications for informing macroevolutionary patterns within Ralloidea

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