Abstract

The Arkadelphia Formation—Midway Group (Maastrichtian—Paleocene) contact near Malvern, Arkansas preserves a K-Pg boundary assemblage of turtle species consisting of skull, shell, and non-shell postcranial skeletal elements. The Malvern turtles are preserved within a coquina lag deposit that comprises the basalmost Midway Group and also contains an abundance of other reptiles, as well as chondrichthyans, osteichthyans, and invertebrates. This coquina lag deposit records a complex taphonomic history of exhumation and reburial of vertebrate skeletal elements along a dynamic ancestral shoreline in southwestern Arkansas during the late Cretaceous-early Paleocene. Based on stratigraphic occurrence, the Malvern turtle assemblage indicates that these marine reptiles were living at or near the time of the K-Pg mass extinction and represent some of the latest Cretaceous turtles yet recovered from the Gulf Coastal Plain of the United States.

Highlights

  • To date, only a few published reports identify the occurrence of fossil turtles from theLate Cretaceous of Arkansas

  • InteriorSeaway; Seaway; physiographic provinces in Arkansas turtle discussed in this study indicated by by (X);(X); (C)(C)

  • Formation—Midway Group turtle site discussed in this study identified by arrows

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Summary

Introduction

Only a few published reports identify the occurrence of fossil turtles from the. The earliest of these reports was written over half a century ago [1], and described a new species of turtle from the Brownstone Formation which Schmidt named Podocnemis barberi. Schmidt [2] described two additional turtle species, Phyllemys barberi and Catapleura arkansasensis from the Marlbrook Marl. The present report identifies an assemblage of skull, shell, and non-shell postcranial turtle skeletal elements of uncertain taxonomic status. This turtle assemblage consists of nineteen specimens preserved in matrix and was recovered from a coquina lag deposit composing the basalmost Midway Group along the Ouachita River in Hot. Spring County, Arkansas (Figures 1 and 2).

Location
Age ofMultiple the Arkadelphia
Geologic
Methods
Repository
Turtle neurals and peripherals from the basalmost
Turtle costals from the basalmost
Turtle
Origin of the Turtle Lag Deposit
Impact Generated Tsunamis for Lag Deposit Formation
Third Order Sea Level Generated Lag Deposits
Combined Impact Generated Tsunamis and Third Order Sea Level Cyclicity
Future Research
Full Text
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