T205 Growing a Skeleton: Methodological and Theoretical Approaches to Unraveling the Stories Preserved in Skeletal Materials II
Thursday, 29 October 2020
1:30 PM - 5:30 PM
Meeting Rooms
PRESERVED INTERNAL MEMBRANES OF DINOSAUR EGGSHELL FRAGMENTS, UPPER JURASSIC MORRISON FORMATION, DALTON WELLS, UTAH
Paper number: T205-13
Program: Technical Sessions
Time: 4:10 PM – 4:20 PM
Authors
-
Ian StoutKutztown University, Kutztown, PA
-
Grace HetrickKutztown University, Kutztown, PA
-
Abigail KeeblerWest Chester University of PA, Perkiomenville, PA
-
Edward SimpsonKutztown University, Kutztown, PA
-
Michael WizevichCentral Connecticut State University, New Britain, CT
Abstract
The internal membrane of modern bird eggs is composed of type X collagen fibers that vary in lengths and widths and comprise several interlaced layers. Embedded in this fibrous matrix are “calcium reserve” deposits that are utilized for embryonic development. Features common to both modern birds’ eggs and the dinosaur egg fragments include: 1) irregular shaped-calcium carbonate “floating” in an organic matrix, 2) external calcium carbonate molds of fibers in the mammillary bodies that form the foundation for building the egg shell, 3) three-dimensional organic fiber matrix, and 4) organic matrix with oval to circular pore. Unlike modern birds’ eggs, the dinosaur eggs’ calcium carbonate tubes were observed to have organic fibers inside that are traced into a fluidized/gel deposit.
The recognition of well-preserved internal membrane features on fragments of hard-shelled dinosaur eggs from the Morrison Formation indicates newfound opportunities to explore the preservation of probable organic compounds associated with fragmental dinosaur eggs.
Geological Society of America Abstracts with Programs. Vol. 52, No. 6
doi: 10.1130/abs/2020AM-357344
© Copyright 2020 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.