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Did shell-crushing predators drive the evolution of ammonoid septal shape?

Published online by Cambridge University Press:  13 April 2021

Erynn H. Johnson*
Affiliation:
Department of Earth and Environmental Science, University of Pennsylvania, Philadelphia, Pennsylvania 19104, U.S.A. E-mail: erynnj@upenn.edu, caja@seas.upenn.edu.
Briana M. DiMarco
Affiliation:
Department of Biology, Drexel University, Philadelphia, Pennsylvania 19104, U.S.A. E-mail: bmd78@drexel.edu
David J. Peterman
Affiliation:
Department of Earth and Environmental Sciences, Wright State University, Dayton, Ohio 45435, U.S.A
Aja M. Carter
Affiliation:
Department of Earth and Environmental Science, University of Pennsylvania, Philadelphia, Pennsylvania 19104, U.S.A. E-mail: erynnj@upenn.edu, caja@seas.upenn.edu.
Warren D. Allmon
Affiliation:
Paleontological Research Institution, Ithaca, New York 14850, U.S.A.; and Department of Earth and Atmospheric Science, Cornell University, Ithaca, New York 14850, U.S.A. E-mail: wda1@cornell.edu
*
*Corresponding author.

Abstract

For centuries, paleontologists have sought functional explanations for the uniquely complex internal walls (septa) of ammonoids, extinct shelled cephalopods. Ammonoid septa developed increasingly complex fractal margins, unlike any modern shell morphologies, throughout more than 300 million years of evolution. Some have suggested these morphologies provided increased resistance to shell-crushing predators. We perform the first physical compression experiments on model ammonoid septa using controlled, theoretical morphologies generated by computer-aided design and 3D printing. These biomechanical experiments reveal that increasing complexity of septal margins does not increase compression resistance. Our results raise the question of whether the evolution of septal shape may be tied closely to the placement of the siphuncle foramen (anatomic septal hole). Our tests demonstrate weakness in the centers of uniformly thick septa, supporting work suggesting reinforcement by shell thickening at the center of septa. These experiments highlight the importance of 3D reconstruction using idealized theoretical morphologies that permit the testing of long-held hypotheses of functional evolutionary drivers by recreating extinct morphologies once rendered physically untestable by the fossil record.

Information

Type
Articles
Copyright
Copyright © The Author(s), 2021. Published by Cambridge University Press on behalf of The Paleontological Society
Figure 0

Figure 1. Fossil and model septa. Images showing cephalopod septa (inner chamber walls) and sutures (where septa meet the outer shell wall); complexity decreases from left to right. Top row: sutures visible on fossil cephalopods from the Paleontological Research Institution research collections: A, ammonite sutures on Cadoceras sublaeve (PRI 70580); B, ceratitic sutures on Gymnotoceras beachi (PRI 43629); C, goniatitic Imitoceras rotatorium (PRI 44566); D, nautiloid sutures on Actinoceras beloitense (PRI 70326). Bottom row: computer-generated models of cephalopod chambers, bisected to show cross section of septa. E, ammonitic septa of Diplomoceras; F, ceratitic septa of Otoceras; G, goniatitic septa of Schistoceras; H, nautiloid septa of Eifeloceras.

Figure 1

Figure 2. Fossil, computer-generated, and 3D-printed ammonoids. Comparison of fossil and model ammonoids. A, Baculites sp. (PRI 70605). Fossil is infilled such that suture lines remain visible. B, 3D Baculites model with slightly laterally compressed shell generated in Blender 2.76. C, 3D-printed Diplomoceras model created in Blender, printed on Formlabs Form 2.

Figure 2

Table 1. Taxa used to make models. List of select septal types and representative genus and species whose sutures were used to create 3D models (Arkell et al. 1957; Jones 1963; Teichert et al. 1964; Wright 1996; Peterman and Barton 2019). Scaling exponents used to quantify complexity following Peterman and Barton (2019).

Figure 3

Figure 3. Models in compression. Sample images of models during compression tests in Instron Universal testing machine. Instron plates are lined with sandpaper. Top row: ammonitic models A, Diplomoceras; B, Baculites; C, Douvilleiceras. Second row: ceratitic models D, Otoceras; E, Pearylandites; F, Xenaspis. Third row: goniatitic models G, Schistoceras; H, Manticoceras; I, Diaboloceras. Bottom row: nautiloid models J, Eifeloceras; K, Endoceras; L, Orthoceras.

Figure 4

Figure 4. Septal shape and peak load sustained. A, Violin plot peak load (kN) sustained by models with different septal types decreasing in complexity from left to right: ammonitic, ceratitic, goniatitic, nautiloid, and straight (control). Width of spindles indicates distribution of data points. Means for each septal shape are represented by red triangles. Straight septa (representing controls) were stronger than ammonitic and goniatitic septa (p ≤ 0.025). There was no significant difference between models of real septal types (ammonitic, ceratitic, goniatitic, or nautiloid). B, Examples of load (kN) vs. displacement (mm) curves for each septal shape tested. Figure created in ggplot2 (Wickham 2016).

Figure 5

Figure 5. Peak loads of different septal morphologies. Peak loads sustained by models based on genera with different septal morphologies. A, Violin plot peak load (kN) sustained by models of different genera decreasing in septal complexity from left to right. Width of spindles indicated distribution of data points. Load (kN) versus displacement (mm) curves for B, ammonitic; C, ceratitic; D, goniatitic; E, nautiloid and straight septa. Diplo., Diplomoceras; Bac., Baculites; Douvill., Douvilleiceras; Oto., Otoceras; Pearyl., Pearylandites; Xen., Xenaspis; Schisto., Schistoceras; Mantico., Manticoceras; Diabolo., Diaboloceras; Eifelo., Eifeloceras; Endo., Endoceras; Ortho., Orthoceras.

Figure 6

Table 2. Dunn test significant pairwise comparisons (p ≤ 0.025) of 3D-printed cephalopod models. Gray boxes show significant differences where the genus in the first row was stronger than the affiliated genus in the first column (e.g., Diplomoceras was significantly stronger than Baculites).