REPORT OF SHELL PALEOPATHOLOGIES IN ANTARCTIC AMMONOIDS OF THE LÓPEZ DE BERTODANO FORMATION (LATE CRETACEOUS, ANTARCTIC PENINSULA)

Authors

  • Daniel A. Morón-Alfonso Asociación Paleontológica ArgentinaUniversidad de Buenos Aires. https://orcid.org/0000-0002-8865-8370
  • Leticia Luci Universidad de Buenos Aires, Facultad de Ciencias Exactas y Naturales, Departamento de Ciencias Geológicas, Área de Paleontología, Ciudad Universitaria, Pab. 2, C1428EGA, Buenos Aires, Argentina. CONICET-Universidad de Buenos Aires, Instituto de Estudios Andinos “Don Pablo Groeber” (IDEAN), Buenos Aires, Argentina. https://orcid.org/0000-0002-7283-1079
  • René Hoffmann Institute of Geology, Mineralogy, & Geophysics, Ruhr-Universität Bochum, 44801 Bochum, Germany. https://orcid.org/0000-0001-7992-1264
  • Verónica Vennari Instituto de Evolución, Ecología Histórica y Ambiente (IDEVEA), Universidad Tecnológica Nacional, Facultad Regional San Rafael (UTN-FRSR). Gral. J.J. Urquiza 314, M5602GCH, San Rafael, Mendoza, Argentina. Consejo Nacional de Investigaciones, Científicas y Técnicas (CONICET).
  • Marcela Cichowolski Instituto de Estudios Andinos Don Pablo Groeber (UBA-CONICET)

DOI:

https://doi.org/10.5710/AMGH.20.08.2024.3602

Keywords:

Ammonoid, Ammonite, Paleopathology, Scar, Pathologies, Injuries, injury, Traces, Shell wall

Abstract

This study documents ten potential cases of paleopathologies observed in Antarctic ammonoids from the López de Bertodano Formation. Specifically, four cases are identified in the species Grossouvrites joharae, while six are exhibited by Maorites densicostatus shells. The observed pathologies vary in severity, ranging from minor lesions along the apertural margin to more extensive abnormalities or injuries affecting up to 180° of the whorl. These anomalies include alterations in ribbing patterns, small constrictions, and malformation of ornamental elements. Various interpretations have been proposed to explain these pathologies, such as fractures or injuries that could affect the shell secreting soft-tissues (resulting in recurrent anomalies during healing), illness, toxicity, and/or environmental stress. Additionally, a specific case involving a M. densicostatus specimen is described, wherein three enigmatic annular traces were observed in the ventral region of a steinkern of the body chamber. These traces were interpreted as likely attachment sites of an unknown organism following soft-tissues degradation. The discovery of these paleopathologies can be attributed to several factors, including the excellent preservation state of the available specimens, which retained multiple layers of the original shell wall, the utilization of methodologies aimed at enhancing the visualization of surface features (such as Reflectance Transformation Imaging), and specific characteristics of the unit (Klb9) from which the majority of the specimens were recovered.

Published

2024-12-27

How to Cite

REPORT OF SHELL PALEOPATHOLOGIES IN ANTARCTIC AMMONOIDS OF THE LÓPEZ DE BERTODANO FORMATION (LATE CRETACEOUS, ANTARCTIC PENINSULA). (2024). Ameghiniana, 61(5), 194-212. https://doi.org/10.5710/AMGH.20.08.2024.3602