New subfossil bones of a Réunion Giant Tortoise, Cylindraspis indica (Schneider, 1783), from a lava tunnel under a mid-elevation windward rainforest on Réunion Island

Authors

  • Arnaud Rhumeur Initiative pour la Restauration Écologique en Milieu Insulaire, Saint-Pierre, Réunion, France
  • Sébastien Albert Université de Lorraine, AgroParisTech, Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement, Silva, Nancy, France https://orcid.org/0000-0002-4070-2117
  • Kalyan Leclerc Initiative pour la Restauration Écologique en Milieu Insulaire, Saint-Pierre, Réunion, France
  • Sohan Sauroy-Toucouère Initiative pour la Restauration Écologique en Milieu Insulaire, Saint-Pierre, Réunion, France https://orcid.org/0000-0003-1137-5484
  • Gilles David Derand Initiative pour la Restauration Écologique en Milieu Insulaire, Saint-Pierre, Réunion, France
  • Grégory Cazanove Muséum d'Histoire naturelle de La Réunion, Saint-Denis, Réunion, France https://orcid.org/0000-0001-6756-6269
  • Gaël Potin Muséum d'Histoire naturelle de La Réunion, Saint-Denis, Réunion, France
  • Dominique Strasberg Université de la Réunion, Saint-Denis, Réunion, France https://orcid.org/0000-0003-3012-252X
  • Hélène Silhouette Institut National de Recherches Archéologiques Préventives, Bègles, France
  • Jérémie Souchet Association Nature Océan Indien, Petite-Île, Réunion, France https://orcid.org/0000-0001-9296-1332
  • Julian P. Hume Natural History Museum, Tring, United Kingdom https://orcid.org/0000-0001-5890-9696

Keywords:

Réunion Island, Cylindraspis indica, subfossil, palaeontology, extinct tortoise, ecological restoration

Abstract

We report the discovery of subfossil remains of a juvenile Réunion Giant Tortoise, Cylindraspis indica, in a lava tunnel beneath remnant mid-elevation native tropical rainforest on Réunion Island. Located at an elevation of 726 m in the Plaine des Grègues managed forest, this find is the highest fossil record of the species on the island. For the first time, these remains provide paleontological confirmation of historical accounts from the 17th–18th century reporting tortoises in upland areas. These specimens also highlight the potential of submontane and montane lava tubes as paleontological archives. Radiocarbon dating yielded an age of 665 ± 30 BP with 95.4% probability, corresponding to AD 1296–1399 and indicating that the specimen predates permanent human settlement (ca. 1665) by approximately three centuries. Although palynological analyses were unsuccessful, flora inventories revealed a diverse assemblage of native fleshy-fruited trees, suggesting that C. indica may have played a crucial role as megafaunal seed disperser. Beyond its paleontological significance, this discovery thus lends legitimacy to rewilding experiments involving functional analogues of extinct tortoises.

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Published

2026-06-10

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