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Landman N.H., Mapes R.H., Cochran J.K., Lignier V., Hembree D.I., Goiran C., Folcher Eric, Brunet P. (2014). An unusual occurrence of Nautilus macromphalus in a cenote in the Loyalty Islands (New Caledonia). Plos One, e113372 [13 p.] ISSN 1932-6203

Fichier PDF disponiblehttp://horizon.documentation.ird.fr/exl-doc/pleins_textes/divers15-11/010065811.pdf[ PDF Link ]

Lien direct chez l'éditeur doi:10.1371/journal.pone.0113372

An unusual occurrence of Nautilus macromphalus in a cenote in the Loyalty Islands (New Caledonia)
Année de publication2014
Type de documentArticle référencé dans le Web of Science WOS:000349128700025
AuteursLandman N.H., Mapes R.H., Cochran J.K., Lignier V., Hembree D.I., Goiran C., Folcher Eric, Brunet P.
SourcePlos One, 2014, e113372 [13 p.] ISSN 1932-6203
RésuméExploration of a landlocked cenote on Lifou (Loyalty Islands) revealed 37 shells of the cephalopod Nautilus macromphalus Sowerby, 1849, in saltwater on the cenote floor, approximately 40 m below the water surface. The occurrence of these shells is unusual because N. macromphalus is restricted to the open marine waters surrounding the island. All of the shells are mature, and nearly all of them are unbroken, with faded red-brown color stripes. We analyzed seven shells to determine their age. Radiocarbon dating yielded ages of 6380¡30 to 7095¡30 y BP. The 238U-series radionuclides 210Pb (half-life 522.3 y) and 226Ra (half-life 51600 y) also were measured. Two of the samples showed radioactive equilibrium between the nuclides, consistent with the old radiocarbon dates, but the other five samples showed excess 210Pb. When corrected for radioactive decay, the 226Ra activities were much greater than those found in living Nautilus. We conclude that exposure to high activities of 222Rn and 226Ra in the salty groundwater of the cenote altered the activities originally incorporated into the shells. Human placement of the shells in the cavity is rejected based on their radiocarbon age and the geometry of the cenote. The most probable explanation is that the animals entered the flooded karstic system through a connection on the seaward side at approximately 7,000 y BP, during an interval of slowly rising sea level. Unable to find an exit and/or due to anoxic bottom waters, the animals were trapped and died inside. The open connection with the sea persisted for ,700 y, but after ,6400 y BP, the connection was lost, probably due to a roof collapse. This is a rare example of Nautilus in a karstic coastal basin and provides a minimum age for the appearance of N. macromphalus in the Loyalty Islands.
Plan de classementAutres invertébrés [034BIOINV05]
LocalisationFonds IRD [F B010065811]
Identifiant IRDfdi:010065811
Lien permanenthttp://www.documentation.ird.fr/hor/fdi:010065811

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