Bivalves percés - Clams drilled

Cliquez sur une photo pour une vue agrandie utilisez la touche F11 pour plus de confort

Click on a picture for a larger view seashell,shell,cowrie, use the F11 key for comfort.


bivalves percés

Différents bivalves de l'Aquitaine (Mont de Marsan), Miocène, Aquitanien. Ce sont très certainement des natices (Naticidae) qui sont à l'origine des trous compte-tenu des proies.

Different bivalve of Aquitaine (Mont de Marsan), Miocene, Aquitanian. This is certainly the moon snails that are the cause of holes in view of prey.

Article japonais sur le sujet (pompé sur le net mais je ne sais à qui demander!!!):Japanese paper on the subject (stolen on the net but I do not know who to ask !!!):

TEMPORAL PATTERN OF NATICID PREDATION ON GLYCYMERIS YESSOENSIS (SOWERBY) DURING THE LATE CENOZOIC IN JAPAN

KAZUTAKA AMANO1

1 Department of Geoscience, Joetsu University of Education, 1 Yamayashiki, Joetsu City, Niigata Prefecture, 943-8512, Japan amano@juen.ac.jp

No temporal trend in the intensity of drilling by naticids on Glycymeris yessoensis can be recognized during the late Cenozoic. Drilling sites shifted from the umbo to the center of the valve during the late Cenozoic. This shift might reflect the change of predators from Glossaulax in the Miocene to Cryptonatica or Euspira in the Pleistocene. Borehole sites in the middle Pleistocene were more stereotyped than in the early Pleistocene population despite the same predators. Edge drilling, which is a faster drilling method, first appeared in the population showing high drilling intensities in the early Pleistocene. Because a prediction of the hypothesis of escalation is that changes in predators' behavior developed through time, these changes in drilling location may be the results of escalation. In contrast with the stereotypic trend of borehole sites, correlation coefficients of predator-prey size decreased from the early to the middle Pleistocene.

Plus de documentation: ICI