Title of article :
Rhinocerotid tooth enamel 18O/16O variability between 23 and 12 Ma in southwestern France
Author/Authors :
Bentaleb، نويسنده , , Ilhem and Langlois، نويسنده , , Cyril and Martin، نويسنده , , Céline and Iacumin، نويسنده , , Paula and Carré، نويسنده , , Matthieu and Antoine، نويسنده , , Pierre-Olivier and Duranthon، نويسنده , , Francis and Moussa، نويسنده , , Issam and Jaeger، نويسنده , , Jean-Jacques and Barrett، نويسنده , , Nicholas and Kandorp، نويسنده , , Ron، نويسنده ,
Issue Information :
روزنامه با شماره پیاپی سال 2006
Abstract :
The relationship between the oxygen isotope ratio of mammal tooth enamel and that of drinking water was used to reconstruct changes in the Miocene oxygen isotope ratio of rainfall (meteoric water δ 18 OMW). These, in turn, are related to climatic parameters (temperature, precipitation and evaporation rate). δ 18 O values of rhinocerotid teeth from the Aquitaine Basin (southwestern France) suggest a significant climatic change between 17 and 12 Ma, characterized by cooling together with precipitation increase, in agreement with other terrestrial and oceanic records. To cite this article: I. Bentaleb et al., C. R. Geoscience 338 (2006).
Keywords :
Miocene , oxygen isotopes , Enamel , Palaeoclimate , Mammal , Mammifère , Aquitaine , Aquitaine , paléoclimats , isotopes de lיoxygène , ةmail , Miocène
Journal title :
Comptes Rendus Geoscience
Journal title :
Comptes Rendus Geoscience
