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Stable oxygen isotopes in freshwater mussels (Unionidae) as a proxy for late Holocene floods and droughts of Rhine and Meuse Emma Versteegh Hubert Vonhof Simon Troelstra Dick Kroon
Freshwater mussels ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Stable oxygen isotopes
Rivers Rhine and Meuse
δ 18 O rivers Glacier melting High discharge Flood Dry summer
Aim ,[object Object],[object Object],[object Object],[object Object],[object Object]
Methods ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Setup of the project ,[object Object],[object Object],[object Object]
Monitoring experiment ,[object Object],[object Object],[object Object]
20 th  century shells ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Late Holocene shells
Palaeogeography
Results  Average  δ 18 O per shell
Seasonal patterns Slowing down of growth
20 th  century shells
Predicted shell  δ 18 O  ,[object Object],Grossman & Ku (1986); Dettman et al. (1999)
Measured  δ 18 O vs. Predicted  δ 18 O
Measured  δ 18 O vs. Predicted  δ 18 O:  20 th  century shells   Juvenile stage
Measured  δ 18 O vs. Predicted  δ 18 O:  20 th  century shells   Glacier melting Dry summer ???
Measured  δ 18 O vs. Predicted  δ 18 O: monitoring
Late Holocene shells
Conclusions ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
[object Object]

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