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Benthic foraminiferal response to trophic changes across the last glacial-Holocene transition in the abyssal eastern Mediterranean Sea. Katharina Müller-Navarra*, A. Lochte & G. Schmiedl University of Hamburg *[email protected]. Study Area . Study Area. - PowerPoint PPT Presentation
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Benthic foraminiferal response to trophic changes across the last glacial-
Holocene transition in the abyssal eastern Mediterranean Sea
Katharina Müller-Navarra
Katharina Müller-Navarra*, A. Lochte & G. Schmiedl
University of Hamburg*[email protected]
Study Area
Study Area
SL71-2
Katharina Müller-Navarra
3
Sapropel formation
0.1 mm
0.1 mm
Chilostomella oolina
Globobulimina affinis
Approach
Katharina Müller-Navarra
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Results & Discussion I
Baseline Baseline3xNutri3xNutri Nile+NutriNile+NutriIniGlacIniGlacIniGlac+3xNutriIniGlac+3xNutri
>1800 m
Levantine
Katharina Müller-Navarra
[R. Grimm 2012, unpubl.]
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Results & Discussion II
oligotroph mesotrophultra-oligotrophfood content oligotroph
Sapr
opel
S1
Katharina Müller-Navarra
PC1 M. subrotunda
PC2 A.tubulosa
PC4 C. laevigata
PC3 Q. viennensis
0.1 mm
0.1 mm
Cal. years BP
Q-mode PCA
Results & Discussion III
20 µm
Eponides pusillus
Individuals>125µmSa
prop
el S
1
Bolivina spp
Katharina Müller-Navarra
Cal. years BP
Cal. years BP
Individuals63–125µm
Sapr
opel
S1
Ind./g
Anomalinoides minimus
20 µm
Conclusions
- Benthic foraminiferal faunas are lacking evidence for eutrophication in the Levantine Basin before sapropel S1 formation
- The model shows: there is the potential to develope an oxygen depletion within a time periode of 6000 years due to enhanced fresh water supply
(- We are currently measuring benthic isotope data)
Katharina Müller-Navarra
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Thanks!
Katharina Müller-Navarra
Katharina Müller-Navarra*, A. Lochte & G. Schmiedl
University of Hamburg*[email protected]