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List of Accepted Contributions - CL016 Deep Time Perspectives on Climate Change: Marrying the Signal from Computer Models & Biological Proxies
Please, click Abstract Number to find the corresponding abstract as PDF
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EGU06-A-00076
Haywood, A. M.; Valdes, P. J.
A permanent El-Nino state during the Pliocene? A modelling perspective |
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EGU06-A-01149
von der Heydt, A.; Dijkstra, H.A.
What determines the Atlantic-Pacific salinity contrast through the Cenozoic? |
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EGU06-A-02266
Prange, M.; Schulz, M.
Panamanian gateway closure chilled North America: A dynamical impact of the atmosphere on Northern Hemisphere Glaciation |
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EGU06-A-02370
Salzmann, U.; Haywood, A. M.
Synthesising, translating and mapping Tertiary vegetation data for global climate modelling studies |
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EGU06-A-02820
Vautravers, M.J.
Records of climatic change during the late Miocene: Preliminary results from atlantic sites ODP 925, 1088 and 982, using planktonic foraminifera fauna variability |
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EGU06-A-03386
Dupont, L.M.
Late Pliocene vegetation and climate in Namibia (southern Africa) |
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EGU06-A-04845
Dowsett, H.
Pliocene sea surface temperature and the PRISM reconstruction |
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EGU06-A-04864
Lamarque, J.-F.; Kiehl, J.; Shields, C.; Boville, B.; Kinnison, D.
Modeling the response to changes in tropospheric methane concentration: application to the Permian-Triassic boundary |
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EGU06-A-04913
Robinson, M.; Dowsett, H.; Dwyer, G.
Multi-proxy Sea-surface Temperature Estimates for the mid-Pliocene North Atlantic |
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EGU06-A-04929
Lunt, D.J.; Haywood, A.; Valdes, P.J.
The formation of the Panama Isthmus during the Pliocene in a fully coupled GCM - implications for northern hemisphere cooling. |
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EGU06-A-06732
Hill, D.; Haywood, A.; Hindmarsh, R.; Valdes, P.
Testing scenarios of Pliocene East Antarctic Ice Sheet behaviour: towards a coupled ice sheet-climate modelling approach |
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EGU06-A-07340
Fauquette, S.; Suc, J.-P.; Jiménez-Moreno, G.; Favre, E.; Jost, A.; Micheels, A. ; Pollen data contributors
Latitudinal climatic gradients in western European and Mediterranean regions from the Mid-Miocene (~15 Ma) to the Mid-Pliocene (~3.5 Ma) as quantified from pollen data |
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EGU06-A-07890
Groeneveld, J.; Steph, S.; Tiedemann, R.; Nuernberg, D.
Progressive Closure of the Panamanian Gateway during the Pliocene |
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EGU06-A-08325
Butzin, M.; Lohmann, G.; Bickert, T.; Haak, H.
Simulating middle Miocene ocean circulation changes and the potential effect on climate |
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EGU06-A-09210
Page, A.A.; Williams, M; Zalasiewicz, J.A.
Were transgressive black shales a negative feedback mechanism modulating glacio-eustastic cycles in the Early Palaeozoic Icehouse? |
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EGU06-A-09231
Williams, M; Haywood, A; Hillenbrand, C; Wilkinson, I; Miller, C
How far do fossil Neogene surface-dwelling planktonic foraminifera record properties of the ancient ocean surface? |
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EGU06-A-10054
Donnadieu, Y.; Godderis, Y.; Pierrehumbert, R.; Dromart, G.; Fluteau, F.; Jacob, R.
Pangea break up and Mesozoic climatic evolution simulated by the GEOCLIM model |
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