Dr Christian Maerz
Dr Britta Beckmann
Professor Thomas Wagner
| Geochemical environment of the Coniacian-Santonian western tropical Atlantic at Demerara Rise | 2009 |
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Dr Britta Beckmann
Dr Christian Maerz
Professor Thomas Wagner
| Coniacian-Santonian deep ocean anoxia/euxinia inferred from molecular and inorganic markers: Results from the Demerara Rise (ODP Leg 207) | 2008 |
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Dr Britta Beckmann
Professor Thomas Wagner
| Cyclic changes in Turonian to Coniacian planktic foraminiferal assemblages from the tropical Atlantic Ocean | 2008 |
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Dr Britta Beckmann
Professor Thomas Wagner
| Evolution of tropical watersheds and continental hydrology during the Late Cretaceous greenhouse; impact on marine carbon burial and possible implications for the future | 2008 |
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Dr Britta Beckmann
Professor Thomas Wagner
| Isotopic evidence for glaciation during the cretaceous supergreenhouse | 2008 |
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Dr Christian Maerz
Professor Simon Poulton
Dr Britta Beckmann
Professor Thomas Wagner
| Redox sensitivity of P cycling during marine black shale formation: Dynamics of sulfidic and anoxic, non-sulfidic bottom waters | 2008 |
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Dr Britta Beckmann
Professor Thomas Wagner
| Linking Coniacian-Santonian (OAE3) black shale formation to African climate variability: a reference section from the eastern tropical Atlantic at orbital time scales (ODP Site 959, off Ivory Coast/Ghana) | 2005 |
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Dr Britta Beckmann
Professor Thomas Wagner
| Orbital forcing of Cretaceous river discharge in tropical Africa and ocean response | 2005 |
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Professor Thomas Wagner
Dr Britta Beckmann
| Euxinia and primary production in Upper Cretaceous eastern equatorial Atlantic surface waters fostered orbital-driven formation of marine black shales | 2004 |
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Professor Thomas Wagner
Dr Britta Beckmann
| Millennial- to centennial-scale record of African climate variability and organic carbon accumulation in the Coniacian-Santonian eastern tropical Atlantic (Ocean Drilling Program Site 959, off Ivory Coast/Ghana) | 2003 |
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Dr Britta Beckmann
Professor Thomas Wagner
| Geochemical characterization of Cenomanian/Turonian black shales from the Tarfaya Basin (SW Morocco): relationships between paleoenvironmental conditions and early sulfurization of sedimentary organic matter | 2002 |
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Professor Thomas Wagner
Dr Britta Beckmann
| Morocco basin’s sedimentary record may provide correlations for Cretaceous paleoceanographic events worldwide | 2001 |
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