Stable carbon isotope gradients in benthic foraminifera as proxy for organic carbon fluxes in the Mediterranean Sea by M. Theodor, G. Schmiedl, F. Jorissen, A. Mackensen

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Distinct oxygenation modes of the Gulf of Oman over the past 43 000 years – a multi-proxy approach by N. Burdanowitz, G. Schmiedl, B. Gaye, P. M. Munz, H. Schulz

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Changes in the Red Sea overturning circulation during Marine Isotope Stage 3 by R. Hubert-Huard, N. Andersen, H. W. Arz, W. Ehrmann, G. Schmiedl

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Monsoon-driven changes in aeolian and fluvial sediment input to the central Red Sea recorded throughout the last 200 000 years by W. Ehrmann, P. A. Wilson, H. W. Arz, H. Schulz, G. Schmiedl

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Sediment transport on the inner shelf off Khao Lak (Andaman Sea, Thailand) during the 2004 Indian Ocean tsunami and former storm events: evidence from foraminiferal transfer functi... by Y. Milker, M. Wilken, J. Schumann, D. Sakuna, P. Feldens, K. Schwarzer, G. Schmiedl

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<i>Corrigendum to</i> "Upper ocean climate of the Eastern Mediterranean Sea during the Holocene Insolation Maximum – a model study" published in Clim. Past, 7, 1103–1122, 2011 by G. Schmiedl, E. Maier-Reimer, M. Kučera, R. Grimm, U. Mikolajewicz, F. Adloff, K.-C. Emeis

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