Last Glacial Maximum (LGM) paleoproductivity, organic carbon (C-org) fluxes, and seasonality was reconstructed from benthic foraminiferal faunas and the stable carbon and oxygen isotopes of foraminiferal calcite. Sediments of the LGM between 23,000 to 19,000 cal-yr BP of sixteen cores from the upwelling region off Morocco between Cape Ghir (31 degrees N) and Cape Yubi (27.5 degrees N) were investigated. Four regions with distinct paleo-C-org fluxes and seasonality were reconstructed based on faunal assemblages and delta C-13 values of Hoeglundina elegans: (1) the Cape Yubi Upwelling Region with high paleoproductivity, high paleo-C-org fluxes and very low seasonality as indicated by the Bolivina albatrossi/Uvigerina mediterranea Assemblage and lowest mean delta C-13(H.elegans); (2) the Cape Ghir Upwelling Region with moderate to high paleoproductivity and paleo-C-org fluxes and low seasonality as indicated by the Bulimina mexicana/Gavelinopsis translucens Assemblage, and low mean delta C-13(H.elegans); (3) the Cape Yubi Filament Region with moderate to high paleoproductivity, high paleo-C-org fluxes and high seasonality as indicated by the Cassidulina laevigata/Nonionella iridea Assemblage, and delta C-13(H.elegans) as low as those from the Cape Ghir Upwelling Region; (4) the Cape Ghir Filament Region with highest paleoproductivity, high paleo-C-org fluxes and seasonality as indicated by the Epistominella exigua Assemblage, and highest delta C-13(H.elegans). Productivities during the LGM and today were compared based on faunal assemblages and Delta delta C-13 values (Delta delta C-13 =delta C-13(LGM)-delta C-13(Present)) of three infaunal species. Generally, during the LGM, the upwelling region was characterized by higher paleo-C-org fluxes, particularly in the area between the capes, similar seasonality along the coast, and higher seasonality further offshore than at present-day. For the reconstruction of LGM water mass stratification we used the delta C-13 of Cibicidoides wuellerstorfi and equilibrium adjusted 6180 of several species. Deep water mass stratification is characterized by glacial North Atlantic Central Water above 800 in, by glacial Mediterranean Outflow Water between 800 and 1900 in and glacial North Atlantic Deep Water below 1900 in and a southern source deep water mass. This means, considering the lowered glacial sea level, water mass stratification during the LGM was similar to present-day conditions. (C) 2007 Elsevier B.V. All rights reserved.
