Articles | Volume 45, issue 1
https://doi.org/10.5194/jm-45-117-2026
https://doi.org/10.5194/jm-45-117-2026
Research article
 | 
30 Jan 2026
Research article |  | 30 Jan 2026

Environmental changes at the seafloor of the Faro drift (Gulf of Cadiz) during the transition from the Early to the Middle Pleistocene

Giulia Silveira Molina, Gerhard Schmiedl, Francisco Jiménez-Espejo, Henning Kuhnert, Teresa Rodrigues, and Antje Helga Luise Voelker

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Short summary
Benthic foraminifera from sediment cores collected in the Gulf of Cadiz were analysed to track ocean changes between 1014 and 761 kyr ago. Our results reveal shifts in species composition throughout the climate cycles. Oxygen loss occurred in the Mediterranean Outflow Water during warmer periods when solar insolation was intensified and productivity was higher. During cold periods, stronger bottom currents were identified by sand content and the abundance of the species Planulina ariminensis.
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