Relative abundance and fluxes of coccospheres, planktonic foraminifera ( >63 µm) and diatoms in sediment trap ALB-5 sampled from July 1997 to May 1998 in the Alboran Sea , Western Mediterranean Sea

• Main Authors: Hernández-Almeida, Iván, Bárcena, María Angeles, Flores, José-Abel, Sierro, Francisco Javier, Sanchez-Vidal, Anna, Calafat, Antonio M
• Format: Dataset
• Language: English
• Published: PANGAEA 2018
• Subjects: Planktonic foraminifera
• Online Access: https://doi.pangaea.de/10.1594/PANGAEA.891257; https://doi.org/10.1594/PANGAEA.891257

The present work analyses the seasonal evolution of planktonic assemblages and particle fluxes through the water column in the Eastern Alboran Sea (Western Mediterranean) at 35º55.47'N/01º30.77'W. A Sediment trap was deployed below the influence of the Almeria-Oran Front (AOF), a semi-permanent geostrophic front, during July 1997 to June 1998. Overall, the temporal variability of coccolithophore, planktonic foraminifer, diatom, benthic and wind-carried biogenic particle fluxes is linked to the seasonal evolution of sea surface hydrological structures. Maximum planktonic fluxes were found during high-productivity periods and wind-induced upwelling, following a trimodal pattern, with maximum fluxes in July 1997, November-December 1997, and April-May 1998. These periods were characterized by vertical mixing and the full development of anticyclonic gyres in the Alboran Sea. The annual flux of coccolithophores was dominated by the "small Gephyrocapsa Group" and Emiliania huxleyi, whereas Turborotalita quinqueloba and Globigerina bulloides dominated the foraminiferal fluxes, and Chaetoceros Resting Spores (RS) were predominant in the diatom assemblage. Benthic specimens were also collected with the sediment trap, suggesting a variable influence of bottom water activity. Wind-driven particles (phytoliths and fresh-water diatoms) were collected along the year, but their fluxes followed the local wind regime.