Description: The aim of this study is to investigate the transfer of biogenic (BSi, organic carbon, carbonate) and lithogenic particles from different types of eddies to sequestration depths against oligotrophic background conditions. We use a multi-year sediment trap record (2009-2016) of particle fluxes at the oligotrophic site CVOO, which documents fall-winter conditions with different low oxygen eddies passing through the study site and during oligotrophic, low-seasonality conditions prevailing north of the Cape Verde islands.

Description: A multiannual, continuous sediment trap experiment was conducted at the mooring site CBeu (Cape Blanc eu- trophic, ca. 20 °N, ca. 18 °W; trap depth = 1256-1296 m) in the high-productive Mauritanian coastal upwelling. Here we present fluxes and the species-specific composition of the diatom assemblage, and fluxes of biogenic silica (BSi, opal) and total organic carbon (TOC) for the time interval June 2003-Feb 2010. Flux ranges of studied parameters are (i) total diatoms = 1.2 ∗ 108-4.7 ∗ 104 valves m−2 d−1 (average = 5.9 × 106 valves ± 1.4 × 107); (ii) BSi = 296-0.5 mg m−2 d−1 (average = 41.1 ± 53.5 mg m−2 d−1), and (iii) TOC = 97-1 mg m−2 d−1 (average = 20.5 ± 17.8 mg m−2 d−1). Throughout the experiment, the overall good match of total diatom, BSi and TOC fluxes is reasonably consistent and reflects well the temporal occurrence of the main Mauritanian upwelling season. Spring and summer are the most favorable seasons for diatom pro- duction and sedimentation: out of the recorded 14 diatom maxima of different magnitude, six occurred in spring and four in summer. The diverse diatom community at site CBeu is composed of four main assemblages: benthic, coastal upwelling, coastal planktonic and open-ocean diatoms, reflecting different productivity conditions and water masses. A striking feature of the temporal variability of the diatom populations is the persistent pattern of seasonal groups' contribution: benthic and coastal upwelling taxa dominated during the main upwelling season in spring, while open-ocean diatoms were more abundant in fall and winter, when the upper water column becomes stratified, upwelling relaxes and productivity decreases. The relative abundance of benthic diatoms strongly increased after 2006, yet their spring-summer contribution remained high until the end of the trap experiment. The occurrence of large populations of benthic diatoms at the hemipelagic CBeu site is interpreted to indicate transport from shallow waters via nepheloid layers. We argue that a significant amount of valves, BSi and TOC produced in waters overlying the Banc d'Arguin and the Mauritanian shelf is effectively transported to the CBeu trap in intermediate waters at the outer Mauritanian slope. The impact of the intermediate and bottom-near nepheloid layers-driven transport in the transfer of valves and bulk particulates and its potential contribution to the export of biogenic materials from the shelf and uppermost slope might play a significant role in hemipelagial fluxes off Mauritania.

Description: Long 1, midchain alkane-diols have been analyzed from sediment trap CBeu (off Mauritania) samples collected from 2003-2008 (CBeu1-5). The changes in diol composition and diol indices have been compared with changes in environmental parameters. New and hardly available data are deposited here. These include the diol flux data, the corrected UK'37 record, the relative abundances of upwelling indicating species and the 11 years moving average of wind speed and direction from Nouadhibou Airport. Data that are readily available from the World Ocean Atlas 2018, NOAA and earlier publications on CBeu have not been deposited here. These include solar insolation, sea surface temperatures, as well as water temperature, salinity and phosphate for different water depths.

Description: We present the first analysis of the relative contribution of variability in shell flux, shell size, and calcification intensity (weight/size) in individual species to the total calcite flux by the planktonic foraminifera community on intra-annual (seasonal) and interannual timescales. We investigated the export flux of planktonic foraminifera in two one-year sediment trap time series from the Northeastern Atlantic Ocean and placed the observed variability of shell flux, shell size, and calcification intensity of each species in the context of the resulting calcite flux. For this issue, we selected 1990-1991 (Cape Blanc-3) and 2007-2008 (Cape Blanc-18) time series from the Cape Blanc upwelling area. Each of these deployments covered an entire year continuously, with an average sampling resolution of ~20 days. Here, we provide the data concerning the species individual size during the studied time series, which were picked from size fractions 〉 150 µm.