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author Ribeiro, Sofia
Gebara, Livia
Abrantes, Fatima F
author_facet Ribeiro, Sofia
Gebara, Livia
Abrantes, Fatima F
collection Datos científicos de ciencias marinas y ambientales
contents The Iberian Margin, located in the mid-latitude North Atlantic at the western edge of the European continent, is a key region for climate and oceanographic research. The Portuguese western coast marks the northernmost boundary of the Canary Current upwelling system, experiencing seasonal wind-driven coastal upwelling from May to September. Eastern Boundary Upwelling Systems (EBUS) are among the most productive regions in the global ocean. They play a vital role in climate regulation and support both local and global fisheries. As part of the ICW3P project (PTDC/CTA-CLI/2884/2021) 'Impact of climate warming in the coastal upwelling system and primary production off Portugal: a study linking classical and emerging proxies', this study presents multi-proxy records from three inner-shelf sediment sequences. The project aimed to evaluate different nutrient sources and paleoceanographic features of the Iberian Margin and to reconstruct primary productivity and phytoplankton community variability over the past 1,000 years. This dataset presents the biogenic silica (BSi) content from a sediment record collected off the mouth of the Douro River (POS287-06G), in the north-western region of the Portuguese continental shelf, using a gravity coring system during the Poseidon cruise POS287 in 2002. Biogenic silica was measured at the Geological Survey of Denmark and Greenland using the weak base (Na2CO3) extraction method (DeMaster, 1991) and determined by spectrophotometry (blue ammonium-molybdate method, Mullin and Riley, 1955). Biogenic silica concentrations were calculated and corrected for mineral dissolution using the intercept of a linear regression, with the basic assumption that mineral-derived silica dissolves at a constant rate throughout the extraction whereas the biogenic silica dissolves within the first two hours (Barão et al., 2015).
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_991490
institution PANGAEA
language en
publishDate 2026
publisher PANGAEA
record_format pangaea
spellingShingle Biogenic silica of sediment core POS287_06-1B and POS287_06-2G
Ribeiro, Sofia
Gebara, Livia
Abrantes, Fatima F
BC; biogenic silica; Biogenic silica, per unit sediment dry mass; Biogenic silica, per unit sediment dry mass, standard deviation; Box corer; coastal upwelling; Date/Time of event; DEPTH, sediment/rock; Depth, sediment/rock, bottom/maximum; Depth, sediment/rock, top/minimum; Elevation of event; Event label; GC; Gravity corer; Iberian margin; ICW3P; Impact of climate warming in the coastal upwelling system and primary production off Portugal: a study linking classical and emergent proxies; Last millennium; Latitude of event; Longitude of event; opal; PALEO 1; Portuguese Margin; POS287; POS287_06-1B; POS287_06-2G; POS287_06-3G; POS287-06; POS287-26; Poseidon; Sample code/label; see description in data abstract; spectrophotometry
The Iberian Margin, located in the mid-latitude North Atlantic at the western edge of the European continent, is a key region for climate and oceanographic research. The Portuguese western coast marks the northernmost boundary of the Canary Current upwelling system, experiencing seasonal wind-driven coastal upwelling from May to September. Eastern Boundary Upwelling Systems (EBUS) are among the most productive regions in the global ocean. They play a vital role in climate regulation and support both local and global fisheries. As part of the ICW3P project (PTDC/CTA-CLI/2884/2021) 'Impact of climate warming in the coastal upwelling system and primary production off Portugal: a study linking classical and emerging proxies', this study presents multi-proxy records from three inner-shelf sediment sequences. The project aimed to evaluate different nutrient sources and paleoceanographic features of the Iberian Margin and to reconstruct primary productivity and phytoplankton community variability over the past 1,000 years. This dataset presents the biogenic silica (BSi) content from a sediment record collected off the mouth of the Douro River (POS287-06G), in the north-western region of the Portuguese continental shelf, using a gravity coring system during the Poseidon cruise POS287 in 2002. Biogenic silica was measured at the Geological Survey of Denmark and Greenland using the weak base (Na2CO3) extraction method (DeMaster, 1991) and determined by spectrophotometry (blue ammonium-molybdate method, Mullin and Riley, 1955). Biogenic silica concentrations were calculated and corrected for mineral dissolution using the intercept of a linear regression, with the basic assumption that mineral-derived silica dissolves at a constant rate throughout the extraction whereas the biogenic silica dissolves within the first two hours (Barão et al., 2015).
title Biogenic silica of sediment core POS287_06-1B and POS287_06-2G
topic BC; biogenic silica; Biogenic silica, per unit sediment dry mass; Biogenic silica, per unit sediment dry mass, standard deviation; Box corer; coastal upwelling; Date/Time of event; DEPTH, sediment/rock; Depth, sediment/rock, bottom/maximum; Depth, sediment/rock, top/minimum; Elevation of event; Event label; GC; Gravity corer; Iberian margin; ICW3P; Impact of climate warming in the coastal upwelling system and primary production off Portugal: a study linking classical and emergent proxies; Last millennium; Latitude of event; Longitude of event; opal; PALEO 1; Portuguese Margin; POS287; POS287_06-1B; POS287_06-2G; POS287_06-3G; POS287-06; POS287-26; Poseidon; Sample code/label; see description in data abstract; spectrophotometry
url https://doi.org/10.1594/PANGAEA.991490