Sedimentary processes on the NW Iberian continental Shelf since the late Little Ice Age

• Main Authors: Martins, V., Figueira, R.C.L., França, E.J., Ferreira, P.A.L., Martins, P., Santos, J.F., Dias, J.M.A., Laut, L.M., Ferreira da Silva, E., Rocha, F.
• Format: Conference Object
• Language: English
• Published: Universidade de Aveiro 2012
• Subjects: Douro Muddy Patch; 210Pb and 137Cs chronology; North Atlantic Oscillation; benthic foraminifera; sediment supply; Pb and W concentrations; Iceland; North Atlantic; North Atlantic oscillation
• Online Access: http://hdl.handle.net/10773/9015

The OMEX core CD110 W90, retrieved from the Douro Muddy Patch (DMP) off the River Douro in the north of Portugal, records the last ≈150 years, i.e. the period since the late Little Ice Age (LIA). The core chronology is mainly based upon 210Pb and 137Cs activities. Geochemical, granulometric and microfaunal (benthic foraminifera) data suggest the occurrence of precipitation changes which may have been, at least partially, influenced by the North Atlantic Oscillation (NAO). Southwesterly Atlantic storm track is associated with the negative phases of the NAO, when the Azores High is anomalously weak and strong oceanographic hydrodynamism, downwelling events and increased rainfall generally occur. Prevalence of these characteristics in the late LIA is recorded in this core between AD ≈1870-1900. During this period the DMP received a higher contribution of relatively coarse-grained terrigenous sediments, enriched in quartz particles which diluted the contribution of other minerals, as indicated by reduced concentrations of several lithogenic chemical elements such as: Al, As, Ba, Ce, Co, Cu, Fe, K, La, Li, Mg, Mn, Mo, Na, Ni, P, Rb, Sc, Sn, Th, V and Y. The presence of biogenic carbonate particles also underwent dilution, as revealed by the smaller abundance of foraminifera and correlative lower concentrations of Ca and Sr. In the same period, the DMP received a significant contribution of organic matter, indicated by higher values of both lignin remains and benthic foraminifera high productivity index (BFHP), which gave rise to early diagenetic changes with pyrite formation. Since the beginning of the 20th century this contribution diminished, probably due to several drier periods and the impact of human activities in the Douro basin and in the littoral areas. During the first half of the 20th century mainly positive phases of the NAO prevailed, caused by the above normal strengthening of the subtropical high pressure centre of the Azores and the deepening of the low pressure centre in Iceland. These phases may have ...