Living, dead and fossil benthic foraminifera on a river dominated shelf (northern Gulf of Cadiz) and their use for paleoenvironmental reconstruction

• Published in: Continental shelf research Vol. 68; pp. 91 - 111
• Main Authors: Mendes, I., Dias, J.A., Schönfeld, J., Ferreira, Ó., Rosa, F., Lobo, F.J.
• Format: Journal Article
• Language: English
• Published: Elsevier Ltd 01.10.2013
• Subjects: Benthic foraminifera; Continental shelf; Guadiana River; Gulf of Cadiz; Holocene; Paleoenvironmental reconstruction; Paleoenvironmental reconstruction; Benthic foraminifera; Gulf of Cadiz; Continental shelf; Guadiana River; Holocene
• ISSN: 0278-4343; 1873-6955
• DOI: 10.1016/j.csr.2013.08.013

Same-area comparison between patterns of Recent (living) and Holocene benthic foraminiferal assemblage composition is essential to validate their utility as proxies for paleoenvironmental reconstructions. Such reconstructions have scarcely been attempted in shelf environments. In this study, we compared living (stained), dead and Holocene benthic foraminiferal assemblages from the Gulf of Cadiz continental shelf off the Guadiana River. On average, 99% of the living benthic foraminiferal species were preserved in the dead assemblage and 95% in the fossil record. Several common species were assessed as indicators for certain environmental factors, including river discharge, supply of terrestrial organic matter, heavy metal concentrations, oxygen levels, substrate properties, hydrodynamic energy levels, sea-level rise and human impact. The paleoenvironmental reconstruction depicted five stages of Holocene environmental evolution of the Guadiana shelf over the last 11,500calyr BP. The characteristics of the stages, and the transitions between them, were in particular driven by changes in sea-level, influx of terrestrial organic matter and limits of productivity. •Same-area comparison between living, dead and Holocene benthic foraminifera.•Validation of benthic foraminifera as environmental proxies in shelf environments.•Identification of five evolutionary stages during the Holocene.•Stages react to changes in sea-level, influx of organic matter and limits of productivity.