Foraminiferal palaeodiversity and palaeoenvironments at the NE coastal plain of Buenos Aires province (Argentina) during the Mid-Holocene sea level highstand

ANGÉLICA BALLESTEROS PRADA; LUENGO MARIEL; VILANOVA ISABEL; FUCKS ENRIQUE; BERNASCONI EMILIANA

HOLOCENE (SEVENOAKS)

SAGE PUBLICATIONS LTD

Lugar: London; Año: 2021

0959-6836

In this investigation, we carried out a Mid-Holocene palaeoenvironmental reconstruction based on fossilized benthic foraminifera, retrieved from sedimentary deposits located in Bahía Samborombón coastal plain. A total of 38 species, grouped into 19 genera, were identified. The assemblage, constituted mainly by Buccella peruviana (d´Orbigny), Cribroelphidium poeyanum (d´Orbigny), Ammonia parkinsoniana (d´Orbigny) and Ammonia tepida (Cushman), indicate predominantly abnormal marine conditions, characterized by low oxygen levels between ca. 6882-6641 and 5600-5430 yrs. cal. BP. During this interval, a quantitative analysis carried out on the assemblages as well as indexes suggest found three different palaeoenvironments. The first one, occurring ca. 6880 yrs cal. BP, was a brackish environment with low oxygenation levels and low bottom energy. Then, ca. 6500-6250 yrs cal. BP, an environment with more marine influence, increased oxygen levels and higher energy prevailed. This higher oxygenation could be related to the flow of seawater into the area during the Mid-Holocene sea-level highstand. The third palaeoenvironment developed ca. 5590-5430 yrs cal. BP, was under a gradual transition back to a brackish environment with low oxygen levels as well as low energy.