Diatom-inferred salinity changes in relation to Holocene sea-level fluctuations in estuarine environments of Argentina

ESPINOSA, MARCELA A.; HASSAN, GABRIELA S.; ISLA, FEDERICO I.

ALCHERINGA

TAYLOR & FRANCIS LTD

Año: 2012 vol. 36 p. 373 - 386

0311-5518

The analysis of diatoms from three sedimentary sequences in the Quequén Grande river basin (Buenos Aires province, Argentina) has allowed for the reconstruction of local and regional palaeosalinity changes in relation to Holocene sea level fluctuations. An established diatom-based salinity transfer function is used in combination with  autecological methods to reveal a maximum sea level between ca 7000 and 6000 14C years BP. This marine influence was recorded in deposits exposed 2 km and 12 km upstream, but not 32 km from the mouth. The fossil diatom assemblages are characteristic of an estuarine lagoon with maximum inferred salinities of 15 ?. When the Holocene transgression began to flood the former valley (ca 7000 14C years BP), brackish lagoons that evolved into estuarine setting in the lower valley but shallow freshwater ponds with salinities < 4? persisted at 32 km fromfor the reconstruction of local and regional palaeosalinity changes in relation to Holocene sea level fluctuations. An established diatom-based salinity transfer function is used in combination with  autecological methods to reveal a maximum sea level between ca 7000 and 6000 14C years BP. This marine influence was recorded in deposits exposed 2 km and 12 km upstream, but not 32 km from the mouth. The fossil diatom assemblages are characteristic of an estuarine lagoon with maximum inferred salinities of 15 ?. When the Holocene transgression began to flood the former valley (ca 7000 14C years BP), brackish lagoons that evolved into estuarine setting in the lower valley but shallow freshwater ponds with salinities < 4? persisted at 32 km from