The upper Miocene diatom-bearing section of Pecetto di Valenza (Piedmont, NW Italy) represents a unique site for reconstructing the paleoceanographic processes that occurred before the onset of the Messinian salinity crisis in the northernmost Mediterranean basin. The combined analysis of foraminifera, calcareous nannofossils, diatoms and other siliceous microfossils observed in the marly and diatomaceous sediments allowed us to define four main evolutionary stages of the biogenic sedimentation. Each stage was typified by specific water column and seafloor conditions, tentatively correlated to the precession/insolation variability. In particular, the variation of the benthic assemblages allowed us to distinguish two stages in the evolution of the diatomaceous deposition, which would be otherwise impossible from the lithology. The accumulation of the diatomaceous sediments was likely controlled by the interplay between riverine runoff, water column stratification and convective mixing, rather than with upwelling and seafloor anoxia as inferred for the Western and Eastern sectors of the Mediterranean.
Integrated micropaleontological study of the Messinian diatomaceous deposits of the Monferrato Arc (Piedmont basin, NW Italy): New insights into the paleoceanographic evolution of the northernmost Mediterranean region
Luca PELLEGRINO;Rocco GENNARI;Francesca LOZAR;Francesco DELA PIERRE;Marcello NATALICCHIO;Giorgio CARNEVALE
2020-01-01
Abstract
The upper Miocene diatom-bearing section of Pecetto di Valenza (Piedmont, NW Italy) represents a unique site for reconstructing the paleoceanographic processes that occurred before the onset of the Messinian salinity crisis in the northernmost Mediterranean basin. The combined analysis of foraminifera, calcareous nannofossils, diatoms and other siliceous microfossils observed in the marly and diatomaceous sediments allowed us to define four main evolutionary stages of the biogenic sedimentation. Each stage was typified by specific water column and seafloor conditions, tentatively correlated to the precession/insolation variability. In particular, the variation of the benthic assemblages allowed us to distinguish two stages in the evolution of the diatomaceous deposition, which would be otherwise impossible from the lithology. The accumulation of the diatomaceous sediments was likely controlled by the interplay between riverine runoff, water column stratification and convective mixing, rather than with upwelling and seafloor anoxia as inferred for the Western and Eastern sectors of the Mediterranean.File | Dimensione | Formato | |
---|---|---|---|
Pellegrino et al. 2020 - Integrated micropaleontological study of Messinian diatomaceous deposits of the Monferrato Arc.pdf
Accesso riservato
Tipo di file:
PDF EDITORIALE
Dimensione
7.61 MB
Formato
Adobe PDF
|
7.61 MB | Adobe PDF | Visualizza/Apri Richiedi una copia |
I documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.