Short-term middle Eocene (Bartonian) paleoenvironmental changes in the sedimentary succession of Olivetta San Michele (NW Italy): the response of shallow-water biota to climate in NW Tethys

• Published in: Facies
• Main Authors: Arena, Luca, Giraldo-Gómez, Victor M., Baucon, Andrea, Piazza, Michele, Papazzoni, Cesare A., Pignatti, Johannes, Gandolfi, Antonella, Briguglio, Antonino
• Other Authors: Pignatti, Johanne
• Format: Article in Journal/Newspaper
• Language: English
• Published: SPRINGER 2024
• Subjects: Paleoecology; Macrofauna; Larger benthic foraminifera; Ichnofossil; Photic zone; Carbonate ramp; Planktonic foraminifera
• Online Access: https://hdl.handle.net/11573/1700810; https://doi.org/10.1007/s10347-023-00677-4

This study focuses on the paleontological content of the middle Eocene (Bartonian) carbonate-siliciclastic sediments of the Capo Mortola Calcarenite Formation from Olivetta San Michele (Liguria, Italy). Along the succession, there are significant paleoecological changes triggered by the variation in neritic input as a consequence of tectonic and climatic instability. Among microfossils, nummulitids prevail, followed by orthophragmines, smaller benthic, and planktonic foraminifera, whereas mollusks and ichnofossils are the most abundant macrofossils. The sudden changes in the benthic communities due to the progressive increase in fluvial input are recorded throughout the sedimentary succession. An increase in water turbidity caused stressful conditions for autotrophic taxa, reducing their size and abundance. In contrast, filter feeders became dominant, suggesting an increase in dissolved and suspended nutrients. Ichnological analysis shows environmental fluctuations controlled by the transport of neritic material offshore, thus confirming the general deepening trend of the studied succession. In the upper part of the succession, we recorded an alternation between gravity flows and marly sediments that are interpreted as short-term alternations between low and intense precipitations. The gravity flows yield taxa such as larger benthic foraminifera (LBF), smaller benthic and planktonic foraminifera, mollusks, and corals. In turn, marls display only a few LBF and abundant smaller benthic and planktonic foraminifera. In these intervals, the increase in planktonic foraminifera also suggests a deepening of the carbonate ramp coinciding with a reduction of light that did not favor the development of LBF. These changes are probably related to the climatic dynamics that occurred in the Bartonian in the western Tethys.