Neanderthal populations occupied caves and rockshelters across the Mediterranean, leaving behind evidence of their daily activities, including plant remains. By studying these remains, we can gain a better understanding of how these populations used plant resources and adapted to their environment. A critical period for studying Neanderthal behaviour is Marine Isotope Stage 3 (MIS 3) which was characterized in Europe by millennial-scale climatic instability involving fluctuations between warming and cooling events. These changes may have impacted the dispersal and dynamics of Neanderthal populations, prompting new behavioural, subsistence and settlement adaptations. A key site for studying Neanderthal groups in southern Italy during MIS 3 is Riparo l'Oscurusciuto in the Ginosa Ravine. The site's long stratigraphic sequence and well-preserved faunal and material culture remains, including hearths, span the period from ∼55 ka to ∼42.8 ka BP. This makes the site central to our understanding of Neanderthal life and how they adapted to the environment until their disappearance from the region. Here, we present the results of a high-resolution study of plant microremains (phytoliths and pollen) and aquatic siliceous microremains (diatoms and chrysophyte cysts), alongside the mineralogical characterisation of their sedimentary contexts using Fourier Transform Infrared (FTIR) spectroscopy. The ∼12,200-year long reconstruction of the palaeoenvironment reveals a changing landscape starting with semi-open woodlands and forests at ∼55 ka and changing to more open woodland steppe environments starting sometime before ∼52 ka. The woody vegetation was composed of evergreen and deciduous oak woodlands with a continued presence of other mesophytes and Mediterranean woody taxa, including gymnosperms. The grasses (mostly C3 Pooid), are associated with a wide range of herbaceous species, probably reflecting the opening up of the landscape. Neanderthals responded to these changes by adapting their activities to the surrounding vegetation, by for example using grasses for the hearths, the ashes of which were later spread around the site.

Albert, R.M., Ochando, J., Martini, I., Rivera-Rondon, C.A., Crezzini, J., Dominici, C., et al. (2025). The palaeoenvironmental context of MIS 3 and the use of plants by Neanderthal groups in southern Italy: results from the Riparo l'Oscurusciuto site. JOURNAL OF ARCHAEOLOGICAL SCIENCE: REPORTS, 67 [10.1016/j.jasrep.2025.105399].

The palaeoenvironmental context of MIS 3 and the use of plants by Neanderthal groups in southern Italy: results from the Riparo l'Oscurusciuto site

Martini I.;Crezzini J.;Dominici C.;Spagnolo V.;Boscato P.;Ronchitelli A.;Boschin F.;Berna F.
2025-01-01

Abstract

Neanderthal populations occupied caves and rockshelters across the Mediterranean, leaving behind evidence of their daily activities, including plant remains. By studying these remains, we can gain a better understanding of how these populations used plant resources and adapted to their environment. A critical period for studying Neanderthal behaviour is Marine Isotope Stage 3 (MIS 3) which was characterized in Europe by millennial-scale climatic instability involving fluctuations between warming and cooling events. These changes may have impacted the dispersal and dynamics of Neanderthal populations, prompting new behavioural, subsistence and settlement adaptations. A key site for studying Neanderthal groups in southern Italy during MIS 3 is Riparo l'Oscurusciuto in the Ginosa Ravine. The site's long stratigraphic sequence and well-preserved faunal and material culture remains, including hearths, span the period from ∼55 ka to ∼42.8 ka BP. This makes the site central to our understanding of Neanderthal life and how they adapted to the environment until their disappearance from the region. Here, we present the results of a high-resolution study of plant microremains (phytoliths and pollen) and aquatic siliceous microremains (diatoms and chrysophyte cysts), alongside the mineralogical characterisation of their sedimentary contexts using Fourier Transform Infrared (FTIR) spectroscopy. The ∼12,200-year long reconstruction of the palaeoenvironment reveals a changing landscape starting with semi-open woodlands and forests at ∼55 ka and changing to more open woodland steppe environments starting sometime before ∼52 ka. The woody vegetation was composed of evergreen and deciduous oak woodlands with a continued presence of other mesophytes and Mediterranean woody taxa, including gymnosperms. The grasses (mostly C3 Pooid), are associated with a wide range of herbaceous species, probably reflecting the opening up of the landscape. Neanderthals responded to these changes by adapting their activities to the surrounding vegetation, by for example using grasses for the hearths, the ashes of which were later spread around the site.
2025
Albert, R.M., Ochando, J., Martini, I., Rivera-Rondon, C.A., Crezzini, J., Dominici, C., et al. (2025). The palaeoenvironmental context of MIS 3 and the use of plants by Neanderthal groups in southern Italy: results from the Riparo l'Oscurusciuto site. JOURNAL OF ARCHAEOLOGICAL SCIENCE: REPORTS, 67 [10.1016/j.jasrep.2025.105399].
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/11365/1301215