Late Quaternary deformation on the island on Pantelleria: New constraints for the recent tectonic evolution of the Sicily Channel Rift (southern Italy)

2009 ◽  
Vol 48 (2) ◽  
pp. 75-82 ◽  
Author(s):  
Stefano Catalano ◽  
Giorgio De Guidi ◽  
Gianni Lanzafame ◽  
Carmelo Monaco ◽  
Luigi Tortorici
2015 ◽  
Vol 51 (4) ◽  
pp. 670-681 ◽  
Author(s):  
Vincenzo Festa ◽  
Giacomo Prosser ◽  
Alfredo Caggianelli ◽  
Antonietta Grande ◽  
Antonio Langone ◽  
...  

2021 ◽  
Author(s):  
Lisa Carrera ◽  
Daniele Scarponi ◽  
Fabio Martini ◽  
Lucia Sarti ◽  
Marco Pavia

<p>Grotta del Cavallo, a well-known Paleolithic site in Southern Italy (Nardò, Apulia), preserves one of the most important Italian Middle Paleolithic sequences. Its stratigraphic succession records the presence of Neanderthals from Marine Isotope Stage (MIS) 7 to 3, providing substantial insights on their lifeways. Here we present the taxonomic and taphonomic analysis of the bird assemblages associated to Neanderthal occupation. The rich avifaunal assemblages allowed paleoenvironmental and paleoclimatic reconstructions, noticeably improving the reconstruction of the landscape that was exploited by Neanderthals throughout the last glacial-interglacial cycles. Based on the bird taxa identified in the assemblages, Grotta del Cavallo was mainly surrounded by extensive grasslands and shrublands, with scattered open woodland and rocky outcrops, during MIS 7, 6 and 3. The coastal plain, that is currently underwater due to Holocene relative sea-level rise, hosted wetlands in the cooler periods, when it was exposed. In the cool-temperate climatic phase attributed to MIS 3, bird taxa of water and wet environments proportionally increased, as well as coverage-based rarefied richness values. This is possibly due to the expansion of wetland areas, linked to more humid conditions, or to the shorter distance of the wetland settings from the cave, compared to MIS 6 (glacial period). A consequent higher heterogeneity of the landscape is retained to drive the increased richness. The sampling effort allowed to retrieve bird taxa that provided significant paleoclimatic insights, such as Branta leucopsis, an arctic breeder, and other species currently spread at higher altitudes, that reinforce previously obtained geochemical derived inference of climate conditions cooler than the present ones. The bird assemblages also provided the first occurrence ever of Larus genei, the first Italian occurrence of Emberiza calandra, the oldest Italian occurrence of Podiceps nigricollis, and the occurrence of Sylvia communis (a species rarely retrieved in the fossil record). Ordination analyses of the bird dataset detected the drivers of taphonomic degradation and the agents responsible for the accumulation of the avian bones: modifications are mainly due to physical sin- and post-depositional processes, whereas accumulation is mainly attributed to short-range physical processes of sediment accumulation, feeding activities of nocturnal raptors and, to a lesser extent, human activities. In detail, traces found on a few bones suggest that Neanderthals introduced some of the birds in the cave with alimentary purposes, providing the earliest Italian evidence of bird exploitation ever.</p>


Author(s):  
Andrea Columbu ◽  
Veronica Chiarini ◽  
Christoph Spötl ◽  
Jo De Waele ◽  
Stefano Benazzi ◽  
...  

<p>Western Mediterranean speleothem palaeoclimate records covering the entire Last Glacial period are extremely rare and discontinuous, because the progressive aridity and temperature decrease inhibited continuous carbonate deposition (Budsky et al., 2019; Perez-Mejias et al., 2019). This lack of high-resolution archives impedes a better understanding of key issues regarding the Late Quaternary, such as: 1) The spatio-temporal teleconnection between the northern latitudes and the Western Mediterranean area during the expansion/contraction of ice sheets related to DO cyclicity and AMOC changes; and 2) the palaeoclimate and palaeoenvironmental conditions during the scarcely known MIS 3, when the first Anatomically Modern Humans arrived on the Italian peninsula about 45.5 ka (Benazzi et al., 2011), sharing the territory with the already settled Neanderthals until the disappearance of the latter around 42 ka.</p><p>We present a well-dated continuous stalagmite record from Pozzo Cucù cave (southern Italy, Apulia) spanning from 106.0 <sup>+2.8</sup>/<sub>-2.7</sub> to 26.6 <sup>+0.8</sup>/<sub>-0.9 </sub>ka, with an average uncertainty of less than 1 ka. The age model is based on 27 U-Th dates and about 2600 δ<sup>18</sup>O and δ<sup>13</sup>C analyses were performed at an average resolution of about 40 years. δ<sup>18</sup>O and δ<sup>13</sup>C are interpreted as rainfall and soil bioproductivity indicators, respectively, although moisture source possibly had a role in modulating δ<sup>18</sup>O. The δ<sup>18</sup>O-δ<sup>13</sup>C timeseries is the first western Mediterranean speleothem record duplicating the Greenland ice core record (NGRIP) for MIS 5 to 3, and showing a striking resemblance for most of the DO cycles, especially from DO 22 to DO 16 and from DO 11 to DO 4. Discrepancies exist too, especially during the early MIS 3. Interestingly, the speleothem does not show evidence of many of the most severe climate events affecting the northern latitudes (e.g. Heinrich events). This calls for a re-evaluation of the role of the northern high latitudes in triggering major cooling/drying events across the Mediterranean region.</p><p>The oldest remains of Anatomically Modern Humans in Europe were found in Apulia (about 45.5 ka), and Neanderthals are known to have existed there at least until 42 ka. Thus, our new record provides a palaeoclimate-palaeoenvironmental background for the arrival of Anatomically Modern Humans in southern Europe, their coexistence with the Neanderthals, and the disappearance of the latter, which marks one of the most important biocultural transitions in human history (Wolf et al., 2018).</p><p> </p><p><strong>References</strong></p><p><strong> </strong></p><p>Benazzi S et al., 2011. Early dispersal of modern humans in Europe and implications for Neanderthal behavior. Nature</p><p> </p><p>Budsky A et al., 2019. Western Mediterranean climate response to Dansgaard/Oeschger Events: New Insights From Speleothem Records. GRL</p><p> </p><p>Pérez-Mejías C et al., 2019. Orbital-to-millennial scale climate variability during Marine Isotope Stages 5 to 3 in northeast Iberia. QSR</p><p> </p><p>Wolf D et al., 2018. Climate deteriorations and Neanderthal demise in interior Iberia. SR</p>


2006 ◽  
Vol 38 (2) ◽  
pp. 227-239 ◽  
Author(s):  
Giovanni Zanchetta ◽  
Alessandra Borghini ◽  
Anthony E. Fallick ◽  
Francesco P. Bonadonna ◽  
Gabriello Leone

Sign in / Sign up

Export Citation Format

Share Document