The European badger Meles meles from Middle Pleistocene to Early Holocene of Italian Peninsula

• The first occurrence of Meles meles is form the late Early Pleistocene (1.3 Ma). • European badger is widely widespread across Europe during the Early Pleistocene to Late Pleistocene. • The size variability of Meles meles is not linked to evolutionary trend through the Middle Pleistocene to Early Holocene and/or considered as response to climatic changes

Body-mass estimation from Middle Pleistocene fallow deer of Europe

• Analysis of a sample covering a period of time ranging from 700,000 to 250,000 years ago. • Body mass comparison between fallow deer species of the Middle Pleistocene. • Comparison of the overall averages obtained for each site considered. • Considerations on the correlation between size variability and climatic situation

Braincase With Natural Endocast of a Juvenile Rhinocerotinae From the Late Middle Pleistocene Site of Melpignano (Apulia, Southern Italy)

Cranial remains of juvenile fossil rhinoceroses are rarely described in literature and very few is known about the ontogenetic development of their inner anatomy. In this study, we report the first CT based description of a juvenile braincase and its natural brain endocast of a late Middle Pleistocene Rhinocerotinae from Melpignano (Apulia, Italy). The specimen belongs to an individual about 12–18 months old, representing to date the youngest Pleistocene rhinoceros of Mediterranean Europe documented by neurocranial material. Through digital visualization methods the neurocranium has been restored and the anatomy of both the brain and the paranasal sinuses has been obtained and compared with those of juvenile and adult Pleistocene rhinoceroses. We evidence a different morphological development of the inner cranial anatomy in fossil and extant African species

The Quaternary paleontological research in the Campagna Romana (central Italy) at the 19th- 20th century transition. Historical overview

The Rome Basin, including the historical region of Campagna Romana, is considered as one of the most important sedimentary basin of Peninsular Italy for a paleontological viewpoint. A very high number of fossiliferous findings were collected from deposit which have a strong relationship with the evolution of the Tiber River fluvio-deltaic evolution (the “Paleo-Tiber” system). This evolution is the result of complex geological processes including tectonic, volcanism and glacio-eustatic fluctuations. A myriad of fossils were recovered during the end of 1800 and the beginning of 1900, mainly thank to the intense urbanization which affected the city of Rome. The majority of these historical fossil collection are today stored at “Museo Universitario di Scienze della Terra”, Sapienza, University of Rome (MUST), whereas sporadic specimens are kept in the scientific cabinets of several high school of the city or Latium villages. Several personalities of that time played a key role in the study of Quaternary fossiliferous deposits describing stratigraphical succession and fossil remains. The knowledge of these researchers and their histories have a crucial importance to reconstruct the storytelling of the historical fossil collection and to get more information on fossiliferous deposit today destroyed by urbanization or buried below anthropogenic deposits

Large Mammals from the Middle Pleistocene (MIS 11) site of Fontignano 2 (Rome, central Italy), with an overview of "San Cosimato" assemblages

Here we describe fossil mammal remains recovered from the late Middle Pleistocene (MIS 11) of Fontignano 2 (Rome, central Italy). Two species are recognized: the aurochs Bos primigenius and the red deer Cervus elaphus. The presence of B. primigenius represents one of the earliest diagnostic evidence of the species. Conversely, remains of C. elaphus are not fully diagnostic at a subspecies level, despite being long considered among the reference occurrences of C. e. eostephanoceros in Italy. This reconsideration, concurrent with the revised chronology of several localities of the area of Rome, questions the validity of the chronosubspecific and evolutionary repartition of the red deer as often envisioned in the literature, i.e., C. e. acoronatus, C. e. eostephanoceros, C. e. rianensis, C. e. elaphus. Remains of Fontignano 2 are part of those recovered within the San Cosimato Formation, also including Via di Brava (MIS 13 or MIS 11), with Palaeoloxodon antiquus, and San Cosimato (MIS 11), with Stephanorhinus sp., B. primigenius, Castor fiber, and Emys orbicularis

Cuon alpinus (Pallas, 1811) from the Late Pleistocene site of Ingarano (Foggia, southern Italy) and insights on the Eurasian Middle to Late Pleistocene record

In this study, we report for the first time the presence of Cuon alpinus from the Late Pleistocene site of Ingarano (Foggia, southern Italy), represented by an right upper first molar. Considering the intricate and debated taxonomy of fossil dholes, our comparative analyses on dental samples (P4, M1, and M1) of the extant and Middle to Late Pleistocene dholes from Europe, has been performed evidencing a relevant degree of morphological variability and a biometric uniformity of the considered teeth. Our results indicate the lack of clear morphological and biometric features for a reliable teeth-based classification of fossil dholes, questioning the validity of the fossil taxa currently proposed in the literature. Finally, to avoid the propagatio

Rediscovering Lutra lutra from Grotta Romanelli (southern Italy) in the framework of the puzzling evolutionary history of Eurasian otter

A river otter hemimandible has been rediscovered during the revision of the historical collections of G.A. Blanc from Grotta Romanelli, complementing the ongoing multidisciplinary research fieldwork on the site. The specimen, recovered from the level G (“terre rosse”; early Late Pleistocene or late Middle Pleistocene), is here assigned to Lutra lutra. Indeed, morphological and morphometric comparisons with other Quaternary Lutrinae fossils from Europe allow to exclude an attribution to the relatively widespread and older Lutra simplicidens, characterized by distinctive carnassial proportions. Differences with Cyrnaonyx antiqua, which possessed a more robust, shellfish-feeding dentition, support the view of a successful niche repartition between the two species during the late Middle to Late Pleistocene of Europe. The occurrence of Lutra lutra from the “terre rosse” of Grotta Romanelli suggests deep modifications of the landscapes due to the ecological adaptation of the taxon, and indicates that the Eurasian otter spread into Europe at the Middle–Late Pleistocene transition

An introduction to the early Holocene eolian deposits of Grotta Romanelli, Apulia, Southern Italy

Due to its geographic position and geomorphological configuration, Grotta Romanelli acted as a sediment trap since at least MIS 5. The so-called 'terre brune' sequence is a deposit mainly of eolian origin bearing upper Palaeolithic artefacts and fossil re-mains of vertebrate fauna; it was deposited during the Glacial-Interglacial transition and the Holocene. Sedimentology and mineralogy of this deposit are investigated. The stratigraphic sequence provides a promising archive within which both human and climatic impacts can be studied

An introduction to the early Holocene eolian deposits of Grotta Romanelli, Apulia, Southern Italy

Due to its geographic position and geomorphological configuration, Grotta Romanelli acted as a sediment trap since at least MIS 5. The so-called ‘terre brune’ sequence is a deposit mainly of eolian origin bearing upper Palaeolithic artefacts and fossil remains of vertebrate fauna; it was deposited during the Glacial-Interglacial transition and the Holocene. Sedimentology and mineralogy of this deposit are investigated. The stratigraphic sequence provides a promising archive within which both human and climatic impacts can be studied

Stratigraphic reassessment of Grotta Romanelli sheds light on Middle-Late Pleistocene palaeoenvironments and human settling in the Mediterranean

During the last century, Grotta Romanelli (Southern Italy) has been a reference site for the European Late Pleistocene stratigraphy, due to its geomorphological setting and archaeological and palaeontological content. The beginning of the sedimentation inside the cave was attributed to the Last Interglacial (MISs 5e) and the oldest unearthed evidence of human occupation, including remains of hearths, was therefore referred to the Middle Palaeolithic. Recent surveys and excavations produced new U/Th dates, palaeoenvironmental interpretation and a litho-, morpho- and chronostratigraphical reassessment, placing the oldest human frequentation of the cave between MIS 9 and MIS 7, therefore embracing Glacial and Interglacial cycles. These new data provide evidence that the sea reached the cave during the Middle Pleistocene and human occupation occurred long before MISs 5e and persisted beyond the Pleistocene- Holocene boundary