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Panthera spelaea was recorded in Poland from 18 open-air and 42 cave sites dated in the range 750–28 ka. Most of these records are located in southern Poland (Silesia) and neighbouring areas. Among them, the find of Panthera spelaea in Kozi Grzbiet mentioned here for the first time is one of the oldest European records of the species. Most of the obtained AMS dates are concentrated on the second half of MIS 3 and showed that the Pleistocene lion disappeared more or less synchronously across Poland. The findings of its remains from open-air sites are mostly accidental discoveries during field works, while those in caves are mostly connected with archaeological research and the exploitation of cave sediments for producing fertilizers. Aside of a few juvenile bones and milk teeth, the remains of adult individuals, mostly males, predominate in the studied sample. Their behavior to hunting cave bear during the times, when the other, more typical food sources were scarce, tendention to hunt very big preys and went into the conflicts with other carnivores than females do, resulted in higher injuries and mortalities. Within the species, three chronosubspecies were recognized, with P. s. fossilis recorded from 7 sites, dated between 750 and 240 ka and P. s. intermedia only partially recognized in Wierzchowska Gorna Cave. The most numerous are the remains of P. s. spelaea which were found in 48 localities dated between 150 and 28 ka. With the exception of four caves, the Polish finds of P. spelaea are generally less abundant at sites where they occur. Older P. s. fossilis, dated on MIS 19–12, was a large form with robust stature and broad cheek teeth. Younger P. s. fossilis dated on MIS 11–9 was represented by a large and massive specimens, but with more advanced morphological dental features. Polish individuals of P. s. spelaea were slightly smaller and less massive than P. s. fossilis, with narrower cheek teeth. Since MIS 3, a dwarf and gracile specimens appeared, which is correlated with the genetic turnover ca. 48–45 ka. The Pleistocene lion was one of the earliest disappeared large carnivores predated only by a cave hyena. There are no direct evidences of P. spelaea encounters with humans. The extinction of P. spelaea is broadly correlated with the general collapse of the “mammoth steppe” ecosystem and was resulted of multiple reasons like climatic changes, re-building of herbivore guilds, competition and human pressure. Wolf and, to a lesser extent, bears were the main competitors for the Pleistocene lion in Poland.

The purpose of this article is to yield new insights into the topic of provisioning places of late Neanderthals using records from the central European Micoquian workshop Pietraszyn 49a, located in southwestern Poland. The site has been radiometrically dated back, using optically stimulated luminescence, to the final phase of Marine Isotope Stage (MIS) 4 or the beginning of MIS 3. The technological study, supported by numerous refits, shows that the main goals of manufacturing were shaped tools typologically corresponding to knives, handaxes, and bifacial scrapers. Considering the large variety of lithic raw materials and technical features, it can also be concluded that this assemblage resulted from the activity of at least several individuals. A microscopic investigation of use-wear traces indicates that this place was integrated within other elements of foraging zones, such as killing or butchering sites.

Marine Isotope Stage 3 is considered a period with several climate oscillations that drove the environments to rapid changes. To understand how these stadial-interstadial cycles affected southern Poland, we combined the results of eight proxies analysed in the samples from the old excavations and a new 2017 trench of Koziarnia Cave (Ojcow National Park, Krakow-Czestochowa Upland, Poland) in layers related to Middle Palaeolithic, Jerzmanowician, and Early Gravettian. Among the studied proxies were charcoals, pollen record, remains of malacofauna, and vertebrates (including rodents, birds and large mammals, and ZooMS analysis of fragmented bones). Moreover, sediment samples have been analysed for lipid composition (by Gas Chromatography-Mass Spectrometry, GC–MS). Despite several taphonomic issues, it was possible to recognise two oscillations. The first one, reflected in pollen record and lipid analysis, took place during Dansgaard-Oeschger (DO) 14 to 8 and included Heinrich Stadial (HS) 4. The second one, recorded by rodents and bird proxies, was related to DO 8/7 to DO 6 and included HS 3. Charcoal and large mammal proxies provided the broad context of our study. The Jerzmanowician occupation was connected with a relatively cold episode in a landscape characterized mainly by grassland and periglacial environments, while the Late Middle Palaeolithic and Early Gravettian groups settled the cave during milder climatic conditions, where environments were open with sparse boreal woodlands. Such trends provide additional arguments in a broad discussion on Middle-Upper Palaeolithic transition in Central Europe.

Recent excavations in Ciemna Cave in the Prądnik valley near Ojcow, southern Poland have brought to light new stratigraphic and techno-typological evidence concerning Late Middle Palaeolithic groups and their cultural affinities. In 2007, excavations began in the hitherto-unexplored main chamber of Ciemna Cave, with the goal of clarifying the results of previous work in other parts of the cave. During excavation the rocky floor of the cave was reached. About 1000 stone artifacts have been collected to date. Three cultural traditions have been documented: Mousterian, Taubachian, and Micoquian. Within the Micoquian tradition, three cultural levels were observed, which enriches the previous understanding of occupational phases at the site. These findings permit revision of the traditional terms “Prądnik industry” and “Prądnik technique.”

Ciemna Cave is a key Micoquian site located in Ojcow National Park, in the southern part of the Krakow-Czestochowa Upland. The site is known for a distinct group of asymmetrical knives, prądniks, as well as the associated cultural assemblage, the “Prądnik industry” or “Micoquo-Prondnikiens”—both named after the Prądnik stream flowing through the valley. Excavation of Ciemna Cave carried out in the early twentieth century provided a series of stratified archaeological materials. The published sections indicated explicitly diverse sequences and contexts in various parts of the site. In Ogrojec (sector CO), a collapsed part of the cave, two cultural layers were recognized within loess deposit: an upper layer with Prądnik industry implements and a lower layer with Prądnik industry artifacts and mixture of older cultural units, including those with handaxes. A different situation was encountered at the entrance to the cave (sector C), where a much longer stratigraphic section with a few artifactually poor cultural levels was discovered. Current excavations began in 2007 targeted a new area of the cave chamber, with a primary goal of correlating geologic and cultural sequences from the previous excavations. At this stage a complete section has been exposed, which comprises 19 major geological layers and 9 archeological levels. The area has provided new lithics finds and chronological data that have allowed us to make preliminary cultural linkages.