New research at the Doroshivtsi site in Ukraine has provided data that allow fresh insights into a well-known and important Gravettian site in the Middle Dniester Valley.

The Gravettian settlements of Europe are considered as an expression of human adaptation to harsh climates. In Southern Europe, however, favorable vegetation-climate conditions supported hunters-gatherer subsistence and the maintenance of their large-scale networks. This was also the case of the North-Adriatic plain and the Apennine mountain ridge in Italy. Traditionally considered lacking evidence, the northern part of the Apennine ridge has recently yielded the Early Gravettian site of Piovesello, located at 870 m a.s.l. Survey and excavation revealed lithic artifacts in primary position embedded in loamy sediments. Radiocarbon dating, anthracological and extended palynological and microcharcoal analyses have been integrated to reconstruct the palaeoecological context of this camp which was probably positioned above the timberline in an arid rocky landscape, bounding the fronts of local glaciers close to their maximum expansion at the time of Greenland Stadial (GS) 5 (32.04 - 28.9 ka cal BP). Human activity left ephemeral traces represented by lithic artefacts, charcoal, and the introduction of radiolarites from sources in proximity to the site and of chert from very far western sources. Evidence from Piovesello contributes to the reconstruction of human and vegetation ecology during Late Pleistocene glaciations and also provides hints for the historical biogeography of petrophytic plants and their orographic relics in the northern Apennine.

The woolly mammoth (Mammuthus primigenius) was widespread in almost all of Europe during the late Pleistocene. However, its distribution changed because of population fluctuations and range expansions and reductions. During Marine Oxygen Isotope Stage 2 (MIS 2), these processes were highly dynamic. Our analyses of 318 radiocarbon dates from 162 localities, obtained directly from mammoth material, confirmed important changes in mammoth range between ~28.6 and ~14.1 ka. The Greenland stadial 3 interval (27.5–23.3 ka) was the time of maximum expansion of the mammoth in Europe during MIS 2. The continuous range was soon fragmented and reduced, resulting in the disappearance of Mammuthus during the last glacial maximum from ~21.4 to ~19.2 ka in all parts of the North European Plain. It is not clear whether mammoths survived in the East European Plain. The mammoth returned to Europe soon after ~19.0 ka, and for the next 3–4 millennia played an important role in the lifeways of Epigravettian societies in eastern Europe. Mammoths became extinct in most of Europe by ~14.0 ka, except for core areas such as the far northeast of Europe, where they survived until the beginning of the Holocene. No significant correlation was found between the distribution of the mammoth in Europe and human activity.

Palaeolithic burials are few and far between, and establishing their chronology is crucial to gaining a broader understanding of the period. A new programme of radiocarbon dating has provided a revised age estimate for the Palaeolithic burial at Kostënki 18 in European Russia (west of the Urals). This study reviews the need for redating the remains, and contextualises the age of the burial in relation to other Upper Palaeolithic funerary sites in Europe and Russia. The new date, obtained using a method that avoided the problems associated with previous samples conditioned with glue or other preservatives, is older than previous estimates, confirming Kostënki 18 as the only plausibly Gravettian burial known in Russia.

The Gravettian is known for its technological innovations and artisanal craftwork. At the same time, continued climatic deterioration led to the coldest and driest conditions since the arrival of Homo sapiens sapiens in Europe. This article examines the palaeodemographic development and provides regionally differentiated estimates for both the densities and the absolute numbers of people. A dramatic population decline characterises the later part of the Gravettian, while the following Last Glacial Maximum experienced consolidation and renewed growth. The results suggest that the abandonment of the northern areas was not a result of migration processes, but of local population extinctions, coinciding with a loss of typological and technological complexity. Extensive networks probably assured the maintenance of a viable population.

It is now 20 years since the discovery of the Grotte Chauvet with its impressive cave art, but controversy continues over the antiquity of the images. Radiocarbon assays have been used to argue that the ‘black series’ charcoal drawings date to the Aurignacian period, more than 20 000 years earlier than traditional stylistic models would suggest. This paper questions the validity of the radiometric dating and cautions against reliance solely on the date of the charcoal. Instead, the authors propose an alternative chronology for the art of Chauvet based on stylistic comparanda, palaeontological remains and stratigraphic evidence.

The classic image of Upper Palaeolithic hunter-gatherers in Europe envisages them hunting large mammals in largely treeless landscapes. That is partly due to the nature of the surviving archaeological evidence, and the poor preservation of plant remains at such ancient sites. As this study illustrates, however, the potential of Upper Palaeolithic sites to yield macrofossil remains of plants gathered and processed by human groups has been underestimated. Large scale flotation of charred deposits from hearths such as that reported here at Dolní Vӗstonice II not only provides insight into the variety of flora that may have been locally available, but also suggests that some of it was being processed and consumed as food. The ability to exploit plant foods may have been a vital component in the successful colonisation of these cold European habitats.

The authors deconstruct the basis for dating the Palaeolithic cave paintings of France and find it wanting. Only five per cent are directly dated and the remainder belong to a stylistic framework that has grown organically, and with much circularity, as new paintings were brought to light. Following a constructive bouleversement, the authors recommend a new chronometric foundation based on chains of evidence anchored by radiocarbon dates. The story so far is striking: it brings many of the themes and techniques thought typical of the later painters into the repertoire of their much earlier predecessors.

Presented here is the so far unique discovery and interpretation of an occupation area directly associated with Upper Palaeolithic cave paintings. The paintings, of red spots and hand stencils, overlook two hearths with selected flints. There were also fragments of stalactite, deduced by analysis and experiment to be waste products from the manufacture of beads. The authors deduce that the hearths and their assemblage complement the ritual nature of the paintings.

The authors explore the arrival of the earliest Gravettian in north-west Europe, using new high precision radiocarbon dates for bone excavated at Maisières-Canal in Belgium to define a short-lived occupation around 33 000 years ago. The tanged points in that assemblage have parallels in British sites, including Goat's Hole (Paviland). This is the site of the famous ochred burial of a young adult male, confusingly known as the ‘Red Lady’, now dated to around 34 000 BP. The new results demonstrate that this British ‘rich burial’ and the Gravettian with tanged points may belong to two different occupation horizons separated by a cold spell.

This newly discovered and excavated site defines an Upper Palaeolithic activity unit consisting of a roasting pit at the centre of an area 5m across. Although the main task was the processing of two mammoths, there were numerous other wild animals in the assemblage. The occupants used flint knives, made bone tools and modelled in baked clay – on which they left their fingerprints, along with imprints of reindeer hair and textiles. Pavlov VI offers an exemplary picture of the basic living unit that made up the settlement clusters of the Gravettian people in Central Europe.

Two new examples of decorative art have turned up at the Gravettian site of Předmostí, dating to the twenty-sixth to twenty-fifth millennium BP: rectilinear grid patterns are executed on one side of flat bones, probably of reindeer. The authors speculate that the two pieces may have come from a single larger decorated object. The grids themselves join a growing repertoire of patterns known from Upper Palaeolithic society, but their role remains enigmatic: counting, calendars or ornament? Art or science?

The authors have identified starch grains belonging to wild plants on the surface of a stone from the Gravettian hunter-gatherer campsite of Bilancino (Florence, Italy), dated to around 25000bp. The stone can be seen as a grindstone and the starch has been extracted from locally growing edible plants. This evidence can be claimed as implying the making of flour – and presumably some kind of bread – some 15 millennia before the local ‘agricultural revolution’.

The Gravettian is considered one of the first pan-European cultures of the Upper Palaeolithic, spreading from Portugal to Russia between 28-20000 years BP and characterised by backed blades and points. The Noaillian is a local variant in southern Europe (Northern Spain, Southern France and Italy). In France Noaillian is supposedly evolving into the Rayssian which is replaced later by recent Gravettian. By reconsidering the formation processes of some key stratigraphic sequences, the author demonstrates that the Rayssian is an idiosyncratic culture that does not have abrupt-backed bladelets, and that runs chronologically in parallel with the others. A case study, based on new work at the site of La Picardie (Indre-et-Loire), suggests that we should expect to define different contemporary regional groups during this long period.

The famous upper Palaeolithic (Gravettian) burial with shell ornaments known as “Il Principe” was discovered in Italy sixty years ago. Here the authors present recent scientific research on his skeleton, leading to new assessments of the date of the burial and indications of diet.

This study considers exploitation of marine molluscs at Riparo Mochi (Italy) in cultural and ecological context. Five shell assemblages from this site represent the early Upper Palaeolithic (c. 36,000 BP) through Late Epigravettian (c. 9000 BP) periods. Taphonomic analysis reveals four kinds of shell debris: ornaments, food refuse, marine sponge inclusions, and land snails. While human foraging agendas at Riparo Mochi shifted over the five Palaeolithic phases, the kinds of marine shells favoured as ornaments remained nearly constant.

AMS and other dating methods have been applied to the problem of Upper Palaeolithic occupation in Central Europe. The results from the excavations at the Rhineland site of Wiesbaden-Igstadt provide an opportunity for comparison and discussion of whether central Europe was really subject to abandonment at various times during Glacial/Pleniglacial episodes.