Paleolithic Sites Research Articles

A quantitative paleoclimatic reconstruction of the non-analogue environment of oxygen isotope stage 3: new data from small mammal records of southwestern Germany

Ensuring comparability between results is a key goal of all paleoecological reconstructions. Quantitative estimates of meteorological variables, as opposed to relative qualitative descriptions, provide the opportunity to compare local paleoenvironmental records against global estimates and incrementally build regional paleoclimatic records. The Bioclimatic Method provides quantitative and qualitative estimates of past landscape composition and climate along with measures of statistical accuracy by applying linear discriminant functions analysis and transfer functions to faunal taxonomic abundance data. By applying this method to the rodent data from Geißenklösterle and Hohle Fels, two Paleolithic cave sites located in the Ach Valley of southwestern Germany, we classify the regional vegetation according to Walters’ zonobiome model. We also present new estimates of meteorological variables including mean annual temperature, mean annual precipitation, and vegetative activity period of the Ach Valley for the period spanning ~ 60,000 to 35,000 cal BP. The results suggest the Ach Valley contained a non-analogous landscape of arctic tundra and temperate deciduous woodland with occasional arid steppe expansion. Meteorological estimates suggest the climate was significantly colder during the Middle and Upper Paleolithic than today, with higher annual precipitation and dramatic temperature shifts between seasons. These results fit well with climatic reconstructions from Switzerland and the Netherlands based on a variety of proxies. They also provide further evidence of a localized climatic response within southwestern Germany to the stadial-interstadial shifts preceding the Heinrich 4 event. Finally, these results reinforce our previous claims that climatic volatility was not a driving force in the loss of Neanderthal groups throughout the Swabian Jura during OIS 3.

Spatio-temporal variability of topoclimates and local palaeoenvironments in the Upper Dniester River Valley: Insights from the Middle and Upper Palaeolithic key-sites of the Halych region (western Ukraine)

The lowest section of the Upper Dniester River Valley (DRV), located between the uplands of Opillia and Eastern Subcarpathians, was a separate and specific Pleistocene geoecosystem, interesting for the hunter-gatherer communities. This is evidenced by three main (Yezupil, Mariampil and Halych), and a dozen or so additional Palaeolithic open-air sites. They occur as cultural layers within the loess-palaeosol sequences (LPSs) and represent semi-permanent settlement (except for the periods with the maximum intensity of the loess sedimentation); the oldest occur in the Eemian palaeosol. All sites are located on both sides of the river. In the past, the DRV was characterized by local environmental diversity changing with time. In consequence, it has very individual features, so the analysis of environmental changes is a local case study. In order to obtain information about the changes of climate and environment, the multi-proxy analyses were carried out. Chronology was based on the luminescence and radiocarbon dating. The diversity of habitats was local. Its degree was changing with time: it was minimal in the periods with extreme climatic conditions, such as the climate optimum and pessimum, and clearly greater in the climatically intermediate periods with fluctuations. Based on the materials indicating the mesoclimate and local vegetation diversity during the human occupation episodes as well as the location of the Palaeolithic sites, we found that generally the possibilities of choosing a warmer or sheltered place for a camp were not significant for hunters representing different cultures of different ages. Palaeolithic groups very often occupied the same places in the DRV. The camps had a hunting function, the choice of places was dictated primarily by the need to find a good place to observe game animals and to organize hunting – first of all – in the mouth sections of the tributaries of the Dniester River, regardless of the situation of localities relative to riverplains. The settlement attractiveness of such places was essentially timeless.

Palaeolithic archaeology: a review of recent research

In contrast to a relatively long history of Palaeolithic investigations in western Europe, research on the Palaeolithic period in Greece has lagged behind considerably. This article reviews the last decade of Palaeolithic research in Greece, with the aim of highlighting key aspects of recent developments in the field. Newly discovered Lower Palaeolithic sites, such as Marathousa 1 in Megalopolis, have offered rare, high-resolution windows into hunter-gatherer adaptations during the earliest-known peopling of the Greek peninsula. Palaeolithic sites in insular settings, exemplified by the latest discoveries in Crete and Naxos, have stirred up intriguing discussions about early seafaring but, most importantly, provide support to a revised view of the role of the Aegean in early human dispersals. Zooarchaeological, palaeoenvironmental and dating analyses of Middle and Upper Palaeolithic materials from new and older assemblages have provided valuable insights that help contextualize the information distilled from lithic industries. In sum, recent excavations, surveys and assessments of new and older collections have together contributed to the compilation of an important corpus of novel and significant data. Palaeolithic Greece is no longer a terra incognita, and it carries the potential to become a key player in understanding early human societies in southern Europe.

L’étude des pointes foliacées dans l’archipel du Japon

Approximately 10,000 Paleolithic sites have been approved in Japan. Transitions of the hunting weapons that represent stone implements are as follows.1. Stone implements that represent the Trapezoids and the Proto knives appeared approximately 32,000 years ago.2. Stone implements that represent bilaterally retouched knives of willow-leaf sharp and bilaterally retouched transversal knives developed approximately 29,000 years ago.3. Approximately 28,000 years ago, after Aira-Tn volcanic ash fell down, the Kakusuijo-sekki appeared. This Kakusuijo-sekki got involved in the appearance of Bifacial points.4. As Bifacial points developed, Backed Blades also gradually declined approximately 20,000 years ago.5. Consequently, this led to the development of Micro-blades, which went well with Bifacial points approximately 19,000 years ago.6. Although Micro-blades became extinct under the influence of the appearance of Tanged points, Arrow-heads, and Potteries approximately 16,000 years ago, Bifacial points kept being produced.Approximately 18,000 years ago, bifacial points which were produced symmetrically and bifacially were widely developed in Japan; however, the stones, the size of the material by exfoliate technique, and the processing method were different from what was expected.Such transitions have been investigated in each region, which helps us understand that stone implements in the Paleolithic Era were found at multiple stratified sites in the thickly sedimented Pleistocene tephra at the Sagamino Terra, Kanagawa Prefecture.

Les problèmes géologiques et typologiques des sites paléolithiques dans le Nord-Est du Japon

The northeastern area of Honshu is composed of six departments: Aomori, Iwate, Akita, Miyagi, Yamagata and Fukushima. The study of Paleolithic began in 1927 and has given place to the discovery of the site of Hanaizumi. Subsequently, one pushed the research below on land and the discovery of the first paleolithic site in Iwajyuku happened in 1946. Then, H. Nakagawa took back a success of survey of the geomorphological processes and the ordering of the fluviatile terraces with some layers from the volcano-sedimentary deposit of the Pleistocene in the basin of Kitakami and the one of Mabechi. Therefore, we understood that the archaeological levels of the region contain several sedimentary deposits volcano of quaternary origin from the Mounts Öu. In the basin of Kitakami, one noted the deposit of fall pyroclastic of Aiçra (AT) above the layer of the local volcanic ash from Kurosawajiri. Especially, it is one key of an important layer, the last horizon located under AT and above the tephra of Daïfudô from the local volcano, the pyroclastic stream of Towada and the involution of the layer of the volcanic ash from Kurosawajiri. More than 610 paleolithic sites has been counted in the Northeast.

Le Paléolithique supérieur dans l’île d’Hokkaïdo

Since the discovery of the first Paleolithic site in Hokkaido, we consider that the time in the half more than centuries already passed, and float today. However, our research is still a way. By today, we have not discovered the trace about a Pithecantropines (Homo erectus) and a Paleanthropic man (Homo sapiens neanderthalensis) at all in this region. We know that a Neanthropic man (Homo sapiens sapiens) dominated all the continents except Antarctica in the final time of the Pleistocene era. And they passed along the dried shoal which appeared to the north in the same time from the Asian Continent to the Island of Hokkaido, and reached it to this place. The first attainment time is an age which exceeds 20,000-years before a little from the present. We are not checking a fact which exceeds it you to be much. However, the habitants of these beginnings left the trace of the activity of them in large numbers, so that he was wonderful to inside of this island. The studies-of-prehistory research in Hokkaido has little proof of the natural science field concerned on age determination or chronology. This has serious restriction. However, the tephra-chronology of volcanic ashes has played the big role uniquely. The eruption of the Eniwa volcano of the Hokkaido central part is especially a very important index. This volcano blows off ash fall (En-a) in large quantities, and covered all large ranges. This deposited volcanic-ashes layer plays a big role to discernment of an old industry and a recent industry on the cultural chronology. The obsidian from this island and nearby hard shale was used for many industries of this Upper Paleolithic cultures as main materials. Although obsidians in the island where the different four outcrops are known well. This rock was mined in large quantities, and was carried in various places. As well as many examples in the world, we divided this rock, and the human beings of the prehistoric age were demanded for it, and it was often utilized. In it, especially the outcrop of Shirataki was located in the northern part of Hokkaido, and was very important. Large quantities of obsidian from Shirataki outcrop is discovered in a large number of Paleolithic sites within a segment 700km in diameter at least. It covered the territory in Hokkaido and circulated further also except this island. This fact circulated as important trade materials on stone-tool fabrication among the human-beings groups from whom this island's every place differed. In this time, human beings’ activity in Hokkaido is a clear proof, which was not isolated at all. As for the studies of the prehistorians of Hokkaido distinguish, the exception put the technical process of eight different microblade productions. The technical process of some of them was limited only to the specific narrow area. Or it is proved that other technical processes are widely connected with the human-beings group of the Asian Continent on the contrary. At present, our research grasps the whole second-half Paleolithic culture, and has not yet established the year system edited by locally complete. The oldest industry of this area composed the typical stone tool of second-half Paleolithic culture from the beginning, and was accompanied by the manufacturing technique of a braid and microblade. The feature is the example in which the ruins of Kashiwadai-I were most excellent. These ruins correspond at time older than deposition of the Eniwa volcano tephra. It is located at the chill time in the second half of a Würm glacial period. The second continuing step is an industry of succession newer than this volcano tephra. It is raised as an example with Ôsatsu-16 typical ruins etc. The third phase is an industry of the end term of second-half Paleolithic culture. It is simultaneously located in the dawn of Jōmon culture. The feature of this cultural aspect is a transitional cultural stage which earthenware appears and is called what is called “Sub-Neolithic-Culture”. We can check having passed expansively, while the aspect of this last continues within a short period of time relatively.

Le Paléolithique supérieur dans l’ouest de l’île principale du Japon

The Kinki, Chugoku and Shikoku regions are located in the western part of the Japanese mainland. This area lacks the Pleistocene volcanic soil except a part of Chugoku Mountains. For this reason, the chronology of the late Paleolithic stone industries has been mainly studied by technology and typology of the fields excavated. However, after the late 1980s, the analysis of volcanic ash that contained the Paleolithic sediments had remarkable development. As a result, the cultural layer between the distant Paleolithic sites is compared by several widespread volcanic ashes such as Aira-Tanzawa (in short AT) as key bed. In this paper, we offered chronological order of the late Paleolithic culture in these regions by comparing cultural layers on the basis of the widespread volcanic ashes, referring to typological analysis of industries. The Sétoüchi technique and Ku industry characterize the late Paleolithic culture in these regions. The Sétoüchi technique is the unique one to produce the Ku type backed knife blunting on only one side, using the particular side-blow flaking technology based on physical characteristics of sanukite stone which is a kind of andesite. However, a hypothesis named the “Sétoüchi concept” was proposed in 2001, and it has been used as a substitute of the “Sétoüchi technique” by a few Japanese researchers. So we point out the mistake of the Sétoüchi concept relying on the fact which yielded stratigraphically two different industries in the Suncheon site.

Le Paléolithique supérieur du plateau de Musashino et les hauteurs de Tama aux alentours de Tokyo

The Upper Paleolithic at the region of Tokyo that itself called also the Japanese Preceramic age that possesses a large number of excavations and those studies during the dawn of Paleolithic study in this country. The Preceramic age or the Upper Paleolithic has been raised the curtain by the discovery of a piece in obsidian, in 1949, in the loam of Kantô, at Iwajyuku site. We explain above, on the stratigraphy, the chronology and the situation and the evolution of site around Tokyo. It is a region to the highest density of the Upper Paleolithic sites in the archipelago of Japan and the systematic excavation according to the stratigraphy of loam formation has been done for the first time in the country. The authentic chronology has been proposed to the years 60s that based on the discovered lithic industries on the plateau of Sagamino and Musashino. This chronology was used for a long time that it made a role like a norm for the whole country. Not only, after again an accumulation of the research until the present, we understand the different periodic activities between the Tama hills, the plateau of Musashino, the plateau of Sagamino, the North of Kantô district and the plateau of Simôssa. Of course, there is a complex circumstance that the apparition and the disappearance of various types of lithic instruments are different, and every type tools are not universal around Tokyo area, in the district of Kantô. The final of Upper Paleolithic on the archipelago of Japan divides extensively in two parts East-west that the East of Japan is characterized by the well-organized aspect microlithic tendency and the west is characterized by the trend of microlite, trapeze and tool on transverse blade. In such general tendency, the region of Kantô is located therefore in the center on the archipelago of Japan that it showed sets of every different time.

Existe-t-il un Paléolithique inférieur au Japon ?

All Lower Paleolithic sites discovered by Mr. Shinïchi FUJIMURA from 1981 to 2000 were falsified by himself. We wonder if Lower Paleolithic sites really exist (corresponding to a period of 30,000years ago in Japan) in the archipelago of Japan. We examined cultures of sites likely dating to the Early Upper Paleolithic and Lower Paleolithic discovered in the archipelago of Japan. While Japan was continuous with the continent in the Mindel glaciation (400,000years ago) or in the Riss glaciation (200,000years ago), Homo erectus or Homo heidelbergensis with the lithic industry of the Acheulean arrived in the archipelago of Japan. Thereafter, they survived on the islands of Japan cut the continent to the Upper Paleolithic while keeping the industry.

Quelques considérations sur la relation entre le Paléolithique chinois et le Paléolithique japonais

We present a description of the cultural connection between the Chinese and Japanese Paleolithic as the main topic of this article. In this special issue, Takehana and his collaborators discuss the relationship between Paleolithic culture in Hokkaido of north Japan and the coastal Siberian Paleolithic culture. Accordingly, we focus on the Paleolithic cultures of Paleo-Honshu Island and China. This region is made up of three large islands: Honshu, Shikoku, Kyushu, and several islets on their periphery. However, these islands were once connected to each other during the Ice Age and formed one large island: PaleoHonshu Island. Now, the East China Sea, the Yellow Sea, the Bohai sea and the Sea of Japan separate these islands from the Asian mainland. It appears that human beings who lived before Homo sapiens must have used the land bridge as the passage from the mainland to this region because their sea-crossing ability was extremely poor. We assume that because Homo sapiens of the Upper Paleolithic also chose narrow and shallow seas that were easy to cross for moving from the Asian mainland to the Paleo-Honshu Island, their migration did not happen at any time other than during the cold period that caused marine regression. In this article, we present three routes connecting the Asian mainland and Paleo-Honshu Island. The first is the southern route that connected southern China and south Kyusyu via Taiwan, the Sakishima Islands, the Yaeyama Islands, the Ryukyu Islands, and the Amami Islands. The second route is the western route that reached Kyushu through the Korean Peninsula and is thought to have passed through the so-called three seas Plain (a vast land area formed by the drying up of the East China Sea, the Yellow Sea, and the Bohai Sea). The third route is the northern route that passed through the Sakhalin Island and Hokkaido, reaching the northeastern part of Honshu. We think that gateways from the Asian mainland to the Paleo-Honshu Island might be limited to these three routes. However, the southern route presents a challenge. In the northern part of this series of islands, the Tokara Strait interrupted the passage from the Osumi Islands to the Amami Islands since it was so deep that it never dried up at any time.In addition to those, the distribution of the Paleolithic sites in China had remained roughly south of 40 degrees north latitude until 62,000 years ago. Therefore, it appears that paleolithic culture began to flow into Japan through the northern route after 62,000 years ago. For this reason, it is assumed that befor those years, the only route for cultural diffusion from the Asian mainland to Japan was the western route.

Chronologie du Paléolithique supérieur dans le Nord-Est de la principale île du Japon

Palaeolithic archaeology in Tohoku region has long been discussed on constructing chronology, however it is difficult to build reliable chronological order because of poor stratigraphic excavations. In recent radiocarbon dating has advanced. In this paper I discuss the relation between chronology and radiocarbon dating in Tohoku region. At first, I categorize the Palaeolithic industries and establish the chronology by analyzing tool typology, lithic technology, and stratigraphic data. I correlate it with radiocarbon data from sites in Tohoku region. The result of analysis shows that Upper Palaeolithic industries are divided into 18 categories and 8 periods on chronology. The calibration curve IntCal 13 indicated that oldest Early Upper Palaeolithic site appeared around 37,000cal BP, and late Upper Palaeolithic started about 27,000cal BP. The pottery first appeared as far back as around 16,000cal BP. Now we do not have enough radiocarbon data, so we have to gather and examine more 14C data.

Szeletian or not Szeletian. Bifacial industries from three open-air Middle Palaeolithic sites from the Cserhát Mountains (Northern Hungary).

Szeletian or not Szeletian. Bifacial industries from three open-air Middle Palaeolithic sites from the Cserhát Mountains (Northern Hungary).

Timing of Neanderthal occupations in the southeastern margins of the Massif Central (France): A multi-method approach

The middle Rhône valley, located at the southeastern margins of the Massif Central in France, produced a large number of Middle Palaeolithic sites, most of which dated to the Middle and Late Pleistocene. Due to its position, connecting northern Europe and the Mediterranean basin, this corridor and the surrounding plateaus are of particular interest in the study of human cultural evolution, including the emergence of Middle Palaeolithic technology around 300,000 years ago and its variability over time, as well as the subsistence and mobility strategies of Neanderthals.In the last 20 years, several research projects undertaken in this region allowed to revise key Middle Palaeolithic sequences. This work aims at synthesising previous and new chronological data obtained by using uranium-series of speleothems and bones, infrared stimulated luminescence of feldspar and electron spin resonance of tooth enamel and quartz. We review previous ages obtained in the area and present 43 new ages that are discussed together to propose a reliable spatiotemporal framework for Neanderthal occupations. We focus on major sites in the region: Payre, Ranc-Pointu 2, Baume Flandin, Abri du Maras, Grotte des Barasses II, Abri des Pêcheurs, Grotte du Figuier and Grotte de Saint-Marcel. They all provided significant information related to the biological and behavioural evolution of Neanderthal populations on the right bank of the Rhône valley. We present here the updated chronology for the Middle Palaeolithic of this area, ranging from ca. 300,000 to 40,000 years ago.

The past in dust: current trends and future directions in Pleistocene geoarcheology of European loess

ABSTRACTLoess is a main archive of Pleistocene landscapes and environments and therefore has an important connection to the preservation and interpretation of Paleolithic sites. In Europe, anthropogenic sites have been found in loess because of past local occupation. At one extreme, sites are well preserved with minimal disturbance often accompanied by embedded proxies to estimate ecological parameters. On the other hand, loess deposits have undergone post‐depositional alterations such as weathering, pedogenesis or bioturbation due to changing environmental conditions or other disturbances that obscure anthropogenic sites. We outline the current state of research and connections between Paleolithic archeology and loess research while introducing a series of subsequent regional case studies as part of a special issue. We also make recommendations for future work to incorporate a wider variety of methods to create more robust inferences on hominin and environmental evolution and their connections.

Horashim East: a newly discovered Middle Palaeolithic site in central Israel

ABSTRACTHorashim East is a newly discovered Middle Palaeolithic open‐air occurrence in central Israel, revealed during a thematic prehistoric survey. Hundreds of lithic items were found, including an early‐stage biface, Levallois cores and products. As only a few open‐air settlements are known from the Middle Palaeolithic Levant, the discovery of Horashim East sheds new light on human land‐use patterns during this period and reinforces the notion that central‐eastern Israel was favourable for human settlement throughout the Palaeolithic.

ESR dating of the Hougou Paleolithic site in the Nihewan Basin, North China, using both additive and regenerative dose methods

The Nihewan Basin is one of the most important areas for the study of early human evolution and land mammals in East Asia. More than 100 Paleolithic sites have been discovered in the basin, spanning the Early Pleistocene to the Late Pleistocene. The chronological framework for the Early Pleistocene sites is well established using magnetostratigraphy. However, few independent ages are associated with Middle Pleistocene sites; one such example is the Hougou Paleolithic site, where interpolated magnetostratigraphic ages are not precise and accurate enough, owing to the artifact layer of the site is far relative to the Matuyama/Brunhens (M/B) boundary. In this study, we use the ESR signals of Al and Ti–Li centers in quartz to date the Hougou site. The advantages of the regenerative dose method over the additive dose method were discussed. Our ESR results indicate that the age of the Hougou Paleolithic site is between 436 ± 30 and 416 ± 42 ka, approximately with an average of 426 ± 36 ka, which corresponds to Marine Isotope Stage (MIS) 12 or loess layer L5. In addition, the disappearance time of the eastern part of the Nihewan paleolake may be approximately 430 ka.

Organization of the Living Space and the Inferred Economic Activity at the Middle Paleolithic Site in Saradj-Chuko Grotto (based on materials of layer 6B)

The use of modern methods of microstratigraphic and planigraphic analyses allows the authors to speak about features of organizing life space in the Middle Paleolithic sites. The layer 6B at Saradj-Chuko grotto can be defined as an actively occupied Middle Paleolithic habitation site, where ancient humans were engaged in manufacture and use of obsidian tools. A tracelogical analysis allowed the authors to reconstruct various economic activities of ancient humans. For the first time for the Middle Paleolithic site in the northern slope of the central Caucasus, a tracelogical analysis was carried out taking into account the space distribution of tools over the site area, which allowed us to study features of human activity at different areas of the site. The new data are considered within a broad context of the Middle Paleolithic of the Caucasus, as well as the available data on economic activity and residential structures in various sites are analyzed.

A Multi-Dimensional Approach to Investigate Use-Related Biogenic Residues on Palaeolithic Ground Stone Tools

ABSTRACT Recent advances in the role played by dietary carbohydrates in human food webs during the Palaeolithic highlight that starchy foods were part of the diet well before crop domestication. Although certain plants can be eaten raw, intentional processing such as mechanical reduction using stone tools and thermal treatment readily increases the assimilation of nutrients for metabolic functions and for storing. We present a multi-techniques approach designed to combine micro to nanoscale analyses applied to percussive stones to identify their function using micro-wear traces and use-related biogenic residues. The starch grains extracted from functionally active areas of the ground stone tools were scanned using optical microscopy (OM) down to the nanoscale (SEM) and by applying different spectroscopic and spectrometric techniques like FTIR, ToF-SIMS, and IRMS. The combined analyses carried out at different resolutions – morpho-structural and molecular levels – contribute to an unprecedented methodological refinement regarding the intentional processing of starch-rich plants as early as 40,000 years ago at the boreal latitudes. Our preliminary data on pestles and grinding stones from Early Upper Palaeolithic sites of the Pontic steppe (Moldova and Russia) show the suitability of the analytical techniques involved and also the difficulties encountered in detailing authentication procedures of ancient starch candidates.

OSL Chronology of the Siling Co Paleolithic Site in Central Tibetan Plateau

When and how was the Tibetan Plateau (TP), one of the least habitable regions on Earth, occupied by humans are important questions in the research of human evolution. Among tens of Paleolithic archaeological sites discovered over the past decades, only five are considered coeval with or older than the Last Glacial Maximum (LGM, ∼27–19 ka). As one of them, the Siling Co site in the central TP was previously announced to be ∼40–30 ka based on radiocarbon dating and stratigraphic correlation. Given the loose chronological constraint in previous studies, we here re-examined the chronology of the Siling Co site with the optically stimulated luminescence (OSL) dating technique. Four sections from the paleo-shoreline at an elevation of ∼4,600 m in southeastern Siling Co were investigated, with stone artifacts found from the ground surface. Dating results of nine samples delineated the age of ∼4,600 m paleo-shoreline to be ∼10–7 ka (∼8.54 ± 0.21 ka in average). This age indicates that the Siling Co site is not earlier than the early Holocene, much younger than the former age. The revised age of the Siling Co site is consistent with the wet and humid climate conditions on the TP during the early Holocene.

A new chronological framework and site formation history for Cova del Gegant (Barcelona): Implications for Neanderthal and Anatomically Modern Human occupation of NE Iberian Peninsula

The chronological framework for Neanderthal occupation and demise across Europe continues to be debated. In particular, there is still uncertainty regarding the nature, timing and regional expressions of the Middle to Upper Palaeolithic transition associated with the disappearance of Neanderthals and the broader expansion of modern human populations in Europe around 42–40 thousand years ago (ka). The geographical and chronological distribution of Neanderthal populations also remains difficult to evaluate owing to the practical challenges of directly dating human fossils at many sites, and the fact that a large proportion of Neanderthals sites lie close to, or well-beyond, the limits of radiocarbon dating. Cova del Gegant – one of the few sites in north-eastern Iberian Peninsula to yield Neanderthal fossil remains, associated Mousterian archaeological layers, and occupations related to the Middle and Upper Palaeolithic transition – is a key locality for informing these ongoing debates. Here we provide a comprehensive chronological framework for the Cova del Gegant site using multiple radiometric dating techniques (uranium-thorium (U–Th), radiocarbon and luminescence dating), sedimentological and micromorphological analyses, and Bayesian modelling. This integrated chronostratigraphic approach enables us to reliably reconstruct site formation processes and history, and undertake improved correlations with other sites regionally. The results allow us to sub-divide the Cova del Gegant sequence into three sections spanning ∼94 ka to ∼32 ka, namely: a Middle Palaeolithic sequence covering ∼94–59 ka, a Châtelperronian/Aurignacian section spanning ∼43–39 ka, and a Late Aurignacian/Gravettian section spanning ∼34–32 ka. The Neanderthal fossil remains accumulated in the cave between the end of Marine Isotope Stage (MIS) 5/MIS 4 and the beginning of MIS 3, during two different events dated to ∼72–67 ka and ∼60–52 ka. The chronological framework for Cova del Gegant is in accordance with that reported for other Middle and Upper Palaeolithic sites in north-eastern Iberian Peninsula, and reveals a record of successive human occupation coinciding with a period of progressive global cooling and lowering sea levels (end of MIS 5 through to MIS 2). Sedimentological evidence points to the emergence of a coastal platform in front of the cave and indicates that local palaeoenvironmental conditions likely benefited human displacements along the littoral margin, and favoured repeated occupation of the cave during the Late Pleistocene.