It remains a little-known fact that from March 1766 to May 1767 Jean-Jacques Rousseau – fleeing from persecution in France and Switzerland – stayed in the remote hamlet of Wootton in Staffordshire. There he composed the first half of his Confessions in a garden hermitage, a structure half natural and half architectural, ever since known as Rousseau’s Cave. Our paper records the hermitage in its current state (exposed to the elements); it creates a digital reconstruction of the hermitage as it was in Rousseau’s lifetime; and it provides digital access to a monument that is otherwise not generally accessible.

Our paper records a modest but fairly typical eighteenth-century garden hermitage and also, with the highest quality digital reconstructions and fly-throughs, provides a new insight into the creation of one of the world’s greatest works of literature.

The paper contributes substantial new material to the study of Jean-Jacques Rousseau and also contributes to garden history and the phenomenon of the garden hermitage.

The consolidation of village life in the southern Andes implied profound transformations in human lifeways and in people’s relationships with the environment, plants, and animals. Contributions from archaeological sciences have the potential to shed light on these transformations, particularly by providing new information about patterns of food production and consumption. In this article, we present the first results of organic residue analysis on ceramic containers of early village societies of northwestern Argentina (La Ciénega Valley, AD 200–600) by gas chromatography coupled with mass spectrometry (GC-MS). We tested previous characterizations of La Ciénega village’s subsistence strategies through the lens of absorbed organic residues in pottery. Preliminary evidence indicates a predominance of biomarkers associated with vegetable products in the vessels and a lower contribution of animal fats, suggesting a strong reliance on plant-based foods among early villager groups in La Ciénega settlements.

Pole-and-thatch structures built directly on the ground surface were likely common in antiquity in the Maya area as residences, kitchens, workshops, storehouses, and for other uses, although the actual wooden architecture normally decays and often leaves no mounded remains. Various estimates are made to account for these “invisible sites” in population estimates based on mound or plazuela groups. Wooden building posts and associated artifacts preserved in mangrove peat below the sea floor in Punta Ycacos Lagoon, southern Belize provide an opportunity to address population size, material wealth, and household activities at “invisible sites.” The distribution of wooden building posts and artifacts at the Ch’ok Ayin underwater site indicates it was a residential household group with several pole-and-thatch buildings around a plaza. The householders focused on salt production, with artifactual evidence of brine enrichment and brine boiling, in addition to other supporting activities, and participated in Late Classic marketplace trade for goods from varying distances. Holocene sea-level rise that flooded low-lying coastal areas also obscured ancient Maya sites, making them “invisible” in the modern landscape.

In this paper a part of a new multi-proxy results obtained from the Kotoń landslide fen deposits (the Beskid Makowski Mountains, the Outer Western Carpathians, S Poland), including loss on ignition analysis, plant macrofossil analysis and radiocarbon dating is presented. The aim of the study was to verify whether the reconstructed local palaeoecological stages of the Kotoń fen development could be correlated with the Bølling-Older Dryas-Allerød sequence and to verify whether the rarely recognised short GI-1d/Older Dryas climate cooling affected the regional and local palaeoecological record of the Kotoń deposits. Results showed that four palaeoecological stages of development (poor-in-vegetation waterbody, waterbody with aquatic succession, calcareous extremely rich fen and moderately rich fen) determined for the Kotoń landslide fen deposits between ca. 14,600–13,500 cal BP stay in agreement with the earlier pollen division of the Kotoń deposits and with the extraregional chronology of the Greenland ice cores. The influence of GI-1d/Older Dryas climate cooling on the surrounding and regional vegetation was recognised for the deposits of Kotoń and other localities in a form of open-space habitats with herbs, shrubs and sparse tree stands, e.g. steppe-tundra, reflecting the cold and dry climatic conditions. In case of local vegetation and palaeohydrological changes, the Older Dyas climatic oscillation was recorded as a shallowing of the existing palaeo-waterbodies. Although for other localities this process was attributed to the dry climatic conditions, in case of Kotoń site more detail multi-proxy research is necessary to distinguish the climatic impact from the autogenic succession.

This article concerns the interpretation of refuse dumps discovered at three abandoned Soviet tactical nuclear bases in Poland and how their analysis prompted a reassessment of archaeological remote sensing results. The study employed a range of methods to document the remnants of these secret sites, including declassified spy satellite images, aerial photographs, airborne and terrestrial laser scanning, UAV prospection, and field surveys, supplemented by CIA reports and Warsaw Pact military documents. These data bridge significant gaps in archival records, offering valuable insights into the history of these sites. However, the discovery of Cold War-era refuse dumps near the bases containing materials that do not conform to other evidence present an interpretative challenge. It exposed ‘survivorship bias’ in the dataset, prompting a re-evaluation of earlier conclusions.

Bone and tissue fractions, obtained in 2017 following hip replacement surgery on a healthy Caucasian male, born in 1944, reflect in their 14C concentrations the integrated effect of the lifetime metabolic uptake and replacement of atmospheric bomb 14C at different tissue-specific turnover rates. The 14C content of hair and nails reflects recent carbon uptake. The 14C values in healthy cartilage and bone collagen/apatite correspond to those of the “local” atmosphere during the 2005–2009 Northern Hemisphere growing seasons, while those from damaged areas of the femur head correspond to the atmosphere in 2013–2014. A simple bone growth and regeneration model used in combination with the NH atmospheric 14C concentrations indicates remodelling rates around 9% per year in the healthy bone and a doubling to tripling in the damaged area depending on the model chosen. The differences in 14C concentration observed in the fractions provide both a caveat for sample selection for the 14C dating of archaeological bones and an indication of its potential in forensics and as a diagnostic tool for turnover rates in medical studies.