We present the ‘SISAL webApp’—a web-based tool to query the Speleothem Isotope Synthesis and AnaLysis (SISAL) database. The software provides an easy-to-use front-end interface to mine data from the SISAL database while providing the SQL code alongside as a learning tool. It allows for simple and increasingly complex querying of the SISAL database based on various data and metadata fields. The SISAL webApp version currently hosts SISALv2 of the database with 691 records from 294 sites, 512 of which have standardized chronologies. The SISAL webApp has sufficient flexibility to host future versions of the SISAL database, which may include allied speleothem information such as trace elements and cave-monitoring records. The SISAL webApp will increase accessibility to the SISAL database while also functioning as a learning tool for more advanced ways of querying paleoclimate databases. The SISAL webApp is available at http://geochem.hu/SISAL_webApp.

The nineteenth century was a dynamic period for hacienda workers on the south coast of Peru. Former Jesuit vineyards with two of the largest enslaved African-descended populations in rural coastal Peru—the haciendas of San Joseph (San José) and San Francisco Xavier (San Javier)—and their annexes in Nasca's Ingenio Valley underwent dramatic transformations with the replacement of their grapevines with cotton and the introduction of new types of workers. Cantonese indentured workers were contracted beginning in the 1830s, and the majority-enslaved workforce was legally emancipated in 1854. Seasonally, highland Andean workers joined the demographically shifting permanent hacienda population. We use evidence from excavated midden contexts at San Joseph, San Xavier, and San Joseph's annex of Hacienda La Ventilla to explore these changing agroindustrial dynamics and worker well-being in the eighteenth and nineteenth centuries. Despite the transformations at the estates, we find that culinary practices developed by enslaved Africans and their descendants during the Jesuit administration, such as the preparation of one-pot meals and stews, continued into the republican era among Cantonese indentured laborers and wage workers of Indigenous, mestizo, and Cantonese origins. We argue that such strategies centered on foodways were a crucial aspect of worker self-care regimes and broader well-being.

Arid regions are especially vulnerable to climate change and land use. More than one-third of Earth's population relies on these ecosystems. Modern observations lack the temporal depth to determine vegetation responses to climate and human activity, but paleoecological and archaeological records can be used to investigate these relationships. Decreasing rainfall across the Late Holocene provides a case study for vegetation response to changing hydroclimate. Rock hyrax (Procavia capensis) middens preserve paleoenvironmental indicators in arid environments where traditional archives are unavailable. Pollen from modern middens collected in Dhofar, Oman, demonstrates the reliability of this archive. Pollen, stable isotope (δ13C, δ15N), and microcharcoal data from fossil middens reveal changes in vegetation, relative moisture, and fire from 4000 cal yr BP to the present. Trees limited to moister areas (e.g., Terminalia) today existed farther inland at ~3100 cal yr BP. After ~2900 cal yr BP, taxa with more xeric affiliations (e.g., Senegalia) had increased. Coprophilous fungal spores (Sporormiella) and grazing indicator pollen revealed an amplified signal of domesticate grazing at ~1000 cal yr BP. This indicates that trees associated with semiarid environments were maintained in the interior desert during ~3000–4000 yr of decreasing rainfall and that impacts of human activity intensified after the transition to a drier environment.

Sea-level rise and settlement are investigated at Ta'ab Nuk Na, an ancient Maya salt works in Belize, by examining samples from wooden posts and marine sediment. The samples included Post 145 of Building B and the Nunavut beam, along with marine sediment columns cut from beside both wooden posts. The sediment columns were sampled at 2 cm intervals. Loss-on ignition confirmed the presence of organic material. Identifying the organic content involved removing nonorganic material from the sediment and sorting the organic material under magnification. This procedure established that most of the organic material was red mangrove (Rhizophora mangle). Red mangroves tolerate salt water, but under conditions of sea-level rise, the plants grow vertically to keep their leaves above water. Sediment, leaves, and detritus trapped in the prop roots form mangrove peat, which serves as a proxy for sea-level rise. AMS dating of fine red mangrove roots determined that the local sea levels rose at Ta'ab Nuk Na throughout the Late Classic period and continued into the Postclassic period. Radiocarbon dates obtained from the wood-post samples yielded Late Classic–period dates. Comparing the radiocarbon dates from the wooden posts and the sediment core samples determined that the site was abandoned before the rising seas flooded the area. Evidently, sea-level rise did not play a role in site abandonment.

The coastline of Cyrenaica, Libya, is rich in cultural heritage dating from prehistory to the modern periods. Despite the region's long-standing and strong connection to the sea, maritime archaeology remains a peripheral, but growing, branch of archaeology in Libya. This paper aims to provide an overview of the maritime projects that have been carried out in Cyrenaica in the past. Furthermore, it will highlight the main threats and damages that coastal heritage faces today and will provide some suggestions on how the discipline could develop in the future. The Cyrenaica Coastal Survey (CCS), a collaboration between the Maritime Endangered Archaeology (MarEA) project and the Department of Antiquities (DoA), Libya, will serve as a case study of an ongoing project that documents and assesses the condition of sites along the Cyrenaican coast between Tocra and Apollonia.

The discovery of a major archaeological complex at Faughan Hill, County Meath, was first reported on in the Proceedings of the Prehistoric Society in 2015. Comprising a series of large hilltop enclosures, probable burial sites, and associated features, the character and scale of the complex marked this out as an important focal centre in a region populated with some of Ireland’s largest and most spectacular monument ensembles, not least at the Hill of Tara, 15 km to the south-east. A more complete picture of the site has since been revealed through further geophysical survey followed by test excavations by the Discovery Programme’s Tara Research Project. Two trenches excavated across the hilltop enclosures in 2017 yielded evidence of four discrete phases of activity spanning some 3000 years, from the mid-4th to mid-1st millennia bc. During the Middle Neolithic the hilltop was encircled by a fenced enclosure (3635–3380 cal bc) possibly associated with the production of stone tools. At 250 m in projected diameter it is one of the largest enclosures of the 4th millennium known in Ireland. This was superseded in the Late Bronze Age by a far more substantial, 400 m diameter multivallate enclosure (1280–920 cal bc) representing the only excavated hillfort of its type in Meath. The hill was the focus of renewed activity during the Early Iron Age (800–520 cal bc) and later became central to the political ambitions of aspiring, early Uí Néill kings of Tara, achieving particular reknown as the burial place of their eponymous ancestor, Niall of the Nine Hostages. Developments at Faughan are illuminated further by a wealth of prehistoric settlement and ritual sites in the surrounding area, as well as early documentary sources, and, collectively, speak to a regional centre and gathering place with long-lived social, symbolic, and political significance.

We constructed a laser ablation (LA) system using a diode laser for the accelerator mass spectrometry radiocarbon (AMS 14C) measurement of organic materials. The system could extract adequate CO2 to analyze small masses (0.1 mg C) at a resolution of 250 µm by a 5.5 W diode laser. The LA system was assessed using standard materials (IAEA-C1, IAEA-C2, IAEA-C3, IAEA-C6, and Ox II) and applied to natural tree ring samples. For the LA sampling of organic samples, which generally results in incomplete combustion, tungsten (VI) oxide was used as an oxidant to achieve complete burning. The results of the measurement of standard materials showed a low 14C background of F14C 0.0085 ± 0.0005 and reasonable reproduction of 14C values. Finally, we applied this system to a single-year analysis of tree-ringed spruce timber in Alaska. It was observed to have a detectable background for the 14C bomb peak.