Geoarchaeology-An International Journal最新文献

Ridge and furrow cultivation is the most widely used agricultural technique in medieval and postmedieval Europe, but the fertilization of soils during their use is not yet fully understood. Pedological analyses of this cultivation technique provided information, which led to the assumption that some of the investigated sites in Northern and Central Germany were manured with livestock excrements during cultivation. The objective of this study is to determine whether and how the soils have been fertilized and which materials were applied for this purpose. We investigated soils at five sites using phosphate and steroid analyses (stanols and bile acids), black carbon analyses, and a micromorphology study. The results showed that livestock waste was likely used as fertilizer at four of the five studied sites at low intensities, with pigs and herbivores being the probable sources of the excrement. But also the application of human feces to the soil might be possible at least at one site. Often used agricultural methods such as plaggen cultivation and an intentional charcoal input to enhance soil fertility could not be clearly verified for our study sites.

We examined 2947 basalt and volcanic glass artifacts from 38 sites in leeward Kohala. Nondestructive energy-dispersive X-ray fluorescence provided initial geochemical characterizations. Wavelength-dispersive X-ray fluorescence (WDXRF) and thermal ionization mass spectrometry (TIMS) analyses were completed on samples from ambiguously sourced groups. No more than 13.9% of the probable and definite adze-related debitage originated in leeward Kohala. Notably absent are lithic materials from the nearby Pololū Adze Quarry in windward Kohala. Material from the more distant Mauna Kea Adze Quarry accounts for 41.6% of the adze debitage. Another 38.8% of the adze debitage matches with a tholeiitic source or sources long assumed to be Kīlauea Volcano in Kaʻū, but WDXRF and TIMS isotopic data do not support a Kīlauea source. Centralized adze production and distribution networks best explain adze distribution. Scoria abraders appear to have been regularly transported from the Kona district to leeward Kohala. Volcanic glass sources loosely align with distance-decay trends, but show greater reliance on Puʻuwaʻawaʻa material by 1650 CE.

Beach sand dredging projects off the coast of Southern California provide data for improved understanding of the stratigraphic setting for early Holocene sediments and the potential for offshore buried archaeological materials. Geophysical data, core sediments, and invertebrate fossils allow models to be developed for six borrow sites within drown river valleys off San Diego County. These site-specific models were tested during dredging operations, and the dredge spoil was monitored for archaeological materials. Two of the borrow sites yielded stone bowls consistent with those found in previous offshore archaeological investigations in this region. These artifacts, however, were determined to come from nearshore and lagoonal sediments, not appropriate for direct occupation, raising questions about both the function of stone bowls and the process that resulted in their deposition. The competing hypotheses presented are that these bowls originated in settlements located adjacent to the lagoons, but were eroded and redeposited into the lagoon during transgression, or that they were part of a fishing toolkit used from boats or in shallow waters within the lagoon. This project illustrates the potential for commercial development projects to yield information on submerged archaeological resources, as well as the challenges.

Central Asian caves with Palaeolithic deposits are few, but they provide a rich record of human fossils and cultural assemblages that has been used to model Late Pleistocene hominin dispersals. However, previous research has not yet systematically evaluated the formation processes that influence the frequency of Palaeolithic cave sites in the region. To address this deficiency, we combined field survey and micromorphological analyses in the piedmont zone of south Kazakhstan. Here, we present our preliminary results focusing on selected sites of the Qaratau mountains. Sediment cover varies among the surveyed caves, and loess-like sediments dominate the cave sequences. The preservation of cave deposits is influenced by reworking of cave sediments within the caves but also by the broader erosional processes that shape semiarid landscapes. Ultimately, deposits of potentially Pleistocene age are scarce. Our study provides new data in the geoarchaeologically neglected region of Central Asia and demonstrates that micromorphology has great analytical potential even within the limitations of rigorous survey projects. We outline some of the processes that influence the formation and preservation of cave deposits in Kazakhstan, as well as broader implications for the distribution of Palaeolithic cave sites in Central Asia and other semiarid environments.

The provenance of medieval building stones links historic constructions with their quarrying areas, thereby revealing medieval trade routes and the spatial organization of past societies. In northern France, the Duchy of Normandy played a significant role in the medieval history of Europe, situated at the centre of the disputes between the English and French kingdoms. However, the historical documentation from this period is scarce, particularly in terms of the quarrying industry. Our study aims to define the quarrying areas and their diffusion zones and map the territorial organization of Eastern Normandy during the 10th–14th centuries. A multidisciplinary procedure using archaeological, geological and geochemical techniques was designed to establish the provenance of Normandy Chalkstone. First, we obtained a representative assembly of building stones by the selection and strategic sampling of 22 buildings. Second, we determined areas of chalk bedrock from a geological map rendered through GIS and sampled chalkstones from natural outcrops and quarries. In total, 118 samples from buildings, quarries and natural outcrops were characterized via optical microscopy and geochemical analyses for major, minor and trace elements (XRF, ICP-MS and ICP-OES), as well as for ⁸⁷Sr/⁸⁶Sr isotope ratios (MC-ICP-MS). The application in situ of pXRF analysis allows for the identification of Normandy Chalkstone sources preserved in archaeological sites. The results indicate that all chalkstones came from five local varieties of Normandy Chalkstone and one of Shelly Limestone imported from nearby regions. The suitability of chalkstone as construction material was evaluated in situ using a sclerometer, which revealed that the singular and local geological features of the chalkstone make it suitable for walling. Our study demonstrates the development of a prominent and relatively continued quarrying industry over the 10th to 14th centuries in Eastern Normandy. The main quarrying areas were constituted of three chalkstone diffusion zones that run coevally with smaller and apparently sporadic quarries. The chalkstone diffusion was strongly related to the occurrence of singular and local geological resources and the stone transport system, which favoured the use of effective fluvial and maritime navigation for transport over 50 km from the quarrying areas.

Mahkemağcin Underground City (MUC) is a four-floored rock-cut dwelling complex carved into ignimbrite tuffs of the Early-Middle Miocene age in central Anatolia. The whole interior of the complex is covered by a 1–5 cm thick alteration crust that is not detected in any cave or outcrop in the region. This crust is investigated using microscopy, scanning electron microscopy, X-ray diffraction and X-ray fluorescence analyses, and the results are discussed from the geomechanical point of view. The colour of the outer surface of the crust is black, which turns red inside and grades into pale yellow above the white parent rock. The compaction and solidity of the crust are relatively high, as much as double that of the parent rock. The crust seems to have prevented and/or significantly decreased the erosion of the surfaces of the room walls. Mineralogical and chemical analyses together with experimental studies on selected samples suggest that such a crust could have formed because of thermal alteration at high temperatures ca. 600–950°C. On examination of the heated samples, the main geochemical changes within heated rocks were (i) an increase in silica concentration by ca. 2%–3% and (ii) the disappearance of zeolites and sericites. Thermoluminescence dating of the crust revealed thermal resetting of quartz crystals within the ignimbrite tuff at 243 ± 260 CE. All the analytical methods applied to the site indicate that the crust was obtained intentionally, possibly by burning woods indoors, aiming to harden the wall surfaces, mainly by Galatian people of the early Medieval time.

Asaviec 2 in the Kryvina wetland is one of the best known and the most thoroughly investigated Stone and Bronze Age lake settlement sites in Northern Belarus. Previously, research on the site used excavations and coring, typological analysis and radiocarbon dating of the find material, as well as stratigraphic, lithological and palynological analyses. However, geophysical methods were not used. This study was carried out to test the use of ground-penetrating radar (GPR) both at this particular site and in peaty sediments generally. The main goal was to determine the lateral spread of the occupation layer and traces of ancient habitation activity. The GPR reflection profiles have been correlated with coring data and previously excavated archaeological profiles. The chaotic pattern in the GPR reflection profiles has been interpreted as disturbed peat, thereby indicating human activity. The areas of disturbed peat and the lower boundary of the peat body were traced and mapped. The occupation layer and signs of human activity are irregularly distributed and largely coincide with the high and intermediate forms of the subsoil relief, but not with the low forms. As a result, we have concluded that GPR is a valuable tool for determining occupational layers in wetlands when verified by excavations and coring.