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The paper proposes a methodology based on near‐infrared (NIR) spectrometry for studying stratigraphy and depth profiles in archaeological excavations. The NIR spectra can be used to describe and complement the wet chemical analysis. Soil samples were collected from a 0.8 m deep stratigraphy of a Neolithic site that were analyzed by three different NIR instrumentations. Phosphate‐ and magnetic susceptibility and inductively‐coupled plasma mass spectrometry measurements were also conducted as reference analysis. Principal component analysis on the data from three different NIR instrumentations gave useful score plots that allowed grouping of the samples. The results from the lab spectrometer were most useful, although the hyperspectral NIR camera was the fastest method to obtain spectra of many samples from one image. The paper shows how the NIR spectral data can be used for multivariate analysis to get meaningful conclusions on archaeological soils and sediments, especially in terms of understanding site development/phases and soil formation. [ABSTRACT FROM AUTHOR]

Middle Palaeolithic sites frequently present bones with a double function, linked to subsistence and technology, which are generally referred to as "retouchers" or "bone retouchers." These have been identified in several European sites from the Middle Pleistocene to Holocene, but different explanations of their origin and functionality have been cited. Although bone retouchers were made using various animal parts, they were usually produced from diaphyseal fragments of medium to large hoofed mammals. We present a small assemblage of six bone retouchers recovered from Stratigraphic Unit Xa (52.3 ± 4.6 ka), in the Middle Palaeolithic site of El Salt (Alicante, Spain), and compare our data with previous studies from several sites in south‐western France, northern Italy, and north‐eastern Spain. These tools were generated using diaphyseal fragments from red deer, horses, and other large mammals previously exploited by humans for meat and marrow. Our findings add to the existing knowledge on the behaviour and faunal resource management of the last Neanderthal groups on the western Iberian Peninsula before they disappeared from the region around 45–40 ka. [ABSTRACT FROM AUTHOR]

The Middle Neolithic tell of Imvrou Pigadi (~6920–6570 cal. years before present) belongs to a cluster of sites at the southern edge of the Plain of Thessaly, Greece. Following a specifically tailored geoarchaeological methodology comprising micromorphology coupled with Fourier‐transformed infrared spectroscopy, X‐ray diffraction, X‐ray fluorescence, and particle size analyses, we were able to reveal site formation processes linked with the construction of floors/occupational surfaces and successfully clarify a rather complicated archaeological stratigraphy. Moreover we present early evidence for specialized ceramic production contained in red, burnt strata rich in remnants of constructed combustion features and in situ pottery. The exclusion of a deliberate or accidental domestic fire as the cause of combustion, coupled with evidence of high firing temperatures of 600–700°C further supports a specialized ceramics workshop function of the site. The successful implementation here of an integrated analytical methodology enabled us to reveal the archaeological potential of Imvrou Pigadi and can be used to address similar archaeological questions at other Neolithic sites. [ABSTRACT FROM AUTHOR]

Microspatially offset Raman spectroscopy (micro‐SORS) is a recently developed analytical technique combining SORS with microscopy. With this method, highly diffusely scattering microlayers such as painted stratigraphies can be noninvasively probed. In this study, we explore micro‐SORS for identifying the chemical composition of subsurface layers in real, street art mural paintings as a new nondestructive method for the characterization of their stratigraphy. Two micro‐SORS variants, defocusing and full micro‐SORS, were tested and compared. Microspatially offset Raman spectroscopy (micro‐SORS) is an innovative nondestructive method for the characterization of turbid microlayered stratigraphies. In this paper, the method was used to identify the chemical composition of subsurface layers in real, street art mural paintings. Both the variants of micro‐SORS were shown to provide relevant information, also in challenging situation of heterogeneous real samples. [ABSTRACT FROM AUTHOR]

Archaeological science and field investigations are making greater use of multi-element geochemical survey as a tool for site prospection and intra-excavation analysis. This increasing use of geochemical survey is allowing a new field of geoprospection to develop, a technique that has specific relevance to the investigation of sites containing archaeometallurgical evidence, due to the high geochemical loadings within archaeological contexts produced from past metalworking activities. Correspondingly, there have been relatively few published examples that compare the results of geochemical surveys against excavation data. This study reports the use of geochemical data to investigate a multi-period mining site-scape at Alderley Edge, Cheshire, UK. The geochemical data is analysed using principle component analysis, which facilitates the identification of a number of geochemical anomalies. The site taphonomy and stratigraphic evolution of this mining site-scape is complex, with naturally occurring areas of lead and copper mineralization and a history of exploitation since the early Bronze Age. The geochemical anomalies were compared to the results of excavation within the survey area and this combination of excavation and prospection data allowed the reasons for the different geochemical anomalies to be explained. The article highlights the potential of using multi-element geochemical survey to investigate sites containing archaeometallurgical remains and provides a discussion of why context specificity is essential to correctly interpret multi-element geochemical data. Copyright © 2017 John Wiley & Sons, Ltd. [ABSTRACT FROM AUTHOR]

A new paleoecology record from the El Palmar Cival adds to the emerging geoarchaeological record of El Zotz, Guatemala. El Palmar's 3 m stratigraphic record began in the Archaic period before 1500 B.C. at or just before initial Maya impacts. From the lowest level, Late Archaic organic deposition, with evidence for diverse tropical forest and a steady water table, transitioned to Early Preclassic clay deposition, decreased forest taxa, three known food taxa, and more economic species. Clay deposition continued through the Preclassic, with occasional organic and high charcoal deposition, increasing maize, and other possible economic pollen. Classic El Palmar saw a new land use type with continued disturbance evidence but diverse and greater forest cover. Human impacts continued, leaving high amounts of disturbance taxa, charcoal, and the highest maize pollen level, concomitant with lower deposition rates, δ13C evidence of increased, diverse tropical forest taxa and organic sediments. El Zotz Aguada's Early Classic to Postclassic sediment record overlaps this, with maize and squash pollen evidence changing to Classic period copal tree pollen dominance. Both records indicate the maximum quantity of C4 taxa derived organic matter was about 40%, leaving at least half from C3 taxa such as tropical forest species. [ABSTRACT FROM AUTHOR]

The Late Pleistocene/Holocene Tiber delta succession represents the most recent and one of the best preserved, high-frequency/low-rank depositional sequences developed along the Latium continental margin of the Italian peninsula. Several previous studies have established a robust data set from which it has been possible to describe the stratigraphic architecture of the entire Tiber depositional sequence from the landward to seaward sectors and over a distance of 60 km. The Tiber depositional sequence shows many characteristics found in other Late Pleistocene to Holocene deltaic and coastal successions of the Mediterranean area. The stratigraphic architecture of the Tiber depositional sequence is controlled mainly by glacioeustasy, although factors such as tectonic uplift, volcanism and subsidence, exert an influence at a local scale. The resulting depositional model allowed discussion of some important points such as: (1) the genesis of the Tiber mixed bedrock-alluvial valley, extending from the coastal plain to the innermost portion of the shelf, recording (i) multiple episodes of incision during relative sea-level fall, and (ii) a downstream increase of depth and width of the valley during the base-level fall and the subsequent base-level rise; (2) the different physical expression of the Tiber depositional sequence boundary from landward to seaward, and its diachronous and composite character; (3) the maximum depth reached by the Tiber early lowstand delta at the end of the sea-level fall is estimated at ca 90 m below the present sea-level and not at 120 m as suggested by previous works; (4) the backward position of the Tiber late lowstand delta relative to the deposit of early lowstand; (5) the change of the channel pattern and of the stacking pattern of fluvial deposits within the Lowstand Systems Tract, Transgressive Systems Tract and Highstand Systems Tract. All of these features indicate that the Late Pleistocene/Holocene Tiber delta succession, even if deposited in a short period of time from a geological point of view, represents the result of the close interaction among many autogenic and allogenic factors. However, global eustatic variations and sediment supply under the control of climatic changes can be considered the main factors responsible for the stratigraphic architecture of this sedimentary succession, which has been heavily modified by human activity only in the last 3000 years. [ABSTRACT FROM AUTHOR]

Shellmound formation processes are greatly influenced by human inputs associated with an intensive exploitation of marine and estuarine resources. The complex stratigraphy of shellmounds has been difficult to decipher and few studies have focused on the microstratigraphic record of midden formation, especially in European Mesolithic contexts. Cabeço da Amoreira is a long-known Mesolithic shellmound located on the shores of the Muge River, a tributary of the Tagus River in central Portugal. The abundance of shellfish refuse favors an intricate and laterally variable stratigraphic succession of layers and lenses, which results in an extensive artificial mound. Here, we use micromorphological and microfacies analysis to investigate aspects pertaining to site formation, and the nature of individual anthropogenic activities at the site. This methodology allowed for a distinction between primary activities (e.g., discrete shell tossing events, trampled occupational surfaces, and activity areas), and secondary position of the sediments in intentionally raked-up and dumped deposits. Nondepositional hiatuses and discrete geogenic sedimentation are associated with periods of abandonment. The complex superposition of events seen at Cabeço da Amoreira underlines the role of micromorphology for the identification of behavioral signatures and its relevance in deciphering shellmound adaptations. [ABSTRACT FROM AUTHOR]

The Fanta Stream site is an archaeological and paleontological locality in Addis Ababa, Ethiopia. The site contains a rich assemblage of fossil mammals and Acheulean artifacts of approximately 600 ka located in a rare high-altitude context. A ground-penetrating radar (GPR) survey was conducted in order to provide three-dimensional imaging of the subsurface, which the authors use to interpret the geometry and distribution of fossil-containing stratigraphic units. Utilizing the stream's natural cut bank exposure, we calibrate GPR data to known geologic units through radar facies analysis. Shallow, high-amplitude coherent reflection geometries are attributed to volcanic tuff deposits, as these units exhibit subparallel continuous reflections consistent with planar stratified sedimentary deposition. Deeper, discontinuous reflection packages are interpreted as conglomeritic, fossil-containing deposits. The results of the GPR survey outline the location of the Fanta Stream's paleodepositional features as well as suggest the extent of fossiliferous stratigraphic units for use in future excavations. [ABSTRACT FROM AUTHOR]

This paper presents the results of analyses carried out on the paintings on the rock-hewn walls of the Forty Martyrs church at Şahinefendi in Cappadocia (a UNESCO World Heritage Site), a central region of Turkey, performed during conservation work from 2007 to 2012. The micro-samples were investigated by spectroscopic, micro-stratigraphic and scanning electron microscopy analysis in order to study the painting technique, the materials and the degradation products. The micro-stratigraphic analysis showed a white, sometimes pinkish, plaster. Micro-Raman analysis, performed on cross-sections of the mortars, enabled the detection of calcite, gypsum, anhydrite and calcium oxalate. Scanning electron microscopy and energy-dispersive spectroscopy revealed a similar composition among all investigated phases, aside from minor differences such as the presence of diatoms in the second and third phases and of biotite, lime lumps and plants fragments in the fourth one. Apart from traditional pigments of medieval wall paintings, micro-Raman analysis revealed the presence of lead-based compounds and jarosite. [ABSTRACT FROM AUTHOR]

In 2011, an engraved limestone block was found in the cave of Arlanpe ( Lemoa, northern Iberian Peninsula). One of the figures represented on it was identified as a schematic feminine representation similar to those of the Gönnersdorf- Lalinde style. The stratigraphical position of the block is not totally clear owing to severe disturbance in the Upper Pleistocene deposits located near the entrance sector of the cave. Nevertheless, the most probable stratigraphical correlation is with Level I, which has been dated to the beginning of the Middle Magdalenian. This finding extends the distribution range of this kind of representation to the northern Iberian Peninsula, where, up to now, only two other, less clear, Gönnersdorf- Lalinde style representations have been found. It also extends its chronological range, pushing it back to the beginning of the Middle Magdalenian. In this paper, we present the archaeological context of the engraved block, followed by a detailed description of technological and stylistic features. These data will be used to discuss the implication of this discovery for an understanding of the origins, expansion and diffusion of this kind of feminine representation across Europe. [ABSTRACT FROM AUTHOR]

ABSTRACT It is widely accepted that most larger Australian vertebrates were extinct by 40 ka. The reliability of <20-ka radiocarbon (14C) ages on charcoal stratigraphically associated with sthenurine (short-faced) kangaroo tooth fragments from Seton Rockshelter, Kangaroo Island, have therefore proven contentious. Some researchers have argued these fossils were in situ, while others have claimed they were reworked. To address this we obtained new 14C ages on bones from the site. These bone ages are not only consistent with earlier charcoal ages, but are in near-perfect stratigraphic order, providing strong support for the site's stratigraphic integrity. Our analyses indicate units aged 21−17 ka were primarily accumulated by Tasmanian devils ( Sarcophilus harrisii) and owls ( Tyto species), after which humans became the primary accumulation agent. The tight chronology, faunal trends and current lack of evidence for older layers from which specimens could have been reworked suggest the sthenurine remains may be in situ. However, because attempts to directly date sthenurine material failed, we cannot confidently assert that they survived to this time. Therefore, Seton Rockshelter may be best excluded from the Pleistocene extinction debate until the site can be re-excavated and more conclusive evidence collected, including more complete or directly datable sthenurine remains. Copyright © 2015 John Wiley & Sons, Ltd. [ABSTRACT FROM AUTHOR]

This paper presents the results of the analysis carried out on a polychrome wood mask from Papua New Guinea during conservation work at Pigorini Museum's restoration laboratory. The significance of this study is that no prior work has characterized the painting materials of Papua New Guinea masks both with spectroscopic and internal microstratigraphic analysis. In fact, these objects were studied especially from an anthropological or conservative point of view and the wood was wrongly defined by its visual appearance. Microstratigraphic and spectroscopic investigations discovered a refined execution technique that up to now has not been demonstrated. The stratigraphy of the painted layers demonstrates a deep knowledge of the materials and of the application techniques on the part of the Papua New Guinea people, together with the ability to foresee the aesthetic result for the artefact. The analysis of the constitutive materials and of the stylistic features supplied valid results in favour of provenance of the mask from Papua New Guinea. [ABSTRACT FROM AUTHOR]

The concept of cultural evolution in the Acheulean is linked to a number of important anatomical, phylogenetic, adaptive, cultural and cognitive research questions. Yet there are very few studies which are able to demonstrate advancements in material culture (technological and/or conceptual) supported by large bodies of empirical data. Derek Roe's work at Olduvai Gorge is one of the few exceptions and here, in my opinion, raw material considerations affect the evidence of increasing diachronic sophistication (Leakey and Roe 1994). Otherwise, evidence for such material culture evolution is largely anecdotal. This study takes large bodies of handaxe data from South Africa and Britain, and using dated assemblages, wherever possible, explores the idea of hominins paying increasing attention to shape and morphological regularity (not symmetry) over time. The results give no reason to believe such a diachronic trend exists. These data are set against the latest research in chronostratigraphic studies and hominin taxonomy. [ABSTRACT FROM AUTHOR]

After the severest mass extinction event in the Phanerozoic, biotic recovery from the extinction at the Permian-Triassic boundary required approximately 5 my, which covers the entire Early Triassic. It is important to obtain information on the superocean Panthalassa, which occupied most of the world ocean, to explore paleoenvironmental changes during the Early Triassic at the global scale. In order to establish the continuous lithostratigraphy of pelagic sediments in Panthalassa during the Early Triassic, high-resolution reconstruction of the Lower Triassic pelagic sequence in Japan was conducted for the first time based on detailed field mapping and lithostratigraphic correlation in the Inuyama area, central Japan. The reconstructed Early Triassic sequence is approximately 9.5 m thick, consists of five rock types, and is divided into eight lithological units. For the reconstructed continuous sequence, measurement of carbon isotopic composition of sedimentary organic matter (δ13Corg) was carried out. Stratigraphic variation of the δ13Corg value shows large-amplitude fluctuations between −34.4 and −21.0‰ throughout the sequence. In order to establish a higher resolution age model for the reconstructed Lower Triassic pelagic sequence, we correlated δ13Corg records in the Inuyama area with high-resolution isotopic profiles of carbonate carbon (δ13Ccarb) from shallow-marine carbonate sequences in southern China based on the similarity in general variation patterns with age constraints by radiolarian and conodont biostratigraphy. The result provides a high-resolution time scale for the pelagic sequence of Panthalassa during the Smithian and Spathian. The age model suggests a drastic increase in sedimentation rate during the late Smithian, which should have been caused by the increase in terrigenous input to this site. [ABSTRACT FROM AUTHOR]

In this paper we compare four types of stratigraphic architectures around the continental margins in the South China Sea (SCS) based on a plentiful of seismic profiles. The results indicate that stratigraphic patterns are not only related closely to structure regimes of peripheral of the SCS, but also are restrained by crust structure from continental crust to oceanic crust. In the extensional setting, depositional centres during the syn‐spreading stage are located in the strong extensional area. A wedge‐decrease continental crust represented by the Pearl River Mouth type is characterized by high deposition and subsidence rate during the syn‐rifting and syn‐spreading stages in the distal zone. And in the Zhongjiannan type with a continental ribbon, high deposition and subsidence rate during the syn‐rifting and syn‐spreading stages are present in the proximal zone. However, in the southern and eastern margins with compressional setting, the Liyue and Zengmu microcontinent blocks are separated from the South China with the seafloor spreading of SCS, in which a confined or relative thin syn‐spreading deposits are presence. High deposition and subsidence rate is closely related to the collision or subduction condition during the post‐spreading stage in the Liyue bank type and the Zengmu type, a huge progradational clinoforms are present along the subduction and collision margin. Therefore, this study shows distinct stratigraphic architecture in different continental rifted margins, distinct depositional and subsidence characteristics formed during the process of lithospheric rupture can provide an effective method for the study on the continental marginal sea in the western Pacific. [ABSTRACT FROM AUTHOR]