Search

This paper describes the results of the damage diagnosis performed on Ponte Rotto, a Roman bridge on the ancient Appia way located close to the city of Benevento (southern Italy). Despite it can be considered one of the most important remains of this type of monument in Campania region, the bridge was abandoned for centuries, being in a rather poor state of conservation; therefore, an accurate damage diagnosis has been carried out using an interdisciplinary approach, in order to plan conservative, preventive and restoration work for the requalification of this archaeological heritage. Photogrammetric survey and damage diagnosis following the Fitzner's method allowed identifying and quantifying the geomaterials adopted for the construction of the bridge and the weathering forms affecting it. Georeferenced orthoimages permitted the mapping of their areal distribution, the definition of the damage categories, and the estimation of the linear and progressive damage indexes, that revealed a definitely bad conservation state.

The island of Vivara represents today one of the most important sites for the study of the relations between the Mycenaean world and Western Mediterranean cultures of the Bronze Age. This report presents the most significant results acquired through archaeological excavations in the last decade of research: the main housing structures, the corpus of Aegean-Mycenaean ceramics, the study of the topographical characteristics of the settlement, the traces of the ancient prehistoric port preserved under the surface of the sea. Further important results in the fields of petrographic, bioarchaeological, archaeometallurgical and three-dimensional surveys carried out with scanlaser, stereophotogrammetry and aerofotogrammetry are added.

The Tomb of the Diver has been subject for many decades of fierce debate among archaeologists and classicists. Since its discovery in 1968, some scholars have considered it a unique example of the lost tradition of Greek painting, others have emphasized Etruscan or Italic parallels. More recently, a possible local production has been suggested. With the aim of trying to solve the archaeological question, an archaeometric comparison among this well-known artwork and several frescoed tombs coming from Hellenistic and Lucan necropolis was carried out. The multi-analytical study was focused on the identification of peculiar features of executive techniques and raw materials since the first period of the archaeological site. The analytical investigation has been preliminary based on a non-destructive approach, performed in-situ by portable equipment including imaging diagnostics and compositional spectroscopic techniques for identifying pigments and the conservation state of original painted surface; subsequently, a further deepening by using destructive techniques was performed in-lab for the mortar-based supports characterization. Archaeometric study suggested that technological choices slightly changed in a time span of about two centuries, highlighting important markers that allow clustering the contemporary artistic productions. Moreover, a comparison with mortars from temples decorations was provided to better understand the whole artistic context. The archaeometric data showed that the Tomb of the Diver could be traced back to a local artisanal tradition and therefore is neither Etruscan nor Greek, but the first and foremost an expression of the local elite culture of Paestum.

Protohistoric metal objects coming from the archaeological sites of Pontecagnano (Salerno, Italy) and Striano (Naples, Italy), preserved in the Pontecagnano National Archaeological Museum and the Paleontological Museum of Naples University “Federico II” have been studied by means of an archaeometric approach. A multi-analytical procedure including X-ray powder diffraction (XRPD), scanning electron microscopy and energy dispersive X-ray spectroscopy (SEM-EDS), micro X-ray fluorescence (µ-XRF) and lead isotope ratio mass spectrometry (LIRMS), was used to characterize these objects thus providing hypotheses on the possible provenance of metallic raw materials. The investigated samples are represented by lead, silver, copper and tin bronze-based objects. Corrosion processes affecting the bronze objects were recognized as well as crusts and patinae at different stages of evolution. LIRMS analyses suggested that most of Pontecagnano artifacts were manufactured with metals from southern Tuscany, where important metal reserves were located. On the other hand, due to the limited number of samples, the provenance of the Striano objects cannot be unambiguously identified although data so far available suggest a Sardinian source.

Thirty artefacts from the Archaeological Park of Paestum were investigated by means of scientific techniques on the occasion of the 2016 exhibition 'Possessione. Trafugamenti e falsi di antichita a Paestum'. The multi-analytic diagnostic campaign was aimed at identifying forgeries. Results provided a deeper understanding of both ancient technology and contemporary forgery techniques.

This paper represents the first result of an active collaboration between the University of Sannio and the San Pio Hospital (Benevento, Italy), started in the 2018, that aims to a detailed mineralogical investigation of urinary stones of patients from Campania region. Herein, selected human bladder stones have been deeply characterized for clinical purposes and environmental biomonitoring, focusing on the importance to evaluate the concentration and distribution of undesired trace elements by means of microscopic techniques in the place of conventional wet chemical analyses. A rare bladder stones with a sea-urchin appearance, known as jackstone calculus, were also investigated (along with bladder stones made of uric acid and brushite) by means a comprehensive analytical approach, including Synchrotron X-ray Diffraction and Simultaneous Thermal Analyses. Main clinical assumptions were inferred according to the morpho-constitutional classification of bladder stones and information about patient’s medical history and lifestyle. In most of the analyzed uroliths, undesired trace elements such as copper, cadmium, lead, chromium, mercury and arsenic have been detected and generally attributable to environmental pollution or contaminated food. Simultaneous occurrence of selenium and mercury should denote a methylmercury detoxification process, probably leading to the formation of a very rare HgSe compound known as tiemannite.

The northern slope of Mt. Vesuvius contains some interesting archaeological sites, including the site discovered in the town of Pollena Trocchia, where the remains, dated to between the 79 and 472 CE eruptions, document the transition from the Roman to late Roman cultural and socioeconomic settings. Profound changes occurred in this time interval, which can be inferred from changes in the ceramic manufacturing processes. Common wares, as the most widespread ceramic class in the archaeological record, are a useful example that illustrates this technological transformation. Seventeen samples of tableware, distinguished into three ceramic classes according to the method of slip application (i.e., Slipped Ware, Painted Ware “a straccio,” and Painted Ware), were analyzed. The results highlight the use of high-CaO clayey raw materials compositionally similar to Apennine clayey deposits. The clay bodies were occasionally tempered with sandy-silt materials composed of volcanic grains with lesser amounts of siliciclastic fragments. Firing temperatures ranged from 800 to 950°C, as suggested by quantitative X-ray powder diffraction and microstructural analyses combined with colorimetric measurements of the ceramic bodies. Micro-Raman analyses performed on slips revealed the use of ochre for decorating the vessels; it was applied in a different way, representing an actual technological change.

The technological performance of a chabazite-rich rock belonging to the Campanian Ignimbrite formation, outcropping in the nearby of San Mango sul Calore (southern Italy), has been evaluated for the sorption and release of ibuprofen sodium salt after a surface modification of the starting geomaterial using two different chlorinated surfactants. Equilibrium sorption isotherms and in vitro loading tests demonstrated that the maximum sorption capacities of this geomaterial reach up to 24.5 and 13.5 mg/g, respectively, for zeolite modified with cetylpyridinium and benzalkonium. These results, obtained by non-linear mathematical modeling of the experimental curves, are definitely compatible with the concentrations of the most common non-steroidal anti-inflammatory drugs (such as ibuprofen) in wastewaters, which have been recently considered as contaminants of emerging concern. This investigation also encourages a new possible sustainable exploitation of the lithified yellow facies of Campanian Ignimbrite, although future developments will be focused on using more stable and eco-friendlier two-tailed surfactants.

The Bobaomby volcanic field (10–11 Ma) is the northernmost volcanic area of Madagascar, and is a monogenetic volcanic field comprising outcrops of lava flows, dykes, scoria cones, tuff rings and plugs, widely scattered over an area of roughly 500 km2. The volcanic rocks range in composition from nephelinite, basanite and tephrite, through tephritic phonolite, to F- and Cl-rich peralkaline phonolite (MgO from 13 to 0.01 wt%), and the serial affinity varies from sodic to potassic. A few mica-amphibole-rich lamprophyric dykes have tephritic composition and ultrapotassic affinity. The mafic lavas host intrusive xenoliths with evident cumulate features (wehrlites, composite olivine gabbros s.l., amphibole clinopyroxenites and “kaersutitites”), as well as various types of mantle-derived xenoliths and xenocrysts in the most primitive rocks. The very wide compositional variations of the observed phases (olivine, clinopyroxene, amphibole, oxides, feldspars, feldspathoids, apatite, titanite, aenigmatite and other accessories) in lavas, dykes and cognate xenoliths are fully consistent with the variable degree of differentiation of the host lavas/dykes, and pointing out to limited open-system or polybaric crystallization. The mafic lavas have marked enrichment in incompatible elements and light rare-earth element (LREE) (e.g., Lan/Ybn = 19–27), whereas concave REE patterns are found in the peralkaline phonolites, as a result of removal of accessory titanite starting from tephritic phonolite magmas. The gabbroic/ultramafic xenoliths are interpreted as crustal cumulates of basanitic and tephritic magmas. Several liquid lines of descent in the basanites and tephrites are evident from the trace-element distribution, and from the differing geochemistry of the evolved rocks. The isotopic compositions reach extreme values (e.g., 206Pb/204Pb = 20.065 in the ultrapotassic lamprophyre) when compared to the rest of the Cenozoic/Recent Madagascan volcanic rocks, but similar to those of the Comoros archipelago, suggesting analogies of mantle sources and enrichment processes in the lithosphere of this volcanic archipelago. The origin of the Bobaomby mafic rocks is compatible from a derivation from low degree partial melting of an incompatible element-enriched peridotite source (possibly located in the lowermost lithospheric mantle) rich in volatile-rich phases (pargasite, locally also phlogopite and possibly carbonates), matching the sources of other Cenozoic volcanic areas throughout Madagascar, and perhaps Comoros.

Excavations at the north-eastern side of the city Cumae (modern Cuma) brought to light the Tomba del Banchetto per l’Eternità, a hypogeum chamber tomb with vaulted ceiling built in tuff blocks dated back to the first decades of the 1st century BCE. The exceptional nature of the discovery, resembling an Oscan tradition, is due to the peculiar decorative scheme, reporting a banquet scene and three funerary beds along with a table, reproducing a sort of triclinium.The investigation performed on decorated plasters, in situ by a spectroscopic approach and in-lab via minero-petrographic techniques, allowed us to infer the production technology of wall paintings and mortar-based support, and the type of pigments used for decorating the tomb.The multi-layered plasters were made with specific mix-designs in the different part of the tomb; similarly, different painting techniques were adopted according to the architectural scheme. In the lower part of the walls, lime cocciopesto mortars adhere on the tuff blocks, likely to lend better hydraulic properties to the mortar-based supports in humid and wet environments. This part of the tomb, as well as the funerary beds, was painted in red using the fresco technique. On the other hand, in the upper part of walls and on the vault, the arriccio layer, containing volcanic sand, was covered with a thick and white intonachino layer composed of lime binder, constituting the support for the pictorial layer, applied with a mezzo fresco technique.The investigation on pigments used for wall paintings points out to the use of a characteristic Roman palette, consisting of pure, natural and synthetic pigments (calcite, red and yellow ochre, hematite, organic black pigments, Egyptian blue), and skilful mixtures of colouring materials (mixture of yellow ochre and organic carbon black for the brown, mixture of kaolinite-rich clay, Egyptian blue, and Fe-oxides for grey and mixture of organic –madder- and inorganic pigments for pink).Geographical Coordinates: 40°51’3.13’’N; 14°3’27.33’’E

Porcelain stone used at the early kilns of Arita, Japan, has never been identified due to the lack of written records. Ryumon and Shirakawa deposits are considered to have possibly been exploited before Izumiyama was discovered in the early 1630s, but there are no records or any previous scientific research aimed at resolving such crucial issue. This work presents the first systematic scientific study of clays from the three deposits and shards excavated at early kiln sites. Portable ED-XRF and SEM-EDS were used to identify the chemical compositions of bodies, glazes, and geochemical characteristics of clays. XRD, TG-DSC, and FTIR-ATR spectroscopy were also used for the mineralogical characterization of clay bodies. Results show that the earliest production was marked by the mineralogical characteristics of the available raw materials. A gradual improvement in material selection and processing will lead to the development of the nigoshide (milky-white) body in the mid-17th century.

The important discoveries at the recent archaeological excavations at Punta d'Alaca site in the west side of the Vivara island (Campania region) highlighted the presence of a Bronze Age thriving settlement attesting the development of a flourishing ceramic production, mainly specialized in the manufacturing of common wares. The archaeometric study performed on twenty representative samples by means of chemical and minero-petrographic techniques revealed that pottery was produced in-situ; however, locally-manufactured vessels here coexisted with imported ones. Coarse-textured, local potteries were made by low-CaO clays mixed with volcanic temper consistent with the volcanic products of Campanian volcanoes. The firing (likely a pit firing) was done in rough conditions, as proved by mineralogical evidence that suggest variable firing temperatures. In fact, low firing temperatures (

The history of brick manufacturing in Madagascar dates back to the early 1800 s when European colonisers imparted to the local population the basic knowledge for firing clayey sediment to obtain a more durable construction material. The evaluation of the entire production cycle accounting for the involved natural resources such as raw materials, fuels and derived bricks, represents the aim of this research started in 2015 and focused on both rural and urban contexts. Clayey raw materials from lateritic soils widely occur in central Madagascar whereas, in southern coastal sites, carbonate-bearing clays definitely prevail since their composition are influenced by the reef. Bricks are prepared on site with no additional manipulation of the base clay and, depending on the climatic conditions, the bricks are dried and fired from one week up to ten days. Furnaces are powered by rice husk in south-western part of the island whereas in central Madagascar the use of peat and wood was also recorded. The calorific performances of these common fuels allow achieving temperatures of 800–900 °C; however, the huge loss of heat due to the poor quality of the furnaces determine low equivalent firing temperatures (EFT) that negatively affect the quality of the bricks. The above described ceramic process has remained unchanged for more than 200 years and even if new social and economic opportunities arose, this unvirtuous system slowly (but inexorably) contributed to the impoverishment of important energy sources and, above all, of natural resources.

This research has focused on the assessment of the compositional features and mechanical and antifouling performances of two different mortars formulated for an underwater setting, and which contain Mg(OH)2 as an antifouling agent. Regarding the mechanical characterization, the uniaxial compressive strength and flexural strength were measured. The composition of the materials was explored by differential thermal/thermogravimetric analysis (DTA-TG), X-ray diffraction analysis (XRPD), and scanning electronic microscopy (SEM) coupled with EDS microanalysis. The assessment of the biological colonization was evaluated with colorimetric analysis and image analysis. The results suggest that both mortars have good mechanical resistance once set underwater. Moreover, the adding of Mg(OH)2 improves the resistance toward biofouling; this was observed both in laboratory and sea-exposed specimens.

Ceramic building materials (CBM) are interesting archaeological items for gathering the material culture identity and urban setting of the ancient populations since their production is generally related to the local availability of clayey raw materials and advancements of technological skills of ancient makers. This paper investigates the Hellenistic and Roman productions of ceramic building materials from the archaeological site of Témesa on the Tyrrhenian coastline of Calabria region (southern Italy), a settlement where a flourishing ceramic tradition has been attested for all of its occupation phases, from the late Archaic to the Roman period. Here, the local availability of clayey and sandy raw materials permitted the development of a thriving worksite. A combined study of mineralogical, petrographic and micropaleontological features of archaeological samples and geological raw materials collected nearby the archaeological settlement, permitted to constrain the raw materials sources, and investigate the technological level achieved between the second half of the 4th century BCE and the 3rd century CE. This study highlighted that most of CBM was made by mixing sands from a nearby fluvial deposit with upper Miocene clayey raw materials. Chemical composition and micropaleontological investigation of the foraminiferal content of archaeological samples and clays validated the possible exploitation of local raw materials. Textural parameters and the mineralogical assemblage of temper grains, characterized by the peculiar presence of metamorphic lithics, also attested the use of Savuto river sands. Ceramic technology accounts for a firing process at reasonably high temperatures, evidencing the good technological level of production. Moreover, the presence of samples characterized by mix-designs and mineralogical assemblages consistent with geological materials from Campania region witnesses the importation of ceramic materials from other sites, suggesting the existence of operating trades as already attested for other sites of Tyrrhenian coast.

High-precision 40 Ar/ 39 Ar ages, major and trace element, and radiogenic isotope data are presented for the basanites and alkali basalts forming the southwesternmost monogenetic volcanic field in Madagascar. The volcanic rocks were erupted along fissure zones and aligned cones in a nearly flat area covered by the Cenozoic sediments of the Morondava basin. The high-precision 40 Ar/ 39 Ar ages constrain the beginning of the magmatism in the Ankililoaka area to about 12 Ma, significantly earlier than suggested by previously published K/Ar ages. The Ankililoaka basanites include primitive compositions (MgO >10 wt%, Ni >200 ppm and Cr >400 ppm), whereas other basanites and alkali basalts experienced limited removal of olivine, chromiferous spinel and clinopyroxene. Initial Sr and Nd isotope ratios of the basanites are 0.70343–0.70445 and 0.51279–0.51282, respectively. The Pb isotope compositions are in the ranges 206 Pb/ 204 Pb = 19.08–19.38, 207 Pb/ 204 Pb = 15.61–15.64 and 208 Pb/ 204 Pb = 39.1–39.4. The alkali basalts have similar 87 Sr/ 86 Sr, 143 Nd/ 144 Nd and 207 Pb/ 204 Pb, but slightly lower 206 Pb/ 204 Pb and 208 Pb/ 204 Pb than the basanites. The isotopic composition of the Ankililoaka rocks partially overlaps with that of the Cenozoic volcanic mafic rocks of northern Madagascar, and differs significantly from that of the mafic volcanic rocks of central Madagascar, which have lower 206 Pb/ 204 Pb and 207 Pb/ 204 Pb, and higher 87 Sr/ 86 Sr. Major and trace element systematics and geochemical modelling suggest that the Ankililoaka mafic alkaline rocks are low-degree melts of an incompatible element enriched peridotite source starting from depths where garnet is stable. Crustal contamination during ascent was insignificant. We argue that the genesis of the Ankililoaka alkaline magmas was triggered by melting an enriched, volatile-rich lithospheric mantle uplifted in the Cenozoic. Supplementary material: Analytical techniques, X-ray fluorescence whole-rock data, mineral compositions, 40 Ar/ 39 Ar dataset, mantle source modelling and figures showing volcanological features and thin sections are available at https://doi.org/10.6084/m9.figshare.c.4065743

The present research deals with the evaluation of a clinoptilolite-rich rock, occurring in the Nižný Hrabovec deposit (Slovakia), for high-value technological applications based on sorption and in vitro release of nonsteroidal anti-inflammatory drugs (i.e., ibuprofen sodium salt). This georesource was surface modified (SMNZ) using four cationic surfactants. Results demonstrate that ibuprofen sorption is very fast and SMZNs can sorb up to ˜26 mg/g of drug as a function of the type of counterion and morphology of surfactant, as well as the hydrophobicity and molecular structure of the drug. Maximum sorption capacities observed for all SMNZs are fully comparable to other adsorbent carriers usually used for removal of contaminants in wastewaters. Sorption of ibuprofen is controlled by a dual mechanism: external anionic exchange and partition into the hydrophobic portion of the patchy bilayer. A prompt drug release in simulated intestinal fluid (SIF) was also observed, making this natural material also suitable to provide rapid soothing effects in potential pharmacological applications. Comparing the results of this study with other recent investigations, a good technological performance of clinoptilolite-rich rock can be inferred despite the relatively low zeolite content (˜56 wt.%).

A stratigraphic analysis applied to the architectural remains of the medieval domus Apicii (Calvi, Benevento) allowed to define four main building periods characterized by different materials and masonry techniques. Intense biological colonization and other damage pathologies affect the building geomaterials. A quantitative evaluation of the conservation state of the monument accounts for a moderate to a very severe damage, with a progressive damage index (DIprog) up to 3.3 value. The results of this multidisciplinary investigation represent an important starting point for an ethically acceptable making-decision process within a modern restoration and conservation of the monument.

The use of vibrational spectroscopy is gaining more and more relevance in the field of the identification and characterization of Cultural Heritage materials. In this frame we propose and discuss a copious collection of Fourier Transform Infrared (FTIR) spectra acquired in external reflectance (ER) mode (4000–400 cm−1), which is a non-destructive and inexpensive analytical technique. Up to 192 spectra were collected, processed and made free-available to the scientists and professionals working in the Cultural Heritage sector. Color and inclusions, optical anisotropy, polymorphism and isomorphism, water content, crystallinity index, polyphasicity are some properties that have driven to rationale of the paper for discriminating groups of geomaterials usually found in studies aimed at the valorization and conservation of Cultural Heritage. Finally, this study offers a robust opportunity to beginners who intend to use ERFTIR as a tool in the field of qualitative and non-destructive mineralogical analysis.

Since 1960s, mortars have been exploited as a potential material for radiocarbon dating and, despite the fact that this methodology appears very simple in its principles, some measured radiocarbon ages were definitely different from the expected historic ages. The paper concerns to the characterisation of mortars from three Andalusian castles (Spain) by means of different mineralogical techniques in order to control “contamination effect” that could affect age estimation. Several mixtures of binders and aggregates composed the archaeological mortars; lime-based or gypsum-based binders were distinguished whereas the aggregates varied from carbonates to intrusive igneous rocks. The radiocarbon dating provided good results for lime-based mortars with silicate aggregate; conversely, for other specimens the method for sample preparation (Cryo2SoniC) was improved increasing the ultrasonic time and decreasing the mesh size. The research points out the importance of a multi-analytical approach aimed at improving a widely accepted protocol for 14C dating of archaeological mortars.

International audience

This paper focuses on the application of external reflection Fourier Transform Infrared spectroscopy for the classification of some minerals commonly used as gemstones and mineral collection: quartz (colourless, tourmalinated and smoky varieties), calcite and aragonite. The results highlight the differences between reflectance and absorbance spectra, allowing a faster, cheaper and non-destructive approach for the identification of monocrystalline minerals.

An interdisciplinary study, involving geologists, chemists and pedologists, started aiming at identifying a "Geo-Pedo-Fingerprint" (GPF) univocally linking the wine to its origin, namely, the Piedirosso vineyards growing in the Campi Flegrei volcanic area. The focal point of this research was the characterization of the whole parent material-soil-vineyard-wine system, achieved by correlating the elemental pattern - with special reference to micro-nutrients and Rare Earth Elements (REEs) - and Sr isotopic ratios, to identify a reliable and convenient 'GPF', as a guaranteed indicator of wine provenance. A representative soil/Piedirosso vineyard system was identified and characterized. Samples from each soil horizon as well as from vine branches, leaves, grapes and wine were collected and analyzed. All samples were analyzed by multi-collector inductively coupled mass spectrometry (MC-ICPMS) to determine their 87Sr/86Sr isotopic composition, by ICP-Quadrupole MS to measure multi-elemental composition including REE, and by X-Ray Powder Diffraction (XRPD) for the quantitative evaluation of the mineral phases occurring in soil samples.Statistical analysis (Hierarchical Cluster Analysis, Factor Analysis) revealed the existence of separate correlations of element distribution between: i) soil, as nutrient pool source, and vegetative compartments, i.e. branches and leaves, as biochemical yards for nutrient elaboration and marshaling, ii) vegetative compartments and the productive compartment, i.e. grapes as the metabolic outcome of the vine, and, iii) the productive compartment and its artifact produced by man, i.e. wine. However, no sequential correlation of elements from soil to wine did appear, likely because clusters of elements were discriminated due to the varying takeup and fractionation processes in plants, as well as during vinification processes. Therefore, none of the investigated elements was a liable 'GPF' as a candidate tracer from soil to wine.In contrast, the use of a petrogenetic tracer such as 87Sr/86Sr isotopic composition provided satisfactory responses. In fact, the values of such a ratio within the entire studied chain vary in a very small range from 0.7076 to 0.7084, thus falling within the typical range for volcanites of Campi Flegrei (0.7065-0.7086). These results currently represent the only study focusing on a geotracer, such as the 87Sr/86Sr isotopic ratio, linked with a pedological survey to identify the volcanic Campanian wine-producing chains from soil parent material-to-wine. © 2013 Elsevier B.V.

The Via Lepanto site is one of the best examples showing how the Vesuvian region was partially reconstructed and earlier re-occupied after Vesuvius's eruption in the year 79 AD. The large amount of ceramic finds illustrates the typology in use in this area during the IV and V century AD. Analyses were focused on table and cooking ware productions. Archaeometric data were obtained using chemical and minero-petrographical methods (OM, XRD, XRF and SEM). Grain size measurements using Image Analyses on thin sections and a geochemical comparison with clayey deposits outcropping in the Campania region permitted the identification of the raw materials used for these pottery productions. XRD and SEM completed the data set, establishing the protocols used for pottery production in the Pompeii area during Late Roman period. The Via Lepanto site was part of an exchange network of markets with a periodic frequency, where locally produced and imported pottery was sold, indicating a flourishing network of exchanges spanning short, medium and long distances.

Industrial minerals, particularly bentonites, have long been used in treatments to improve the stability and shelf life of white wines. We evaluated a new combination of rocks and minerals, including steam-treated bentonites and natural zeolites (chabazite and phillipsite), to greatly reduce the risk of protein and tartaric instability of wines. Detailed mineralogical, chemical and electrokinetic studies of these materials were conducted using powder X-ray diffraction (PXRD), X-ray fluorescence (XRF), microporosimetry, BET surface-area analysis and zeta-potential measurements. Several model wine solutions containing Bovine Serum Albumin (BSA) were prepared to evaluate the oenological performance of the rock/mineral combinations. UV-VIS spectrophotometry and ion chromatography were used to evaluate the degree of wine stabilization from the protein and tartaric point of view.The experimental results showed that steam treatment modifies both the microporosity and external surface area of the bentonite. These changes in surface area, along with creation of hydrophobic surfaces, significantly modified the behaviour of the steam-treated bentonites, requiring an increase in the amount of material necessary to bring the protein content to required levels. An important benefit derived from the use of steam-treated bentonites is that the pre-mixing with water before addition to wine is not necessary, as the material is readily dispersed. Finally, the addition of natural zeolites effectively decreased the potassium content, thereby improving the tartaric stability of white wines. In addition, this procedure results in minimal waste, as the bentonite-zeolite mixture can be reused as soil amendments in agriculture.

Domus of Octavius Quartio occupies the entire insula 2 of Region II in Pompeii, representing one of the most important village of this archaeological site. An interdisciplinary approach has been adopted in order to plan conservative, preventive and restoration actions aimed at the requalification of Pompeii within the frame of "Grande Progetto Pompei" program. 3D Laser scanner surveys and damage diagnosis following Fitzner's method were carried out. The identification and description of weathering forms was carried out using ICOMOS-ISCS and NorMaL 1/88 recommendations, readapted and reinterpreted also for frescoes. Ten different weathering forms were identified; the frescoed room and the fountain are mainly affected by fissures, convex deformations, lacuna, efflorescence, discoloration, moist areas and patinas; the surrounding wall shows back weathering due to the disaggregation of bedding mortars; moreover the blocks are interested by rounding and biological colonization (lichens). Mapping the areal distribution of weathering forms and defining the damage categories, allowed an estimation of the linear and progressive damage index. Actually, a good conservation state of frescoed room (1.5 - 2.0) and fountain (0.7 - 1.2) was identified; a definitely worse conservation state, instead, was observed in the external wall, where the highest progressive damage index value (3) was measured.

Detailed stratigraphical, archaeological, micropalaeontological, archaeometrical and petrochemical analyses of samples from trenches and boreholes at insula of Casti Amanti, in Pompeii, allowed a faithful reconstruction of the recent environmental evolution of the site. The present data clearly indicate the alternation of both subaerial and shallow marine conditions during Holocene times. Taking into account the relative local sea level variations, a similar to 30 m ground uplift event in the last 6 kyr (with an average vertical uplift rate of similar to 5 mm/yr) was inferred for the first time.

Bulk-rock and mineralogical characterization of massive samples (lava flows, lava domes, scoria, spatter), chosen to be representative of different activity periods and of the whole known compositional range of Ischia island (Roman Magmatic Province, Campanian district) is reported in this paper. The rocks vary in composition from shoshonites to peralkaline trachyphonolites. Crystallization started with Al-rich chromite inclusions and their host magnesian olivine in shoshonites and latites, and ended with lavenite, rinkite, kochite, hiortdahlite, hainite, Mn-aenigmatite, britholite and Ti–Zr-rich aegirine in the groundmass of the peralkaline trachyphonolites. Removal of feldspar-bearing assemblages (with calcic-to-sodic plagioclase in shoshonites and latites, sodic sanidine and anorthoclase in trachytes and trachyphonolites) is established throughout the compositional range, and is accompanied by interaction between variably evolved magmas (with their differing phenocryst assemblage), mostly in mafic and intermediate compositions. This led to enrichment in Mn, alkalis, Zr, Nb, REE, Rb, Th, U, Cl and F, and depletion in Mg, Fe, V, Ca, Ba, Sr and Eu in the most evolved magmas. The Ischian rocks have a tendency to sodic affinity and by peculiar mineral compositions and compositional trends, which do not indicate extremely oxidizing conditions. The Ischian rocks thus differ from the Phlegrean Fields analogues and the ultrapotassic, more silica undersaturated rocks of Somma–Vesuvius. Overall, variations in the chemical compositions of the rocks and their trends imply unrelated feeding systems and thus are inconsistent with the hypothesis of a common magma reservoir beneath the main volcanic areas of the Campanian Plain.

Late Cretaceous dykes and lavas from central-eastern coastal Madagascar (Vatomandry and Mahatsara districts) span a compositional range from basalt to rhyolite. The dykes strike N–S, parallel to the coast, and intrude the Precambrian schists and gneisses of the area. 40Ar/39Ar age determinations on rhyolite from Sakanila massif (western Vatomandry) gave an age of 86.4 ± 0.3 Ma, which is statistically equivalent to the mean age of eastern rifted-margin rocks of Madagascar. Basaltic dykes are generally tholeiitic varying from olivine-normative to quartz-normative, and characterized by relatively low MgO (4.8–8.0 wt%), Cr (61–341 ppm) and Ni (36–128 ppm) contents. The mantle-normalized diagrams have bell-shaped patterns, with the most Mg-rich dykes having

International audience; Samples of table and cooking ware, dating back to the Byzantine period of the ancient Greek colony of Cuma, were analysed by optical microscopy, X-ray diffraction, X-ray fluorescence and scanning electron microscopy, in order to reconstruct the main technological properties of these manufactures. The comparison of minero-petrographical data from these samples with those of some kiln wastes allowed us to hypothesize a local manufacture for most of the investigated specimens and to confirm the relative reference groups. A restricted number of samples did not link with the main groups, indicating a regional (or maybe extra-regional) production, in agreement with the widespread circulation of this high-medieval ceramic production in southern Italy.

Gli scavi effettuati a Cuma dai ricercatori del Centre Jean Bérard hanno riportato alla luce una grande quantità di reperti ceramici. Il presente studio è stato concentrato su ceramiche comuni da cucina e su di un particolare tipo di ceramica da cucina a vernice rossa interna, denominato Rosso Pompeiano. Tutti i frammenti sono costituiti da degrassante vulcanico: feldspato, clinopirosseno, scorie, pomici, litici e, in minor quantità biotite, anfibolo, granato e scorie a leucite. Dal punto di vista chimico i campioni analizzati si suddividono in due gruppi principali costituiti indifferentemente da campioni di entrambe le tipologie. La distinzione fra i due raggruppamenti è dovuta alla differente quantità di inclusi presente nei frammenti, come messo in evidenza dall’analisi modale. I dati XRD e SEM indicano che la maggioranza dei campioni fu sottoposta a temperature di cottura in un intervallo compreso fra 900 e 1000°C. Fanno eccezione alcuni campioni di un gruppo di ceramica a vernice rossa interna per i quali sono ipotizzate temperature inferiori, comprese fra 800 e 850°C.

The Gran Potenza clay and the Pomici di Avellino pyroclastics, respectively the clay sediments and temper of the typical ceramic manufacture in Benevento area (Italy). were mixed in different proportion and fired at 850 degrees, 900 degrees and 950 degrees C. These experimental replicas were compared with historical ceramic products of Benevento. The similarities and/or differences between archaeological materials and replicas (in terms of amount of temper, firing temperature, pore system, etc.) have been discussed. The whole data confirm the wide utilization of the local available clayey raw material and the Pomici di Avellino, and give a new contribution on the petrophysical modifications of volcanic-rich ceramic pastes that occur in the firing temperature range comprised between 850 degrees and 950 degrees C. Some peculiar features in the historical manufacturing are also reported.

I risultati di scavi recenti mostrano la relativa vitalità dell’area vesuviana dopo la disastrosa eruzione del 79 d.C. In particolare, i materiali ceramici provenienti dallo scavo di via Lepanto possono offrire una esemplificazione dei prodotti circolanti in quest’area tra lo scorcio del IV e gli inizi del V secolo. Essi provengono da una serie di scarichi che almeno in un’area dello scavo risultavano sigillati da un piano di battuto a sua volta coperto dal materiale piroclastico dell’eruzione cd. di «Pollena» (473 d.C.) Sulla base della sigillata chiara D, questi materiali possono essere datati al più tardi ai primi decenni del V secolo. Le analisi archeometriche eseguite su un ampio campione di materiali suggeriscono per larga parte delle ceramiche comuni e da fuoco una produzione locale, pur non mancando prodotti di importazione

The production of glazed ceramics in Italy started in 13th century, following Islamic tradition and techniques. Protomajolica samples from two medieval archaeological sites in Benevento were analyzed from mineralogical and petrographical points of view to identify and characterize the local production of fine glazed wares. Samples are represented by jugs, amphorae, bowls and dishes finely decorated and covered by thin inner and/or outer glazed surfaces. The colour of almost all the investigated sherds varies from creamy to orange even though, from the same archaeological levels, dark grey coloured ceramic fragments likely affected by overburning of the paste (kiln refuses) were collected.Optical microscopy observations, chemical (XRF) and physical (XRD) analyses allowed to reconstruct the steps of the manufacture process, and to identify a homogeneous group of samples likely belonging to a local production area of Protomajolica, a ceramic class widespread over the Central-Southern Italy between the 13th and the 15th century.