Petrology and Provenance of Lithic Raw Materials used to knap stone: A Case Study From the Inner Ionian Sea

Η μελέτη εξετάζει τη λιθολογία και την προέλευση των πρώτων υλών των λαξευμένων λίθινων τεχνέργων από προϊστορικές θέσεις στο Μεγανήσι Λευκάδος, τα οποία εντόπισε και περισυνέλλεξε η αρχαιολογική έρευνα επιφανείας στο Εσωτερικό Αρχιπέλαγος του Ιονίου. Η ερευνητική δραστηριότητα εγγράφεται στην ευρύτερη αρχαιολογική έρευνα με το διεπιστημονικό της χαρακτήρα και είχε διπλό στόχο. Στο πεδίο πραγματοποιήθηκε επιτόπια μελέτη της γεωλογίας του νησιού και συλλογή γεωλογικών δειγμάτων και στο εργαστήριο, πραγματοποιήθηκε πετρολογική εργασία χρησιμοποιώντας τις ενόργανες αναλυτικές μεθόδους LM (οπτική μικροσκοπία), XRD (περιθλασιμετρία ακτίνων-X), SEM (ηλεκτρονική μικροσκοπία σάρωσης) και ICP-MS (φασματοσκοπία μάζης με επαγωγικά συζευγμένο πλάσμα). Το μεγαλύτερο ποσοστό των υλικών που χρησιμοποιήθηκαν για την κατασκευή των εργαλείων συνίστανται σε σχεδόν καθαρό SiO2, με μορφή στρωσιγενών ή κονδυλωδών πυριτολίθων ηλικίας κυρίως Μαλμίου-Τουρωνίου και Ηωκαίνου. Οι πυριτόλιθοι συλλέχθηκαν από προϊστορικούς λιθοξόους από τοπικές πηγές πλησίον των αρχαιολογικών θέσεων. Οι πατίνες που εμφανίζουν τα τέχνεργα είναι κυρίως περιοχές ατελούς πυριτικής διαγένεσης εμπλουτισμένες σε ασβεστιτικό υλικό, και δευτερευόντως προϊόν ύστερης αποσάθρωσης και εξαλλοίωσηςThis paper examines the lithology and raw material provenance of knapped stone artifacts recovered from prehistoric sites on Meganisi in the course of the Inner Ionian Sea Archipelago survey. Research was twofold: in the field to map the geology of the island and collect raw material samples, and in the laboratory to conduct a petrological study using LM, XRD, SEM and ICP-MS techniques. The greater part of the materials used to produce stone tools consists of almost pure SiO2, bedded or nodular cherts mainly of Malm–Turonian and Eocene ages. The cherts were collected by prehistoric knappers from local sources. Patinas present on the artifacts are relatively enriched in calcite material of incomplete silica diagenesis and subsequently a product of late weathering and alteration

A geophysical insight of the lithostratigraphic subsurface of Rodafnidia area (Lesbos Isl., Greece)

The study area of Rodafnidia on the island of Lesbos (Greece) is considered of archaeological interest, as Paleolithic stone tools have been recovered through excavation and collected from the ground surface in recent years. Geologically, the area is mostly covered by Quaternary post-alpine deposits and volcanic rocks. This paper presents the application of a local geophysical survey to determine the volume of the upper Quaternary deposits in which the Paleolithic artefacts can be found and the identification of their ignimbrite substrates. For this reason, the geoelectrical method was selected as the most appropriate for determining the lithostratigraphic subsurface layers. More specifically, a grid of twenty-one (21) Vertical Electrical Soundings (VES) along with an Electrical Resistivity Tomography (ERT) was carried out. The interpretation of the results of these surveys, in conjunction with the results of older excavation trenches, revealed that the Quaternary deposits have been investigated at depths ranging from 0.5 up to 28.5 meters. Furthermore, the lithological boundary of these post-alpine deposits and their underlying pyroclastic ignimbrite flow (with resistivity 24.0–58.0 Ohm.m) seem to dip to the north. The volume of the Quaternary layer is proposed as the maximum depth for archaeological investigation with high chances to recover more Paleolithic material

The legal, historical and industrial context of underwater heritage: Introduction

Interactions between commercial and industrial exploitation of the seabed and archaeological and scientific investigation have been at the heart of developments in the understanding of Europe’s submerged landscapes and prehistory since at least the early twentieth century. This introduction considers some of the ways in which that relationship has evolved since that time, including the adoption of international laws under the aegis of United Nations Conventions, the development of close relationships between Dutch fishermen operating beam-trawl fishing nets in the North Sea and a network of private collectors specialising in Pleistocene fossils and artefacts, the imposition of European Union regulations on offshore industrial projects to include monitoring of underwater archaeology and palaeoenvironments and most recently the incorporation of seabed mapping and underwater cultural heritage in the European Union’s 2020 Blue Growth agenda. These developments have played an important role in the growth of knowledge about the underwater cultural heritage notwithstanding the potentially destructive effects of offshore industrial activity. The impact of economic growth and industrial exploitation in the coastal zone, coupled with sea-level rise, is likely to intensify the threats to the underwater cultural heritage in the coming decades, posing new challenges as well as opportunities in the further development of relationships between industrial operators, government agencies and scientific and archaeological researchers