Two sediment sections are investigated at Cape Arkhangelos, island of Rhodes, where Pleistocene marine sediments crop out in horsts and grabens of a Mesozoic basement. There, hemipelagic sediments characterized by upper bathyal communities are atypically mixed with much shallower faunal components because they were deposited close to rugged coastal landforms. Biostratigraphic analyses show that the sections were deposited between 1.8 and 0.9 Ma, and between 1.8 and 1.6 Ma, respectively. By combining the planktonic/benthic foraminiferal ratio with 31 bathymetric indicators chosen among extant species of benthic foraminifera, mollusks, and bryozoans, we show that relative sea-level fluctuations can be reconstructed in these atypical settings despite the proximity of steep slopes that favored transportation of allochthonous fauna. The shallow-water components (including gravels and calcareous algae) were transported downslope by the combined action of gravity, currents, and tectonic disturbance that promoted drowning (with a maximum flooding recorded at ca. 1.7 Ma) and then uplift of fault-bounded paleovalleys that formed during the Early Pleistocene. Abrupt facies changes and age differences between sections have been triggered by the irregular paleotopography of the Mesozoic basement, which fostered differential depositional settings, with outer to middle neritic deposits above the horsts and upper bathyal deposits in paleovalleys.

The Çanakkale-Balıkesir Coastline Palaeolithic Survey Project covers the Çanakkale and Balıkesir coastlines of the Aegean. It aims to reveal Palaeolithic assemblages and their connection to the surrounding islands—primarily Lesbos. In 2021, four important findspots were detected on the Çanakkale coastline, and more than 500 lithics were uncovered, exhibiting the characteristics of large cutting tools, as well as pebble and prepared core technologies. These tools attest to the presence of hominins along the Çanakkale coastline during the Lower Palaeolithic.

The discovery of a burial pit at Uğurlu on the Aegean island of Gökçeada, in which bodies were deposited one on top of another, raises questions about whether this apparently careless discarding of the dead was local burial custom or a ceremonial ritual.

Recent archaeological survey on the Greek island of Kythera yielded prehistoric quartz that offers new information on the island's role in early Aegean occupation.

The Early Bronze Age (EBA) is associated with technological and cultural changes that may suggest the onset of a new culture. The question usually posed is whether the spread of the EBA culture is a matter of contemporary evolutionary practices or a matter of migration of peoples. We contribute to this discussion by tracing the appearance and spread of the EBA in the Aegean using an absolute time-frame provided by more than 200 radiocarbon (14C) dates from 25 different Aegean sites. These have been compiled and statistically treated, individually, and in geographical groups to allow temporal and spatial comparisons. A new model is constructed for the first time for northern Greece. The dates are compared between various settlements and areas in each of the traditional cultural divisions EBA I, EBA II, and EBA III and possible subdivisions. The statistical treatment and comparisons indicate that the EBA appeared slightly earlier, around 3300 BC, in northern Greece than in southern Greece, and the Cycladic Islands and also lasted longer in some areas in northern Greece, ending at around 1900 BC.

The development of an advanced stone-working technology in the Aegean Bronze Age is suggested by the putative Mycenaean pendulum saw. This device seems to have been used to cut through hard sedimentary rock at a number of sites on the Greek mainland and, according to some scholars, also in central Anatolia. As no pendulum saws are preserved in the archaeological record, understanding the machine relies on preserved tool marks and experimental research. This paper presents the results of stone-cutting experiments conducted with a modern reconstruction of a pendulum saw. The research investigates blade shape, size, design and the mechanics of the device, while questioning the accuracy of earlier reconstructions.

Knossos, on Crete, has long been famous both for its Minoan period remains and for the presence, at the base of the stratigraphy, of an early Neolithic settlement. The chronology and development of the Neolithic settlement, however, have hitherto been unclear. New light is now thrown on this formative period by combining new and older radiocarbon dates with contextual information in a Bayesian modelling framework. The results from Crete and western Anatolia suggest that an earlier, small-scale Aceramic colonisation preceded the later Neolithic reoccupation of Knossos.

Inscriptions on new archaeological finds in the Aegean, examined alongside linguistic evidence relating to Greek and Phrygian vowels, are here used to explore the origins and spread of the Greek alphabet. The ‘invention’ of vowels happened just once, with all of the various Greek, Phrygian and Italic alphabets ultimately deriving from this single moment. The idea spread rapidly, from an absence of writing in the ninth century BC to casual usage, including jokes, by 725 BC. The port of Methone in the northern Aegean emerges as a probable candidate for the site of origin. A place where Greeks and Phoenicians did business together, with international networks; was this where Semitic, Greek and Phrygian letters first coalesced?

Andros is a key island for understanding both the timing of high-pressure–low-temperature (HP-LT) metamorphism and the dynamics of crustal-scale detachment systems exhuming high-grade units in the Cyclades (Greece). Using phengite 40Ar–39Ar geochronology coupled with thermobarometry, as well as data from literature, we constrain the pressure–temperature–time (P-T-t) paths of the Makrotantalon and Attic–Cycladic Blueschist units on Andros. Peak conditions of the HP-LT episode in the Makrotantalon unit are 550°C and 18.5 kbar, dated at 116 Ma. We correlate this episode with Early Cretaceous blueschist facies metamorphism recognized in the Pelagonian zone of continental Greece. This is a new argument favouring a Pelagonian origin for the Makrotantalon unit. In the Attic–Cycladic Blueschist unit, the P-T-t path is characterized by: (1) exhumation after peak conditions in HP-LT conditions between 55 and 35 Ma; (2) isobaric heating at 7 kbar until 30 Ma; and (3) isothermal decompression until 21 Ma. This thermal evolution and timing are similar to those of the neighbouring Tinos Island, emphasizing major thermal re-equilibration at the transition between stable and retreating subduction. Modifications of the crustal thermal state played a major role in the evolution of the North Cycladic Detachment System, below which Andros HP-LT units were exhumed.

The author shows how better recovery techniques have allowed the early history of the Mediterranean olive to be rewritten. Small scale exploitation is detectable in the Neolithic, and is widespread by the Early Bronze Age. Users appear to be first attracted by the olive wood, the fruit benefitting from the pruning effect as the olive bush becomes a tree. This process eventually results in domestication—but this is an unintended consequence of a production process driven by demand. The story now aligns better with the model put forward in Colin Renfrew's thesis of 1972.

The bronze razor with the horse-head handle appeared in Scandinavia in the fifteenth century BC. Where did it come from and what did it mean? The author shows that the razor had some antecedents in the Aegean, although none of these objects were imported to the north. He argues that the Scandinavian warrior class consciously adopted elements of the Mycenaean warrior package, including a clean-shaven face. This vividly exposes new aspects of the busy and subtle nature of international communication in the Bronze Age.

A distinct spatial relationship between surface faulting, magmatic intrusions and volcanic activity exists in the Aegean continental crust. In this paper, we provide detailed structural observations from key onshore areas, as well as compilations of lineament maps and earthquake locations with focal plane solutions from offshore areas to support such a relationship. Although pluton emplacement was associated with low-angle extensional detachments, the NNE- to NE-trending strike-slip faults also played an important role in localizing the Middle Miocene plutonism, providing ready pathways to deeper magma batches, and controlling the late-stage emplacement and deformation of granites in the upper crust. Additionally, the linear arrangements of volcanic centres, from the Quaternary volcanoes along the active South Aegean Volcanic Arc, are controlled primarily by NE-trending faults and secondarily by NW-trending faults. These volcanic features are located at several extensional settings, which are associated with the main NE-trending faults, such as (i) in the extensional steps or relay zones between strike-slip and oblique-normal fault segments, (ii) at the overlap zones between oblique-normal faults associated with an extensional strike-slip duplex and (iii) at the tip zone of a NE-trending divergent dextral strike-slip zone. The NE trend of volcano-tectonic features, such as volcanic cone alignments, concentration of eruptive centres, hydrothermal activity and fractures, indicates the significant role of tectonics in controlling fluid and magma pathways in the Aegean upper crust. Furthermore, microseismicity and focal mechanisms of earthquakes in the area confirm the activity and present kinematics of these NE- trending faults.

The sanctuary on the island of Keros takes the form of deposits of broken marble vessels and figurines, probably brought severally for deposition from elsewhere in the Cyclades. These acts of devotion have now been accurately dated, thanks to Bayesian analyses of the contemporary stratigraphic sequence on the neighbouring islet of Dhaskalio. The period of use—from 2750 to 2300 cal BC—precedes any identified worship of gods in the Aegean and the site is among the earliest ritual destinations only accessible by sea. The authors offer some preliminary thoughts on the definition of these precocious acts of pilgrimage.