archeology (arts and humanities)

Estimating C4plant consumption in Bronze Age Northeastern Italy through stable carbon and nitrogen isotopes in bone collagen

The application of biomolecular techniques for the study of food practices in the Italian Bronze Age has revealed an interesting complexity. This is particularly true for the Po plain, in northern Italy, where the use of “alternative” grains (i.e., the millets) has been assessed isotopically through the measurement of stable carbon (?13C) and nitrogen (?15N) isotope ratios in human and animal bone collagen at the site of Olmo di Nogara (Verona). This work provides new isotopic data from 12 Early, Middle, and Late Bronze Age sites from western Veneto and Friuli.

Organic geochemical and palynological evidence for Holocene natural and anthropogenic environmental change at Lake Dojran (Macedonia/Greece)

In this study, we present lipid biomarker and palynological data for a sediment core from Lake Dojran (Macedonia/Greece), which covers the entire Holocene period. We analyzed vascular plant-derived n-alkanes, combustion-derived polycyclic aromatic hydrocarbons (PAHs), fecal steroids, and bacterial and archaeal glycerol dialkyl glycerol tetraether (GDGT) lipids in concert with microcharcoal and pollen assemblages to reconstruct climatic, environmental, and human impact in the Dojran catchment and the greater Dojran area.

Quaternary disappearance of tree taxa from Southern Europe. Timing and trends

A hundred pollen and plant macrofossil records from the Iberian Peninsula, Southern France, the Italian Peninsula, Greece and the Aegean, and the southwestern Black Sea area formed the basis for a review of the Quaternary distribution and extirpation of tree populations from Southern Europe. Following a discussion of the caveats/challenges about using pollen data, the Quaternary history of tree taxa has been

From Aterian notch to Aterian tang. How to make a technological invention

The Aterian lithic techno-complex that characterizes the late Middle Stone Age in North Africa is well known especially for its tanged or stemmed points. Recent techno-morphological and use-wear analyses have added new data to support the identification of the tang as the hafted portion of an artifact. They have also highlighted the presence of this attribute on tools other than projectile points, in contrast with the widespread idea that the tanged point is the Aterian fossile directeur.

How much is known about glassy materials in Bronze and Iron Age Italy? New data and general overview

Knowledge of glass trading in protohistoric Southern Italy has been limited by a lack of archeometrical data available to date, preventing comparison with the well-known Northern Italian context. The aim of the present work is to help fill the data gap for Southern Bronze-Iron Age vitreous items and enable a general overview of protohistoric Italian glass supply routes.

What is ‘European archaeology’? What should it be?

‘European archaeology’ is an ambiguous and contested rubric. Rooted in the political histories of European archaeology, it potentially unites an academic field and provides a basis for international collaboration and inclusion, but also creates essentialized identities and exclusionary discourses. This discussion article presents a range of views on what European archaeology is, where it comes from, and what it could be.

Tyrrhenian central Italy. Holocene population and landscape ecology

This paper compares changes in vegetation structure and composition (using synthetic fossil pollen data) with proxy data for population levels (including settlements and radiocarbon dates) over the course of the last 10 millennia in Tyrrhenian central Italy. These data show generalised patterns of clearance of woodland in response both to early agriculturalists and urbanism, as well as the specific adoption of tree crops and variations in stock grazing.

The lateglacial and Holocene vegetation and climate history of Lago di Mezzano (central Italy)

The top 12 m of a lacustrine sediment sequence from Lago di Mezzano (42°36?N, 11°46?E, 452 a.s.l., Latium, central Italy) have been palynologically investigated. The chronology was established on the basis of radiocarbon dates, measures of annual laminations and volcanic ashes. The continuous sequence provides new fundamental information on the Lateglacial and Holocene, periods often fragmented in Italian pollen records, identifying vegetation dynamics and climate changes occurring in the last 15,300 years.

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