Mediterranean Obsidian Trade/Exchange Flashcards
What can we learn from trade?
- Production and consumption
- Relations or contacts between peoples and groups
- Social and economic developments
- Ideas of value, symbolic importance of things
- Chronology/dating
Polanyi (1957): 3 types of trade/exchange
- Reciprocal: reciprocating with the normal equivalence of the thing received without delay
- Redistribution: collecting material centrally and reallocating it
- Market or commerical: Purchase and movement of goods without the knowledge of the identity of further purchaser
Obsidian formation
- Rock form as a result from volcanic activity
- Special circumstances of cooling are required and high viscosity in the rock
- Isotropic in structure, easy to work
Use of obsidian and eras in which they’re found
- Very likely used to manufactured of cutting and piercing tools
- In Prehistoric Europe, it was mainly used for making tools
- In Egypt it was used for decorative or symbolic objects (chipping, grinding, abrasion)
- Most Neolithic sites in the Med and the Near East have obsidian artefacts in them
Why is obsidian useful in exchange studies
- Because of its chemical and geological nature
- Limited sources of workable obsidian, all are on island in the central western Med
- Artefacts occur hundreds of miles away from these sources: importable items
- Not all obsidian is of exactly the same quality
4 main sites for workable obsidian
- Lipari:
- One of main sources in Western Med
- Very pure obsidian, clear glassy appearence, easy to work
- Coastal location: maritime travel and trade
- Old pumice works (white hills of pumice)
- Malta:
- Variable in quality
- Pantelleria:
- Greenish hue
- Volcanic island
- Melos:
- Major source for obsidian in Greece and Aegean
Annerman, 1985
- Wanted to conduct a detailed survey on obsidian
- Went fieldworking in Calabria (source)
- Found 200 sites within a few seasons
- Made a map dislpaying the percentage of obsidian in lithic assemblages at select neolithic sites
- Concluded that most on the sites on the West Coast had over 90% obsidian
- Didn’t find rough lumps, obsidian had been pre-prepared into cores on the island and then shipped
- More waste near the source: abundant supply
- Less waste further from the source: better looked after
Franchthi cave site
- Obsidian from Melo found in late Palaeolithic-Mesolithic layers
- Been sourcing obsidian long before farming
- Could venture via paddling easily to Melos
- Humans adept to sea travel
Renfrew & Bahn (2020) - Optical Emission Spectrometry (OES)
- Used in 1950s-60s for the characterisation of Obsidian (as well as metallurgy and faience beads)
- Based on the principle that the outer electrons of the atoms of every chemical element emit a light of a particular wavelength and colour when a sample is excited (heated in a carbon arc)
- The light given off is composed of different wavelengths, which can be seperated into a spectrum
- The presence or absence of various elements can be established by looking for the appropriate spectral line of their characteristic wavelengths
- Accuracy of about 25%
Renfrew & Bahn (2020): Inductively Coupled Plasma Atomic Emission Spectrometry (ICP-AES)
- Follows same basic principles of OES but the sample in solution is atomized and excited in a stream of argon plasma rather than in a carbon arc
- Very high temps can be reached which reduced problem of interference between elements
- 10mg needed for elemental analysis, accuracy of +5%
- Not excessively expensive, high rate of sampling achieved
Renfrew & Bahn (2020): Neutron Activation Analysis (NAA)
- Used in 1970s for trace element analysis of pottery, obsidian, rocks, semi-precious stones
- Depends on the transmutation of the nuclei of the atoms of a sample’s various elements by bombarding them with slow thermal neutron
- Leads to the production of radioactive isotopes of most elements present in the sample
- Isotopes decay into stable ones by emitting radiation (often gamma)
- The energies of these gamma rays are characteristic of the radioactive isotopes, and are measured to identify the elements present
- The intensity of radiation of a given energy can be compared with that emitted by a standard that was irradiated together with the sample, hence the quality of the element in the sample can be calculated
- +5% accuracy
Tykot (2017) - Obsidian studies in central Med over last 50 years
- Detailed analysis on 4 Italian Islands
- Minimally (ICP-MS) or totally (XRF, pXRF) non-destructive analysis
- > 10,000 analyses in last decade
Tykot (2017) - Obsidian studies in the 60s
The first successsful analyses of obsidian distinguishing between sources was accomplished using OES (Cann & Renfrew, 1964)
Tykot (2017) - Obsidian studies in the 70s
- NAA was applied and this method used trace elements to clearly distinguish between idland sources
- NAA is automated which allowed for analysis of a significant number of artefacts
- Renfew et al developed a hypothesis using interaction zones to compare geographic obsidian distribution patterns in central Med
- Clear that obsidian from Lipari and Sardinia travelled over great distances from the Neolithic
Tykot (2017) - Lipari Obsidian and sub-sources
- Clear evidenec of Neolithic settlement in Lipari
- The obsidian was only geologically formed late in the Mesolithic, 1000-2000 years earlier
- A detailed survey of the outcrops has been studied and may be distinbuished chemically
- Monte della Guardia obsidian is too small to make stone tools
- Canneto Dentro sources appear to have been fairly small in size and quantity
The Gabellotto Gorge source is much larger in quantity and accessible