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Capo Alfiere:
A Neolithic site near Crotone, Calabria, Italy
by Jon Morter
Contents:
Background
Architecture
Other Artifacts
Absolute Dating
Related Publications
Background
Capo Alfiere is the name of a Neolithic site located on a small headland
on the eastern coast of Calabria. Archaeological excavations at the site
were conducted by a team from the University of Texas in the summers of
1987 and 1990. The digging was directed by Jon Morter. The work is part
of a broad study of the landscape of the territory of the Classical Greek
colonial city of Kroton (modern Crotone) under the supervision of Prof.
Joe Carter.[1]
The excavations have revealed the surviving portions of a stratified
deposit dating to the Middle Neolithic period. Two main strata have been
defined to date, each with sub-phases. The majority of the pottery appears
to be of the Stentinello tradition, a type first defined in eastern Sicily
by Paolo Orsi at the end of the last century. Other finds include both
ground and chipped stone objects. A large floral and faunal assemblage
is currently under analysis at the Laboratorio per Bioarcheologia in Rome
under the supervision of Dott. Lorenzo Costantini.
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Architecture
The site's architectural remains are particularly interesting. These
are best preserved in the upper stratum (II). Two stretches of an extremely
large stone wall were discovered. These form an angle and appear to enclose
the cobble floor of a house. We estimate that about 50% of the latter has
survived. A reflooring of this structure had sealed a large quern and the
stone-lined hearth of the hut, both features being built into the original
cobble floor. The floor appears to have been about 4.8m on its surviving
complete side and probably at least that long in the incomplete dimension.
The corners of the paving are curved. The hearth was probably originally
central to the structure and the large emplaced quern was beside it. A
small portion of a similar pavement (from a structure now largely destroyed
by recent agriculture) was found in the earlier stratum (I).
The
massive walls are of a peculiar construction. A central core of large blocks
was faced on one or both sides by large slabs set vertically. Unfortunately,
due to plough damage, the large walls had not survived above the first
course or two. Thus it is impossible to say with certainty how high they
originally stood. As they are a metre or more thick, it seems logical that
they originally stood quite high. There was considerable rock and daub
tumble above the hut paving in the area delimited by the walls.
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Other Artifacts
Studies of the ceramics, lithics, floral and faunal collections from
the site are still in progress, but some preliminary observations can be
made.
Stentinello
ceramics are distinguished by their use of elaborate impressed and incised
decorative design work. This seems to represent a divergence from the painted
finewares produced elsewhere in the lower Italian peninsula at this time.
At Capo Alfiere, there are definite differences between the Stentinello
style ceramics from the upper and lower strata. The earlier material is
more consistently black in colour and the finer decoration makes use of
coloured pastes (ochres and calcium carbonate) in a variety of colours
(yellow through red and also white) to enhance the decoration. The use
of ochres seems to have fallen out of favour by the period of the upper
stratum but the actual impressed designs are, if anything, more elaborate.
The site has produced very little painted pottery; what there is seems
to be on a distinct and possibly imported, fabric (Morter
and Iceland 1995).
Although the chipped stone artifacts from this site are not in of themselves
particularly exciting technologically, being a fairly straightforward microblade
industry, an examination of the raw materials used is very interesting.
There appears to have been a shift in raw material usage or availability
over time. The lithics from the lower stratum (I) contained 28% obsidian
(by count), while the upper stratum had almost 67% obsidian. The balance
of the lithic material was cherts and quartzites available fairly locally.
This apparent increase in obsidian availability, only obtainable from
Lipari by long distance exchange, may be signaling an increase in material
traffic by the upper level. This may also be reflected in the discovery
of a cache of large ground stone axes in that level--also probably derived
from some distance from the site.
Analysis of the floral and faunal remains from the 1990 excavations
and hence the lower stratum is not quite complete. The recovery of floral
remains from the upper stratum (II) has been good with a variety of wheats
and barley represented plus a good selection of legumes and weeds (information
provided by Dott. L. Costantini listed in Morter
1990). Although the proportion of identifiable animal bones is small,
the collection has demonstrated a good selection of domesticate and some
vermin (Scali 1990). Domesticated animals
predominate over game as is typical for this period.
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Absolute Dating
We were fortunate in obtaining a series of radiocarbon dates from the
site which give a general and broadly consistent picture of its overall
date.
Three dates from the upper stratum (5650+/-70 bp, 5450+/-60
bp, 5410+/-80 bp) date the hearth and the surface sealing it to the second half of the
5th millennium BC, after calibration. There was no suitable carbon from
stratum I so resort had to be made to dating with animal bone. This gave
a date of 5950+/-100 bp, indicating a calibrated range towards the beginning
of the 5th millennium BC.
These dates are interesting as they put the upper stratum rather late
in the accepted range for Stentinello sites. The lack of ceramics attributable
to the supposedly successive Serra d'Alto phase, and discovery of some
closer to the purportedly Late Neolithic, Diana types, has led us to question
the general applicability of the accepted southern Italian ceramic sequence
hereabouts.
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Related Publications
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