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Tichitt-Walata and the Middle Niger - PanAfrican Association of ...

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436 Kevin C. MacDonald<br />

fact remains <strong>the</strong> almost exclusive temper <strong>of</strong> <strong>the</strong> <strong>Tichitt</strong> tradition .throughout its long span <strong>of</strong> years,<br />

with s<strong>and</strong> <strong>and</strong> grog occasionally added or substituted. Everted rims, as well as red slip, only begin to<br />

appear in <strong>the</strong> Nkahl <strong>and</strong> Naghez phases (IV-V), with twisted twine remaining <strong>the</strong> dominant decor.<br />

By <strong>the</strong> Chebka <strong>and</strong> Arriane phases (VI-VII) everted rims have become common accounting for<br />

c.40-50% <strong>of</strong> all rims. Cord-wrapped stick motifs become common again, <strong>and</strong> start to be used as<br />

roulettes instead <strong>of</strong> only for impression (cf. Fig. 5 for ceramics from phases VI-VII). Finally, in <strong>the</strong><br />

AkJinjeir phase (VIII) applied plastic motifs become common, <strong>and</strong> vessels grow much larger <strong>and</strong><br />

have less decor.<br />

The <strong>Tichitt</strong> assemblages only become analogous with those· <strong>of</strong> Ndondi Tossokel'during <strong>the</strong><br />

Chebka <strong>and</strong> Arriane phases (e.g. higher proportions <strong>of</strong> everted rims, rouletted cord-wrapped decor,<br />

etc.). Their resemblance is not absolute, however, as some <strong>Tichitt</strong> vessels <strong>of</strong> <strong>the</strong>se phases feature<br />

knotted twine decor (cf. Hurley 1979: Type 165), a manipulation entirely absent in <strong>the</strong> Merna.<br />

Discussion: regional chronology<br />

Dating <strong>the</strong> Kobadi facies<br />

The earliest known date for <strong>the</strong> human occupation <strong>of</strong> <strong>the</strong> <strong>Middle</strong> <strong>Niger</strong> comes from <strong>the</strong> site <strong>of</strong> Tiabel<br />

Goudiodie. This site has been dated on freshwater oyster shells (E<strong>the</strong>ria elliptica) to between 2570<br />

<strong>and</strong> 2410 cal BC (Togola <strong>and</strong> Raimbault 1991). As usual with dates on freshwater materials, however,<br />

a carbonate reservoir effect <strong>of</strong> several hundred years should be allowed for, thus an initial<br />

occupation date <strong>of</strong> around 2000 BC is more likely for <strong>the</strong> site.<br />

It is difficult to know what <strong>the</strong> sequence <strong>of</strong> dates from <strong>the</strong> site <strong>of</strong> Kobadi actually date culturally,<br />

since all but one <strong>of</strong> <strong>the</strong>m are conventional collagen dates run on surface-collected bone, <strong>and</strong><br />

Ndondi Tossokel materials are known to also occur on <strong>the</strong> site (Raimbault <strong>and</strong> Dutour 1989,<br />

MacDonald 1994). The earliest date, 1740-1510 BC, was run on burned hippopotamus bone, <strong>and</strong> is<br />

thus most likely associated with <strong>the</strong> aquatically based Kobadi tradition. More recently, an as yet<br />

incompletely published date (Georgeon et al. 1992: 86) was run on an unspecified material from <strong>the</strong><br />

1989 excavations. Its result, 1740-1440 BC (3305±80 BP), is very close to that <strong>of</strong> <strong>the</strong> early 'hippo<br />

bone'. The middle dates are less certain, coming from indeterminate burned bone (1260-900 BC)<br />

<strong>and</strong> mammalian vertebrae (930-610 BC) respecti vely, <strong>the</strong> latter date coming from samples collected<br />

by Mauny in 1954 (Georgeon et at. 1992). The most recent date (770 to 380 BC) was run on <strong>the</strong><br />

cranium <strong>of</strong> a late inhumation recovered eroding from <strong>the</strong> midden surface. It is evident that we are<br />

dealing with a lengthy <strong>and</strong> probably multi-faceted occupation at Kobadi (c. 1750-400 BC). How<br />

punctuated this may have been by gaps in occupation, <strong>and</strong> <strong>the</strong> extent to which typical Kobadi wares<br />

continued throughout it, will only be clarified with <strong>the</strong> publication <strong>of</strong> a complete excavation report<br />

by Raimbault.<br />

A single radiocarbon date has recently been run on hippo ivory from <strong>the</strong> lowest Kobadi facies<br />

occupation layer <strong>of</strong> Kolima-Sud (layer V, KLS- l lv.25). The result <strong>of</strong> this apatite determination was<br />

as follows: 3365±70 BP11740-1530 cal BC (GX-21192-AMS). This date is comparable to <strong>the</strong> two<br />

earliest dates from Kobadi itself, <strong>and</strong> when bracketed by a date associated with Ndondi-Tossokel<br />

ceramics in <strong>the</strong> upper Kolima-Sud sequence (see below), suggests a minimum temporal range <strong>of</strong><br />

1750 to 1300 BC for <strong>the</strong> Kobadi facies.<br />

Dating <strong>the</strong> Ndondi Tossokel <strong>and</strong> Beretouma facies<br />

Test excavations carried out at <strong>the</strong> site <strong>of</strong> Kolima-Sud in 1990 provide our only definitive date for<br />

Ndondi Tossokel <strong>and</strong> Beretouma ceramics in context. There, two sondages revealed occupational<br />

deposits <strong>of</strong> 2.5 m in depth containing four principal occupational layers (MacDonald 1994). In

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