Fitz Jenő (szerk.): Die aktuellen Fragen der Bandkeramik - István Király Múzeum közelményei. A. sorozat 18. A Pannon konferenciák aktái 1. (Székesfehérvár, 1972)
R. R. Newell: A hollandiai vonaldíszes kerámia korakő-eszközeinek rokonsága a közéső kőkori kőeszköziparral
Borer of cruciform type (PL 2, E 338) finds its origins in Sweykhuizen II (PI. 20, 22). The Long Blade Borer (PL 2; E 373, E 354) however is more difficult to trace. An analysis of the Mesolithic material failed to produce a progenitor. This type can only be interpreted as an internally developed form, possibly derived from the Short Blade Borer. Quite the opposite is true of the Flake Borer (PL 3, S 157). This type was anticipated at Sweykhuizen II (PL 20, 33) and Zuid Hijkerzand (PL 17, 33) Even more closely resembling Oldesloe forms is the Disc Borer, (PL 3; E 190, S 183, E 11), which is comparable with Kesseleik I (PL 27, 1, 2) and many other Western Oldesloe sites. Bandkeramik Blade Burins (PL 3, S 153; PL 4; E 61, Sd 208, E 014) find their origins at Sweykhuizen II (PL 20, 30). Flake Burins (PL 4, E 014) are ecjually common in the Atlantic Period Mesolithic, Zid Hijkerzand (PL 18, 1, 2). Finally, Oise Burins (PI. 4; E 1, S 190: PL 5; E 175, S 139) are exact reproductions of those from Kesseleik I (PL 28, 1 — 3), Zuid Hijkerzand (PL 18, 9—11) etc. The Bandkeramik end scrapers are divided into a number of type-groups which find their antecedents in the equivalent Mesolithic groups, the smallest are the Miniature Scrapers. Miniature Blade Scrapers (PL 7 ; S 14, S 104, E 125, E 90) resemble very closely microblade scrapers from Zuid Hijkerzand (PL 17, 42 — 43). Miniature Round Scrapers (PL 7; E 114, E 42, S 7) are related to the very common Mesolithic microscrapers. Double Scrapers (PL 7 ; S 90, S 162, E 356) are almost universally represented in the Atlantic Period Mesolithic: Kesseleik I (PL 26, 2 — 3), Zuid Hijkerzand (PL 17, 40), etc. The Straight Short End Scraper (PL ; S 25, S 108) is found at Kesseleik I and Convex Short End Scrapers (PL 5; S 24, S 213, S 27) occur at Sweykhuizen II )P1. 21, 1 — 3), Zuid Hijkerzand (PL 17, 17) and many other sites. The Oblique Short End Scrajeer (PL 5; S 141, S 27, S 109) is also paralleled at the above sites and the Denticulate Short End Scraper (PL 6; E 4, S 143, S 58) occurs frequently in Mesolithic contexts. The following type-group is the Long End Scrapers. Straight types (PL 0; 3, S 244, S 109) are anticipated at Zuid Hijkerzand (PL 17, 40) while the Convex Long End Scrapers (PL 6 ; S 130, S 109) occur at Sweykhuizen II (PL 21, 4), Zuid Hijkerzand (PL 17, 39), and many other core and flake axe sites. Oblique Long End Scrapers (PL 6; S 30, S 210, S 31) parallel specimens from Sweykhuizen II (PL 21, 6). The Denticulated form (PL 6; S 72, S 187, S27) is also found at Sweykhuizen II (PL 21, 5). The first of the Discoid Scrapers is the Keeled Scraper (PL 7 ; E 355, S 124: PL 8; Sd 371, S 27). This Bandkeramik tool form can be derived from typical handgrip scrapers such as Sweykhuizen II (PL 21, 7). More commonly, the Mesolithic forms are broader ; Keseleik I (PL 26, 1), Sweykhuizen II (PL 21, 8). Large Discoid Scrapers (PL 8; E 491, E 229) are exactly matched at Sweykhuizen II (PI. 21, 9) and Kesseleik I (PL 27, 1). The same degree of similarity is found between Mesolithic and Bandkeramik Oblong Discoid Scrapers (PL 8; Sd 281, S 215): Kesseleik I (PL 27, 3)• Small Round Discoid Scrapers are equally typical (PL 9; E 610, E 12 E 354) of pieces from Sweykhuizen II (PL 21, 12), Kesseleik I (PL 26, 6; PL 27, 4) and Zuid Hijkerzand (PL 17, 43 — 44). Finally, Small Keeled Scrapers (PL 9; E 458, E 484) are exactly paralleled at Sweykhuizen II (PL 21, 10—11), Kesseleik I (PL 26, Í) and Zuid Hijkerzand (PL 18, 1). As in Mesolithic industries, the Bandkeramik Side Scrapers are separated into types according to the form of the working edge. The Convex Side Scrajjers (PL 10; E 355, E 111: PL 11; S 210, E 622) are duplicates of scrapers from Kesseleik I (PL 26, 10) and Zuid Hijkerzand (PL 18; 2, 4). Concave Side Scrapers (PL 11;E 107, E 608, E 185) are less frequently found in the Mesolithic but a parallel does come from Sweykhuizen II (PL 21, 13). Notched Side Scrapers (PL 11; E 261, E 426) occur in comparable forms at Zuid Hijkerzand (PL 18, 3). Bandkeramik Planes (PL 12; E 49, E 228, E 239) must be seen a developed and specialized side scrapers. They are, in fact, merely higher and narrower forms than the Bandkeramik specimen on PL 5, S 210. Exact parallels come from Kesseleik I (PL 28, 4 — 5). Blade Knives (PL 12; E 1) are not so clearly represented in the Western Oldesloe sites but are typical in the classic culture area. The same impression is given by the Two-Edged Knife (PL 12; E 73, 8 90, S 19). This latter type is represented at Kesseleik I (PL 26, 11) and Zuid Hijkerzand (PL 17, 36) but in a much more primitive state of development. Flake Knives (PL 13; E 116, E 361) are clearly Mesolithic in form and origin: Kesseleik I (PL 26, 12). Bandkeramik Pics (PL 13 ; E 170, E 334, E 137) are poor in quality. Nevertheless, a typological affinity with Mesolithic forms is apparent : Kesseleik I (PL 29, 2), Sweykhuizen II (PL 24, 1), and others. The Bandkeramik Typical Flake Axe is unquestionably Mesolithic in morphology, technology, and origin. Specimens with tranchet edges, (PL 14, Sd 46,) match Younger Oldesloe axes from Kesseleik I (PL 30, 3). Flake axes with a retouched edge (PL 13; E 149: PL 14, E 62) are exact duplicates of axes from Sweykhuizen II (PL 22, 3). The Typical Flake Axe with a retouched ventral face (PL 13, Sd 430) confirms the contemporaneity of the Younger Oldesloe tsage with that of the local Bandkeramik. The identical form from Sweykhuizen II (PL 22, 1) and Kesseleik I (PL 30, 2) serve as positive indications of the postulated Mesolithic-Bandkeramik contact and acculturation. The Diminutive Flake Axes (PL 14; Sd 65, E 354, E 111, E 258) are in agreement with pieces from Kesseleik I (PL 30, 5 — 6) and elsewhere. Axe Insets (PL 15; 9, S 9 S 217) match specimens from Sweykhuizen II (PL 24, 3) and Triangular Implements (PL 15; S 160: PL 16; S 45, S 389) occur in a number of Mesolithic contexts. In conclusion, it has been clearly demonstrated that almost every technological, morphological, and typological element which characterises the flint industry of the Dutch Limburg Linearbandkeramik has an exact or immediate parallel and antecedent in the 3* 35
