Deciphering the complexity of a 'simple' mesolithic phenomenon:Indicators for construction, use and taphonomy of pit hearths in Kampen (the Netherlands)

Pit hearth features form a common phenomenon in the Mesolithic of North-West Europe, and the Netherlands and adjacent parts of Germany and Belgium in particular. Using soil micromorphology, we investigated the genesis and taphonomy of several pit hearth features, embedded in sandy podzolic soils from Kampen (the Netherlands). This is one of the first studies to investigate one of such pits in its entirety, instead of only the lower, charcoal-rich fill. Our results show that the upper fill of these pits contains considerable amounts of non-charred degraded organic matter. The lower fill typically contains fragments of charcoal and some wood tar, but also black coatings around sand grains, that is interpreted as charred humus from a podzol B-horizon. These coatings indicate that material from the upper horizons of a podzol profile – e.g. in the form of turves - was used to control a fire on the floor of the pit. Fine charred material postdepositionally leached from the pit feature into the underlying deposits, associated with increased formation of limped clay coatings. This indicates that ash-induced alkaline charcoal degradation and associated clay translocation played a role in this process. The Kampen case provides strong evidence that fine charred organic material may contaminate underlying archaeological or sedimentary unit

Trapeze shaped flint tips as proxy data for occupation during the Late Mesolithic and the Early to Middle Neolithic in the northern part of the Netherlands

In the northern part of the Netherlands (defined here as the area situated above the river Rhine), the Late Mesolithic is dated to the period between ca. 8100 and 6000 BP, and is characterised by the occurrence of trapeze shaped flint tips. Trapezes continue to be in use during the Swifterbant culture (ca. 6000-4800 BP), including the ceramic Mesolithic phase (Early Swifterbant) which is dated between 6000 and 5600 BP. During the Funnelbeaker culture or TRB (ca. 4800-4100 BP) transverse points dominate. With the onset of the Single Grave Culture (SGC) transverse points are no longer the 'preferred weapon of choice'; they are replaced by surface-retouched (tanged) points. In this paper some of the basic premises of the typological development of trapezes (narrow to broad) and the chronological relevance of 'subtypes' (symmetric, asymmetric, right-angled and rhombic) are discussed based on analyses of trapezes from four excavated Mesolithic and Swifterbant sites. For comparison a random sample of TRB transverse points was included in several analyses as well. One of the main conclusions of this paper is that it is possible, based on analyses of metric and non-metric traits of trapeze shaped flint tips, to distinguish between true 'Mesolithic' trapezes, trapezes belonging to the (Neolithic) Swifterbant culture, and transverse points of the TRB. The outcomes of these analyses may help in obtaining a relative date for undated (surface) assemblages, and may furthermore lead to the positive identification of Swifterbant settlements in the higher (situated above the present-day sea level) Pleistocene areas in the northern and eastern part of the study area which are so far unknown. The results presented here will be put to the test in a forthcoming paper. (C) 2008 Elsevier Ltd. All rights reserved