Hartz, S., Müller, J., 2018 (2014/2015). Spätneolithische Transformationsprozesse: Die Bedeutung ... more Hartz, S., Müller, J., 2018 (2014/2015). Spätneolithische Transformationsprozesse: Die Bedeutung von Quern-Neukirchen LA 28 (Tegelbarg)für die Rekonstruktion einer Übergangszeit, Offa 71/72, 149–154.
Quern-Neukirchen LA 28 (Tegelbarg) is the only known shell midden of the Late Neolithic in the Western Baltic. Within transformational processes, which might be linked to climatic deteriorations, the diversification of subsistence production was probably necessary. This would explain the increasing exploitation of marine resources and thus
resulting in the formation of such a Late Neolithic shell midden.
Hartz, S., Müller, J., 2018 (2014/2015). Spätneolithische Transformationsprozesse: Die Bedeutung ... more Hartz, S., Müller, J., 2018 (2014/2015). Spätneolithische Transformationsprozesse: Die Bedeutung von Quern-Neukirchen LA 28 (Tegelbarg)für die Rekonstruktion einer Übergangszeit, Offa 71/72, 149–154.
Quern-Neukirchen LA 28 (Tegelbarg) is the only known shell midden of the Late Neolithic in the Western Baltic. Within transformational processes, which might be linked to climatic deteriorations, the diversification of subsistence production was probably necessary. This would explain the increasing exploitation of marine resources and thus
resulting in the formation of such a Late Neolithic shell midden.
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Quern-Neukirchen LA 28 (Tegelbarg) is the only known shell midden of the Late Neolithic in the Western Baltic. Within transformational processes, which might be linked to climatic deteriorations, the diversification of subsistence production was probably necessary. This would explain the increasing exploitation of marine resources and thus
resulting in the formation of such a Late Neolithic shell midden.
Quern-Neukirchen LA 28 (Tegelbarg) is the only known shell midden of the Late Neolithic in the Western Baltic. Within transformational processes, which might be linked to climatic deteriorations, the diversification of subsistence production was probably necessary. This would explain the increasing exploitation of marine resources and thus
resulting in the formation of such a Late Neolithic shell midden.