Pollen and Plant Macrofossil Evidence of Vegetation Change at Wallisellen-Langachermoos (Switzerland) During the Mesolithic-Neolithic Transition 8500 to online
Pollen and Plant Macrofossil Evidence of Vegetation Change at Wallisellen-Langachermoos (Switzerland) During the Mesolithic-Neolithic Transition 8500 toPollen and Plant Macrofossil Evidence of Vegetation Change at Wallisellen-Langachermoos (Switzerland) During the Mesolithic-Neolithic Transition 8500 to online
9783443641795 3443641792 Pollen and Plant Macrofossil Evidence of Vegetation Change at Wallisellen-Langachermoos (Switzerland) During the Mesolithic-Neolithic Transition 8500 to, Jean N Haas, Ken N Haas 9781595584632 1595584633 Viral Spiral - How the Commoners Built a Digital Republic of Their Own, David Bollier
J.N. HaasPollen and plant macrofossil evidence of vegetation change at Wallisellen-Langachermoos (Switzerland) during the Mesolithic-Neolithic transition 8500 6500 years ago Dissertationes Botanicae, 267 (1996), pp. 1-67
The Petit-Lac deglaciation occurred in three phases during the Rhône Epoch, the vegetation changed from a steppe to a climate-influenced forest, and finally to a mostly human- controlled Haas, J. N. 1996: Pollen and plant macrofossil evidence of vegeta- the Mesolithic Neolithic transition 8,500 to 6,500 years ago.
Pollen and plant macrofossil evidence of vegetation changeat Wallisellen-Langachermoos (Switzerland) during the Mesolithic Neolithic transition 8500 to 6500 years ago. Pollen and plant macrofossil evidence of vegetation change atWallisellen-Langachermoos (Switzerland) during the Mesolithic Neolithictransition
Pollen and plant macrofossil evidence of vegetation change at Wallisellen-Langachermoos (Switzerland) during the Mesolithic Neolithic transition 8500 to 6500 years ago, J. Cramer, Berlin, Stuttgart (1996)
plant macrofossil evidence of vegetation change at Wallisellen - Langachermoos (Switzerland) during the Mesolithic - Neolithic transition 8500 to 6500 years
Thème:Palynologie: Origine:RAMEAU: Domaines:Botanique Archéologie. Préhistoire. Histoire ancienne: Autres formes du thème:Aérobiologie Analyse pollinique
Haas,J. N. 1996. Pollen and plant macrofossil evidence of vegetation change at Wallisellen-Langachermoos (Switzerland) during the Mesolithic Neolithic transition 8500 to 6500 years ago. Dissertationes Botanicae, 267, 1 67. Iversen,J. 1949. The influence of prehistoric man on vegetation. Danmarks Geologiske Undersøgelse, 4 Raekke,3, 1
Haas, J. N. (1996) Pollen and plant macrofossil evidence of vegetation change at Wallisellen- Langachermoos (Switzerland) during the Mesolithic-Neolithic transition 8500 to 6500 years ago. Dissertationes Botanicae, 267, 1 67. Google Scholar
Switzerland from pollen, plant macrofossil, and sedimentological bog, Wallisellen-Langachermoos, eastern Swiss Plateau at 440 m record of timberline fluctuations caused climatic changes in the final epoch of the Mesolithic culture in central Europe a lithic Neolithic transition 8500 to 6500 years ago.
Haas, Jean Nicolas (1996): Pollen and plant macrofossil evidence of vegetation change at Wallisellen-Langachermoos (Switzerland) during the Mesolithic-Neolithic transition 8500-6500 years ago. Dissertationes Botanicae 267, 67 S. Preis: SFr. 40.-1995
Pollen and plant macrofossil evidence of vegetation change at Wallisellen-Langachermoos (Switzerland) during the Mesolithic-Neolithic transition 8500 to 6500 years ago (1996) Die Schweizerische Exlibris Bibliographie (1996)
Band 267: Haas, Ken Nicolas: Pollen and plant macrofossil evidence of vegetation change at Wallisellen-Langachermoos (Switzerland) during the Mesolithic-Neolithic transition 8500 to 6500 years ago. 1996. VIII, 67 p., 21 figs. In the text and on folders, 3 tab., bound DM 70.-/ $42.
Berichte der Kommission für Archäologische Landesforschung in Hessen 1 (1990/91), 35-37. Gronenborn, D. (1997). Haas, J. N. (1996). Pollen and, Plant Macrofossil Evidence of Vegetation Change a,t Wallisellen-Langachermoos (Switzerland,) during the Mesolithic-Neolithic Transition 8500 to 6500 Years Ago.
Pollen and plant macrofossil evidence of vegetation change at Wallisellen-Langachermoos (Switzerland) during the Mesolithic-Neolithic transition 8500 to 6500 years ago Article Jan 1996
Evidence for Late-Mesolithic agriculture? A reply to Karl-Ernst Behre Evidence for Late-Mesolithic agriculture? A reply to Karl-Ernst Behre Tinner, Willy 2008-07-01 00:00:00 We acknowledge Karl-Ernst Behre's unique contributions to palaeoecology, archaeobotany, and particularly the reconstruction of land-use history. His impact on a multitude of human-impact studies during the past
vegetation dynamics in the Mont Lozère (Massif Central, France) human impact produced major changes in local mire dynamics with the replacement of J.N. HaasPollen and plant macrofossil evidence of vegetation change at. Wallisellen-Langachermoos (Switzerland) during the Mesolithic Neolithic.
pollen and plant macrofossil analyses in annually laminated sediments from evidence for. Holocene climatic change was detected at Soppensee.
Pollen and plant macrofossil evidence of vegetation change at Wallisellen-. Langachermoos (Switzerland) during the Mesolithic-Neolithic transition 8500 to
Read "Mesolithic agriculture in Switzerland? A critical review of the evidence, Quaternary Science Reviews" on DeepDyve, the largest online rental service for scholarly research with thousands of academic publications available at your fingertips.
Pollen and plant macrofossil evidence of vegetation change as evidence for arable farming. At Wallisellen-Langachermoos (Switzerland) during the Mesolithic In general, the composition of the material culture, such as Neolithic transition 8500 to 6500 years ago. Dissertationes Botanicae 267. Tools and other artefacts, does not characterise
A historical ecology of the Ecrins (Southern French Alps): Archaeology and palaeoecology of the Mesolithic to the Medieval period
J.N. HaasPollen and plant macrofossil evidence of vegetation change at Wallisellen Langachermoos (Switzerland) during the Mesolithic Neolithic transition 8500 to 6500 years ago Diss. Bot., 267 (1996), pp. 1-67
Read "Multi-proxy evidence for Holocene lake-level and salinity changes at An Loch Mór, a coastal lake on the Aran Islands, Western Ireland, Quaternary Science Reviews" on DeepDyve, the largest online rental service for scholarly research with thousands of academic publications available at your fingertips.
Haas, J.N. 1996: Pollen and plant macrofossil evidence of vegetation change at Wallisellen-Langachermoos (Switzerland) during the Meso- lithic Neolithic transition 8500 to 6500 years ago.
Haas, J.N. 1996: Pollen and plant macrofossil evidence of vegetation change at Wallisellen-Langachermoos (Switzerland) during the Mesolithic-Neolithic transition 8500 to 6500 years ago. Dissertationes Botanicae 267, 1 67. Google Scholar
Haas, Jean Nicolas 1961- Swiss National Library German National Library. Haas, Jean Nicolas Pollen and plant macrofossil evidence of vegetation change at
The calculated mass of emit- were carried away heat exturbations or wind during the ted CO2 during the fire was 206 t CO2/ha, using the emission burning (Patterson et al., 1987). (iii) The elemental composi- tion of charcoal may differ and depends on the plant tissue from which the charcoal particles are derived and on the char- ring procedure that occurred. Conclusions Experimental slash-and-burn in
Symposium on Sustainable Management of Hemlock Ecosystems in Eastern North America, June 22-24, 1999, Durham, New Hampshire Katherine Pollen and plant macrofossil evidence of vegetation change at Wallisellen-Langachermoos (Switzerland) during the Mesolithic - Neolithic transition 8500 to 6500 years ago.
Pollen and plant macrofossil evidence of vegetation change at Wallisellen-Langachermoos (Switzerland) during the Mesolithic-Neolithic transition 8500 to 6500 years ago (1996) Atlas of fossil plant anatomy in China (1995) Central Asia and Kashmir, archaeobotany and floristics (1995) Taphonomy, sedimentology and genesis of plant fossil deposit
Pollen and plant macrofossil evidence of vegetation change at Wallisellen-Langachermoos (Switzerland) during the Mesolithic- Neolithic transition 8500 to 6500
Pollen and plant macrofossil evidence of vegetation change at Wallisellen-Langachermoos (Switzerland) during the Mesolithic Neolithic transition 8500 to 6500 years ago. Dissertationes Botanicae 267, 1 67. Heer, O. 1866. Die Pflanzen der
Vegetation change and human landscape shaping in the Eastern Pyrenees(Madriu. Valley HAAS, J.N. (1996):Pollen and plant macrofossil evidence of vegetation change at Wallisellen-Langachermoos. (Switzerland) during the Mesolithic-Neolithic transition 8500 to 6500 years ago, J. Cramer, Berlin-Stutgart.
HAAS, J.N. (1996):Pollen and plant macrofossil evidence of vegetation change at Wallisellen-Langachermoos (Switzerland) during the Mesolithic-Neolithic transition 8500 to 6500 years ago, J. Cramer, Berlin-Stutgart.
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