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Climate change and the adoption of agriculture in north-west Europe

Published online by Cambridge University Press:  25 January 2017

Clive Bonsall*
Affiliation:
Department of Archaeology, University of Edinburgh, UK
Mark G. Macklin*
Affiliation:
Institute of Geography and Earth Sciences, University of Wales, Aberystwyth, UK
David E. Anderson*
Affiliation:
School of Geography and the Environment, University of Oxford, UK
Robert W. Payton*
Affiliation:
Department of Agricultural and Environmental Science, University of Newcastle upon Tyne, UK

Abstract

Farming can be shown to have spread very rapidly across the British Isles and southern Scandinavia around 6000 years ago, following a long period of stasis when the agricultural ‘frontier’ lay further south on the North European Plain between northern France and northern Poland. The reasons for the delay in the adoption of agriculture on the north-west fringe of Europe have been debated by archaeologists for decades. Here, we present fresh evidence that this renewed phase of agricultural expansion was triggered by a significant change in climate. This finding may also have implications for understanding the timing of the expansion of farming into some upland areas of southern and mid-latitude Europe.

On peut démontrer que, il y a 6000 ans, l'agriculture s'est répandue très rapidement dans les îles Britanniques et dans la Scandinavie méridionale. Cette expansion survenait après une longue période de stagnation où la “frontière” de l'agriculture se situait plus au sud de la plaine de l'Europe septentrionale, entire le nord de la France et le nord de la Pologne. Depuis des décennies, les archéologues débattent sur les raisons de ce retard dans l'adoption de l'agriculture aux limites nord-ouest de l'Europe. Nous présentons ici de nouvelles évidences pour prouver que l'expansion de l'agriculture fût revivée par un changement significatif due climat. Ce fait pourrait aussi expliquer le rythme de la progression de l'agriculture jusque sur certains plateaux de l'Europe méridionale et centrale.

Zusammenfassung

Zusammenfassung

Nachweisbar breitete sich die Landwirtschaft vor ca. 6.000 Jahren – nach einer langen Periode der Stagnation, in der die landwirtschaftliche „Grenze” weiter im Süden, im Nordeuropäischen Tiefland zwischen Nordfrankreich und Nordpolen lag – sehr schnell über die Britischen Inseln und Südskandinavien aus. Die Ursachen dieses verspäteten Einsetzens der Landwirtschaft am nordwestlichen Rand Europas werden von Archäologen seit Jahrzehnten diskutiert. Hier werden neue Hinweise darauf vorgestellt, daß diese erneute Phase landwirtschaftlicher Expansion durch einen signifikanten Klimawechsel ausgelöst wurde. Diese Erkenntnisse könnten auch zum Verständnis des Zeitpunktes der Ausdehnung der Landwirtschaft in einige Hochlagen südlicher und mittlerer Breitengrade Europas beitragen.

Type
Articles
Copyright
Copyright © 2002 Sage Publications 

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References

Anderson, D.E., 1998. A reconstruction of Holocene climatic changes from peat bogs in north-west Scotland. Boreas 27:208224.CrossRefGoogle Scholar
Anderson, D.E., Heather, A. BINNEY and Melanie, A. SMITH, 1998. Evidence for abrupt climatic change in northern Scotland between 3900 and 3500 calendar years BP. The Holocene 8:97103.Google Scholar
Avery, B.W., 1980. Soil Classification for England and Wales. Harpenden: Soil Survey of England and Wales Technical Monograph 14.Google Scholar
Avery, B.W., 1990. Soils of the British Isles. Wallingford: CAB International.Google Scholar
Baillie, M.G.L., 1992. Dendrochronology and past environmental change. Proceedings of the British Academy 77:523.Google Scholar
Baillie, M.G.L. and Brown, D.M., 1999. Dendrochronology of Irish bog trackways. Irish Archaeological Wetland Unit Transactions 3:395402.Google Scholar
Bennett, K.D., 1989. A provisional map of forest types for the British Isles 5000 years ago. Journal of Quaternary Science 4:141144.CrossRefGoogle Scholar
Bennett, K.D., 1995. Post-glacial dynamics of pine (Pinus sylvestris L.) and pinewoods in Scotland. In Aldhous, J.R. (ed.), Our Pinewood Heritage: 2339. Inverness: Forestry Commission, RSPB, SNH.Google Scholar
Bianchi, G.G. and Mccave, I.N., 1999. Holocene periodicity in North Atlantic climate and deep-ocean flow south of Iceland. Nature 397:515517.CrossRefGoogle Scholar
Binney, HEATHER A., 1997. Holocene environmental change in the Scottish Highlands: multiproxy evidence from blanket peats. Unpublished , London Guildhall University.Google Scholar
Bogucki, P., 1998. Holocene climatic variability and early agriculture in temperate Europe: the case of northern Poland. In Zvelebil, M., Dennell, R. and Lucyna, Domanska (eds), Harvesting the Sea, Farming the Forest: 7785. Sheffield: Sheffield Academic Press.Google Scholar
Bond, G., Showers, W., Cheseby, M., Lotti, R., Almasi, P., Demenocal, P., Priore, P., Cullen, M., Hajdas, I. and Bonani, G., 1997. A pervasive millennial-scale cycle in North Atlantic Holocene and glacial climates. Science 278:12571266.CrossRefGoogle Scholar
Bonsall, C., Anderson, D.E. and Macklin, M.G., in press. The Mesolithic-Neolithic transition in western Scotland and its European context. In Saville, A. (ed.), Mesolithic Scotland: The Early Holocene Prehistory of Scotland and its European Context. Edinburgh: Society of Antiquaries of Scotland.Google Scholar
Briffa, K.R., 1994. Mid and late Holocene climate change: evidence from tree growth in northern Fennoscandia. In Funnell, B.M. and Kay, R.L.F. (eds), Palaeoclimate of the Last Glacial/Interglacial Cycle: 6165. Swindon: NERC Earth Sciences Directorate, Special Publication No. 94/2.Google Scholar
Digerfeldt, G., 1988. Reconstruction and regional correlation of Holocene lake-level fluctuations in Lake Bysjon, South Sweden. Boreas 17:165182.CrossRefGoogle Scholar
Dupont, Lydie M., 1986. Temperature and rainfall variation in the Holocene based on comparative palaeoecology and isotope geology of a hummock and a hollow (Bourtangerveen, The Netherlands). Review of Palaeobotany and Palynology 48:71159.CrossRefGoogle Scholar
Girling, Maureen A., 1979. Fossil insects from the Sweet Track. Somerset Levels Papers 5:8493.Google Scholar
Girling, Maureen A., 1984. Investigations of a second insect assemblage from the Sweet Track. Somerset Levels Papers 10:7991.Google Scholar
Hodder, I., 1990. The Domestication of Europe. Oxford: Blackwell.Google Scholar
Hodge, C.A.H., Burton, R.G.O., Corbett, W.M., Evans, R., and R.S.Seale, R., 1984. Soils and their Use in Eastern England. Harpenden: Soil Survey of England and Wales Bulletin 13.Google Scholar
Iversen, J., 1944. Viscum, Hedera and Ilex as climate indicators. Geologiska föreningens i Stockholm firhandlingar 66:463483.CrossRefGoogle Scholar
Jarvis, M.G., Allen, R.H., Fordham, S.J., Hazelden, J., Moffat, A.J. and Sturdy, R.C., 1984. Soils and their Use in South East England. Harpenden: Soil Survey of England and Wales Bulletin 15.Google Scholar
Karlén, W. and Kuylenstierna, J., 1996. On solar forcing of Holocene climate: evidence from Scandinavia. The Holocene 6:359365.CrossRefGoogle Scholar
Lauritzen, S.-E. and Lundberg, J., 1999. Calibration of the speleothem delta function: an absolute temperature record for the Holocene in northern Norway. The Holocene 9:659669.CrossRefGoogle Scholar
Macklin, M.G., Bonsall, C., Fay, M. Davies and Robinson, M.R., 2000. Human-environment interactions during the Holocene: new data and interpretations from the Oban area, Argyll, Scotland. The Holocene 10:109121.CrossRefGoogle Scholar
McVean, D.N., and Ratcliffe, D.A., 1962. Plant Communities of the Scottish Highlands. London: HMSO Nature Conservancy.Google Scholar
Madsen, T., 1986. Where did all the hunters go? – An assessment of an epoch-making episode in Danish prehistory. Journal of Danish Archaeology 5:229239.CrossRefGoogle Scholar
Mays, S., 1998. The Archaeology of Human Bones. London: Routledge.Google Scholar
Moore, Jenny, 1996. Damp squib: how to fire a major deciduous forest. In Pollard, T. and Morrison, A. (eds), The Early Prehistory of Scotland: 6273. Edinburgh: Edinburgh University Press.CrossRefGoogle Scholar
O'Brien, S.R., Mayewski, P.A., Meeker, L.D., Meese, D.A., Twickler, M.S. and Whitlow, S.I., 1995. Complexity of Holocene climate as reconstructed from a Greenland ice core. Science 270:19621964.CrossRefGoogle Scholar
Parker, A.G., Goudie, A.S., Anderson, D.E., Robinson, M.A. and Bonsall, C., in press. A review of the mid-Holocene elm decline in the British Isles. Progress in Physical Geography.Google Scholar
Payton, R.W. and Palmer, R., 1990. Soils of the Alnwick and Rothbury District. Silsoe: Memoir of the Soil Survey of Great Britain, Soil Survey and Land Research Centre.Google Scholar
Richards, M.P., 1998. Bone stable isotope analysis: reconstructing the diet of humans. In A. Whittle and M. Wysocki, ‘Parc le Breos Cwm transepted long cairn, Gower, West Glamorgan: date, contents, and context’. Proceedings of the Prehistoric Society 64:165166.Google Scholar
Richards, M.P. and Hedges, R.E.M., 1999. A Neolithic revolution? New evidence of diet in the British Neolithic. Antiquity 73:891897.CrossRefGoogle Scholar
Sarmaja-Korjonen, K. 2001. Correlation of fluctuations in dadoceran planktonic:littoral ratio between three cores from a small lake in southern Finland: Holocene water-level changes. The Holocene 11:5363.CrossRefGoogle Scholar
Schulting, R.J. and Richards, M.P., 2000. The use of stable isotopes in studies of subsistence and seasonality in the British Mesolithic. In Young, R. (ed.), Mesolithic Lifeways: Current Research from Britain and Ireland: 5565. Leicester: University of Leicester.Google Scholar
Smith, Melanie A., 1996. The role of vegetation dynamics and human activity in landscape changes through the Holocene in the Lairg area, Sutherland, Scotland. Unpublished , University of London, Royal Holloway College.Google Scholar
Stuiver, M. and Paula, J. Reimer, 1993. Extended 14C database and revised CALIB radiocarbon calibration program. Radiocarbon 35:215230.CrossRefGoogle Scholar
Stuiver, M., Paula, J. Reimer, Bard, E., Beck, J.W., Burr, G.S., Hughen, K.A., Kromer, B., McCormac, G., Van Der Plicht, J. and Spukk, M., 1998. INTCAL 98 radiocarbon age calibration, 24,000–0 cal BP. Radiocarbon 40:10411083.CrossRefGoogle Scholar
Tauber, H., 1986. Analysis of stable isotopes in prehistoric populations. In Herrmann, B. (ed.), Innovative Trends in Prehistoric Anthropology: 3138. Berlin: Mitteilungen der Berliner Gesellschaft für Anthropologie, Ethnologie und Urgeschichte 7.Google Scholar
Thomas, J., 1988. Neolithic explanations revisited: the Mesolithic-Neolithic transition in Britain and south Scandinavia. Proceedings of the Prehistoric Society 54:5966.CrossRefGoogle Scholar
Thomas, J. 1991. Rethinking the Neolithic. London: Routledge.Google Scholar
Thomas, J. 2000. Understanding the Neolithic. London: Routledge.Google Scholar
Thomasson, A.J., 1982. Soil and climatic aspects of workability and trafficability. In Proceedings of the 9th International Conference of the Soil Tillage Research Organization, Osijek, Yugoslavia: 551557.Google Scholar
Thomasson, A.J. and Bullock, P., 1976. Pedology and hydrology of some surface water gley soils. Soil Science 119:339348.CrossRefGoogle Scholar
Tipping, R., 1995. Holocene evolution of a lowland Scottish landscape: Kirkpatrick Fleming. Part I, peat- and pollen-stratigraphic evidence for raised moss development and climatic change. The Holocene 5:6981.CrossRefGoogle Scholar
Tipping, R., 1996. Microscopic charcoal records, inferred human activity and climate change in the Mesolithic of northernmost Scotland. In Pollard, T. and Morrison, A. (eds), The Early Prehistory of Scotland: 3961. Edinburgh: Edinburgh University Press.CrossRefGoogle Scholar
Troels-Smith, J., 1960. Ivy, mistletoe and elm: climatic indicators — fodder plants: a contribution to the interpretation of the pollen zone border VII—VIII. Danmarks Geologiske Undersøgelse 2, Series 4:4:132.Google Scholar
Van Zeist, W. and Van Der Spoel-Walvius, M.R., 1980. A palynological study of the late-glacial and the postglacial in the Paris Basin. Palaeohistoria 22:67109.Google Scholar
Zvelebil, M. and Dolukhanov, P., 1991. The transition to farming in eastern and northern Europe. Journal of World Prehistory 5:233278.CrossRefGoogle Scholar
Zvelebil, M. and Rowley-Conwy, P., 1986. Foragers and farmers in Atlantic Europe. In Zvelebil, M. (ed.), Hunters in Transition: 6793. Cambridge: Cambridge University Press.Google Scholar