Fire ecology north and south of the Alps since the last ice age

Holocene - Tập 15 Số 8 - Trang 1214-1226 - 2005
Willy Tinner1, Marco Conedera2, Brigitta Ammann1, André F. Lotter3
1Section of Palaeoecology, Institute of Plant Sciences, University of Bern, Altenbergrain 21, CH-3013 Bern, Switzerland
2WSL Swiss Federal Institute for Forest, Snow and Landscape Research, Sottostazione Sud delle Alpi, via Belsoggiorno 22, CH-6504 Bellinzona-Ravecchia, Switzerland
3Laboratory of Palaeobotany and Palynology, Department of Palaeoecology, Utrecht University, Budapestlaan 4, NL-3584 CD Utrecht, The Netherlands

Tóm tắt

Wildfires are very rare in central Europe, which is probably why fire effects on vegetation have been neglected by most central European ecologists and palaeoecologists. Presently, reconstructions of fire history and fire ecology are almost absent. We analysed sediment cores from lakes on the Swiss Plateau (Lobsigensee and Soppensee) for pollen and charcoal to investigate the relationship between vegetation and fire. Microscopic charcoal evidence suggests increasing regional fire frequencies during the Neolithic (7350-4150 cal. BP, 5400-2200 BC) and the subsequent prehistoric epochs at Lobsigensee, whereas at Soppensee burnings remained rather rare until modern times. Neolithic peaks of charcoal at 6200 and 5500 cal. BP (4250 and 3550 BC) coincided with declines of pollen of fire-sensitive taxa at both sites (e.g., Ulmus, Tilia, Hedera, Fagus), suggesting synchronous vegetational responses to fire at regional scales. However, correlation analysis between charcoal and pollen for the period 6600-4400 cal. BP (4650-2650 BC) revealed no significant link between fire and vegetation at Soppensee, whereas at Lobsigensee increases of Corylus and decreases of Fagus were related to fire events. Fire impact on vegetation increased during the subsequent epochs at both sites. Correlation analyses of charcoal and pollen data for the period 4250-1150 cal. BP (2300 BC -AD 800) suggest that fires were intentionally set to disrupt forests and to provide open areas for arable and pastoral farming (e.g., significant positive correlations between charcoal and Cerealia, Plantago lanceolata, Asteroideae). These results are compared with southern European records (Lago di Origlio, Lago di Muzzano), which are situated in particularly fire-prone environments. After the Mesolithic period (I1 200-7350 cal. BP, 9250-5400 BC), charcoal influx was higher by an order of magnitude in the south, suggesting more frequent fires. Neolithic fires caused similar though more pronounced responses of vegetation in the south (e.g., expansions of Corylus). Post-Neolithic land-use practices involving (controlled) burning culminated in both regions at about 2550 cal. BP (c. 600 BC). However, fire-caused disappearances of entire forest communities were confined to the southern sites. Such differences in fire effects among the sites are explained by the dissimilar importance of fire as a result of different climatic conditions and cultural activities. Our results imply that the remaining (fire-sensitive) fragments of central European vegetation north of the Alps are especially endangered by increasing fire frequencies resulting from predicted climatic change.

Từ khóa


Tài liệu tham khảo

Aber, J.D. and Melillo, J.M. 1991: Terrestrial ecosystems. Philadelphia PA: Saunders College Publishing , pp. 429-429

Atlas der Schweiz 1977: Atlas der Schweiz. Wabern-Bern: Eidgen6ssische Landestopographie, Table pp. 20-20

Ammann, B. 1985: Lobsigensee -Late-Glacial and Holocene environments of a lake on the Central Swiss Plateau. Introduction and palynology: vegetational history and core correlation at Lobsigensee (Swiss Plateau). Dissertationes Botanicae 87, 127-35.

Ammann, B. 1989: Late-Quaternary palynology at Lobsigensee. Regional vegetation history and local lake development. Dissertationes Botanicae 137, 1-157.

Anmmann, B., 1996, Palaeoecological events during the last 15000 years: regional syntheses of palaeoecological studies of lakes and mires in Europe, 647

Bahrenberg, G., Giese, E. and Nipper, J. 1985: Statistische Methoden in der Geographie I -Univariate und bivariate Statistik. Stuttgart: Teubner, B.G., 227 pp.

Behre, K.-E., 1981, Pollen et Spores, 23, 225

10.1007/978-94-009-1499-5

10.1016/0033-5894(88)90089-0

10.2307/2260813

Conedera, M., 2003, Bollettino della Societai ticinese di Scienze naturali, 91, 135

Conedera, M., 2000, I Leponti tra mito e realta, 63

10.1007/0-306-47959-1_14

Conedera, M., Marcozzi, M., Jud, B., Mandallaz, D., Chatelain, F., Frank, C., Kienast, F., Ambrosetti, P. and Corti, G. 1996: Incendi boschivi al Sud delle Alpi: passato, presente e possibili sviluppi futuri. Zurich: vdf, Hochschulverlag ETH Zurich, 143 pp.

Conedera, M., Corti, G., Piccini, P., Ryser, D., Guerini, F. and Ceschi, I. 2004: La gestione degli incendi boschivi in Canton Ticino: tentativo di una sintesi storica. Schweizerische Zeitschrift fur Forstwesen 155, 263-77.

Crotti, P. 1993: Spatpalaolithikum und Mesolithikum in der Schweiz: die letzten Jager. In Die Schweiz vom Palaolithikum bis zumfruhen Mittelalter -Palaolithikum und Mesolithikum, 1. Basel: Verlag Schweizerische Gesellschaft fur Urund Fruihgeschichte, 203 43.

10.2307/3235998

Ellenberg, H. 1996: Vegetation Mitteleuropas mit den Alpen in okologischer Sicht. Stuttgart: E. Ulmer , pp. 1096-1096

10.1016/S0031-0182(00)00178-4

10.1007/BF01299802

10.1007/s00334-003-0017-4

Gross-Klee, E. and Maise, C. 1997: Sonne, Vulkane und Seeufersiedlungen. Jahrbuch der Schweizerischen Gesellschaft fur Urund Fruhgeschichte 80, 85-94.

Haaland, S. 2002: Feuer und Flamme fur die Heide. Verlag Bremen: H.M. Hauschild, 160 pp.

Haas, J.N. 1996: Pollen and plant macrofossil evidence of vegetation change at Wallisellen-Langachemoos (Switzerland) during the Mesolithic-Neolithic transition 8500 to 6500 years ago. Dissertationes Botanicae 267, 67.

Haas, J.N. and Hadorn, P. 1998: Die Vegetationsund Kulturlandschaftsgeschichte des Seebachtals von der Mittelsteinzeit bis zum Fruihmittelalter anhand von Pollenanalysen. Archaologie im Thurgau 4, 221-55.

10.1007/BF00209748

Hofmann, C., Conedera, M., Delarze, R., Carraro, G. and Giorgetti, P. 1998: Effets des incendies de foret sur la vegetation au Sud des Alpes Suisses. Mitteilungen der Eidgenossischen Forschungsanstalt Wald, Schnee und Landschaft 73, 1-90.

Huster-Plogmann, H., 1999, Internationale Archaologie -Studia honoraria, 8, 189

Intergovernmental Panel on Climate Change 2001: Climate change 2001: the scientific basis. Contribution of Working Group I to the Third Assessment Report of the Intergovernmental Panel on Climate Change. Cambridge: Cambridge University Press , 881-881 pp.

Kaland, P.E., 1986, Anthropogenic indicators in pollen diagrams, 19

10.1016/S0277-3791(02)00181-6

10.1016/S0304-3800(02)00011-X

10.1007/BF02342718

10.1002/jqs.3390070302

10.1023/A:1007929422169

10.1126/science.1093877

10.1016/0277-3791(91)90030-X

Magny, M., Maise, C., Jacomet, S. and Burga, C. 1998: Klimaschwankungen im Verlauf der Bronzezeit. In Hochuli, S., Niffeler, U. and Rychner, III, V., editors, Die Schweiz vom Paliiolithikum bis zum fruhen Mittelalter. Bronzezeit. Basel: Verlag Schweizerische Gesellschaft fur Urund Friihgeschichte, 135-40.

Maise, C. 1998: Archaoklimatologie -Vom Einfluss nacheiszeitlicher Klimavariabilitat in der Urund Fruhgeschichte. Jahrbuch der Schweizerischen Gesellschaft fur Urund Frahgeschichte 81, 197-35.

Maise, C. 1999: Klima, Umwelt, Landwirtschaft und Ernahrung. In Muller, F., Kaenel, G. and Luscher, IV, G., editors, Die Schweiz vom Palaolithikum bis zum fruhen Mittelalter. Eisenzeit. Basel: Verlag Schweizerische Gesellschaft fur Urund Friihgeschichte, 93-97.

Merkt, J. and Streif, H. 1970: Stechrohr-Bohrgerate fur limnische und marine Lockersedimente. Geologisahes Sahrbach 88, 137-48.

Moore, P.D. , Webb, J.A. and Collinson, M.E. 1991: Pollen analysis. Second edition. London: Blackwell Scientific Publications , 216-216 pp.

Moreno, J.M., 1998, Largeforestfires, 59

10.1177/095968369200200303

10.1007/978-3-642-55828-3_5

Ozenda, P. 1988: Die Vegetation der Alpen. Stuttgart: Gustav Fischer, 353 pp.

10.1023/A:1020968010349

10.1016/S0034-6667(01)00149-X

Reille, M. 1992: Pollen et spores d'Europe et d'Afrique du nord Marseille: Laboratoire de Botanique hostorique et Palynologie, 520 pp.

Reille, M. 1998: Pollen et spores d'Europe et d'Afrique du nord -supplement 2. Marseille: Laboratoire de Botanique Historique et Palynologie, 523 pp.

Richoz, I. 1998: Etude paleoecologique du lac de Seedorf (Fribourg, Suisse). Histoire de la vegetation et du milieu durant l'Holocene: le role de l'homme et du climat. Dissertationes Botanicae 293, 1-177.

Schibler, J., 1997, Anthropozoologica, 25, 553

Stahii, M. 2004: Holozane Feuergeschichte und Feuerokologie des Schweizerischen Nationalparks. Masters Thesis, University of Zurich, Zurich, 100 pp.

Stockli, W.E. 1995: Geschichte des Neolithikums in der Schweiz. In St6ckli, WE., Niffeler, U. and Gross-Klee, E., editors, Die Schweiz vom Palaolithikum bis zum fruhen Mittelalter -Neolithikum. Basel: Verlag Schweizerische Gesellschaft fulr Urund Friihgeschichte, 19-52.

Stuiver, M., Reimer, P.J., Bard, E., Beck, J.W., Burr, G.S., Hughen, K.A., Kromer, B., McCormac, G., Van der Plicht, J. and Spurk, M. 1998: INTCAL98 radiocarbon age calibration, 24000-0 cal BP. Radiocarbon 40, 1041-83.

10.1016/0033-5894(73)90004-5

Tinner, W. 1998: Quartarbotanische Untersuchungen zur Waldbrandokologie des Sottoceneri (Sudschweiz). Ph.D. Thesis, University of Bern, Bern.

10.1007/1-4020-3508-X_14

10.1191/0959683603hl615rp

10.1191/095968398667205430

10.1046/j.1365-2745.1999.00346.x

10.1191/095968300674242447

10.1016/S0277-3791(03)00083-0

10.1016/S0031-0182(00)00088-2

van der Knaap, W.O., 1997, Revue pal6obiologie, Geneve, 16, 433

Whitlock, C., 2001, Tracking environmental change using lake sediments. Terrestrial, algal, and siliceous indicators, 3, 75

Zelenka, A. 2000: Mittlere monatliche Sonneneinstrahlung. In Anstalt, S.M., editor, Klimaatlas der Schweiz. Wabern-Bern: Verlag des Bundesamtes fur Landestopographie, Table 5.6.

10.1016/S0277-3791(02)00182-8