Lithalsas; Mineral palsa; Palacoclimate; Pingos; Younger dryas; Belgium
Abstract :
[en] This article summarizes current knowledge about the viviers of the Hautes Fagnes Plateau, Belgium. They are best explained as remnants of isolated, elongate lithalsas and lithalsa plateaus. The ice that constituted them was segregation ice formed not only within the permafrost, but also above it (aggradational ice). The lithalsas formed in discontinuous permafrost. The lack of peat during growth implies an annual average temperature of -5 to -6°C in accordance with a model by Seppälä. Data are summarized from nine cuttings made through vivier ramparts. The stratigraphic evidence, including 14C and the study of volcanic dust and pollen, indicates that these periglacial mounds formed during the Younger Dryas. Forms identical with the viviers of the Hautes Fagnes have been observed in northern subarctic Québec, Canada. They result from melting of lithalsas which exist in this area, where summers are cool and permafrost is discontinuous (annual average temperature between -4 and -6°C; temperature of the warmest month between +9 and +11.5°C). Because such conditions exist in few regions, lithalsas are rare nowadays and are only known in northern Québec and Lapland. Traces of lithalsas that appeared during the Younger Dryas are known only from Ireland, Wales and the Hautes Fagnes. Similar but older forms exist in eastern England and some Holocene forms exist in Lapland. The distribution of the features that appeared during the Younger Dryas fits with the palaeoclimatical reconstruction of Isarin. This permits one to understand why these forms exist only in the British Isles and the Belgian Ardennes, but nowhere else.
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Bibliography
Ahman R. (1976) The structure and morphology of minerogenic palsas in Northern Norway. Biuletyn Peryglacjalny 26:25-31.
Ahman R. Palsar I Nordnorge (Palsas in Northern Norway) , Meddelanden fran Lunds Universitets Geografiska Institution; 1977, 78:156.
Akerman H.J. (1982) Observations on palsas within the continuous permafrost zone in eastern Siberia and in Svalbard. Geografisk Tidsskrift 82:45-51.
Akerman H.J., Malmström B. (1986) Permafrost mounds in the Abisko area, northern Sweden. Geografiska Annaler 68 A(3):155-165.
Allard M., Seguin M. (1987) The Holocene evolution of permafrost near the tree line, on the eastern coast of Hudson Bay (Northern Québec). Canadian Journal of Earth Science 24:2206-2222.
Allard M., Seguin M.K., Lévesque R. (1986) Palsas and mineral permafrost mounds in northern Québec. International Geomorphology , Gardiner V (ed.). Wiley; (PART II):285-309.
Allard M., Caron S., Bégin Y. (1996) Climatic and ecological controls on ice segregation and thermokarst: The case history of a permafrost plateau in Northern Québec. Permafrost and Periglacial Processes 7(3):207-227.
An W., Allard M. (1995) A mathematical approach to modelling palsa formation: Insights on processes and growth conditions. Cold Regions Science and Technology 23:231-244.
Bastin B., Juvigné E., Pissart A., Thorez J. (1974) Etude d'une coupe dégagée à travers un rempart d'une cicatrice de pingo de la Brackvenn. Annales De La Société Géologique De Belgique 97:341-358.
Bouillenne R., Bouillenne M., avec la collaboration de Defossez S., I'Abbé Dubois Ch., Damblon J., Willam A. (1937) Les viviers du plateau de la Baraque Michel. Bulletin De La Société Royale Des Sciences De Liège 12:404-427.
Broecker W.S. (1998) Palcocean circulation during the last deglaciation: A bipolar seesaw?. Paleoceanography 13(2):119-121.
Broecker W.S. (1999) What if the conveyor were to shut down. GSA Today , Reflections on a possible outcome of the great global experiment; 9(1):1-7.
Brown J., Ferrians O.J. Jr., Heginbottom J.A., Mclnikov E.S. Circum-Arctic Map of Permafrost and Ground-Ice Conditions, Circum-Pacific map series -45, US Geological Survey 1/10,000,000; 1997.
Brown R.J.E. (1963) Influence of vegetation on permafrost. Proceedings, First International Conference on Permafrost, 11-15 November 1963 , Lafayette, Indiana National Academy of Sciences-National Research Council: Washington, DC. Publication; 1287:20-25.
Brown R.J.E. (1973) Ground ice as an initiator of landforms in permafrost regions. Third Guelph Symposium on Geomorphology. Research in Polar and Alpine Geomorphology, Proceedings , Geobooks: Norwich; 25-42.
Bryant R.H., Carpenter C.P. (1987) Ramparted ground ice depressions in Britain and Ireland. Periglacial Processes and Landforms in Britain and Ireland , (Boardman J (ed.). Cambridge University Press; 183-190.
Burn C.R. (1988) The development of near-surface ground ice during the Holocene at sites near Mayo, Yukon Territory, Canada. Journal of Quaternary Science 3(1):31-38.
Cailleux A., Taylor J. Cryopédologie. Etude Des Sols Gelés , Actualités scientifiques et industrielles, Expéditions polaires françaises. Missions Paul-Emile-Victor, Hermann et al. éditeurs, Paris; 1954, 220.
Coope G.R. (1985) Etude des coléoptères inclus dans la tourbe découverte dans le rempart d'un vivier de la Konnerzvenn. Hautes Fagnes 179:74.
Coxon P. (1986) A radiocarbon dated early post glacial pollen diagram from a pingo remnant near Millstreet, County Cork. Irish Journal of Earth Science 8:9-20.
Coxon P., O'Callaghan P. (1987) The distribution and age of pingo remnants in Ireland. Periglacial Processes and Landforms in Britain and Ireland , Boardman J (ed.). Cambridge University Press; 195-202.
Damblon F., Bastin B. (1986) Etude paléoécologique d'une lentille tourbeuse ensevelie dens le rempart d'une palse de la Konnerzvenn (Hautes Fagnes, Belgique). Bull. Soc. Roy. Bot. Belge 120:20-29.
Dever L., Hillaire-Marcel C., Fontes J.C.H. (1984) Composition isotopique, géochimie et genèse de la glace en lentilles (palsen) dans les tourbières du Nouveau-Québec (Canada). Journal of Hydrology 71:107-130.
Dionne J.C. (1978) Formes et phénomènes périglaciaires en Jamésie, Québec subarctique. Géographie Physique Et Quaternaire 32(3):187-247.
Evseev V.P. (1973) Monticules de boursouflement de migration. Proceedings, Second International Conference on Permafrost, Yakutsk 2:98-102.
Florschutz F., van Oye E. (1938) Over de ouderdomsbepaling van het 'vijvers' op het Plateau van het belgisch Hoogveen. Tijdschrift Kon. Acad. Aardrijskundige Genootschap 55:454-461.
Florschutz F., van Oye E. (1939) Recherches analytiques de pollen dans la région des Hautes Fagnes (Belgique). Biol. Jaarboek Dodonaea 6:227-233.
Forsgren B. (1968) Studies on palsas in Finland, Norway and Sweden, 1964-1966. Biuletyn Peryglacjalny 17:117-123.
Fortier R., Lévesque R., Seguin M.K., Allard M. (1991) Caractérisation du pergélisol de buttes cryogènes à l'aide de diagraphies électriques au Nunavik, Québec. Permafrost and Periglacial Processes 2:79-93.
Fraser J.K. (1956) Physiographic notes on features in the Mackenzie Delta area. The Canadian Geographer 8:18-23.
French H.M. The Periglacial Environment , 2nd edn. Longman; 1996, 341.
Gurney S.D. (1995) A reassessment of the relict pleistocene 'pingos' of west Wales: Hydraulic pingos or mineral palsas?. Quaternary Newsletter 77:6-16.
Hajdas I., Ivy-ochs S., Bonani G., Lotter A., Zolitschka B., Schlüchter C. (1995) Radiocarbon age of the Laacher See tephra: 11230 ± 40 BP. Radiocarbon 37(2):149-154.
Harris S.H. (1993) Palsa-like mounds developed in a mineral substrate, Fox Lake, Yukon Territory. Proceedings, Sixth International Conference on Permafrost, 5-9 July 1993 , Beijing, China South China University of Technology; 1:238-243.
Hirakawa K. (1986) Development of a palsa bog in central highland, Iceland. Geographical Reports of Tokyo Metropolitan University 21:111-122.
Holmes G.W., Hopkins D.M., Foster H. (1968) Pingos in central Alaska. Geological Survey Bulletin , Washington; 1241(H).
Hughes O.L. (1969) Distribution of open-system pingos in central Yukon Territory with respect to glacial limits. Geological Survey of Canada Paper 69:8.
Isarin R.F.B. The Climate in North-Western Europe during the Younger Dryas. A Comparison of Multi-Proxy Climate Reconstructions With Simulation Experiments , Drukkerij Elinkwijk: Utrecht; 1997, 160.
Isarin R.F.B. (1997) Permafrost distribution and temperatures in Europe during the Younger dryas. Permafrost and Periglacial Processes 8(3):313-333.
Isarin R.F.B., Bohncke S.J.P. (1999) Mean July temperatures during the younger dryas in Northwestern and Central Europe as inferred from climate indicator plant species. Quaternary Research 51:158-173.
Iversen J. (1944) Viscum, Hedera and Ilex as climate indicators. Geologiska Föreningens in Stockholm Förhandlingar 66:463-483.
Juvigné E. (1983) Two differents volcanic ash falls of Alleröd age in high Belgium. Geologie En Mijnbouw 62:545-549.
Juvigné E. Contribution à La Tephrostratigraphie Du Quaternaire Et Son Application à La Géomorphologie , Mémoires pour servir à l'explication des cartes géologiques et minières de la Belgique; 1993, 36:66.
Kasse K., Bohncke S. (1992) Weichselian Upper Pleniglacial aeolian ice-cored morphology in the southern Netherlands (Noord-Brabant, Groote Peel). Permafrost and Periglacial Processes 3:327-342.
Lagarec D. (1976) Etude géomorphologique de palses dans la région de Fort Chimo, Nouveau Québec, Canada. Cahiers Géologiques 92:153-163.
Lagaree D. (1982) Cryogenic mounds as indicators of permafrost condition, northern Québec. The Roger J.E. Brown Memorial Volume, Proceedings of the Fourth Canadian Permafrost Conference, Calgary, Alberta. 2-6, March 1981 , French HM (ed.), National Research Council of Canada, Ottawa; 43-48.
Lagerbach R., Rohde L. (1985) Pingos in northernmost Sweden. Geografiska Annaler 67 a(3-4):239-245.
Lundqvist G. (1953) Tillägg till palsfragan. Geol. Fören. Förhandl 73:149-154.
Lundqvist J. (1969) Earth and ice mounds: A terminological discussion. The Periglacial Environment , Péwé TL (ed.). McGill-Queen's University Press, Montreal; 203-215.
Maarlcveld G.C., Van der Toorn J. (1955) Pseudo-sölle in Noord-Nederland. Tijdschrift Van Het Koninklijk Nederlandsch Aardrijskundig Genootschap 72(4):344-360.
Matthews J.A., Dahl S.O., Berrisford M.S., Nesje A. (1997) Cyclic development and thermokarstic degradation of palsas in the mid-Alpine zone at Leirpullan, Doveefjell, Southern Norway. Permafrost and Periglacial Processes 8:107-122.
Meier K.D. (1987) Studien zur periglaziären Landshafts-formung in Finmark (Nordnorwegen). Jahrbuch Des Geographischen Gesellschaft Zu Hannover, Sonderheft 13:298.
Mitchell G.F. (1971) Fossil pingos in the south of Ireland. Nature 230:43-44.
Mitchell G.F. (1973) Fossil pingos in Camaross Townland, Co. Wexford. Irish Royal Academy Proceedings, Section 73 B:269-283.
Muckenhausen E. (1960) Eine besondere Art von Pingos am Hohen Venn/Eifel. Eiszeitalter Und Gegenwart 11:5-11.
Mullenders W., Gullentops F. (1969) The age of the pingos of Belgium. The Periglacial Environment, Past and Present , Péwé TL (ed.). McGill-Queen's University Press: Montreal; 321-335.
Nelson F.E., Hinkel K.M., Outcalt S.I. (1992) Palsa-scale frost mounds. Periglacial Geomorphology: Proceedings of the 22nd Annual Binghamton Symposium in Geomorphology , Dixon JC, Abrahams AD (eds). Wiley: Chichester; 305-325.
Payette S., Filion L. (1993) Origin and significance of subarctic patchy podzolic soils and paleosols. Arctic and Alpine Research 25(4):267-276.
Payette S., Samson H., Lagarec D. (1976) The evolution of permafrost in the taïga and in the forest-tundra, western Québec-Labrador Peninsula. Canadian Journal of Forest Research 6(2):203-220.
Peteet D. (1995) Global younger dryas?. Quaternary International 28:93-104.
Pissart A. (1956) L'origine périglaciaire des viviers des Hautes Fagnes. Annales De La Société Géologique De Belgique 79:119-131.
Pissart A. (1963) Les traces de 'pingos' du Pays de Galles (Grande Bretagne) et du Plateau des Hautes Fagnes (Belgique). Zeitschrift Für Geomorphologie 7(2):147-165.
Pissart A. (1965) Les pingos des hautes Fagnes: Les problèmes de leur genèse. Annales De La Société Géologique De Belgique 88:277-289.
Pissart A. (1967) Les pingos de l'île Prince Patrick (76 °N - 120 °W). Geographical Bulletin 9(3):189-217.
Pissart A. (1974) Les viviers des Hautes Fagnes sont des traces de buttes périglaciaires, mais s'agissait-il vraiment de pingos?. Annales De La Société Géologique De Belgique 97:359-381.
Pissart A. (1976) Les dépôts et la morphologic périglaciaires de la Belgique. Géomorphologie De La Belgique. Hommage Au Professeur P. Macar , Chapter 8, Pissart A (ed.). Laboratoire de Géologie et de Géographie physique, Université de Liège; 115-135.
Pissart A. (1983) Remnants of periglacial mounds in the Hautes Fagnes (Belgium). Geologie En Mijnbouw , Structure and age of the ramparts; 62:551-555.
Pissart A. (1986) Pingos et palses: Un essai de synthèse des connaissances actuelles. Hautes Fagnes 52(3):67-78.
Pissart A. Géomorphologie Périglaciaire-Texte Des Leçons De La Chaire Francqui Belge 1987, Chapter 12, Les indicateurs paléoclimatiques périglaciaires et leurs enseignement. Edition du laboratoire de Géomorphologie et Géologie du Quaternaire de l'Université de Liège; 1987.
Pissart A. (1999) Les traces de buttes cryogènes des Hautes Fagnes. Hautes Fagnes 1999 , Gotes, viviers, pingos, palses, lithalses. Pourquoi la terminologie a-t-elle change; (2):44-50.
Pissart A. (1999) Les viviers des Hautes Fagnes. Hautes Fagnes 1999 , Le mode de formation des palses et des lithalses; (3):75-83.
Pissart A. (1999) Les viviers des Hautes Fagnes. Hautes Fagnes 1999 , Les fouilles réalisées, la formation des remparts, leur âge; (4):99-109.
Pissart A. (2000) Le climat des régions où apparaissent aujourd'hui des lithalses et le climat des Hautes Fagnes pendant le Dernier Dryas. Hautes Fagnes 237:16-25.
Pissart A. (2000) Les traces de lithalses et de pingos connues dans le monde. Hautes Fagnes 239:74-83.
Pissart A., Gangloff P. (1984) Les palses minérales et organiques de la vallée de l'Aveneau, près de Kuujjuaq, Québec subarctique. Géographie Physique Et Quaternaire 38(3):217-228.
Pissart A., Juvigné E. (1980) Genèse et âge d'une trace de butte périglaciaire (pingo ou palse) de la Konnerzvenn (Hautes Fagnes, Belgique). Annales De La Société Géologique De Belgique 103:73-86.
Pissart A., Juvigné E. (1985) L'âge et l'origine des viviers des Hautes Fagnes. Hautes Fagnes 179(3):71.
Pissart A., Juvigné E., Woillard G., Thorez J. (1972) Les cicatrices de pingos de le Brackvenn (Hautes Fagnes). Les Congrès Et Colloques De L'Université De Liège , Compte rendu de l'excursion du 3 juillet 1971; 67:281-294.
Pissart A., Bastin B., Juvigné E. (1975) L'origine des viviers des Hautes Fagnes: Traces de pingos ou de palses?. Hautes Fagnes 1975 (1):9-38.
Pissart A., Harris S., Prick A., Van Vliet-Lanoë B. (1998) La signification paléoclimatique des lithalses (palses minérales). Biuletyn Peryglacjalny 37:141-154.
Ruuhijärvi R. (1960) Uber die regionale Einteilung der nord-finnischen Moore. Ann. Botan. Soc. Vanamo 31(1):360.
Saint-Laurent D., Filion L. (1992) Interprétation paléoécologique des dunes à la limite des arbres, secteur nord-est de la Mer d'Hudson, Québec. Géographie Physique Et Quaternaire 46(2):209-220.
Seppala M. (1972) Pingo-like remnants in the Peltojarvi area of Finnish Lapland. Geografiska Annaler 54 A:38-45.
Seppala M. (1986) The origin of palsas. Geografiska Annaler 68 A(3):141-147.
Seppala M. (1988) Palsas and related forms. Advances in Periglacial Geomorphology , Clark MJ (ed.). Wiley: Chichester; 247-278.
Seppala M. (1994) Snow depth controls palsa growth. Permafrost and Periglacial Processes 5(4):283-288.
Severinghaus J.P., Sowers T., Brook E.J., Alley R.B., Bender M.L. (1998) Timing of abrupt climate change at the end of the Younger Dryas interval from thermally fractionated gases in polar ice. Nature 391:141-146.
Sparks B.W., Williams R.B.G., Bell F.G. (1972) Presumed ground ice depressions in East Anglia. Proceedings of the Royal Society of London, Series A 327:329-343.
Stager J.K. (1956) Progress report on the analysis of the characteristics and distribution of pingos east of the Mackenzie Delta. Canadian Geographer 7:13-20.
Svensson H. (1964) Traces of pingo-like frost mounds. Svensk Geografisk Arsbok 40:93-106.
Svensson H. (1964) Structural observations in the minerogenic core of a palsa. Svensk Geografisk Arsbok 40:137-142.
Svensson H. (1969) A type of circular lake in northernmost Norway. Geografiska Annaler 51 A:1-12.
Tyrtikov A.P. (1959) Permafrost and vegetation. Fondamentals of Geocryology , Chapter 12. Academy of Sciences of the USSR: Moscow (in Russian); 1:399-421.
Van den Bogaard P., Schminke H.U. (1985) Laacher See Tephra: A widespread isochronous late Quaternary tephra layer in central and northern Europe. Geological Society of America Bulletin 96:1554-1571.
Van der Hammen T. H. (1953) Late glacial flora and periglacial phenomena in the Netherlands. Leidse Geol. Meded 17:73-185.
Van Oye L., Florschütz F. (1945) Recherches palynologiques dans les régions des Hautes Fagnes belges. Deuxième partie. Dodonea. Biol. Jaarh 12:307-315.
Warren W.P. (1987) Periglacial periods in Ireland. Periglacial Processes and Landforms in Britain and Ireland , Boardman J (ed.). Cambridge University Press; 101-111.
Washburn A.L. (1983) What is a palsa?. Mathematisch-Physikalische Klasse, Dritte Folge, Mesofirmen Des Reliefs Im Heutingen Periglazialraum. Bericht über Ein Symposium , Poser H, Schunke E (eds). Göttingen: Vandenhoeck & Ruprecht; 35:34-47.
Wastiaux C., Schumacker R., coll Halleux L., Jacqmotte J.M. Rapport Final De La Convention Topographie De Surface Et De Subsurface Des Zones Tourbeuses Des Réserves Naturelles Domaniales Des Hautes Fagnes. Partim 1: Fagne Des Deux-Séries, Ministère de la Région wallonne, Direction des Ressources naturelles et de l'Environnement; 1999.
Watson E. (1971) Remnants of pingos in Wales and the Isle of Man. Geological Journal 7:381-392.
Watson E. (1972) Pingos of Cardiganshire and the latest ice limit. Nature 236:343-344.
Watson E. Mid and North Wales, Inqua-X Congress-Excursion Guide C 9. Geoabstracts: Norwich; 1977.
Watson E., Watson S. (1974) Remains of pingos in the Cletwr Basin, Southwest Wales. Geografiska Annaler 56(3-4):213-225.
Watson E., Watson S. (1972) Investigation of some pingo basins near Aberystwyth, Wales. Proceedings of the 24th International Geological Congress, Montreal , Section; 12:212-223.
Woillard G. (1975) Recherches palynologiques sur le Pléistocène dans l'Est de la Belgique et dans les Vosges lorraines. Acta Geographica Loviensia 14:118.
Worsley P., Gurney S.D., Collins P.E.F. (1995) Late Holocène 'mineral palsas' and associated vegetation pattern: A case study from Lac Hendry, Northern Québec, Canada and significance for European Pleistocene thermokarst. Quaternary Science Reviews 14:172-179.
Wramner P. (1967) Studier av palsmyrar i Laivadalen, Lappland. Teknik Och Natur , (Göteborg); 435-449.
Wramner P. Palslika Bildningar I Mineraljord. Nagra Iakttagelser Fran Taavavuoma, Lappland (Palsa-Like Formation in Mineral Soil. Some Observations from Taavavuoma, Swedish Lapland.) , Göteborgs Universitet Naturgeografiska Institutionen, Guni rapport 1; 1972, 60.
Wramner P. Palsmyrar I Taavavuoma, Lappland (Palsa Bogs in Taavavuoma. Swedish Lapland) , Göteborg Universitets Naturgeografiska Institutionen, Guni rapport 3; 1973, 140.
Yoshikawa K. (1998) The groundwater hydraulics of open system pingos. Proceedings of the Seventh International Conference on Permafrost, 23-27 June 1998 , Lewkowitcz AG, Allard M (ed.). Nordicana; 57:1177-1184.
Zoltaï S.C., Tarnocaï C. (1971) Properties of a wooded palsa in northern Manitoba. Arctic and Alpine Research 3(2):115-129.
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