Abstract
Discrete reddish-brown, predominantly minerogenic detrital layers along the Holocene, annually laminated sediment sequence of Lake Meerfelder Maar represent extreme runoff events. We conducted detailed microfacies analyses and a high-resolution palynological investigation, focusing on ten detrital layers throughout the Holocene. We studied triad samples taken directly under, in and above the detrital layer. Fagus sylvatica (beech) was a dominant species in the regional forest around Lake Meerfelder Maar after ca. 3,800 years ago. Three detrital layers occurring during the Fagus phase exhibit short-term maxima of ascospores of the parasitic fungus Kretzschmaria deusta. In contrast, the ascospore contents are low in the event layers deposited during the early and middle Holocene. Fagus is a vulnerable host species for Kretzschmaria deusta and the fungus is common on Fagus. Ascospores are formed on the trunk base, and under normal weather conditions, few spores appear outside the forest. We interpret the short peaks in abundance of K. deusta in the event layers as indicators for rainstorms during which material was transported from the forest floor into the lake by strong winds and stormwater runoff. The open beech forest facilitated wind transport of the ascospores. We recommend analysis of fungal spores in lake sediments because fungal records may help to identify extreme weather events, even when such events are not macroscopically visible in the sediment sequence.
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References
Brauer A, Endres C, Zolitschka B, Negendank JFW (2000) AMS radiocarbon and varve chronology from the annually laminated sediment record of Lake Meerfelder Maar, Germany. Radiocarbon 42:335–368
Brauer A, Litt T, Negendank JFW, Zolitschka B (2001) Lateglacial varve chronology and biostratigraphy of lakes Holzmaar and Meerfelder Maar, Germany. Boreas 30:83–88
Cannon PF, Hawksworth DL, Sherwood-Pike MA (1985) The British Ascomycotina. An annotated checklist. Commonw Mycol Inst, Slough, UK, p 302
Cugny C (2011) Apports des microfossiles non-polliniques à l’histoire du pastoralisme sur le versant nord Pyrénéen. Entre référentiels actuels et reconstitution du passé. Thèse de doctorat en Géographie, Laboratoire GEODE Géographie de l’environnement, Université Toulouse-Le Mirail,Toulouse, Volume I: pp 280; Volume II: pp 93
Cugny C, Mazier F, Galop D (2010) Modern and fossil non-pollen palynomorphs from the Basque mountains (western Pyrenees, France): the use of coprophilous fungi to reconstruct pastoral activity. Veg Hist Archaeobot 19:391–408
Faegri K, Iversen J (1989) Textbook of pollen analysis. Wiley, Chichester, UK, p 328
Hepting GH (1971) Diseases of forest and shade trees of the United States. U.S. Dep Agric Forest Serv Agric Handbook 386, pp 658
Innes J, Blackford J, Chambers F (2006) Kretzschmaria deusta and the northwest European Mid-Holocene Ulmus decline at Moel Y Gerddi, North Wales, United Kingdom. Palynol 30:121–132
Jasinski JPP, Payette S (2007) Holocene occurrence of Lophodermium piceae, a black spruce needle endophyte and possible paleoindicator of boreal forest health. Quat Res 67:50–56
Jong SC, Rogers JD (1972) Illustrations and descriptions of conidial states of some Hypoxylon species. Wash Agric Exp Sta Bull 71:1–51
Kubitz B (2000) Die holozäne Vegetations- und Siedlungsgeschichte in der Westeifel am Beispiel eines hochauflösenden Pollendiagrammes aus dem Meerfelder Maar. Dissertationes Botanica 339:1–106
Litt T, Schölzel C, Kühl N, Brauer A (2009) Vegetation and climate history in the Westeifel Volcanic Field (Germany) during the past 11, 000 years based on annually laminated lacustrine maar sediments. Boreas 38:679–690
Martin-Puertas C, Brauer A, Dulski P, Brademann B (2012a) Testing climate-proxy stationarity throughout the Holocene: an example from the varved sediments of Lake Meerfelder Maar (Germany). Quaternary Sci Rev 58:56–65
Martin-Puertas C, Matthes K, Brauer A, Muscheler R, Hansen F, Petrick C, Aldahan A, Possnert G, van Geel B (2012b) Regional atmospheric circulation shifts induced by a grand solar minimum. Nature Geosci 5:397–401
Moore PD, Webb JA, Collinson ME (1991) Pollen Analysis. Blackwell, Oxford, UK, p 216
Overbeck F (1975) Botanisch-geologische Moorkunde. Karl Wachholtz Verlag, Neumünster, p 719
Pals JP, van Geel B, Delfos A (1980) Paleoecological studies in the Klokkeweel bog near Hoogkarspel (prov. of Noord Holland). Rev Palaeobot Palynol 30:371–418
Petrini LE, Müller E (1986) Haupt- und Nebenfruchtformen europäischer Hypoxylon- Arten (Xylariaceae, Sphaeriales) und verwandter Pilze. Mycologia Helv 1:501–627
Rogers JD, Ju Y-M (1998) The genus Kretzschmaria. Mycotaxon 68:345–393
Stebich M (1999) Palynologische Untersuchungen zur Vegetationsgeschichte des Weichsel-Spätglazial und Frühholozän an jährlich geschichteten Sedimenten des Meerfelder Maares (Eifel). Dissertationes Botanicae 320:1–127
van Geel B (1978) A palaeoecological study of Holocene peat bog sections in Germany and the Netherlands. Rev Palaeobot Palynol 25:1–120
van Geel B, Andersen STh (1988) Fossil ascospores of the parasitic fungus Ustulina deusta in Eemian deposits in Denmark. Rev Palaeobot Palynol 56:89–93
van Geel B, Aptroot A (2006) Fossil ascomycetes in Quaternary deposits. Nova Hedwigia 82:313–329
van Geel B, Klink AG, Pals JP, Wiegers J (1986) An Upper Eemian lake deposit from Twente, eastern Netherlands. Rev Palaeobot Palynol 47:31–61
Wilkins WH (1934) Studies in the genus Ustulina with special reference to parasitism. I. Introduction, survey of previous literature and host index. Trans Brit Mycol Soc 18:320–346
Acknowledgments
We thank Dr. K.W. Gams for discussions on fungal ecology and Dr. R. McNeil for permission to use his picture of Kretzschmaria deusta. We are grateful to the coring team for recovering excellent cores and thank the team from Maarmuseum Manderscheid for the logistical support and interest in our work. C. Martin-Puertas acknowledges funding from the Alexander von Humboldt Foundation. This study is a contribution to the climate initiative REKLIM Topic 8 ‘Schnelle Klimaänderungen aus Proxy-Daten’ of the Helmholtz Association. The research of SE is funded by the Netherlands Organisation for Scientific Research (NWO, project number 863.11.009).
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10933_2013_9701_MOESM1_ESM.xls
The complete microfossil record of 30 samples from Meerfelder Maar. Percentages are expressed relative to a pollen sum, including trees, shrubs and upland herbs (XLS 52 kb)
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van Geel, B., Engels, S., Martin-Puertas, C. et al. Ascospores of the parasitic fungus Kretzschmaria deusta as rainstorm indicators during a late Holocene beech-forest phase around lake Meerfelder Maar, Germany. J Paleolimnol 50, 33–40 (2013). https://doi.org/10.1007/s10933-013-9701-2
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DOI: https://doi.org/10.1007/s10933-013-9701-2