Climate-pollen relationships AD 1901–1996 in two small mires near the forest limit in the northern and central Swiss Alps

Bibliographic Data

ID12265193
AuthorsWillem O Van Der Knaap (0000-0002-0179-7440, corresponding author), J F N van Leeuwen (Institute of Plant Sciences, Altenbergrain 21, CH-3013 Bern, Switzerland)
Year2003
Volume13
Issue6
Pages809-828
Publication date2003-09-01
Open AccessYes
TypeARTICLE
VenueThe Holocene (JOURNAL)
Journal identifiersISSN: 0959-6836 • E-ISSN: 1477-0911
PublisherSAGE Publishing (PUBLISHER • US)
DOI10.1191/0959683603hl657rp
OpenAlexW2145864690
LanguageEN
Citations received11
References cited19

Climatic relationships were established in two 210 Pb dated pollen sequences from small mires closely surrounded by forest just below actual forest limits (but about 300 m below potential climatic forest limits) in the northern Swiss Alps (suboceanic in climate; mainly with Picea) and the central Swiss Alps (subcontinental; mainly Pinus cembra and Larix) at annual or near-annual resolution from ad 1901 to 1996. Effects of vegetational succession were removed by splitting the time series into early and late periods and by linear detrending. Both pollen concentrations detrended by the depth-age model and modified percentages (in which counts of dominant pollen types are down-weighted) are correlated by simple linear regression with smoothed climatic parameters with one-and two-year timelags, including average monthly and April/September daylight air temperatures and with seasonal and annual precipitation sums. Results from detrended pollen concentrations suggest that peat accumulation is favoured in the northern-Alpine mire either by early snowmelt or by summer precipitation, but in the central-Alpine mire by increased precipitation and cooler summers, suggesting a position of the northern-Alpine mire near the upper altitudinal limit of peat formation, but of the central-Alpine mire near the lower limit. Results from modified pollen percentages indicate that pollen pro duction by plants growing near their upper altitudinal limit is limited by insufficient warmth in summer, and pollen production by plants growing near their lower altitudinal limit is limited by too-high temperatures. Only weakly significant pollen/climate relationships were found for Pinus cembra and Larix, probably because they experience little climatic stress growing 300 m below the potential climatic forest limit

Biology · Bog · Detrended correspondence analysis · Geography · Mire · Ordination · Peat · Physical geography · Pollen · Precipitation · Environmental Science · Geology and Paleoclimatology Research · Lichen and fungal ecology · Peatlands and Wetlands Ecology · Ecology · Geology

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