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Annual pollen traps reveal the complexity of climatic control on pollen productivity in Europe and the Caucasus
Authors:W. O. van der Knaap  Jacqueline F. N. van Leeuwen  Helena Svitavská-Svobodová  Irena A. Pidek  Eliso Kvavadze  Maia Chichinadze  Thomas Giesecke  Bogusław Michał Kaszewski  Florencia Oberli  Laimdota Kalniņa  Heather S. Pardoe  Willy Tinner  Brigitta Ammann
Affiliation:1. Institute of Plant Sciences and Oeschger Centre For Climate Change Research, University of Bern, Altenbergrain 21, 3013, Bern, Switzerland
2. Institute of Botany, Academy of Sciences of the Czech Republic, Castle, 252 43, Pr?honice, Czech Republic
3. Institute of Earth Sciences, Maria Curie-Sk?odowska University in Lublin, al Kra?nicka 2 c/d, 20-718, Lublin, Poland
4. Institute of Paleobiology, National Museum of Georgia, Niagvris 4, 0108, Tbilisi, Georgia
5. Albrecht-von-Haller-Institute for Plant Sciences, Department of Palynology and Climate Dynamics, University of G?ttingen, Untere Karspüle 2, 37073, G?ttingen, Germany
6. Faculty of Geography and Earth Sciences, University of Latvia, Rainis bvld. 19, Riga, 1586, Latvia
7. Department of Biodiversity and Systematic Biology, National Museum Wales, Cathays Park, Cardiff, CF10 3NP, UK
Abstract:Annual PAR (pollen accumulation rates; grains cm?2 year?1) were studied with modified Tauber traps situated in ten regions, in Poland (Roztocze), the Czech Republic (two regions in Krkono?e, two in ?umava), Switzerland (4 regions in the Alps), and Georgia (Lagodekhi). The time-series are 10–16 years long, all ending in 2007. We calculated correlations between pollen data and climate. Pollen data are PAR summarized per region (4–7 traps selected per region) for each pollen type (9–14 per region) using log-transformed, detrended medians. Climate data are monthly temperature and precipitation measured at nearby stations, and their averages over all possible 2- to 6-month windows falling within the 20-month window ending with August, just prior to the yearly pollen-trap collection. Most PAR/climate relationships were found to differ both among pollen types and among regions, the latter probably due to differences among the study regions in the habitats of plant populations. Results shared by a number of regions can be summarized as follows. Summer warmth was found to enhance the following year’s PAR of Picea, Pinus non-cembra, Larix and Fagus. Cool summers, in contrast, increase the PAR of Abies, Alnus viridis and Gramineae in the following year, while wet summers promote PAR of Quercus and Gramineae. Wetness and warmth in general were found to enhance PAR of Salix. Precipitation was found to be more important for PAR of Alnus glutinosa-type than temperature. Weather did not have an impact on the PAR of Gramineae, and possibly of Cyperaceae in the same year. Care is advised when extrapolating our results to PAR in pollen sequences, because there are large errors associated with PAR from sediments, due to the effects of taphonomy and sedimentation and high uncertainty in dating. In addition, in pollen sequences that have decadal to centennial rather than near-annual resolution, plant-interaction effects may easily out-weigh the weather signal.
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