34 research outputs found
Recent growth coherence in long-term oak (Quercus spp.) ring width chronologies in the Czech Republic
Oak ring width measurements compiled from 44 sampling sites throughout the territory of the Czech Republic are analysed for the 1655-2013 period. Measurements taken at all these sites are sorted into 10 sub-chronologies on the basis of 5 environmental factors: soil moisture (dry/wet), elevation (low/high), age (young/old), species (Quercus robur or Q. petraea), and geographical position (east/west). Several statistical tests are applied to investigate existing significant differences between chronologies during 1920-2013. Further, the sensitivities of individual sub-chronologies to precipitation are compared. Three tests indicate 5 pairs of very similar sub-chronologies. Moreover, the growth-response to May-July precipitation totals is very much the same in these sub-chronologies. This analysis demonstrates that, even in the absence of certainty about age structure, species composition and some environmental factors in the earlier parts of oak ring width chronologies, the internal homogeneity of the chronology remains essentially unaffected, and the lack of such information does not preclude their use in dendroclimatology
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Updating the Czech Millennia-Long Oak Tree-Ring Width Chronology
In recent years, a millennia-long oak tree-ring width chronology, consisting of 3194 samples from 387 locations, was developed in the Czech Republic. Despite the collection of such a huge dataset, the replication in the 19th Century was very low and the natural oak distribution in the Czech Republic was insufficiently covered by recent samples, especially in Western Bohemia. This study aimed to remove these weaknesses, which have limited the paleoclimatic potential of this dataset, and to determine the number of sapwood rings, which is crucial for dendrochronological dating. Therefore, new recent samples were randomly collected at numerous sawmills along the Czech-German border. The historical material was usually sampled using a Pressler borer from church belfry constructions traditionally made from oak. In total, 252 recent and 90 historical tree-ring width series were incorporated into the chronology. The newly built chronology cumulatively consists of 3536 series, which covers the continuous period of A.D. 352-2014. The resulting tree-ring width record shows robust signal strength and homogeneous coverage of the territory. We show that the number of sapwood rings is constant over time. Therefore, we recommend using an estimate of 5-24 sapwood rings for a more precise dating of historical wood findings in the Czech Republic. © 2017 by The Tree-Ring Society.This item is part of the Tree-Ring Research (formerly Tree-Ring Bulletin) archive. For more information about this peer-reviewed scholarly journal, please email the Editor of Tree-Ring Research at [email protected]
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Calcium availability affects the intrinsic water-use efficiency of temperate forest trees
Acknowledgements: We are thankful to Natálie Pernicová and Inna Roshka, who contributed to preparing plant samples. This study was supported by the Czech Science Foundation (GACR No. 20-19471S) and partly by GACR No. 23-07583S (conceptualization during the project preparational phase). We acknowledge the SustES project—Adaptation strategies for sustainable ecosystem services and food security under adverse environmental conditions (CZ.02.1.01/0.0/0.0/16_019/0000797).AbstractIntrinsic water-use efficiency (iWUE) of trees is an important component of the Earth’s coupled carbon and water cycles. The causes and consequences of long-term changes in iWUE are, however, still poorly understood due to the complex interplay between biotic and abiotic factors. Inspired by the role calcium (Ca) plays in plant transpiration, we explore possible linkages between tree ring-derived iWUE and Ca availability in five central European forest sites that were affected by acidic air pollution. We show that increasing iWUE was directly modulated by acid air pollution in conjunction with soil Ca concentration. Responses of iWUE to rising atmospheric CO2 concentrations accelerated across sites where Ca availability decreased due to soil acidity constraints, regardless of nitrogen and phosphorus availability. The observed association between soil acidity, Ca uptake, and transpiration suggests that Ca biogeochemistry has important, yet unrecognized, implications for the plant physiological upregulation of carbon and water cycles.</jats:p
Pollen percentage thresholds of Abies alba based on 13-year annual records of pollen deposition in modified Tauber traps: perspectives of application to fossil situations
Abies alba (fir), a submontane tree from Central European mountains and uplands, is of special interest for
palaeoecological and palaeoclimate interpretations due to its sensitivity to air and soil humidity. Its present
distribution limit in the uplands of SE Poland is still a matter of debate. In the Holocene fir expanded to
Poland very late, but early fir populations are supposed to occur in the Šumava Mts (Czech Republic). The
study aims: to estimate pollen thresholds for fir presence/absence in Bohemia (Czech Republic) and Poland
on the basis of modified Tauber pollen traps; to use these thresholds for tracing fir presence in two pollen
diagrams from Poland (Słone and Bezedna lakes) in the border zone between the Roztocze region (with fir
forest stands today) and Polesie (where fir has never played an important role); and to investigate how
the percentage presence/absence threshold can be used to trace the occurrence and abundance of fir trees
in the Šumava Mts based on the pollen diagrams of Rokytecká slat' and Mrtvý luh.
The fir pollen thresholds estimated in terms of PAR (pollen accumulation rates or pollen influx) range from
843 (grains cm−2 year−1) (Roztocze) to 61 (Krkonoše) and 49 (Šumava). Percentage thresholds range
from 0.3% in Krkonoše where fir trees are not present within 4 km to 22% in fir-dominated woodland of
the Roztocze, providing evidence of strong underrepresentation of fir in the pollen deposition. Application
of these percentage thresholds to the Słone and Bezedna pollen diagrams indicates that occurrence of fir in
the region is possible from 3.5 cal ky BP onwards, though the evidence is not decisive. In the Šumava, a
low representation of fir pollen (1–2%) reflecting presence of scattered fir trees was detected as early as ca.
7.0 cal ky BP
Spatial and temporal variations in airborne Ambrosia pollen in Europe
We acknowledge support from EU COST Action FA1203 "Sustainable management of Ambrosia artemisiifolia in Europe (SMARTER)". This work was partly financed by the following COST Short Term Scientific Missions: COST-STSM-FA1203-020215-053027 to CT, COST-STSM-FA1203-20573, ECOST-STSM-FA1203-250415-058150. Skjøth is supported by European Commission through a Marie Curie Career Integration Grant (Project ID CIG631745)Unidad de excelencia María de Maeztu MdM-2015-0552The European Commission Cooperation in Science and Technology (COST) Action FA1203 "SMARTER" aims to make recommendations for the sustainable management of Ambrosia across Europe and for monitoring its efficiency and cost-effectiveness. The goal of the present study is to provide a baseline for spatial and temporal variations in airborne Ambrosia pollen in Europe that can be used for the management and evaluation of this noxious plant. The study covers the full range of Ambrosia artemisiifolia L. distribution over Europe (39°N-60°N; 2°W-45°E). Airborne Ambrosia pollen data for the principal flowering period of Ambrosia (August-September) recorded during a 10-year period (2004-2013) were obtained from 242 monitoring sites. The mean sum of daily average airborne Ambrosia pollen and the number of days that Ambrosia pollen was recorded in the air were analysed. The mean and standard deviation (SD) were calculated regardless of the number of years included in the study period, while trends are based on those time series with 8 or more years of data. Trends were considered significant at p < 0.05. There were few significant trends in the magnitude and frequency of atmospheric Ambrosia pollen (only 8% for the mean sum of daily average Ambrosia pollen concentrations and 14% for the mean number of days Ambrosia pollen were recorded in the air). The direction of any trends varied locally and reflected changes in sources of the pollen, either in size or in distance from the monitoring station. Pollen monitoring is important for providing an early warning of the expansion of this invasive and noxious plant