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1

Pollen-based vegetation and climate reconstruction of the Ferdynandovian sequence from Lukow (eastern Poland)

100%
Pidek I. A.
Acta Palaeobotanica
|
2013
|
tom 53
|
nr 1
2

Carpinus betulus pollen accumulation rates in Roztocze (SE Poland) in relation to presence of Carpinus in Ferdynandovian pollen diagrams

100%
Pidek I. A.
Ecological Questions
|
2017
|
tom 26
Carpinus pollen has been recorded in fossil pollen diagrams of different interglacials. In case of the Ferdynandovian pollen sequence it is of particular importance to know if scattered presence of Carpinus pollen at the decline of Ferdynandovian 1 interglacial represents long distance transport of pollen or small isolated Carpinus populations. The study aims to trace the pollen-vegetation relationship in Roztocze (SE Poland) using Tauber-style pollen traps to understand better the pattern of Carpinus pollen dispersal and deposition. High and low pollen deposition years were recorded for Carpinus betulus in the period 1998–2010. Deposition was extremely high in 2002. Average annual pollen accumulation rate was calculated at 1348 grains cm -2 year -1, which was 4.1% of total pollen spectrum. The study confirms that the earlier pollen presence/absence threshold values of about 5% for the presence of Carpinus trees in vegetation (Huntley & Birks 1983) were too high. The pollen monitoring data from Roztocze support the opinion of Ralska-Jasiewiczowa et al. (2004) that low values of about 0.5% may reflect the presence of Carpinus trees in the forests. These data, in comparison to the scattered Carpinus pollen grains in the last part of the Ferdynandovian 1 interglacial seem to indicate that single trees of this genus may nave occurred in the vegetation at the decline of interglacial optimum.
3

Palynostratigraphy and vegetation changes during the early Middle Pleistocene, based on new studies of deposits from Ferdynandow (central eastern Poland)

100%
Pidek I. A.
Acta Palaeobotanica
|
2015
|
tom 55
|
nr 1
4
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Nine-year record of Alnus pollen deposition in the Roztocze Region [SE Poland] with relation to vegetation data

100%
Pidek I. A.
Acta Agrobotanica
|
2007
|
tom 60
|
nr 2
Pollen deposition of alder has been measured at ground level by means of nine modified Tauber traps in different plant communities according to rules of the Pollen Monitoring Programme (http://pmp.oulu.fi). The series of data covers the period 1998-2006. The area under investigation is situated in the Roztocze (surroundings of the Guciów village) within the protective zone of the Roztocze National Park. During nine years of monitoring, significant variations were observed between single years of deposition. The occurrence of peak years (1998, 2001, 2003 and 2006) connected with higher production of Alnus pollen was observed at many pollen monitoring sites, but its relationship with different proportions of alder within the surrounding vegetation seems rather weak. The average value of annual pollen deposition of Alnus for the whole region was calculated at ca. 1370 grains · cm⁻². At the sites situated within the open landscape, pollen influx values ranged from 442 (in 2005) to 6894 (in 1998). It seems that other factors than the proportion of alder within the vegetation control the deposition of Alnus pollen. Long-distance transport and meteorological factors such as wind speed and direction should be taken into account in future studies.
5

Pollen Monitoring Programme - 6th International Meeting [Jurmala, Lotwa, 3-9 czerwca 2007]

63%
Szczuka E., Pidek I. A.
Wiadomości Botaniczne
|
2007
|
tom 51
|
nr 3-4
112-116
6

Conception of the “Unique Ferdynandovian flora” geosite in the Lukow Plain

63%
Pidek I. A., Orlowska A.
Polish Journal of Natural Sciences
|
2017
|
tom 32
|
nr 3
Geosites are places of particular importance for understanding history of the Earth. An example of such a place may be the Łuków site with fossil Ferdynandovian flora. The development of vegetation covers over 140 000 years of Pleistocene in this reference profile. The Łuków profile is one of only a few European complete profiles, in which two Ferdynandovian interglacial climatic optima are recorded. The scientific uniqueness of the Łuków profile was evidenced by numerous papers. However, the site was not analysed in terms of its usefulness for tourism and educational purposes. In order to fill this gap, the method of geosite evaluation has been used to evaluate geotourism potential. The following features of the site were evaluated: scientific value, educational value, state of the object (including threats), and accessibility. The evaluation was qualitative in a scale 1–5. We propose to establish the geosite named “Unique Ferdynandovian flora”. As a result, it will be possible to improve the accessibility and protect this site, as well as promote it as an object of nature tourism.
7

The quick death of a lake: human impact on Lake Tresssee (N Germany) during the last 6000 years – an approach using pollen, Cladocera and sedimentology

51%
Stolz C., Pidek I. A., Suchora M.
Acta Palaeobotanica
|
2020
|
tom 60
|
nr 1
8

Late Saalian and Eemian Interglacial at the Struga site (Garwolin Plain, central Poland)

51%
Bober A., Pidek I. A., Zarski M.
Acta Palaeobotanica
|
2018
|
tom 58
|
nr 2
9

Znaczenie fauny mieczakow ze stanowisk Ortel Krolewski i Rossosz dla stratygrafii czwartorzedu na Podlasiu.

51%
Albrycht A., Pidek I. A., Skompski S.
Przegląd Geologiczny
|
1995
|
tom 43
|
nr 04
321-330
10

Selected geochemical criteria in mire profiles of Poreby Wojslawskie (Sandomierz Basin, Poland SE)

51%
Plak A., Chodorowski J., Pidek I. A., Dobrowolski J.
Polish Journal of Soil Science
|
2015
|
tom 48
|
nr 1
The geochemical analysis of biogenic sediments was used to reconstruct environmental conditions and the impact of human activity from a small mire geo-system in the Sandomierz Basin (Poland SE). Changes in the nature of selected geochemical indicators show a significant impact on the transformation of the mire during the early stages of human activity. It is reflected in the geochemical record by means of a high proportion of heavy metals – cadmium, lead and copper. Evident variability of main geochemical components concentration is also visible in a vertical record of analysed cores. This is a consequence of the sedimentary basin asymmetric configuration and the ensuing variable biogenic sedimentary succession.
11

Indicator value of pollen analysis of spring mire sediments

51%
Pidek I. A., Noryskiewicz B., Dobrowolski R., Osadowski Z.
Acta Societatis Botanicorum Poloniae
|
2010
|
tom 79
|
nr Suppl.1
12
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Annual pollen sums of Alnus in Lublin and Roztocze in the years 2001-2007 against selected meteorological parameters

51%
Kaszewski B. M., Pidek I. A., Piotrowska K., Weryszko-Chmielewska E.
Acta Agrobotanica
|
2008
|
tom 61
|
nr 2
Alder (Alnus Mill.), as an anemophilous species, produces large quantities of easily dispersed pollen. Annual pollen sums recorded in south-eastern Poland (by the volumetric method – Lanzoni trap) and in the area of the village of Guciów in the Central Roztocze region (pollen deposition in Tauber traps) were compared. The height at which the respective trap sites were located as well as local and regional vegetation and the distance from the nearest alder communities differ in both cases, likewise, the climate of these two regions differ. The analysed pollen data series cover the years 1998-2007 in Roztocze and 2001-2007 in Lublin. Large differences have been noted in Alnus pollen deposition values between particular years. Among them, there were observed years of very high annual sums (2001, 2003, 2006), as well as years of very low pollen deposition values in both regions (2002, 2005, 2007). In the period in question, the mean value of annual Alnus pollen count for Lublin was 5372 alder pollen grains in m3 of air, and in Roztocze 1647 grains per cm2 of area. During the seven-year period of monitoring (2001-2007), very similar trends were noted with respect to airborne alder pollen concentrations at both trap sites. Pollen data have been analysed against meteorological factors affecting alder pollen production and deposition. These are total precipitation and mean monthly air temperature in June, July and August in the year preceding pollen emission and the same weather elements in January and February in the year of pollen emission. In Roztocze a statistically signifi cant negative correlation has been found between Alnus pollen annual sums and total precipitation in August in the year preceding alder pollen emission and in February in the year of pollen emission. In both regions, the Spearman’s correlation coeffi cient does not show any statistically signifi cant values when comparing annual Alnus pollen sums with mean monthly temperatures of both January and February and summer months in the year preceding alder pollen emission.
13
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Comparison of pollen concentration of selected tree taxa in Lublin and in the Roztocze region [SA Poland] - the results of three monitoring methods

51%
Pidek I. A., Weryszko-Chmielewska E., Piotrowska K.
Acta Agrobotanica
|
2006
|
tom 59
|
nr 1
Anemophilous trees of Betula and Alnus genera produce very high amount of easily spreading pollen. Carpinus and Fagus discharge lower amount of pollen to the atmosphere. Trees belonging to the mentioned genera occur in vegetation cover of Lublin and the Roztocze region where the comparative studies were carried out in the years 1998-2004. The objective of these studies was to determine pollen concentration of four tree taxa in these study areas located 120 km apart. Annual pollen sums, obtained by means of three methods, were compared in order to find similarity of alternating high and low pollen production by trees in particular years. In the Roztocze region the studies were continued during the mentioned seven years as a part of Pollen Monitoring Programme, which provides multi-annual data for the palaeoecological reconstructions of Quaternary and the interpretations of phenologic-climatic nature. Standard Tauber traps were used in the Roztocze area. In Lublin the gravimetric method was used in the years 1999-2000, and the volumetric method — in the years 2001- 2004. Similar trends were found in Lublin and in the Roztocze region as to the concentrations in the air of pollen of the mentioned four taxa in particular years of the research period. Betula and Alnus discharged the greatest amount of pollen. In 1999 the great similarity of annual pollen sums of three taxa was recorded by means of the gravimetric method in all measurement points. Fagus was an exception, as its pollen concentration was much higher in the Roztocze region than in Lublin. In the case of Carpinus the enhanced pollen concentration was recorded in both study areas in 2002, and the highest concentration of Fagus occurred in 2003. During several years of studies we recorded great similarity of the obtained results in two study areas far apart.
14

New methods applied to interpretations of pollen data in the Holocene - selected examples from the last decade

45%
Pidek I. A., Filbrandt-Czaja A., Noryskiewicz A. M., Noryskiewicz B., Rasanen S.
Ecological Questions
|
2009
|
tom 11
The results of palynological analyses of the Holocene deposits and modern pollen deposition in Poland and Finland are used to illustrate the progress in pollen analysis - the main palaeoecological method. The increased potential of modern palaeoecology for reconstruction of vegetation and for drawing conclusions on other environmental variables (climate, water conditions, landscape, anthropogenic disturbances) is demonstrated. Pollen analysis - develops at present interpretive tools for precise reconstruction of the structure and composition of vegetation and climate conditions. The progress consists in the quantitative presentation of pollenvegetation-climate relationships based on the examination of modern pollen deposition. The application of numerical analyses to pollen data allows correlating pollen spectrum features with the landscape/vegetation type. Special attention is paid to the Holocene vegetation changes of the transitional zone between boreal forest and tundra in the areas subjected to weak anthropopression (e.g. Lapland), which reflect climatic changes. Databases of modern pollen analogues are based on analysis of samples of surface mosses and contents of Tauber traps. These traps are used in Poland in investigations conducted as a part of the Pollen Monitoring Programme (http://pmp.oulu.fi). The correlation of Tauber-trap data with aerobiological ones contributes to understanding of the relationship between pollen production and climate elements. Additionally, the precise C14 dating allows a near-annual resolution in fossil deposits to be obtained more frequently. Due to time scales comprising hundreds of years, pollen analysis can provide means to resolve questions inaccessible for direct observation.
15
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Airborne birch pollen in Poland and Latvia in the light of data obtained from aerobiological monitoring and Tauber traps in relation to mean air temperature

45%
Pidek I. A., Piotrowska K., Kaszewski B. M., Kalnina L., Weryszko-Chmielewska E.
Acta Agrobotanica
|
2009
|
tom 62
|
nr 2
Birch pollen contains allergens belonging to those with the strongest allergenic properties. In order to trace pollen season patterns of this taxon and pollen annual sums at a wider regional scale, cooperation was established with the University of Latvia in Riga (Latvia). A comparison of the results obtained in the years 2003-2008 in Lublin and in Riga, using volumetric samplers, shows that there was a similar trend in the abundance of birch pollen. The highest sums were noted at both sites in 2003. In all the study years, more birch pollen grains were recorded in Lublin than in Riga, on the average by 7110. The birch pollen seasons started earlier in Lublin than in Riga, on the average by 6 days, and they ended earlier in Lublin, on the average by 18 days. In Riga the birch pollen seasons were longer and less abundant than in Lublin. In addition, in both the regions, i.e. in SE Poland (the Roztocze area) and in Latvia (the area of Marupe near Riga, Taurene, Teici and Rucava), there is pollen data series available obtained from annual pollen deposition monitoring conducted using the modified Tauber traps. These pollen counts have been carried out under the Pollen Monitoring Programme (http://pmp.oulu.fi) since 1998. The 11- year data series in Roztocze and the 10-year data series in Latvia allowed the trends in the occurrence of years of abundant or poor birch pollen release to be traced. In Roztocze maximum Betula pollen deposition occurred in the year 2003, in Latvia – in 1999. The absence of a significant correlation between SE Poland and Latvia with regard to the trends in the occurrence of years of abundant Betula pollen deposition induced the authors to seek climatic factors responsible for increased birch pollen production. The analysis of the Spearman’s rank correlation coefficients between annual Betula pollen sums in Roztocze and mean air temperature in June, July and August in the year preceding pollen emission as well as in spring (January-April) of the year of pollen emission showed a statistically significant negative correlation with air temperature in February of the year of pollen emission.
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