16 results on '"Latałowa, M."'
Search Results
2. Białowieża Primeval Forest: a 2000-year interplay of environmental and cultural forces in Europe's best preserved temperate woodland.
- Author
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Latałowa, M., primary, Zimny, M., additional, Jędrzejewska, B., additional, and Samojlik, T., additional
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- 2015
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3. Regional Differentiation in the Dynamics of the Pollen Seasons of Alnus, Corylus and Fraxinus in Poland (Preliminary Results)
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Kasprzyk, I., Uruska, A., Szczepanek, K., Latałowa, M., Gaweł, J., Harmata, K., Myszkowska, D., Stach, A., and Stępalska, D.
- Published
- 2004
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4. The role of pollen in forest throughfall biochemistry
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Verstraeten, A., Gottardini, E., Bruffaerts, N., de Vos, B., Vanguelova, E., Cristofolini, F., Benham, S., Rautio, P., Ukonmaanaho, L., Merilä, P., Saarto, A., Waldner, P., Hendrickx, M., Genouw, G., Roskams, P., Cools, N., Neirynck, J., de Haeck, A., de Bodt, Y., Nussbaumer, A., Neumann, M., Clarke, N., Timmermann, V., Hansen, K., Dietrich, H.P., Nicolas, M., Schmitt, M., Thimonier, A., Meusburger, K., Schüler, S., Kowalska, A., Kasprzyk, I., Borycka, K., Grewling, K., Święta-Musznicka, J., Latałowa, M., Zimny, M., Malkiewicz, M., Vesterdal, L., Thomsen, I.M., Manninger, M., and Titeux, H.
- Subjects
ICP Forests ,Pollen ,Settore BIO/03 - BOTANICA AMBIENTALE E APPLICATA - Published
- 2019
5. Abrupt Alnus population decline at the end of the first millennium CE in Europe:the event ecology, possible causes and implications
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Latałowa, M. (Małgorzata), Święta-Musznicka, J. (Joanna), Słowiński, M. (Michał), Pędziszewska, A. (Anna), Noryśkiewicz, A. (Agnieszka), Zimny, M. (Marcelina), Obremska, M. (Milena), Ott, F. (Florian), Stivrins, N. (Normunds), Pasanen, L. (Leena), Iivonen, L. (Liisa), Holmström, L. (Lasse), Seppä, H. (Heikki), Latałowa, M. (Małgorzata), Święta-Musznicka, J. (Joanna), Słowiński, M. (Michał), Pędziszewska, A. (Anna), Noryśkiewicz, A. (Agnieszka), Zimny, M. (Marcelina), Obremska, M. (Milena), Ott, F. (Florian), Stivrins, N. (Normunds), Pasanen, L. (Leena), Iivonen, L. (Liisa), Holmström, L. (Lasse), and Seppä, H. (Heikki)
- Abstract
The study, based on the examination of 70 published and unpublished pollen profiles from Poland and supplementary data from the surrounding regions, shows that an abrupt, episodic Alnus population decline at the end of the first millennium CE was a much more widespread event than has been previously reported, spanning large areas of the temperate and boreal zones in Europe. The data from Poland suggest that the decline was roughly synchronous and most likely occurred between the 9th and 10th centuries, with strong indications for the 10th century. The pollen data indicate that human impacts were not a major factor in the event. Instead, we hypothesize that one or a series of abrupt climatic shifts that caused floods and droughts at the end of the first millennium CE could have initiated this ecological disturbance, leading to a higher vulnerability of the alder trees to a pathogen outbreak. Following current observations of the decline of alder stands in Europe due to a Phytophthora outbreak, we suggest that a similar process may have occurred in the past. This study provides insight into long-term alder (mainly Alnus glutinosa) dynamics in a condition of climate change and illustrates its great resilience, enabling the natural, successful regeneration of alder stands after critical diebacks if environmental conditions improve. Our finding that the Alnus pollen decline reflects a roughly synchronous event indicates that the decline could be used as an over-regional chronostratigraphic marker for 800–1000 CE in pollen diagrams from a large part of the European Lowland.
- Published
- 2019
6. Regional climate model simulations for Europe at 6 and 0.2 k BP : sensitivity to changes in anthropogenic deforestation
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Strandberg, G., Kjellström, E., Poska, Anneli, Wagner, S., Gaillard, Marie-José, Trondman, Anna-Kari, Mauri, A., Davis, B.A.S., Kaplan, J.O., Birks, H. J. B., Bjune, A.E., Fyfe, R., Giesecke, T., Kalnina, L., Kangur, M., van der Knaap, W.O., Kokfelt, U., Kuneš, P., Latałowa, M., Marquer, Laurent, Mazier, F., Nielsen, Anne Birgitte, Smith, B., Seppä, H., Sugita, S., Strandberg, G., Kjellström, E., Poska, Anneli, Wagner, S., Gaillard, Marie-José, Trondman, Anna-Kari, Mauri, A., Davis, B.A.S., Kaplan, J.O., Birks, H. J. B., Bjune, A.E., Fyfe, R., Giesecke, T., Kalnina, L., Kangur, M., van der Knaap, W.O., Kokfelt, U., Kuneš, P., Latałowa, M., Marquer, Laurent, Mazier, F., Nielsen, Anne Birgitte, Smith, B., Seppä, H., and Sugita, S.
- Abstract
This study aims to evaluate the direct effects of anthropogenic deforestation on simulated climate at two contrasting periods in the Holocene, similar to 6 and similar to 0.2 k BP in Europe. We apply We apply the Rossby Centre regional climate model RCA3, a regional climate model with 50 km spatial resolution, for both time periods, considering three alternative descriptions of the past vegetation: (i) potential natural vegetation (V) simulated by the dynamic vegetation model LPJ-GUESS, (ii) potential vegetation with anthropogenic land use (deforestation) from the HYDE3.1 (History Database of the Global Environment) scenario (V + H3.1), and (iii) potential vegetation with anthropogenic land use from the KK10 scenario (V + KK10). The climate model results show that the simulated effects of deforestation depend on both local/regional climate and vegetation characteristics. At similar to 6 k BP the extent of simulated deforestation in Europe is generally small, but there are areas where deforestation is large enough to produce significant differences in summer temperatures of 0.5-1 degrees C. At similar to 0.2 k BP, extensive deforestation, particularly according to the KK10 model, leads to significant temperature differences in large parts of Europe in both winter and summer. In winter, deforestation leads to lower temperatures because of the differences in albedo between forested and unforested areas, particularly in the snow-covered regions. In summer, deforestation leads to higher temperatures in central and eastern Europe because evapotranspiration from unforested areas is lower than from forests. Summer evaporation is already limited in the southernmost parts of Europe under potential vegetation conditions and, therefore, cannot become much lower. Accordingly, the albedo effect dominates in southern Europe also in summer, which implies that deforestation causes a decrease in temperatures. Differences in summer temperature due to deforestation range from -1 degree
- Published
- 2014
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7. Temporal and spatiotemporal autocorrelation of daily concentrations of Alnus, Betula, and Corylus pollen in Poland
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Nowosad, J., primary, Stach, A., additional, Kasprzyk, I., additional, Grewling, Ł., additional, Latałowa, M., additional, Puc, M., additional, Myszkowska, D., additional, Weryszko- Chmielewska, E., additional, Piotrowska-Weryszko, K., additional, Chłopek, K., additional, Majkowska-Wojciechowska, B., additional, and Uruska, A., additional
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- 2014
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8. Pollen‐based quantitative reconstructions of Holocene regional vegetation cover (plant‐functional types and land‐cover types) in Europe suitable for climate modelling
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Trondman, A.‐K., primary, Gaillard, M.‐J., additional, Mazier, F., additional, Sugita, S., additional, Fyfe, R., additional, Nielsen, A. B., additional, Twiddle, C., additional, Barratt, P., additional, Birks, H. J. B., additional, Bjune, A. E., additional, Björkman, L., additional, Broström, A., additional, Caseldine, C., additional, David, R., additional, Dodson, J., additional, Dörfler, W., additional, Fischer, E., additional, Geel, B., additional, Giesecke, T., additional, Hultberg, T., additional, Kalnina, L., additional, Kangur, M., additional, Knaap, P., additional, Koff, T., additional, Kuneš, P., additional, Lagerås, P., additional, Latałowa, M., additional, Lechterbeck, J., additional, Leroyer, C., additional, Leydet, M., additional, Lindbladh, M., additional, Marquer, L., additional, Mitchell, F. J. G., additional, Odgaard, B. V., additional, Peglar, S. M., additional, Persson, T., additional, Poska, A., additional, Rösch, M., additional, Seppä, H., additional, Veski, S., additional, and Wick, L., additional
- Published
- 2014
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9. Regional climate model simulations for Europe at 6 k and 0.2 k yr BP: sensitivity to changes in anthropogenic deforestation.
- Author
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Strandberg, G., Kjellström, E., Poska, A., Wagner, S., Gaillard, Marie-José, Trondman, Anna-Kari, Mauri, A., Birks, H.J.B., Bjune, A.E., Davis, B. A. S., Fyfe, R., Giesecke, T., Kalnina, L., Kangur, M., Kaplan, J.O., van der Knaap, W.O., Kokfelt, U., Kuneš, P., Latałowa, M., Marquer, Laurent, Mazier, F., Nielsen, A.B., Smith, B., Seppä, H., Sugita, S., Strandberg, G., Kjellström, E., Poska, A., Wagner, S., Gaillard, Marie-José, Trondman, Anna-Kari, Mauri, A., Birks, H.J.B., Bjune, A.E., Davis, B. A. S., Fyfe, R., Giesecke, T., Kalnina, L., Kangur, M., Kaplan, J.O., van der Knaap, W.O., Kokfelt, U., Kuneš, P., Latałowa, M., Marquer, Laurent, Mazier, F., Nielsen, A.B., Smith, B., Seppä, H., and Sugita, S.
- Abstract
This study aims to evaluate the direct effects of anthropogenic deforestation on simulated climate at two contrasting periods in the Holocene, ~6 k BP and ~0.2 k BP in Europe. We apply RCA3, a regional climate model with 50 km spatial resolution, for both time periods, considering three alternative descriptions of the past vegetation: (i) potential natural vegetation (V) simulated by the dynamic vegetation model LPJ-GUESS, (ii) potential vegetation with anthropogenic land cover (deforestation) as simulated by the HYDE model (V + H), and (iii) potential vegetation with anthropogenic land cover as simulated by the KK model (V + K). The KK model estimates are closer to a set of pollen-based reconstructions of vegetation cover than the HYDE model estimates. The climate-model results show that the simulated effects of deforestation depend on both local/regional climate and vegetation characteristics. At ~6 k BP the extent of simulated deforestation in Europe is generally small, but there are areas where deforestation is large enough to produce significant differences in summer temperatures of 0.5–1 °C. At ~0.2 k BP, simulated deforestation is much more extensive than previously assumed, in particular according to the KK model. This leads to significant temperature differences in large parts of Europe in both winter and summer. In winter, deforestation leads to lower temperatures because of the differences in albedo between forested and unforested areas, particularly in the snow-covered regions. In summer, deforestation leads to higher temperatures in central and eastern Europe since evapotranspiration from unforested areas is lower than from forests. Summer evaporation is already limited in the southernmost parts of Europe under potential vegetation conditions and, therefore, cannot become much lower. Accordingly, the albedo effect dominates also in summer, which implies that deforestation causes a decrease in temperatures. Differences in summer temperature due to defore
- Published
- 2013
- Full Text
- View/download PDF
10. Regional climate model simulations for Europe at 6 k and 0.2 k yr BP: sensitivity to changes in anthropogenic deforestation
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Strandberg, G., primary, Kjellström, E., additional, Poska, A., additional, Wagner, S., additional, Gaillard, M.-J., additional, Trondman, A.-K., additional, Mauri, A., additional, Birks, H. J. B., additional, Bjune, A. E., additional, Davis, B. A. S., additional, Fyfe, R., additional, Giesecke, T., additional, Kalnina, L., additional, Kangur, M., additional, Kaplan, J. O., additional, van der Knaap, W. O., additional, Kokfelt, U., additional, Kuneš, P., additional, Latałowa, M., additional, Marquer, L., additional, Mazier, F., additional, Nielsen, A. B., additional, Smith, B., additional, Seppä, H., additional, and Sugita, S., additional
- Published
- 2013
- Full Text
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11. Holocene land-cover reconstructions for studies on land cover-climate feedbacks
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Gaillard, M.-J., primary, Sugita, S., additional, Mazier, F., additional, Trondman, A.-K., additional, Broström, A., additional, Hickler, T., additional, Kaplan, J. O., additional, Kjellström, E., additional, Kokfelt, U., additional, Kuneš, P., additional, Lemmen, C., additional, Miller, P., additional, Olofsson, J., additional, Poska, A., additional, Rundgren, M., additional, Smith, B., additional, Strandberg, G., additional, Fyfe, R., additional, Nielsen, A. B., additional, Alenius, T., additional, Balakauskas, L., additional, Barnekow, L., additional, Birks, H. J. B., additional, Bjune, A., additional, Björkman, L., additional, Giesecke, T., additional, Hjelle, K., additional, Kalnina, L., additional, Kangur, M., additional, van der Knaap, W. O., additional, Koff, T., additional, Lagerås, P., additional, Latałowa, M., additional, Leydet, M., additional, Lechterbeck, J., additional, Lindbladh, M., additional, Odgaard, B., additional, Peglar, S., additional, Segerström, U., additional, von Stedingk, H., additional, and Seppä, H., additional
- Published
- 2010
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12. Regional Differentiation in the Dynamics of the Pollen Seasons of Alnus, Corylusand Fraxinusin Poland (Preliminary Results)
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Kasprzyk, I., Uruska, A., Szczepanek, K., Latałowa, M., Gaweł, J., Harmata, K., Myszkowska, D., Stach, A., and Stępalska, D.
- Abstract
In 1995–1996 a study of pollen concentrations of Corylus, Alnusand Fraxinuswas performed at seven sites in regions of different climatic and natural conditions. The aim of the study was to determine whether regional differences in the course and duration of pollen seasons occur in Poland. The study was performed using a volumetric method. Several phases during the pollen season were defined for each taxon (1, 2.5, 5, 25, 50, 75, 95, 97.5, 99% of annual total) and duration of the pollen seasons was calculated using 98 and 90% methods. Dynamics and duration of the pollen seasons and a start of particular phases of the season were compared among sites. On the basis of the preliminary analysis it could be supposed that regional differences were most evident in the case of Corylus. The pollen season of this taxon started the earliest in Poznań where thermal conditions were most favourable and the latest in Gdańsk, a place at the furthest to the north (χ2, α≤0.05). In montane regions (Zakopane, Rabka) last phases of the season were significant extended (χ2, α≤0.05). Probably it results from secondary pollen deposition and a long-distance transport by montane wind. In case of Fraxinusthe significant regional differences in the start of the pollen season were not found. The study supported that weather conditions have the substantial influence on the start of consecutive phases of the pollen season.
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- 2004
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13. Palaeoenvironmental changes in the area of the Szczecin Lagoon (The south western Baltic Sea) as recorded from diatoms
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Andrzej Witkowski, Latałowa, M., Borówka, R., Gregorowicz, P., Ba̧k, M., Osadczuk, A., Świȩta, J., Lutyńska, M., Wawrzyniak-Wydrowska, B., and Woziński, R.
14. Pollen-based quantitative reconstructions of Holocene regional vegetation cover (plant-functional types and land-cover types) in Europe suitable for climate modelling.
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Trondman AK, Gaillard MJ, Mazier F, Sugita S, Fyfe R, Nielsen AB, Twiddle C, Barratt P, Birks HJ, Bjune AE, Björkman L, Broström A, Caseldine C, David R, Dodson J, Dörfler W, Fischer E, van Geel B, Giesecke T, Hultberg T, Kalnina L, Kangur M, van der Knaap P, Koff T, Kuneš P, Lagerås P, Latałowa M, Lechterbeck J, Leroyer C, Leydet M, Lindbladh M, Marquer L, Mitchell FJ, Odgaard BV, Peglar SM, Persson T, Poska A, Rösch M, Seppä H, Veski S, and Wick L
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- Europe, Pollen, Biodiversity, Climate Change, Models, Theoretical, Plant Dispersal
- Abstract
We present quantitative reconstructions of regional vegetation cover in north-western Europe, western Europe north of the Alps, and eastern Europe for five time windows in the Holocene [around 6k, 3k, 0.5k, 0.2k, and 0.05k calendar years before present (bp)] at a 1° × 1° spatial scale with the objective of producing vegetation descriptions suitable for climate modelling. The REVEALS model was applied on 636 pollen records from lakes and bogs to reconstruct the past cover of 25 plant taxa grouped into 10 plant-functional types and three land-cover types [evergreen trees, summer-green (deciduous) trees, and open land]. The model corrects for some of the biases in pollen percentages by using pollen productivity estimates and fall speeds of pollen, and by applying simple but robust models of pollen dispersal and deposition. The emerging patterns of tree migration and deforestation between 6k bp and modern time in the REVEALS estimates agree with our general understanding of the vegetation history of Europe based on pollen percentages. However, the degree of anthropogenic deforestation (i.e. cover of cultivated and grazing land) at 3k, 0.5k, and 0.2k bp is significantly higher than deduced from pollen percentages. This is also the case at 6k in some parts of Europe, in particular Britain and Ireland. Furthermore, the relationship between summer-green and evergreen trees, and between individual tree taxa, differs significantly when expressed as pollen percentages or as REVEALS estimates of tree cover. For instance, when Pinus is dominant over Picea as pollen percentages, Picea is dominant over Pinus as REVEALS estimates. These differences play a major role in the reconstruction of European landscapes and for the study of land cover-climate interactions, biodiversity and human resources., (© 2014 The Authors Global Change Biology Published by John Wiley & Sons Ltd.)
- Published
- 2015
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15. Genetic consequences of glacial survival and postglacial colonization in Norway spruce: combined analysis of mitochondrial DNA and fossil pollen.
- Author
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Tollefsrud MM, Kissling R, Gugerli F, Johnsen Ø, Skrøppa T, Cheddadi R, Van der Knaap WO, Latałowa M, Terhürne-Berson R, Litt T, Geburek T, Brochmann C, and Sperisen C
- Subjects
- DNA, Mitochondrial genetics, DNA, Plant genetics, Europe, Evolution, Molecular, Genetic Variation, Geography, Minisatellite Repeats, Phylogeny, Principal Component Analysis, Sequence Analysis, DNA, Trees genetics, Fossils, Genetics, Population, Picea genetics, Pollen genetics
- Abstract
Norway spruce (Picea abies [L.] Karst.) is a broadly distributed European conifer tree whose history has been intensively studied by means of fossil records to infer the location of full-glacial refugia and the main routes of postglacial colonization. Here we use recently compiled fossil pollen data as a template to examine how past demographic events have influenced the species' modern genetic diversity. Variation was assessed in the mitochondrial nad1 gene containing two minisatellite regions. Among the 369 populations (4876 trees) assayed, 28 mitochondrial variants were identified. The patterns of population subdivision superimposed on interpolated fossil pollen distributions indicate that survival in separate refugia and postglacial colonization has led to significant structuring of genetic variation in the southern range of the species. The populations in the northern range, on the other hand, showed a shallow genetic structure consistent with the fossil pollen data, suggesting that the vast northern range was colonized from a single refugium. Although the genetic diversity decreased away from the putative refugia, there were large differences between different colonization routes. In the Alps, the diversity decreased over short distances, probably as a result of population bottlenecks caused by the presence of competing tree species. In northern Europe, the diversity was maintained across large areas, corroborating fossil pollen data in suggesting that colonization took place at high population densities. The genetic diversity increased north of the Carpathians, probably as a result of admixture of expanding populations from two separate refugia.
- Published
- 2008
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16. A new scenario for the quaternary history of European beech populations: palaeobotanical evidence and genetic consequences.
- Author
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Magri D, Vendramin GG, Comps B, Dupanloup I, Geburek T, Gömöry D, Latałowa M, Litt T, Paule L, Roure JM, Tantau I, van der Knaap WO, Petit RJ, and de Beaulieu JL
- Subjects
- Climate, DNA, Chloroplast analysis, Europe, Fagus physiology, Genetic Markers, Genetic Variation, Geography, Haplotypes, Pollen growth & development, Fagus genetics, Fossils
- Abstract
Here, palaeobotanical and genetic data for common beech (Fagus sylvatica) in Europe are used to evaluate the genetic consequences of long-term survival in refuge areas and postglacial spread. Four large datasets are presented, including over 400 fossil-pollen sites, 80 plant-macrofossil sites, and 450 and 600 modern beech populations for chloroplast and nuclear markers, respectively. The largely complementary palaeobotanical and genetic data indicate that: (i) beech survived the last glacial period in multiple refuge areas; (ii) the central European refugia were separated from the Mediterranean refugia; (iii) the Mediterranean refuges did not contribute to the colonization of central and northern Europe; (iv) some populations expanded considerably during the postglacial period, while others experienced only a limited expansion; (v) the mountain chains were not geographical barriers for beech but rather facilitated its diffusion; and (vi) the modern genetic diversity was shaped over multiple glacial-interglacial cycles. This scenario differs from many recent treatments of tree phylogeography in Europe that largely focus on the last ice age and the postglacial period to interpret genetic structure and argue that the southern peninsulas (Iberian, Italian and Balkan) were the main source areas for trees in central and northern Europe.
- Published
- 2006
- Full Text
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