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1. The Eurasian Modern Pollen Database (EMPD), version 2

Author

Davis, B, Chevalier, M, Sommer, P, Carter, V, Finsinger, W, Mauri, A, Phelps, L, Zanon, M, Abegglen, R, Akesson, C, Alba-Sanchez, F, Scott Anderson, R, Antipina, T, Atanassova, J, Beer, R, Belyanina, N, Blyakharchuk, T, Borisova, O, Bozilova, E, Bukreeva, G, Jane Bunting, M, Clo, E, Colombaroli, D, Combourieu-Nebout, N, Desprat, S, Di Rita, F, Djamali, M, Edwards, K, Fall, P, Feurdean, A, Fletcher, W, Florenzano, A, Furlanetto, G, Gaceur, E, Galimov, A, Galka, M, Garcia-Moreiras, I, Giesecke, T, Grindean, R, Guido, M, Gvozdeva, I, Herzschuh, U, Hjelle, K, Ivanov, S, Jahns, S, Jankovska, V, Jimenez-Moreno, G, Karpinska-Kolaczek, M, Kitaba, I, Kolaczek, P, Lapteva, E, Latalowa, M, Lebreton, V, Leroy, S, Leydet, M, Lopatina, D, Lopez-Saez, J, Lotter, A, Magri, D, Marinova, E, Matthias, I, Mavridou, A, Mercuri, A, Mesa-Fernandez, J, Mikishin, Y, Milecka, K, Montanari, C, Morales-Molino, C, Mrotzek, A, Sobrino, C, Naidina, O, Nakagawa, T, Nielsen, A, Novenko, E, Panajiotidis, S, Panova, N, Papadopoulou, M, Pardoe, H, Pedziszewska, A, Petrenko, T, Ramos-Roman, M, Ravazzi, C, Rosch, M, Ryabogina, N, Ruiz, S, Sakari Salonen, J, Sapelko, T, Schofield, J, Seppa, H, Shumilovskikh, L, Stivrins, N, Stojakowits, P, Svitavska, H, Swieta-Musznicka, J, Tantau, I, Tinner, W, Tobolski, K, Tonkov, S, Tsakiridou, M, Valsecchi, V, Zanina, O, Zimny, M, Davis B. A. S., Chevalier M., Sommer P., Carter V. A., Finsinger W., Mauri A., Phelps L. N., Zanon M., Abegglen R., Akesson C. M., Alba-Sanchez F., Scott Anderson R., Antipina T. G., Atanassova J. R., Beer R., Belyanina N. I., Blyakharchuk T. A., Borisova O. K., Bozilova E., Bukreeva G., Jane Bunting M., Clo E., Colombaroli D., Combourieu-Nebout N., Desprat S., Di Rita F., Djamali M., Edwards K. J., Fall P. L., Feurdean A., Fletcher W., Florenzano A., Furlanetto G., Gaceur E., Galimov A. T., Galka M., Garcia-Moreiras I., Giesecke T., Grindean R., Guido M. A., Gvozdeva I. G., Herzschuh U., Hjelle K. L., Ivanov S., Jahns S., Jankovska V., Jimenez-Moreno G., Karpinska-Kolaczek M., Kitaba I., Kolaczek P., Lapteva E. G., Latalowa M., Lebreton V., Leroy S., Leydet M., Lopatina D. A., Lopez-Saez J. A., Lotter A. F., Magri D., Marinova E., Matthias I., Mavridou A., Mercuri A. M., Mesa-Fernandez J. M., Mikishin Y. A., Milecka K., Montanari C., Morales-Molino C., Mrotzek A., Sobrino C. M., Naidina O. D., Nakagawa T., Nielsen A. B., Novenko E. Y., Panajiotidis S., Panova N. K., Papadopoulou M., Pardoe H. S., Pedziszewska A., Petrenko T. I., Ramos-Roman M. J., Ravazzi C., Rosch M., Ryabogina N., Ruiz S. S., Sakari Salonen J., Sapelko T. V., Schofield J. E., Seppa H., Shumilovskikh L., Stivrins N., Stojakowits P., Svitavska H. S., Swieta-Musznicka J., Tantau I., Tinner W., Tobolski K., Tonkov S., Tsakiridou M., Valsecchi V., Zanina O. G., Zimny M., Davis, B, Chevalier, M, Sommer, P, Carter, V, Finsinger, W, Mauri, A, Phelps, L, Zanon, M, Abegglen, R, Akesson, C, Alba-Sanchez, F, Scott Anderson, R, Antipina, T, Atanassova, J, Beer, R, Belyanina, N, Blyakharchuk, T, Borisova, O, Bozilova, E, Bukreeva, G, Jane Bunting, M, Clo, E, Colombaroli, D, Combourieu-Nebout, N, Desprat, S, Di Rita, F, Djamali, M, Edwards, K, Fall, P, Feurdean, A, Fletcher, W, Florenzano, A, Furlanetto, G, Gaceur, E, Galimov, A, Galka, M, Garcia-Moreiras, I, Giesecke, T, Grindean, R, Guido, M, Gvozdeva, I, Herzschuh, U, Hjelle, K, Ivanov, S, Jahns, S, Jankovska, V, Jimenez-Moreno, G, Karpinska-Kolaczek, M, Kitaba, I, Kolaczek, P, Lapteva, E, Latalowa, M, Lebreton, V, Leroy, S, Leydet, M, Lopatina, D, Lopez-Saez, J, Lotter, A, Magri, D, Marinova, E, Matthias, I, Mavridou, A, Mercuri, A, Mesa-Fernandez, J, Mikishin, Y, Milecka, K, Montanari, C, Morales-Molino, C, Mrotzek, A, Sobrino, C, Naidina, O, Nakagawa, T, Nielsen, A, Novenko, E, Panajiotidis, S, Panova, N, Papadopoulou, M, Pardoe, H, Pedziszewska, A, Petrenko, T, Ramos-Roman, M, Ravazzi, C, Rosch, M, Ryabogina, N, Ruiz, S, Sakari Salonen, J, Sapelko, T, Schofield, J, Seppa, H, Shumilovskikh, L, Stivrins, N, Stojakowits, P, Svitavska, H, Swieta-Musznicka, J, Tantau, I, Tinner, W, Tobolski, K, Tonkov, S, Tsakiridou, M, Valsecchi, V, Zanina, O, Zimny, M, Davis B. A. S., Chevalier M., Sommer P., Carter V. A., Finsinger W., Mauri A., Phelps L. N., Zanon M., Abegglen R., Akesson C. M., Alba-Sanchez F., Scott Anderson R., Antipina T. G., Atanassova J. R., Beer R., Belyanina N. I., Blyakharchuk T. A., Borisova O. K., Bozilova E., Bukreeva G., Jane Bunting M., Clo E., Colombaroli D., Combourieu-Nebout N., Desprat S., Di Rita F., Djamali M., Edwards K. J., Fall P. L., Feurdean A., Fletcher W., Florenzano A., Furlanetto G., Gaceur E., Galimov A. T., Galka M., Garcia-Moreiras I., Giesecke T., Grindean R., Guido M. A., Gvozdeva I. G., Herzschuh U., Hjelle K. L., Ivanov S., Jahns S., Jankovska V., Jimenez-Moreno G., Karpinska-Kolaczek M., Kitaba I., Kolaczek P., Lapteva E. G., Latalowa M., Lebreton V., Leroy S., Leydet M., Lopatina D. A., Lopez-Saez J. A., Lotter A. F., Magri D., Marinova E., Matthias I., Mavridou A., Mercuri A. M., Mesa-Fernandez J. M., Mikishin Y. A., Milecka K., Montanari C., Morales-Molino C., Mrotzek A., Sobrino C. M., Naidina O. D., Nakagawa T., Nielsen A. B., Novenko E. Y., Panajiotidis S., Panova N. K., Papadopoulou M., Pardoe H. S., Pedziszewska A., Petrenko T. I., Ramos-Roman M. J., Ravazzi C., Rosch M., Ryabogina N., Ruiz S. S., Sakari Salonen J., Sapelko T. V., Schofield J. E., Seppa H., Shumilovskikh L., Stivrins N., Stojakowits P., Svitavska H. S., Swieta-Musznicka J., Tantau I., Tinner W., Tobolski K., Tonkov S., Tsakiridou M., Valsecchi V., Zanina O. G., and Zimny M.

Abstract

The Eurasian (née European) Modern Pollen Database (EMPD) was established in 2013 to provide a public database of high-quality modern pollen surface samples to help support studies of past climate, land cover, and land use using fossil pollen. The EMPD is part of, and complementary to, the European Pollen Database (EPD) which contains data on fossil pollen found in Late Quaternary sedimentary archives throughout the Eurasian region. The EPD is in turn part of the rapidly growing Neotoma database, which is now the primary home for global palaeoecological data. This paper describes version 2 of the EMPD in which the number of samples held in the database has been increased by 60 % from 4826 to 8134. Much of the improvement in data coverage has come from northern Asia, and the database has consequently been renamed the Eurasian Modern Pollen Database to reflect this geographical enlargement. The EMPD can be viewed online using a dedicated map-based viewer at https://empd2.github.io and downloaded in a variety of file formats at https://doi.pangaea.de/10.1594/PANGAEA.909130 (Chevalier et al., 2019).

Published
2020

2. Pollen-derived biomes in the Eastern Mediterranean–Black Sea–Caspian-Corridor

Author

Marinova, E. Harrison, S.P. Bragg, F. Connor, S. de Laet, V. Leroy, S.A.G. Mudie, P. Atanassova, J. Bozilova, E. Caner, H. Cordova, C. Djamali, M. Filipova-Marinova, M. Gerasimenko, N. Jahns, S. Kouli, K. Kotthoff, U. Kvavadze, E. Lazarova, M. Novenko, E. Ramezani, E. Röpke, A. Shumilovskikh, L. Tanţǎu, I. Tonkov, S.

Abstract

Aim: To evaluate the biomization technique for reconstructing past vegetation in the Eastern Mediterranean–Black Sea–Caspian-Corridor using an extensive modern pollen data set and comparing reconstructions to potential vegetation and observed land cover data. Location: The region between 28–48°N and 22–62°E. Methods: We apply the biomization technique to 1,387 modern pollen samples, representing 1,107 entities, to reconstruct the distribution of 13 broad vegetation categories (biomes). We assess the results using estimates of potential natural vegetation from the European Vegetation Map and the Physico-Geographic Atlas of the World. We test whether anthropogenic disturbance affects reconstruction quality using land use information from the Global Land Cover data set. Results: The biomization scheme successfully predicts the broadscale patterns of vegetation across the region, including changes with elevation. The technique discriminates deserts from shrublands, the prevalence of woodlands in moister lowland sites, and the presence of temperate and mixed forests at higher elevations. Quantitative assessment of the reconstructions is less satisfactory: the biome is predicted correctly at 44% of the sites in Europe and 33% of the sites overall. The low success rate is not a reflection of anthropogenic impacts: only 33% of the samples are correctly assigned after the removal of sites in anthropogenically altered environments. Open vegetation is less successfully predicted (33%) than forest types (73%), reflecting the under-representation of herbaceous taxa in pollen assemblages and the impact of long-distance pollen transport into open environments. Samples from small basins (

Published
2018

3. Pollen-derived biomes in the Eastern Mediterranean-Black Sea-Caspian-Corridor

Author

Marinova, E, Harrison, SP, Bragg, F, Connor, S, de Laet, V, Leroy, SAG, Mudie, P, Atanassova, J, Bozilova, E, Caner, H, Cordova, C, Djamali, M, Filipova-Marinova, M, Gerasimenko, N, Jahns, S, Kouli, K, Kotthoff, U, Kvavadze, E, Lazarova, M, Novenko, E, Ramezani, E, Roepke, A, Shumilovskikh, L, Tantau, I, Tonkov, S, Marinova, E, Harrison, SP, Bragg, F, Connor, S, de Laet, V, Leroy, SAG, Mudie, P, Atanassova, J, Bozilova, E, Caner, H, Cordova, C, Djamali, M, Filipova-Marinova, M, Gerasimenko, N, Jahns, S, Kouli, K, Kotthoff, U, Kvavadze, E, Lazarova, M, Novenko, E, Ramezani, E, Roepke, A, Shumilovskikh, L, Tantau, I, and Tonkov, S

Abstract

AIM: To evaluate the biomization technique for reconstructing past vegetation in the Eastern Mediterraneanâ Black Seaâ Caspianâ Corridor using an extensive modern pollen data set and comparing reconstructions to potential vegetation and observed land cover data. LOCATION: The region between 28â 48°N and 22â 62°E. METHODS: We apply the biomization technique to 1,387 modern pollen samples, representing 1,107 entities, to reconstruct the distribution of 13 broad vegetation categories (biomes). We assess the results using estimates of potential natural vegetation from the European Vegetation Map and the Physicoâ Geographic Atlas of the World. We test whether anthropogenic disturbance affects reconstruction quality using land use information from the Global Land Cover data set. RESULTS: The biomization scheme successfully predicts the broadscale patterns of vegetation across the region, including changes with elevation. The technique discriminates deserts from shrublands, the prevalence of woodlands in moister lowland sites, and the presence of temperate and mixed forests at higher elevations. Quantitative assessment of the reconstructions is less satisfactory: the biome is predicted correctly at 44% of the sites in Europe and 33% of the sites overall. The low success rate is not a reflection of anthropogenic impacts: only 33% of the samples are correctly assigned after the removal of sites in anthropogenically altered environments. Open vegetation is less successfully predicted (33%) than forest types (73%), reflecting the underâ representation of herbaceous taxa in pollen assemblages and the impact of longâ distance pollen transport into open environments. Samples from small basins (<1 km²) are more likely to be reconstructed accurately, with 58% of the sites in Europe and 66% of all sites correctly predicted, probably because they sample an appropriate pollen source area to reflect regional vegetation patterns in relatively heterogeneous landscapes. While methodol

Published
2018

4. predictability of biomass burning in response to climate changes

Author

Daniau, A. -L, Bartlein, P. J., Harrison, S. P., Prentice, I. C., Brewer, S., Friedlingstein, P., Harrison-Prentice, T. I., Inoue, J., Izumi, K., Marlon, J. R., Mooney, S., Power, M. J., Stevenson, J., Tinner, W., Andric, M., Atanassova, J., Behling, H., Black, M., Blarquez, O., Brown, K. J., Carcaillet, C., Colhoun, E. A., Colombaroli, D., Davis, B. A. S., D'Costa, D., Dodson, J., Dupont, L., Eshetu, Z., Gavin, D. G., Genries, A., Haberle, S., Hallett, D. J., Hope, G., Horn, S. P., Kassa, T. G., Katamura, F., Kennedy, L. M., Kershaw, P., Krivonogov, S., Long, C., Magri, D., Marinova, E., McKenzie, G. M., Moreno, P. I., Moss, P., Neumann, F. H., Norström, Elin, Paitre, C., Rius, D., Roberts, N., Robinson, G. S., Sasaki, N., Scott, L., Takahara, H., Terwilliger, V., Thevenon, F., Turner, R., Valsecchi, V. G., Vanniere, B., Walsh, M., Williams, N., Zhang, Y., Daniau, A. -L, Bartlein, P. J., Harrison, S. P., Prentice, I. C., Brewer, S., Friedlingstein, P., Harrison-Prentice, T. I., Inoue, J., Izumi, K., Marlon, J. R., Mooney, S., Power, M. J., Stevenson, J., Tinner, W., Andric, M., Atanassova, J., Behling, H., Black, M., Blarquez, O., Brown, K. J., Carcaillet, C., Colhoun, E. A., Colombaroli, D., Davis, B. A. S., D'Costa, D., Dodson, J., Dupont, L., Eshetu, Z., Gavin, D. G., Genries, A., Haberle, S., Hallett, D. J., Hope, G., Horn, S. P., Kassa, T. G., Katamura, F., Kennedy, L. M., Kershaw, P., Krivonogov, S., Long, C., Magri, D., Marinova, E., McKenzie, G. M., Moreno, P. I., Moss, P., Neumann, F. H., Norström, Elin, Paitre, C., Rius, D., Roberts, N., Robinson, G. S., Sasaki, N., Scott, L., Takahara, H., Terwilliger, V., Thevenon, F., Turner, R., Valsecchi, V. G., Vanniere, B., Walsh, M., Williams, N., and Zhang, Y.

Abstract

Climate is an important control on biomass burning, but the sensitivity of fire to changes in temperature and moisture balance has not been quantified. We analyze sedimentary charcoal records to show that the changes in fire regime over the past 21,000 yrs are predictable from changes in regional climates. Analyses of paleo-fire data show that fire increases monotonically with changes in temperature and peaks at intermediate moisture levels, and that temperature is quantitatively the most important driver of changes in biomass burning over the past 21,000 yrs. Given that a similar relationship between climate drivers and fire emerges from analyses of the interannual variability in biomass burning shown by remote-sensing observations of month-by-month burnt area between 1996 and 2008, our results signal a serious cause for concern in the face of continuing global warming., AuthorCount:62

Published
2012
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5. Predictability of biomass burning in response to climate changes

Author

Daniau, A. -L., Bartlein, P. J., Harrison, S. P., Prentice, I. C., Brewer, S., Friedlingstein, P., Harrison-Prentice, T. I., Inoue, J., Izumi, K., Marlon, J. R., Mooney, S., Power, M. J., Stevenson, J., Tinner, W., Andric, M., Atanassova, J., Behling, H., Black, M., Blarquez, O., Brown, K. J., Carcaillet, C., Colhoun, E. A., Colombaroli, D., Davis, B. A. S., D'Costa, D., Dodson, J., Dupont, L., Eshetu, Z., Gavin, D. G., Genries, A., Haberle, S., Hallett, D. J., Hope, G., Horn, S. P., Kassa, T. G., Katamura, F., Kennedy, L. M., Kershaw, P., Krivonogov, S., Long, C., Magri, D., Marinova, E., McKenzie, G. M., Moreno, P. I., Moss, P., Neumann, F. H., Norstrom, E., Paitre, C., Rius, D., Roberts, N., Robinson, G. S., Sasaki, N., Scott, L., Takahara, H., Terwilliger, V., Thevenon, F., Turner, R., Valsecchi, V. G., Vanniere, B., Walsh, M., Williams, N., Zhang, Y., Daniau, A. -L., Bartlein, P. J., Harrison, S. P., Prentice, I. C., Brewer, S., Friedlingstein, P., Harrison-Prentice, T. I., Inoue, J., Izumi, K., Marlon, J. R., Mooney, S., Power, M. J., Stevenson, J., Tinner, W., Andric, M., Atanassova, J., Behling, H., Black, M., Blarquez, O., Brown, K. J., Carcaillet, C., Colhoun, E. A., Colombaroli, D., Davis, B. A. S., D'Costa, D., Dodson, J., Dupont, L., Eshetu, Z., Gavin, D. G., Genries, A., Haberle, S., Hallett, D. J., Hope, G., Horn, S. P., Kassa, T. G., Katamura, F., Kennedy, L. M., Kershaw, P., Krivonogov, S., Long, C., Magri, D., Marinova, E., McKenzie, G. M., Moreno, P. I., Moss, P., Neumann, F. H., Norstrom, E., Paitre, C., Rius, D., Roberts, N., Robinson, G. S., Sasaki, N., Scott, L., Takahara, H., Terwilliger, V., Thevenon, F., Turner, R., Valsecchi, V. G., Vanniere, B., Walsh, M., Williams, N., and Zhang, Y.

Abstract

Climate is an important control on biomass burning, but the sensitivity of fire to changes in temperature and moisture balance has not been quantified. We analyze sedimentary charcoal records to show that the changes in fire regime over the past 21,000 yrs are predictable from changes in regional climates. Analyses of paleo-fire data show that fire increases monotonically with changes in temperature and peaks at intermediate moisture levels, and that temperature is quantitatively the most important driver of changes in biomass burning over the past 21,000 yrs. Given that a similar relationship between climate drivers and fire emerges from analyses of the interannual variability in biomass burning shown by remote-sensing observations of month-by-month burnt area between 1996 and 2008, our results signal a serious cause for concern in the face of continuing global warming.

Published
2012

6. Predictability of biomass burning in response to climate changes

Author

Daniau, A.‐L., primary, Bartlein, P. J., additional, Harrison, S. P., additional, Prentice, I. C., additional, Brewer, S., additional, Friedlingstein, P., additional, Harrison‐Prentice, T. I., additional, Inoue, J., additional, Izumi, K., additional, Marlon, J. R., additional, Mooney, S., additional, Power, M. J., additional, Stevenson, J., additional, Tinner, W., additional, Andrič, M., additional, Atanassova, J., additional, Behling, H., additional, Black, M., additional, Blarquez, O., additional, Brown, K. J., additional, Carcaillet, C., additional, Colhoun, E. A., additional, Colombaroli, D., additional, Davis, B. A. S., additional, D'Costa, D., additional, Dodson, J., additional, Dupont, L., additional, Eshetu, Z., additional, Gavin, D. G., additional, Genries, A., additional, Haberle, S., additional, Hallett, D. J., additional, Hope, G., additional, Horn, S. P., additional, Kassa, T. G., additional, Katamura, F., additional, Kennedy, L. M., additional, Kershaw, P., additional, Krivonogov, S., additional, Long, C., additional, Magri, D., additional, Marinova, E., additional, McKenzie, G. M., additional, Moreno, P. I., additional, Moss, P., additional, Neumann, F. H., additional, Norström, E., additional, Paitre, C., additional, Rius, D., additional, Roberts, N., additional, Robinson, G. S., additional, Sasaki, N., additional, Scott, L., additional, Takahara, H., additional, Terwilliger, V., additional, Thevenon, F., additional, Turner, R., additional, Valsecchi, V. G., additional, Vannière, B., additional, Walsh, M., additional, Williams, N., additional, and Zhang, Y., additional

Published
2012
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11. Predictability of biomass burning in response to climate changes

Author

Daniau, AL, Bartlein, PJ, Harrison, SP, Prentice, IC, Brewer, S, Friedlingstein, P, Harrison-Prentice, TI, Inoue, J, Izumi, K, Marlon, Mooney, S, Power, MJ, Stevenson, J, Tinner, Willy, Andric, M, Atanassova, J, Behling, H, Black, M, Blarquez, O, Brown, KJ, Carcaillet, C, Colhoun, EA, Colombaroli, D, Davis, BAS, D'Costa, D, Dodson, J, Dupont, L, Eshetu, Z, Gavin, DG, Genries, A, Haberle, S, Hallett, DJ, Hope, G, Horn, SP, Kassa, TG, Katamura, F, Kennedy, LM, Kershaw, P, Krivonogov, S, Long, C, Magri, D, Marinova, E, McKenzie, GM, Moreno, PI, Moss, P, Neumann, FH, Norstrom, E, Paitre, C, Rius, D, Roberts, N, Robinson, GS, Sasaki, N, Scott, L, Takahara, H, Terwilliger, V, Thevenon, F, Turner, R, Valsecchi, VG, Vanniere, B, Walsh, M, Williams, N, and Zhang, Y

Subjects
13. Climate action, 15. Life on land
Abstract

Climate is an important control on biomass burning, but the sensitivity of fire to changes in temperature and moisture balance has not been quantified. We analyze sedimentary charcoal records to show that the changes in fire regime over the past 21,000 yrs are predictable from changes in regional climates. Analyses of paleo- fire data show that fire increases monotonically with changes in temperature and peaks at intermediate moisture levels, and that temperature is quantitatively the most important driver of changes in biomass burning over the past 21,000 yrs. Given that a similar relationship between climate drivers and fire emerges from analyses of the interannual variability in biomass burning shown by remote-sensing observations of month-by-month burnt area between 1996 and 2008, our results signal a serious cause for concern in the face of continuing global warming.

12. The Eurasian Modern Pollen Database (EMPD), version 2

Author

Juliana Atanassova, Christine M. Åkesson, Piotr Kołaczek, Marco Zanon, Kari Loe Hjelle, Lyudmila S. Shumilovskikh, Heikki Seppä, Nathalie Combourieu-Nebout, Vachel A. Carter, James Edward Schofield, Krystyna Milecka, Iria García-Moreiras, Takeshi Nakagawa, Walter Finsinger, Willy Tinner, Castor Muñoz Sobrino, Anne Birgitte Nielsen, José Antonio López-Sáez, Elena Marinova, Philipp Stojakowits, Tatiana G. Antipina, Silvia Sabariego Ruiz, Roman Abegglen, Vlasta Jankovská, Oksana G. Zanina, Mariusz Gałka, Arsenii T. Galimov, Maria Papadopoulou, Manfred Rösch, Kevin J. Edwards, Patricia L. Fall, Basil A. S. Davis, Philipp Sommer, Elissaveta Bozilova, Ulrike Herzschuh, Verushka Valsecchi, Natalia Ryabogina, Ikuko Kitaba, Elena Novenko, Michelle Leydet, Anna Pędziszewska, Nata K. Panova, Almut Mrotzek, Donatella Magri, Eleonora Clo, Isabelle Matthias, R. Scott Anderson, Tatiana Blyakharchuk, Kazimierz Tobolski, Vincent Lebreton, Leanne N. Phelps, Irina G. Gvozdeva, André F. Lotter, Nina I. Belyanina, Assunta Florenzano, William J. Fletcher, Ioan Tantau, Suzanne A.G. Leroy, Roxana Grindean, Normunds Stivrins, Elena G. Lapteva, Francisca Alba-Sánchez, J. Sakari Salonen, Tatiana I. Petrenko, Tatyana V. Sapelko, Angelica Feurdean, Anna Maria Mercuri, Yuri A. Mikishin, G Furlanetto, Susanne Jahns, Cesare Ravazzi, Helena Svobodova Svitavska, Anastasia Mavridou, Carlo Alessandro Montanari, Jose Manuel Mesa-Fernández, Sampson Panajiotidis, Ruth Beer, Stéphanie Desprat, Federico Di Rita, María J. Ramos-Román, Emna Gaceur, Joanna Święta-Musznicka, Małgorzata Latałowa, Thomas Giesecke, Olga K. Borisova, Galina Bukreeva, M. Jane Bunting, Manuel Chevalier, Achille Mauri, Maria Angela Guido, Darya A. Lopatina, César Morales-Molino, Spassimir Tonkov, Marcelina Zimny, Monika Karpińska-Kołaczek, Sergey Ivanov, Gonzalo Jiménez-Moreno, Daniele Colombaroli, Morteza Djamali, Heather S. Pardoe, Olga D. Naidina, Margarita Tsakiridou, Université de Lausanne, Swiss National Science Foundation, López Sáez, José Antonio [0000-0002-3122-2744], Institute of Earth Surface Dynamics [Lausanne], Université de Lausanne = University of Lausanne (UNIL), Institut des Sciences de l'Evolution de Montpellier (UMR ISEM), Centre de Coopération Internationale en Recherche Agronomique pour le Développement (Cirad)-École Pratique des Hautes Études (EPHE), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Montpellier (UM)-Institut de recherche pour le développement [IRD] : UR226-Centre National de la Recherche Scientifique (CNRS), Charles University [Prague] (CU), Lomonosov Moscow State University (MSU), Oeschger Centre for Climate Change Research (OCCR), University of Bern, Histoire naturelle de l'Homme préhistorique (HNHP), Muséum national d'Histoire naturelle (MNHN)-Université de Perpignan Via Domitia (UPVD)-Centre National de la Recherche Scientifique (CNRS), Environnements et Paléoenvironnements OCéaniques (EPOC), Observatoire aquitain des sciences de l'univers (OASU), Université Sciences et Technologies - Bordeaux 1 (UB)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Sciences et Technologies - Bordeaux 1 (UB)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-École Pratique des Hautes Études (EPHE), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Centre National de la Recherche Scientifique (CNRS), Institut méditerranéen de biodiversité et d'écologie marine et continentale (IMBE), Avignon Université (AU)-Aix Marseille Université (AMU)-Institut de recherche pour le développement [IRD] : UMR237-Centre National de la Recherche Scientifique (CNRS), Department of physical chemistry, Uppsala University, Senckenberg biodiversität und klima forschungszentrum (BIK-F), Forschungsinstitut Senckenberg (SGN), Laboratorio di Palinologia e Paleobotanica, Adam Mickiewicz University in Poznań (UAM), Department of Palynology and Climate Dynamics, Georg-August-University = Georg-August-Universität Göttingen, Alfred Wegener Institute for Polar and Marine Research (AWI), Natural History Collections, University of Bergen (UiB)-University of Bergen (UiB), A.F. Ioffe Physical-Technical Institute, Russian Academy of Sciences [Moscow] (RAS), Brandenburgisches Landesamt für Denkmalpflege und Archäologisches Landesmuseum, Universidad de Granada = University of Granada (UGR), Institute of Geoecology and Geoinformation, Department of Plant Ecology, Gdansk University, University of Gdańsk (UG), Laboratoire de Recherche en Sciences Humaines (Lares-Las), Université de Rennes 2 (UR2), Dipartimento di biologia ambientale, Università degli Studi di Roma 'La Sapienza' = Sapienza University [Rome] (UNIROMA), Department of Botany, Sofia University 'St. Kliment Ohridski', NASA Ames Research Center (ARC), Department of Biogeography and Palaeoecology, Institut Méditerranéen d'Ecologie et de Paléoécologie (IMEP), Université Paul Cézanne - Aix-Marseille 3-Université de Provence - Aix-Marseille 1-Avignon Université (AU)-Centre National de la Recherche Scientifique (CNRS), Lund University [Lund], Laboratoire d'Informatique, Systèmes, Traitement de l'Information et de la Connaissance (LISTIC), Université Savoie Mont Blanc (USMB [Université de Savoie] [Université de Chambéry]), CNR-IDPA, Dipartimento di Scienze dell'Ambiente e del Territorio, Università degli Studi di Milano-Bicocca = University of Milano-Bicocca (UNIMIB), Department of Physics and Astronomy [Turku], University of Turku, Helsingin yliopisto = Helsingfors universitet = University of Helsinki, Department of Geography [Riga], Софийски университет = Sofia University, University of Portsmouth, Aix Marseille Université (AMU), Avignon Université (AU), López Sáez, José Antonio, Davis, B, Chevalier, M, Sommer, P, Carter, V, Finsinger, W, Mauri, A, Phelps, L, Zanon, M, Abegglen, R, Akesson, C, Alba-Sanchez, F, Scott Anderson, R, Antipina, T, Atanassova, J, Beer, R, Belyanina, N, Blyakharchuk, T, Borisova, O, Bozilova, E, Bukreeva, G, Jane Bunting, M, Clo, E, Colombaroli, D, Combourieu-Nebout, N, Desprat, S, Di Rita, F, Djamali, M, Edwards, K, Fall, P, Feurdean, A, Fletcher, W, Florenzano, A, Furlanetto, G, Gaceur, E, Galimov, A, Galka, M, Garcia-Moreiras, I, Giesecke, T, Grindean, R, Guido, M, Gvozdeva, I, Herzschuh, U, Hjelle, K, Ivanov, S, Jahns, S, Jankovska, V, Jimenez-Moreno, G, Karpinska-Kolaczek, M, Kitaba, I, Kolaczek, P, Lapteva, E, Latalowa, M, Lebreton, V, Leroy, S, Leydet, M, Lopatina, D, Lopez-Saez, J, Lotter, A, Magri, D, Marinova, E, Matthias, I, Mavridou, A, Mercuri, A, Mesa-Fernandez, J, Mikishin, Y, Milecka, K, Montanari, C, Morales-Molino, C, Mrotzek, A, Sobrino, C, Naidina, O, Nakagawa, T, Nielsen, A, Novenko, E, Panajiotidis, S, Panova, N, Papadopoulou, M, Pardoe, H, Pedziszewska, A, Petrenko, T, Ramos-Roman, M, Ravazzi, C, Rosch, M, Ryabogina, N, Ruiz, S, Sakari Salonen, J, Sapelko, T, Schofield, J, Seppa, H, Shumilovskikh, L, Stivrins, N, Stojakowits, P, Svitavska, H, Swieta-Musznicka, J, Tantau, I, Tinner, W, Tobolski, K, Tonkov, S, Tsakiridou, M, Valsecchi, V, Zanina, O, Zimny, M, University of St Andrews. School of Geography & Sustainable Development, University of St Andrews. Environmental Change Research Group, Department of Geosciences and Geography, Université de Lausanne (UNIL), École pratique des hautes études (EPHE), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Montpellier (UM)-Centre de Coopération Internationale en Recherche Agronomique pour le Développement (Cirad)-Centre National de la Recherche Scientifique (CNRS)-Institut de recherche pour le développement [IRD] : UR226, Department of Botany, Faculty of Science, Charles University, Université Sciences et Technologies - Bordeaux 1-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Sciences et Technologies - Bordeaux 1-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-École pratique des hautes études (EPHE), Georg-August-University [Göttingen], Departamento de Estratigrafía y Paleontología, Universidad de Granada, Universidad de Granada (UGR), Université de Rennes (UNIV-RENNES)-Université de Rennes (UNIV-RENNES), Università degli Studi di Roma 'La Sapienza' = Sapienza University [Rome], Sofia University 'Sv. Kliment Ohridski', Université Paul Cézanne - Aix-Marseille 3-Centre National de la Recherche Scientifique (CNRS)-Avignon Université (AU)-Université de Provence - Aix-Marseille 1, Department of Geology, Lund University, Sölvegatan 12, SE-22362 Lund, Sweden, Università degli Studi di Milano-Bicocca [Milano] (UNIMIB), University of Helsinki, and University of Sofia

Subjects
0106 biological sciences, LAKE CONSTANCE REGION, Palynology Palaeoecology Palaeoclimatology, 010504 meteorology & atmospheric sciences, HUMAN IMPACT, recent pollen deposition, 580 Plants (Botany), medicine.disease_cause, 01 natural sciences, 2417.10 Paleobotánica, [SDV.SA.SF]Life Sciences [q-bio]/Agricultural sciences/Silviculture, forestry, ddc:550, SURFACE POLLEN, SOUTHERN NORWAY, SDG 13 - Climate Action, ComputingMilieux_MISCELLANEOUS, lcsh:Environmental sciences, SDG 15 - Life on Land, lcsh:GE1-350, 0303 health sciences, CLIMATE-CHANGE, GE, APUSENI NATURAL PARK, lcsh:QE1-996.5, Foundation (engineering), European pollen database, [SDV.BV.BOT]Life Sciences [q-bio]/Vegetal Biology/Botanics, [SDV.BIBS]Life Sciences [q-bio]/Quantitative Methods [q-bio.QM], Europe, LAST GLACIAL MAXIMUM, Geography, NORTHERN IBERIAN PLATEAU, pollen, GE Environmental Sciences, 1171 Geosciences, 010506 paleontology, [SDE.MCG]Environmental Sciences/Global Changes, Earth and Planetary Sciences(all), Library science, Climate change, [SDU.STU]Sciences of the Universe [physics]/Earth Sciences, 010603 evolutionary biology, neotoma, 03 medical and health sciences, Eurasian Modern Pollen Database, 2502.05 Paleoclimatología, Pollen, medicine, SIERRA-NEVADA, [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces, environment, 0105 earth and related environmental sciences, 030304 developmental biology, Botánica, HOLOCENE VEGETATION HISTORY, DAS, 15. Life on land, 2416.03 Palinología, [SDE.ES]Environmental Sciences/Environmental and Society, lcsh:Geology, [SDU]Sciences of the Universe [physics], MCP, General Earth and Planetary Sciences, [SDE.BE]Environmental Sciences/Biodiversity and Ecology
Abstract

The Eurasian (née European) Modern Pollen Database (EMPD) was established in 2013 to provide a public database of high-quality modern pollen surface samples to help support studies of past climate, land cover, and land use using fossil pollen. The EMPD is part of, and complementary to, the European Pollen Database (EPD) which contains data on fossil pollen found in Late Quaternary sedimentary archives throughout the Eurasian region. The EPD is in turn part of the rapidly growing Neotoma database, which is now the primary home for global palaeoecological data. This paper describes version 2 of the EMPD in which the number of samples held in the database has been increased by 60% from 4826 to 8134. Much of the improvement in data coverage has come from northern Asia, and the database has consequently been renamed the Eurasian Modern Pollen Database to reflect this geographical enlargement. The EMPD can be viewed online using a dedicated map-based viewer at https://empd2.github.io and downloaded in a variety of file formats at https: //doi.pangaea.de/10.1594/PANGAEA.909130 (Chevalier et al., 2019)., Swiss National Science Foundation (SNSF) 200021_169598, University of Lausanne

Published
2020

13. Pollen and Chemical Content of Beebreads from Serpentine Areas in Albania and Bulgaria.

Author

Pavlova D, Atanassova J, Karadjova I, and Bani A

Subjects
Albania, Animals, Bees, Bulgaria, Food Safety, Soil, Pollen chemistry, Trace Elements analysis
Abstract

Beebread from serpentine localities in Albania and Bulgaria were characterized based on their pollen and chemical element content (macroelements K, Ca, Mg, P and microelements Cd, Co, Cr, Cu, Fe, Mn, Na, Ni, Pb, Zn) aiming to (1) evaluate the effect of serpentine soil on the quality of beebread; (2) compare elemental concentrations in samples from serpentine areas in Albania and Bulgaria; and (3) compare the differences in pollen spectra. Chemical element content was determined using microwave digestion of beebread samples followed by ICP-OES measurements. The analytical procedure developed was validated by added/found method. Analytical figures of merit of analytical method proposed were presented. The melissopalynological analysis was applied for pollen characterization. The results demonstrate clear difference in the pollen spectra between the two sets of samples, confirming differences in local serpentine flora in both countries, but specific pollen type is difficult to be suggested. The pollen content is related to the flowering period, climatic conditions, and bees forage preferences. The samples vary in their elemental concentrations depending on the pollen type and year of collection. The highest average concentrations found for K, Ca, Mg, and P are close to values reported in the literature. However, elevated concentrations observed for Ni, Cr, Mn, and Fe in beebread, especially from Albania, are in line with the serpentine characteristics of studied areas. The concentrations of Cd and Pb for all beebread samples are below permissible limits. The results should be taken into consideration in future specific food safety regulations at national and international level., (© 2021. The Author(s), under exclusive licence to Springer Science+Business Media, LLC part of Springer Nature.)

Published
2022
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14. Characteristics of Honey from Serpentine Area in the Eastern Rhodopes Mt., Bulgaria.

Author

Atanassova J, Pavlova D, Lazarova M, and Yurukova L

Subjects
Bulgaria, Food Analysis, Honey analysis, Metals analysis, Trace Elements analysis
Abstract

Honey samples collected during 2007-2010 from serpentine and non-serpentine localities in the Eastern Rhodopes Mt. (Bulgaria) were characterized on the basis of their pollen content by qualitative melissopalynological analysis and physicochemical composition. Water content, pH, electrical conductivity, macroelements-K, Ca, Mg, P, and microelements-As, Cd, Co, Cr, Cu, Fe, Mn, Na, Ni, Pb, and Zn were determined after the Harmonised Methods of the International Honey Commission and ICP-AES method. The results from serpentine honey samples were compared with data from bee pollen collected from the same serpentine area. Different elements have different concentrations in honey from the same botanical type even collected from the same geographical region, same locality, and same beehive but in different vegetation season. The elements Mg, Mn, Ni, and P contribute mostly for separation of the serpentine honey samples based on measured elemental concentrations and performed principal component analysis. The element concentrations were higher in bee pollen and above the permissible limits for the toxic metals Cd and Pb. No specific indicator plant species was found for identification of the geographical origin of serpentine honey in relation to the forage of bees.

Published
2016
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