0000000000413501

AUTHOR

Małgorzata Latałowa

Holocene fires in the central European lowlands and the role of humans

International audience; A major debate concerns the questions of when and to what extent humans affected regional landscapes, especially land cover and associated geomorphological dynamics, significantly beyond natural variability. Fire is both, a natural component of many climate zones and ecosystems around the globe and also closely related to human land cover change. Humans clearly affected natural fire regimes and landscapes in the most recent centuries, acting as prime ignition triggers and later fire suppressors, while Holocene trends in sedimentary charcoal have been mainly associated with climatic factors and partly with Neolithic land cover change. However, little is known since wh…

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ESM_Figure_S1_The_results_of_the_SiZer_analyses_of_Alnus_pollen_curves_in_selected_sites_in_Poland – Supplemental material for Abrupt Alnus population decline at the end of the first millennium CE in Europe – The event ecology, possible causes and implications

Supplemental material, ESM_Figure_S1_The_results_of_the_SiZer_analyses_of_Alnus_pollen_curves_in_selected_sites_in_Poland for Abrupt Alnus population decline at the end of the first millennium CE in Europe – The event ecology, possible causes and implications by Małgorzata Latałowa, Joanna Święta-Musznicka, Michał Słowiński, Anna Pędziszewska, Agnieszka M NoryŚkiewicz, Marcelina Zimny, Milena Obremska, Florian Ott, Normunds Stivrins, Leena Pasanen, Liisa Ilvonen, Lasse Holmström and Heikki Seppä in The Holocene

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Latalowa_M_et_al._ESM_Table_S2 – Supplemental material for Abrupt Alnus population decline at the end of the first millennium CE in Europe – The event ecology, possible causes and implications

Supplemental material, Latalowa_M_et_al._ESM_Table_S2 for Abrupt Alnus population decline at the end of the first millennium CE in Europe – The event ecology, possible causes and implications by Małgorzata Latałowa, Joanna Święta-Musznicka, Michał Słowiński, Anna Pędziszewska, Agnieszka M NoryŚkiewicz, Marcelina Zimny, Milena Obremska, Florian Ott, Normunds Stivrins, Leena Pasanen, Liisa Ilvonen, Lasse Holmström and Heikki Seppä in The Holocene

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The Eurasian Modern Pollen Database (EMPD), version 2

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…

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Holocene fire activity during low-natural flammability periods reveals scale-dependent cultural human-fire relationships in Europe

Abstract Fire is a natural component of global biogeochemical cycles and closely related to changes in human land use. Whereas climate-fuel relationships seem to drive both global and subcontinental fire regimes, human-induced fires are prominent mainly on a local scale. Furthermore, the basic assumption that relates humans and fire regimes in terms of population densities, suggesting that few human-induced fires should occur in periods and areas of low population density, is currently debated. Here, we analyze human-fire relationships throughout the Holocene and discuss how and to what extent human-driven fires affected the landscape transformation in the Central European Lowlands (CEL). W…

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Latalowa_M_et_al._ESM_Table_S1 – Supplemental material for Abrupt Alnus population decline at the end of the first millennium CE in Europe – The event ecology, possible causes and implications

Supplemental material, Latalowa_M_et_al._ESM_Table_S1 for Abrupt Alnus population decline at the end of the first millennium CE in Europe – The event ecology, possible causes and implications by Małgorzata Latałowa, Joanna Święta-Musznicka, Michał Słowiński, Anna Pędziszewska, Agnieszka M NoryŚkiewicz, Marcelina Zimny, Milena Obremska, Florian Ott, Normunds Stivrins, Leena Pasanen, Liisa Ilvonen, Lasse Holmström and Heikki Seppä in The Holocene

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Holocene land-cover reconstructions for studies on land cover-climate feedbacks

The major objectives of this paper are: (1) to review the pros and cons of the scenarios of past anthropogenic land cover change (ALCC) developed during the last ten years, (2) to discuss issues related to pollen-based reconstruction of the past land-cover and introduce a new method, REVEALS (Regional Estimates of VEgetation Abundance from Large Sites), to infer long-term records of past land-cover from pollen data, (3) to present a new project (LANDCLIM: LAND cover – CLIMate interactions in NW Europe during the Holocene) currently underway, and show preliminary results of REVEALS reconstructions of the regional land-cover in the Czech Republic for five selected time windows of the Holocene…

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Regional climate model simulations for Europe at 6 and 0.2 k BP: sensitivity to changes in anthropogenic deforestation

International audience; This study aims to evaluate the direct effects of anthropogenic deforestation on simulated climate at two contrasting periods in the Holocene, ∼ 6 and ∼ 0.2 k BP in Eu-rope. 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 anthro-pogenic land use (deforestation) from the HYDE3.1 (History Database of the Global Environment) scenario (V + H3.1), and (iii) potential vegetation with anthropogenic land …

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Comparing pollen spectra from modified Tauber traps and moss samples: examples from a selection of woodlands across Europe

This paper compares pollen spectra derived from modified Tauber traps and moss samples from a selection of woodland types from Bulgaria, the Czech Republic, Georgia, Greece, Poland, Switzerland and Wales. The study examines the representation of individual taxa in the two sampling media and aims to ascertain the duration of pollen deposition captured by a moss. The latter aim was pursued through the calculation of dissimilarity indexes to assess how many years of pollen deposited in a pollen trap yield percentage values that are most similar to those obtained from the moss. The results are broadly scattered; the majority of moss samples being most similar to several years of pollen depositi…

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Latalowa_M_et_al._ESM_Table_S3 – Supplemental material for Abrupt Alnus population decline at the end of the first millennium CE in Europe – The event ecology, possible causes and implications

Supplemental material, Latalowa_M_et_al._ESM_Table_S3 for Abrupt Alnus population decline at the end of the first millennium CE in Europe – The event ecology, possible causes and implications by Małgorzata Latałowa, Joanna Święta-Musznicka, Michał Słowiński, Anna Pędziszewska, Agnieszka M NoryŚkiewicz, Marcelina Zimny, Milena Obremska, Florian Ott, Normunds Stivrins, Leena Pasanen, Liisa Ilvonen, Lasse Holmström and Heikki Seppä in The Holocene

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Abrupt Alnus population decline at the end of the first millennium CE in Europe - The event ecology, possible causes and implications

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…

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