Detecting ecological signatures of long-term human activity across an elevational gradient in the Sumava Mountains, Central Europe

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Publikace nespadá pod Ústav výpočetní techniky, ale pod Přírodovědeckou fakultu. Oficiální stránka publikace je na webu muni.cz.
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KRAKLOW Vachel A DRESLEROVÁ Dagmar DIACONU Andrei-Cosmin MORAVCOVÁ Alice KADLEC Martin NÝVLT Daniel TINNER Willy HEURICH Marco FINSINGER Walter FEURDEAN Angelica KUNEŠ Petr FLORESCU Gabriela

Rok publikování 2024
Druh Článek v odborném periodiku
Časopis / Zdroj Quaternary Science Reviews
Fakulta / Pracoviště MU

Přírodovědecká fakulta

Citace
www https://www.sciencedirect.com/science/article/pii/S0277379124004451
Doi http://dx.doi.org/10.1016/j.quascirev.2024.108944
Klíčová slova Peat bog; Testate amoebae; Water table depth; Fire; Pollen; Plant macrofossils; Climate change; Human impact; Holocene; Generalized additive models
Popis Central European mountains, including the Šumava Mountains located along the Czechia/Germany border, have a long and rich anthropogenic history. Yet, documenting prehistoric human impact in Central European mountain environments remains a challenge because of the need to disentangle climate and human-caused responses in terrestrial systems. Here, we present the first reconstructed water table depths (WTDs) from two sites, Pěkná and Blatenská slať, located in the Šumava Mountains. We compare these local WTD records with new and published pollen, non-pollen palynomorphs (NPPs), plant macrofossils, geochemistry and archeological records to investigate how changes in local hydrology and human activities impacted forest succession and fire activity throughout the Holocene across an elevational gradient. Using a generalized additive model, our results suggest that changes in forest succession and fire activity have been primarily caused by climate throughout the Holocene. However, humans have been utilizing mountain environments and their resources continuously since ~4600 cal yr BP, thus playing a secondary role in modifying forest succession to increase resources beneficial to both humans and grazers. Over the last 1000 years, we provide evidence of directly observed human-caused modifications to the landscape. These results contribute to a growing body of literature illustrating human activities and landscape modifications in Central European mountains.
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