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

Author:

Latałowa Małgorzata1ORCID,Święta-Musznicka Joanna1,Słowiński Michał2ORCID,Pędziszewska Anna1,Noryśkiewicz Agnieszka M3,Zimny Marcelina1,Obremska Milena4,Ott Florian56,Stivrins Normunds78ORCID,Pasanen Leena9,Ilvonen Liisa10,Holmström Lasse9,Seppä Heikki11

Affiliation:

1. Laboratory of Palaeoecology and Archaeobotany, Department of Plant Ecology, Faculty of Biology, University of Gdańsk, Poland

2. Department of Environmental Resources and Geohazards, Institute of Geography and Spatial Organization, Polish Academy of Sciences, Poland

3. Institute of Archaeology, Faculty of History, Nicolaus Copernicus University in Toruń, Poland

4. Institute of Geological Sciences, Polish Academy of Sciences, Poland

5. Section 5.2 – Climate Dynamics and Landscape Evolution, GFZ German Research Centre for Geosciences, Germany

6. Department of Archaeology, Max Planck Institute for the Science of Human History, Germany

7. Department of Geography, Faculty of Geography and Earth Sciences, University of Latvia, Latvia

8. Department of Geology, School of Science, Tallinn University of Technology, Estonia

9. Research Unit of Mathematical Sciences, University of Oulu, Finland

10. Department of Mathematics and Statistics, University of Helsinki, Finland

11. Department of Geosciences and Geography, University of Helsinki, Finland

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The study, based on the examination of 70 published and unpublished pollen profiles from Poland and supplementary data from the surrounding regions, shows that an abrupt, episodic Alnus population decline at the end of the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.

Funder

gdański uniwersytet medyczny

Virtual Institute of Integrated Climate and Landscape Evolution Analyses (ICLEA)

academy of finland

Polish Ministry of Science and Higher Education

Publisher

SAGE Publications

Subject

Paleontology,Earth-Surface Processes,Ecology,Archaeology,Global and Planetary Change

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