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      Development of high diversity beech forest in the eastern Carpathians

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          Abstract

          Aim

          In recent decades, a surge in the number of significant and uncontrolled wildfires has occurred worldwide. Global warming may amplify this trend and threaten most ecosystems worldwide. Deciduous forests are characterized by high plant diversity, and understanding their long‐term dynamics is crucial to anticipate changes in these ecosystems during ongoing global warming. The aim of this study is to understand how European beech forests have colonized the inner Eastern Carpathians and how changes in fire regime and human activities have affected their biodiversity.

          Location

          Inner Eastern Carpathian Mountains, Slovakia.

          Taxon

          Plantae, gymnosperms, angiosperms.

          Methods

          Peat core was extracted from the centre of Ďurova mláka mire in 2018. A multi‐proxy approach has been applied to investigate the development of beech forest. Charcoal analysis has been done each centimetre to reconstruct the fire signal. Pollen analysis has been done at 2 cm resolution to reconstruct the vegetation composition and dynamics, and the variation in palynological richness (PRI), evenness and turnover has been analysed. Macro‐remains analysis has been performed at 10 cm resolution to add more information about the local vegetation.

          Results

          Low diversity spruce forest was dominant until 5200 cal. BP during a fire‐prone period due to specific climatic conditions (drier climate than the following period). The higher fire frequency and intensity following this period is simultaneous with the first expansion of Fagus which indicate that Fagus could occupy post‐fire habitats, at least at the local scale. However, its dominance coincided with major gaps in fire events from 3900 cal. BP. The PRI has increased during the transition from spruce to beech forest highlighting the importance of beech forests in maintaining plant biodiversity. However, the stronger increase in the richness is synchronous with the increase in human activities around 2000 cal. BP, and then 350 cal. BP.

          Main Conclusions

          Climate‐driven fire frequency has been a natural driver of vegetation changes in the Carpathians by promoting the emergence of high diversified beech forest. These changes were significantly modified by later increase in human activities.

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          Most cited references126

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          Diversity in tropical rain forests and coral reefs.

          The commonly observed high diversity of trees in tropical rain forests and corals on tropical reefs is a nonequilibrium state which, if not disturbed further, will progress toward a low-diversity equilibrium community. This may not happen if gradual changes in climate favor different species. If equilibrium is reached, a lesser degree of diversity may be sustained by niche diversification or by a compensatory mortality that favors inferior competitors. However, tropical forests and reefs are subject to severe disturbances often enough that equilibrium may never be attained.
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            VEGAN, a package of R functions for community ecology

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              Is Open Access

              THE INTCAL20 NORTHERN HEMISPHERE RADIOCARBON AGE CALIBRATION CURVE (0–55 CAL kBP)

              Radiocarbon ( 14 C) ages cannot provide absolutely dated chronologies for archaeological or paleoenvironmental studies directly but must be converted to calendar age equivalents using a calibration curve compensating for fluctuations in atmospheric 14 C concentration. Although calibration curves are constructed from independently dated archives, they invariably require revision as new data become available and our understanding of the Earth system improves. In this volume the international 14 C calibration curves for both the Northern and Southern Hemispheres, as well as for the ocean surface layer, have been updated to include a wealth of new data and extended to 55,000 cal BP. Based on tree rings, IntCal20 now extends as a fully atmospheric record to ca. 13,900 cal BP. For the older part of the timescale, IntCal20 comprises statistically integrated evidence from floating tree-ring chronologies, lacustrine and marine sediments, speleothems, and corals. We utilized improved evaluation of the timescales and location variable 14 C offsets from the atmosphere (reservoir age, dead carbon fraction) for each dataset. New statistical methods have refined the structure of the calibration curves while maintaining a robust treatment of uncertainties in the 14 C ages, the calendar ages and other corrections. The inclusion of modeled marine reservoir ages derived from a three-dimensional ocean circulation model has allowed us to apply more appropriate reservoir corrections to the marine 14 C data rather than the previous use of constant regional offsets from the atmosphere. Here we provide an overview of the new and revised datasets and the associated methods used for the construction of the IntCal20 curve and explore potential regional offsets for tree-ring data. We discuss the main differences with respect to the previous calibration curve, IntCal13, and some of the implications for archaeology and geosciences ranging from the recent past to the time of the extinction of the Neanderthals.
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                Author and article information

                Contributors
                (View ORCID Profile)
                (View ORCID Profile)
                Journal
                Journal of Biogeography
                Journal of Biogeography
                Wiley
                0305-0270
                1365-2699
                April 2023
                January 11 2023
                April 2023
                : 50
                : 4
                : 699-714
                Affiliations
                [1 ] Department of Forest Ecology, Faculty of Forestry and Wood Sciences Czech University of Life Sciences Prague Czechia
                [2 ] Department of Paleoecology Institute of Botany of the Czech Academy of Sciences Brno Czechia
                [3 ] Institute of Geochemistry, Mineralogy and Mineral Resources, Faculty of Science Charles University Prague Czechia
                [4 ] Department of Geosciences and Geography University of Helsinki Helsinki Finland
                [5 ] Department of Geology Babeş‐Bolyai University Cluj‐Napoca Romania
                [6 ] Geophysical Institute University of Alaska Fairbanks Alaska USA
                [7 ] Institute of Hydrogeology, Engineering Geology and Applied Geophysics, Faculty of Science Charles University Prague Czechia
                [8 ] Department of Botany, Faculty of Science Charles University Prague Czechia
                Article
                10.1111/jbi.14562
                94b8aa38-445b-412c-bfc0-48dda06fc4a1
                © 2023

                http://onlinelibrary.wiley.com/termsAndConditions#vor

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