Small vertebrate and mollusc community response to the latest Pleistocene-holocene environment and climate changes in the Kraków-Częstochowa Upland (Poland, Central Europe)

Author(s):  
Claudio Berto ◽  
Marcin Szymanek ◽  
Hugues-Alexandre Blain ◽  
Andrea Pereswiet-Soltan ◽  
Magdalena Krajcarz ◽  
...  
2020 ◽  
Author(s):  
Daniele Scarponi ◽  
Michele Azzarone ◽  
Rafal Nawrot ◽  
Michal Kowalewski

<p>The ecological consequences of climate change on marine ecosystems remains poorly understood, particularly for ecological communities that reside in enclosed basins, which limit marine species in their ability to migrate. Here we use assemblages of late Quaternary fossils mollusks preserved in nearshore sediments to explore how nearshore marine benthic communities responded to past climate changes in the northern Adriatic.   We focus on three time periods: (1) the last interglacial (<125ka BP), when regional temperatures were higher than today, representing a possible analogue for the near-future global warming; (2) the last late glacial 14.5-18.0 ka BP; and (3) the mid-Holocene 6.0-1.0 ka BP, when conditions were similar to today but with a minimal human impact. Temporal dynamics of benthic communities was assessed by applying multivariate and resampling approaches to abundance data for core-derived samples of fossil mollusks. Results demonstrate that the penultimate interglacial benthic assemblages shifted to a new community state during the subsequent glacial period. The shift represented a decline in abundance of exclusively Mediterranean nearshore species and a concurrent increase in abundance of nearshore species of cosmopolitan and boreal affinity. This shift was, most likely, driven by global climate cooling. Following this major community restructuring, the local nearshore communities had reversed back to their previous state during the mid-Holocene, when interglacial climate conditions were fully reestablished again. We conclude that the nearshore community responded to long-term climate changes by displaying a resilient (rather than persistent or stochastic) behavior, with Holocene biota reversing back to the pre-existing interglacial state. However, regional pollution, trawling and the threat of spreading invasive species are already taking their toll and the present-day communities are shifting to a novel, historical unprecedented community state. Nonetheless, our findings indicate that if local and regional threats can be mitigated, the coastal marine communities of the northern Adriatic would be resilient against limited climate warming in the near future.</p>


2013 ◽  
Vol 2 (1) ◽  
pp. 22-25
Author(s):  
Eva Balážová ◽  
Viera Petrášová

Abstract Currently the land tax causes difficulties to the managers of agricultural and forest land as it does not fulfill its historical function. Stagnant market for agricultural products together with damages caused by climate changes (floods or droughts) brings complications to the land managers by decreasing their profit. The research focuses on an analysis of land tax in Central Europe and its functioning as a municipal economic tool taking into account environmental protection and usage of nonrenewable resources. The article offers suggestions for municipalities with regard to changes in land taxation which are derived from their influence on agricultural and forest land usage.


2011 ◽  
Vol 56 (6) ◽  
pp. 2211-2222 ◽  
Author(s):  
Làszló G.-Tóth ◽  
Laura Parpala ◽  
Csilla Balogh ◽  
Istvàn Tàtrai ◽  
Eszter Baranyai

The Holocene ◽  
2017 ◽  
Vol 27 (8) ◽  
pp. 1132-1145 ◽  
Author(s):  
Petra Houfková ◽  
Tomáš Bešta ◽  
Alexandra Bernardová ◽  
Daniel Vondrák ◽  
Petr Pokorný ◽  
...  

Former Lake Komořany, located in Northwest Bohemia in Central Europe, provides multiple proxies (pollen, plant macrofossils, diatoms, chironomids and sediment chemistry) that allowed reconstruction of the development of its aquatic environment and catchment, throughout the Holocene. In order to reconstruct the climatic forcing of this development, we performed a pollen-based reconstruction of climate changes using the best modern analogue method. The climate reconstruction was successful for the interval of 10.0–3.2 ka BP. We demonstrate that shifts in climate were coupled with biotic changes within the lacustrine environment. Both processes were interconnected mainly through changes in the water level status of the lake. The most significant climatic and environmental changes were recorded at 9.1, 6.3, 4.8/4.7, 3.8 and 3.5 ka BP.


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