Shift in Plant Species Composition Reveals Environmental Changes During the Last Decades: A Long-Term Study in Beech (Fagus sylvatica) Forests in Bavaria, Germany

2013 ◽  
Vol 48 (4) ◽  
pp. 467-491 ◽  
Author(s):  
Matthias C. Jantsch ◽  
Anton Fischer ◽  
Hagen S. Fischer ◽  
Susanne Winter
2021 ◽  
Vol 10 (3) ◽  
pp. 72-76
Author(s):  
Gavriil Mikhailovich Melkumov

The work is devoted to a long-term study of the species composition and ecologo-trophic features of basidial macromycetes growing in diverse communities in the Novousmansky district of the Voronezh Region. The mycological study revealed 405 species of macromycetes belonging to 2 divisions, 3 classes, 14 orders, 67 families and 145 genera. Most species of fungi belong to the orders Agaricales (177), Russulales (69), Polyporales (47) and Boletales (46). It was found that saprotrophs (187 species), represented by mono- (126) and polysaprotrophs (61), predominate in the forest coenoses in the Novousmansky district of the Voronezh Region. Macromycetes with a mixed type of nutrition (58) make up a large proportion of the detected fungi, among which facultative xylosaprotrophs dominate (21). Symbiotrophs include 58 taxa and form an exomycorrhiza with deciduous and coniferous trees. The overwhelming number of macromycete species are classified as edible (188) fungi. A smaller number of inedible (152), poisonous (51) and conditionally edible (14) representatives are represented. Special attention is paid to the issues of protection of rare and endangered basidiomycetes growing on the territory of the study. As a result of the survey of the Novousmansky district territory, 11 taxa of basidial fungi included in the 2nd edition of the Red Book of the Voronezh Region (2018) were identified.


Author(s):  
S.V. Shchepetov ◽  
◽  
V.Yu. Neshataeva ◽  

The Cretaceous fossil floras from the formations of the Okhotsk-Chukotka volcanogenic belt differ significantly by its systematic composition from the same-age fossil floras from the coastal lowland sedimentations. The peculiarities of fossil floras from the volcanogenic disposals are the most obvious in Chaun Flora firstly found in the volcanogenic formations of Pegtymelski Arch in Central Chukotka. L.B. Golovneva presented the results of the long-term study of this flora in the monograph published in 2018. On the base of these data and using our own experience in the stratigraphy of the Okhotsk-Chukotka volcanogenic belt and the study of the vegetation cover dynamics in the areas of modern volcanism of Kamchatka we showed that most likely Chaun Flora formed on juvenile substrata in the central parts of the vast volcanic fields being isolated form the sources of diasporas. The Chaun Flora has not clear affinity in neither lateral nor stratigraphic localization, because the fossil remains of characteristic plant species occur in different-age formations on all extent of the volcanogenic belt. The species characteristic for Chaun Flora are indicators of the certain environmental conditions and reflect the peculiarities of the processes of fossilization in the areas of terrestrial volcanism from Turon until Campanian inclusive.


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