Communities of the class Koelerio-Corynephoretea Klika in Klika et Novák 1941 in the Bryansk region of Russia

2017 ◽  
pp. 29-34 ◽  
Author(s):  
A. D. Bulokhov ◽  
A. M. Petrenko

Only few publications on the classification of vegetation of Koelerio–Corynephoretea canescentis Klika in Klika et Novák1941 class, that unites pioneer communities on sandy soils, dunes or an exposed sands, is known for Bryansk region of Russia (Bulokhov, 2001; Bulokhov, Kharin, 2008). This region is located in the western part of the East European plain, on the watershed of two large river (Dnieper and Volga) systems, occupying the central part of the Desna river pool and the woody watershed between Desna and Oka. The territory (34.9 thousand кm2) is extended from the west to the east on 270 km (between 31°10′ and 35°20′ E) and from the north to the south — on 190 km (between 54°05′ and 52°10′ N). The main item of this paper is to submit the results of the classification carried out upon thebasis of 57 releves made in 2003–2016 in Bryansk region and to characterize the composition, distribution and syntaxonomical position of thepioneer vege­tation of sandy and shallow soils communities within it. Three new associations are described according to Braun-Blanquet floristic classification. The syntaxon nomenclature of the higher ranks follows Mucina et al. (2016) The ass. Thymo serpylli–Koelerietum glaucae ass. nov. hoc loco, with synecological optimum on dry poor sandy soils, is diagnosed by character species Artemisia campestris, Koeleria glauca, Thymus serpyl­lum. Its communities occur on fringes of the lichen pine forests, sandy river terraces and outwash plains. Two subassociations are distinguished within the association: T. s.–K. g. typicum (with var. typica and Corynephorus canescens) and agrostietosum vinealis subass. nov. hoc loco (with var. typica and Calluna vulgaris) with Agrostis vinealis, Dianthus arenarius, Cladonia arbuscula as differential species. The ass. Koelerio glaucae–Plantaginetum arena­riae ass. nov. hoc loco, with synecological optimum on dry poor sandy soils or exposed sands, is diagnosed by Plantago arenaria and Koeleria glauca. Its communities occuron the exposed sands, fringes of lichen pine forests and not flooded sandy river crests. The ass. Diantho borbasii–Festucetum polesicae ass. nov. hoc loco with synecological optimum on dry, weekly acidic, poor of mineral nitrogen, sandy soils or the exposed sands, is diagnosed by Festuca pole­sica, Astragalus arenarius, Jurinea cyanoides, Otites parviflora. Communities occur on the exposed sands, fringes of lichen pine forests. Two variants are distinguished within association: Sempervivum ruthenicum (on dunes with dry, poor, weekly developed soils) and typica. These three associations are the early stages of the progressive succession of oligotrophic lichen pine fo­rests on the river terraces or of the heath meadows in flood river plains.

2015 ◽  
pp. 108-128 ◽  
Author(s):  
T. A. Sokolova

The results of geobotanical survey of Alnus glu­ti­nosa arena forests at three sandy areas within the North of the Rostov and the West of the Volgograd regions of the Russian Federation are given. The territory is situated at the East European Plain where steppes are zonal type of vegetation. This territory is well developed agricultural region with highly transformed lands. Nevertheless, the fragments of natural vegetation support rather high floristic and phytocoenotic diversity and they contain a number of endemic species also (Fedyaeva, 2002). Small patches of alder forest stands generally occur in roundish and tape-like depressions on the second and third sandy terraces of the Don River. These woods were in a focus of interest of many scientists, e.g. G. M. Zozulin (1992) who studied these more than 30 years. But the special papers including the ecologo-floristic characteristic of natural arena alder forests were missing up to now. According to vegetation classification based on the Braun-Blanquet approach (Braun-Blanquet, 1964) the alder forests are referred to four formerly described associations of the alliances Alnion incanae and Alnion glutinosae: Aceri tatarici–Alnetum glutinosae, Urtico dioicae–Alnetum glutinosae, Ficario–Ulmetum minoris and Carici elongatae–Alnetum glutinosae. Proposed 4 subassociations and 10 variants reveal the syntaxonomical structure of these associations. The comparative analysis of syntaxa of the forests of the alliances Alnion incanae and Alnion glutinosae within the Rostov region, in the Russian Southern Nechernozemje, in Ukraine and the Central Europe was done. It is emphasized that the differentiation of the alder communities is complicated due to their intrazonal positions in a landscape. There are a very few character species at the association level. At the same time a lot of plant communities reflect the ecotone features between the meso-hygrophyte forests of the class Querco-Fagetea and the mire woods of the class Alnetea glutinosae. Therefore we had to apply both the classical and nonclassical syntaxonomical analysis (Mirkin et al., 2009). It is obvious that the alder forests syntaxonomy at the lowest level will be specified in the nearest future. There are noticeable differences in species composition of studied communities depen­ding on their position in landscape. For example, there are communities with a large amount of species of the class Querco-Fagetea occurring in the forest margins and on slopes. The role of species of the class Alnetea glutinosae increases on the gradient from the outskirts of wood massifs to their central parts in lowlands also. Species of the alliance Alnion incanae are widely presented in all communities. Although the described communities are small in size and rather rare on the territory studied they contain 27 vascular plant species included in the Red Data Book of the Rostov region (Krasnaya…, 2004). These woods considerably increase the biodiversity within the steppe zone as well. The organization of a number of nature reserves is necessary to protect the certain types of alder forests.


1995 ◽  
Vol 43 (2) ◽  
pp. 147-158 ◽  
Author(s):  
Anatoly V. Lozhkin ◽  
Patricia M. Anderson

AbstractAlluvial, fluvial, and organic deposits of the last interglaciation are exposed along numerous river terraces in northeast Siberia. Although chronological control is often poor, the paleobotanical data suggest range extensions of up to 1000 km for the primary tree species. These data also indicate that boreal communities of the last interglaciation were similar to modern ones in composition, but their distributions were displaced significantly to the north-northwest. Inferences about climate of this period suggest that mean July temperatures were warmer by 4 to 8°C, and seasonal precipitation was slightly greater. Mean January temperatures may have been severely cooler than today (up to 12°C) along the Arctic coast, but similar or slightly warmer than present in other areas. The direction and magnitude of change in July temperatures agree with Atmospheric General Circulation Models, but the 126,000-year-B.P. model results also suggest trends opposite to the paleobotanical data, with simulated cooler winter temperatures and drier conditions than present during the climatic optimum.


2017 ◽  
Vol 30 (4) ◽  
pp. 1028-1038 ◽  
Author(s):  
NAILSON LIMA SANTOS LEMOS ◽  
ANA CLARA RODRIGUES CAVALCANTE ◽  
THIERES GEORGE FREIRE DA SILVA ◽  
JOSÉ RICARDO MACEDO PEZZOPANE ◽  
PATRÍCIA MENEZES SANTOS ◽  
...  

ABSTRACT This study aimed to define areas suitable, and the irrigation water requirement for, cultivation of Tanzania guineagrass in the state of Ceará, Brazil. Tanzania guineagrass yield was estimated by a mathematical model, which considers the crop actual evapotranspiration, resulting from the crop climatological water balance. The water requirement throughout the year was estimated for soils with a water holding capacity of 20 (shallow soils), 40 (sandy soils), 60 (soils with medium texture) and 100 mm (clay soils). The relative frequency of occurrence of monthly productions greater than 2,750 kg DM ha-1 month-1 was obtained for different areas in Ceará, representative of most of the state's economic mesoregions. Tanzania guineagrass annual yields in the state of Ceará were between 20,000-30,000 kg DM ha-1 year-1. During the rainy season, the productive potential varies with the economic mesoregion, which presents different climatic conditions. The state of Ceará is only suitable for the rainfed production of Tanzania guineagrass for 4 months each year, predominantly from February to May, while weather conditions do not favor the development of this grass in the remaining months.


2016 ◽  
Vol 88 (suppl 1) ◽  
pp. 689-703 ◽  
Author(s):  
ANTONIO GALÁN-DE-MERA ◽  
ISIDORO SÁNCHEZ-VEGA ◽  
ELIANA LINARES-PEREA ◽  
JOSÉ CAMPOS ◽  
JUAN MONTOYA ◽  
...  

ABSTRACT A phytosociological approach to dry forest and cactus communities on the occidental slopes of the Peruvian Andes is presented in base of 164 plots carried out following the Braun-Blanquet method. From them, 52 have been made recently, and the other 112 were taken from the literature. After a multivariate analysis, using a hierarchical clustering and a detendred correspondence analysis, the Acacio-Prosopidetea class (dry forest and cactus communities, developed on soils with some edaphic humidity or precipitations derived from El Niño Current), the Opuntietea sphaericae class (cactus communities of central and southern Peru, on few stabilized rocky or sandy soils) and the Carico-Caesalpinietea class (dry forests of the Peruvian coastal desert, influenced by the maritime humidity of the cold Humboldt Current), are differentiated. Within the Acacio-Prosopidetea class, two alliances are commented: the Bursero-Prosopidion pallidae (with two new associations Loxopterygio huasanginis-Neoraimondietum arequipensis and Crotono ruiziani-Acacietum macracanthae), and the new alliance Baccharido-Jacarandion acutifoliae (with the new associations Armatocereo balsasensis-Cercidietum praecocis and Diplopterydo leiocarpae-Acacietum macracanthae). For the Opuntietea sphaericae class, the association Haageocereo versicoloris-Armatocereetum proceri (Espostoo-Neoraimondion) is described on the basis of plots from hyperarid localities of central Peru. Finally, a typological classification of the studied plant communities is given.


1937 ◽  
Vol 7 (19) ◽  
pp. 25-27
Author(s):  
E. M. Blaiklock

A cycling holiday is necessarily one of limited baggage, but this was not the only reason why I took Catullus in my pocket to Rotorua. I enjoy reading a well-known book in new surroundings. I once read the Greek Gospel of Saint John on the Christchurch-Dunedin Express and filled its simple pages, like a medieval manuscript, with pictures of white beach and headland, smooth plains of wheat and snow-capped hills, from that incomparable stretch of railway that runs down the coast of New Zealand's South Island. So did the beauty of the North Island lakeland illuminate a well-thumbed Catullus. How wrong to read our poets always in the study! We have lost them when they remind us only of grammar and philology, German tomes and prosody. We discover them anew when we can fill their lines with new associations and colour them with a colour sometimes all our own. With my eyes full of scenes from a day's wandering, guideless and off the beaten track, where Maori legends cluster thick about lakes, hot pools, and dark green woods, I read Catullus.


2010 ◽  
Vol 36 (-1) ◽  
pp. 47-54 ◽  
Author(s):  
Anto Raukas ◽  
Wojciech Stankowski ◽  
Vitālijs Zelčs ◽  
Petras Šinkunas

Chronology of the Last Deglaciation in the Southeastern Baltic Region on the Basis of Recent OSL DatesThe study of the deglaciation chronology in the south-eastern Baltic Region belonging to the outer zone of the last Pleistocene glaciation has a long history. The Finnish investigator H. Hausen (1913) who worked in the north-western portion of the East-European Plain at the beginning of the 20thcentury was the first to attempt a reconstruction of the course of glacial retreat during the last glaciation. At that time investigators had no physical dating methods and the time scale based on varvometric method, introduced by the Swedish geologist G. de Geer (1912) who divided the deglaciation history of Scandinavia into Daniglacial, Gotiglacial and Finiglacial, each of which had different palaeoglaciological conditions. During last decades different dating methods, including14C, ESR, luminescence methods and10Be techniques have been used, but they could not help essentially improve the existing stratigraphical charts and many problems of topical interest in the history of deglaciation have not been solved yet. During last years the first two authors have studied the suitability of OSL method for the geochronological purposes, paying the most attention to the waterlaid sediments. In the first step they have found the most promising genetical varieties of glaciofluvial sediments (glaciofluvial deltas and sandurs) and in this paper they widened the study area to all three Baltic states with close cooperation with Latvian and Lithuanian colleagues. The obtained results demonstrated, that not all mineral grains in the uppermost glaciofluvial and glaciolacustrine sediments were fully bleached during the last deglaciation. Probably the older sediments also influenced to the luminescence results. It means, that stratigraphic conclusions based on single dates or their small sets are inadmissible and in each case luminiscence dating requires a verification using other methods.


2018 ◽  
Vol 90 (3) ◽  
pp. 439-456 ◽  
Author(s):  
Adam Nadachowski ◽  
Grzegorz Lipecki ◽  
Mateusz Baca ◽  
Michał Żmihorski ◽  
Jarosław Wilczyński

AbstractThe woolly mammoth (Mammuthus primigenius) was widespread in almost all of Europe during the late Pleistocene. However, its distribution changed because of population fluctuations and range expansions and reductions. During Marine Oxygen Isotope Stage 2 (MIS 2), these processes were highly dynamic. Our analyses of 318 radiocarbon dates from 162 localities, obtained directly from mammoth material, confirmed important changes in mammoth range between ~28.6 and ~14.1 ka. The Greenland stadial 3 interval (27.5–23.3 ka) was the time of maximum expansion of the mammoth in Europe during MIS 2. The continuous range was soon fragmented and reduced, resulting in the disappearance of Mammuthus during the last glacial maximum from ~21.4 to ~19.2 ka in all parts of the North European Plain. It is not clear whether mammoths survived in the East European Plain. The mammoth returned to Europe soon after ~19.0 ka, and for the next 3–4 millennia played an important role in the lifeways of Epigravettian societies in eastern Europe. Mammoths became extinct in most of Europe by ~14.0 ka, except for core areas such as the far northeast of Europe, where they survived until the beginning of the Holocene. No significant correlation was found between the distribution of the mammoth in Europe and human activity.


2021 ◽  
pp. 113-149
Author(s):  
E. D. Lapshina ◽  
I. V. Filippov ◽  
V. E. Fedosov ◽  
Yu. V. Skuchas ◽  
P. Lamkowski ◽  
...  

There are very few publications on the classification of mountain mire vegetation in Russia. Several associations in the Southern Siberia mountains (Lapshina, 1996; Lashchinsky, 2009) and the Khibiny Mountains (Koroleva, 2001) are described. Mire vegetation in the Southern Urals is relatively well studied and described in the traditions of the ecological-phytocenotic dominant classification (Ivchenko, 2013; Ivchenko, Znamenskiy, 2015) while the knowledge on that of the Northern and Sub-Polar Urals is extremely limited. There is no information about the mires in the Polar Urals. The paper presents the results of classification of the class Scheuchzerio–Caricetea fuscae of the Yanganape mountain massif (67.68°—67.75° N, 67.72°—68.00° E) and adjacent plains in the Eastern macroslope of the Polar Urals, within the southern tundra subzone. The study area is mountain massif of about 250 m a. s. l., composed of limestone outcrops, with a wavy flat (60–90 m a. s. l.) plain around (Fig. 1–2). The classification is based on 138 relevés made in July 27–August 8, 2017 (Fig. 3). Relevés of similar syntaxa, established in the north of the Western Europe and the East European tundras (Ruuhijärvi, 1960; Dierssen, 1982; Lavrinenko et al., 2016), were included in analysis. DCA and t-SNE (t-distributed stochastic neighbor embedding) methods were used for ordination of syntaxa in multidimensional space (Maaten, Hinton, 2008). The calculations were made using the machine learning package for Python-Scikit-learn. In total, 13 associations, 11 subassociations, 12 variants from 6 alliances and 3 orders of the class Scheuchzerio–Caricetea fuscae were identified on the relatively small (about 70 km2) area. Within the order Caricion davallianae, syntaxa of the alliance Caricion atrofuscae-saxatilis, comprising low sedge-hypnum communities on carbonate mineral and organomineral soils in the mountains of the Western Europe, were identified and described for the first time on the territory of Russia. Three new associations (Ditricho flexicauli—Caricetum redowskianae, Tomentypno nitentis–Equisetetum palustre, Tomentypno nitentis–Eriophoretum vaginati) were described on the the Yanganape mountain massif (Table 1), which significantly expands the area of the alliance to the East. Alliance’ communities have some similarities with syntaxa of zonal dwarf shrub-grass-moss tundra vegetation (Lavrinenko, Lavrinenko, 2018), but are generally well differed by the species composition and community structure (Table 5). The order Caricetalia fuscae in the Eastern macroslope of the Polar Urals is represented by 4 alliances. In addition to Drepanocladion exannulati and Sphagno-Caricion canescentis, listed in the “Classification of Vegetation of Europe” (Mucina et al., 2016), we include into order the alliance Caricion stantis — moderately rich sedge-moss fen vegetation of the Subarctic and tundra zones, and the alliance Stygio–Caricion limosae, containing extremely waterlogged meso-oligotrophic and slightly acidic to neutral low sedge fens. There are 4 associations within the alliance Caricion stantis, including new ass. Scorpidio cossonii–Caricetum rariflorae (Table 2). Taking into account statistically significant differences in the species composition of sedge-moss communities dominated by various moss species (Fig. 15, 5-6), ass. Scorpidio scorpioidis–Caricetum chordorrhizae was taken out from ass. Drepanoclado revolventis–Caricetum chordorrhizae Osvald 1925 ex Dierssen 1982 broadly understood in the Western Europe. Its nomenclature type is the only relevé of Carex chordorrhizae-Amblistegium scorpioides-Ass. (Osvald 1925: 37), which sufficient for the original diagnosis, because it contains list of species with abundance and both name-giving taxa (ICPN, 2b, 7). The communities of both associations were identified in the Eastern macroslope of the Polar Urals, where they are represented by new subassociations, which significantly expands the distribution area of these associations to the East. Recently validly described in the Eastern European tundras (Lavrinenko et al., 1916) ass. Scorpidio revolventis–Caricetum rariflorae is also known for the North of the Western Europe (Dierssen, 1982). Its difference from western syntaxa is the absence of many boreal species, which are not able to exist in the severe climate in the North of Western Siberia, as well as the great number of plant communities with the diagnostic species of the alliance Caricion atrofuscae-saxatilis due to rich mineral nutrition, associated with the carbonate soils and calcium-rich groundwaters in the study area. New associations are established in two allian­ces: Carici aquatilis–Warnstorfietum tundrae in Drepanocladion exannulati and Sphagno squarrosi–Caricetum chordorrhizae in Sphagno–Caricion canescentis (Table 3). The floristic features of the latter alliance, whose communities on the northern limit of their distribution have a certain similarity to the arctic sedge-moss mire vegetation of the alliance Caricion stantis, are discussed. Oligotrophic communities of the alliance Scheuch­zerion palustris, occuring in acidic habitats, are placed in the order Scheuchzerietalia palustris that is in agreement with new interpretation of this alliance in the paper by Mucina et al. (2016). Two associations (Carici rotundatae–Sphagnetum baltici, Sphagno compaci–Caricetum rotundatae) are assigned to this alliance. There are few relevés for both Scheuchzerion palustris and Stygio–Caricion limosae alliances in the study area that is why their classification is preliminary, and it will be considered in the near future for the whole North of the Western Siberia on a larger data set. The classification results are confirmed by DCA-ordination of selected syntaxa (Fig.15, Б). However, the differentiation of communities is more clearly demonstrated by the t-SNE method, which allows displaying multidimensional hyperspaces on the plane (Fig.15, А).


<em>Abstract.</em>—From its headwaters in the Rocky Mountains, the Platte River drains 230,362 km<sup>2</sup> in Colorado, Wyoming, and Nebraska. The Platte River is formed by the confluence of the North Platte and South Platte near the city of North Platte, Nebraska, and receives additional flow from the Loup and Elkhorn rivers that drain the Sand Hills region of Nebraska. Water diversions for mining and irrigation began in the 1840s in Colorado and Wyoming, and irrigation diversions in Nebraska began in the 1850s. Construction of dams for control of river flows commenced on the North Platte River in Wyoming in 1904. Additional dams and diversions in the North Platte, South Platte, and Platte rivers have extensively modified natural flow patterns and caused interruptions of flows. Pollution, from mining, industrial, municipal, and agricultural sources, and introductions of 24 nonnative species have also taken their toll. Fishes of the basin were little studied before changes in land use, pollution, and introduction of exotic species began. The current fish fauna totals approximately 100 species from 20 families. Native species richness declines westward, but some species find refugia in western headwaters streams. Declines in 26 native species has led to their being listing as species of concern by one or more basin states.


Author(s):  
Robert Van de Noort

The North Sea is not renowned for its islands, and much of the modern land–sea interface is sharp, especially along the coasts of Jutland, North and South Holland and much of England. Nevertheless, the North Sea does contain a surprisingly large number of islands and archipelagos, which can be presented with reference to a clear north–south divide. In the northern half of the North Sea, most islands are of hard rock with shallow soils, and their islandness is the result of ongoing glacio-isostatic uplift of previously drowned lands and sea-level rise. With the exception of the Shetland and Orkney archipelagos, few of these islands are found at a great distance from the mainland, and the majority of the countless islands, islets, and rock outcrops off the North Sea coasts of Norway, Sweden, Scotland, and north-east England can be found within a few miles of the mainland. In the southern half of the North Sea, the islands are mainly made up of sand and clay and, in their history if not today, were frequently sandbanks formed by the sea utilizing both marine and riverine sediments. Most of the islands of the Wadden Sea in Denmark, Germany, and Holland are sandbanks elevated by aeolian-formed sand dunes. Further south, the core of the large islands of Zeeland is principally formed of riverine sands and marine clays intercalated with peat, reflecting coastal wetland conditions at various times in the Post-glacial and Holocene (Vos and Van Heeringen 1997). As with Zeeland, the islands on the English side of the North Sea, such as Mersey Island in the Blackwater estuary and Foulness Island in Essex, have now been incorporated into the mainland. Only a few islands cannot be so simply classified:Helgoland in the German Bight, a Sherwood Sandstone stack of Triassic date, is the best known example. Island archaeology, as we have seen (chapter 2), has for many decades approached islands as environments that were relatively isolated from the wider world.


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