Environments of the Russian Plain during the Middle Valdai Briansk Interstade (33,000–24,000 yr B.P.) Indicated by Fossil Mammals and Plants

2002 ◽  
Vol 57 (3) ◽  
pp. 391-400 ◽  
Author(s):  
Anastasia K. Markova ◽  
Alexandra N. Simakova ◽  
Andrei Yu Puzachenko ◽  
Lev M. Kitaev

AbstractAbundant mammal (45 localities) and plant (52 sections) fossil data collected from the Russian Plain deposits of the Middle Valdai Briansk Interstade indicate a period of noticeable warming. These materials were jointly analyzed. The data were organized in the database software PARADOX and then moved to the GIS program ARC/INFO. Mathematical methods as well as traditional research methods were used for the analysis. The reconstructed biogeographical provinces illustrate the specific environmental and climatic conditions of the Briansk Interstade. Analogues of modern natural zones did not exist at this time on the Russian Plain. The Briansk landscapes reflect the moderate-cool climate of this period, when the majority of northern subarctic plant and mammal species extended their ranges considerably to the south to the Central Russian Plain. At the same time, steppe species penetrated farther north and west. This combination shows that the continuous forest zone was destroyed during the Briansk Inter-stade. Five biogeographical provinces have been reconstructed from the north to the south for the Russian Plain during the Briansk warming on the basis of joint analysis of mammalian and botanical data.

2019 ◽  
pp. 29-78 ◽  
Author(s):  
N. V. Zolotareva ◽  
A. Yu. Korolyuk ◽  
S. M. Yamalov

There is a series of forest-steppe islands in the forest zone of the Middle Cis-Ural region. Two of these (Krasnoufimskaya and Mesyagutovskaya forest-steppes) of the considerable size and are of great interest for the study of steppe and meadow-steppe vegetation diversity in the northern locations of the Cis-Urals region. In the recent decades the studies of Mesyagutovskaya forest-steppe herbaceous vegetation with their syntaxonomy were done (Yamalov, Kucherova, 2009; Yamalov et al., 2013). For Krasno­ufimskaya forest-steppe such research was not carried out. Our aim was to make the revision of previously described syntaxa on this territory using the new data and to determine their position within the class Festuco-Brometea according to modern views. Existence of the forest-steppe landscape in the forest zone of Middle Cis-Urals region is due tothebarrier effect of the Ufa Plateau, intercepting part of the rainfall coming from the Atlantic transport. The climate of the study area is continental with moderately cold winter and moderately warm summer. Bedrocks here are limestones, sandstones and slates. The extrazonal northern forest-steppe extends for two degrees in the latitudinal direction. Mountainousness increases from the north to the south, while the climate becomes drier and warmer (Table 1). The central part of Krasnoufimskaya forest-steppe is flat; its agricultural development began in 17th century, so therefore the steppe areas were preserved only on the slopes of river valleys and hills. The territory of Mesyagutovskaya forest-steppe is more mountainous, therefore, the number of preserved steppe plots here is greater than in the Krasnoufimsk area (Fig. 2, 8). The initial dataset includes 295 relevés collected in the course of the field study in 2007–2014 in some locations of the Sverdlovsk Region and the Bashkor­tostan Republic. After the revision according to EuroVegChecklist Expert System (Mucina et al., 2016) the relevés previously assigned to the class Moli­nio-Arrhenatheretea were excluded, thus the data of this paper are based on the analysis of 260 relevés. All relevés were classified using the modified TWINSPAN algorithm (Roleček et al., 2009) in JUICE 7.0 (Tichý, 2002). According to TWINSPAN results the dataset was divided into 9 groups which formed two clusters (Fig. 1). Each of them is differentiated by group of species: cluster A — by the meso-xerophyte species of meadow steppes and xeric meadows, including 18 diagnostic species of the order Brachypodietalia pinnati (syn. Brometalia erecti) (Willner et al., 2017, 2019): Amoria montana, Brachypodium pinnatum, Carex caryophyllea, Dactylis glomerata, Festuca pratensis, Lathyrus pratensis, Leucanthemum vulgare, Ranunculus polyanthemos, Trifolium pratense, Vicia cracca, etc.; cluster B — by the widespread steppe species, including diagnostic ones of the class Festuco-Brometea (Anemone sylvestris, Artemisia latifolia, Campanula sibirica, Koeleria cristata, Scabiosa ochroleuca, Stipa capillata) and the order Helictotricho-Stipetalia (Helictotrichon desertorum, Onosma simplicissima, Oxy­tropis pilosa, Pilosella echioides, Potentilla humifusa, Salvia stepposa) (Korolyuk, 2017). Thus, cluster A combines meadow steppes and xeric meadows on rich soil habitats, and these communities correspond to the order Brachypodietalia pinnati. Cluster B combines petrophytic steppes on dry rocky habitats of insolated slopes, and these communities correspond to the order Helictotricho-Stipetalia. Ordination showed that such ecological factors as habitat moisture, soil fertility and rockiness are important in differentiation of syntaxa of the class Festuco-Brometea (Fig. 13). The vegetation of the class Festuco-Brometea in the northern forest-steppe of the Cis-Urals region belongs to 2 orders, 6 associations, 9 subassociations, 2 variants and 3 communities. Among them 1 association (Centaureo sibiricae–Stipetum pulcherrimae Yamalov ass. nov. hoc loco), 9 subassociations (Leucanthemo vulgaris–Stipetum pennatae typicum subass. nov. hoc loco, L. v.–S. p. festucetosum pratensis subass. nov. hoc loco, L. v.–S. p. vicietosum tenuifoliae subass. nov. hoc loco, Drabo sibiricae–Primu­letum macrocalycis typicum subass. nov. hoc loco, D. s.–P. m. potentilletosum humifusae subass. nov. hoc loco, Fragario viridis–Caraganetum fruticis poetosum angustifoliae Yamalov subass. nov. hoc loco, Stipo pennatae–Centauretum sibiricae typicum subass. nov. hoc loco, S. p.–C. s. polygonatetosum odorati subass. nov. hoc loco, S. p.–C. s. polygaletosum sibiricae subass. nov. hoc loco) and 3 communities (Spiraea crenata, Festuca valesiaca–Alyssum tortuosum, Anthemis subtinctoria–Aster alpinus) are new. One association (Stipo pennatae–Centauretum sibiricae Yamalov et al. ex Zolotareva, Korolyuk, Yamalov ass. nov. hoc loco) has been validated. Syntaxa of the order Brachypodietalia pinnati represent the base of the class Festuco-Brometea in the study area. Currently, only meadow steppes of the ass. Leucanthemo vulgaris–Stipetum pennatae are widespread throughout the extrazonal forest-steppe. Steppe-meadows of the ass. Drabo sibiricae–Primuletum macrocalycis) are found in the Mesyagutovskaya area; in the northern part the same landscape positions are occupied by communities of the class Molinio-Arrhenatheretea. The steppe shrubs in the northern and the southern parts of the forest-steppe area are also different: in the south these are dominated by Caragana frutex and corresponds to the ass. Fragario viridis–Caraganetum fruticis, in the north (Krasnoufimskaya area) Caragana frutex is not found and shrub communitiesaredominated by Spiraea crenata (Fig. 2). Syntaxa of the order Helictotricho-Stipetalia occur on limestones exposures. Currently, the petrophytic steppes of the ass. Stipo pennatae–Centauretum sibiri­cae are known overall in the extrazonal forest-steppe, while the communities of the ass. Centaureo sibiricae–Stipetum pulcherrimae are registered only in the southern part of Mesyagutovskaya forest-steppe; northwards locations of this association diagnostic species are rare, some of these are absent in the Krasnoufimskaya forest-steppe area. The other syntaxa of petrophytic steppes with many relict and endemic species occur locally on the slopes of ancient reeves due to the unique combination of factors (Fig. 8).


2017 ◽  
Vol 63 (No. 9) ◽  
pp. 401-407
Author(s):  
Nakvasina Elena N ◽  
Demina Nadezhda A ◽  
Prozherina Nadezhda A

Adaptation variability and ecological plasticity in the “genotype-environment” system of 22 provenances of Picea abies (Linnaeus) H. Karsten, Picea obovata (von Ledebour) and their introgressive hybrids growing within the Russian Plain were studied. Provenances grow in provenance trials located in the Arkhangelsk, Vologda Regions, and Komi Republic. For assessment of provenances in the “genotype-environment” system, the ranking method was used. Based on a complex ranking index (survival, diameter, height) two local areas of the most adaptive geographic races of P. abies, P. obovata and their hybrid forms were distinguished. In the south-western part of the Russian Plain the best provenances are represented by P. abies and related hybrids from Karelia, Vologda, Leningrad, and Pskov Regions. In the north-eastern part they are represented by P. obovata and its hybrids from the Komi Republic, Arkhangelsk, Sverdlovsk Regions. Provenances of local P. abies and related hybrid forms demonstrate high ecological plasticity on their growing in harsh climatic conditions of the north outside of the species distribution area.


Author(s):  
В.Д. ХУДИК ◽  
Ю.Д. ЗАХАРОВ

Приведены результаты изучения остатков фаун двустворчатых моллюсков из миоценовых отложений Южного Сахалина. Их анализ позволил выделить три бореальных комплекса моллюсков: невельский, раннечеховский и курасийский, фиксирующие периоды похолодания климата в миоцене региона. Изучение неогеновых представителей родов Lucinoma и Mya позволило обозначить среди них ряд таксонов, имеющих стратиграфическое значение. Установленное присутствие тепловодных двустворок в фаунах позднечеховского времени Южного Сахалина, очевидно, отражает собой начальный этап тенденции нарастающего потепления климата в миоцене региона с климатическим оптимумом в верхнедуйско-сертунайское время. Высказывается следующее мнение: неустойчивые климатические условия в позднем палеогене – раннем неогене северной части Япономорского региона могли быть основной причиной возникновения здесь одного из мощных центров эволюции морских малакофаун бореальных районов северной Пацифики. The results on the studying of the faunae of bivalve mollusks remains from miocene deposits of the South Sakhalin are presented. The analysis of the last ones allowed distinguishing the following three boreal assemblages of mollusks: Nevelskiy, early Chekhovskiy and Kurasiiskiy, recording the period of climatic cooling in miocene of the region. Studying of Neogene representatives of Lucinoma and Mya generas allowed identifying some taxa among them which have stratigraphic significance. The detected presence of warm water bivalves in the faunae of the late Chekhovsky time of the South Sakhalin appears to reflect the initial stage of the tendency of the intensifying climate warming happened during miocene, with climatic optimum during the Verkhneduysky – Sertunaysky times. An opinion is expressed that the unstable climatic conditions in the northern part of the Japan Sea region during late Paleogene – early Neogene could have been the main reason for originating of one of the high-potential centers of evolution of the marine malacofaunae of boreal regions of the North Pacific.


2009 ◽  
Vol 48 (12) ◽  
pp. 2487-2512 ◽  
Author(s):  
Yves Durand ◽  
Gérald Giraud ◽  
Martin Laternser ◽  
Pierre Etchevers ◽  
Laurent Mérindol ◽  
...  

Abstract Since the early 1990s, Météo-France has used an automatic system combining three numerical models to simulate meteorological parameters, snow cover stratigraphy, and avalanche risk at various altitudes, aspects, and slopes for a number of mountainous regions (massifs) in the French Alps and the Pyrenees. This Système d’Analyse Fournissant des Renseignements Atmosphériques à la Neige (SAFRAN)–Crocus–Modèle Expert de Prévision du Risque d’Avalanche (MEPRA) model chain (SCM), usually applied to operational daily avalanche forecasting, is here used for retrospective snow and climate analysis. For this study, the SCM chain used both meteorological observations and guess fields mainly issued from the newly reanalyzed atmospheric model 40-yr ECMWF Re-Analysis (ERA-40) data and ran on an hourly basis over a period starting in the winter of 1958/59 until recent past winters. Snow observations were finally used for validation, and the results presented here concern only the main climatic features of the alpine modeled snowfields at different spatial and temporal scales. The main results obtained confirm the very significant spatial and temporal variability of the modeled snowfields with regard to certain key parameters such as those describing ground coverage or snow depth. Snow patterns in the French Alps are characterized by a marked declining gradient from the northwestern foothills to the southeastern interior regions. This applies mainly to both depths and durations, which exhibit a maximal latitudinal variation at 1500 m of about 60 days, decreasing strongly with the altitude. Enhanced at low elevations, snow depth shows a mainly negative temporal variation over the study period, especially in the north and during late winters, while the south exhibits more smoothed features. The number of days with snow on the ground shows also a significant general signal of decrease at low and midelevation, but this signal is weaker in the south than in the north and less visible at high elevation. Even if a statistically significant test cannot be performed for all elevations and areas, the temporal decrease is present in all the studied quantities. Concerning snow duration, this general decrease can also be interpreted as a sharp variation of the mean values at the end of the 1980s, inducing a step effect in its time series rather than a constant negative temporal trend. The results have also been interpreted in terms of potential for a viable ski industry, especially in the southern areas, and for different changing climatic conditions. Presently, French downhill ski resorts are economically viable from a range of about 1200 m MSL in the northern foothills to 2000 m in the south, but future prospects are uncertain. In addition, no clear and direct relationship between the North Atlantic Oscillation (NAO) or the ENSO indexes and the studied snow parameters could be established in this study.


2018 ◽  
Vol 31 (4) ◽  
pp. 900-906 ◽  
Author(s):  
RAMON IVO SOARES AVELAR ◽  
CÂNDIDO ALVES DA COSTA ◽  
FERNANDO DA SILVA ROCHA ◽  
NELSON LICÍNIO CAMPOS DE OLIVEIRA ◽  
WARLEY MARCOS NASCIMENTO

ABSTRACT In Brazil, studies on chickpeas (Cicer arietinum L.) have demonstrated the high productive potential of this crop, especially in the Cerrado areas of Cristalina, GO, and Brasília, DF. Due to dry winter climatic conditions, the North of Minas Gerais may be very suitable for the production of this crop. However, more information on chickpea sowing dates is needed. Therefore, the objective of the present study was to evaluate different chickpea sowing times in two municipalities of Minas Gerais State in Brazil: Montes Claros and Januária. The experiment was carried out in a randomized block design, comprising three sowing dates (12 May, 23 June, and 22 July, 2015), and seven replications. The cultivar used was BRS Aleppo, and the chickpeas were harvested 121 days after sowing. The variables evaluated included plant height, productivity, number of pods with one grain, and number of pods with two grains. The data were submitted to analysis of variance, and joint analysis of the experiments was performed. The highest yields were obtained when chickpeas were sown in May in Montes Claros, with a yield of 5.3 t ha-1. In Januária, chickpeas sown in May and June produced yields greater than 3.0 t ha-1. The plants sown in July, considered late for planting, were harvested during the rainy season, which compromised the quality and yield of the grains. In addition, maximum temperatures above 30ºC were recorded from September onwards in both locations, which also resulted in a reduction in the number of grains per plant. Thus, this sowing season is not recommended in the studied region.


Radiocarbon ◽  
2013 ◽  
Vol 55 (01) ◽  
pp. 201-203 ◽  
Author(s):  
Yaroslav V Kuzmin

Recently, an article was published in this journal (Hartz et al. 2012), presenting new data on the age of early ceramics in eastern Europe (in particular, the central Russian Plain) and discussing the issues related to the appearance of pottery (i.e. Neolithization) in this region, with wider implications of the results for northern Eurasia. I was one of the reviewers of this paper, which is acknowledged by the authors. However, despite my numerous remarks and comments, many of them were not taken into account. As a result, the work by Hartz et al. (2012) suffers from several flaws; here I point them out and briefly discuss the issue of the Neolithization of Eurasia.


Author(s):  
Fatih Karaosmanoglu

On the ecological conditions and distribution of vegetation in any geographical area; The mutual interaction of factors such as climate (temperature-precipitation), topography (altitude-mountain extent), soil plays an important role. In addition, these factors also determine the ecological and geographical distribution of vegetation at micro and macro levels. In this study, geographic information systems (GIS) are used as a method and here; Digital elevation model of the basin (30x30), multi-year climate data (precipitation, temperature), Erinc climate type results, soil distribution, stand distribution, plant profiles and field photographs are the materials used in the study. By processing these data, the type and distribution of vegetation in the Goksu basin were determined. According to these findings, physical factors such as altitude and the extent of the mountains have created significant differences in the precipitation and temperature distribution of the basin. This difference was clearly observed in the Erinc climate classification results, and the south of the basin presented humid and semihumid climate characteristics, and the north presented semi-arid climate characteristics. These climatic conditions also affected the soil formation and type,causing a wide distribution of non-calcareous brown soils and non-calcareous brown forest soils in the field. As a result of all these conditions, plant species showed different vertical and spatial distribution. In the part from the south of the basin to Saimbeyli, plant species such maquis, pinus brutia, pinus nigra, Cedrus libani, Abies, Juniperus are distributed, while in the north, oak species such as oak, Bromus torhentallus, Astragalus, Thymus have been distributed. Thus, factors such as climate, topography and soil played an important role in the spread of vegetation and species in the Goksu Basin.


1960 ◽  
Vol 152 (949) ◽  
pp. 568-571 ◽  

In principle, the fauna of the southern temperate zone should present a general distribution pattern similar to that of the northern temperate zone. The rich invertebrate material preserved in the early Tertiary Baltic amber indicates that, at that time, the similarity was much closer than it is today. But during the Tertiary the cooling climate, in the north, resulted in the recession and extinction of many of those organisms which were rigidly fixed to a certain combination of environmental factors. The Pleistocene glaciations very effectively put a stop to the existence of many such invertebrate species and species groups whose relatives are now regarded as typical relicts. There is no doubt that the influence of the ice ages was comparatively small in the southern temperate zone of the Old World compared to what happened in the north. As regards the African continent it has been supposed that the highest areas in southern Africa, the Maluti Range in eastern Basutoland, at that time were covered with ice. But it was not so. On visiting that area we found that it has been free from ice, and moreover, that it is inhabited by an interesting, largely endemic fauna. Likewise, there is nothing indicating that the South Atlantic islands, the Tristan group and Gough Island, were capped with ice or carried isolated glaciers during the Pleistocene glaciations. Comparatively unchanged climatic conditions made the survival of the preglacial fauna possible.


2021 ◽  
Vol 906 (1) ◽  
pp. 012048
Author(s):  
Tatiana Kuderina ◽  
Otto Chkhetiani ◽  
Arseni Kudikov ◽  
Maria Artamonova

Abstract Climate and environmental changes on Earth have become modern challenges to humanity. The main factor affecting the landscapes of Russia is an increase in air temperature and a decrease in precipitation. Because of these processes, the amount of aerosols in the near-ground atmosphere of the landscapes of the ETR (European territory of Russia) increases. The aim of the study is to determine the atmogeophysical and atmogeochemical indicators that reveal the interaction of the atmosphere and the diversity of natural landscapes in European Russia. Landscape-geochemical research methods make it possible to study geosystems with the participation of all landscape components and actual migration processes, especially the atmospheric migration of chemical elements. To determine the modern atmogeochemical existence, field comprehensive studies of the potential emission of matter in all natural zones of the ETR were carried out submeridionally - in the landscapes of the steppe, forest-steppe, forest and tundra zones of the ETR. The research results show that in the submeridional profile, the mass concentration of aerosols decreases regularly from south to north, the minimum concentrations of atmospheric aerosols are observed in the forest zone, in the tundra there was a slight increase due to anthropogenic landscapes and the influence of the sea. Analysis of the chemical composition of aerosols revealed that, among the elements of global importance, aluminosilicates naturally increase to the south of the ETR as elements of clay minerals that are widespread in the Russian Plain. The maximum phosphorus content occurs in the residential area with agricultural landscapes. Sulfur concentrations are confined to the semiarid zone of the ETR, then decrease in the forest zone and increase again in the technogenic regions and the tundra belt of the Kola Peninsula, surrounded by the sea. The concentrations of chemical elements of regional and local distribution in atmospheric aerosols are more differentiated on the ETR and depend on the natural and technogenic features of each region. Thus, heavy metals are more common in the Plain territories of the forest-steppe and forest zones of the ETR and are confined to the bedrock and technogenic sources. High concentrations of calcium and strontium are associated with areas of weathering of carbonate rocks. In general, increased concentrations of atmospheric aerosols with an increased content of anthropogenic elements are observed during the western and southern transport of air masses. At the same time, the amount of rainstorm precipitation increases when these aerosols act as condensation nuclei. To assess the current state of the atmosphere at the ETR, it is necessary to continue field measurements and organize European annual and seasonal geochemical monitoring at stationary observation points.


2020 ◽  
Vol 157 ◽  
pp. 02028
Author(s):  
Boris Aparin ◽  
Maria Zakharova ◽  
Elena Sukhacheva ◽  
Vitaly Terleev ◽  
Aleksandr Nikonorov ◽  
...  

A progressive growth of anthropogenic soils and non-soil formations in the soil cover of the taiga forest zone and a general decrease in the ecological potential of soils necessitate the development of policies for the rational use of soil resources. The analysis of approaches to forest vegetation assessment of soils is carried out. The concepts of specific and resource potentials are introduced, and our own methodology for their assessment is developed. The methodology for calculating potentials was tested on the example of the Leningrad region, typical of the North-West of the European part of Russia and the North of the Russian Plain. Natural soil areas were calculated using a digital soil map. The analysis of changes in forest growing potential of soils is carried out from the beginning of intensive development of the territory to the modern period. These calculations can form the basis for assessing the potential contribution of the region to ensuring the reproduction of forest resources.


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