273 resultados para steppe


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There is a major problem with dating human skeletal material in Eurasian
steppe, possibly due to the freshwater reservoir effects (FRE). The goal of the
project is to examine the extent of the FRE in key areas of Siberia and
Kazakhstan through AMS 14C dating and stable isotope (δ13C, δ15N, δ34S)
analysis of c. 150 archaeological and modern samples. Here, we present the
very first results of the tests. We hope that within next years the study will
provide advanced knowledge of FRE across the region; improved 14C sampling
protocols for 14C and isotopic studies; new data on the chronology, diet and
isotopic ecology of particular archaeological sites, and a database on the
extent and variability of the FRE in the region

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Freshwater reservoir effects (FRE) can cause a major problem with radiocarbon dating human skeletal material in the Eurasian steppe. We present the first results of research into the extent of the FRE in the sites of Borly 4 (Eneolithic), and Shauke 1 and 8b (Early Bronze Age), North-Eastern Kazakhstan. AMS 14C dating and stable isotope (δ13C, δ15N) analysis of associated groups of samples (32 samples, 11 groups in total) demonstrate that: a) the diet of the humans and fauna analysed was based on the C3 foodchain with no evidence of a C4 plant (such as millet) contribution; aquatic resources apparently were a continuous dietary feature for the humans; b) the first 14C dates obtained for the Upper and Middle Irtysh River region attribute the Eneolithic period of the area to the 34th-30th c. BC, and the Early Bronze Age – to the 25th-20th c. BC; there is a ca. 450 years hiatus between the two periods; c) the maximum fish-herbivore freshwater reservoir offset observed equals 301±47 14C yrs. As such, 14C dates from aquatic and human samples from the area need to be interpreted with caution as they are likely to be affected by the offset (i.e. appear older).
The paper also discusses the effect of a sodium hydroxide (NaOH) wash on δ13C, δ15N, C:Natomic levels and collagen yields of the bone samples. Our results indicate a minor but significant effect of NaOH treatment only on C:Natomic ratios of the samples.

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Freshwater reservoir effects (FRE) can cause a major problem with radiocarbon dating human skeletal material in the Eurasian steppe. Recent research has demonstrated that, for the Eneolithic to Early Bronze Age sites of North-Eastern Kazakhstan, the maximum fish-herbivore freshwater reservoir offset observed equals 301±47 14C yrs, as such indicating that 14C dates from aquatic and human samples from the area apparently need to be interpreted with caution as they are likely to be affected by the offset. The current paper presents the new data on the FRE of the Eneolithic to the Early Iron Age sites of Kazakhstan and South of Siberia.

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Grasslands in semi-arid regions, like Mongolian steppes, are facing desertification and degradation processes, due to climate change. Mongolia’s main economic activity consists on an extensive livestock production and, therefore, it is a concerning matter for the decision makers. Remote sensing and Geographic Information Systems provide the tools for advanced ecosystem management and have been widely used for monitoring and management of pasture resources. This study investigates which is the higher thematic detail that is possible to achieve through remote sensing, to map the steppe vegetation, using medium resolution earth observation imagery in three districts (soums) of Mongolia: Dzag, Buutsagaan and Khureemaral. After considering different thematic levels of detail for classifying the steppe vegetation, the existent pasture types within the steppe were chosen to be mapped. In order to investigate which combination of data sets yields the best results and which classification algorithm is more suitable for incorporating these data sets, a comparison between different classification methods were tested for the study area. Sixteen classifications were performed using different combinations of estimators, Landsat-8 (spectral bands and Landsat-8 NDVI-derived) and geophysical data (elevation, mean annual precipitation and mean annual temperature) using two classification algorithms, maximum likelihood and decision tree. Results showed that the best performing model was the one that incorporated Landsat-8 bands with mean annual precipitation and mean annual temperature (Model 13), using the decision tree. For maximum likelihood, the model that incorporated Landsat-8 bands with mean annual precipitation (Model 5) and the one that incorporated Landsat-8 bands with mean annual precipitation and mean annual temperature (Model 13), achieved the higher accuracies for this algorithm. The decision tree models consistently outperformed the maximum likelihood ones.

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In this paper we search the concept of nonviolent resistance inquiring a rural experience from Rio Negro´s steppe. The initiative highlights the need to recognize  the context of the resistance exercise and the consideration of three aspects: the evaluation and interpretation of space, the dispute to public policy and the  restructuring of the family order. These three elements, which overlap material  and symbolic aspects, are discussed from an organization of trade domestic craft production. The notion of “development” is discovered on the basis of the  frameworks of values from which the reproduction of subordination is associated  with this idea, and even the challenge of change is the basis of the proposal which reviews that development idea, and illuminates from this complexity the notion  of “nonviolent resistance”.

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Mit der vorliegenden Arbeit wurden erstmals prähistorische Bevölkerungsstrukturen in der osteuropäischen Steppe von der Oberthrakischen Tiefebene bis zur Wolga populationsgenetisch untersucht. Mit Multiplex-PCR und 454-Sequencing wurden von 65 kupfer- und bronzezeitlichen Individuen die Hypervariable Region I und 30 Abschnitte der coding region der mitochondrialen DNA analysiert. Außerdem wurden bis zu 20 putativ selektierte autosomale SNPs und ein geschlechtsspezifischer Locus genotypsiert. Zu Vergleichszwecken wurden veröffentlichte prähistorische DNA-Daten aus Westeurasien und moderne DNA-Sequenzen herangezogen. Die Ergebnisse stützen die Annahme, dass frühneolithische Bauern aus Südosteuropa durch demische Diffusion an der Etablierung der Viehwirtschaft in der Steppe beteiligt waren. Die durchweg niedrigen FST-Werte zwischen der frühbronzezeitlichen Jamnaja-Kultur in der Steppe und den aufeinanderfolgenden neolithischen Kulturen Mitteleuropas sprechen für regelmäßige Kontakte. Die der Jamnaja-Kultur nachfolgende Katakombengrabkultur ist von einem hohen Anteil der in nord- und osteuropäischen Jäger/Sammler-Populationen verbreiteten Haplogruppe U4 geprägt. Niedrige FST-Werte zwischen den prähistorischen Steppenpopulationen und der heutigen Bevölkerung Mittel- und Osteuropas weisen auf genetische Kontinuität hin. Die nukleären Genotypenfrequenzen bestätigt dies. Der moderne europäische Genpool lässt sich nach aktuellem Kenntnisstand auf drei Wurzeln zurückführen: indigene Mesolithiker, frühe Bauern aus dem Nahen Osten und eine nordeurasische Komponente jungpalaeolithischen Ursprungs. Letztere könnte vielleicht über die nordpontische Population in das Erbgut spätneolithischer Europäer gelangt sein.

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Vorliegende Dissertation beschäftigt sich mit der Populationsgenetik eisenzeitlicher Bevölkerungen der Eurasischen Steppe, die mit der skythischen Kultur assoziiert werden. Für die Analysen wurden 30 Fragmente der kodierenden Region und die HVR1 (16040–16400) des mitochondrialen Genoms, sowie 20 phänotypische Marker untersucht. Die Marker wurden durch Multiplex-PCRs angereichert, mit einem probenspezifischen barcode versehen und einer parallelen Sequenzanalyse mit dem 454 GS FLX Sequenzierer unterzogen. 97 Individuen wurden erfolgreich analysiert, von denen 19 aus dem Westen der Eurasischen Steppe und 78 aus dem Bereich des Altai-Gebirges stammen. Die populationsgenetischen Analysen ergaben geringe genetische Distanzen zwischen den skythischen Populationen aus dem Bereich des Altai-Gebirges, die sich vom 9. bis zum 3. Jahrhundert vor Christus erstrecken, was für eine kontinuierliche Bevölkerungsentwicklung sprechen könnte. Weiterhin finden sich geringe genetische Distanzen zwischen den Gruppen im Osten und Westen der Eurasischen Steppe, was auf eine gemeinsame Ursprungspopulation, oder zumindest Genfluss hinweisen kann. Die Ergebnisse aus dem Vergleich mit neolithischen und bronzezeitlichen Referenzpopulationen aus Zentralasien und den angrenzenden Gebieten weisen auf die Möglichkeit eines gemeinsamen zentral-asiatischen Ursprungs hin, zeigen aber auch, dass die östlichen und westlichen Gruppen der Eisenzeit jeweils zusätzlich lokalem Genfluss ausgesetzt waren. Die Allelfrequenzen der phänotypischen Marker deuten auf einen größeren europäischen Einfluss auf das östliche Zentralasien in der Eisenzeit hin, oder ansteigenden Genfluss aus Ostasien nach der Eisenzeit.

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The closed Tangra Yumco Basin underwent the strongest Quaternary lake-level changes so far recorded on the Tibetan Plateau. It was hitherto unknown what effect this had on local Holocene vegetation development. A 3.6-m sediment core from a recessional lake terrace at 4,700 m a.s.l., 160 m above the present lake level of Tangra Yumco, was studied to reconstruct Holocene flooding phases (sedimentology and ostracod analyses), vegetation dynamics and human influence (palynology, charcoal and coprophilous fungi analyses). Peat at the base of the profile proves lake level was below 4,700 m a.s.l. during the Pleistocene/Holocene transition. A deep-lake phase started after 11 cal ka BP, but the ostracod record indicates the level was not higher than similar to 4,720 m a.s.l. (180 m above present) and decreased gradually after the early Holocene maximum. Additional sediment ages from the basin suggest recession of Tangra Yumco from the coring site after 2.6 cal ka BP, with a shallow local lake persisting at the site until similar to 1 cal ka BP. The final peat formation indicates drier conditions thereafter. Persistence of Artemisia steppe during the Holocene lake high-stand resembles palynological records from west Tibet that indicate early Holocene aridity, in spite of high lake levels that may have resulted from meltwater input. Yet pollen assemblages indicate humidity closer to that of present potential forest areas near Lhasa, with 500-600 mm annual precipitation. Thus, the early mid-Holocene humidity was sufficient to sustain at least juniper forest, but Artemisia dominance persisted as a consequence of a combination of environmental disturbances such as (1) strong early Holocene climate fluctuations, (2) inundation of habitats suitable for forest, (3) extensive water surfaces that served as barriers to terrestrial diaspore transport from refuge areas, (4) strong erosion that denuded the non-flooded upper slopes and (5) increasing human influence since the late glacial.

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