scholarly journals A biodiverse package of southwest Asian grain crops facilitated high-elevation agriculture in the central Tien Shan during the mid-third millennium BCE

2020 ◽  
Author(s):  
Giedre Motuzaite Matuzeviciute ◽  
Taylor R. Hermes ◽  
Basira Mir-Makhamad ◽  
Kubatbek Tabaldiev

AbstractWe report the earliest and the most abundant archaeobotanical assemblage of southwest Asian grain crops from Early Bronze Age Central Asia, recovered from the Chap II site in Kyrgyzstan. The archaeobotanical remains consist of thousands of cultivated grains dating to the mid-late 3rd millennium BCE. The recovery of cereal chaff, which is rare in archaeobotanical samples from Central Asia, allows for the identification of some crops to species and indicates local cultivation at 2000 m.a.s.l., as crop first spread to the mountains of Central Asia. The site’s inhabitants cultivated two types of free-threshing wheats, glume wheats, and hulled and naked barleys. Highly compact morphotypes of wheat and barley grains represent a special variety of cereals adopted to highland environments. Moreover, glume wheats recovered at Chap II represent their most eastern distribution in Central Asia so far identified. Based on the presence of weed species, we argue that the past environment of Chap II was characterized by an open mountain landscape, where animal grazing likely took place, which may have been further modified by people irrigating agricultural fields. This research suggests that early farmers in the mountains of Central Asia cultivated a high diversity of southwest Asian crops during the initial eastward dispersal of agricultural technologies, which likely played a critical role in shaping montane adaptations and dynamic interaction networks between farming societies across highland and lowland cultivation zones.

The Holocene ◽  
2020 ◽  
pp. 095968362097277
Author(s):  
Suzanne AG Leroy ◽  
Santiago R Giralt

Central Asia, with its high mountains, despite its location between Europe and eastern Asia remains a data poor area. However, mountain glaciers are strongly affected by global change and have a wide-ranging impact. A new pollen record over the last 5600 years shows the extension of a dry Artemisia steppe around Lake Issyk-Kul, with a slightly wetter period from 4.5 to 2.7 ka BP (less Ephedra). Picea schrenkiana forest growing on north-facing slopes of the northern Tien Shan Range, are exposed to Westerlies-related precipitation. The pollen record of Picea is therefore a very good marker of wetter and cold conditions. A comparison to a nearby synchronous pollen record at a higher altitude indicates that the whole forest belt moved down, and that it was not a downwards extension of the lower forest limit only. Four cold and humid phases were evidenced over the last 5.6 ka: 5.5 ka, 4.2 ka and following centuries, 3.2 ka and following centuries (before the end of the Bronze Age) and finally the Little Ice Age, with the latter two being more strongly expressed. These climatic changes, in agreement with other Arid Central Asia investigations, corroborate the driving role of the Westerlies far inland. Human activities were more intense in the Mid and Late Bronze Age (4.5–3.2 ka) and in the last 800 years, confirmed by archaeological and historical information. Issyk-Kul and surrounding rich pastureland were most likely an important step in the ancient Silk Road.


2020 ◽  
Vol 12 (22) ◽  
pp. 9467
Author(s):  
Roy C. Sidle

Central Asia is a vital link in the huge Chinese Belt and Road Initiative (BRI) that follows much of the ancient Silk Road routes in this region. Other than the economic expansion and trade benefits associated with this complex infrastructure system, little is known about the many of the exogenous issues and direct environmental and socioeconomic impacts surrounding the BRI in Central Asia. This opinion paper takes a sharper look at some of these externalities and potential effects through a sustainability lens. Major environmental concerns focus on the proliferation of spur roads that will develop off upgraded or new Belt Roads to promote exploitation of natural resources. Steep, high-elevation landscapes in the Pamirs and Tien Shan pose problems for road location and construction, and the history of road building in less formidable terrain in Yunnan, China is unsustainable, leading to epic landslide and gully erosion, which degrade river systems. Furthermore, many socioeconomic issues may arise like debt dependencies of poor countries, spread of communicable diseases into remote communities, depletion of mineral resources, and implicit compliance with pro-China policies. While some of the poorer post-Soviet nations can reap short-term benefits from BRI plans, it is urged that they assess the long-term sustainability of BRI development and play an active role in determining the conditions for implementation.


2014 ◽  
Vol 8 (5) ◽  
pp. 5433-5483
Author(s):  
T. Smith ◽  
B. Bookhagen ◽  
F. Cannon

Abstract. Central Asia has been strongly impacted by climate change, and will continue to be impacted by diverse climate stressors in the coming decades. This study aims to decipher the impact of climate change on glaciers in the central Tien Shan Mountain Range, a large and understudied region located northeast from the Pamir Knot. To address glacier characteristics over a wide swath of Central Asia, the authors designed and implemented a glacial mapping algorithm which delineates both clean glacial ice – methods which are well documented – and glacial debris tongues, which often require extensive manual digitization. This research improves upon methods developed to automatically delineate glacial areas using spectral, topographic, velocity, and spatial relationships. The authors found that the algorithm misclassifies between 2 and 10% of glacial areas, as compared to a ~750 glacier control dataset. After validating the algorithm against multiple manually digitized control datasets, the authors applied it to a study area encompassing eight Landsat scene footprints stretching from the central Pamir through the central Tien Shan. A statistically significant, though minor, gradient in glacier area loss was found, where glaciers in the west of the study area have shrunk less than those glaciers in the east. This gradient is explained by differences in regional climate, where extratropical cyclones propagating from the west weaken and disband under continued topographic influence, as well as differences in topography, where high-elevation glaciers are thermally insulated from some of the impacts of changing temperatures in the region.


The Holocene ◽  
2021 ◽  
pp. 095968362110332
Author(s):  
Valentí Rull ◽  
Núria Cañellas-Boltà ◽  
Teresa Vegas-Vilarrúbia

Palynological analysis of the last ca. 4300 cal year BP using a sediment core taken from high mountain (ca. 1900 m elevation) Lake Sant Maurici sediments (southern-central Pyrenees) showed remarkable vegetation constancy during the Bronze Age and the Middle Ages. Records of the Iron Age and the Roman period were missing due to a major sedimentary gap. During the studied periods, the vegetation around the lake was largely dominated by pine ( Pinus) forests with birch ( Betula), oak ( Quercus) and hazel ( Corylus) trees, as is the case today. The composition of these forests and the abundance of their components remained quite stable, despite the occurrence of temperature and moisture shifts. The degree of human disturbance, notably that of pastoralism and cereal cultivation by scattered and temporary settlements, was very low and had little or no effect on the dominant forests. This situation contrasts with most high-elevation (subalpine and alpine) environments of the central Pyrenees that were massively anthropized during the Middle Ages. Further research should be aimed at finding sediments corresponding to the Iron Age and the Roman period to verify whether the vegetation constancy can be extended throughout the Late-Holocene. Past records of this type may allow the estimation of natural and anthropogenic thresholds for irreversible forest changes, which would be useful for conservation purposes.


1995 ◽  
Vol 100 (B10) ◽  
pp. 20321-20343 ◽  
Author(s):  
Albert A. Lukk ◽  
Sergei L. Yunga ◽  
Vladimir I. Shevchenko ◽  
Michael W. Hamburger

Geology ◽  
1990 ◽  
Vol 18 (2) ◽  
pp. 128 ◽  
Author(s):  
B. F. Windley ◽  
M. B. Allen ◽  
C. Zhang ◽  
Z-Y Zhao ◽  
G-R Wang
Keyword(s):  

2007 ◽  
Vol 56 (3-4) ◽  
pp. 311-327 ◽  
Author(s):  
S.S. Marchenko ◽  
A.P. Gorbunov ◽  
V.E. Romanovsky

2009 ◽  
Vol 58 (1) ◽  
pp. 55-69 ◽  
Author(s):  
Stefan Meng ◽  
Matthias H. Hoffmann

Abstract. LOŽEK (1986) is of the opinion that Pupilla loessica has been found recently in Central Asia. The aim of this study is to provide some initial, concrete contributions to the discussion of this subject. It should be understood as a basis for further investigations. During recent visits on site between 1995 and 2006 in Central Asia in the Russian Altay, in Northern Mongolia, in the Baikal region and in the Tien Shan, numerous recent malacocenoses were examined. In many places evidence was found of a form of Pupilla which had not previously been described from this region; its shell morphology cannot be distinguished from Pupilla loessica. Its distribution is concentrated in the strongly continental Khrebet Saylyugem in the South Eastern Altay. The probability of the occurrence of Pupilla loessica in Central Asia is supported, apart from the shell morphology criteria, by the preference of this species for more continental types of habitat with average annual temperatures markedly below 0° C and the corresponding accompanying fauna adapted to the cold, including e.g. Columella columella, Vertigo genesii, Vallonia tenuilabris, etc., which make these fauna easily comparable to the Pleistocene glacial associations of the Central European region.


Author(s):  
Emily Baker

The small glaciers of Grand Teton National Park (GTNP) are iconic landmarks, enhancing the experience of millions of visitors to the park each year. They are valuable far beyond their beauty, and play a critical role in the park’s unique high-elevation ecosystems.


Sign in / Sign up

Export Citation Format

Share Document