Archaic inheritance: supporting high-altitude life in Tibet

2015 ◽  
Vol 119 (10) ◽  
pp. 1129-1134 ◽  
Author(s):  
Emilia Huerta-Sánchez ◽  
Fergal P. Casey
Keyword(s):  
Tibetan Plateau ◽  
High Altitude ◽  
Candidate Genes ◽  
Physiological Response ◽  
The Tibetan Plateau ◽  
Sequencing Technologies ◽  
Human Dna ◽  
Extreme Altitude ◽  
The World ◽  
Human Colonization

The Tibetan Plateau, often called the roof of the world, sits at an average altitude exceeding 4,500 m. Because of its extreme altitude, the Plateau is one of the harshest human-inhabited environments in the world. This, however, did not impede human colonization, and the Tibetan people have made the Tibetan Plateau their home for many generations. Many studies have quantified their markedly different physiological response to altitude and proposed that Tibetans were genetically adapted. Recently, advances in sequencing technologies led to the discovery of a set of candidate genes which harbor mutations that are likely beneficial at high altitudes in Tibetans. Since then, other studies have further characterized this impressive adaptation. Here, in this minireview, we discuss the progress made since the discovery of the genes involved in Tibetans' adaptation to high altitude with a particular emphasis on describing the series of studies that led us to conclude that archaic human DNA likely contributed to this impressive adaptation.

The earliest human occupation of the high-altitude Tibetan Plateau 40 thousand to 30 thousand years ago

Science ◽  
2018 ◽  
Vol 362 (6418) ◽  
pp. 1049-1051 ◽  
Author(s):  
X. L. Zhang ◽  
B. B. Ha ◽  
S. J. Wang ◽  
Z. J. Chen ◽  
J. Y. Ge ◽  
...  
Keyword(s):  
Tibetan Plateau ◽  
High Altitude ◽  
Sea Level ◽  
Archaeological Site ◽  
The Tibetan Plateau ◽  
Human Occupation ◽  
Modern Humans ◽  
The World ◽  
History Of

The Tibetan Plateau is the highest and one of the most demanding environments ever inhabited by humans. We investigated the timing and mechanisms of its initial colonization at the Nwya Devu site, located nearly 4600 meters above sea level. This site, dating from 40,000 to 30,000 years ago, is the highest Paleolithic archaeological site yet identified globally. Nwya Devu has yielded an abundant blade tool assemblage, indicating hitherto-unknown capacities for the survival of modern humans who camped in this environment. This site deepens the history of the peopling of the “roof of the world” and the antiquity of human high-altitude occupations more generally.

scholarly journals Condensing Life Substances within the House: The Rice-Boiling Shuhi of Southwest China

2017 ◽  
Vol 71 (1) ◽  
Author(s):  
Elisabeth Hsu ◽  
Franz K. Huber ◽  
Caroline S. Weckerle
Keyword(s):  
Tibetan Plateau ◽  
Southeast Asia ◽  
High Altitude ◽  
Sea Level ◽  
Ethnic Groups ◽  
Southwest China ◽  
Cultural Practice ◽  
The Tibetan Plateau ◽  
Regional Culture ◽  
Fault Line

AbstractThe Shuhi of Muli County, Sichuan Province, are one of multiple ethnic groups inhabiting the river gorges of the Qinghai-Gansu-Sichuan corridor between the Tibetan plateau and the Chinese lowlands. The Shuhi have grown paddy rice since times immemorial at an unusually high altitude (ca. 2,300 m above sea level). This article aims to explain this conundrum not merely through the ecology (as is common among Tibetan area specialists), but by researching the cultivation and consumption of rice as a historically-evolved cultural practice. According to a recently formulated agro-archaeological hypothesis regarding the macro-region of Eurasia, it is possible to identify two supra-regional culture complexes distinguished by their respective culinary technologies: rice-boiling versus wheat-grinding-and-baking. The hypothesis posits that the fault line between the two supra-regional cultural complexes is precisely along this river gorges corridor. In this article we provide support for this hypothesis arguing that Shuhi ritual and kinship practices have much affinity with those of other rice-boiling peoples in Southeast Asia, whereas certain of their current religious practices are shared with the wheat-grinding Tibetans.

Melting Ice Rivers

2012 ◽  
Author(s):  
Cheryl Colopy
Keyword(s):  
Global Warming ◽  
Tibetan Plateau ◽  
The Netherlands ◽  
Sea Level ◽  
The Tibetan Plateau ◽  
Mount Everest ◽  
The Past ◽  
The North ◽  
The World ◽  
The Government

From a remote outpost of global warming, a summons crackles over a two-way radio several times a week: . . . Kathmandu, Tsho Rolpa! Babar Mahal, Tsho Rolpa! Kathmandu, Tsho Rolpa! Babar Mahal, Tsho Rolpa! . . . In a little brick building on the lip of a frigid gray lake fifteen thousand feet above sea level, Ram Bahadur Khadka tries to rouse someone at Nepal’s Department of Hydrology and Meteorology in the Babar Mahal district of Kathmandu far below. When he finally succeeds and a voice crackles back to him, he reads off a series of measurements: lake levels, amounts of precipitation. A father and a farmer, Ram Bahadur is up here at this frigid outpost because the world is getting warmer. He and two colleagues rotate duty; usually two of them live here at any given time, in unkempt bachelor quarters near the roof of the world. Mount Everest is three valleys to the east, only about twenty miles as the crow flies. The Tibetan plateau is just over the mountains to the north. The men stay for four months at a stretch before walking down several days to reach a road and board a bus to go home and visit their families. For the past six years each has received five thousand rupees per month from the government—about $70—for his labors. The cold, murky lake some fifty yards away from the post used to be solid ice. Called Tsho Rolpa, it’s at the bottom of the Trakarding Glacier on the border between Tibet and Nepal. The Trakarding has been receding since at least 1960, leaving the lake at its foot. It’s retreating about 200 feet each year. Tsho Rolpa was once just a pond atop the glacier. Now it’s half a kilometer wide and three and a half kilometers long; upward of a hundred million cubic meters of icy water are trapped behind a heap of rock the glacier deposited as it flowed down and then retreated. The Netherlands helped Nepal carve out a trench through that heap of rock to allow some of the lake’s water to drain into the Rolwaling River.

Roof of the World: Tibet, Pamirs

2013 ◽  
Author(s):  
Mike Searle
Keyword(s):  
Tibetan Plateau ◽  
High Elevation ◽  
Tien Shan ◽  
Palm Tree ◽  
The Tibetan Plateau ◽  
Wet Season ◽  
North West ◽  
Mountain Ranges ◽  
The North ◽  
The World

The Tibetan Plateau is by far the largest region of high elevation, averaging just above 5,000 metres above sea level, and the thickest crust, between 70 and 90 kilometres thick, anywhere in the world. This huge plateau region is very flat—lying in the internally drained parts of the Chang Tang in north and central Tibet, but in parts of the externally drained eastern Tibet, three or four mountain ranges larger and higher than the Alps rise above the frozen plateau. Some of the world’s largest and longest mountain ranges border the plateau, the ‘flaming mountains’ of the Tien Shan along the north-west, the Kun Lun along the north, the Longmen Shan in the east, and of course the mighty Himalaya forming the southern border of the plateau. The great trans-Himalayan mountain ranges of the Pamir and Karakoram are geologically part of the Asian plate and western Tibet but, as we have noted before, unlike Tibet, these ranges have incredibly high relief with 7- and 8-kilometre-high mountains and deeply eroded rivers and glacial valleys. The western part of the Tibetan Plateau is the highest, driest, and wildest area of Tibet. Here there is almost no rainfall and rivers that carry run-off from the bordering mountain ranges simply evaporate into saltpans or disappear underground. Rivers draining the Kun Lun flow north into the Takla Makan Desert, forming seasonal marshlands in the wet season and a dusty desert when the rivers run dry. The discovery of fossil tropical leaves, palm tree trunks, and even bones from miniature Miocene horses suggest that the climate may have been wetter in the past, but this is also dependent on the rise of the plateau. Exactly when Tibet rose to its present elevation is a matter of great debate. Nowadays the Indian Ocean monsoon winds sweep moisture-laden air over the Indian sub-continent during the summer months (late June–September). All the moisture is dumped as the summer monsoon, the torrential rains that sweep across India from south-east to north-west.

scholarly journals Plant phenological sensitivity to climate change on the Tibetan Plateau and relative to other areas of the world

Ecosphere ◽  
2019 ◽  
Vol 10 (1) ◽  
Author(s):  
Ji Suonan ◽  
Aimée T. Classen ◽  
Nathan J. Sanders ◽  
Jin‐Sheng He
Keyword(s):  
Climate Change ◽  
Tibetan Plateau ◽  
The Tibetan Plateau ◽  
The World ◽  
Phenological Sensitivity

scholarly journals Early evidence for the use of wheat and barley as staple crops on the margins of the Tibetan Plateau

2015 ◽  
Vol 112 (18) ◽  
pp. 5625-5630 ◽  
Author(s):  
Jade A. d’Alpoim Guedes ◽  
Hongliang Lu ◽  
Anke M. Hein ◽  
Amanda H. Schmidt
Keyword(s):  
Tibetan Plateau ◽  
East Asia ◽  
High Altitude ◽  
Niche Modeling ◽  
Western China ◽  
The Tibetan Plateau ◽  
Thermal Niche ◽  
Early Evidence ◽  
Early Use ◽  
Staple Crops

We report directly dated evidence from circa 1400 calibrated years (cal) B.C. for the early use of wheat, barley, and flax as staple crops on the borders of the Tibetan Plateau. During recent years, an increasing amount of data from the Tibetan Plateau and its margins shows that a transition from millets to wheat and barley agriculture took place during the second millennium B.C. Using thermal niche modeling, we refute previous assertions that the ecological characteristics of wheat and barley delayed their spread into East Asia. Rather, we demonstrate that the ability of these crops to tolerate frost and their low growing degree-day requirements facilitated their spread into the high-altitude margins of western China. Following their introduction to this region, these crops rapidly replaced Chinese millets and became the staple crops that still characterize agriculture in this area today.

scholarly journals Ancient mitogenomes show plateau populations from last 5200 years partially contributed to present-day Tibetans

2020 ◽  
Vol 287 (1923) ◽  
pp. 20192968 ◽  
Author(s):  
Manyu Ding ◽  
Tianyi Wang ◽  
Albert Min-Shan Ko ◽  
Honghai Chen ◽  
Hui Wang ◽  
...  
Keyword(s):  
Mitochondrial Dna ◽  
Deep Learning ◽  
Tibetan Plateau ◽  
High Altitude ◽  
Simulation Models ◽  
The Tibetan Plateau ◽  
Limited Evidence ◽  
Complete Continuity ◽  
Genetic Origins ◽  
Low Altitude

The clarification of the genetic origins of present-day Tibetans requires an understanding of their past relationships with the ancient populations of the Tibetan Plateau. Here we successfully sequenced 67 complete mitochondrial DNA genomes of 5200 to 300-year-old humans from the plateau. Apart from identifying two ancient plateau lineages (haplogroups D4j1b and M9a1a1c1b1a) that suggest some ancestors of Tibetans came from low-altitude areas 4750 to 2775 years ago and that some were involved in an expansion of people moving between high-altitude areas 2125 to 1100 years ago, we found limited evidence of recent matrilineal continuity on the plateau. Furthermore, deep learning of the ancient data incorporated into simulation models with an accuracy of 97% supports that present-day Tibetan matrilineal ancestry received partial contribution rather than complete continuity from the plateau populations of the last 5200 years.

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