Baishiya Karst Cave
|Location||Xiahe County, Gansu, China|
|Region||Ganjia Basin, Tibetan Plateau|
|Altitude||3,280 m (10,761 ft)|
|Length||> 1 km (3,281 ft)|
|Width||20 m (66 ft)|
|Height||10 m (33 ft)|
|Archaeologists||Zhang Dongju, Chen Fahu|
Baishiya Karst Cave (Chinese: 白石崖溶洞) is a Tibetan Buddhist sanctuary and a high-altitude paleoanthropological site located on the northeastern edge of the Tibetan Plateau in Xiahe County, Gansu, China. This karst cave is the site of the discovery of the earliest hominin fossil found on the Tibetan Plateau, the Xiahe mandible. The mandible, by way of palaeoproteomic analysis, is the first confirmed discovery of a Denisovan fossil outside of Denisova Cave. This fossil discovery shows that archaic hominins were present in a high-altitude, low-oxygen environment by around 160,000 years ago.
Baishiya Karst Cave is located in Ganjia (甘加镇), Xiahe County, Gannan Tibetan Autonomous Prefecture, Gansu, China, on the northeastern edge of the Tibetan Plateau. It lies on the southern side of Dalijiashan Mountain, at the foot of a white cliff. The cave is situated in the Ganjia Basin, at the mouth of the Jiangla River, a tributary of the Yangqu River. The cave is over 1 km (3,281 ft) in length. Within 80 metres (260 ft) from the entrance, the cave's winter daytime temperature is normally 8–9 °C (46–48 °F), suitable for habitation in the harsh winters of the Tibetan Plateau.
Baishiya Karst Cave is a Tibetan Buddhist sanctuary lying north of Baishiya Temple. Said to be a former abode of Padmasambhava and the bodhisattva Tara, it is a popular location for monks to fast and meditate. It is also a pilgrimage site for Tibetan Buddhists and a tourist attraction. In 1982, the 10th Panchen Lama paid homage to the site. According to legend, the cave is more than 50 kilometres (31 mi) long and goes all the way to Xunhua County in Qinghai province.
In 1980, a Tibetan monk who was meditating in the cave discovered the Xiahe mandible. He passed the fossil to Jigme Tenpe Wangchug, the sixth Gungthang tulku, who donated it to Lanzhou University. The mandible was so unusual that researchers did not know how to classify it. Scientists Chen Fahu and Zhang Dongju began studying the site in 2010, while collaboration with the Max Planck Institute for Evolutionary Anthropology began in 2016. The first archaeological survey at the site was performed in 2016, while the first systematic excavation did not take place until 2018. Several lithic artefacts and animal bones with cut marks were discovered at the entrance to the cave.
The Xiahe mandible consists of the right half of a partial mandible with two attached molars. By way of protein analysis, researchers concluded that the Xiahe specimen belonged to a population that was closely related to the Denisovan specimens from Denisova Cave. This is the first time that an ancient hominin was successfully identified using only protein analysis. It is the most complete known Denisovan fossil.
- Chen, Fahu; Welker, Frido; Shen, Chuan-Chou; Bailey, Shara E.; Bergmann, Inga; Davis, Simon; Xia, Huan; Wang, Hui; Fischer, Roman; Freidline, Sarah E.; Yu, Tsai-Luen; Skinner, Matthew M.; Stelzer, Stefanie; Dong, Guangrong; Fu, Qiaomei; Dong, Guanghui; Wang, Jian; Zhang, Dongju; Hublin, Jean-Jacques (2019-05-01). "A late Middle Pleistocene Denisovan mandible from the Tibetan Plateau" (PDF). Nature. Springer Science and Business Media LLC. 569 (7756): 409–412. doi:10.1038/s41586-019-1139-x. ISSN 0028-0836. PMID 31043746.
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