The Penghu Channel (Chinese: 澎湖水道; pinyin: Pēnghú Hángdào) or Pescadores Channel is the body of water that separates the Penghu islands from the main island of Taiwan and links the Taiwan Strait to the northeastern South China Sea. The channel has been considered narrow and potentially difficult to navigate in monsoon season. The channel is known for Pleistocene aged fossils dredged up from bottom sediments, including the archaic human mandible Penghu 1 as well as the extinct elephant Palaeoloxodon huaihoensis.
>>>PUT SHARE BUTTONS HERE<<<
👉 Penghu Channel in the context of Penghu
The Penghu (/ˈpʌŋˈhuː/ PUNG-HOO, Hokkien POJ: Phîⁿ-ô͘ or Phêⁿ-ô͘ ) or Pescadores Islands are an archipelago of 90 islands and islets in the Taiwan Strait, about 50 kilometres (25 nautical miles) west of the main island of Taiwan across the Penghu Channel, covering an area of 141 km (54 sq mi). The archipelago collectively forms Penghu County. The largest city is Magong, on the largest island, which is also named Magong.
The Penghu islands first appear in the historical record in the Tang dynasty and were inhabited by Chinese people under the Southern Song dynasty, during which they were attached to Jinjiang County of Fujian. The archipelago was formally incorporated as an administrative unit of China in 1281 under Tong'an County of Jiangzhe Province in the Yuan dynasty. It continued to be controlled by Imperial China with brief European occupations by the Dutch Empire (1622–1624) and Second French colonial empire (1885), until it was ceded to the Empire of Japan in 1895. Japan’s surrender in 1945 ended its colonial rule over the Islands, which has since then been governed by the Republic of China (ROC). Under the terms of the Sino-American Mutual Defense Treaty and the subsequent Taiwan Relations Act between the ROC and the United States, Penghu is defined and geographically acknowledged as part of Taiwan.
In this Dossier
Penghu Channel in the context of Denisovan
The Denisovans or Denisova hominins (/dəˈniːsəvə/ də-NEE-sə-və) are an extinct species or subspecies of archaic human that ranged across Asia during the Middle to Late Pleistocene, approximately 200,000–32,000 years ago. Most of what is known about Denisovans comes from DNA evidence. While many recent fossils have been found and tentatively identified as Denisovan, the first Denisovans discovered were known from few physical remains. Consequently, no formal species name has been established. However, an analysis of the mitochondrial DNA and endogenous proteins from the Harbin cranium, which had been given the name Homo longi, showed with great certainty that this species represents a Denisovan.In a study published in September 2025, remains from six additional sites in China including the 1 million year old Yunxian man were proposed to be included in the species Homo longi along with the genetically confirmed Denisovans.
The first identification of a Denisovan individual occurred in 2010, based on mitochondrial DNA (mtDNA) extracted from a juvenile finger bone excavated from the Siberian Denisova Cave in the Altai Mountains in 2008. Nuclear DNA indicates close affinities with Neanderthals. The cave was also periodically inhabited by Neanderthals. Additional specimens from Denisova Cave were subsequently identified, as were specimens from the Baishiya Karst Cave on the Tibetan Plateau, Tam Ngu Hao 2 Cave in the Annamite Mountains of Laos, the Penghu channel between Taiwan and the mainland, and Harbin in Manchuria.