Prehistory of Taiwan

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Most information about Taiwan before the arrival of the Dutch East India Company in 1624 comes from archaeological finds throughout the island. The earliest evidence of human habitation dates back 20,000 to 30,000 years, when lower sea levels exposed the Taiwan Strait as a land bridge. Around 5,000 years ago, farmers from the southeast Chinese coast settled on the island. These people are believed to have been speakers of Austronesian languages, which dispersed from Taiwan across the islands of the Pacific and Indian Oceans. The current Taiwanese aborigines are believed to be their descendants.

Contents

Geographical context

Taiwan is separated from southeast China by the shallow Taiwan Strait. Taiwan relief location map.png
Taiwan is separated from southeast China by the shallow Taiwan Strait.

The island of Taiwan was formed approximately 4 to 5 million years ago on a complex convergent boundary between the continental Eurasian Plate and the oceanic Philippine Sea Plate. The boundary continues southwards in the Luzon Volcanic Arc, a chain of islands between Taiwan and the Philippine island of Luzon including Green Island and Orchid Island. From the northern part of the island the eastward continuation of the boundary is marked by the Ryukyu chain of volcanic islands. [1] [2]

The island is separated from the coast of Fujian to the west by the Taiwan Strait, which is 130 km (81 mi) wide at its narrowest point. The most significant islands in the Strait are the Penghu islands 45 km (28 mi) from the southwest coast of Taiwan and 140 km (87 mi) from the Chinese coast. Part of the continental shelf, the Strait is no more than 100 m (330 ft) deep, and has become a land bridge during glacial periods. [3]

Taiwan is a tilted fault block, with rugged longitudinal mountain ranges making up most of the eastern two-thirds of the island. They include more than two hundred peaks with elevations of over 3,000 m (9,800 ft). The western side of the island slopes down to fertile coastal plains. The island straddles the Tropic of Cancer, and has a humid subtropical climate. [4] The original vegetation ranged from tropical rainforest in the lowlands through temperate forests, boreal forest and alpine plants with increasing altitude. [5]

Late Paleolithic

Partial jawbone found between Penghu and Taiwan, designated Penghu 1 Fossil of Mandible of Penghu 1.JPG
Partial jawbone found between Penghu and Taiwan, designated Penghu 1

During the Late Pleistocene glaciation, sea levels in the area were about 140 m (460 ft) lower than in the present day. As a result, the floor of the Taiwan Strait was exposed as a broad land bridge that was crossed by mainland fauna until the beginning of the Holocene 10,000 years ago. [3] A concentration of vertebrate fossils has been found in the channel between the Penghu Islands and Taiwan, including a partial jawbone designated Penghu 1, apparently belonging to a previously unknown species of genus Homo . These fossils are likely to date from one of the two most recent periods when the Strait was exposed, 10–70 kya and 130–190 kya. [6]

The Ryukyu Islands to the northeast of Taiwan were settled during marine isotope stage (MIS) 3, which ended around 30,000 years ago. It is likely that the southern (and possibly central) Ryukyus were settled via voyages from Taiwan. [7]

In 1972, fragmentary fossils of anatomically modern humans were found at Chouqu and Gangzilin, in Zuojhen District, Tainan, in fossil beds exposed by erosion of the Cailiao River. Though some of the fragments are believed to be more recent, three cranial fragments and a molar tooth have been dated as between 20,000 and 30,000 years old. The find has been dubbed "Zuozhen Man". No associated artifacts have been found at the site. [8] [9]

The oldest known artifacts are chipped-pebble tools of the Changbin culture (長濱文化), found at cave sites on the southeast coast of the island. The sites are dated 15,000 to 5,000 years ago, and similar to contemporary sites in Fujian. The primary site of Baxiandong (八仙洞), in Changbin, Taitung was first excavated in 1968. The same culture has been found at sites at Eluanbi on the southern tip of Taiwan, persisting until 5,000 years ago. The earliest layers feature large stone tools, and suggest a hunting and gathering lifestyle. Later layers have small stone tools of quartz, as well as tools made from bone, horn and shell, and suggest a shift to intensive fishing and shellfish collection. [10] [11]

The distinct Wangxing culture (網形) was discovered in Miaoli County in northwest Taiwan in the 1980s. The assemblage consists of flake tools, becoming smaller and more standardized over time, and indicating a shift from gathering to hunting. [12]

Analysis of spores and pollen grains in sediment of Sun Moon Lake suggests that traces of slash-and-burn agriculture started in the area since 11,000 years ago, and ended 4,200 years ago, when abundant remains of rice cultivation were found. [13]

The only Paleolithic burial that has been found on Taiwan was in Xiaoma cave in Chenggong in the southeast of the island, dating from about 4000 BC, of a male similar in type to Negritos found in the Philippines. There are also references in Chinese texts and Formosan Aboriginal oral traditions to pygmies on the island at some time in the past. [14] [15]

In December 2011, a skeleton dated about 8,000 years ago was found on Liang Island, off the north coast of Fujian. In 2014, the mitochondrial DNA of the Liangdao Man skeleton was found to belong to Haplogroup E, which is today found throughout Maritime Southeast Asia. Morover, it had two of the four mutations characteristic of the E1 subgroup. From this, Ko et al. infer that Haplogroup E arose 8,000 to 11,000 years ago on the north Fujian coast, travelled to Taiwan with Neolithic settlers 6,000 years ago, and from there spread to Maritime Southeast Asia with the Austronesian language dispersal. [16] Soares et al. caution against overemphasizing a single sample, and maintain that a constant molecular clock implies an earlier date (and more southerly origin) for Haplogroup E remains more likely. [17]

Neolithic

Expansion of Austronesian languages and associated archeological cultures Chronological dispersal of Austronesian people across the Pacific.svg
Expansion of Austronesian languages and associated archeological cultures

Between 4000 and 3000 BC, the Dapenkeng culture (named after a site in Taipei county) abruptly appeared and quickly spread around the coast of the island, as well as Penghu. Dapenkeng sites are relatively homogeneous, characterized by pottery impressed with cord marks, pecked pebbles, highly polished stone adzes and thin points of greenish slate. The inhabitants cultivated rice and millet, and engaged in hunting, but were also heavily reliant on marine shells and fish. Most scholars believe this culture is not derived from the Changbin culture, but was brought across the Strait by the ancestors of today's Taiwanese aborigines, speaking early Austronesian languages. No ancestral culture on the mainland has been identified, but a number of shared features suggest ongoing contacts. [18] [19] However, the overall neolithic-era of Taiwan strait is said, by scholars, to have been descended from Neolithic cultures in the lower Yangtze area, particularly the Hemudu and Majiabang cultures. [20] Physical similarity has been noted between the people of these cultures and the Neolithic inhabitants of Taiwan. [21]

Monolith from the Beinan culture Beinan monolith.png
Monolith from the Beinan culture

In the following millennium, these technologies appeared on the northern coast of the Philippine island of Luzon (250 km south of Taiwan), where they, and presumably Austronesian languages, were adopted by the local population. This migration created a branch of Austronesian, the Malayo-Polynesian languages, which have since dispersed across a huge area from Madagascar to Hawaii, Easter Island and New Zealand. All other primary branches of Austronesian are found only on Taiwan, the urheimat of the family. [22] [23] [24]

The successors of the Dapenkeng culture throughout Taiwan were locally differentiated. The Fengpitou (鳳鼻頭) culture, characterized by fine red cord-marked pottery, was found in Penghu and the central and southern parts of the western side of the island, and a culture with similar pottery occupied the eastern coastal areas. These later differentiated into the Niumatou and Yingpu cultures in central Taiwan, the Niuchouzi (牛稠子) and Dahu cultures in the southwest, the Beinan Culture in the southeast and the Qilin (麒麟) culture in the central east. The Yuanshan culture (圓山) in the northeast does not appear to be closely related to these, featuring sectioned adzes, shouldered-stone adzes and pottery without cord impressions. Some scholars suggest that it represents another wave of immigration from southeast China, but no similar culture is known from there either. [25]

Archaeological evidence of prehistoric cultures dating back 4500 years before present was found in Nangang Village, Cimei, Penghu in 1983. [26] :314

The Niuchouzi Culture flourished around what is now Tainan 2,500 BC to 1,000 BC. They are known for orange pottery decorated with rope patterns. [27]

In the early Neolithic period, jade was used only for tools such are adzes, axes and spear points. From about 2500 BC, jade ornaments began to be produced, peaking in sophistication between 1500 BC and 1 AD, particularly in the Beinan Culture of southern Taiwan. All the jade found on Taiwan came from a deposit of green nephrite at Fengtian, near modern Hualien City. Nephrite from Taiwan began to appear in the northern Philippines between 1850 and 1350 BC, spawning the Philippine jade culture. Around the beginning of the Common Era, artisans in Taiwan switched from jade to metal, glass and carnelian. However, Philippine craftsmen continued to work jade from Taiwan until around 1000 AD, producing lingling-o pendants and other ornaments, which have been found throughout southeast Asia. [28] [29]

Iron Age

A young Tsou man Tsou youth of Taiwan (pre-1945).jpg
A young Tsou man

Artifacts of iron and other metals appeared on Taiwan around the beginning of the Common Era. At first these were trade goods, but by around AD 400 wrought iron was being produced locally using bloomeries, a technology possibly introduced from the Philippines. Distinct Iron Age cultures have been identified in different parts of the island: the Shihsanhang Culture (十三行文化) in the north, the Fanzaiyuan Culture (番仔園) in the northwest, the Daqiuyuan Culture (大邱園) in the hills of southwest Nantou County, the Kanding Culture in the central west, the Niaosung Culture in the southwest, the Guishan Culture (龜山) at the southern tip of the island, and the Jingpu Culture (靜浦) on the east coast. The earliest trade goods from China found on the island date from the Tang dynasty (618–907 AD). [30] [31]

Burial customs

Prehistoric groups in Taiwan practiced a wide variety of burial practices with each culture having distinct practices. Excavations of ancient gravesites are key to archeologists understanding of these early Taiwanese cultures. Grave goods buried with the dead also provide concrete evidence of complex trade linkages and intercultural exchange. Some of these ancient funerary customs are practiced by modern Taiwanese indigenous cultures but many have been lost. [32]

See also

Related Research Articles

<span class="mw-page-title-main">Taiwan</span> Country in East Asia

Taiwan, officially the Republic of China (ROC), is a country in East Asia. It is located at the junction of the East and South China Seas in the northwestern Pacific Ocean, with the People's Republic of China (PRC) to the northwest, Japan to the northeast, and the Philippines to the south. The territories controlled by the ROC consist of 168 islands with a combined area of 36,193 square kilometres. The main island of Taiwan, also known as Formosa, has an area of 35,808 square kilometres, with mountain ranges dominating the eastern two-thirds and plains in the western third, where its highly urbanized population is concentrated. The capital, Taipei, forms along with New Taipei City and Keelung the largest metropolitan area. With around 23.9 million inhabitants, Taiwan is among the most densely populated countries.

<span class="mw-page-title-main">History of Taiwan</span> History of the island of Taiwan

The history of the island of Taiwan dates back tens of thousands of years to the earliest known evidence of human habitation. The sudden appearance of a culture based on agriculture around 3000 BCE is believed to reflect the arrival of the ancestors of today's Taiwanese indigenous peoples. Han Chinese gradually came into contact with Taiwan starting in the late 13th century and started settling there by the early 17th century. Named Formosa by Portuguese explorers, the south of the island was colonized by the Dutch in the 17th century whilst the Spanish built a settlement in the north which lasted until 1642. These European settlements were followed by an influx of Hoklo and Hakka immigrants from Fujian and Guangdong.

<span class="mw-page-title-main">Taiwan Strait</span> Strait between Mainland China and Taiwan

The Taiwan Strait is a 180-kilometer -wide strait separating the island of Taiwan and Asian continent. The strait is part of the South China Sea and connects to the East China Sea to the north. The narrowest part is 130 km wide.

<span class="mw-page-title-main">Lapita culture</span> Neolithic archaeological culture in the Pacific

The Lapita culture is the name given to a Neolithic Austronesian people and their material culture, who settled Island Melanesia via a seaborne migration at around 1600 to 500 BCE. They are believed to have originated from the northern Philippines, either directly, via the Mariana Islands, or both. They were notable for their distinctive geometric designs on dentate-stamped pottery, which closely resemble the pottery recovered from the Nagsabaran archaeological site in northern Luzon. The Lapita intermarried with the Papuan populations to various degrees, and are the direct ancestors of the Austronesian peoples of Polynesia, eastern Micronesia, and Island Melanesia.

<span class="mw-page-title-main">Liangzhu culture</span> Neolithic jade culture in the Yangtze River Delta

The Liangzhuculture or civilization was the last Chinese Neolithic jade culture in the Yangtze River Delta. The culture was highly stratified, as jade, silk, ivory and lacquer artifacts were found exclusively in elite burials, while pottery was more commonly found in the burial plots of poorer individuals. This division of class indicates that the Liangzhu period was an early state, symbolized by the clear distinction drawn between social classes in funeral structures. A pan-regional urban center had emerged at the Liangzhu site in northwestern Hangzhou, Zhejiang, and elite groups from this site presided over the local centers. The Liangzhu culture was extremely influential and its sphere of influence reached as far north as Shanxi and as far south as Guangdong. The primary Liangzhu site was perhaps among the oldest Neolithic sites in East Asia that would be considered a state society. The type site at Liangzhu was discovered in Yuhang County, Zhejiang and initially excavated by Shi Xingeng in 1936.

<span class="mw-page-title-main">Paddy field</span> Flooded parcel of arable land used for growing semiaquatic rice

A paddy field is a flooded field of arable land used for growing semiaquatic crops, most notably rice and taro. It originates from the Neolithic rice-farming cultures of the Yangtze River basin in southern China, associated with pre-Austronesian and Hmong-Mien cultures. It was spread in prehistoric times by the expansion of Austronesian peoples to Island Southeast Asia, Southeast Asia including Northeastern India, Madagascar, Melanesia, Micronesia, and Polynesia. The technology was also acquired by other cultures in mainland Asia for rice farming, spreading to East Asia, Mainland Southeast Asia, and South Asia.

<span class="mw-page-title-main">Nephrite</span> Variety of jade

Nephrite is a variety of the calcium, magnesium, and iron-rich amphibole minerals tremolite or actinolite (aggregates of which also make up one form of asbestos). The chemical formula for nephrite is Ca2(Mg, Fe)5Si8O22(OH)2. It is one of two different mineral species called jade. The other mineral species known as jade is jadeite, which is a variety of pyroxene. While nephrite jade possesses mainly grays and greens (and occasionally yellows, browns, black or whites), jadeite jade, which is rarer, can also contain blacks, reds, pinks and violets. Nephrite jade is an ornamental stone used in carvings, beads, or cabochon cut gemstones. Nephrite is also the official state mineral of Wyoming.

<span class="mw-page-title-main">Sa Huỳnh culture</span>

The Sa Huỳnh culture was a culture in modern-day central and southern Vietnam that flourished between 1000 BC and 200 AD. Archaeological sites from the culture have been discovered from the Mekong Delta to Quảng Bình province in central Vietnam. The Sa Huynh people were most likely the predecessors of the Cham people, an Austronesian-speaking people and the founders of the kingdom of Champa.

<span class="mw-page-title-main">Austronesian peoples</span> Speakers of Austronesian languages

The Austronesian peoples, sometimes referred to as Austronesian-speaking peoples, are a large group of peoples in Taiwan, Maritime Southeast Asia, parts of Mainland Southeast Asia, Micronesia, coastal New Guinea, Island Melanesia, Polynesia, and Madagascar that speak Austronesian languages. They also include indigenous ethnic minorities in Vietnam, Cambodia, Myanmar, Thailand, Hainan, the Comoros, and the Torres Strait Islands. The nations and territories predominantly populated by Austronesian-speaking peoples are sometimes known collectively as Austronesia.

<span class="mw-page-title-main">Peopling of China</span> History of ancient China

In the course of the peopling of the World by Homo sapiens, East Asia was reached about 50,000 years ago. The "recent African origin" lineage of 70 kya diverged into identifiable East Eurasian and West Eurasian lineages by about 50 kya. This early East Asian lineage diverged further during the Last Glacial Maximum, contributing outgoing from Mainland Southeast Asia significantly to the peopling of the Americas via Beringia about 25 kya. After the last ice age China became cut off from neighboring island groups. The previous phenotypes of early East Asians became either replaced or prevailed among more geographically distant groups.

<span class="mw-page-title-main">Economic history of Taiwan</span> Aspect of history

The recordkeeping and development of the economic history of Taiwan started in the Age of Discovery. In the 17th century, the Europeans realized that Taiwan is located on the strategic cusp between the Far East and Southeast Asia. Two main European empires that competed to colonize it were the Dutch and Spanish Empires. Taiwan also became an intermediate destination for trade between Western European empires and East Asia states. The history of Taiwan as a colony of the Dutch Empire, Kingdom of Tungning, Qing China, and Empire of Japan between 1630 and 1945 was based heavily on economics.

In a hypothesis developed by Wilhelm Solheim, the Nusantao Maritime Trading and Communication Network (NMTCN) is a trade and communication network that first appeared in the Asia-Pacific region during its Neolithic age, or beginning roughly around 5000 BC. Nusantao is an artificial term coined by Solheim, derived from the Austronesian root words nusa "island" and tao "man, people". Solheim's theory is an alternative hypothesis to the spread of the Austronesian language family in Southeast Asia. It contrasts the more widely accepted Out-of-Taiwan hypothesis (OOT) by Peter Bellwood.

<span class="mw-page-title-main">Prehistory of the Philippines</span> History of the Philippines up to 900 AD

The prehistory of the Philippines covers the events prior to the written history of what is now the Philippines. The current demarcation between this period and the early history of the Philippines is April 21, 900, which is the equivalent on the Proleptic Gregorian calendar for the date indicated on the Laguna Copperplate Inscription—the earliest known surviving written record to come from the Philippines. This period saw the immense change that took hold of the archipelago from Stone Age cultures in 50000 BC to the emergence of developed thalassocratic civilizations in the fourth century, continuing on with the gradual widening of trade until 900 and the first surviving written records.

<span class="mw-page-title-main">Models of migration to the Philippines</span>

Since H. Otley Beyer first proposed his wave migration theory, numerous scholars have approached the question of how, when and why humans first came to the Philippines. The current scientific consensus favors the "Out of Taiwan" model, which broadly match linguistic, genetic, archaeological, and cultural evidence.

The Dapenkeng culture was an early Neolithic culture that appeared in northern Taiwan between 4000 and 3000 BC and quickly spread around the coast of the island, as well as the Penghu islands to the west. Most scholars believe this culture was brought across the Taiwan Strait by the ancestors of today's Taiwanese aborigines, speaking early Austronesian languages. No ancestral culture on the mainland has been identified, but a number of shared features suggest ongoing contacts.

The Kalanay Cave is a small cave located on the island of Masbate in central Philippines. The cave is located specifically at the northwest coast of the island within the municipality of Aroroy. The artifacts recovered from the site were similar to those found to the Sa Huynh culture of Southern Vietnam. The site is part of the "Sa Huynh-Kalanay Interaction Sphere" which was an Iron Age maritime trading network associated with the Austronesian peoples of the Philippines, Vietnam, Taiwan, as well as most of northeastern Borneo and Southern Thailand. The type of pottery found in the site were dated 400 BC to AD 1500. The "Sa Huynh-Kalanay Interaction Sphere" is characterized by a remarkable continuity in trade goods, including decorated pottery and double-headed pendants and earrings known as lingling-o.

<span class="mw-page-title-main">Philippine jade culture</span>

Philippine jade culture, or jade artifacts, made from white and green nephrite and dating as far back as 2000–1500 BC, have been discovered at a number of archaeological excavations in the Philippines since the 1930s. The artifacts have been both tools like chisels and ornaments such as lingling-o earrings, bracelets, and beads.

<span class="mw-page-title-main">Maritime Silk Road</span> Ancient and medieval maritime trade route

The Maritime Silk Road or Maritime Silk Route is the maritime section of the historic Silk Road that connected China, Southeast Asia, the Indian subcontinent, the Arabian peninsula, Somalia, Egypt and Europe. It began by the 2nd century BCE and flourished later on until the 15th century CE. Major players in the Maritime Silk Road include the merchants from the Tang, Song, Yuan and Ming dynasties of imperial China, Austronesian sailors in Southeast Asia, Tamil merchants in India and Southeast Asia, and Persian and Arab traders in the Arabian Sea and beyond. The network followed the footsteps of older maritime networks in Southeast Asia, as well as the maritime spice networks of Southeast Asia, Sri Lanka, India, and the Indian Ocean, coinciding with these ancient maritime trade roads by the current era.

<i>Lingling-o</i> Prehistoric Austronesian ornament

Lingling-o or ling-ling-o, are a type of penannular or double-headed pendant or amulet that have been associated with various late Neolithic to late Iron Age Austronesian cultures. Most lingling-o were made in jade workshops in the Philippines, and to a lesser extent in the Sa Huỳnh culture of Vietnam, although the raw jade was mostly sourced from Taiwan.

The Chimei lithic workshops were workshops for making stone tools in the mid-Neolithic period scattered around Chimei Island in Penghu County. These workshops are located at Nankang Village, Tunghu Village, and Hsihu Village in Chimei Township, Penghu County, and they can be dated back to 3,800 to 4,500 years ago.

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Further reading