Min Chinese
A diverse Sinitic language group with deep historical roots.
via Wikipedia: Min Chinese · see source
Min refers to a broad family of Sinitic languages spoken by around 75 million people as their first language. These languages are primarily found in China, centered on modern Fujian Province, and extending from southern Zhejiang to eastern Guangdong, as well as on Hainan Island and the nearby Leizhou Peninsula. Min varieties are also used in Taiwan and among large overseas communities, especially in Southeast Asia. The term "Min" comes from the Min River in Fujian and also serves as the province's abbreviated name. Different Min languages are not mutually intelligible with each other or with other Chinese varieties.
Outside China, the most widespread Min variety is Hokkien, a form of Southern Min originating in southern Fujian. In Fujian, the prestige dialect of Hokkien is Amoy Hokkien, while most people in Taiwan speak a dialect known as Taiwanese Hokkien or simply Taiwanese. The majority of Chinese Singaporeans, Chinese Malaysians, Chinese Filipinos, Chinese Indonesians, Chinese Thais, and Chinese Cambodians trace their roots to Southern Min-speaking communities (especially Hokkien and Teochew), though some of these groups are shifting to national or regional languages. Communities speaking Eastern Min, Pu-Xian Min, Haklau Min, Leizhou Min, and Hainanese also exist in parts of the diaspora, such as in Malaysia, Singapore, and Indonesia.
Unlike other Chinese language branches that descend from Middle Chinese of the Sui and Tang dynasties, Min languages have preserved some features of Old Chinese that were lost elsewhere. They are also thought to have a linguistic substrate from the languages spoken in the region before it was sinicized.
**History**
The Min homeland of Fujian was opened to Han Chinese settlement after Emperor Wu of Han defeated the Minyue state in 110 BC. The area is rugged and mountainous, with short rivers flowing into the South China Sea. Most later migration from northern to southern China passed through the valleys of the Xiang and Gan rivers to the west, so Min varieties experienced less northern influence than other southern groups. Consequently, while most Chinese varieties derive from Middle Chinese—the language described in rhyme dictionaries like the *Qieyun* (601 AD)—Min varieties contain traces of even older distinctions. Linguists estimate that the oldest layers of Min dialects split from the rest of Chinese around the time of the Han dynasty.
Significant waves of migration from the North China Plain followed: the Upheaval of the Five Barbarians during the Jin dynasty, especially the Disaster of Yongjia in 311 AD, triggered a tide of immigration southward. In 669, Chen Zheng and his son Chen Yuanguang from Gushi County in Henan established a regional administration in Fujian to suppress a rebellion by the She people. Wang Chao was appointed governor of Fujian in 893, near the end of the Tang dynasty, and brought tens of thousands of troops from Henan. In 909, after the Tang fell, his son Wang Shenzhi founded the Min Kingdom, one of the Ten Kingdoms during the Five Dynasties and Ten Kingdoms period.
Jerry Norman identifies four main layers in the vocabulary of modern Min varieties: a non-Chinese substratum from the original languages of Minyue, which Norman and Mei Tsu-lin hypothesized were Austroasiatic; the earliest Chinese layer, brought to Fujian by settlers from Zhejiang during the Han dynasty (comparable to Eastern Han Chinese); a layer from the Northern and Southern dynasties period, largely consistent with the phonology of the *Qieyun* dictionary (Early Middle Chinese); and a literary layer based on the koiné of Chang'an, the Tang dynasty capital (Late Middle Chinese). Laurent Sagart (2008) disagrees with Norman and Mei Tsu-lin's analysis of an Austroasiatic substratum in Min. The hypothesis of an Austroasiatic homeland along the middle Yangtze has been largely abandoned by most scholars and lacks support from the majority of Austroasiatic specialists. Instead, recent analysis of archaeological evidence suggests an Austronesian layer rather than an Austroasiatic one.
**Geographic location and subgrouping**
Min is usually classified as one of seven or ten groups of Chinese varieties, but it has greater dialectal diversity than any other group. Varieties used in neighboring counties—and even in adjacent villages in the mountains of western Fujian—are often mutually unintelligible. Early classifications, such as those by Li Fang-Kuei in 1937 and Yuan Jiahua in 1960, divided Min into Northern and Southern subgroups. However, a 1963 survey report by Pan Maoding and colleagues argued that the primary split is between inland and coastal groups. A key difference between the two is a set of words that have a lateral initial /l/ in coastal varieties but a voiceless fricative /s/ or /ʃ/ in inland varieties, contrasting with another group that has /l/ in both areas. Norman reconstructs these initials in Proto-Min as voiceless and voiced laterals that merged in coastal varieties.
**Coastal Min**
Coastal varieties account for the vast majority of speakers and have spread from their homeland in Fujian and eastern Guangdong to Taiwan, Hainan, other coastal areas of southern China, and Southeast Asia. Pan and colleagues divided them into three groups: Eastern Min (Min Dong), centered on Fuzhou, the capital of Fujian, with the Fuzhou dialect as the prestige form (also including the Fuqing dialect, etc.); the Longdu and Nanlang dialects of Zhongshan Min in Guangdong province; and Pu-Xian Min, spoken in the city of Putian and Xianyou County. Li Rulong and Chen Zhangtai examined 214 words and found that Pu-Xian Min shares 62% with the Quanzhou dialect (Southern Min) and 39% with the Fuzhou dialect.
- native_speakers
- about 75 million
- region
- Fujian Province, Southern Zhejiang, Eastern Guangdong, Hainan Island, Leizhou Pe
- language_family
- Sinitic (Chinese)
- notable_feature
- retains features of Old Chinese lost in other branches; believed to have a lingu
- most_widely_spoken_outside_China
- Hokkien (Southern Min)
Verified Timeline
Lore & Background
The Min homeland of Fujian was opened to Han Chinese settlement by the defeat of the Minyue state by the armies of Emperor Wu of Han in 110 BC. The area features rugged mountainous terrain, with short rivers that flow into the South China Sea. Most subsequent migration from north to south China passed through the valleys of the Xiang and Gan rivers to the west, so that Min varieties have experienced less northern influence than other southern groups. As a result, whereas most varieties of Chinese can be treated as derived from Middle Chinese, the language that is described by rhyme dictionaries such as the Qieyun (601 AD), Min varieties contain traces of older distinctions. Linguists estimate that the oldest layers of the Min dialects diverged from the rest of Chinese around the time of the Han dynasty. Significant waves of migration from the North China Plain occurred: the Upheaval of the Five Barbarians during the Jin dynasty, particularly the Disaster of Yongjia in 311 AD, caused a tide of immigration to the south. In 669, Chen Zheng and his son Chen Yuanguang from Gushi County in Henan set up a regional administration in Fujian to suppress an insurrection by the She people. Wang Chao was appointed governor of Fujian in 893, near the end of the Tang dynasty, and brought tens of thousands of troops from Henan. In 909, following the fall of the Tang dynasty, his son Wang Shenzhi founded the Min Kingdom, one of the Ten Kingdoms in the Five Dynasties and Ten Kingdoms period. Jerry Norman identifies four main layers in the vocabulary of modern Min varieties: a non-Chinese substratum from the original languages of Minyue, which Norman and Mei Tsu-lin hypothesize were Austroasiatic; the earliest Chinese layer, brought to Fujian by settlers from Zhejiang to the north during the Han dynasty; a layer from the Northern and Southern dynasties period, which is largely consistent with the phonology of the Qieyun dictionary (Early Middle Chinese); and a literary layer based on the koiné of Chang'an, the capital of the Tang dynasty (Late Middle Chinese). Laurent Sagart (2008) disagrees with Norman and Mei Tsu-lin's analysis of an Austroasiatic substratum in Min. The hypothesis proposed by Jerry Norman and Mei Tsu-lin arguing for an Austroasiatic homeland along the middle Yangtze has been largely abandoned in most circles and left unsupported by the majority of Austroasiatic specialists. Rather, recent movements of analyzing archeological evidence, posit an Austronesian layer, rather than an Austroasiatic one.
Reader's Guide
Min is usually described as one of seven or ten groups of varieties of Chinese but has greater dialectal diversity than any of the other groups. The varieties used in neighbouring counties, and in the mountains of western Fujian even in adjacent villages, are often mutually unintelligible. Early classifications, such as those of Li Fang-Kuei in 1937 and Yuan Jiahua in 1960, divided Min into Northern and Southern subgroups. However, in a 1963 report on a survey of Fujian, Pan Maoding and colleagues argued that the primary split was between inland and coastal groups. A key discriminator between the two groups is a group of words that have a lateral initial /l/ in coastal varieties, and a voiceless fricative /s/ or /ʃ/ in inland varieties, contrasting with another group having /l/ in both areas. Norman reconstructs these initials in Proto-Min as voiceless and voiced laterals that merged in coastal varieties. The coastal varieties have the vast majority of speakers, and have spread from their homeland in Fujian and eastern Guangdong to the islands of Taiwan and Hainan, to other coastal areas of southern China, and to Southeast Asia. Pan and colleagues divided them into three groups: Eastern Min (Min Dong), centered around the city of Fuzhou; Pu-Xian Min, spoken in the city of Putian and the county of Xianyou County; and Southern Min (Min Nan), originating from the south of Fujian and the eastern corner of Guangdong. In popular usage, Southern Min usually refers to dialects of the Quanzhang type, which originated in southern Fujian (around Quanzhou, Zhangzhou and Xiamen) and spread to Southeast Asia, where they are known as Hokkien, and Taiwan, where they are known as Taiwanese. The dialects of the Teoswa / Chaoshan region of eastern Guangdong, including Teochew and Swatow dialects, have difficult mutual intelligibility with the Amoy dialect of Hokkien. The Language Atlas of China (1987) distinguished two further groups previously included in Southern Min: Leizhou Min, spoken on the Leizhou Peninsula in southwestern Guangdong, and Hainanese, spoken on the island of Hainan. Coastal varieties feature some uniquely Min vocabulary, including pronouns and negatives. All but the Hainan dialects have complex tone sandhi systems. Although they have far fewer speakers, the inland varieties show much greater variation than the coastal ones. Pan and colleagues divided the inland varieties into two groups: Northern Min (Min Bei), spoken in Nanping prefecture in Fujian, with Jian'ou dialect taken as typical, and Central Min (Min Zhong), spoken in Sanming prefecture. The Language Atlas of China (1987) included a further group: Shao-Jiang Min, spoken in the northwestern Fujian counties of Shaowu and Jiangle, which were classified as Hakka by Pan and his associates, but Jerry Norman suggested they were inland varieties of Min that had been subject to heavy Gan or Hakka influence. Inland varieties have little or no tone sandhi.
Did You Know?
- The Min languages are not mutually intelligible with one another or with other varieties of Chinese.
- Linguists estimate that the oldest layers of the Min dialects diverged from the rest of Chinese around the time of the Han dynasty.
- Jerry Norman identifies four main layers in the vocabulary of modern Min varieties, including a non-Chinese substratum hypothesized to be Austroasiatic.
- The Min homeland of Fujian was opened to Han Chinese settlement by the defeat of the Minyue state by the armies of Emperor Wu of Han in 110 BC.
- In 909, Wang Shenzhi founded the Min Kingdom, one of the Ten Kingdoms in the Five Dynasties and Ten Kingdoms period.
Frequently Asked Questions
What is Min Chinese?
Min is not a single language but a diverse group of Sinitic (Chinese) languages that share deep historical roots. Its varieties are not mutually intelligible with one another or with other branches of Chinese.
How many people speak Min and where are they found?
Roughly 75 million native speakers use Min varieties. The core area is Fujian Province, but Min is also spoken in Southern Zhejiang, Eastern Guangdong, Hainan Island, the Leizhou Peninsula, Taiwan, and across a large Southeast Asian diaspora.
What makes Min linguistically distinctive?
Min varieties retain phonological and grammatical features of Old Chinese that have disappeared in other Sinitic branches. Researchers also believe they carry a linguistic substrate inherited from the pre-sinicization populations of the region.
Which Min variety has the largest presence outside mainland China?
Hokkien, often called Southern Min, is the most widely spoken Min variety beyond China's borders. It enjoys a particularly strong foothold within the Southeast Asian diaspora.
Can a Min speaker understand Mandarin or Cantonese?
No. Min varieties are not mutually intelligible with each other, nor with other Chinese varieties such as Mandarin or Cantonese, which is why they are treated as a distinct branch within the Sinitic family.
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