Min Chinese

Min is a broad group of Sinitic languages with about 75 million native speakers. These languages are spoken in China in a region centered on modern Fujian Province, stretching from Southern Zhejiang to Eastern Guangdong, as well as on Hainan Island and the neighbouring Leizhou Peninsula. Min varieties are also spoken in Taiwan, and by a large international diaspora, particularly in Southeast Asia. The name Min is shared with the Min River in Fujian, and is also the abbreviated name of Fujian Province. Min languages are not mutually intelligible with one another nor with other varieties of Chinese.

The most widely spoken variety of Min outside of China is Hokkien, a variety of Southern Min which has its origin in Southern Fujian. Amoy Hokkien is the prestige dialect of Hokkien in Fujian, while a majority of Taiwanese people speak a dialect called Taiwanese Hokkien or simply Taiwanese. The majority of Chinese Singaporeans, Chinese Malaysians, Chinese Filipinos, Chinese Indonesians, Chinese Thais, and Chinese Cambodians are of Southern Min-speaking background (particularly Hokkien and Teochew), although some of these communities are shifting to national or regional languages. Communities speaking Eastern Min, Pu-Xian Min, Haklau Min, Leizhou Min, and Hainanese can also be found in parts of the Chinese diaspora, such as in Malaysia, Singapore, and Indonesia.

While other branches of Chinese descend from Middle Chinese of the Sui and Tang dynasties, Min languages have retained some features of Old Chinese lost in other branches. The Min languages are also believed to have a linguistic substrate from the languages of the inhabitants of the region before its sinicization.

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 described by rhyme dictionaries such as the Qieyun (601 AD)—Min varieties contain traces of older distinctions. Linguists estimate that the oldest layers of Min dialects diverged from the rest of Chinese around the time of the Han dynasty. However, significant waves of migration from the North China Plain occurred:

Jerry Norman identifies four main layers in the vocabulary of modern Min varieties:

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.

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.