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Southern Min

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(Redirected from ISO 639-3:nan)
Southern Min
  • Hoklo-Taiwanese
  • 閩南語; 闽南语
  • Bàn-lâm-gú
Geographic
distribution
Ethnicity
Linguistic classificationSino-Tibetan
Early forms
Subdivisions
Language codes
ISO 639-3nan
Linguasphere79-AAA-j
Glottologminn1241
  Southern Min in mainland China and Taiwan

Subgroups of Southern Min in mainland China and Taiwan
Chinese name
Simplified Chinese闽南语
Traditional Chinese閩南語
Literal meaning"Language of Southern Min [Fujian]"
Transcriptions
Standard Mandarin
Hanyu PinyinMǐnnányǔ
Wade–GilesMin3-nan23
IPA[mìnnǎn ỳ]
Gan
RomanizationMîn-lōm-ngî
Hakka
RomanizationMîn-nàm-ngî
Yue: Cantonese
Yale RomanizationMáhn-nàahm yúh
JyutpingMan5-naam4 jyu5
Southern Min
Hokkien POJBân-lâm-gí/Bân-lâm-gú
Eastern Min
Fuzhou BUCMìng-nàng-ngṳ̄
Northern Min
Jian'ou RomanizedMâing-nâng-ngṳ̌
Notes
  1. ^ ChaozhouShantou
  2. ^ Min is believed to have split from Old Chinese, rather than Middle Chinese like other varieties of Chinese.[1][2][3]

Southern Min (simplified Chinese: 闽南语; traditional Chinese: 閩南語; pinyin: Mǐnnányǔ; Pe̍h-ōe-jī: Bân-lâm-gí/gú; lit. 'Southern Min language'), Minnan (Mandarin pronunciation: [mìn.nǎn]) or Banlam (Min Nan Chinese pronunciation: [bàn.lǎm]), is a group of linguistically similar and historically related Chinese languages that form a branch of Min Chinese spoken in Fujian (especially the Minnan region), most of Taiwan (many citizens are descendants of settlers from Fujian), Eastern Guangdong, Hainan, and Southern Zhejiang.[4] Southern Min dialects are also spoken by descendants of emigrants from these areas in diaspora, most notably in Southeast Asia, such as Singapore, Malaysia, the Philippines, Indonesia, Brunei, Southern Thailand, Myanmar, Cambodia, Southern and Central Vietnam, San Francisco, Los Angeles and New York City. Minnan is the most widely-spoken branch of Min, with approximately 48 million speakers as of 2017–2018.[5]

The most widely spoken Southern Min language is Hokkien, which includes Taiwanese. Other varieties of Southern Min have significant differences from Hokkien, some having limited mutual intelligibility with it, others almost none. Teochew, Longyan, and Zhenan are said to have general mutual intelligibility with Hokkien, sharing similar phonology and vocabulary to a large extent.[6] On the other hand, variants such as Datian, Zhongshan, and Qiong-Lei have historical linguistic roots with Hokkien, but are significantly divergent from it in terms of phonology and vocabulary, and thus have almost no mutual intelligibility with Hokkien. Linguists tend to classify them as separate languages.

Geographic distribution

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Mainland China

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Southern Min dialects are spoken in southern Fujian, specifically in the cities of Xiamen, Quanzhou, Zhangzhou, and much of Longyan, hence the name. In addition, varieties of Southern Min are spoken in several southeastern counties of Wenzhou in Zhejiang, the Zhoushan archipelago off Ningbo in Zhejiang, the town of Sanxiang at the southern periphery of Zhongshan in Guangdong,[7] and in the Chaoshan (Teo-swa) region in Guangdong.

The variant spoken in Leizhou, Guangdong as well as in Hainan is classified as Hainanese and is not mutually intelligible with mainstream Southern Min or Teochew.[citation needed] Hainanese is classified in some schemes as part of Southern Min and in other schemes as separate.[example needed][citation needed]

Puxian Min was originally based on the Quanzhou dialect, but over time became heavily influenced by Eastern Min, eventually losing intelligibility with Southern Min.[8]

Taiwan

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The Southern Min dialects spoken in Taiwan, collectively known as Taiwanese, is a first language for most of the Hoklo people, the main ethnicity of Taiwan. The correspondence between language and ethnicity is not absolute, as some Hoklo have very limited proficiency in Southern Min while some non-Hoklo speak Southern Min fluently.[9]

Southeast Asia

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There are many Southern Min speakers among overseas Chinese in Southeast Asia. Many ethnic Chinese immigrants to the region were Hoklo from southern Fujian and brought the language to what is now present-day Malaysia and Singapore (formerly British Malaya, the Straits Settlements, and British Borneo), Indonesia (the former Dutch East Indies), the Philippines (former Spanish East Indies and later, US Philippine Islands (P.I.)), Brunei (former part of British Borneo), Southern Thailand, Myanmar (British Burma), Cambodia (former French Cambodia of French Indochina), Southern Vietnam (former French Cochinchina of French Indochina) and Central Vietnam (former French Annam of French Indochina). In general, Southern Min from southern Fujian is known as Hokkien, Hokkienese, Fukien, or Fookien in Southeast Asia and is mostly mutually intelligible with Hokkien spoken elsewhere. Many Southeast Asian ethnic Chinese also originated in the Chaoshan region of Guangdong and speak Teochew language, the variant of Southern Min from that region, particularly Thailand, Cambodia, Southern Vietnam, Malaysia, Singapore, Indonesia, etc. In the Philippines, Philippine Hokkien is reportedly the native or heritage language of up to 98.7% of the Chinese Filipino community in the Philippines, among whom it is known in Hokkien Chinese: 咱人話 / 咱儂話; Pe̍h-ōe-jī: Lán-nâng-ōe / Lán-lâng-ōe / Nán-nâng-ōe; lit. 'our people's language'.

Southern Min speakers form the majority of Chinese in Singapore, with Hokkien being the largest group and the second largest being Teochew. Despite the similarities, the two groups are rarely viewed together as "Southern Min".

Classification

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The variants of Southern Min spoken in Zhejiang province are most akin to that spoken in Quanzhou. The variants spoken in Taiwan are similar to the three Fujian variants and are collectively known as Taiwanese.

Those Southern Min variants that are collectively known as "Hokkien" in Southeast Asia also originate from these variants. The variants of Southern Min in the Chaoshan region of eastern Guangdong province are collectively known as Teo-Swa or Chaoshan. Chaoshan Min is of great importance in the Southeast Asian Chinese diaspora, particularly in Malaysia, Thailand, Cambodia, Vietnam, Sumatra, and West Kalimantan. The Philippines variant is mostly from the Quanzhou area as most of their forefathers are from the aforementioned area.

The Southern Min language variant spoken around Shanwei and Haifeng differs markedly from Teochew and may represent a later migration from Zhangzhou. Linguistically, it lies between Teochew and Amoy. In southwestern Fujian, the local variants in Longyan and Zhangping form a separate division of Southern Min on their own. Among ethnic Chinese inhabitants of Penang, Malaysia and Medan, Indonesia, a distinct form based on the Zhangzhou dialect has developed. In Penang, it is called Penang Hokkien while across the Malacca Strait in Medan, an almost identical variant[citation needed] is known as Medan Hokkien.

Varieties

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There are two or three divisions of Southern Min, depending on the criteria for Leizhou and Hainanese inclusion:

More recently, Kwok (2018: 157)[10] has proposed an alternative classification, with a divergent Northern branch that includes Quanzhou dialect but not Zhangzhou dialect, as shown below:

Hokkien

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Hokkien is the most widely spoken form of Southern Min, including Amoy dialect and Taiwanese. Both of these developed as a combination of Quanzhou and Zhangzhou speech. Varieties in South-East Asia include Singaporean Hokkien, Penang Hokkien, Southern Peninsular Malaysian Hokkien, Medan Hokkien, and Philippine Hokkien.

Chaoshan (Teo-Swa)

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Teo-Swa or Chaoshan speech (潮汕片) is a closely related variant of Southern Min that includes the Kekyeo dialect, Teochew and Swatow dialects, and some consider Haklau Min to also be part of. It has limited mutual intelligibility with Hokkien, though they share some cognates with each other. Chaoshan Min is significantly different from Hokkien in both pronunciation and vocabulary, and mutual intelligibility is difficult.[11]

Phonology

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Southern Min has one of the most diverse phonologies of Chinese varieties, with more consonants than Mandarin or Cantonese. Vowels, on the other hand, are more-or-less similar to those of Mandarin. In general, Southern Min dialects have five to six tones, and tone sandhi is extensive. There are minor variations within Hokkien, and the Teochew system differs somewhat more.

Southern Min's nasal finals consist of /m/, /n/, /ŋ/, and /~/.


Sino-Xenic comparisons

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Southern Min can trace its origins through the Tang dynasty, and it also has roots from earlier periods. Hokkien people call themselves "Tang people", (Tn̂g-lâng 唐人/唐儂) which is synonymous to "Chinese people". Because of the widespread influence of the Tang culture during the Great Tang dynasty, there are today still many Southern Min pronunciations of words shared by the Sino-xenic pronunciations of Vietnamese, Korean and Japanese languages.

English Han characters Mandarin Chinese Hokkien[12] Teochew Cantonese Korean Vietnamese Japanese
book chhek/chheh cêh4 caak3 chaek () sách saku/satsu/shaku (さく/さつ/しゃく)
bridge qiáo kiâu/kiô giê5/gio5 kiu4 gyo () kiều kyō (きょう)
dangerous 危險 wēixiǎn / wéixiǎn guî-hiám guîn5/nguín5 hiem2 ngai4 him2 wiheom (위험) nguy hiểm kiken (きけん)
embassy 大使館 dàshǐguǎn tāi-sài-koán dai6 sái2 guêng2 daai6 si3 gun2 daesagwan (대사관) đại sứ quán taishikan (たいしかん)
flag kî5 kei4 gi () ki ()
insurance 保險 bǎoxiǎn pó-hiám bó2-hiém bou2 him2 boheom (보험) bảo hiểm hoken (ほけん)
news 新聞 xīnwén sin-bûn sing1 bhung6 san1 man4 shinmun (신문) tân văn shinbun (しんぶん)
student 學生 xuéshēng ha̍k-seng hak8 sêng1 hok6 saang1 haksaeng (학생) học sinh gakusei (がくせい)
university 大學 dàxué tāi-ha̍k/tōa-o̍h dai6 hag8/dua7 oh8 daai6 hok6 daehak (대학) đại học daigaku (だいがく)

Writing systems

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Both Hokkien and Chaoshan (Teochew and Shantou dialects) have romanized writing systems and also respective Chinese characters. In mainland China, it is known as 閩南文 (Bân-lâm-bûn), while in Taiwan, it is known as 台文 (Tâi-bûn). The Han Chinese characters are known in mainland China and Taiwan as 漢字 (Hàn-jī / Hàn-lī). In Malaysia and Singapore, the Chinese characters are sometimes known as 唐儂字 / 唐人字 (Tn̂g-lâng-jī / Tn̂g-lâng-lī). In the Philippines, the Chinese characters are known as 咱儂字 / 咱人字 (Lán-nâng-dī) or 漢文字 (Hàm-bûn-dī).

History

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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.[13] 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.[14] 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.[15] Linguists estimate that the oldest layers of Min dialects diverged from the rest of Chinese around the time of the Han dynasty.[16][17] However, significant waves of migration from the North China Plain occurred.[18] These include:

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

  1. A non-Chinese substratum from the original languages of Minyue, which Norman and Mei Tsu-lin believe were Austroasiatic.[19][20]
  2. The earliest Chinese layer, brought to Fujian by settlers from Zhejiang to the north during the Han dynasty.[21]
  3. A layer from the Northern and Southern Dynasties period, which is largely consistent with the phonology of the Qieyun dictionary.[22]
  4. A literary layer based on the koiné of Chang'an, the capital of the Tang dynasty.[23]

See also

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References

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  1. ^ Mei, Tsu-lin (1970), "Tones and prosody in Middle Chinese and the origin of the rising tone", Harvard Journal of Asiatic Studies, 30: 86–110, doi:10.2307/2718766, JSTOR 2718766
  2. ^ Pulleyblank, Edwin G. (1984), Middle Chinese: A study in Historical Phonology, Vancouver: University of British Columbia Press, p. 3, ISBN 978-0-7748-0192-8
  3. ^ Hammarström, Harald; Forkel, Robert; Haspelmath, Martin; Bank, Sebastian (2023-07-10). "Glottolog 4.8 - Min". Glottolog. Leipzig: Max Planck Institute for Evolutionary Anthropology. doi:10.5281/zenodo.7398962. Archived from the original on 2023-10-13. Retrieved 2023-10-13.
  4. ^ Cai Zhu, Huang Guo (1 October 2015). Chinese language. Xiamen: Fujian Education Publishing House. ISBN 978-7533469511.
  5. ^ Southern Min at Ethnologue (23rd ed., 2020) Closed access icon
  6. ^ Lee, Tong Soon (2009). Chinese Street Opera in Singapore. University of Illinois Press. ISBN 9780252032462.
  7. ^ Bodman, Nicholas C. (1985). Acson, Veneeta; Leed, Richard L. (eds.). The Reflexes of Initial Nasals in Proto-Southern Min-Hingua. Oceanic Linguistics Special Publications. Vol. 20. University of Hawaii Press. pp. 2–20. ISBN 978-0-8248-0992-8. JSTOR 20006706.
  8. ^ Lien, Chinfa (2000-09-01). "Denasalization, Vocalic Nasalization and Related Issues in Southern Min: A Dialectal and Comparative Perspective". In Ting, Pang-Hsin; Yue, Anne O. (eds.). In Memory of Professor Li Fang-Kuei: Essays of Linguistic Change and the Chinese Dialects. Taipei: Academic Sinica. ISBN 957-671-725-6. Retrieved 1 September 2024.
  9. ^ "The politics of language names in Taiwan". www.ksc.kwansei.ac.jp. Retrieved 2020-06-15.
  10. ^ Kwok, Bit-Chee (2018). Southern Min: comparative phonology and subgrouping. Routledge studies in East Asian linguistics. Vol. 2. New York: Routledge. ISBN 978-1-138-94365-0.
  11. ^ Minnan/ Southern Min at Ethnologue (18th ed., 2015) (subscription required)
  12. ^ Iûⁿ, Ún-giân. "Tâi-bûn/Hôa-bûn Sòaⁿ-téng Sû-tián" 台文/華文線頂辭典 [Taiwanese/Chinese Online Dictionary]. Archived from the original on 6 October 2014. Retrieved 1 October 2014.
  13. ^ Norman (1991), pp. 328.
  14. ^ Norman (1988), pp. 210, 228.
  15. ^ Norman (1988), pp. 228–229.
  16. ^ Ting (1983), pp. 9–10.
  17. ^ Baxter & Sagart (2014), pp. 33, 79.
  18. ^ Yan (2006), p. 120.
  19. ^ Norman & Mei (1976).
  20. ^ Norman (1991), pp. 331–332.
  21. ^ Norman (1991), pp. 334–336.
  22. ^ Norman (1991), p. 336.
  23. ^ Norman (1991), p. 337.

Sources

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Further reading

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