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| script = [[Latin characters]] (as [[Pe̍h-ōe-jī]])<br>[[Chinese characters]]
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'''Southern Min''' ({{zh|s={{linktext|闽南语}}|t={{linktext|閩南語}}|l=Southern Min language|p=Mǐnnányǔ|poj=Bân-lâm-gí/gú}}), '''Minnan''' (<small>[[Standard Chinese|Mandarin]] pronunciation:</small> {{IPAc-cmn|m|in|3|.|n|an|2}}) or '''Banlam''' ({{IPA|nan|bàn.lǎm}}), is a group of linguistically similar and historically related [[Varieties of Chinese|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),
The most widely spoken Southern Min language is [[Hokkien]], which includes [[Taiwanese Hokkien|Taiwanese]].
Other varieties of Southern Min have significant differences from Hokkien, some having limited [[mutual intelligibility]] with it, others almost none. [[Teochew dialect|Teochew]], [[Longyan Min|Longyan]], and [[Zhenan Min|Zhenan]] are said to have general mutual intelligibility with Hokkien, sharing similar phonology and vocabulary to a large extent.<ref>{{Cite book|last=Lee|first=Tong Soon|title=Chinese Street Opera in Singapore|url=https://books.google.com/books?id=Yz9CW59OsuIC&dq=chaozhou+percent+intelligible+amoy&pg=PA4|date=2009|publisher=[[University of Illinois]] Press|isbn=9780252032462}}</ref> On the other hand, variants such as [[Datian Min|Datian]], [[Zhongshan Min|Zhongshan]]
==Geographic distribution==
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==Phonology==
{{main|Hokkien#Phonology|Teochew dialect#Phonetics and phonology}}
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
Southern Min's [[Nasal consonant|nasal]] [[Final (linguistics)|finals]] consist of {{Ipa|/m/}}, {{Ipa|/n/}}, {{Ipa|/ŋ/}}, and {{Ipa|/~/}}.
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==History==
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.{{sfnp|Norman|1991|pp=328}} 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 River|Xiang]] and [[Gan River (Jiangxi)|Gan]] rivers to the west, so that Min varieties have experienced less northern influence than other southern groups.{{sfnp|Norman|1988|pp=210, 228}} As a result, whereas most [[varieties of Chinese]] can be treated as derived from [[Middle Chinese]], the language described by [[rime dictionary|rhyme dictionaries]] such as the ''[[Qieyun]]'' (601 AD), Min varieties contain traces of older distinctions.{{sfnp|Norman|1988|pp=228–229}} Linguists estimate that the oldest layers of Min dialects diverged from the rest of Chinese around the time of the [[Han dynasty]].{{sfnp|Ting|1983|pp=9–10}}{{sfnp|Baxter|Sagart|2014|pp=33, 79}} However, significant waves of migration from the [[North China Plain]] occurred.{{sfnp|Yan|2006|p=120}} These include:
* The [[Uprising of the Five Barbarians]] during the [[Jin dynasty (265–420)|Jin dynasty]], particularly the [[Disaster of Yongjia]] in 311 AD, caused a tide of immigration to the south.
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* {{citation
| contribution = The Mǐn dialects
| given = Jerry | surname = Norman
| title = Languages and Dialects of China
|