Sinitic languages in the context of "Analytic language"

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⭐ Core Definition: Sinitic languages

The Sinitic languages, also known as the Chinese languages (simplified Chinese: 汉语族; traditional Chinese: 漢語族; pinyin: Hànyǔ zú), often synonymous with the Chinese language if the whole group is considered as varieties of the same language, are a group of East Asian analytic languages that constitute a major branch of the Sino-Tibetan language family. It is frequently proposed that there is a primary split between the Sinitic languages and the rest of the family (the Tibeto-Burman languages). This view is rejected by some researchers but has found phylogenetic support among others. The Macro-Bai languages, whose classification is difficult, may be an offshoot of Old Chinese and thus Sinitic; otherwise, Sinitic is defined only by the many varieties of Chinese unified by a shared historical background, and usage of the term "Sinitic" may reflect the linguistic view that Chinese constitutes a family of distinct languages, rather than variants of a single language.

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Sinitic languages in the context of Chinese language

Chinese (spoken: simplified Chinese: 汉语; traditional Chinese: 漢語; pinyin: Hànyǔ, written: 中文; Zhōngwén) is an umbrella term for Sinitic languages in the Sino-Tibetan language family, widely recognized as a group of language varieties, spoken natively by the ethnic Han Chinese majority and many minority ethnic groups in China, as well as by various communities of the Chinese diaspora. Approximately 1.39 billion people, or 17% of the global population, speak one of the Chinese languages as their first language.

The Chinese languages form the Sinitic branch of the Sino-Tibetan language family. The Chinese government considers the spoken varieties of the Chinese languages dialects of a single language. However, their lack of mutual intelligibility means they are considered to be separate languages in a family by linguists. Investigation of the historical relationships among the varieties of Chinese is ongoing. Currently, most classifications posit 7 to 13 main regional groups based on phonetic developments from Middle Chinese, of which the most spoken by far is Mandarin with 66%, or around 800 million speakers, followed by Min (75 million, e.g., Southern Min), Wu (74 million, e.g., Shanghainese), and Yue (68 million, e.g., Cantonese). These branches are unintelligible to each other, and many of their subgroups are unintelligible with the other varieties within the same branch (e.g., Southern Min). There are, however, transitional areas where varieties from different branches share enough features for some limited intelligibility, including New Xiang with Southwestern Mandarin, Xuanzhou Wu Chinese with Lower Yangtze Mandarin, Jin with Central Plains Mandarin and certain divergent dialects of Hakka with Gan. All varieties of Chinese are tonal at least to some degree, and are largely analytic.

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Sinitic languages in the context of Mandarin Chinese

Mandarin (/ˈmændərɪn/ MAN-dər-in; simplified Chinese: 官话; traditional Chinese: 官話; pinyin: Guānhuà; lit. 'officials' speech') is the largest branch of the Sinitic languages. Mandarin varieties are spoken by 70 percent of all Chinese speakers over a large geographical area that stretches from Yunnan in the southwest to Xinjiang in the northwest and Heilongjiang in the northeast. Its spread is generally attributed to the greater ease of travel and communication in the North China Plain compared to the more mountainous south, combined with the relatively recent spread of Mandarin to frontier areas.

Many varieties of Mandarin, such as those of the Southwest (including Sichuanese) and the Lower Yangtze, are not mutually intelligible with the Beijing dialect (or are only partially intelligible). Nevertheless, Mandarin as a group is often placed first in lists of languages by number of native speakers (with nearly one billion). Because Mandarin originated in North China and most Mandarin varieties are found in the north, the group is sometimes referred to as Northern Chinese (simplified Chinese: 北方话; traditional Chinese: 北方話; pinyin: Běifānghuà; lit. 'northern speech').

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Sinitic languages in the context of Standard Chinese

Standard Chinese (simplified Chinese: 现代标准汉语; traditional Chinese: 現代標準漢語; pinyin: Xiàndài biāozhǔn hànyǔ; lit. 'modern standard Han speech') is a modern standard form of Mandarin Chinese that was first codified during the republican era (1912–1949). It is designated as the national lingua franca of China, one of the official languages of the United Nations and of Singapore, and one of the national languages of Taiwan. It is largely based on the Beijing dialect. Standard Chinese is a pluricentric language with local standards in mainland China, Taiwan and Singapore that mainly differ in their lexicon. Hong Kong written Chinese, used for formal written communication in Hong Kong and Macau, is a form of Standard Chinese that is read aloud with the Cantonese reading of characters.

Like other Sinitic languages, Standard Chinese is a tonal language with topic-prominent organization and subject–verb–object (SVO) word order. Compared with southern varieties, the language has fewer vowels, final consonants and tones, but more initial consonants. It is an analytic language, albeit with many compound words.

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Sinitic languages in the context of Sinophone

Sinophone, which means "Chinese-speaking", typically refers to an individual who speaks at least one variety of Chinese (that is, one of the Sinitic languages). Academic writers often use the term Sinophone in two definitions: either specifically "Chinese-speaking populations where it is a minority language, excluding mainland China, Hong Kong, Macau, and Taiwan" or generally "Chinese-speaking areas, including where it is an official language". Many authors use the collocation Sinophone world or Chinese-speaking world to mean the Chinese-speaking world itself (consisting of Greater China and Singapore) or the distribution of the Chinese diaspora outside of Greater China.

Mandarin Chinese is the most commonly spoken variety of the Chinese languages today, with over 1 billion total speakers (approximately 12% of the world population), of which about 900 million are native speakers, making it the most spoken first language in the world and second most spoken overall. It is the official variety of Chinese in mainland China, Taiwan, and Singapore. Meanwhile, Cantonese is the official variety of Chinese in Hong Kong and Macau and is also widely spoken among significant overseas Chinese communities in Southeast Asia as well as the rest of the world.

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Sinitic languages in the context of Sino-Vietnamese vocabulary

Sino-Vietnamese vocabulary (Vietnamese: từ Hán Việt (IPA: [tɯ̀ hǎn viə̂ˀt]), Chữ Hán: 詞漢越, 'Chinese-Vietnamese words') is a layer of about 3,000 monosyllabic morphemes of the Vietnamese language borrowed from Literary Chinese with consistent pronunciations based on Middle Chinese. Compounds using these morphemes are used extensively in cultural and technical vocabulary. Together with Sino-Korean and Sino-Japanese vocabularies, Sino-Vietnamese has been used in the reconstruction of the sound categories of Middle Chinese. Samuel Martin grouped the three together as "Sino-Xenic". There is also an Old Sino-Vietnamese layer consisting of a few hundred words borrowed individually from Chinese in earlier periods, which are treated by speakers as native words. More recent loans from southern Chinese languages, usually names of foodstuffs such as lạp xưởng 'Chinese sausage' (from Cantonese 臘腸; 腊肠; laahpchéung), are not treated as Sino-Vietnamese but more direct borrowings.

Estimates of the proportion of words of Sinitic origin in the Vietnamese lexicon vary from one third to half and even to 70%. The proportion tends towards the lower end in speech and towards the higher end in technical writing. In the famous Từ điển tiếng Việt [vi] dictionary by Vietnamese linguist Hoàng Phê [vi], about 40% of the vocabulary is of Sinitic origin.

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Sinitic languages in the context of Sino-Tibetan languages

Sino-Tibetan (also referred to as Trans-Himalayan) is a family of more than 400 languages, second only to Indo-European in number of native speakers. Around 1.4 billion people speak a Sino-Tibetan language. The vast majority of these are the 1.3 billion native speakers of Sinitic languages. Other Sino-Tibetan languages with large numbers of speakers include Burmese (33 million) and the Tibetic languages (6 million). Other languages of the family are spoken in the Himalayas, the Southeast Asian Massif, and the eastern edge of the Tibetan Plateau. Most of these have small speech communities in remote mountain areas, and as such are poorly documented.

Several low-level subgroups have been securely reconstructed, but reconstruction of a proto-language for the family as a whole is still at an early stage, so the higher-level structure of Sino-Tibetan remains unclear. Although the family is traditionally presented as divided into Sinitic (i.e. Chinese languages) and Tibeto-Burman branches, a common origin of the non-Sinitic languages has never been demonstrated.

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Sinitic languages in the context of 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.

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Sinitic languages in the context of Wu Chinese

Wu (simplified Chinese: 吴语; traditional Chinese: 吳語; pinyin: Wúyǔ; Wugniu and IPA:wu-gniu6 [ɦu˩.nʲy˦] (Shanghainese), ghou-gniu6 [ɦou˨.nʲy˧] (Suzhounese)) is a major group of Sinitic languages spoken primarily in Shanghai, Zhejiang province, and parts of Jiangsu province, especially south of the Yangtze River, which makes up the cultural region of Wu. The Wu languages are at times simply called Shanghainese, especially when introduced to foreigners. The Suzhounese variety was the prestige dialect of Wu as of the 19th century, but had been replaced in status by Shanghainese by the turn of the 20th century, coinciding with a period of rapid language change in the city. The languages of Northern Wu constitute a language family and are mutually intelligible, while those of Southern Wu do not form a phylogenetic language family and are not mutually intelligible.

Historical linguists view Wu of great significance because of its obviously distinct nature. The Wu languages typically preserve all voiced initials of medieval Chinese, as well as the checked tone in the form of a glottal stop. Wu varieties also have noticeably unique morphological and syntactic innovations, as well as lexicon exclusively found in the Wu grouping. It is also of note that the influential linguist Chao Yuen Ren was a native speaker of Changzhounese, a variety of Northern Wu. The Wu varieties, especially that of Suzhou, are traditionally perceived as soft in the ears of speakers of both Wu and non-Wu languages, leading to the idiom "the tender speech of Wu" (吴侬软语; 吳儂軟語).

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