2.1. Lateral Obstruents Cross-Linguistically
The term “lateral obstruents” refers to the combined class of lateral fricatives and lateral affricates (
Maddieson, 2013). For fricatives, the channel through which the air flows is narrowed so that the flow of air is turbulent (
Ladefoged & Maddieson, 1996, p. 137). In the case of lateral fricatives, i.e., voiceless /ɬ/ and voiced /ɮ/, the airstream flows over one or both sides of the tongue (
Ladefoged & Maddieson, 1996, p. 182). Lateral affricates are stops such as /t/, /d/, or /k/ released into a lateral fricative via the lowering of the tongue. Examples include /t͡ɬ/, /d͡ɮ/ or prenasalized /ⁿt͡ɬ/ or /ⁿd͡ɮ/. As lateral is a manner of articulation, lateral obstruents can be articulated at varying places. The alveolar place of articulation is the most common, but some Southern Bantu languages also use a velar lateral affricate (/k͡ʟ̝̊/), while certain East African language, such as Hadza (
Sands, 2013) and Dahalo (
Sands, 2007), have palatal lateral obstruents.
Lateral obstruents are relatively rare in the world’s languages. Databases such as the World Atlas of Language Structures (WALS) (
Dryer & Haspelmath, 2022), and the Phonetics Information Base and Lexicon (PHOIBLE) (
Moran & McCloy, 2019) give us several useful insights into the phonological trends. WALS (
Maddieson, 2013) surveys the occurrence of lateral obstruents in 567 languages, which includes a single Southern Bantu language, Zulu (S42). Moreover, 54 (9.5%) of the languages in their sample have lateral obstruents, 51 of which have lateral fricatives and 25 of which have lateral affricates, more frequently voiceless than voiced. Lateral affricates, on the contrary, are less common, only occurring in 25 languages of the sample (4.4%). 22 of these 25 languages also have a lateral fricative in their consonant inventory. The map in
Figure 2 visualizes all languages included in the sample of WALS recognized as having lateral obstruents in their phoneme inventory.
The PHOIBLE database has cross-linguistic phonological data from 2186 languages, which includes five Southern Bantu languages, Shona (S10), Zimbabwean Ndebele (S44), Xhosa (S41), Zulu (S42), and Ronga (S54). They report the following frequency of occurrence of lateral obstruents. We have selected lateral obstruents from this database based on whether they also occur as phonemes in Nguni languages, as presented in
Table 1.
This database shows a similar picture to WALS: /ɬ/ is the most common lateral obstruent, followed by its voiced counterpart /ɮ/. This is in line with recent work by
Shinagawa and Lee (
2024), who propose an implicational relation between voiceless and voiced lateral fricatives based on phonetic observations in selected Southern Bantu languages. Lateral affricates are far more uncommon, and the velar lateral affricate /k͡ʟ̝̊’/ is especially unique.
Ladefoged and Maddieson (
1996, p. 206) state that the velar lateral ejective affricate is ‘an unusual sound’ and that it had been described as a palatal lateral ejective because velar laterals were thought not to be possible as speech sounds. However, they explain there is no reason to doubt that these two components of the affricate are velar in articulation and its fricative component is auditorily similar to the velar fricative /x/ but lateral. Within Africa, apart from Southern Africa, lateral obstruents are concentrated around Lake Chad, where they are a feature of Chadic languages (
Newman, 1977), and in East Africa, where they are a feature of the Tanzanian Rift Valley linguistic area (
Kießling et al., 2008) and their occurrence across language families may be a case of contact-induced retention (
Beer et al., forthcoming). In Southern Africa, lateral obstruents occur in Southern Bantu and in languages of the Kx’a, Tuu, and Khoe-Kwadi families, three separate families subsumed under the areal umbrella term “Khoisan” (
Güldemann, 2014). Khoisan languages with lateral obstruents are listed in
Table 2.
In Khoisan, lateral obstruents often result from click loss, a sound change changing clicks into non-clicks, for instance in certain varieties of Angolan !Xung (
Traill & Vossen, 1997), in Kwadi (
Fehn, 2020a;
Fehn & Rocha, 2023), and Ju (
Fehn, 2020b), and in ǁXegwi, where lateral obstruents correspond to clicks in closely related Nǀuu (
Sands, 2007).
In Southern Bantu, lateral obstruents are attested in some Shona (S10) languages (
Mkanganwi, 1972, p. 117;
Doke, 1931, pp. 75–79), in some Sotho-Tswana (S30) languages, and in all languages of the Nguni (S40) and Tsonga (S50) subgroups (for a summary, see
Doke, 1954, p. 42;
Gunnink et al., 2022;
Van der Vlugt, 2023). Little is known about the lateral obstruents in Southern Bantu. On the acoustic side,
Ladefoged and Maddieson (
1996, p. 204–206) present data on Zulu lateral obstruents, including the rare velar lateral affricate, which is only sparsely attested in the world’s languages. Based on spectrogram data from a Zulu speaker, they conclude that the alveolar lateral affricate only occurs as an allophone of /ɬ/ after a nasal. Postnasal affrication of fricatives is common in Bantu, attested, for example, in Kongo, Yaka, Tuki, and Venda (
Hyman, 2001, pp. 169–170). As discussed in
Section 2.2 and
Section 3.2, this process also seems to apply to at least some Nguni languages.
Shinagawa and Lee (
2024) provide a typological overview of the variation of lateral fricatives in the Southern Bantu languages Northern Sotho (S32), Southern Ndebele (S407), Xhosa (S41), Zulu (S42), Swati (S43) and Tsonga (S53), looking into word position and interaction with prenasalization. In contrast to
Ladefoged and Maddieson (
1996, pp. 204–206), their acoustic data do not show that the prenasalized lateral fricative in Zulu (or any other language in their sample) turns into an affricate. We will elaborate in more detail on Nguni lateral obstruents in the following section.
2.2. Lateral Obstruents in Nguni
Lateral obstruents are known to occur in all Nguni languages on which sufficient documentation is available.
Table 3 lists the lateral obstruents described for each Nguni language in the available sources.
All Nguni languages make use of lateral obstruents. Voiced and voiceless alveolar lateral obstruents /ɬ, t͡ɬ/, and /ɮ, d͡ɮ/ occur in all languages, but the voiceless velar lateral affricate /k͡ʟ̝̊/ is restricted to Nhlangwini (S405), Zulu (S42), Swati (S43), and Zimbabwean Ndebele (S44). This velar lateral affricate is often noted to have an allophone /k͡x/, e.g., a central velar affricate, as shown in more detail in
Section 3.3.2.
Most lateral obstruents can be prenasalized, except in Phuthi (S404), due to a loss of prenasalization everywhere in the language (
Msimang, 1989, pp. 198–199;
Donnelly, 2007, pp. 43–45). Prenasalized lateral obstruents are variably described as fricatives (
Ziervogel, 1952, p. 9, on Swati) or affricates (
Finlayson et al., 1990, p. 60, on Xhosa;
Doke, 1947, p. 17, on Zulu). In the case of Nguni, it might represent a difference in analysis rather than a difference in the phonetic realization of this phoneme between different language varieties because prenasalization tends to change continuants like fricatives into stops or affricates through assimilation to the complete closure of the preceding nasal. This process is described for certain Nguni languages, e.g., Zulu (
Poulos & Msimang, 1998, pp. 516–517), but for many other Nguni languages, which are less thoroughly described and analyzed, the effect of prenasalization on continuants and the phonetic and phonological status of prenasalized lateral fricatives or affricates is not discussed. However, there are no Nguni languages for which a phonemic contrast between prenasalized lateral fricatives and obstruents is described, and as seen in
Section 3.2, phonemes described as prenasalized lateral affricates in one language typically correspond to phonemes described as prenasalized lateral fricatives in others.
In many nouns, the initial nasal is not part of the lexical root but functions as the noun class prefix of class 9 and 10. This is illustrated for Zulu in (1)–(2), which show a verb being derived into a noun of class 9. This includes the addition of the nasal as the noun class prefix.
- (1)
i-n-ɬambi
AUG-NP9-swimmer
from -ɬamba ‘swim’
- (2)
i-n-ɬeɓi
AUG-NP9-slanderer
from -ɬeɓa ‘slander’
The status of lateral obstruents in Lala (S406) is particularly obscure but of great interest. According to
Van Dyk (
1960), Lala only has velar lateral affricates.
Zungu (
1999) does identify alveolar and velar lateral obstruents in Lala, whereas
Msimang (
1989) attributes alveolar lateral obstruents only to Southern Lala, and notes that they are absent in Northern Lala. Lala varieties or doculects that lack alveolar lateral obstruents make use of velar fricatives instead (cf.
Msimang, 1989, p. 109), as shown in (3)–(5), with the original Afrikaans and English translation.
This highly variable situation is very relevant for the historic interpretation of lateral obstruents in Nguni. The striking differences between different sources on what is referred to as the same language is likely due to regional variation and possibly changes over time, but also due to the definition of the term “Lala” itself. Rather than describing a speech community using a distinct language variety, the term
ama-lala may have been used to describe a socially defined class of people (
J. Wright, 2012). The language varieties spoken by people identifying as Lala do therefore not necessarily constitute a linguistically coherent class. Given these difficulties, combined with the relatively small amount of data in the available sources on Nguni varieties named Lala, we have decided to exclude Lala data from the present study. However, when available, the linguistic data on Lala is included in the
Supplementary Materials.
2.3. Proposed Origins of Lateral Obstruents in Nguni and Southern Bantu
While systematic and comprehensive approaches on the historical phonological development of Nguni languages are rare, previous work has looked at both regular sound change and contact to explain the presence of lateral obstruents in Nguni. On the one hand, some analyses suggest that certain Nguni lateral obstruents have a Bantu-internal origin.
Janson (
1991) discusses the phonological development of Southern Bantu languages in comparison with the Makua (P30) cluster of northern Mozambique that shares a number of remarkable developments with certain Southern Bantu languages.
Janson (
1991, pp. 84–88) shows some evidence for lateral obstruent reflexes of Proto-Bantu palatals in Nguni, but only considers three Nguni languages, i.e., Zulu (S42), Xhosa (S41), and Swati (S43), and does not analyze lateral obstruents that are not the result of regular sound change.
Msimang (
1989), who studies the reflexes of Proto-Bantu consonants in Nguni languages of the Tekela group
1, identifies /ɬ/ as a reflex of reconstructed *c (
Msimang, 1989, pp. 167–168), but with little to no detail on the development of other lateral obstruents.
Jimenez (
2017,
2022) are mostly concerned with Nguni subclassification, but identifies few sound changes. Her reconstructions are not based on the identification of regular sound correspondences, and therefore shed little light on the diachronic phonology of Nguni.
On the other hand, contact has also been suggested as the possible driving force behind the development of lateral obstruents in Nguni.
Louw and Finlayson (
1990) consider lateral obstruents in Southern Bantu to be mostly restricted to roots that do not occur in Bantu languages outside zone S, but are rather Southern Bantu innovations. They suggest a Southern Cushitic origin for Southern Bantu lateral obstruents, in which case contact would have taken place in East Africa, where Cushitic languages are spoken. However, as noted by
Gunnink et al. (
2022, p. 99), no other Southern Cushitic influence is established in Southern Bantu as of yet. Furthermore, as described in
Section 3.2, lateral obstruents in Nguni languages are very common in roots of Proto-Bantu origin, which are unlikely to be lexical loans. Thus, Southern Cushitic languages do not seem the most likely donor for lateral obstruents in Southern Bantu.
Instead,
Gunnink et al. (
2022) propose contact with Khoisan languages as a source for lateral obstruents. Southern Bantu languages have clearly undergone contact-induced changes from Khoisan languages, especially in their phonologies. Clicks occur as loan phonemes in the Sotho-Tswana language Southern Sotho (S33) and almost all Nguni languages (
Pakendorf et al., 2017). These contact-induced structural changes likely involved language shift from Khoisan to Bantu, which ties in with genetic evidence for Khoisan admixture in Southern Bantu-speaking groups (
Pakendorf et al., 2017;
Sengupta et al., 2021). Clicks are the most clear-cut cases of Khoisan phonological influence, but not the only ones, given the much larger phoneme inventories of certain Southern Bantu languages compared to other modern Bantu languages and Proto-Bantu, including many phonemes for which no Bantu origin can be found (
Lanham, 1964;
Schadeberg, 2009). Furthermore, since lateral obstruents occur in certain Khoisan languages (see
Table 2), Khoisan influence may have played a role in their development in Southern Bantu.
Gunnink et al. (
2022) offer two possible contact scenarios that could account for the development of lateral obstruents in Southern Bantu. Firstly, language contact with Khoisan could have influenced a sound change resulting in lateral obstruents. Secondly, Southern Bantu lateral obstruents may be reflexes of earlier click phonemes, given the frequently found pattern of lateral obstruents resulting from click loss. These possible contact scenarios have not yet been investigated more closely. The possible role of Khoisan contact in the development of lateral obstruents in Southern Bantu therefore remains unknown.
Finally, contact is prominent in the linguistic macro-area theory of
Güldemann (
2011,
2019) arguing for a pre-Bantu linguistic area uniting Eastern and Southern Africa with lateral obstruents as one of its defining phonological features. Although these features now only occur in some Eastern and Southern African languages, they may once have been more prevalent. Intermediate languages with lateral obstruents may have disappeared following the arrival of Bantu languages, which have a very different typological profile. This theory is relatively similar to proposals of both Cushitic and Khoisan contact. However, as it does not identify specific contact situations or donor languages, it is hard to test.
In conclusion, previous work has proposed that at least some lateral obstruents arose as the result of language-internal, diachronic phonological processes. Alternatively, contact may have played a role in the development of lateral obstruents in Southern Bantu. It is not clear yet what concrete contact situations, donor languages, and linguistic changes could explain the current distribution and use of lateral obstruents.