This paper outlines a theoretical approach to speech sound systems based on the notion of phonological potentials: physical ‘pressures’ or biases that give rise to discrete structure and the tendencies associated with this structure that arise from the physical nature of speech sound systems. We apply this approach to a poorly understood area of phonology – phenomena of the lower vocal tract (LVT) – through a schematic that encapsulates the complex interactions among the vocal tract structures responsible for producing LVT sounds. With the framework, we provide an account of a range of LVT phenomena from several languages, illustrating how tonal, phonatory, and vowel qualities interact. Finally, we consider how the idea of phonological potentials extends across various physical domains and might exhibit patterns of alignment across these domains, thereby serving to guide the formation of patterns found in speech sound systems.

This paper presents an acoustic study of the vowel system of Southern Ute, a Southern Numic Uto-Aztecan language spoken in southwestern Colorado. Previous auditory accounts proposed an inventory of five vowel phonemes that participate in three allophonic processes and contrast in length and stress. We investigate how the vowels are realized at the phonetic level by analyzing F1, F2, duration, spectral emphasis and f0 in over 6000 vowel tokens produced by eight fluent speakers (four female and four male). Our findings provide new phonetic detail for the earlier non-instrumental descriptions of the language, including both expected and previously unreported effects. We confirm the existence of five distinct phonemic categories but show that their prototypical phonetic realizations and positional allophones do not always match the earlier descriptions. We also describe how phonemic length and stress are marked in Southern Ute.

Upper Necaxa Totonac is a Totonacan language spoken in the Necaxa River valley in the Sierra Norte of Puebla State, Mexico. While the Totonacan languages historically have three phonemic vowel qualities, the Upper Necaxa system consists of five vowels that contrast length and laryngealization. With acoustic data from six native speakers from the Totonacan communities of Patla and Chicontla, we explore the phonetic properties of vowels with respect to the first and second formant frequencies, quantity (duration), vowel phonation (modal vs. laryngeal), and stress. The data indicate that long, short, modal and laryngeal vowels occupy a similar formant space and that duration is the primary phonetic correlate of phonemic vowel length. A shift in vowel quality and an increase in duration and pitch were shown to be the acoustic characteristics of stress. The study provides a first acoustic analysis of vowels in Upper Necaxa, and contributes to typological descriptions of the properties of vowels connected with quality, quantity, stress, and phonation.

The IPA currently does not specify how to represent prenasalization, preglottalization or preaspiration. We first review some current transcription practices, and phonetic and phonological literature bearing on the unitary status of prenasalized, preglottalized and preaspirated segments. We then propose that the IPA adopt superscript diacritics placed before a base symbol for these three phenomena. We also suggest how the current IPA Diacritics chart can be modified to allow these diacritics to be fit within the chart.

Malacca Portuguese Creole (MPC) (ISO 639-3; code: mcm), popularly known as Malacca Portuguese or locally as (Papiá) Cristang, belongs to the group of Portuguese-lexified creoles of (South)east Asia, which includes the extinct varieties of Batavia/Tugu (Maurer 2013) and Bidau, East Timor (Baxter 1990), and the moribund variety of Macau (Baxter 2009). MPC has its origins in the Portuguese presence in Malacca, and like the other creoles in this subset, it is genetically related to the Portuguese Creoles of South Asia (Holm 1988, Cardoso, Baxter & Nunes 2012).

Malagasy is the westernmost Austronesian language and belongs to the South East Barito subgroup of the Western Malayo-Polynesian subfamily (Dahl 1988, Rasoloson & Rubino 2005). Dahl (1951) presents widely-accepted evidence that Malagasy is most closely related to the Indonesian language Ma’anyan of Kalimantan (South Borneo). The term Malagasy refers to a macrolanguage (Lewis, Simons & Fennig 2014), with many regional dialects distributed throughout the island of Madagascar, which lies off the east African coast across from Mozambique (see Figure 1) and has a population of over 22 million (INSTAT 2018). The central area of the country, or the ‘Central Highlands’, is a plateau of up to 5000 feet and includes the capital city of Antananarivo, with a metropolitan population of about four million. The dialect historically spoken in and around Antananarivo is called Merina, and it served as the primary basis for development of the standardized, institutional language referred to as Malagasy Ofisialy ‘Official Malagasy’ (OM).

Urarina (ISO 639-3, code ura – Lewis, Simons & Fennig 2016) is an Amazonian language isolate spoken in the Loreto Region of Peru. Most Urarina communities are located on the banks of the rivers Corrientes, Chambira and Urituyacu, which are tributaries of the Marañon River, which in turn is the mainstem source of the Amazon River. Figure 1 shows the map of Peru and the location of the Urarina territory.