where malay come from

8/2/2019 Where Malay Come From

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K. ALEXANDER ADELAAR

Where does Malay come from?Twenty years of discussions about homeland,migrations and classifications

Introduction

The Malay language consists of many dialects. Furthermore, various otherlanguages are closely related to Malay, including M inangka bau, Kerinci, Ibanand Kendayan. Together, these dialects and languages form the 'Malayic'linguistic subgroup within the (West) Malayo-Polynesian branch of theAustronesian language family (Adelaar 1992:1).This article* discusses several issues involving the homeland 1 and clas-sifications of the Malayic language subgroup and of Malay in particular.Following an overview of proposed theories about the Malay(ic) homeland(section 1), I discuss the Borneo hypothesis and the applicability of Sapir's(1968) model for the location of linguistic homelands (section 2). I treat thedifficulties in assessing language divergence and genetic depth in the Malayicsubgroup (section 3), and evaluate the claim of a Malay back-migration fromSumatra to Borneo (section 4). I also compare the locations that have beenproposed for a Malayic homeland within Borneo (section 5) and give anoverview of classifications of Malayic languages with other Austronesian

I am grateful to Adrian Clynes (Universiti Brunei Darussalam), Antho ny Jukes (Universityof Melbourne), and two anonym ous readers for their careful reading and comm ents on an earlierdraft of this article. They are in no w ay responsible for any errors in this version.1 That is the region where speakers of the hypothetical proto-language ancestral to a linguis-tic subgrou p must have lived before they dispersed to other regions. In the case of speakers ofMalayic isolects, this is the region where speakers of Proto Malayic originally lived.K. Alexander Adelaar is Associate Professor and Reader at the Melbourne Insitute of AsianLanguages and Societies (MIALS) and holds a PhD from Leiden University. His main field ofacademic interest is Austronesian historical and descriptive linguistics, especially regarding thelanguages of Madagascar, Taiwan and Borneo. He is the author of Proto-Malayic, Canberra:Pacific Linguistics, 1992, and 'Retrieving Siraya phonology: a new spelling for a dead language',in: E. Ze ito un a nd P. Jen-ku ei Li (eds), Selected papers from the Eighth International Conferenceon Austronesian Linguistics, pp . 313-54, Taipei: Institute of Linguistics, Academia Sinica, 1999.Professor Adelaar may be reached at MIALS, University of Melbourne, VIC 3010, Australia.

Bijdragen tot de Taal-, Land- en Volkenkunde (BKI) 160-1 (2004):l-30 2004 Koninklijk In stituut voor Taal-, Land- en Volkenkunde


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Palembani(Srivijaya)

Indian O cean L O M B O KS U M B AW A ~ V

Map of the most important toponyms and languages referred to in this articleNote: Numbers following language names correspond to numbers on the map indicating the approximatelocation of the languages in question. Num bers on the map run m ore or less from west to east but are groupedby area.AcehneseBacan Malay (eastern Indonesia)BalineseBangka MalayBanjarese MalayBelitung MalayBengkulu MalayBerau MalayBrunei MalayCham(ic) (Indo-China)DuanoDusun DeyahEast BaritoEmbaloh

13835132914

53426191132312 8 .

IbanJakarta Malay/JakartaneseJavaneseKelantan MalayKendayanKerinciKutai MalayLampungLand DayakMaanyan (> East Barito)MadureseMinangkabauMualangNgaju (> West Barito)

2415171023

333

8223118

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Palembang M alayRejangSalakoSambas MalaySarawak MalaySasakSeraway MalaySumbawaSundaneseTioman MalayUrak Lawoi'(South-West T hailand)West Barito

6420212536

7371612

930


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Where does Malay come from? 3languages (section 6). A large section assesses attempts at internal classifica-tions of the M alayic su bgro up m ad e in the last twe nty years (section 7), fol-lowed by some concluding remarks (section 8).

1. Overview of theories about the homeland of Malay and of the Malayic subgroupTheories about the hom elan d of the Malay langua ge are not new. In the late nine-teenth cen tury the philologist and linguist H . Kern wro te an im portan t article inwhich he used the W orter undSachen'2 m ethod to reconstruct the Austronesiannatural environm ent (on the basis of predom inantly animal an d p lant names)and to determine where they came from. In his view, the early Austronesiansoriginally lived in coastal Indo-China and from there moved south overlandprior to sailing into the areas where they presently live. Operating on thisassump tion, he believed that the Ch am s and peninsular M alays were the stay-beh inds in a migration process tow ards the east, rather tha n recent arrivals of awe stward migration, as is generally believed n ow aday s.

Kern, who did not distinguish between Malay and Malayic, argued thatthe Malay hom eland wa s in the Malay peninsula. M alay has a term for 'sou th'which basically means 'strait ' {salat/an). Kern took this as an indication thatthe earliest Malays had a sea strait to their south, which m akes sense from thegeographical perspective of the Malay peninsula. H e did not believe that thehom eland w as in Borneo because that w ould leave unexplained w hy the earlyMalays had left this fertile3 and sparsely populated island to establish them-selves on the coasts of more p opu lated lands elsewhere. Their migrations m usthave been triggered by external pressure. Kern believed that such pressure wa spresent in m ainland Southeast Asia, where Vietnamese and Khm ers are kno wnto have gained large territories at the expense of the Austronesian-speakingChams. Although it is sometimes unclear whether Kern is referring to theAustronesian or the Malay homeland, it is implicit in his argument that theM alays and C ham s are the last vestiges of an earlier Austronesian h om eland.

Kern's hypothesis of a homeland in the Malay peninsula was met withsome scepticism by historians and philologists wh o realized th at the establish-ment of Malay communities in the Malay peninsula was generally of a morerecent date than that of Malay communities in Sumatra. These scholars alsocame to appre ciate the authe nticity of the ancient em pire of Srivijaya in south -ern Sum atra (Coedes 1948). Althou gh this empire w as m entioned in Malay2 A method combining the comparison of tangible objects an d their various labels for prehis-torical reconstruction (Malkiel 1993:x).3 According to Kern (1889:287). Kern's description of Borneo as 'geenszins onvruchtbaar'('not at all infertile') does not appear to reflect reality.


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4 K. Alexander Adelaar

folklore and literature (for example in the Sejarah Melayu or 'Malay A nnals'), itwas not until the discovery of seventh-century inscriptions in an archaic formof Malay4 that scholars began to consider it to rest on historical fact.Archaeological and linguistic research on Formosan languages (theAustronesian languages of Taiwan) in the last three decades has made itincreasingly clear that the Au stronesian ho meland wa s either in Taiwan or inneighbouring coastal southern China (Bellwood 1997:106). The Austronesianmigrations into western Indonesia must therefore have been from Taiwansouth into the Philippines and then westwards, and the Southeast Asianmainland has come to be viewed as a rather late Austronesian settlementfar to the west.Blust (1984-85) was the first to propose Borneo5 as the Malay(ic) home-land. Inspired by his hypo thesis, Adelaar (1985) argued that the M alays weremore likely to have travelled by sea than by land (as believed by Kern):the demographic pattern of the Malay peninsula is a clear indication thatthis area had been populated by Malays more recently than had Borneo,where speakers of many Malayic isolects6 live rather far inland. Adelaar(1988) challenges Kern's rather weak evidence based on the term sdlat/an'south', showing that sdlat/an and utara 'north' were at odds with the inter-

nal terminological consistency of the Malay cardinal direction system andmust have supplanted earlier terms *daya? ' towards the inland; south' and*laut 'towards the sea; north'. Some other terms in this system still testify totheir former presence, namely barat-daya 'southwest ' ; barat-laut 'northwest';timur-laut 'northeast'). This state of affairs would fit with a position of theancient Malay kingdo m Srivijaya at the mo uth of the Musi River in southeastSumatra (due to siltation the ancient site is now ada ys further inland).Adelaar (1985) and Blust (1988) also believe that the presence of Malaysalong the Borneo coasts was the result of back-migrations. The Bornean

homeland hypothesis combined with back-migrations is compatible withboth linguistic and extra-linguistic findings including the traditionally heldbelief among M alays that the cradle of the Malay na tion w as in the region ofPalembang in southern Sumatra (Andaya and Andaya 1994:31-4). At some4 Teeuw (1959) remains cautious about qualifying Old Malay as a form of Malayic butAdelaar (forthcoming b) gives phonological an d m orphosy ntactic evidence for it. Compare alsoMahdi (forthcoming) who considers it a form of Malay.5 More particularly, so uthw est Borneo; see section 6.6 Our present state of knowledge about Malayic dialects and languages often makes itimpossible to determine whether the speech of a certain community represents a language inits own right or a dialect vis-a-vis other varieties of Malayic that are identified as separate lan-guages. In these cases, the cover term 'isolect' is often used, which is 'connotationally neutral inregard to language-dialect identification' (Hudson 1967:12). The term is also used when referringsimultaneously to dialects as well as to languages, hence 'Malayic isolects' instead of the m orecumbersome 'Malayic dialects and languages'.


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W here does Ma lay come from? 5prehistorical stage, Malayic speakers must have left Borneo and settled insouthern Sum atra, where they founded a maritime em pire and developed aseparate M alay identity (probably und er Ind ian influence, which also bro ugh tthe idea of statehood to Southeast Asia). Blust (1988,1994) places the M alayichom eland in southw est Borneo. H e believes that Borneo is also the hom elandof the Chamic languages of Vietnam and Kampuchea (see section 6).

Various other linguists have since adopted the Bornean homelandhypothesis. Collins and Nothofer have taken the hypothesis as a startingpoint for more far-reaching internal classifications of the Malayic languagegroup. They place the hom eland in western B orneo or northw est Borneo (seesection 5). The archaeologist and prehisto rian P eter Bellwood also seems toaccept Borneo as a homeland in some of his earlier publications, but in arecent revision of hi s book Prehistory of the Indo-Malaysian archipelago h e takesa more cautious position (Bellwood 1997:287).

Other linguists, however, do not consider the Bornean hom eland hypo th-esis in their historical linguistic studies of Malay, for instance Asmah HajiOmar (1985) and Ismail Hussein (1992:2-5). The latter believes that theM alayo-Polynesian hom eland was in Yunnan (southern China). He does notspecifically add ress the question of the M alay(ic) h om eland .

2. Borneo as the Malay homeland: theoretical justificationO ne of the assu m ptions beh ind the Borneo hypo thesis is Sap ir's mod el (1968)claiming that in the quest for a linguistic homeland, the area with the larg-est genetic diversity in relation to its size is most likely to be the homeland.This mo del is useful, all thing s being equ al; bu t in practice other factors ofteninterfere with it. If one compares Europe to the situation in the Americas,where the spread of Spanish, English, Portuguese and French is relativelyrecent, the model seems to make sense: the dialect diversity within each ofthese four languages is as a rule much less (and of less genetic depth) thanit is in Europe. In Europe itself, however, it is doubtful whether the modelwould be helpful for tracing the homeland of, say, French. It would probablysingle out southern Belgium, an area with a relatively great dialect diversitycompared to France itself. Nevertheless, the southern Belgian diversity doesnot necessarily reflect a greater time d ep th for the settleme nt of French speak-ers in this area. Rather, it is largely a co nsequ ence of the fact that this area h asnever been subjected to the same intensive political centralization and con-comitant dialect levelling as have French-speaking areas within the bordersof France. Neither is Sap ir's m ode l likely to be very helpful in areas affectedby extensive incoming migrations, lasting foreign occupations, and epidem-ics, to nam e only a few factors that bring about language-ind uced change and


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langu age shift. Finally, the reliability of the outcom es of the mod el should alsobe tested against indep enden tly acquired extra-linguistic evidence.

3 . Borneo as the Malay homeland: practical considerationsIf we adopt Borneo as the Malayic homeland on the basis of Sapir's model,it need s to be dem ons trated that the diversity of Malayic isolects in westernBorneo is in fact significantly greater than it is elsewhere. There is indeedconsiderable linguistic diversity in Borneo, particularly the w estern p art, bu tto what extent is it genetically relevant? And how should we measure thisdiversity? There are at least three configurations distinct en oug h to represen tseparate languages: Iban-like or 'Ibanic' isolects, Kendayan7 isolects, andother isolects (including various local Malay dialects but possibly also otherdistinct languages). A separate language status for Ibanic and Kendayan iswarran ted on the basis of the differences they sho w at several linguistic lev-els between each other and with Malay: the evidence consists of phonologi-cal, morphosyntactic and lexical data. Considering our limited knowledgeof the linguistic diversity of western Borneo, it would be speculative at thisstage to distinguish other separate Malayic languages.Much of the evidence for Malayic subgroups in western Borneo adducedby Collins and Nothofer is based on very limited phonological and lexicaldata and does not make use of morphosyntactic features. Moreover, someof the phonological changes and lexical replacements proposed by Collinsand Nothofer may seem critical for a proposed subgroup of languages in aparticular area but turn out not to be critical when other (not directly relat-ed) languages from outside that area are brought into the comparison. TheMalayic isolects of western Borneo have apparently influenced each otherconsiderably, and variou s phono logical and lexical innov ations are recu rrentthroughout the area. If one's research is limited to a small part of that area,it is easy to lose perspective and to develop tunnel vision, obtaining conflict-ing results for subgroup s dep ending on where fieldwork was conducted andhow the territory was divided up. Some other phonological changes consid-ered critical by Collins and Nothofer are too general to be considered diag-nostic for a classification (for example, raising or rounding of schwa, changeof *s to h, loss of *h, loss of *-? (final glottal stop), monophthongization of7 The term 'Kendayan' is in itself a cover term for several mutually understandable dialectsincluding Ahe, Banana' (Pontianak Bengkayang, and Landak Regencies, West KalimantanProvince), and Salako (Sambas Regency and Bengkayang Regencies West Kalimantan Provinceand Lundu District, Sarawak; Collins 1997). However, as a linguistic term 'Kendayan' is awk-ward in that it does not always match 'Ke nday an' as an ethnic label. Thel latter is often mea nt toinclude speakers of some of the neighbouring Land Dayak languages.


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Where does Malay come from? 7

final vowel-glide sequences). This also applies to preploded final nasals (-pm,-tn, -krj). Although they constitute a phonetically salient development, theyare a relatively recent phenomenon attested right through several linguisticsubgroups (including Malayic, Land Dayak/Ulu, and even West Barito andEast Barito, compare Dusun Deyah in southern Kalimantan, Djantera Kawiet al. 1983), dividing their respective member languages into those that havepreplosive nasals and those that do not. They seem to be the result of an arealfeature that has also spread to the western shores of the South China Seaand beyond.8 The phenomenon has also been observed among many non-Austronesian languages on the Southeast Asian mainland (Blust 1997).

Malayic diversity in other parts of Borneo is also considerable, withBanjarese Malay, Kutai Malay and Brunei Malay in southern, eastern andnorthern Borneo, respectively, to list only the more prominent ones. In princi-ple, the case for a Malay homeland in the genetically most diverse area wouldbe stronger if the entire island were considered as a homeland, because itwould represent an even greater Malayic speech diversity with the inclusionof the habitat of Banjarese Malay, Kutai Malay and Brunei Malay. However,a greater diversity of Malayic speech forms does not necessarily represent agreater genetic diversity, and the genetic diversity in northern, eastern andsouthern Borneo does seem to be less than in western Borneo (see section 7.1).What about Malayic diversity in areas to the west of Borneo? We havecome to assume that this diversity is less than in western Borneo, or atleast that the diversity is of a more recent nature and therefore geneticallyless relevant. Kelantan Malay, Urak Lawoi' Malay, Minangkabau, Kerinci,Jakartanese and Duano represent a bewildering diversity and can be consid-ered languages in their own right, but their linguistic diversity does not nec-essarily represent a commensurate genetic depth. The phonological changesthat make Minangkabau and Kerinci so different from Standard Malay arerather superficial: if traced back, they lead to an earlier phonology that isalmost identical to that of Standard Malay. The complex morphosyntacticchanges of Kerinci can also be explained as a function of these phonologicalchanges (Prentice and Usman 1978; Steinhauer and Usman 1978; Adelaar1992a; Steinhauer 2002). Similar explanations can be argued for KelantanMalay, Urak Lawoi' Malay, Duano and other Malayic isolects to the west andsouth of the South China Sea. Nevertheless, that the phonological changesin these languages are relatively recent and superficial is something whichremains to be demonstrated (as it remains to be demonstrated that the chang-es in some recently identified West Bornean Malayic isolects in fact reflect agreater historical depth, see section 7.2 and section 7.4).

8 One example is Urak Lawoi', a Malayic isolect in southwest Thailand (Hogan andPattemore 1988).


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8 K . A le x a n d e r A d e la a rMinangkabau, Kerinci, Bengkulu and other Malayic areas in westernSumatra also present a demographic complication. If speakers of Malayicmigrated from Borneo and are relatively new to Sumatra, how did it happenthat they penetrated the island from east to west and came to occupy almosttwo thirds of it instead of remaining in coastal areas? What ethnic accul-turation processes took place here, and can they account for the present-dayspread of Malayic speakers in Sumatra? This also needs to be addressed inthe discussion about a ho m eland.

4. A back-migration from Sumatra?Adelaar (1985, 1992a, 1995) and Blust (1988, 1994) believe that the presenceof M alays in (predom inantly coastal) Borneo is the result of b ack-m igrationsof Sum atran (and later, pen insular) M alays. This hyp othesis bring s the occur-rence of Malay communities in coastal Borneo in line with the existence ofMalay-speaking communities elsewhere in Southeast Asia (Moluccas, north-ern Java, the coasts of Sum atra and the M alay peninsu la). It also brings it inline with the trad ing and seafaring trad itions of the Malays, w ho often estab -lished trading posts in the places they visited. The hypothesis is supportedby the fact that the oldest unequivocal manifestations of Malay civilizationare found in southern Sumatra (stone inscriptions in Old Malay, archaeo-logical sites). The existence of an early Malay empire in southern Sumatra(Srivijaya, M alayu) is corroborated by M alay historiography and by evidencefrom Chinese historical records (Andaya and Andaya 1994 Chapter 1). Oneof the nam es for this empire, 'Ma layu', is conceivably the origin of the ethno -nym 'Melayu', w hich is also used in Borneo.

The hypothesis does not exclude the notion of a huge acculturation andassimilation process that must have taken place in the last two millennia.It does not mean that the speakers of Malay dialects that resulted from thisback-migration can trace all their ancestors to Sumatra or the Malay penin-sula. Banjarese Malays primarily descend from Ngajus, Maanyans or othernon-Malay ethnic groups living inland from Banjarmasin. Likewise, mostBrunei Malays probably descend from members of local non-Malay commu-nities who were assimilated into Brunei Malay society.9 Some coastal Malaystherefore m ay not even have any Su matran ancestors. M uch of wha t BorneanMalays know about their early history may be based on knowledge after thefact and may be part of a somewhat selective collective memory. The claim,however, is that, after Malayic speakers had left Borneo and had crossed over9 Brown 1970; Clynes forthcoming. This was also argued by Prentice (1988), althoug h for edi-torial reasons beyond his control the published version of his paper does not make this clear.


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to the opposite shores of the South China Sea where they developed a distinctMalay (as opposed to a Malayic) identity, some nuclear groups of SumatranMalays back-migrated to Borneo. They must have brought with them their(Malay) variety of Malayic as well as some (Sumatran) Malay cultural notions.Their ethnic awareness and cultural impact account for the presence of com-munities with a Malay identity in Borneo today.

Nor does the hypothesis exclude the possibility that these back-migratedMalays or their descendants might occasionally have penetrated rather farinland (Collins 1998a, note 5), and might have continued the acculturationprocess in these interior areas.

Finally, it does not require that the Bornean Malay dialects today are inevery way distinct from the inland forms of Malayic in Borneo, which areoften genetically more remote from Standard Malay. Dialect convergence andlinguistic osmosis are to be expected in areas where different speech formsare in contact.

Collins and Nothofer reject the notion of a back-migration. However, itis difficult to see what their advocacy of a local genesis of Bornean Malaylanguages could be based on. What compelling evidence do they have for thelocal development of a Malay identity and civilization in Borneo? And whatexactly do they mean by their rejection of a back-migration?It is fair to question the notion of a back-migration of large numbers ofMalays from Sumatra who would subsequently make up the entire present-day Malay stock in Borneo. But then again, this simplistic interpretation doesnot do justice to the original concept of a back-migration, which is primarilya linguistic one (Adelaar 1985,1992a; Blust 1988) with important cultural his-torical implications. It is not based on demographic or 'racial' considerations,even if it requires people to bring about such a movement (see above).

One could argue that the choice of the city-state of Srivijaya as a histori-cal starting point of Malay civilization is a random one. The Kutai area hasinscriptions that are at least two centuries older, and Indian artefacts foundin western Borneo date back to about the fourth century AD (Collins 1998b:5 referring to McKinnon 1994). But the evidence of Kutai inscriptions shouldnot be overestimated. Sanskrit inscriptions of similar antiquity are also foundelsewhere in Indonesia (western Java) and are moreover not unequivo-cal evidence for a distinct Malay settlement since they are in Sanskrit. Theoccurrence of Indian artefacts in western Borneo is open to several interpreta-tions, ranging from occasional and indirect trade relations with India to theone-time establishment of a Hindu-Malay settlement that has left no tracesapart from the artefacts in question. Such artefacts may become subsidiaryevidence if they are part of a larger set of evidence drawn from several disci-plines, but this is not the case for any part of Borneo. It is, however, the casein southern Sumatra, where we find a convergence of epigraphic, linguistic,


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10 K. Alexander Ade laararchaeological, historiographic and literary evidence for the existence of anancient Malay king dom . This kingd om may n ot have been the first one of itskind. Some scholars believe that Funan, an earlier settlement (in the Gulf ofSiam in present-day Kampuchea), might have been a Malayo-Chamic city.How ever, this remains uncertain,1 0 and even if Funa n turns out to be an earli-er Malay kingdo m, this wou ld have little impact on the view that M alayhooddeveloped on the western shores of the bouth China Sea, and not in Borneo.

Although the origins of Malay civilization are not entirely clear, Malaysby and large do share some cultural historical notions. These include a com-mo n ethnic awareness (now adays based largely on a common language an dreligion), a common literary tradition (no matter how diverse some of itsproducts have become), and the claim to a common origin on the westernshores of the South China Sea.Finally, returning to the main question of back-migrations, what is thelinguistic evidence against it? Collins (1994 and elsewhere) has argued thatall Bornean Malay dialects form a distinct subgroup. H owever, his evidencecan be refuted, and, if anyth ing, the idea of a single Bornean M alay sub grou psomehow weakens the argument that Borneo is the homeland of Malay(ic)(see section 7.1).

5 . A m o r e precise location of th e h o m e l a n d w ith i n B or n e oIf we take Borneo as the Malayic homeland, we need to addre ss the exact loca-tion of this homeland within Borneo. Adelaar (1985,1992a) simply mentionsBorneo as a possible hom eland . Blust (1988; 1994:32,46), however, places thehomeland in southwest Borneo, whereas Adelaar (1995) and Collins (1994,1 997,1 998a, 1998b) mention w estern Borneo, and Nothofer (1 997a) me ntionsnorth we st Borneo. Consequently, it seems that there is a 'defau lt' consensusamo ng these writers that the homeland was in western Borneo.1 1

The matter may seem merely cosmetic, but it has wider implications.Southwest Borneo is relatively close to the Barito area, which is the home-1 0 (Joedes (1947) believed that it was a Khmer settlement and interpreted its name as a sini-cized form of the Khmer word for 'hill', which is bnam in Old Khmer and phnom in modernKhmer.1 1 This may be less of a compromised decision than it seems. Blust (1994:46) locates theMalayic and Chamic homeland in 'southwest Borneo probably in or near the basin of the KapuasRiv er'. Purely geographically, however, the Kap uas basin lies in the centre of the wes tern p art ofthe Borneo island, a nd slightly m ore to the north of the (absolute) centre than to its south. Blustseems to take the political border between East Malaysia ('Malaysian North Borneo') and WestKalimantan (a province in Indonesian Borneo) as critical for a north /so ut h divide . If that is thecase, there is considerably m ore convergence in the locations pro pose d by A delaar, Blust, Collinsand Nothofer.


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Where does Malay come from ? 11

land of Malagasy (Dahl 1951). In an earlier publication, Blust (1984-85) sug-gests a c lose re la t ionship be tw een Javanese and som e of the Bari to lang uage s.This would open the door to some wider speculat ions of southern Borneoas the area of d ispersal of many more West-Malayo-Polynesian languages.How ever , our p resen t sta te of know ledge ab out the subg roup ing and spreadof M alayic isolects do es no t justify suc h specul ation s, ho w ev er attrac tive the ym ay seem . They are not corrobo rated by evidence from other d isc ipl ines suchas prehistory and archaeology (Bellwood 1997).

6. External classifications of the Malayic subgroupIn Dyen's lexicostatistical classification (1965) of Austronesian, Malay is clas-sified with Javanese, Madurese and Sundanese and some other languages inthe Malayo-Javanic subgroup, which in turn is part of larger classificatoryconfigurations such as the Javo-Sumatran Hesion, the Western IndonesianCluster, and the Hesperonesian Linkage within the Austronesian languagefamily. On the basis of this subgroup, Nothofer (1975) makes a phonologi-cal reconstruction of Proto-Malayo-Javanic, which he proposes had splitinto a Javanese, a Sundanese, and a Malay-Madurese branch. In his evalu-ation of Nothofer (1975), Blust (1981) argues that Javanese is geneticallyrather different from the other members of this proposed subgroup, andthat several other languages not included in the comparison (Salako, Iban,Rejang, Embaloh Land Dayak, Acehnese, Chamic) are closer to Malay thanis Javanese. Nothofer (1985) offers a readjustment of the Malayo-Javanicsubgro up, placing Malay together with M adurese, Iban, Lam pun g an d (pos-sibly) Sundanese in a different branch from Javanese.

Hudson (1970) offers an alternative and lower-order classification ofMalay: Malay forms the Malayic subgroup together with dialects and lan-guag es that are very closely related to Malay such as Minangkabau , Banjareseand Iban. Adelaar (1985 and elsewhere) uses this classification as a startingpoint for the reconstruction of Proto Malayic. Nothofer (1988) questions thisuse of the term 'Malayic' because it does not conform to the way it is usedin Blust (1981). He proposes a wider 'Malayic' subgroup including Salako,Embaloh and Rejang as well as a narrow Iban 'Malayan' branch, splittinginto an Iban branch on the one hand and the various Malay dialects on theother. Adelaar (1992a, 1993, 1994) rejects this classification. He demonstratesthat Embaloh and other Tamanic languages are not directly related to Malayand that there is no diagnostic device for assigning a separate branch statusto Iban. An earlier study by Blust demonstrates that Rejang does not belongto M alayic either (Blust 1984). Adelaar (1992a:2), who is reluctant to use lexi-costatistics for the definition of his Malayic subgrou p, propose s the following


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configuration of phonological innovations instead:1. Devoicing of PAn final stops2. PAn *j > PM % *-t3. PAn *z > PM */4. PAn *R > PM *r5. Reduction of PAn consonant clusters to their last com ponent6. The nasal in PAn heterorganic nasal + stop clusters becamehomorganic7. PAn initial *w was lost8. . PAn % *-ey, *-uy, *-iw > PM *i9. PAn *u, *-ew > PM *u10. PAn*PM*/j11. PAn*/ i , *?>PM*?or0Later subgrouping assumptions (Blust 1994; Collins 1997, 1998a; Nothofer1995, 1997a, 1997b) seem to conform at least implicitly to the delineation ofMalayic as proposed in Adelaar (1992a).The similarity betw een Malay, Cham ic languages, and A cehnese has longbeen recognized.12 Blust (1994) gives lexical evidence for a close genetic linkbetw een these languages. As noted in section 1, he believes that the langua geancestral to Malay(ic), Chamic and Acehnese was spoken in southwestBorneo, and that some of its speakers must have migrated from there tomainland Southeast Asia and Sumatra. He speculates that at one point theremust have been a Chamic-Malayic dialect continuum in mainland SoutheastAsia and S umatra: it m ust have run along the east coasts of Sumatra and theMalay peninsula and further north along the Gulf of Siam and the Mekongdelta to the Champa kingdom in southern Vietnam. The continuum wassubsequently disrupted by incoming Khmers (sixth century AD) and Thais(probably from the thir teenth centu ry AD o nw ard s; Blust 1994:46-7). Decisivefurther evidence for a Malayo-Chamic subg roup is Th urgo od's (1999) recon-struction of Proto Cham ic. Structural similarities between Proto Chamic andProto Malayic are particularly clear in their phonologies.

Ad elaar (forthcoming a) proposes a 'Malayo-Sum bawan ' subgrou p, whichexcludes Javanese and has a Madurese branch, a Sundanese branch, and onebran ch com prising the Malayic, Chamic, and Bali-Sasak-Sumbawa languages(see Figure 1). He finds th at Balinese, Sasak and S umbaw a share a significantpar t of their phonological history w ith M alayic and Cham ic. He reaches this12 Com pare Marrison 1975, Adelaar 1985, Blust 1988. A close relationship between Cham iclanguages and Acehnese was noticed by Niemann (1891) and several other scholars. It is dem-onstrated in detail by Thurgood (1999).


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Where does Malay come from? 13conclusion by using low-register lexicon in the comparison of the languagesinvolved (excluding high-register vocabulary because it is significantly moresusceptible to borrow ing). Altho ugh som e of the phonological develo pm entsare not forceful in themselves, or even unique to Balinese-Sasak-Sumbawaand Malayic, their configuration is striking. It includes PAn *w- > 0; PAn*q > *h; PAn *R, *r > *r; PAn *z > *;; PAn *;, *d > *d. In contrast, Madurese,Sundanese and particularly Javanese are phonologically m ore divergent fromMalayic as well as from Chamic or Bali-Sasak-Sumbawa. Balinese, Sasak an dSumbawa also have some basic vocabulary in common with Malayic as wellas formal similarities in vocabulary such as the metathesis in *qudip 'to live'which is reflected in Malay hidup and in Balinese and Sasak idup (but not inChamic *hudip). These comm on features sho uld be seen against the history ofLombok and especially of Bali, where linguistic and cultural influence fromJava has been ov erwh elming since the twelfth century, whereas M alay influ-ence has been relatively w eak.

Proto Malayo Sumbawan

Proto Malayic Chamic BSS

M adurese Sundanese Sasak Sum bawa Balinese Cham ic MalayicFigure 1. The Malayo Sum bawan subgro up


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14 K. Alexander Adelaar7. Internal classifications of the Malayic subgroupAdelaar (1985) classified the six Malayic isolects that formed the basis ofhis Malayic subgroup into an Iban branch and a branch including all otherMalayic isolects. In Nothofer's definition of M alayic (1988), Iban is also in aseparate branch (and so is Salako/K enday an).How ever, Adelaa r (1992a, 1993) has subsequen tly refrained from an inter-nal classification of the Malayic subgroup. In contrast, Collins and Nothoferhave recently proposed some detailed genetic subdivisions within Malayic,which I now turn to.7.1 The proposition of one single B ornean Malay subgroupCollins (1994) believes that the Malay dialects of Borneo form a single sub-group. Troto Malay' ('Bahasa Melayu Purba') began as one language or sev-eral closely related Aus tronesian langu ages som e 2,000 years ago . It split intoa Sumatra/Malay peninsula branch and a Borneo branch; the Borneo branchdeveloped into a northern branch (including Sambas Malay and variousBrunei Malay dialects) and a southeastern branch. The latter consists of SouthBornean Malay (with the various Banjarese Malay dialects) and East BorneanMalay (with Kutai and Berau Malay). This classification is also followed inJalud in C huch u (2003), a stud y on the classification of Brunei Malay dialects.

Collins's evidence for a single Bornean Malay subgroup is very limitedand does not stand scrutiny. His argum ent for it is the change of p enu ltimateschwa to a with concomitant gemination of the following consonant, whichhe claims took place in all its mem bers. Collins (1994) does no t distinguishbetween Malay and Malayic, and he does not include Iban and Kendayan/Salako in his classification. One might conclude from this that the descend-ants of his Proto Malay only represent the Malay branch of the Malayic sub-gro up . How ever, Collins (1994) does not make this explicit, nor does he makereference to previous studies on the classification of Malay. That it is in factthe Malay branch that he has in mind only becomes clear in some of his laterpublications (Collins 1997,1998a).

The change of penu ltimate schwa to a as a criterion for a Bornean M alaysubg roup is refuted by the existence of dialects such as Sarawak Malay w hichretaine d th is schwa as a schw a (C lynes forthcom ing, no te 9; Collins 1987:33).It is also refuted by the existence of several Bornean Malay isolects wherepenultimate schwa became o in contradistinction to final-syllable schwawhich became a (as documented, among others, by Collins himself (1997)and by Nothofer (1997b)). Furth erm ore, in Banjar M alay, there is no ev idencefor Collins's alleged consonant gemination after a historical schwa.Another observation in relation to Collins's Bornean Malay subgroupinghypothesis (1994) (be it an observation of a somewhat theoretical nature)


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is that it reduces the possibility of a homeland of Malay in Borneo. If allMalay dialects in Borneo were members of one exclusively Bornean Malaysubgroup, the island would be more homogeneous than if they belonged tovarious subgroups (whether exclusively Bornean or not). As a Malay home-land, however, one would in principle expect it to be genetically more diversethan other areas.

So it appears that the evidence for an exclusive Bornean Malay subgroupis wanting on several counts. Nevertheless, in his attempt to establish thissubgroup, Collins seems to have found evidence for a more limited geneticconfiguration, although the evidence for it is not without problems. Collins(1996:83-4) observes that Brunei Malay and Banjarese Malay share the possi-bility for verbs to combine the locative -i suffix with a following recipient-ori-ented suffix -akan. This combination points to a possible close historical rela-tionship. Collins (1996) furthermore believes that Bacan Malay (spoken onBacan Island in the North Moluccas) is an offshoot of Brunei Malay (Collins1996). Bacan Malay also allows a concatenation of a (location-oriented) suffix-i following (recipient-oriented) -akay. A link is not unlikely, considering thenature of the argument and the fact that both Bacan and Brunei were on thenorthern spice route between the western and eastern parts of the Indonesianarchipelago. Further evidence adduced by Collins (1996) for a Bacan Malay- Brunei Malay link is the maintenance of a nasal ligature {rj) in the first-per-son singular possessive pronoun {-rjku) and a number of lexical innovations.However, this evidence is not critical because the ligature in -rjku is a reten-tion. It is also found in Old Malay (gatru-rjku 'my enemies', De Casparis 1956:33,36) and should be attributed to Proto Malayic. Moreover, six out of nine ofCollins's lexical innovations are not exclusively shared (Adelaar 1999).7.2 The proposition of subgroups in western BorneoCollins (1997) distinguishes three linguistically distinct areas in westernBorneo: a Northwest Sector, a Central Sector and a Southwest Sector. Thesesectors are based on evidence from a comparison of basic vocabulary. Theevidence is insufficient to support the distinctiveness of the Central andSouthwest Sectors.

The distinction of a Northwest Sector is based on lexical and phonologicalevidence. It.includes Ahe, Banana' and Salako. These are dialects of a languagewhich Collins labels 'Kendayan'. The dialect group is no revelation consider-ing that it was already discussed in Hudson (1970) and in Adelaar (1992b,1995).13 A serious problem with Collins's evidence is that it is too limited inquantity and in scope. It does not make use of grammatical data although13 Ad elaar (1995) calls the subgroup 'West Malayic D ayak' but 'Kendayan' is more appropri-ate (see footnote 7).


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these are available in the form of several (published and unpublished) gram-matical sketches and many texts (Dunselm an 1949,1950; Ina Anak K alom andHudson 1970; Hudson 1970; Syahroen Alan et al. 1980; Thomas et al. 1984,1985; Adelaar 1991,1992b, 2002). Collins also overlooks an imp ortan t p hono-logical change, the reduction of voiced stops in original homorganic nasal +voiced stop clusters, as in *m/andi? 'to bathe > Kendayan, Salako tnani?.14 Ifnot evidence for a subgrouping, this change at least illustrates some of thephono logical history that Kendaya n isolects (or Northw est Sector) share w ithLand Dayak isolects. It also reinforces the position of Kendayan isolects as asubgroup that is phonologically distinct from Sambas Malay, in spite of thefact that Sambas Malay and Kendayan share the merger of *a and *d and theoccurrence of a final glottal stop. Collins's suggestion that Sambas Malaymay belong in a subgroup with Kendayan is unconvincing. An occasionalphonological resemblance between Sambas Malay and Kendayan is to beexpected con sidering that they are neigh bou ring isolects. Moreover, C ollins'streatment of ? as an innovation is aprioristic (section 7.3), and even if it turnsout to be an innovation, it is shared by too many forms of Malayic to haveany direct significance for subgrouping. Sambas Malay and Kendayan musthave been in contact for quite a long time, and some linguistic osmosis isexpected. Unless we can distinguish betwee n phonological innovations dueto common inheritance and phonological innovations due to convergence,we have very little reason indeed to use widespread features such as a finalglottal stop or merger of schwa to a as evidence for an exclusive commonorigin. One would also like to see morphosyntactic evidence (from SambasMalay) for such a claim, especially since Ke ndayan isolects have an aspectualsystem that clearly sets them apar t from all other forms of Malayic (Adelaar1992b, 2002).

The Central Sector includes the speech isolects of four villages along theKapuas River and its tributaries: Bagan Asam, Kalampok, Sungai Ringinand Ilir Kota. If these speech forms are meant to form a subgroup, the evi-dence is too weak. It consists of four phonological developments and a fewlexical innovations. The phonological developments are the change frompenultimate schwa to o, the presence of a glottal stop after final vowels incertain words, the change of *-y to -n after *i, and preplosion of final nasals.According to Collins, only one lexical innovation is unambiguous (PM*kamah/*kumuh 'dirty' was replaced by combe?, come?). In another case PMhas two etyma whereas the Central Sector has reflexes of only one of them:

14 According to Sipol Strassman anak Ambun (1992:xxxvii), in Salako as spoken in Lundudistrict (Sarawak) this voiced stop is still present a lthough ba rely aud ible. He does not write it inhis orthography. From my o bservations of Kendayan dialects in western Kalimantan, the voicedstop in question has disappeared.


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Where does Malay come rom? 17

P M *kA-iri, *kiba? ' l e f thand ' > Cen tral Sector kiba?. Som e other lexical innov a-t ions are not sh a re d a mo n g all m e m b e r s of the s u b g r o u p and are thereforenot d iagnost ic : jayi, jawi ' h a n d ' ( c o mp a re PM *tayan);jiawa ' mo u th ' ( c o mp a reP M *mulut); \okoy ' neck ' (compare PM *lihdr). The prob lem wi th these dis-t inctive features is tha t mos t of them a lso app ly to Iban ic languages . Apar tf rom rounding of p e n u l t ima te s c h wa and the lexical replacement of *kamah/*kumuh ' d i r t y ' by combe?, come?, all these features a lso apply to M u a l a n g 1 5and, except for prep los ion of final nasals, to Iban itself (compare Voanjiawa' m o u t h ' , rakuy ' neck ' , kiba? ' le f thand ' , jari ' h a n d ' ; *pirirj > pirin ' p la te , saucer ' ,*dagitj > dagin 'meat , f lesh ' ) . Preplosion of final nasals is a widespread a rea lfeature in western , centra l and sou thern Borneo . It is usua l ly not diagnos t icfo r subgrouping , which in the present case is d e mo n s t r a t e d by the fact thatit is not exhibi ted in Ilir Kota. Basically, this leaves rounding of p e n u l t ima tesc h wa as the only evidence for th i s subgroup , which is insufficient. Such asu b g ro u p wo u ld mo re o v e r not be a major divis ion in West Bornean Malayic:as far as the l imi ted ev idence shows , it wo u ld r a th e r be a subdiv is ion ofIbanic (Hudson 1970) . At any ra te , its pos i t ion has to be reassessed againstthe evidence of Ibanic .

The South we st Sector includ es the isolects spoken in Batu M as, Batu Tajamand Pan ta i Mas . 1 6 These isolects agree in that they exhibi t o for *a. The rest ofthe ev idence suppor ts a close l ink between Batu Mas and Baru Tajam alone.There are four phonological changes and three lexical replacements as wel las a fourth lexical replacement which Coll ins a t t r ibutes to Land Dayak inf lu-ence. The phonolog ica l changes in Batu Mas and Batu Tajam are 1. penul t i -m a t e *3 > o; 2. *r (a velar fricative) > a trill (in Panta i Mas it b e c a m e a u v u la rfricative); 3. *-ahu- > owu, ohu (as in *tahu ' k n o w ' > town, tohu?); and 4. theoccurrence of a final glottal stop. In Panta i Mas and possibly Batu Mas thisglottal stop is p h o n e m i c . In Batu Tajam, however, it is not , as it is heard afterany final vowel. The lexical replacements are mdjiomak ' chew' (compare PM*kujiah/*mamah, but com pare a l so Salakojiampa? 17 ' to chew bete l ' ) ; powi, poha?' leg' (compare PM *kaki); akaran porut 'intestines' (compare PM *pdrut); fur-thermore, silu?, silo? 'fingernail' must be a Land Dayak loan that replaced anearlier PM *kuku (Adelaar 1992a:131). Collins (1997:15) sees a pattern of twoseparate but closely related languages, with on the one hand Pantai Mas, andon the other hand Batu Tajam and Batu Mas as dialects of a single language .Clearly, there are some differences that set Pantai Mas off from Batu Mas andBatu Tajam. However, from the scanty and ambiguous evidence it is impossi-15 Compare Dunselman (1955). Mualang is an Ibanic dialect spoken east of Sanggau town inWest K alimantan.16 Precise locations are not specified.17 The final -k in the Southwest reflexes remains unexplained and is most likely due to amistranscription.


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ble to see how much these isolects differ from Co llins's Central Sector isolects,and how they fit in with the general p icture of West Bornean M alayic.Nothofer (1997b) challenges Collins's three West Bornean Malayic sub-groups. He makes a bipartite distinction into West Bornean Malayic (com-bining Collins's Northwest and Central Sectors) and Southwest BorneanMalayic. His evidence is a set of phonological, lexical and sema ntic inno va-tions. Phonologically, Southw est Bornean M alayic show s metathesis of h andliquid, nasal accretion in *hasdp 'smoke' and *basdh 'wet', and substitution ofy for *r in *ddndr ' to hear'.18 There are furthermore eight lexical innovationsand two semantic inno vations. This evidence is insufficient in itself, and partof it can be refuted as to its exclusivity. Salako, a West Bornean M alayic isolectaccording to Nothofer's classification, show s metathe sis of *h and liquid in allforms where *h historically p recede d a liquid, as in PM *baharu > barahu; PM*ba/hira? ' d ia r rhoea ' > bariha?; PM *di *hulu(?) ' ahead, in front ' > (*daloho? >)daoho?. Furthermore, as a rule, it exhibits nasal accretion before intervocalic*s in inherited vocabulary, compare PM *hi(ji)sdp ' to suck' > rj-ijisap; PM *isi?'meat, contents' > ijisi?; compare also Standard Malay musarj 'civet-cat' withSalako munsakn. Of the eight lexical innovations, sompak, sampak 'to chew' (aformal innovation rather than a lexical one in view of PM *sdpah 'to chew') ismatched by Salako sampa?; it is therefore not exclusive.In summary, it seems that we still have a very long way to go in arrivingat a solid classification of Malayic isolects in western Borneo. The evidencecollected by Collins and Nothofer is far too limited an d in some cases amb iv-alent and even contradictory.7.3 The classification of Jakarta Malay w ith B angka Malay and other 'southwestcorner' dialectsNothofer (1995) considers the areas w here Jakarta M alay, Bangka M alay andPalembang Malay are spoken - the 'southwest corner' - as a relic area inwhich several Proto Malayic suffixes only app ear in morphologically reduc edform, and where final syllable schwa never underwent the merger with *athat is reflected in all other Malayic isolects.19 The dialects in this southwestcorner are claimed to form a subgroup: 'the evidence appears to show thatJ[akarta] M[alay] most closely links to the dialect of Palembang and to thoseof the islands east of this area on the sou theastern coast of Sum atra. J[akarta]18

The changes in these three lexical items are actually a sporadic 'formal' innovation withina (certain) lexeme rather than a regular phonological innovation.19 Nothofer's claim (1995:89) that Pa lembang Malay retains final-syllable schwa is demonstratedwith one example only: Proto Austronesian *lafoj 'fly' > Pelambang Malay laht (p. 89). As I do nothave his source for Palembang M alay at my disposal, I am not able to verify whether the retentionof this schwa is systematic. His evidence for the re tention of final-syllable schwa in Bangka Malayis also insufficient bu t is backed u p convincingly with additiona l evidence in Nothofer (1997a).


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Where does Malay come from ? 19M[alay] spr ings f rom B[angka] M[alay] with which i t shares more innova-tions than with any other Malayic dialect ' (Nothofer 1995:95). Nothoferbases his c la im on a com binat ion of phonological , sem antic and lexical inno-vat ions . The c la im is not substant ia ted by the evidence, which is moreovertoo l imited to Jakarta Malay and Bangka Malay data to make a case for theinclusion of Palembang Malay and other southwest corner d ia lects . I re jectit for the following reasons.

N oth ofe r 's pho nolo gica l eviden ce consists of 1. loss of final *h , 2. frontingand ra is ing of *a (in final position or before final * h ) , 3. m etathes is in som eforms, 4. excrescent -? (glottal stop), and 5. initial *$ became Bangka Malayh - and Jakarta Malay 0 (stil l h - in Dewall 1909).1. Lo ss of final *h is typologica lly not a very significant s ou nd chan ge. Itis m oreove r very com m on in Malayic isolects as well as in other A ustrone sianlanguages. In Bangka Island it did not affect the dialects of the centre and ofPerlang (Nothofer 1997a:67, 70 (maps 9,11)).

2 . Raising (usually w ith sub seq uen t fronting or back ing) of final *a is alsofrequently observed in languages around the Java Sea and South China Sea.It is seen in Balinese, Javanese, sou the rn Borneo lang ua ges (includin g Ngaju,Maanyan and Malagasy) , Sambas Malay, var ious Peninsular Malay dia lectsand var ious Sumatran Malay dia lects ( including Minangkabau Malay ones) .This suggests that raising of * -a may have been an areal feature with sub-sequent minor vowel changes in individual languages. 2 0 Furthermore, th isra is ing ha pp en ed in Jakarta Malay to a ll V s that were f inal or w ere fol lowedby a final glottal stop. On the other hand, i t was a more highly conditionedchange in Bangka Malay dialects. The latter moreover exhibit very differentcondi t ion ing pa t te rns amo ng them se lves .

3. Nothofer g ives only two examples of metathesis , and these do notlend themselves to a phonological general izat ion. PMP *lipat ' fold ' > Jakartaand Bangka Malay ngdtepit idem, and Jakarta Malay kdlokopan, Bangka Malaykdlukup ' eyel id ' which correspond to Standard Malay kdlupak, kdlopak, pdlopak,pdlupok, and Sundanese kalopok (al l with the sam e m eaning ) .

4. Adelaar (1985, 1992a) gives an extensive treatment of final ?. Theevidence for -? in various Malayic isolects is ambivalent and does not allowan easy historical interpretation. Although there are cases where Iban -? isclearly innovative ,2 1 Adelaar interprets i t as a Proto Malayic retention because2 0 See Clynes (1989), who argues that as a resul t of the prest ige of the East Javanese kingdomof Majapahit , raising and backing of *-a spread through eastern Java t o central Java, and fromMalacca to Johore and further into the Malay peninsula; i t also spread eastward t o Bali. On thesame topic, compare also Tadmor (forthcoming).2 1 For instance, i n some loanwords (kicu? ' cheese ' < Malay kecu ' i d em ' < Por t uguese queijo' i dem' ) , or in words historical ly ending i n a d i p h t h o n g (kayu? ' w o o d ' < Proto Aust rones ian*kaSiw ' idem') .


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Zorc's (1982) arguments that it is a retention from Proto Austronesian cannotbe entirely refuted. It remains uncertain towhat extent -? is a Proto M alayicretention or an innovation, although Nothofer (1995) simply treats it as aninnovation w ithout m uch further elaboration. He thereby overlooks an impor-tant element inAdelaar's discussion of the Malayic evidence: unlike Iban -?which to some extent corresponds to reflexes of *H, *h and *S in Philippineand Formosan languages, Jakarta Malay -? does not do so at all and seems tobe an independent development. Neither does Jakarta Malay -? correspondto Bangka Malay -? . This may not appea r from the nine examples add uced inNothofer (1995), but a larger sample demonstrates that Jakarta Malay -? andBangka Malay -? have a different distribu tion. Elsew here, Nothofer (1997a:87-9) presents 26 Bangka M alay w ords inorder to show that their final -? corre-spond s regularly to that of Malayic isolects from western Borneo and TiomanIsland. When tested, it turns o ut that only three of these wo rds have a corre-sponding -? in Jakarta Malay (namely nasi? 'cooked rice', ddpe? 'fathom' andtume? 'louse') whereas 12 have -0 (namely Jakarta Malay lagi/lage 'again', aku'to confess', daki 'dirt', ton 'give', is i 'content', mandi 'bathe', mude 'young',22narjke 'jackfruit', paku 'fern', pejiu 'turtle', tajie 'ask', tdrime 'receive'). Foranother eleven w ords , neither Ab dul Chaer (1976) nor Kaehler (1966) gives aJakarta Malay cognate (namely Bangka Malay asow? 'dog', gdsi? 'gum s', fora?'monkey', palu 'hammer, blow', paya? ' swamp' , pari? 'ray fish', pdria? (?), puki?,'vagina', saba? 'python', turjku? 'hearth' and ru? 'casuarina').

No thofer's a-priori assessment of - ? as an innovation is furthermore con-tradicted by the fact that -? is particularly w ell represented in the supposedMalayic homeland itself, western Borneo. The evidence that he has accu-mulated from Bangka Malay and elsewhere shows that -? is more generalthan previously assum ed: on the face of it, his evidence actually gives moremo me ntum to the hypothesis that -? is a retention rather than an innovation.This is not to say that we can rule out -? as an innova tion (at this point I donot know how to interpret it). It only demonstrates that there is no quicksolution to the historical interpretation of -? in the Malayic subgroup , andthat Nothofer's new evidence calls for a reassessment of the whole issue.

5. Like the loss of *h-, the change from *s- to h- is not very significanttypologically. Adelaar (1992a:93) observes that the change in Jakarta Malayonly occurred incertain function words, but Nothofer also found six pairs ofJakarta Malay lexical w ord s with and w ithout s- which show that the changewa s more widespread. H e speculates that loss of *s- at some point in the pastmay have affected Jakarta Malay lexicon more generally but wa s later 'reestab -lished due to the tendency of "leveling out" the differences between J[akarta]M[alay] and Indonesian, Javanese, Sundanese, and Balinese' (Nothofer 1995:94). This is a plausible scenario. Note, however, that it does not necessarily2 2 F o u n d in Kaehler (1966:164).


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Where does Malay come rom? 21

su pp ort a close re la t ionship w ith Bangka M alay. M ost impo rtant ly , in BangkaM alay, loss of *s is not a gen eral feature bu t only affected the sou the rn dialectsof Arungdalem, Pakuk and Garung (Nothofer 1997a:74 (mapl5)) . I t is there-fore not part of the common history of Bangka Malay dialects.

Nothofe r p roposes th ree semant ic innova t ions in Jakar ta Malay andBangka Malay, which are general ly not d iagnost ic : 1 . the form bdri m e a n s'hit ' as well as 'give ' , 2. puhn ' tough, s t icky ' is the ' antonym' of StandardMa la y pulan ' nonadhes ive , c r i sp ' , and 3 . putri mandi ' r a inbow' con t ras t swi th S tandard Malay putri mandi ' s u g a re d d u m p l in g ' . F ro m A b d u l C h a e r ' sexample of Jakar ta Malay bdri ' to h i t ' i t appears that th is is merely an id i-omatic extension of the meaning ' to g ive ' in the sense of 'g ive a blow' . Thec o m p o u n d putri mandi is relatively recent (it cannot be older than the intro-duct ion of Sanskri t loanwords in Malayic as putri is a Sanskri t loanword) . I tacqu i red i t s mean ings th rough metaphor ic change and p robab ly o r ig ina tedin l i terary Malay ra ther than in a vernacular form.

Nothofer proposes only one lexical innovation: Bangka Malay drjga? ' no tw ant to ' co r respo nding to Jakar ta Malay drjga? ' n o ' a n d S a ra wa k M a la y r/ga?' on ly ' .

Summar iz ing Nothofe r ' s a rguments , h i s phonolog ica l ev idence i s no tcompell ing. Rais ing of *-a can be attributed to an areal feature of widergeographical scope. The s ta tus of Bangka Malay ? as an innova t ion cannotbe ascer ta ined , bu t m ore impor tan t ly , th is -? do es no t cor respon d to Jakar taMa la y -? . There is no case for structural metathesis. Loss of *h- and change of*s- to h are of a ra ther general nature . Most important ly , both these changeshave only partially affected the Bangka Malay area: for instance, whereasthe nor the rn dia lect area lost bo th *s- an d *h-, the central dialect area hasundergone nei ther change, and the southern dia lect area lost only *s-. (Thisd is t r ibu t ion in i t se l f would nar row down Nothofe r ' s subgrouping case to aclass if icat ion of Jakar ta Malay with Northern Bangka Malay only) . The lexi-cal and semantic evidence is very limited. Finally, there seems to be no cor-roborat ing extra l inguis t ic evidence for Nothofer ' s hypothesis .

I t so happens that the four major sound changes proposed by Nothoferfor h is su bg rou pin g (ra is ing of *-a, excrescence of - ? , loss of *h- and loss of *s-)a l so app ly to M aanya n , a non-Malay ic Au s t rones ian lang uage f rom sou th ernBorneo. The c ircumstance is anecdo tal , bu t i t goes to sho w that som e of thesechanges a re no t un ique in the h is to ry o f wes te rn Indones ian languages andmay eas i ly deve lop independen t ly .7.4 The classification of 'southwest corner' isolects with Malayic isolectsfrom north-west BorneoNothofer (1995:95) states that 'B[angka] M[alay] itself was probably set-tled from northwest Borneo and appears most closely related to Iban and


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Kendayan [...]'. In Nothofer (1997a:85-92) he classifies Bangka Malay,Belitung M alay, Palembang Malay an d Seraway Malay with the Malayic iso-lects from north we st Borneo (including Iban, Sarawak M alay and Kendayan)and with Tioman Malay (spoken on Tioman Island off the Malay peninsula'seast coast). His phonological evidence consists of the following innov ations:

1. Final *r was replaced with a glottal stop in *air 'water ' , *ikur 'tail',*kapur 'chalk', *gugur 'fall', *s3butir 'a grain (used as a noun classifier)' and(in Bangka Malay and Sarawak Malay only) *tidur 'sleep'.2. Final */ became Iban, Sarawak Malay and Bangka Malay glottal stopin certain words: the only example given is *ambil ' take' > ambi?.3 . Accretion of a glottal stop after original final vowels.4. In some cases, -h was replaced by a glottal in Bangka Malay, Ibanand Sarawak Malay: the examples given are reflexes of PM *basuh 'wash'(> Bangka Malay, Sarawak Malay, Iban basu? idem), *m-dntah/m-antah 'raw,unripe' (> Bangka Malay, Sarawak Malay mania?, Iban mata? id.), *ayah'father' (> Bangka Malay aya? 'older sibling', Iban aya? 'uncle, step-father'),*kujiah 'to chew' (> Iban, Sarawak M alay kupa? idem).5. Reduction of homorganic nasal + voiced-stop clusters to their nasalbefore the pe nultim ate syllable in trisyllabic wo rds in Iban, Palembang Malay

and Sarawak Malay.6. Irregu lar loss of *b in ^ukari23 'no( t)' > Bangka Malay, Belitung M alayukan, Iban ukay.7. Irregular loss of *n- in *nini 'grandmother '24 > Bangka Malay eney?,Iban ini?, Kendayan ene?.8. *h betwe en like vow els was lost in Iban, Sarawak Malay and BangkaMalay.9. Palatalization of final velars after * i in Iban, Sarawak Malay andBangka Malay.10. Preplosion of final nasals in Bangka Malay and Kendayan.

Nothofer gives the following morphological innovations:1. Loss of suffixes in Bangka Malay and in Iban.2. PM *paN- (which derived attributively a nd predicatively u sed no un sfrom verbs) became a general deriver of nouns in Iban and (apparently also)in Bangka M alay.25

2 3 *buksn ' n o , n o t ; o t h e r ' i n Adelaar (1992a:76ff ) .2 4 *nini? ' g r a n d p a r e n t , a n c e s t o r ' i n A delaa r (1992a :46 ) .2 5 T h i s i s m y qua l i f i ca t ion bas ed o n t h e m e a n i n g of paN- i n I b a n . N o t h o f e r ' s d e s c r i p t i o n oft h e m e a n i n g of I b a n a n d B a n g k a M a l a y pdN- i s s o m e w h a t i m p l i c i t : ' B A N [ B a n g k a M a l a y ] d a nI B N [ I b a n ] m e n g g u n a k a n a w a l a n pd - y a n g f u n g s i n y a s a m a d e n g a n S M [ S t a n d a r d M a l a y ] -an,m i s a l n y a S M makanan, B A N psmakan, I B N psmakai' (N o tho fe r 1997a :91 ) . E l s ew here h e specif iest h a t ' S e m u a d i a l e k B a n g k a [ .. .] d a n I B N m e m a k a i p r e f i x pd - y a n g m a k n a n y a ob j ek , i n s t r u m e n '(N o tho fe r 1997b :54 ) .


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Where does M alay come from? 233. The genitive suffix *-jta is also used as a nom inative pron ou n in Dul(a subdialect of Bangka Malay) an d in Sarawa k.

Finally, Nothofer gives eight lexical innovations and three semantic innova-tions.Nothofer's evidence is largely limited to data from Bangka Malay, Ibanand Sarawak Malay, and there are consequently no grounds for assumingthat Palembang, Tioman, Seraway or Jakarta Malay belong to his putativesubgroup.Evidence from Palembang Malay is virtually absent (it consists of onlysix words). Evidence from Tioman is also very limited, although it seems toconfirm the first and third phonological innovations (which are probably themost important ones). In the case of Seraway, there is no evidence that thisdialect shares any of the morphological, lexical and semantic innovationsgiven above, nor does it share any of the above phonological innovationsexcept for the substitution of a glottal for final *-r (the distribution of whichis moreover not entirely parallel in Seraway).

At this point it is important to note that none of Nothofer's phonological,morphological and lexical evidence for a subgroup including his southwestcorner languages and northwest Bornean isolects applies to Jakarta Malay,which, as discussed earlier, he claims to be an offshoot of Bangka Malay(section 7.3). (As dem on strate d above, the final glottal stop in Jakarta M alayis historically an idiosyncratic development.) Of the three semantic innova-tions, only one is documented with a possible Jakarta Malay cognate {erjga?'no(t) ' versus Bangka Malay and Iban erjga? 'not wa nt to ' ).

Consequ ently, the evidence on ly has imp lications for the position of Iban,Saraw ak an d B angka Malay. Fu rtherm ore, preplo sion of final nasals is no evi-dence for subgrouping (section 3), and the loss of suffixes affected Iban andBangka Malay26 in rather different wa ys so that it is not clear ho w this can beinterpreted as a com mo n innov ation. The loss of *-l in *ambil also occurs inseveral other M alayic isolects (including M inang kab au) a nd this change is ofa more general nature (Adelaar 1992a:90). Nevertheless, the remaining evi-dence is significant enough in that it indicates a common history - and pos-sibly a direct com m on origin - of Bangka Malay, Saraw ak M alay and Iban.

26 Resulting in the loss of all inherited suffixes in Iban while bringing about some flexionalderivation in Bangka Malay.


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8. ConclusionMalay historical linguists agree on the likelihood of the Malay homelandbeing in western Borneo. Viewed from the wider perspective of Taiwan asthe Austronesian ho meland, Borneo as the Malay hom eland certainly makesmore sense than the M alay peninsula, or even S umatra.

The hypothe sis of a back-migration of M alays from the w estern shores ofthe South China Sea (primarily Sumatra) to Borneo brings into perspectivesome im portan t cultural, historical and linguistic factors that w ould otherwiseremain unexplained. Although it has not yet met with full acceptance, criticsof this hypo thesis have no t so far produ ced substantive evidence against it.Although it still needs further elaboration, the idea of a Malayo-Chamicdialect continuum along the mainland Southeast Asian east coast offers someinteresting perspectives for M alay and ma inland Southeast Asian prehistory.Consensus amon g historical linguists with regard to the 'Borneo hy poth-esis' notw ithstand ing, the idea has at times been presen ted in an a priori way.It has also generated diverse and often incompatible theories on the earlymigrations of Malayic speakers and on the internal classification of their lan-guages. Most of the theories proposed in Collins (1994, 1997) and Nothofer(1995,1997a, 1997b) must be rejected for lack of solid evidence. In a few casesthese publications contain interesting observations, such as the phonologi-cal agreements between Bangka Malay and some Northwest Bornean Malayisolects (Nothofer 1997a), or the similarities in verbal morphology betweenBrunei Malay, Banjarese Malay and Bacan Malay (Collins 1996). In general,however, the past twenty years have not brought us any closer to a solidinternal classification of the M alayic language sub group .

The score is better for the external classification of Malayic. Thurgood'sreconstruction (1999) of Proto Chamic and Adelaar's comparison (forth-coming) of the Bali-Sasak-Sumbawa group w ith Cham ic, Javanese, M adureseand Sundanese, demonstrate that Chamic and Bali-Sasak-Sumbawa are moreclosely related to Malayic than any of these langu age grou ps is to Sundanese,M adurese or especially to Javanese.

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