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Research Article
Biogeographic history of the endangered dwarf buffalo, subgenus Anoa (Bovidae: Bubalus quarlesi and Bubalus depressicornis): a perspective based on mitochondrial DNA phylogeny
expand article infoDwi Sendi Priyono, Dedy Duryadi Solihin§, Achmad Farajallah§, Bambang Purwantara§
‡ Universitas Gadjah Mada, Yogyakarta, Indonesia
§ IPB University, Bogor, Indonesia
Open Access

Abstract

The Anoa, including the Mountain Anoa (Bubalus quarlesi) and the Lowland Anoa (Bubalus depressicornis) according to current taxonomy, are endangered bovid species endemic to the tropical island of Sulawesi. They are grouped in their own subgenus Anoa. The historical biogeography and phylogeny of this subgenus have not been well characterized. There are two hypotheses describing the colonization routes of large mammals in Southeast Asia: land-bridges and insular route. The present study aimed to understand the molecular phylogeny and test the historical colonization route of Anoa. A total of 71 mitochondrial DNA (cyt b gene and control region) sequence datasets from Anoa and other related species were analyzed. Molecular phylogeny reconstruction was done using a Bayesian inference model. Calibration points were used to estimate divergence time in Anoa based on a Bayesian phylogeny tree. Estimation of ancestral areas in Anoa ancestors using Reconstruct Ancestral State in Phylogenies was carried out to test the Anoa colonization route. The phylogenetic tree revealed the existence of two groups of Anoa, lowland and mountain Anoa, which diverged during the Middle Pleistocene 1.42 Mya (highest posterior density interval: 1.14–1.71 Mya). The Sundaland area is the most probable (P > 0.7) ancestral area for the Bubalus spp. in the Indonesian archipelago. The most probable Anoa colonization route appears to be through land-bridges, which geological records indicate formed between Sundaland and Sulawesi during the Pleistocene.

Key Words

Anoa, historical biogeography, insular dwarfisme, Land-bridge hypothesis, mtDNA phylogeny

Introduction

The genus Bubalus includes several species of wild and domesticated buffaloes, primarily found in Asia and Africa. The most notable species within this genus are the water buffalo (Bubalus bubalis), the Anoas (Bubalus depressicornis and Bubalus quarlesi), and the African buffalo (Syncerus caffer), which is sometimes classified under the same genus due to historical taxonomic confusion (Bibi and Vrba 2010). The Anoas, specifically, are endemic to Indonesia and are recognized for their smaller size compared to their relatives, which is a result of insular dwarfism, a phenomenon where species evolve to be smaller in size on islands due to limited resources and space (Benítez‐López et al. 2020). The taxonomy of Bubalus has undergone revisions, with ongoing debates regarding the classification and relationships among species, particularly between domesticated and wild forms (Bibi and Vrba 2010).

The Anoa, comprising Bubalus quarlesi and Bubalus depressicornis in the subgenus Anoa, have declined by 90% over the past 16 years, and they are even believed to be extinct in some locations. In 2016, the International Union for the Conservation of Nature (IUCN) Red List categorized both the Mountain Anoa (Bubalus quarlesi) and the Lowland Anoa (Bubalus depressicornis) as endangered species, with estimated populations of fewer than 2,500 individuals for each species (Burton et al. 2005). The Convention on International Trade in Endangered Species of Wild Fauna and Flora (CITES) included it in Appendix I in 2010, which means that Anoa are protected and cannot be traded. Anoa are grouped into lowland and mountain Anoa based on morphology and habitat. The taxonomic ambiguity surrounding the subgenus Anoa, is a significant issue in the field of wildlife conservation and biology (Burton et al. 2005). This ongoing debate highlights the necessity for comprehensive genetic and morphological assessments to clarify the taxonomic status of these endemic species and ensure effective conservation strategies (Tanaka et al. 1996; Pitra et al. 1997; Priyono et al. 2018, 2020, 2022).

Bubalus, a genus of Asiatic bovines within the family Bovidae, includes species that vary in body size. In descending order, from largest to smallest, these species are: Bubalus arnee (Kerr 1792) also known as the wild water buffalo, and its domesticated form, Bubalus bubalis (Linnaeus, 1758), from mainland Asia; tamaraw (Bubalus mindorensis Heude, 1888) from Mindoro Island, Philippines; Bubalus cebuensis (Croft, Heaney, Flynn & Bautista, 2006; extinct) from Cebu Island; Bubalus depressicornis (Smith, 1872), known as the lowland Anoa, from lowland areas of Sulawesi Island; and Bubalus quarlesi (Ouwens, 1910), known as the mountain Anoa (Fig. 1). Average body weight for each species, are provided in Fig. 1 to facilitate comparison, based on previous studies (Rozzi 2017, 2018; Shrestha et al. 2019). This size reduction is often attributed to limited resources, reduced predation pressures, and ecological niches that favor smaller body sizes (Benítez-López et al. 2021). For example, studies have shown that large mammals, such as elephants and hippos, significantly reduce size when isolated on islands (Benítez-López et al. 2021). Other mammals in Sulawesi, such as Stegodon sompoensis (Falconer, 1847) and Elephas celebensis (Hooijer, 1949), have also evolved according to insular dwarfism (Hooijer 1949). In the case of the Anoas, their smaller stature compared to other buffalo species is a direct result of these insular pressures, allowing them to thrive in the unique ecological conditions of Sulawesi (Benítez-López et al. 2021). Tougard (2001) stated that body size gradation, especially in large mammals, correlated with the possibility of their colonization of Sulawesi via Taiwan and the Philippine archipelago.

Figure 1.

Map of Southeast Asia depicting conditions around the Pleistocene period. The solid line shows the colonization route of large mammals according to the land-bridge hypothesis; dotted lines interpret the colonization route according to the insular hypothesis. This study aims to test these routes using mitochondrial DNA phylogeny to better understand the biogeographic history and evolutionary relationships of the Anoa (adapted from Tougard 2001).

Von Koenigswald (1935, 1939) proposed that mammals migrated during the Pleistocene era to Indonesia through the Philippines; his hypothesis was based on affinities between animals found in China and Java. An alternative theory postulates that the most probable colonization route for mammals to Sulawesi was through ancient corridors or land-bridges via Myanmar, Thailand, or Indochina (Bird et al. 2005; De Vos et al. 2007). At present, the relationship between body size gradation and insularism in Bubalus and its connection to potential colonization routes, as suggested by Tougard (2001), remains unknown. However, the specific colonization route of the Anoa to Sulawesi remains uncertain.

Tracing the biogeographic history of the Anoa group and related species is necessary to determine a possible colonization route for Anoa. Many studies have addressed this question using phylogenetic analysis, molecular dating, and reconstruction of ancestral geographic ranges. However, most of these studies focus predominantly on the Bovidae family in general such as Pseudois (Tan et al., 2017). Tan et al. (2017) effectively demonstrated the utility of Reconstruct Ancestral State in Phylogenies (RASP) in reconstructing the biogeographic history of the Pseudois genus within the Bovidae family. By integrating molecular data with advanced biogeographic modeling, the study provided valuable insights into the evolutionary dynamics and historical factors influencing the distribution of these species.

Molecular and particularly mitochondrial DNA data on Bubalus is abundant in GenBank. Mitochondrial DNA is inherited maternally and does not undergo recombination, which allows for clearer lineage tracing and a more straightforward interpretation of phylogenetic relationships. This characteristic makes mtDNA particularly useful for reconstructing colonization histories, as it can serve as a “molecular clock” that reflects historical population dynamics and colonization events more directly than nuclear DNA, which is subject to recombination and more complex inheritance patterns (Hassan et al. 2009; Hassanin et al. 2012; Budakva 2022). Statistical analysis of mitochondrial DNA cytochrome b (cyt b) gene and control region (CR) using Reconstruct Ancestral State in Phylogenies (RASP) has solved numerous biogeographic and historical questions (Banguera-Hinestroza et al. 2014; Lauron et al. 2014; Song et al. 2014; Clementz et al. 2014; Mahmoudi et al. 2017; Tan et al. 2017). The use of RASP is a powerful approach for tracing the biogeographic history of species. RASP allows researchers to reconstruct ancestral geographic ranges based on phylogenetic trees derived from molecular data, particularly mitochondrial DNA, which is advantageous due to its relatively high mutation rate and maternal inheritance patterns Song et al. (2016). This method facilitates the identification of historical colonization routes and the ecological factors influencing species distribution. RASP provides a comprehensive framework for understanding the evolutionary processes that have shaped the distribution of the Anoa and its relatives, thereby contributing valuable insights into the dynamics of insular dwarfism and the ecological adaptations of these unique mammals. The present study aims to test two hypothesized colonization routes (land-bridge and insular routes) and trace the biogeographic history of the Anoa using mitochondrial DNA phylogeny. This includes examining whether the two Anoa species are monophyletic, understanding their evolutionary relationship, and determining the significance of colonization patterns. Investigating these questions provides insight into the evolutionary mechanisms shaping biodiversity on islands and informs conservation strategies for these endangered species.

Materials and methods

Sampling and genomic DNA extraction

A total of 14 Anoa fecal samples were obtained in October 2020 from the Anoa Breeding Center, Manado, and Bontomarannu Education Park (Suppl. material 1). Eight samples were from lowland Anoa (Bubalus depressicornis) and six samples were from mountain Anoa (Bubalus quarlesi). We also collected six water buffalo (Bubalus bubalis) fecal samples as a comparison for the genus Bubalus. All fecal samples were collected in their entirety from each animal for genomic DNA extraction. Fecal samples were collected and stored in 50 mL tubes in Longmire’s Buffer. Fecal samples were preserved on ice until they arrived in the laboratory for molecular processing. Genomic DNA was extracted from the fecal samples according to the manufacturer’s protocol using the QIAamp Fast DNA Stool Mini Kit (Qiagen) and preserved at -25 ºC until analysis.

Polymerase chain reaction (PCR) and sequencing

To obtain a fragment of the cyt b gene and CR, we used Primer3 v. 4.0 (bioinfo.ut.ee/primer3-0.4.0) to design a specific primer set based on the lowland Anoa sequence (accession number NC020615). Each PCR amplification was performed in a total volume of 25 µL containing 5 μL of 1 × PCR buffer (Promega), 5 μL of 1 × GC enhancer, 1 μL of 0.2 mM dNTPs (Qiagen), 3 μL with 10 pg DNA template, 8,8 μL double-distilled water, 0.2 μL of 0.02 U/μL Taq polymerase (New England, BioLab), and 1 μL with 0.02 µM of each primer. The following primers were used to amplify cyt b and CR, respectively: CytB_Depress (F), 5′-CATTCATTGACCTCCCTGCT-3′; Cyt B_Depress (R), 5′-GCCGGAACATCATACTTCGT-3′; AFM22, 5′-CGTACGCAATCTTACGATCA-3′; AFM23, 5′-GTAGCTGGACTTAACTGCAT-3′. PCR thermo-cycling conditions were as follows: 5 min at 94 °C, followed by 35 cycles of 45 s at 94 °C, 45 s at 53.4 °C, 1 min at 72 °C, and a final 10 min at 72 °C. A 1.2% agarose gel was used to visualize the PCR amplicons. The PCR products were then purified and sequenced at the Integrated Research and Testing Laboratory (LPPT), Universitas Gadjah Mada (UGM). Cyt b and CR sequences were read in both forward and reverse directions to minimize errors and confirm nucleotide integrity, ensuring a reliable consensus sequence for analysis.

Phylogenetic analysis

The sequences were aligned by ClustalW in MEGA 7 (Kumar et al. 2016). Additionally, sequence data for Anoa from GenBank were included to supplement the dataset (Suppl. material 1). A phylogenetic tree was constructed according to a Bayesian inference (BI) algorithm using Bayesian evolutionary analysis and tree sampling in BEAST 2.4 (Bouckaert et al. 2014). The best-fit model for this sequence was HKY+G, with -lnL = 1984.8411, ti/tv ratio = 9.6353, p-invar = 0, and Gamma shape = 0.1260, as determined by the Akaike information criterion in jModelTest 2.1.7 (Darriba et al. 2012). BI used Markov Chain Monte Carlo (MCMC) iteration for up to 10,000,000 generations with every tree sample from every 1,000 generations. Out of 10,000 trees produced, 25% of those in the first generation were discarded and designated as “burn-in”. The remaining trees were combined to calculate posterior probability in a 50% majority-rule consensus tree. Branches from BI phylogenetic trees with posterior probability below 0.5 collapsed. The two consensus trees were then edited in FigTree 1.4.4 (http://tree.bio.ed.ac.uk/software/figtree/).

Reconstruction of ancestral areas

To determine the biogeographic history of Anoa based on the animal’s ancestry, we applied a statistical Dispersal Vicariance Analysis (S-DIVA) in a Bayesian framework implemented in RASP 4 (Yu et al. 2015). This method estimates the probability in an ancestral area from every possible phylogenetic node. Using RASP, MCMC Bayesian binary analysis calculated the default uncertainty from phylogenetic inference by optimizing the ancestor’s area in multiple trees (Yu et al. 2015). The following geographic regions were analyzed (Fig. 2): Sundaland, which comprises the biogeographic regions of Borneo and Java (representing Bos javanicus d’Alton, 1823 and B. bubalis); Wallacea, which includes both the lowland regions of Sulawesi, characterized by elevations ranging from 0 to 1000 meters above sea level (representing the lowland Anoa B. depressicornis), and highland Sulawesi (representing the mountain Anoa B. quarlesi) (Burton et al. 2005); and the Philippines (representing B. mindorensis). Bayesian binary MCMC analysis in RASP ran based on a set of Bayesian trees implemented in BEAST (as described above). A dataset including cyt b and CR sequences was used to reconstruct the Bayesian tree with a relaxed-clock model and a prior Yule speciation process tree model. The program was run for 10,000,000 generations and 1,000 generations of tree samples. After 25% of trees were discarded as burn-in, a maximum clade probability was obtained out of the remaining 7,500 trees. Bayesian binary MCMC analysis in RASP was performed on 7,500 post-burn-in trees by applying BEAST maximum clade probability. Analysis was carried out using the evolutionary HKY+G model running for 50,000 cycles with ten chains, sampling every 100 cycles, and discarding 100 trees.

Figure 2.

Representative DNA mitochondrial sequence datasets used to reconstruct ancestral areas. Sundaland is represented by Bos javanicus and Bubalus bubalis, Sulawesi lowland is represented by Bubalus depressicornis, Sulawesi mountains are represented by Bubalus quarlesi, and the Philippines are represented by Bubalus mindorensis.

Divergence time estimation

To estimate the time of speciation in Anoa, we used a Bayesian relaxed molecular clock model analysis implemented in BEAST and based on a dataset with cyt b mitochondrial DNA. For calibration, we chose three time-constraints:

  1. within the genus Bubalus, the split between B. depressicornis and B. bubalis was set at 1.3 ± 0.5 million years ago (Mya) (Ropiquet et al. 2012);
  2. within the subgenus Bubalus, the split between B. mindorensis and B. bubalis was set at 1.5 ± 0.2 Mya (Tanaka et al. 1996);
  3. the split between B. javanicus and the genus Bubalus was set at 13.68 ± 1.85 Mya (Hassanin and Ropiquet 2004).

As per the Bayesian tree model recommendation above, analysis was performed using the HKY+G model and a log-normal autocorrelated clock relaxation model. We tested the results using a uniform model on divergence time and a prior Yule speciation process tree combined with the previous three calibration points. All calculations were conducted with 10,000 cycles using ten chains, sampling every 100 cycles, and discarding 100 trees.

Results

Phylogenetic analysis

Cyt b (906 bp) and CR (696 bp) Anoa sequences were deposited in GenBank under accession numbers MK455804MK455817 and MK499408MK499433, respectively. Additional sequences from the genus Bubalus and sequences from the genera Bos and Bubalaphus were retrieved from GenBank, resulting in a total of 71 sequences used for the analysis. The phylogenetic trees constructed in this study include sequences labeled Bubalus depressions Charles and Bubalus depressions Ferguson. These labels reflect the naming conventions used in the GenBank sequence database and stem from historical inconsistencies in the taxonomy of Anoa. Because the BI phylogenetic tree for cyt b and CR showed identical topology, we are showing only the BI cyt b phylogenetic tree (Fig. 3). Boselaphus tragocamelus (Pallas, 1766) was used as an outgroup. The phylogenetic tree revealed two main clades: I and II. Clade I comprised all Anoa species (mountain and lowland Anoa) and included two sub-clades forming a monophyletic group. Posterior probability of 0.99 and bootstrap value of 100 revealed that lowland and mountain Anoa were a sister clade. Clade II comprised the tamaraw (B. mindorensis) and the water buffalo (B. bubalis), which formed a monophyletic group with high statistical support.

Figure 3.

Bayesian phylogenetic tree of mtDNA cyt b gene among Anoa and related species, with posterior probabilities (P > 0.70) shown on branches. The colors indicate clades: blue for Clade I (mountain Anoa Bubalus quarlesi and lowland Anoa Bubalus depressicornis), green for lowland Anoa, and yellow for Clade II (buffalo Bubalus bubalis and tamaraw Bubalus mindorensis). The CR tree exhibited the same topology.

Reconstruction of ancestral areas

MCMC Bayesian binary analysis in RASP using the cyt b gene and CR generated an ancestral area for the various Bubalus taxa at genus level (Fig. 4). Every node in the Bayesian binary MCMC tree is represented by a pie chart and assigned a colored portion to indicate the ancestral area’s possibility (P) of different taxa on a given tree branch.

Figure 4.

Ancestral area reconstruction in Anoa and related species: A. cyt b; B. CR. Pie charts on each node show the probability of each ancestral node having occurred at an inferred ancestral geographic location using the RASP method. Geographic locations are shown in different colors.

Node I represents taxa from the Bubalus group. The ancestral area for the genus Bubalus comprised the Sundaland area (P, 0.73) for both topologies. Node I then separated into two main groups: Node II (subgenus Bubalus) and Node III (subgenus Anoa). The subgenus Bubalus included B. bubalis and B. mindorensis. Sundaland was the most probable ancestral area for Node II (CR P, 0.69; cyt b P, 0.72). Analysis of Node III, which focused on the subgenus Anoa (Node III) revealed that Anoa’s ancestor inhabited mainly the Sulawesi Mountain area (CR P, 0.42; cyt b P: 0.43) and Sulawesi lowlands (CR P, 0.44; cyt b P: 0.46), with a minor proportion assigned to the Sundaland area (CR P, 0.06; cyt b P: 0.05) but none to the Philippines.

Divergence time estimation

The estimated divergence time for the Bubalus group was obtained by a time-calibrated tree formed with BEAST and based on BI topology (Fig. 5). The data show that Bubalus diverged during the Early to Middle Pleistocene 1.6 Mya (highest posterior density interval (HPD), 1.36–1.87 Mya). The subgenus Anoa diverged during the Middle Pleistocene 1.42 Mya (HPD, 1.14–1.71), whereas the subgenus Bubalus diverged during the Middle Pleistocene 1.35 Mya (HPD, 1.07–1.64).

Figure 5.

BEAST analysis shows the timeframe estimated for the evolutionary history of Anoa and related species in the genus Bubalus based on the cyt b gene. Bars at each node indicate the highest posterior density interval.

Discussion

Studies on insular dwarfism, such as those by Meiri (2007) and Lomolino (2005), emphasize the significance of ecological factors influencing body size evolution in island environments. RASP’s ability to integrate phylogenetic uncertainty into biogeographical reconstructions allows researchers to understand better the dynamics of size evolution in isolated populations (Nylander et al. 2008). This integration is crucial for elucidating the mechanisms behind insular dwarfism, as demonstrated in analyses of various taxa, including lizards and mammals (Meiri 2007; Geer and Lyras 2016).

This study included Boselaphus as an outgroup in phylogenetic tree to clarify the evolutionary relationships within the Bubalus genus and its subgenus Anoa. Including Boselaphus as an outgroup helps better understand the divergence between Anoa and other species of the Bovidae family. Previous studies, such as those by Pitra et al., (1997), suggested a closer relationship between the lowland Anoa and Boselaphus using noncoding regions of aromatase cytochrome P450 and lactoferrin. However, these studies were limited by small sample sizes (only 1–2 Anoa samples). In contrast, our phylogenetic analysis demonstrates that Boselaphus is more distantly related to Bubalus, reinforcing the classification of Anoa as a subgenus within Bubalus, rather than suggesting a closer relationship with Boselaphus. Most morphological and genetic studies seem to agree with our findings, grouping Anoa into the Bubalus genus rather than the Boselaphus one (Schreiber et al. 1993; Kakoi et al. 1994; Kikkawa et al. 1997; Burton et al. 2005; Groves and Grubb 2011; Rozzi 2017). Recent genetic studies, including those by subgenus Kakoi et al. (1994) and Tanaka et al. (1996), have suggested that Anoa is a subgenus of Bubalus.

The phylogenetic tree of Bubalus, based on this mitochondrial DNA, revealed two distinct clades: Clade I, which includes Bubalus arnee and Bubalus cebuensis, and Clade II, which includes Bubalus bubalis and Bubalus mindorensis. This topology supports the classification of Anoa species (Bubalus quarlesi and Bubalus depressicornis) as part of the Bubalus genus, specifically within the subgenus Anoa. The separation of Anoa species in Clade I from B. bubalis and B. mindorensis in Clade II highlights the distinct evolutionary trajectory of Anoa, suggesting a unique biogeographic history compared to other Bubalus species.

The designation of specimens as B. d. quarlesi and B. d. fergusoni across all phylogenetic trees in this study follows the naming conventions used in the GenBank sequence database, which stem from historical inconsistencies in the nomenclature of Anoa. This taxonomic ambiguity, resulting from the morphological similarities and overlapping ecological niches of Bubalus depressions and Bubalus Charles, complicates their classification. The Biological Species Concept, which focuses on reproductive isolation, may not fully apply to these species due to their restricted geographical ranges and potential hybridization in overlapping habitats (Burton et al. 2005; Frantz et al. 2018; Priyono et al. 2018, 2022).

The RASP analysis conducted in this study suggests that the colonization route of Anoa in Sulawesi likely occurred through Sundaland, rather than via the insular route through the Philippines. Previous molecular studies on the Bubalus distribution in Indonesia have also suggested that Bubalus migrated from mainland Asia to Sundaland and then onward to the western part of Indonesia (Sumatra and Java) (Barker et al. 1997; Lau et al. 1998). These studies are in agreement with the fossil record, whereby the oldest water buffalo and other large herbivores in the Southeast Asia archipelago were found within the Sundaland region during the Pleistocene (Pitra et al. 1997; Price and Webb 2006; Louys et al. 2007; Hassanin et al. 2012). During prehistoric time, dry spells were common and they formed a sort of land corridor that connected mainland Asia with the Indonesian Archipelago (Cockrill and Mahadevan 1974; Nachtsheim and Stengel 1977). Our result suggests that Bubalus used a land-bridge corridor from mainland Asia to the Indonesian Archipelago. This result complies with the fossil record, which indicates that the oldest modern water buffalo ancestor, Bubalus palaeokerabau (Dubois, 1908), existed in Cisaat, Java, Sundaland, during ancient times (Louys et al. 2007). At that time, the sea level was lower by 40–50 m, which allowed the Sunda Shelf to connect the Malay Peninsula to Java and Borneo; whereas a decrease of the sea level of 120 m extended the dry land mass to include the Philippines and Sulawesi (Voris 2000; Tougard 2001; Woodruff and Turner 2009). We believe that B. mindorensis, which is endemic to the Philippines, migrated from Sundaland to the Mindoro Island by way of Borneo and Palawan, Philippine Archipelago. The high similarity between mammals in mainland Asia and Palawan indicates that Palawan is an extension of Sundaland (Esselstyn et al. 2010) and supports the colonization of an ancestor of B. mindorensis through the same route.

This shows that the Anoa’s ancestor evolved as an endemic species after colonizing the Sulawesi Island from Sundaland rather than from the Philippines. A confirmation of the land-bridges colonization from the nearest parts of Sundaland to Sulawesi (especially from the west or east) is also found in modern mammals of Sulawesi, such as the babirusa (Thenius 1970; Van Den Bergh 1999; Bergh et al. 2001; De Vos et al. 2007), macaque (Abegg 2002; Blancher et al. 2008), and tarsier (Merker et al. 2009). Moreover, during the latest glacial phase, the Makassar strait separating South Sulawesi and the eastern coast of Borneo was only some 50 km wide (Bergh et al. 2001), allowing corridors from Sundaland to the southern or western part of Sulawesi. Additional fossil evidence includes a prehistoric painting (Rozzi 2017) of what appears to be Anoa, and which was found in Gua Batti, South Sulawesi. In summary, this and previous findings point to the land-bridges hypothesis as the most likely Sundaland-to-Sulawesi colonization route.

Previous studies on genomic age estimates have proposed the divergence time for Bubalus to be between 2 and 1 Mya (Tanaka et al. 1996; Hassanin and Douzery 1999; Hassanin et al. 2012; Bibi 2013; Bibi and Métais 2016), which implies Early Pleistocene as the time for the first island colonization by mainland water buffalo. This hypothesis agrees with the fossil record’s earliest indication of water buffalo and other large herbivores from the Southeast Asia Archipelago on Java during the Pleistocene (Pitra et al. 2004; Louys et al. 2007; Ropiquet et al. 2012). Fossil records indicate as well that the ancestor of the Anoa appeared in Sundaland between Early to Middle Pleistocene (Bergh et al. 2001; Tougard 2001). Other fossil records have revealed that the Anoa is closely related to hemibos from Tatrot and the Pinjor formation of the Siwaliks. Magnetostratigraphic analysis assigned the specimens to a time during the Middle-Late Pleistocene (Azzaroli 1983). Calibration of this time interval was dated to between 3.20 Mya and 1.78 Mya (Spell and McDougall 1992), which is similar to our molecular dating analysis. However, other studies suggest an even longer divergence time for the Anoa, for example 12,4 Mya according to Pitra et al. (1997) or 4,3 Mya according to (Stelbrink et al. 2012). The exact time may be influenced by the distant phylogenetic relationship between Bubalus species and the close relationship to Boselaphus (Pitra et al. 1997) discussed before. In conclusion, our result is supported by previous research which indicates that the Anoa is a plesiomorphic member of the Bovini clade and supports the placement of Anoa as a subgenus within Bubalus, whose ancestor it diverged from around 1.42 Mya. Although our knowledge of the endemic Sulawesi buffalo is hindered by limited sample size, the present study provides important information on the biogeographic history of the Anoa, especially its colonization of Sulawesi.

While mitochondrial DNA (mtDNA) analysis provides valuable insights due to its low mutation rate, this method may limit the resolution of more recent evolutionary changes. Incorporating genomic approaches and expanding the sample size can provide a higher resolution of evolutionary history, enabling more comprehensive genetic diversity and population structure analyses. Integrating genomic data and fossil evidence can refine interpretations of phylogenetic relationships and historical colonizations. In this present study, we tested existing hypotheses for large colonization routes to the Indonesian archipelago using molecular data, with a particular focus on the case of Anoa. Our results support the previous hypothesis that the migration of Anoa followed one of the major migration routes to the Indonesian archipelago, specifically through Sundaland. In the evolutionary history of Anoa, habitat conditions have played a crucial role in preserving their genetic diversity. Mountains and lowland Anoa were separated 1.42 million years ago. They are separated due to fragmentation, which is exacerbated by deforestation pressures, leading to a reduction in genetic diversity (Aninta et al. 2024). Connectivity refers specifically to the ability of Anoa populations to move between fragmented habitats, maintaining gene flow between isolated populations. Sulawesi is an island with a high level of endemism, so by protecting the two Anoa species in Sulawesi, it will also help conserve many other species. Future studies should incorporate fossil records alongside genomic data to build a more complete evolutionary framework for Anoa, providing deeper insights into their historical biogeography.

Acknowledgments

We would like to thank the Indonesia Secretariat of Scientific Authority for Biodiversity (SKIKH) BRIN for the research recommendation and the Directorate General of Nature Resources and Ecosystem (KSDAE) Indonesia for granting permission for this research. We also thank Arin from Anoa Breeding Center, Manado, Indonesia, and Bontomarannu Education Park, Gowa, Indonesia. Finally, we extend our gratitude to Montana Stone and Peter Keaney (Cornell University) and Gita Alvernita (IPB University) for their valuable assistance in reviewing and proofreading this manuscript.

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Supplementary material

Supplementary material 1 

Information of samples used in this research

Dwi Sendi Priyono, Dedy Duryadi Solihin, Achmad Farajallah, Bambang Purwantara

Data type: docx

This dataset is made available under the Open Database License (http://opendatacommons.org/licenses/odbl/1.0). The Open Database License (ODbL) is a license agreement intended to allow users to freely share, modify, and use this Dataset while maintaining this same freedom for others, provided that the original source and author(s) are credited.
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