Distribution

Read full entry

Distribution

 This is the representative of Bassaricyon neblina on the eastern slopes of the Western Andes of Colombia (e.g., Castilla Mountains [AMNH]; Sabanetas [FMNH]; El Tambo [NMS]; the vicinity of Cali [Poglayen-Neuwall 1976]; El Duende [Saavedra-Rodríguez and Velandia-Perilla 2011]; Gallera: “western slope of most eastern ridge of southern Western Andes” [AMNH, Paynter 1997:222]) and the western slopes of the Central Andes of Colombia (Cerro Munchique [FMNH]). One specimen (AMNH 42351, from Santa Elena, Antioquia Department) derives from the eastern slopes of the Central Andes in northern Colombia (habitat described as “deforested, grassy, and bushy (Chapman 1917:61)”; Paynter 1997:403); this shows that this subspecies also crosses to the eastern slopes of the Central Andes in Antioquia. Further south, in the department of Huila, the smaller subspecies Bassaricyon neblina hershkovitzi subsp. n. (see below) occurs on the eastern slopes of the Central Andes.  Records to date of Bassaricyon neblina osborni are from 1500 to at least 2750 m elevation in Cauca, Valle del Cauca, and Antioquia Departments of Colombia (Figure 16). Bassaricyon medius medius is also recorded from the Cauca Valley (east slopes of Western Andes and western slopes of Central Andes) at elevations up to at least 725 m (UV-3774: Saavedra-Rodríguez and Velandia-Perilla 2011; see account of Bassaricyon medius below), so these two taxa (Bassaricyon medius medius and Bassaricyon neblina osborni) are presumably regionally sympatric (and probably elevationally stratified) across the range of this Olinguito subspecies on the slopes of the Western and Central Andes.

Trusted

Creative Commons Attribution 3.0 (CC BY 3.0)

© Kristofer M. Helgen, C. Miguel Pinto, Roland Kays, Lauren E. Helgen, Mirian T. N. Tsuchiya, Aleta Quinn, Don E. Wilson, Jesús E. Maldonado

Source: ZooKeys

Belongs to 0 communities

This taxon hasn't been featured in any communities yet.

Learn more about Communities

Disclaimer

EOL content is automatically assembled from many different content providers. As a result, from time to time you may find pages on EOL that are confusing.

To request an improvement, please leave a comment on the page. Thank you!