bioRxiv Science⌕ Search

Biology subjects

Masroor, R.

Publications and source records attributed to Masroor, R..

2 recordsLinked to original sources

The Hindu Kush, not the Indus Valley, divides amphibian biogeographic realms

The boundary between the Palearctic and Oriental biogeographic realms is one of the oldest unresolved problems in Eurasian biogeography. In Central and South Asia, this transition is remarkable and has often been linked to the Indus River Valley, yet the role of adjacent mountain systems and arid landscapes has remained largely untested because critical regions, especially Afghanistan, have been chronically under-sampled due to difficult, long-term socio-political situation. Here we use a unique amphibian material from Afghanistan and adjacent northwestern Pakistan to test whether the Hindu Kush marks the effective boundary between these two realms. Combining molecular barcoding across all seven amphibian genera inhabiting the region with updated distribution records, we find a strikingly consistent lineage turnover centered on the eastern Hindu Kush and adjacent arid systems. Palearctic taxa reach their southeastern limits along the massif, whereas Oriental taxa extend only to its southern foothills. By contrast, Oriental lineages cross the Indus River without detectable phylogeographic break, indicating that the river valley does not function as a major biogeographic boundary for the taxa examined. The Hindu Kush also harbors endemic relict taxa of both Palearctic and Oriental affinities, revealing a dual role as both refugium and dispersal barrier. Thus, our results identify the Hindu Kush as the de facto boundary between the Palearctic and Oriental realms in this part of Eurasia and show that under-sampled arid-montane regions can disproportionately improve global biogeographic frameworks.

evolutionary biology↗

Relict groups of spiny frogs indicate Late Paleogene-Early Neogene trans-Tibet dispersal of thermophile faunal elements

BackgroundThe Himalaya-Tibet orogen (HTO) presents an outstanding geologically active formation that contributed to, and fostered, modern Asian biodiversity. However, our concepts of the historical biogeography of its biota are far from conclusive, as are uplift scenarios for the different parts of the HTO. Here, we revisited our previously published data set of the tribe Paini extending it with sequence data from the most western Himalayan spiny frogs Allopaa and Chrysopaa and using them as an indirect indicator for the paleoecological development of Tibet. MethodsWe obtained sequence data of two mitochondrial loci (16S rRNA, COI) and one nuclear marker (Rag1) from Allopaa samples from Kashmir Himalaya as well as Chrysopaa sequence data from the Hindu Kush available from GenBank to complement our previous data set. A Maximum likelihood and dated Bayesian gene tree were generated based on the concatenated data set. To resolve the inconsistent placement of Allopaa, we performed different topology tests. ResultsConsistent with previous results, the Southeast Asian genus Quasipaa is sister to all other spiny frogs. The results further reveal a basal placement of Chrysopaa relative to Allopaa and Nanorana with an estimated age of ca. 26 Mya. Based on the topology tests, the phylogenetic position of Allopaa as a sister clade to Chaparana seems to be most likely, resulting in a paraphyletic genus Nanorana and a separation from the latter clade around 20 Mya. Both, the placements of Chrysopaa and Allopaa support the presence of basal Paini lineages in the far north western part of the HTO, which is diametrically opposite end of the HTO with respect to the ancestral area of spiny frogs in Southeast Asia. These striking distributional patterns can be most parsimoniously explained by trans-Tibet dispersal during the late Oligocene (subtropical Chrysopaa) respectively early Miocene (warm temperate Allopaa). Within spiny frogs, only members of the monophyletic Nanorana+Paa clade are adapted to the colder temperate climates, indicating that high-altitude environments did not dominate in the HTO before ca. 15 Mya. Our results are consistent with fossil records suggesting that large parts of Tibet were characterized by subtropical to warm temperate climates at least until the early Miocene.

evolutionary biology↗