A new frog species Microhyla laterite has been discoverd in laterite habitats in
and around the coastal town of Manipal, India. The frog, which is the size of a
thumbnail, was discovered by a team of researchers from India and the National
University of Singapore (NUS). The research team was led by Mr
Seshadri K S, a PhD student from the Department of Biological Sciences at the
NUS. The frog was delimited using molecular, morphometric and bioacoustics
comparisons. The frog
has a call that can be easily mistaken for that of a cricket.
The laterite rock formations date as far back as the Cretaceous-Tertiary boundary and are considered to be wastelands in-spite of their intriguing geological history.
The laterite rock formations date as far back as the Cretaceous-Tertiary boundary and are considered to be wastelands in-spite of their intriguing geological history.
The
researchers sign off saying “With molecular tools becoming increasingly
reliable and affordable; studies could shed light into the population dynamics
of these small frogs found in isolated and severely fragmented landscapes. In
context of laterite habitats, studies have estimated the early diversification
period of Microhylidae to be at the late Cretaceous period and that of Microhyla to
be in the lower Tertiary period; signifying that several lineages survived
through the KT boundary. Since M. laterite appears
to be restricted to laterite rock formations along the West coast, further
research on determining divergence times of M. laterite and
testing for an association with laterite formations would enable a better
understanding of biogeography, systematics and paleo-ecology. This will enable
us to explore interesting evolutionary ecology questions inMicrohyla.”
Journal
Reference:
K.
S. Seshadri, Ramit Singal, H. Priti, G. Ravikanth, M. K. Vidisha, S. Saurabh,
M. Pratik, Kotambylu Vasudeva Gururaja. Microhyla laterite sp. nov., A
New Species of Microhyla Tschudi, 1838 (Amphibia: Anura: Microhylidae) from a
Laterite Rock Formation in South West India. PLOS ONE, 2016; 11
(3): e0149727
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