Japan Geoscience Union Meeting 2016

Presentation information


Symbol M (Multidisciplinary and Interdisciplinary) » M-IS Intersection

[M-IS17] Paleoclimatology and paleoceanography

Mon. May 23, 2016 1:45 PM - 3:15 PM A04 (APA HOTEL&RESORT TOKYO BAY MAKUHARI)

Convener:*Tomohisa Irino(Faculty of Environmental Earth Science, Hokkaido University), Minoru Ikehara(Center for Advanced Marine Core Research, Kochi University), Akira Oka(Atmosphere and Ocean Research Institute, The University of Tokyo), Yusuke Okazaki(Department of Earth and Planetary Sciences, Graduate School of Science, Kyushu University), Ikuko Kitaba(Research Centre for Palaleoclimatology, Ritsumeikan University), Akihisa Kitamura(Institute of Geosciences, Faculty of Science, Shizuoka University), Masaki Sano(Research Institute for Humanity and Nature), Ryuji Tada(Department of Earth and Planetary Science, Graduate School of Science, The Univeristy of Tokyo), Takeshi Nakagawa(Ritsumeikan University), Akira Hayashida(Department of Environmental Systems Science, Doshisha University), Chair:Tomohisa Irino(Faculty of Environmental Earth Science, Hokkaido University)

3:00 PM - 3:15 PM

[MIS17-06] Assessment of time-dependent evolutionary rates of rodent mitochondrial DNA based on paleoclimatic calibrations of the Japanese Islands

★Invited papers

*Hitoshi Suzuki1 (1.Faculty of Environmental Earth Science, Hokkaido University)

Keywords:mitochondrial DNA, evolutionary rate, Japanese Islands, Apodemus species, Quaternary glaciation

Use of the reliable time-dependent evolutionary rates of mitochondrial DNA might allow us to built realistic evolutionary scenario with phylogenetic inferences, covering a broad time scale based on the phylogenetic inferences. Other than using fossil evidence, it is possible to estimate evolutionary rates by relying on the well-established temporal framework of the Quaternary glacial cycles that would likely have promoted both rapid expansion events and interisland dispersal events. We are now focusing on the mitochondrial cytochrome b (Cytb; 1140 bp) sequences of a temperate species of wood mice (Apodemus argenteus and A. speciosus) from the Japanese Islands to assess evolutionary rates (site/million years) and obtained ca. 11% and 3% under assumption of rapid expansion and a priori information of the Quaternary climate fluctuation around 10 and 130 k years ago (ka), respectively (Suzuki et al., 2015). In addition, assuming that land-bridge like structures were created intermittently at glacial maxima of 100 k year intervals and shaped divergence patterns of the Cytb sequences of the larger Japanese wood mice A. speciosus, we obtained estimated evolutionary rates of 3.3 to 2.7% with presumed calibrations of 140, 250, 350 and 440 ka, through comparison of sequences from peripheral remote islands. In survey of rapid expansion signals in the lesser Japanese wood mouse Apodemus argenteus and three continental congeneric species from Asia and Europe, three levels of t values can be categorized into three levels, 3.9, 5.0-5.7 and 7.8-8.1. Adopting the idea in which the climate turned to be warm after preceded time of rapid cooling at 15, 53, 82 and 119 ka based on available pollen fossil evidence of trees including Quercus species, the evolutionary rates were estimated to be 11.4, 4.4-5.0, 3.1%, respectively. Here we propose the use of the time-dependent evolutionary rates (11~2.7%/site/million years) for the time span of 10 to 450 ka, hoping that it can be applicable to other species of murine rodents including mice and rats.
Reference: Suzuki Y, Tomozawa M, Koizumi Y, Tsuchiya K, Suzuki H (2015) Estimating the molecular evolutionary rates of mitochondrial genes referring to Quaternary Ice Age events with inferred population expansions and dispersals in Japanese Apodemus. BMC Evolutionary Biology, 15,187.