Abstract

The giant lobelias in East African mountains are good models for studying molecular mechanisms of adaptation to different altitudes. In this study, we generated RNA-seq data of a middle-altitude species Lobelia aberdarica and a high-altitude species L. telekii, followed by selective pressure estimation of their orthologous genes. Our aim was to explore the important genes potentially involved in adaptation to different altitudes. About 9.3 Gb of clean nucleotides, 167,929–170,534 unigenes with total lengths of 159,762,099–171,138,936 bp for each of the two species were generated. OrthoMCL method identified 3,049 1:1 orthologous genes (each species was represented by one ortholog). Estimations of non-synonymous to synonymous rate were performed using an approximate method and a maximum likelihood method in PAML. Eighty-five orthologous genes were under positive selection. At least 8 of these genes are possibly involved in DNA repair, response to DNA damage and temperature stimulus, and regulation of gene expression, which hints on how giant lobelias adapt to high altitudinal environment that characterized by cold, low oxygen, and strong ultraviolet radiation. The negatively selected genes are over-represented in Gene Ontology terms of hydrolase, macromolecular complex assembly among others. This study sheds light on understanding the molecular mechanism of adaptation to different altitudes, and provides genomic resources for further studies of giant lobelias.

Highlights

  • The upland East Africa is characterized by isolated mountains that reach alt. of 4000 m or higher

  • The results indicated that 79,825 unigenes of L. aberdarica (48%) and 84,296 unigenes of L. telekii (49%) have significant matches (E-value < 10−5)

  • The RNA-seq data are informative for SSR marker development and population genetic studies of the giant lobelias

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Summary

Introduction

The upland East Africa is characterized by isolated mountains that reach alt. of 4000 m or higher. The upland East Africa is characterized by isolated mountains that reach alt. Vegetation in these mountains displays a conspicuous altitudinal zonation, starting with a montane forest belt, followed by an (subalpine) ericaceous belt, and an afro-alpine belt above 3500– 4000 m alt. The climate of montane forest is relatively temperate and seasonal, with temperatures falling below 10◦C in cold season and rising to above 30◦C in warm season. The belt contains moderate levels of species richness, which is higher than the surrounding lowlands (Agnew and Shirley-Agnew, 1994). Species richness decreases with increase in altitude and fluctuating temperature (Hedberg, 1969). The afro-alpine belt is characterized by an extreme weather pattern with “summer every

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