Abstract

High-affinity K+ (HAK) transporters are encoded by a large family of genes and are ubiquitous in the plant kingdom. These HAK-type transporters participate in low- and high-affinity potassium (K+) uptake and are crucial for the maintenance of K+ homeostasis under hostile conditions. In this study, the full-length cDNA of CcHAK1 gene was isolated from roots of the habanero pepper (Capsicum chinense). CcHAK1 expression was positively regulated by K+ starvation in roots and was not inhibited in the presence of NaCl. Phylogenetic analysis placed the CcHAK1 transporter in group I of the HAK K+ transporters, showing that it is closely related to Capsicum annuum CaHAK1 and Solanum lycopersicum LeHAK5. Characterization of the protein in a yeast mutant deficient in high-affinity K+ uptake (WΔ3) suggested that CcHAK1 function is associated with high-affinity K+ uptake, with Km and Vmax for Rb of 50 μM and 0.52 nmol mg−1 min−1, respectively. K+ uptake in yeast expressing the CcHAK1 transporter was inhibited by millimolar concentrations of the cations ammonium () and cesium (Cs+) but not by sodium (Na+). The results presented in this study suggest that the CcHAK1 transporter may contribute to the maintenance of K+ homeostasis in root cells in C. chinense plants undergoing K+-deficiency and salt stress.

Highlights

  • Plants require a variety of mineral nutrients throughout their ontogeny to complete their growth and development (Marschner, 2012)

  • Total RNA was isolated from the roots of C. chinense seedlings exposed to K+ starvation for 15 days to identify putative K+ transporters that can be expressed in this growth conditions

  • The cDNA corresponding to the CcHAK1 gene (KT202302) was isolated from the RNA of habanero pepper roots (C. chinense) grown in the absence of K+

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Summary

Introduction

Plants require a variety of mineral nutrients throughout their ontogeny to complete their growth and development (Marschner, 2012). Potassium (K+) is one of the most important essential macronutrients and the most abundant inorganic cation in plant cells. Despite the abundance of K+ in the earth’s crust (2.1%), its low availability in the soil limits vegetal growth and reduces the productivity of large areas of arable land (Benito et al, 2014; Zörb et al, 2014). K+ fertilization has become a common and necessary practice in agriculture. Such fertilization is very expensive, and a great proportion of the added K+ is lost by lixiviation (Römheld and Kirkby, 2010; Zörb et al, 2014)

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