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Mitogenome Announcement

The complete mitogenome of Acropora nana (Cnidarian: Acroporidae)

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Pages 544-545 | Received 17 Jul 2017, Accepted 07 Aug 2017, Published online: 17 Aug 2017

Abstract

Acropora nana belongs to Cnidaria phylum, Anthozoa class, and staghorn coral groups. Like other corals, Acropora could be an indicator for environmental changes and with great conservational values. In this study, the complete mitogenome sequence of A. nana (Cnidarian: Acroporidae), has been decoded for the first time by low coverage whole genome sequencing method. The overall base composition of A. nana mitogenome is 25.0% for A, 13.8% for C, 24.4% for G, and 36.9% for T, and has low GC content of 38.2%. The assembled mitogenome, consisting of 18,480 bp, has unique 13 protein-coding genes (PCGs), three transfer RNAs, and two ribosomal RNAs genes. The A. nana has one big intron insert in ND5 gene. The complete mitogenome of A. nana provides essential and important DNA molecular data for further phylogenetic and evolutionary analysis for stony corals.

Coral reefs are known as home for many marine species. Climate change causes rising ocean temperature, ocean acidification, and more frequent storm. Rising ocean temperature can lead to coral bleaching. Like other corals, Acropora could be an indicator for environmental changes. Acropora nana can be found in Taiwan, China, Australia, Indonesia, and Japan sea water. Like other corals, A. nana feeds on tiny zooplankton, however, it receives most of the nutrients from single-celled algae ‘zooxanthellae’ which live within its tissues. Stable environment for zooxanthellae to live is provided by A. nana, in returns it receives nutrients from photosynthesis by zooxanthellae. This mutualism symbiosis restricts A. nana to live in shallow, clear, and warm water, where photosynthesis is possible, and makes it to grow quickly and form large reef structure. The colonies are quite delicate and readily breaking apart if disturbed, but the colonies live in high wave current sea (Veron and Stafford-Smith Citation2000). A. nana is morphologically similar to A. valida in wave washed habitats and it can be distinguished by its thicker branchlets and chunkier radial corallites. This issue makes the classification and molecular methods are needed in this coral identification.

Samples of A. nana (TIOSOA-LCC-20150704-Acro.Na) were collected from Houhai coral reefs in Sanya (18°16′32.58″N 109°44′10.74″E), Hainan Province. We used next generation sequencing to perform low-coverage whole genome sequencing according to our previous protocol (Shen et al. Citation2016). Initially, the raw next generation sequencing reads were generated from HiSeqX Ten (Illumina, San Diego, CA). About 0.13% raw reads (32,090 out of 25,616,912) were de novo assembly by using commercial software (Geneious V9, Auckland, New Zealand) to produce a single, circular form of complete mitogenome with about an average 261× coverage.

The complete mitogenome of A. nana was 18,480 bp in size (GenBank KY094488) and its overall base composition is 25.0% for A, 13.8% for C, 24.4% for G, and 36.9% for T, and have GC content of 38.2%, showing 99% identities to A. divaricate (GenBank KF448537) after BLAST search against NCBI nr/nt database. The protein coding, rRNA and tRNA genes of A. nana mitogenome were predicted by using DOGMA (Wyman et al. Citation2004), ARWEN (Laslett and Canback Citation2008), MITOS (Bernt et al. Citation2013) tools and manually inspected. The complete mitogenome of A. nana includes unique 13 protein-coding genes (PCGs), three transfer RNA (trnA, trnM, and trnW) genes and two ribosomal RNA (rrnL and rrnS) genes. All PCGs, tRNA, and rRNA genes were encoded on R-strand. It is interesting to note that one big intron (12,116 bp) is inserted in ND5 gene. It is important to note that six PCGs started with ATG codon (ATP6, ATP8, CYTB, ND2, ND3, and ND4L), one with ATT codon (COX1), one with GTG codon (COX2), three with TTG codon (COX3, ND4, and ND5), two with ATA codon (ND1 and ND6), and one with TTA codon (ND5). Nine of 13 PCGs are inferred to terminate with TAA (ATP6, ATP8, COX1, COX2, ND1, ND2, ND4, ND4L, ND5, and ND6) and four PCGs with TAG (CYTB, COX3, ND3, and ND5). Among 13 PCGs, the longest open reading frame length is ND5 gene (1704 bp), whereas the shortest is ATP8 gene (219 bp).

To validate the phylogenetic position of A. nana, we used MEGA6 software (Tamura et al. Citation2013) to construct a maximum likelihood tree with 100 bootstrap replicates and Kimura 2-parameter (K2P) model containing complete mitogenomes of 14 species derived from Acropora genus of Scleractinia. Montipora cactus derived from Montipora genus was used as outgroup for tree rooting. Result shows A. nana is closed to A. divaricata () with a very high identity of 99% (18,468/18,481) and a very small K2P distance of 0.0007. The average K2P distance within Acropora genus is 0.0027, while the average K2P distance between Acropora sp. with Montipora cactus is 0.4723. This result clearly demonstrates the mitogenome sequences between Acropora sp. are very closely each other. In conclusion, the complete mitogenome of the A. nana deduced in this study provides essential and important DNA molecular data for further phylogenetic and evolutionary analysis for stony coral.

Figure 1. Molecular phylogeny of A. nana and related species based on complete mitogenome. The complete mitogenomes is downloaded from GenBank and the phylogenetic tree is constructed by maximum likelihood method with 100 bootstrap replicates. The gene's accession number for tree construction is listed behind the species name.

Figure 1. Molecular phylogeny of A. nana and related species based on complete mitogenome. The complete mitogenomes is downloaded from GenBank and the phylogenetic tree is constructed by maximum likelihood method with 100 bootstrap replicates. The gene's accession number for tree construction is listed behind the species name.

Disclosure statement

The authors report no conflicts of interest. The authors alone are responsible for the content and writing of the paper.

Additional information

Funding

This research was supported by the grants from Xiamen Southern Oceanographic Center (contract no.: 14CZY037HJ11), Guangxi Natural Science Funds for Distinguished Young Scholar (2016GXNSFBA380228), and Public Science and Technology Research Funds Projects of Ocean (contract no.: 201105012).

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