ABSTRACT. We sequenced the complete mitochondrial genome of Phalera flavescens. The mitogenome is 15,659 bp in length, including 13 protein-coding genes (atp6, atp8, cox1-3, nad1-6, nad4L, cob), two ribosomal RNAs (rrnS and rrnL), 22 transfer RNAs and an AT-rich region, a putative control region (D-loop). Gene order and orientation were found to be identical to those of other completely sequenced lepidopteran mitogenomes. All 13 protein-coding genes start with the common codon ATN, except for the cox1 gene, which uses CGA as the initial codon. Nine of the 13 protein-coding genes stop with codon TAA, while the cox1, cox2, nad5, and nad4 genes stop with the single nucleotide T. All tRNA genes can be folded into canonical cloverleaf secondary structure, except for trnS1, which loses the ''DHU'' arm. Six overlapping sequences totaling 20 bp (1-8 bp for each sequence) and 16 intergenic spacer sequences, totaling 276 bp (1-58 bp for each sequence) are scattered throughout the genome; the largest intergenic spacer is located between the trnQ and nad2 genes. A microsatellitelike structure (AT) 6 ACC(AT) 6 and 16-bp poly-T elements preceded by the ATTTA motif are present in the D-loop region. Additionally, unexpectedly, an extra 190-bp insertion, with unknown function, was found in the small subunit rRNA gene (rrnS); this gene is the longest known (1020 bp) among all of the Lepidoptera.
Blue holes are unique geomorphological features with steep biogeochemical gradients and distinctive microbial communities. Carbon cycling in blue holes, however, remains poorly understood. Here we describe potential mechanisms of dissolved carbon cycling in the world's deepest blue hole, the Yongle Blue Hole (YBH), which was recently discovered in the South China Sea. In the YBH, we found some of the lowest concentrations (e.g., 22 μM) and oldest ages (e.g., 6,810 years before present) of dissolved organic carbon, as well as the highest concentrations (e.g., 3,090 μM) and the oldest ages (e.g., 8,270 years before present) of dissolved inorganic carbon observed in oceanic waters. Sharp gradients of dissolved oxygen, H2S, and CH4 and changes in bacterially mediated sulfur cycling with depth indicated that sulfur‐ and/or methane‐based metabolisms are closely linked to carbon cycling in the YBH. Our results showed that the YBH is a unique and easily accessible natural laboratory for examining carbon cycling in anoxic systems, which has potential for understanding carbon dynamics in both paleo and modern oceans—particularly in the context of global change.
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