CNRS UMR7144/UPMC, EPEP team, Station Biologique de Roscoff, Roscoff, 29682, France.
Marine Biological Association of the United Kingdom, Citadel Hill, Plymouth, Devon, PL1 2PB, UK.
J Phycol. 2014 Feb;50(1):140-8. doi: 10.1111/jpy.12147. Epub 2014 Jan 13.
Emiliania huxleyi and Gephyrocapsa oceanica are abundant coccolithophore morpho-species that play key roles in ocean carbon cycling due to their importance as both primary producers and cal-cifiers. Global change processes such as ocean acidification impact these key calcifying species. The physiology of E. huxleyi, a developing model species, has been widely studied, but its genetic delineation from G. oceanica remains unclear due to a lack of resolution in classical genetic markers. Using nuclear (18S rDNA and 28S rDNA), mitochondrial (cox1, cox2, cox3, rpl16, and dam), and plastidial (16S rDNA, rbcL, tufA, and petA) DNA markers from 99 E. huxleyi and 44 G. oceanica strains, we conducted a multigene/multistrain survey to compare the suitability of different markers for resolving phylogenetic patterns within and between these two morpho-species. The nuclear genes tested did not provide sufficient resolution to discriminate between the two morpho-species that diverged only 291Kya. Typical patterns of incomplete lineage sorting were generated in phylogenetic analyses using plastidial genes. In contrast, full morpho-species delineation was achieved with mitochondrial markers and common intra-morpho-species phylogenetic patterns were observed despite differing rates of DNA substitution. Mitochondrial genes are thus promising barcodes for distinguishing these coccolithophore morpho-species, in particular in the context of environmental monitoring.
赫氏颗石藻和厚壁藻是丰富的颗石藻形态物种,由于它们既是初级生产者又是钙化者,因此在海洋碳循环中起着关键作用。全球变化过程,如海洋酸化,会影响这些关键钙化物种。作为一种正在发展的模式物种,赫氏颗石藻的生理学已经得到了广泛的研究,但由于经典遗传标记分辨率不够,它与厚壁藻的遗传划分仍然不清楚。我们使用了来自 99 株赫氏颗石藻和 44 株厚壁藻的核(18S rDNA 和 28S rDNA)、线粒体(cox1、cox2、cox3、rpl16 和 dam)和质体(16S rDNA、rbcL、tufA 和 petA)DNA 标记,对这两个形态物种进行了多基因/多菌株调查,以比较不同标记在这些两个形态物种内部和之间分辨系统发育模式的适用性。测试的核基因没有提供足够的分辨率来区分这两个形态物种,它们在 291Kya 才开始分化。在使用质体基因进行的系统发育分析中产生了典型的不完全谱系分选模式。相比之下,线粒体标记可以实现完整的形态物种划分,并且尽管存在不同的 DNA 替换率,但仍观察到常见的形态内种内系统发育模式。因此,线粒体基因是区分这些颗石藻形态物种的有前途的条形码,特别是在环境监测方面。