Department Biologie, Systematische Botanik und Mykologie, Ludwig-Maximilians-Universität München, München, Germany.
PLoS One. 2013;8(1):e54038. doi: 10.1371/journal.pone.0054038. Epub 2013 Jan 8.
Biomineralization in calcareous dinophytes (Thoracosphaeracaea, Peridiniales) takes place in coccoid cells and is presently poorly understood. Vacuolar crystal-like particles as well as collection sites within the prospective calcareous shell may play a crucial role during this process at the ultrastructural level. Using transmission electron microscopy, we investigated the ultrastructure of coccoid cells at an early developmental stage in fourteen calcareous dinophyte strains (corresponding to at least ten species of Calciodinellum, Calcigonellum, Leonella, Pernambugia, Scrippsiella, and Thoracosphaera). The shell of the coccoid cells consisted either of one (Leonella, Thoracosphaera) or two matrices (Scrippsiella and its relatives) of unknown element composition, whereas calcite is deposited in the only or the outer layer, respectively. We observed crystal-like particles in cytoplasmic vacuoles in cells of nine of the strains investigated and assume that they are widespread among calcareous dinophytes. However, similar structures are also found outside the Thoracosphaeraceae, and we postulate an evolutionarily old physiological pathway (possibly involved in detoxification) that later was specialized for calcification. We aim to contribute to a deeper knowledge of the biomineralization process in calcareous dinophytes.
钙质甲藻(旋沟藻目,甲藻纲)中的生物矿化作用发生在球形细胞中,目前对此知之甚少。液泡中的结晶状颗粒以及潜在的钙质壳内的收集点可能在超微结构水平上在此过程中发挥关键作用。使用透射电子显微镜,我们研究了 14 株钙质甲藻菌株(至少对应 10 种 Calcidi-nellum、Calcigonellum、Leonella、Pernambugia、Scrippsiella 和 Thoracosphaera)早期发育阶段球形细胞的超微结构。球形细胞的壳由未知元素组成的一层(Leonella、Thoracosphaera)或两层基质(Scrippsiella 及其相关种)组成,而方解石分别沉积在唯一层或外层。我们观察到在 9 株被研究的菌株的细胞质液泡中存在结晶状颗粒,我们假设它们在钙质甲藻中广泛存在。然而,类似的结构也存在于旋沟藻科之外,我们推测这是一种古老的进化生理途径(可能参与解毒),后来专门用于钙化。我们旨在为钙质甲藻生物矿化过程提供更深入的了解。