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来自硬珊瑚鹿角杯形珊瑚的多细胞分离物原代细胞培养物中的文石结晶。

Aragonite crystallization in primary cell cultures of multicellular isolates from a hard coral, Pocillopora damicornis.

作者信息

Domart-Coulon I J, Elbert D C, Scully E P, Calimlim P S, Ostrander G K

机构信息

Department of Biology and Division of Comparative Medicine, Johns Hopkins University, 3400 North Charles Street, Baltimore, MD 21218, USA.

出版信息

Proc Natl Acad Sci U S A. 2001 Oct 9;98(21):11885-90. doi: 10.1073/pnas.211439698. Epub 2001 Oct 2.

Abstract

The foundation of marine coral reef ecosystems is calcium carbonate accumulated primarily by the action of hard corals (Coelenterata: Anthozoa: Scleractinia). Colonial hard coral polyps cover the surface of the reef and deposit calcium carbonate as the aragonite polymorph, stabilized into a continuous calcareous skeleton. Scleractinian coral skeleton composition and architecture are well documented; however, the cellular mechanisms of calcification are poorly understood. There is little information on the nature of the coral cell types involved or their cooperation in biocalcification. We report aragonite crystallization in primary cell cultures of a hard coral, Pocillopora damicornis. Cells of apical coral colony fragments were isolated by spontaneous in vitro dissociation. Single dissociated cell types were separated by density in a discontinuous Percoll gradient. Primary cell cultures displayed a transient increase in alkaline phosphatase (ALP) activity, to the level observed in intact corals. In adherent multicellular isolate cultures, enzyme activation was followed by precipitation of aragonite. Modification of the ionic formulation of the medium prolonged maintenance of isolates, delayed ALP activation, and delayed aragonite precipitation. These results demonstrate that in vitro crystallization of aragonite in coral cell cultures is possible, and provides an innovative approach to investigate reef-building coral calcification at the cellular level.

摘要

海洋珊瑚礁生态系统的基础是碳酸钙,主要由硬珊瑚(腔肠动物门:珊瑚虫纲:石珊瑚目)的活动积累而成。群体硬珊瑚水螅体覆盖着珊瑚礁表面,并以文石多晶型形式沉积碳酸钙,这些碳酸钙会稳定形成连续的钙质骨架。石珊瑚的骨骼组成和结构已有充分记载;然而,钙化的细胞机制却知之甚少。关于参与生物钙化的珊瑚细胞类型的性质或它们之间的协作,几乎没有相关信息。我们报道了在硬珊瑚鹿角杯形珊瑚的原代细胞培养物中观察到文石结晶。通过体外自发解离分离出顶端珊瑚群体片段的细胞。通过在不连续的 Percoll 梯度中根据密度分离单个解离的细胞类型。原代细胞培养物中碱性磷酸酶(ALP)活性短暂升高,达到在完整珊瑚中观察到的水平。在贴壁多细胞分离物培养物中,酶激活后会有文石沉淀。改变培养基的离子配方可延长分离物的维持时间,延迟 ALP 激活,并延迟文石沉淀。这些结果表明,在珊瑚细胞培养物中体外结晶文石是可能的,并且为在细胞水平上研究造礁珊瑚钙化提供了一种创新方法。

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