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颗石藻中的假隐性物种形成。

Pseudo-cryptic speciation in coccolithophores.

作者信息

Saez Alberto G, Probert Ian, Geisen Markus, Quinn Patrick, Young Jeremy R, Medlin Linda K

机构信息

Alfred Wegener Institute for Polar and Marine Biology, Department of Biological Oceanography, Am Handelshafen 12, D-27570 Bremerhaven, Germany.

出版信息

Proc Natl Acad Sci U S A. 2003 Jun 10;100(12):7163-8. doi: 10.1073/pnas.1132069100. Epub 2003 May 20.

Abstract

Coccolithophores are a group of calcifying unicellular algae that constitute a major fraction of oceanic primary productivity, play an important role in the global carbon cycle, and are key biostratigraphic marker fossils. Their taxonomy is primarily based on the morphology of the minute calcite plates, or coccoliths, covering the cell. These are diverse and include widespread fine scale variation, of which the biological/taxonomic significance is unknown. Do they represent phenotypic plasticity, genetic polymorphisms, or species-specific characters? Our research on five commonly occurring coccolithophores supports the hypothesis that such variation represents pseudocryptic speciation events, occurring between 0.3 and 12.9 million years ago from a molecular clock estimation. This finding suggests strong stabilizing selection acting on coccolithophorid phenotypes. Our results also provide strong support for the use of fine scale morphological characters of coccoliths in the fossil record to improve biostratigraphic resolution and paleoceanographic data retrieval.

摘要

颗石藻是一类钙化单细胞藻类,它们构成了海洋初级生产力的主要部分,在全球碳循环中发挥着重要作用,并且是关键的生物地层标志化石。它们的分类主要基于覆盖细胞的微小方解石板(即颗石)的形态。这些形态多种多样,包括广泛存在的细微尺度变化,但其生物学/分类学意义尚不清楚。它们代表表型可塑性、遗传多态性还是物种特异性特征?我们对五种常见颗石藻的研究支持了这样一种假说,即这种变化代表了在0.3至1290万年前从分子钟估计得出的假隐性物种形成事件。这一发现表明对颗石藻表型有强大的稳定选择作用。我们的结果也为在化石记录中使用颗石的细微形态特征以提高生物地层分辨率和古海洋学数据检索提供了有力支持。

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