Micropaleontology-retrospective diatom is an important biological indicator of geologic environment change which has been widely used in the Meso-Cenozoic sediment studies to determine the evolution of ocean environment.
微体古生物——硅藻是追溯地质环境变化过程的重要标志性生物,被广泛应用于中新生代沉积层的研究,以判别环境的演化。
参考来源 - 福建中部近岸海域晚全新世沉积硅藻研究·2,447,543篇论文数据,部分数据来源于NoteExpress
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