来自奥尔多维纪的glomalean真菌
D Redecker1, R Kodner, L E Graham
1Department of Plant and Microbial Biology, 111 Koshland Hall, University of California, Berkeley, CA 94720, USA. redecker@nature.berkeley.edu
概括
来自奥尔多维纪时期的古老真菌化石表明,与早期陆地植物共存的类似Glomales的真菌. 这些发现支持真菌在植物殖民和早期陆地生态系统中的关键作用.
科学领域:
- 古代生物学的古生物学.
- 植物与真菌的相互作用
- 早期的陆地生态系统
背景情况:
- 奥尔多维纪时期 (48.5-43.4亿年前) 见证了植物对陆地的最初殖民.
- 陆地真菌的进化起源受到争议,分子数据表明它们的起源大约在6亿年前.
研究的目的:
- 研究早期陆地真菌的存在和形态.
- 评估这些真菌在促进植物地球化中的潜在作用.
主要方法:
- 微观检查化石的真菌菌株和子.
- 化石真菌与现代真菌群体的形态比较,特别是状菌根真菌.
主要成果:
- 来自威斯康星州奥尔多维纪的化石 (大约. 460万年前) 具有类似于现代树状菌根真菌 (Glomales,Zygomycetes) 的特征.
- 这些类似于Glomales的真菌存在于陆地植物很可能仅限于植物级植物时.
- 这一发现与分子遗传学估计相一致,主要陆地真菌群体的起源大约在6亿年前.
结论:
- 化石证据表明,在植物地球化的早期阶段,存在着类似Glomales的真菌.
- 这些古老的真菌可能有助于使植物能够殖民陆地.
- 化石记录支持分子钟对陆地真菌多样化的估计.
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