Department of Botany, University of British Columbia, Vancouver, British Columbia V6T 1Z4, Canada; email:
Department of Ecology and Evolutionary Biology, University of Michigan, Ann Arbor, Michigan 48109; email:
Annu Rev Microbiol. 2017 Sep 8;71:41-60. doi: 10.1146/annurev-micro-030117-020324. Epub 2017 May 19.
As decomposers or plant pathogens, fungi deploy invasive growth and powerful carbohydrate active enzymes to reduce multicellular plant tissues to humus and simple sugars. Fungi are perhaps also the most important mutualistic symbionts in modern ecosystems, transporting poorly soluble mineral nutrients to plants and thus enhancing the growth of vegetation. However, at their origin over a billion years ago, fungi, like plants and animals, were unicellular marine microbes. Like the other multicellular kingdoms, Fungi evolved increased size, complexity, and metabolic functioning. Interactions of fungi with plants changed terrestrial ecology and geology and modified the Earth's atmosphere. In this review, we discuss the diversification and ecological roles of the fungi over their first 600 million years, from their origin through their colonization of land, drawing on phylogenomic evidence for their relationships and metabolic capabilities and on molecular dating, fossils, and modeling of Earth's paleoclimate.
作为分解者或植物病原体,真菌通过入侵性生长和强大的碳水化合物活性酶将多细胞植物组织分解为腐殖质和简单糖。真菌也许也是现代生态系统中最重要的互利共生体,将难溶性矿物养分输送给植物,从而促进植被生长。然而,在 10 多亿年前,真菌与植物和动物一样,都是单细胞海洋微生物。与其他多细胞生物王国一样,真菌进化出了更大的体型、更复杂的结构和更多的代谢功能。真菌与植物的相互作用改变了陆地生态和地质学,并改变了地球的大气。在这篇综述中,我们讨论了真菌在其最初的 6 亿年中的多样化和生态作用,从它们的起源到它们对陆地的殖民,利用系统基因组学证据来研究它们的关系和代谢能力,以及利用分子定年、化石和地球古气候模型。