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火适应的冈瓦纳被子植物区系在白垩纪进化而来。

Fire-adapted Gondwanan Angiosperm floras evolved in the Cretaceous.

机构信息

Department of Environment and Agriculture, Curtin University, PO Box U1987, Perth, WA 6845, Australia.

出版信息

BMC Evol Biol. 2012 Nov 22;12:223. doi: 10.1186/1471-2148-12-223.

Abstract

BACKGROUND

Fires have been widespread over the last 250 million years, peaking 60-125 million years ago (Ma), and might therefore have played a key role in the evolution of Angiosperms. Yet it is commonly believed that fireprone communities existed only after the global climate became more arid and seasonal 15 Ma. Recent molecular-based studies point to much earlier origins of fireprone Angiosperm floras in Australia and South Africa (to 60 Ma, Paleocene) but even these were constrained by the ages of the clades examined.

RESULTS

Using a molecular-dated phylogeny for the great Gondwanan family Proteaceae, with a 113-million-year evolutionary history, we show that the ancestors of many of its characteristic sclerophyll genera, such as Protea, Conospermum, Leucadendron, Petrophile, Adenanthos and Leucospermum (all subfamily Proteoideae), occurred in fireprone habitats from 88 Ma (83-94, 95% HPD, Mid-Upper Cretaceous). This coincided with the highest atmospheric oxygen (combustibility) levels experienced over the past 150 million years. Migration from non-fireprone (essentially rainforest-climate-type) environments was accompanied by the evolution of highly speciose clades with a range of seed storage traits and fire-cued seed release or germination mechanisms that was diagnostic for each clade by 71 Ma, though the ant-dispersed lineage (as a soil seed-storage subclade) was delayed until 45 Ma.

CONCLUSIONS

Focusing on the widespread 113-million-year-old family Proteaceae, fireproneness among Gondwanan Angiosperm floras can now be traced back almost 90 million years into the fiery Cretaceous. The associated evolution of on-plant (serotiny) and soil seed storage, and later ant dispersal, affirms them as ancient adaptations to fire among flowering plants.

摘要

背景

在过去的 2.5 亿年中,火灾非常普遍,在 60-125 百万年前(Ma)达到顶峰,因此可能在被子植物的进化中发挥了关键作用。然而,人们普遍认为,在 15 Ma 后,全球气候变得更加干旱和季节性时,易燃社区才存在。最近基于分子的研究表明,在澳大利亚和南非,易燃的被子植物植物群的起源要早得多(至 60 Ma,古近纪),但即使是这些起源也受到所研究的进化枝的年龄限制。

结果

使用分子定年的大冈瓦纳家族 Proteaceae 系统发育树,其进化历史为 1.13 亿年,我们表明,许多特征性硬叶属的祖先,如 Protea、Conospermum、Leucadendron、Petrophile、Adenanthos 和 Leucospermum(所有亚科 Proteoideae),出现在 88 Ma(83-94,95%HPD,中-上白垩纪)的易燃生境中。这与过去 1.5 亿年中经历的最高大气氧(可燃性)水平相吻合。从非易燃(本质上是雨林气候类型)环境的迁移伴随着高度多样化的进化枝的出现,这些进化枝具有各种种子储存特征和火引发的种子释放或萌发机制,到 71 Ma 时,每个进化枝都具有可诊断性,尽管蚂蚁传播的谱系(作为土壤种子储存亚谱系)直到 45 Ma 才延迟。

结论

专注于广泛存在的 1.13 亿年的 Proteaceae 家族,冈瓦纳被子植物植物群的易燃性现在可以追溯到近 9000 万年前的火热白垩纪。与植物(结球)和土壤种子储存相关的进化,以及后来蚂蚁的传播,证实了它们是开花植物中古老的适应火灾的适应。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/a1e5/3534566/c0765befb1a0/1471-2148-12-223-1.jpg

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