中新世-上新世澳大利亚内陆干旱化期间樟科植物的多样化

IF 4.3 3区 材料科学 Q1 ENGINEERING, ELECTRICAL & ELECTRONIC
Philipp Hühn , John McDonald , Kelly A. Shepherd , Gudrun Kadereit
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引用次数: 0

摘要

澳大利亚樟科植物代表了一个单系,其多样性包括 12 个属的约 150 种植物,分布在澳大利亚的干旱地区。150 个属,分布在澳大利亚干旱地区的大部分地区。追踪这一祖先耐盐和耐旱品系的起源和扩散为了解澳大利亚干旱栖息地的进化历史和系统发育组装的时间提供了更多证据。利用定制的 RADseq 方法,生成了代表所有 12 个属的 104 种澳大利亚樟科植物的序列数据,并将其纳入系统发育和年代分析。此外,还记录了物种和支系的栖息地类型和偏好。正如所猜测的那样,用于划分当前澳大利亚樟属的特征并不支持单系群,因为系统发生学分析得出了 17 个统计上支持的支系,这些支系跨越了一个大的 Maireana 等级和 Sclerolaena 的冠状辐射。澳大利亚樟科植物的多样化显然与澳大利亚干旱地区的地貌变化和新出现的栖息地类型有关,因为其祖先很可能是在中新世从欧亚大陆的温带半干旱地区向干旱地区迁移的。迁移很可能是多向的,并伴随着由西向东的干旱化过程。冠类的多样化在上新世最为强烈,这可能是由于河流沙漠栖息地由西向东扩张,以及随后新开发的干旱栖息地的扩张和殖民化所推动的。快速的分布范围扩展、栖息地的快速饱和以及干旱栖息地的周期性扩展、收缩和替换,可能造成了较早分化的Maireana级支系与持续分化的Sclerolaena支系相比物种稀少。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Diversification of Camphorosmeae (Amaranthaceae s.l.) during the Miocene-Pliocene aridification of inland Australia

The Australian Camphorosmeae represent a monophyletic lineage that diversified to include ca. 150 spp. across 12 genera, and populate large parts of arid Australia. Tracking the origin and spread of this ancestrally salt and drought tolerant lineage provides additional evidence about the timing of the evolutionary history and phylogenetic assembly of arid habitats in Australia. Using a customized RADseq approach, sequence data for 104 species of the Australian Camphorosmeae representing all 12 genera were generated and included in phylogenetic and dating analyses. Furthermore, habitat type occurrences and preferences of species and clades were recorded. As suspected, the characters used to delimit current Australian Camphorosmeae genera do not support monophyletic groups, as phylogenetic analyses yielded 17 statistically supported clades across a large Maireana grade and crown radiation of Sclerolaena. The diversification of Australian Camphorosmeae is clearly linked to landscape changes and emerging new habitat types in arid Australia since the ancestral element likely arrived from temperate semi-arid to arid parts of continental Eurasia in the Middle Miocene. Migration was likely multidirectional and followed a west-to-east aridification. Crown group diversification was strongest during the Pliocene and likely promoted by the west-to-east expansion of Riverine Desert habitats and subsequent expansion and colonization of newly developing arid habitats. Rapid range expansion, fast habitat saturation, as well as periodic expansion, contraction and replacement of arid habitats, may have caused the rather species-poor clades of the earlier-divergent Maireana grade, compared to the continuously diversifying Sclerolaena clade.

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来源期刊
CiteScore
7.20
自引率
4.30%
发文量
567
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