Korall Petra, Pryer Kathleen M
Systematic Biology, Evolutionary Biology Centre, Uppsala University Norbyvägen 18D, SE-752 36, Uppsala, Sweden.
Department of Biology, Duke University Durham, NC, 27708, USA.
J Biogeogr. 2014 Feb;41(2):402-413. doi: 10.1111/jbi.12222.
Scaly tree ferns, Cyatheaceae, are a well-supported group of mostly tree-forming ferns found throughout the tropics, the subtropics and the south-temperate zone. Fossil evidence shows that the lineage originated in the Late Jurassic period. We reconstructed large-scale historical biogeographical patterns of Cyatheaceae and tested the hypothesis that some of the observed distribution patterns are in fact compatible, in time and space, with a vicariance scenario related to the break-up of Gondwana.
Tropics, subtropics and south-temperate areas of the world.
The historical biogeography of Cyatheaceae was analysed in a maximum likelihood framework using Lagrange. The 78 ingroup taxa are representative of the geographical distribution of the entire family. The phylogenies that served as a basis for the analyses were obtained by Bayesian inference analyses of mainly previously published DNA sequence data using MrBayes. Lineage divergence dates were estimated in a Bayesian Markov chain Monte Carlo framework using beast.
Cyatheaceae originated in the Late Jurassic in either South America or Australasia. Following a range expansion, the ancestral distribution of the marginate-scaled clade included both these areas, whereas is reconstructed as having its origin only in Australasia. Within the marginate-scaled clade, reconstructions of early divergences are hampered by the unresolved relationships among the , and lineages. Nevertheless, it is clear that the occurrence of the and lineages in South America may be related to vicariance, whereas transoceanic dispersal needs to be inferred for the range shifts seen in and .
The evolutionary history of Cyatheaceae involves both Gondwanan vicariance scenarios as well as long-distance dispersal events. The number of transoceanic dispersals reconstructed for the family is rather few when compared with other fern lineages. We suggest that a causal relationship between reproductive mode (outcrossing) and dispersal limitations is the most plausible explanation for the pattern observed.
桫椤科是一类得到充分支持的蕨类植物,大多为树形蕨类,分布于热带、亚热带和南温带地区。化石证据表明该谱系起源于晚侏罗世。我们重建了桫椤科的大规模历史生物地理模式,并检验了这样一个假设,即一些观察到的分布模式在时间和空间上实际上与冈瓦纳大陆解体相关的隔离分布情景相契合。
世界热带、亚热带和南温带地区。
在最大似然框架下使用拉格朗日法分析桫椤科的历史生物地理学。78个类群代表了整个科的地理分布。作为分析基础的系统发育树是通过使用MrBayes对主要是先前发表的DNA序列数据进行贝叶斯推断分析获得的。谱系分歧时间是在贝叶斯马尔可夫链蒙特卡罗框架下使用beast估计的。
桫椤科起源于晚侏罗世的南美洲或澳大拉西亚。在一次范围扩张之后,边缘鳞盖亚科的祖先分布包括这两个地区,而被重建为仅起源于澳大拉西亚。在边缘鳞盖亚科内,早期分歧的重建因、和谱系之间未解决的关系而受阻。然而,很明显,和谱系在南美洲的出现可能与隔离分布有关,而对于和中所见的范围转移则需要推断跨洋扩散。
桫椤科的进化历史涉及冈瓦纳大陆的隔离分布情景以及远距离扩散事件。与其他蕨类谱系相比,该科重建的跨洋扩散次数相当少。我们认为,生殖模式(异交)与扩散限制之间的因果关系是对观察到的模式最合理的解释。