Ian Milne Richard
Institute of Molecular Plant Sciences, School of Biological Sciences, The University of Edinburgh, Daniel Rutherford Building, The King's Buildings, Mayfield Road, Edinburgh EH9 3JH, UK.
Ann Bot. 2006 Sep;98(3):465-72. doi: 10.1093/aob/mcl148. Epub 2006 Jul 15.
This botanical briefing examines how molecular systematics has contributed to progress in understanding the history of Tertiary relict genera, i.e. those that that now occur disjunctly in parts of Eurasia and N America, and how progress in understanding Southern Hemisphere biogeography paradoxically makes unravelling Northern Hemisphere biogeography more complex.
Tertiary relict floras comprise genera of warm wet climates that were once circumboreal in distribution but are now confined to E Asia, south-eastern and western N America, and SW Eurasia. The intercontinental disjunctions among these genera have long been believed to result from land connections between Eurasia and N America, across Beringia and the N Atlantic. This view is reassessed in the light of new evidence for long dispersal of propagules across oceans being responsible for many plant disjunctions involving southern continents. The impact of molecular dating, which has been very different in Southern and Northern Hemisphere biogeography, is discussed.
For N America-Eurasia disjunctions involving Tertiary relict floras, land connections remain the more likely cause of disjunctions but data from fossils or infraspecific variation will be required to exclude long-dispersal explanations for disjunctions in any individual genus. Molecular dating of divergence between disjunctly distributed Tertiary relict floras can tell us which palaeoclimatic or palaeogeographic events impacted on them, and how, but only if migration over land and vicariance can be proved and molecular dating is sufficiently accurate.
本植物学简报探讨了分子系统学如何促进了对第三纪残遗属植物历史的理解,即那些现今在欧亚大陆部分地区和北美洲间断分布的植物,以及理解南半球生物地理学的进展如何反常地使北半球生物地理学的阐释变得更加复杂。
第三纪残遗植物区系包括曾经分布于环北极地区、属于温暖湿润气候的属,如今它们仅局限于东亚、北美洲东南部和西部以及欧亚大陆西南部。长期以来,人们一直认为这些属之间的洲际间断分布是由于欧亚大陆和北美洲之间通过白令陆桥和北大西洋的陆地连接造成的。鉴于有新证据表明繁殖体跨洋远距离扩散是导致许多涉及南半球大陆的植物间断分布的原因,本文对这一观点进行了重新评估。文中还讨论了分子定年在南半球和北半球生物地理学中产生的截然不同的影响。
对于涉及第三纪残遗植物区系的北美洲 - 欧亚大陆间断分布情况,陆地连接仍然更有可能是间断分布的原因,但需要化石或种下变异的数据来排除对任何单个属间断分布的远距离扩散解释。间断分布的第三纪残遗植物区系之间分歧的分子定年能够告诉我们哪些古气候或古地理事件对它们产生了影响以及如何产生影响,但前提是必须证明有陆地迁移和隔离分化情况,并且分子定年足够准确。