Grandcolas Philippe
Institut de Systématique, Evolution, Biodiversité, ISYEB - UMR 7205 CNRS MNHN UPMC EPHE, Muséum national d'Histoire naturelle, Sorbonne Universités, CP 50, 45 rue Buffon, 75005, Paris, France.
Cladistics. 2017 Oct;33(5):481-487. doi: 10.1111/cla.12176. Epub 2016 Nov 1.
The biogeographical paradigm of New Caledonia has recently changed. Although this island is now considered by many as oceanic, its study is still often impeded by some old misconceptions concerning either regional geology or phylogenetic analysis of evolution and biogeography. I discuss ten points that I feel are especially detrimental, to help focus on the real debate and the real questions: (1) its geological history cannot be understood from the basement only; (2) the island submergence was not due simply to sea-level variation; (3) Zealandia/Tasmantis is not a lost continent; (4) short-distance dispersal is not equivalent to permanence on land; (5) long-distance dispersal is not the sole event opposing vicariance, but short-distance dispersal as well; (6) the occurrence of relicts does not prove biota permanence; (7) a major fault system was not observed in New Caledonia; (8) terranes are not rafts; (9) forest climatic refuges do not necessarily equate to centres of endemism or centres of diversity; and (10) New Caledonia is not only a sink but also a source. Study of New Caledonia will need to focus on old and non-relict clades and there is a need to improve the local fossil record.
新喀里多尼亚的生物地理范式最近发生了变化。尽管现在许多人认为这个岛屿是海洋性的,但其研究仍然常常受到一些关于区域地质或进化与生物地理学系统发育分析的旧有误解的阻碍。我讨论了十个我认为特别有害的观点,以帮助聚焦于真正的争论和问题:(1)仅从基底无法理解其地质历史;(2)该岛屿的沉没并非仅仅由于海平面变化;(3)西兰蒂亚/塔斯曼蒂斯不是一个失落的大陆;(4)短距离扩散并不等同于在陆地上的永久性;(5)长距离扩散不是与隔离分化相对立的唯一事件,短距离扩散也是;(6)残遗种的存在并不能证明生物区系的永久性;(7)在新喀里多尼亚未观察到主要的断层系统;(8)地体不是漂浮物;(9)森林气候避难所不一定等同于特有种中心或多样性中心;(10)新喀里多尼亚不仅是一个汇,也是一个源。对新喀里多尼亚的研究需要聚焦于古老的和非残遗的分支,并且有必要改善当地的化石记录。