Institut Teknologi Bandung, School of Life Sciences and Technology, Jalan Ganesha 10, Bandung 40132, Indonesia.
UMR 5554 ISEM (IRD, UM, CNRS, EPHE), Université de Montpellier, Place Eugène Bataillon, 34095 Montpellier cedex 05, France.
Syst Biol. 2021 Aug 11;70(5):940-960. doi: 10.1093/sysbio/syab006.
Pleistocene climatic fluctuations (PCF) are frequently highlighted as important evolutionary engines that triggered cycles of biome expansion and contraction. Although there is ample evidence of the impact of PCF on biodiversity of continental biomes, the consequences in insular systems depend on the geology of the islands and the ecology of the taxa inhabiting them. The idiosyncratic aspects of insular systems are exemplified by the islands of the Sunda Shelf in Southeast Asia (Sundaland), where PCF-induced eustatic fluctuations had complex interactions with the geology of the region, resulting in high species diversity and endemism. Emergent land in Southeast Asia varied drastically with sea-level fluctuations during the Pleistocene. Climate-induced fluctuations in sea level caused temporary connections between insular and continental biodiversity hotspots in Southeast Asia. These exposed lands likely had freshwater drainage systems that extended between modern islands: the Paleoriver Hypothesis. Built upon the assumption that aquatic organisms are among the most suitable models to trace ancient river boundaries and fluctuations of landmass coverage, the present study aims to examine the evolutionary consequences of PCF on the dispersal of freshwater biodiversity in Southeast Asia. Time-calibrated phylogenies of DNA-delimited species were inferred for six species-rich freshwater fish genera in Southeast Asia (Clarias, Channa, Glyptothorax, Hemirhamphodon, Dermogenys, Nomorhamphus). The results highlight rampant cryptic diversity and the temporal localization of most speciation events during the Pleistocene, with 88% of speciation events occurring during this period. Diversification analyses indicate that sea-level-dependent diversification models poorly account for species proliferation patterns for all clades excepting Channa. Ancestral area estimations point to Borneo as the most likely origin for most lineages, with two waves of dispersal to Sumatra and Java during the last 5 myr. Speciation events are more frequently associated with boundaries of the paleoriver watersheds, with 60%, than islands boundaries, with 40%. In total, one-third of speciation events are inferred to have occurred within paleorivers on a single island, suggesting that habitat heterogeneity and factors other than allopatry between islands substantially affected diversification of Sundaland fishes. Our results suggest that species proliferation in Sundaland is not wholly reliant on Pleistocene sea-level fluctuations isolating populations on different islands. [Dispersal; diversification; eustatic fluctuations; freshwater fishes; insular systems; Milankovitch cycles; paleoenvironments; vicariance.].
更新世气候波动(PCF)常被认为是触发生物群落扩张和收缩循环的重要进化引擎。尽管有大量证据表明 PCF 对大陆生物群落的生物多样性有影响,但在岛屿系统中的后果取决于岛屿的地质和栖息在岛屿上的分类群的生态。岛屿系统的特殊性体现在东南亚巽他陆架(巽他兰)的岛屿上,在那里,PCF 引起的海平面波动与该地区的地质有复杂的相互作用,导致了高物种多样性和特有性。东南亚新兴陆地在更新世海平面波动中变化剧烈。气候引起的海平面波动导致了东南亚岛屿和大陆生物多样性热点之间的暂时连接。这些暴露的陆地可能有淡水排水系统,这些系统在现代岛屿之间延伸:古河流假说。本研究基于这样的假设,即水生生物是最适合追踪古代河流边界和陆地覆盖范围波动的模型之一,旨在研究 PCF 对东南亚淡水生物多样性扩散的进化后果。对东南亚六种鱼类属(Clarias、Channa、Glyptothorax、Hemirhamphodon、Dermogenys、Nomorhamphus)的 DNA 界定物种进行了时间校准的系统发育分析。结果突出了隐种多样性的猖獗和大多数物种形成事件在更新世的时间定位,88%的物种形成事件发生在这个时期。多样化分析表明,除了 Channa 之外,海平面依赖的多样化模型对所有进化枝的物种增殖模式都解释得很差。祖先区估计表明,婆罗洲最有可能是大多数谱系的起源地,在过去 500 万年里有两次向苏门答腊和爪哇的扩散。物种形成事件与古流域分水岭的边界更频繁地相关,占 60%,而与岛屿边界相关的占 40%。总的来说,三分之一的物种形成事件被推断发生在单个岛屿的古河流内,这表明栖息地异质性和岛屿之间的非地理隔离以外的其他因素极大地影响了巽他兰鱼类的多样化。我们的结果表明,巽他兰的物种增殖不完全依赖于更新世海平面波动将种群隔离在不同的岛屿上。[扩散;多样化;海平面波动;淡水鱼类;岛屿系统;米兰科维奇循环;古环境;隔离分化。]