Chen Feng, Xue Ge, Wang Yeke, Zhang Hucai, Clift Peter D, Xing Yaowu, He Jun, Albert James S, Chen Jun, Xie Ping
Donghu Experimental Station of Lake Ecosystems, State Key Laboratory of Freshwater Ecology and Biotechnology, Institute of Hydrobiology, Chinese Academy of Sciences, Wuhan 430072, China.
University of Chinese Academy of Sciences, Beijing 100049, China.
Innovation (Camb). 2023 Mar 21;4(3):100417. doi: 10.1016/j.xinn.2023.100417. eCollection 2023 May 15.
Documenting the origins of megadiverse (sub)tropical aquatic ecosystems is an important goal for studies of evolution and ecology. Nonetheless, the geological and ecological establishment of the modern Yangtze River remains poorly understood. Here, we reconstruct the geographic and ecological history of an endemic clade of East Asian fishes based on the mitochondrial phylogenomics analysis of Cyprinidae using 15 fossil calibrations. We estimate an ancestral condition of benthic spawning with demersal or adhesive eggs in southern East Asia before ∼23 Ma and a derived condition of riverine spawning with semibuoyant eggs in the Yangtze by ∼18 Ma. These results imply the formation of Yangtze riverine ecosystems around the Oligocene-Miocene boundary in response to plateau uplift and monsoon strengthening. Some of these cyprinids reverted to benthic spawning with adhesive eggs by ∼15 Ma, a time of rising to peak net diversification rates, indicating the formation of potamo-lacustrine ecosystems by the mid-Miocene during a strong East Asian summer monsoon. Our study provides increased spatiotemporal resolution for the co-evolutionary histories of the Yangtze River and its biodiversity and highlights biological evidence concerning the geomorphological dynamics of the Yangtze River.
记录超级多样化的(亚热带)水生生态系统的起源是进化和生态学研究的一个重要目标。尽管如此,现代长江的地质和生态形成过程仍知之甚少。在此,我们基于鲤科鱼类的线粒体系统基因组学分析,并使用15个化石校准点,重建了东亚鱼类一个特有分支的地理和生态历史。我们估计,在约2300万年前之前,东亚南部存在着底栖产卵且卵为沉性或粘性的原始状态,而到约1800万年前,长江出现了产半浮性卵的河流产卵衍生状态。这些结果表明,在渐新世 - 中新世边界附近,随着高原隆升和季风增强,长江河流生态系统形成。其中一些鲤科鱼类在约1500万年前又恢复到底栖产卵且卵为粘性的状态,这是净多样化率上升至峰值的时期,表明在东亚夏季风强盛的中新世中期形成了河 - 湖生态系统。我们的研究提高了长江及其生物多样性共同进化历史的时空分辨率,并突出了有关长江地貌动态的生物学证据。