Gibbs Samantha J, Bown Paul R, Ward Ben A, Alvarez Sarah A, Kim Hojung, Archontikis Odysseas A, Sauterey Boris, Poulton Alex J, Wilson Jamie, Ridgwell Andy
Ocean and Earth Science, National Oceanography Centre, Southampton, University of Southampton, Southampton SO14 3ZH, UK.
Department of Earth Sciences, University College London, Gower Street, London WC1E 6BT, UK.
Sci Adv. 2020 Oct 30;6(44). doi: 10.1126/sciadv.abc9123. Print 2020 Oct.
The end-Cretaceous bolide impact triggered the devastation of marine ecosystems. However, the specific kill mechanism(s) are still debated, and how primary production subsequently recovered remains elusive. We used marine plankton microfossils and eco-evolutionary modeling to determine strategies for survival and recovery, finding that widespread phagotrophy (prey ingestion) was fundamental to plankton surviving the impact and also for the subsequent reestablishment of primary production. Ecological selectivity points to extreme post-impact light inhibition as the principal kill mechanism, with the marine food chain temporarily reset to a bacteria-dominated state. Subsequently, in a sunlit ocean inhabited by only rare survivor grazers but abundant small prey, it was mixotrophic nutrition (autotrophy and heterotrophy) and increasing cell sizes that enabled the eventual reestablishment of marine food webs some 2 million years later.
白垩纪末期的小行星撞击引发了海洋生态系统的毁灭。然而,具体的致死机制仍存在争议,而且初级生产随后如何恢复仍然不明。我们利用海洋浮游生物微化石和生态进化模型来确定生存和恢复策略,发现广泛的吞噬作用(捕食猎物)对于浮游生物在撞击中存活以及随后初级生产的重新建立至关重要。生态选择性表明撞击后极端的光抑制是主要的致死机制,海洋食物链暂时重置为以细菌为主导的状态。随后,在一个只有罕见的幸存食草动物但有丰富小型猎物的阳光照射的海洋中,是混合营养(自养和异养)以及细胞大小的增加使得大约200万年后海洋食物网最终得以重新建立。