Program in Atmospheres, Oceans, and Climate, Massachusetts Institute of Technology, Cambridge, MA, 02139, USA.
Department of Organismic and Evolutionary Biology, Harvard University, Cambridge, MA, 02138, USA.
Nat Commun. 2020 Nov 6;11(1):5636. doi: 10.1038/s41467-020-19462-w.
Marine ecosystem models predict a decline in fish production with anthropogenic ocean warming, but how fish production equilibrates to warming on longer timescales is unclear. We report a positive nonlinear correlation between ocean temperature and pelagic fish production during the extreme global warmth of the Early Paleogene Period (62-46 million years ago [Ma]). Using data-constrained modeling, we find that temperature-driven increases in trophic transfer efficiency (the fraction of production passed up trophic levels) and primary production can account for the observed increase in fish production, while changes in predator-prey interactions cannot. These data provide new insight into upper-trophic-level processes constrained from the geological record, suggesting that long-term warming may support more productive food webs in subtropical pelagic ecosystems.
海洋生态系统模型预测,随着人为造成的海洋变暖,鱼类产量将会下降,但在更长的时间尺度上,鱼类产量如何与变暖达到平衡还不清楚。我们报告了早古生代(6200 万至 4600 万年前)这一全球极端暖期期间海洋温度与浮游鱼类产量之间呈正非线性相关关系。利用数据约束建模,我们发现,营养传递效率(生产过程中传递到下一营养级的部分)和初级生产力的温度驱动增加可以解释观察到的鱼类产量增加,而捕食者-猎物相互作用的变化则不能。这些数据为从地质记录中得出的上层营养级过程提供了新的见解,表明长期变暖可能支持亚热带浮游生态系统中更具生产力的食物网。