中层带
碳循环
浮游生物
海洋学
生物泵
有机质
环境科学
深海
生态系统
生态学
地质学
远洋带
生物
作者
Flavia Boscolo‐Galazzo,Katherine Crichton,Andy Ridgwell,Elaine Mawbey,Bridget S. Wade,Paul N. Pearson
出处
期刊:Science
[American Association for the Advancement of Science]
日期:2021-03-11
卷期号:371 (6534): 1148-1152
被引量:82
标识
DOI:10.1126/science.abb6643
摘要
Getting more pumped It is thought that the ocean's biological carbon pump, the process that transfers organic matter from the surface to the deep ocean, should be sensitive to climate change because temperature controls photosynthesis and respiration rates. Boscolo-Galazzo et al. show that the efficiency of the biological carbon pump increased over the past 15 million years as the oceans cooled because of a reduction in the rate of the breakdown of sinking organic matter (see the Perspective by Bopp). The resulting redistribution of nutrients at depth could have affected plankton evolution and expanded the mesopelagic “twilight zone” ecosystem. Science , this issue p. 1148 ; see also p. 1099
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