Colder seas may explain a quarter of ice-age CO2 drop

A paper in Nature Communications proposes that plankton respiration slows more than photosynthesis in colder water. The authors estimate this effect explains about a quarter of the fall in carbon dioxide during the last ice age.
The authors argue that when respiration slows more than photosynthesis, more carbon sinks to the deep ocean. This offers a physical explanation for part of a long-debated question in climate science. The paper is peer-reviewed. The quarter figure comes from the authors' modelling, and other researchers have not independently checked it. It is also an estimate of past climate, not a measurement.