The biological pump in a high CO 2 world

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The effects of changing climate on microzooplankton grazing and community structure: drivers, predictions and knowledge gaps (2013, background): “Along with reduced storage of carbon in the deep ocean by the biological pump (Passow and Carlson, 2012), such decreases could also lead to potentially major changes in the deep-sea benthic fauna as a consequence of changes in food availability (Smith et al., 2008).”
Global biogeochemical impacts of phytoplankton: a trait‐based perspective (2015, background): “At the same time, calcification reduces total alkalinity, reducing the ability of the surface ocean to take up atmospheric CO2 (Passow and Carlson 2012).”
Temperature dependency of metabolic rates in the upper ocean: A positive feedback to global climate change? (2018, background): “This may be associated with an expansion and increased efficiency of the microbial carbon pump with greater amounts of POC transferred to the pool of Recalcitrant Dissolved Organic Carbon (RDOC; Jiao et al., 2010, 2014), in parallel with a reduction of the sequestration flux and hence of the efficie”
Dissolved organic matter (DOM) release by phytoplankton in the contemporary and future ocean (2014, background): “TEP plays an important role in the biogeochemistry of the biological carbon pump (Passow & Carlson, 2012) and consequently there is a need to better define its composition to determine its origin and biogeochemical significance.”