Pelagic carbonate production is an important element of the global carbon cycle. Through biomineralization of either calcite or aragonite, marine plankton binds large amounts of dissolved inorganic carbon in their shells, which are then exported from the productive zone (Milliman, 1993). A large part of the aragonite flux, which consists exclusively of pteropods (Buitenhuis et al., 2019;Fabry, 1989;Singh & Conan, 2008), is dissolved before being buried in the sediment (Berner & Honjo, 1981). However, calcite (especially low-magnesium calcite in planktonic foraminifera shells) is less prone to dissolution (Keir, 1980), making the burial of biogenic calcite the main mechanism to transfer carbon from the rapidly cycling ocean-atmosphere-biosphere to the slow geological reservoir (Archer, 1996;Catubig et al., 1998). In addition, biogenic carbonate production has an opposing fast effect on the carbon cycle, as well as the marine biological carbon pump. By consuming alkalinity, it induces degassing of carbon dioxide and thus acts as a "counter pump" in the process of biological carbon sequestration in the ocean (Frankignoulle & Canon, 1994). Planktonic foraminifera shells are a key component of marine biogenic calcite production and flux. Upon death of these organisms, their shells begin to settle through the water column, and the resulting export flux is estimated to constitute up to half of the global calcite flux (Schiebel, 2002;Schiebel et al., 2007). The rest of the pelagic calcite flux is dominated by coccoliths (Baumann et al., 2004;Milliman, 1993). However, in order to quantify the pelagic calcite budget, planktonic foraminifera cannot be ignored. The planktonic foraminifera shell flux is a variable in both space and time (Jonkers & Kucera, 2015;Žarić et al., 2005), yet the factors controlling the shell flux variability are not completely constrained and understood. Furthermore, the subject concerning how shell flux variability relates to mass flux variability has not been explicitly studied before. In theory, variability in the planktonic foraminifera calcite flux could arise from changes in the shell flux and thus reflect population growth and/or changes in the shell mass, which consequently reflect individual