Abstract
Eastern Boundary Upwelling Systems (EBUS) are highly productive ecosystems. However, being poorly sampled and represented in global models, their role as atmospheric CO(2) sources and sinks remains elusive. In this work, we present a compilation of shipboard measurements over the past two decades from the Benguela Upwelling System (BUS) in the southeast Atlantic Ocean. Here, the warming effect of upwelled waters increases CO(2) partial pressure (pCO(2)) and outgassing in the entire system, but is exceeded in the south through biologically-mediated CO(2) uptake through biologically unused, so-called preformed nutrients supplied from the Southern Ocean. Vice versa, inefficient nutrient utilization leads to preformed nutrient formation, increasing pCO(2) and counteracting human-induced CO(2) invasion in the Southern Ocean. However, preformed nutrient utilization in the BUS compensates with ~22-75 Tg C year(-1) for 20-68% of estimated natural CO(2) outgassing in the Southern Ocean's Atlantic sector (~ 110 Tg C year(-1)), implying the need to better resolve global change impacts on the BUS to understand the ocean's role as future sink for anthropogenic CO(2).