Oceanic primary production, primarily through oxygenic photosynthesis, is the main input of energy into marine ecosystems (Karl, 2014), is the first step of the ocean's food web (Ryther, 1969), and produces approximately half of the oxygen (O 2 ) on the planet (Field et al., 1998). In addition, primary production in the ocean fuels the marine biological carbon (C) pump that in turn affects climate (Volk & Hoffert, 1985). Planktonic primary production and respiration can be quantified in terms of energy or material flows (Williams, 1993), but the latter is operationally easier to measure. Therefore, gross primary production (GPP) is commonly defined as the total amount of inorganic C that is reduced to organic C by photosynthetic organisms (Williams, 1993). A large fraction of this C is oxidized back to carbon dioxide (CO 2 ) through community respiration (R) by both autotrophic and heterotrophic organisms. The difference between GPP and R, net community production (NCP), represents the amount of biologically produced organic C that can be potentially transported out of the euphotic zone into the ocean's interior via the biological C pump, mainly through sinking particles, vertically migrating zooplankton (Longhurst & Harrison, 1988), and the export of dissolved organic C (Carlson et al., 1994). Through these processes the biological C pump effectively sequesters CO 2 from the atmosphere for extended periods of time (Volk & Hoffert, 1985) and provides the main C source that fuels mesopelagic and abyssopelagic organisms (Karl & Church, 2017).The oligotrophic subtropical gyres occupy ∼40% of the world's surface (Karl & Church, 2014) and, because of their large areal extent, they contribute substantially to the global oceanic biological C pump (Emerson, 2014;Emerson et al., 1997). However, quantifying metabolic rates in the subtropical oligotrophic gyres is challenging, mostly due to the low rates that characterize these regions of the ocean, the episodic nonsteady state nature of these habitats, and the susceptibility of the microbial communities to small environmental perturbations introduced during incubation procedures (Williams et al., 2004). Proof of this