The atmospheric and deep sea reservoirs of carbon dioxide are linked via physical, chemical, and biological processes. The last of these include photosynthesis, particle settling, and organic matter remineralization, and are collectively termed the "biological carbon pump." Herein, we present results from a 13-y (1992-2004) sediment trap experiment conducted in the permanently oligotrophic North Pacific Subtropical Gyre that document a large, rapid, and predictable summertime (July 15-August 15) pulse in particulate matter export to the deep sea (4,000 m). Peak daily fluxes of particulate matter during the summer export pulse (SEP) average 408, 283, 24.1, 1.1, and 67.5 μmol·m −2 ·d −1 for total carbon, organic carbon, nitrogen, phosphorus (PP), and biogenic silica, respectively. The SEP is approximately threefold greater than mean wintertime particle fluxes and fuels more efficient carbon sequestration because of low remineralization during downward transit that leads to elevated total carbon/PP and organic carbon/PP particle stoichiometry (371:1 and 250:1, respectively). Our long-term observations suggest that seasonal changes in the microbial assemblage, namely, summertime increases in the biomass and productivity of symbiotic nitrogen-fixing cyanobacteria in association with diatoms, are the main cause of the prominent SEP. The recurrent SEP is enigmatic because it is focused in time despite the absence of any obvious predictable stimulus or habitat condition. We hypothesize that changes in day length (photoperiodism) may be an important environmental cue to initiate aggregation and subsequent export of organic matter to the deep sea. Approximately half of the photosynthesis on Earth is attributable to microscopic, single-celled phytoplankton that inhabit the sea (1). Within the marine environment, most (∼90%) of the photosynthetic carbon fixation takes place in the low-biomass, low-nutrient open ocean gyres that are grossly undersampled relative to coastal habitats (2, 3). A small but variable (typically <15% for open ocean ecosystems) portion of the organic matter produced in the sunlit (euphotic) zone is exported to the deeper, dark regions of the ocean by gravitational settling of living and nonliving particulate organic matter (POM). Most of the exported POM undergoes microbial decomposition before reaching the seabed. This POM remineralization process creates a deep sea reservoir of inorganic nutrients, including dissolved inorganic carbon (DIC), nitrate (NO 3 − ), and phosphate (PO 4 3− ). The resupply of these deep sea nutrients to the euphotic zone via turbulent diffusion and upwelling sustains surface ocean productivity over long time scales.The term "carbon pump" (4) is used to describe the oceanic processes that collectively sustain the large ∼272 μmol C·kg −1 global mean surface-to-deep sea increase of DIC in the ocean. The carbon pump ultimately sets the limit for carbon dioxide (CO 2 ) exchange between the ocean and the atmosphere (4). A stated goal of the seminal paper by Volk and Hoffert (4...