Quantifying the surfacesubsurface biogeochemical coupling during

• Main Authors: Philip W Boyd, Mark P Gall, Mary W Silver, Susan L Coale, Robert R Bidigare, James K B Bishop
• Other Authors: The Pennsylvania State University CiteSeerX Archives
• Format: Text
• Language: English
• Published: 2008
• Subjects: Pacific; Subarctic
• Online Access: http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1081.2031

Abstract A central question addressed by the VERTIGO (VERtical Transport In the Global Ocean) study was 'What controls the efficiency of particle export between the surface and subsurface ocean'? Here, we present data from sites at ALOHA (N Central Pacific Gyre) and K2 (NW subarctic Pacific) on phytoplankton processes, and relate them via a simple planktonic foodweb model, to subsurface particle export (150-500 m). Three key factors enable quantification of the surface-subsurface coupling: a sampling design to overcome the temporal lag and spatial displacement between surface and subsurface processes; data on the size-partitioning of Net Primary Production (NPP) and subsequent transformations prior to export; estimates of the ratio of algal-to faecal- This decrease in predicted export at K2 matches the observed trend for E 150 . Also, the low attenuation of export flux from 60 to 150 m is consistent with that between 150 to 500 m. This strong surface-subsurface coupling suggests that phytoplankton productivity and floristics play a key role at K2 in setting export flux, and moreover that pelagic 3 particle transformations by grazers strongly influence to what extent sinking particles are further broken down in the underlying waters of the Twilight Zone. Introduction The biological pump is one of several (such as the solubility pump) that sequester