Abstract

AbstractWe present concentrations of total particulate carbon (PC), carbonate (PIC), total particulate nitrogen (PN), 13C and 15N of suspended particles along a North Pacific transect. In the upper 400 m, suspended PIC to particulate organic carbon (POC) ratios generally follow published sinking PIC/POC ratios. Below 600 m, suspended PIC/POC become significantly lower than sinking PIC/POC, likely indicating PIC dissolution within the suspended load. In three out of the five stations, suspended PN δ15N increase with depth from the euphotic zone to the thermocline, consistent with previous observations in many ocean regions (e.g.,BATS and HOT). However, in the other two stations where phytoplankton blooms were encountered, high suspended PN δ15N (up to 12‰) were observed in the euphotic zone, which was likely caused by the export of low‐δ15N PN during the phytoplankton blooms. Average Corg : N ratio of suspended particles along the transect is 5.1 0.2, with the value in the subtropical gyre (5.8 0.3) slightly higher than the subarctic gyre (4.6 0.2).

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