Depth profiles of suspended carbon and nitrogen along a North Pacific transect: Concentrations, isotopes, and ratios

• Published in: Limnology and Oceanography
• Main Authors: Dong, Sijia, Wang, Xingchen Tony, Subhas, Adam V., Pavia, Frank J., Adkins, Jess F., Berelson, William M.
• Other Authors: Grantham Foundation for the Protection of the Environment, National Science Foundation of Sri Lanka, Simons Foundation
• Format: Article in Journal/Newspaper
• Language: English
• Published: Wiley 2021
• Subjects: Pacific; Subarctic
• Online Access: http://dx.doi.org/10.1002/lno.11989; https://onlinelibrary.wiley.com/doi/pdf/10.1002/lno.11989; https://onlinelibrary.wiley.com/doi/full-xml/10.1002/lno.11989; https://aslopubs.onlinelibrary.wiley.com/doi/pdf/10.1002/lno.11989

Abstract We present concentrations of total particulate carbon (PC), carbonate (PIC), total particulate nitrogen (PN), 13 C and 15 N 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 δ 15 N 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 δ 15 N (up to 12‰) were observed in the euphotic zone, which was likely caused by the export of low‐δ 15 N PN during the phytoplankton blooms. Average C org : 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).