Is Nitrogen Uptake Rate by Phytoplankton below the Euphotic Zone in the Yellow Sea Considerable
Sung-Ryull Yang, Jae-Hyung Shim, Chang-Soo Chung, Gi Hoon Hong, Se-Jin Pae, Dong-Beom Yang, Myung-Gil Park
Abstract
Sung-Ryull Yang, Jae-Hyung Shim, Chang-Soo Chung, Gi Hoon Hong, Se-Jin Pae, Dong-Beom Yang, Myung-Gil Park
Abstract
To determine whether nitrogen (N) uptake by phytoplankton below the euphotic zone in the Yellow Sea is considerable, we measured the uptake rates of nitrate and ammonium using -labeled stable isotope and , in May and November 1997 at total 10 stations. Depth-integrated uptake rates of nitrate and ammonium over the euphotic zone during this study ranged from 1.8 to 15.3 mg N and from 5.0 to 132.2 mg N , respectively, and ammonium uptake predominated at 9 of 10 stations (1.9-19.4 fold). Depth-integrated uptake rates of nitrate and ammonium over the whole water column ranged from 2.9 to 22.0 mg N and from 15.7 to 175.5 mg N , respectively. The significant proportion of whole water column N uptake was attributed to uptake by phytoplankton below the euphotic zone, ranging from 13.0 to 86.2% for nitrate and from 13.8 to 67.8% for ammonium, indicating that phytoplankton N uptake below the euphotic zone is at times considerable in the study area. The results suggest that when phytoplankton below the euphotic zone in the Yellow Sea are again entrained into the euphotic zone by a certain physical forcing such as turbulent mixing and the vertical movement of thermocline, these episodic events may significantly affect the material fluxes within the euphotic zone. Furthermore, the results suggest that a portion of regenerated production estimated from -ammonium uptake should be included in new production estimates, which otherwise could be underestimated in the Yellow Sea.
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To determine whether nitrogen (N) uptake by phytoplankton below the euphotic zone in the Yellow Sea is considerable, we measured the uptake rates of nitrate and ammonium using -labeled stable isotope and , in May and November 1997 at total 10 stations. Depth-integrated uptake rates of nitrate and ammonium over the euphotic zone during this study ranged from 1.8 to 15.3 mg N and from 5.0 to 132.2 mg N , respectively, and ammonium uptake predominated at 9 of 10 stations (1.9-19.4 fold). Depth-integrated uptake rates of nitrate and ammonium over the whole water column ranged from 2.9 to 22.0 mg N and from 15.7 to 175.5 mg N , respectively. The significant proportion of whole water column N uptake was attributed to uptake by phytoplankton below the euphotic zone, ranging from 13.0 to 86.2% for nitrate and from 13.8 to 67.8% for ammonium, indicating that phytoplankton N uptake below the euphotic zone is at times considerable in the study area. The results suggest that when phytoplankton below the euphotic zone in the Yellow Sea are again entrained into the euphotic zone by a certain physical forcing such as turbulent mixing and the vertical movement of thermocline, these episodic events may significantly affect the material fluxes within the euphotic zone. Furthermore, the results suggest that a portion of regenerated production estimated from -ammonium uptake should be included in new production estimates, which otherwise could be underestimated in the Yellow Sea.
Key concepts: Photic zone, Phytoplankton, New production, Ammonium, Water column, Nitrate, Thermocline, Nitrogen