Distributions and stoichiometry of dissolved nitrogen and phosphorus in the iron-fertilized region near Kerguelen (Southern Ocean)

• Published in: Biogeosciences
• Main Authors: Blain, S., Capparos, J., Guéneuguès, A., Obernosterer, I., Oriol, L.
• Format: Text
• Language: English
• Published: 2018
• Subjects: Kerguelen; Kerguelen Island; Southern Ocean
• Online Access: https://doi.org/10.5194/bg-12-623-2015; https://www.biogeosciences.net/12/623/2015/

During KEOPS2 (Kerguelen Ocean and Plateau Compared Study 2), we determined dissolved inorganic and organic nitrogen and phosphorus species in the naturally fertilized region of Kerguelen Island (Southern Ocean). Above 150 m, stations were clearly separated by the polar front (PF), with concentrations of NO 3 - , NO 2 - and PO 4 3- overall lower north of the PF than south. Though less pronounced, a similar trend was detectable for dissolved organic nitrogen (DON) and dissolved organic phosphorus (DOP). At all stations offshore and above the plateau, a subsurface maximum of NH 4 + was observed between 50 and 150 m. We examined nutrient stoichiometry by calculating the linear combination N * = [NO 3 - ]-16 [PO 4 3- ]. The majority of stations and depths revealed N * close to −3 μM; however, for surface waters north of the PF, N * increased up to 6 μM. This suggests a preferential uptake of PO 4 3- versus NO 3 - by fast-growing diatoms. Using the tracer TN xs = [TDN]-16[TDP] (TDN, total dissolved nitrogen; TDP, total dissolved phosphorus) revealed that the dissolved organic fraction significantly contributed to changes in TN xs . TN xs values were negative for most stations and depths, and relatively constant in the 0–500 m layer. As for N * , the stations north of the PF had higher TN xs in the 0–100 m layer. We discuss this stoichiometric anomaly with respect to possible external sources and sinks of N and P. Additional data collected in February 2013 at two sites revealed the occurrence of a subsurface minimum of N * located just below the pycnocline, which denotes a layer where remineralization of particulate organic matter with low N : P ratio P, possibly associated with preferential remineralization of P versus N, persists throughout the season.