Dissolved greenhouse gases (nitrous oxide and methane) associated with the naturally iron-fertilized Kerguelen region (KEOPS 2 cruise) in the Southern Ocean

• Published in: Biogeosciences
• Main Authors: Farías, L., Florez-Leiva, L., Besoain, V., Sarthou, G., Fernández, C.
• Format: Text
• Language: English
• Published: 2018
• Subjects: Austral; Kerguelen; Kerguelen Islands; Southern Ocean
• Online Access: https://doi.org/10.5194/bg-12-1925-2015; https://www.biogeosciences.net/12/1925/2015/

The concentrations of greenhouse gases (GHGs), such as nitrous oxide (N 2 O) and methane (CH 4 ), were measured in the Kerguelen Plateau region (KPR). The KPR is affected by an annual microalgal bloom caused by natural iron fertilization, and this may stimulate the microbes involved in GHG cycling. This study was carried out during the KEOPS 2 cruise during the austral spring of 2011. Oceanographic variables, including N 2 O and CH 4 , were sampled (from the surface to 500 m depth) in two transects along and across the KRP, the north–south (TNS) transect (46°–51° S, ~ 72° E) and the east–west (TEW) transect (66°–75° E, ~ 48.3° S), both associated with the presence of a plateau, polar front (PF) and other mesoscale features. The TEW presented N 2 O levels ranging from equilibrium (105%) to slightly supersaturated (120%) with respect to the atmosphere, whereas CH 4 levels fluctuated dramatically, being highly supersaturated (120–970%) in areas close to the coastal waters of the Kerguelen Islands and in the PF. The TNS showed a more homogenous distribution for both gases, with N 2 O and CH 4 levels ranging from 88 to 171% and 45 to 666% saturation, respectively. Surface CH 4 peaked at southeastern stations of the KPR (A3 stations), where a phytoplankton bloom was observed. Both gases responded significantly, but in contrasting ways (CH 4 accumulation and N 2 O depletion), to the patchy distribution of chlorophyll a . This seems to be associated to the supply of iron from various sources. Air–sea fluxes for N 2 O (from −10.5 to 8.65, mean 1.25 ± 4.04 μmol m −2 d −1 ) and for CH 4 (from 0.32 to 38.1, mean 10.01 ± 9.97 μmol −2 d −1 ) indicated that the KPR is both a sink and a source for N 2 O, as well as a considerable and variable source of CH 4 . This appears to be associated with biological factors, as well as the transport of water masses enriched with Fe and CH 4 from the coastal area of the Kerguelen Islands. These previously unreported results for the Southern Ocean suggest an intense microbial CH 4 production in the study area.