FN Archimer Export Format
PT J
TI Mesopelagic carbon remineralization during the European iron fertilization experiment
BT 
AF JACQUET, S.H.M.
   SAVOYE, N.
   DEHAIRS, F.
   STRASS, V. H.
   CARDINAL, D.
AS 1:1,3,6;2:3,4;3:3;4:5;5:2;
FF 1:;2:;3:;4:;5:;
C1 CEREGE, F-13545 Aix En Provence, France.
   Royal Museum Cent Africa, Dept Geol, B-3080 Tervuren, Belgium.
   Vrije Univ Brussel, Dept Analyt & Environm Chem, B-1050 Brussels, Belgium.
   Univ Bordeaux 1, CNRS, UMR 5805 EPOC, Observat Aquitain Sci Univers,Stn Marine Arcachon, F-33120 Arcachon, France.
   Alfred Wegener Inst Polar & Marine Res, D-27515 Bremerhaven, Germany.
   CEREGE, UMR 6635, Europole Mediterraneen Arbois, Aix En Provence, France.
C2 CEREGE, FRANCE
   ROYAL MUSEUM CENT AFRICA, BELGIUM
   UNIV VRIJE BRUSSEL, BELGIUM
   UNIV BORDEAUX, FRANCE
   INST A WEGENER, GERMANY
   CEREGE, FRANCE
IF 4.09
TC 28
UR https://archimer.ifremer.fr/doc/00237/34870/33193.pdf
   https://archimer.ifremer.fr/doc/00237/34870/33194.pdf
LA English
DT Article
CR MD 145 / KEOPS
BO Marion Dufresne
AB [1] The impact of iron fertilization on mesopelagic carbon (C) remineralization was assessed during the European Iron Fertilization Experiment (EIFEX) in the Southern Ocean by following the temporal change of excess particulate barium (also called biogenic or Ba(xs)) in the mesopelagic waters of a mesoscale eddy. Before the iron infusion the site was already sustaining a significant vertical flux of particles leading to organic remineralization in the mesopelagic. Approximately 35 d after the fertilization, mesopelagic Baxs contents provided evidence of changes in surface particulate export and of enhanced and particularly fast remineralization extending down to 1000 m. At the end of the experiment (day 36) both export and remineralization decreased. Organic carbon remineralization took place mainly in the lower part of the mesopelagic zone (500 - 1000 m) and increased more than 5-fold during EIFEX, reaching values up to 92 +/- 15 mg C m(-2) d(-1). However, such remineralization rates are not particularly high when compared to other values reported for the natural Southern Ocean during summer. Though export and remineralization reached peak values around day 34, remineralization integrated over the 150 to 1000 m layer accounted only for 13 +/- 1.4% of the export at 150 m, suggesting that a substantial amount of exported carbon reached deeper in the water column. Compared to natural blooms in high-nutrient low-chlorophyll (HNLC) waters of the Southern Ocean, the Fe-induced bloom during EIFEX resulted in a lower ratio of remineralized organic carbon over exported carbon, similar to what we recently observed for natural Fe-replete conditions prevailing above the Kerguelen Plateau. Unexpected similarities and phase lags of profiles in the mesopelagic between casts sampled inside and outside the fertilized patch during EIFEX indicated that eddy dynamics were a determinant in setting particle patterns on a broad spatial scale exceeding the extent of the fertilization, thereby homogenizing the signals of mesopelagic remineralization.
PY 2008
PD MAR
SO Global Biogeochemical Cycles
SN 0886-6236
PU Amer Geophysical Union
VL 22
IS 1 / GB1023
UT 000253715700001
BP 1
EP 9
DI 10.1029/2006GB002902
ID 34870
ER

EF