FN Archimer Export Format
PT J
TI Processes controlling the Si-isotopic composition in the Southern Ocean and application for paleoceanography
BT 
AF FRIPIAT, F.
   CAVAGNA, A. -J.
   DEHAIRS, F.
   DE BRAUWERE, A.
   ANDRE, L.
   CARDINAL, D.
AS 1:1,2;2:3;3:3;4:3,4;5:1;6:1;
FF 1:;2:;3:;4:;5:;6:;
C1 Royal Museum Cent Africa, Sect Mineral & Petrog, Tervuren, Belgium.
   Univ Libre Brussels, Dept Earth & Environm Sci, Brussels, Belgium.
   Vrije Univ Brussel, Brussels, Belgium.
   Catholic Univ Louvain, Inst Mech Mat & Civil Engn IMMC, B-1348 Louvain, Belgium.
C2 ROYAL MUSEUM CENT AFRICA, BELGIUM
   UNIV LIBRE BRUXELLES, BELGIUM
   UNIV VRIJE BRUSSEL, BELGIUM
   UCL, BELGIUM
IN DOAJ
IF 3.75
TC 39
UR https://archimer.ifremer.fr/doc/00226/33769/32565.pdf
LA English
DT Article
CR MD 166 / BONUS-GOODHOPE
BO Marion Dufresne
AB Southern Ocean biogeochemical processes have an impact on global marine primary production and global elemental cycling, e.g. by likely controlling glacial-interglacial pCO(2) variation. In this context, the natural silicon isotopic composition (delta Si-30) of sedimentary biogenic silica has been used to reconstruct past Si-consumption:supply ratios in the surface waters. We present a new dataset in the Southern Ocean from a IPY-GEOTRACES transect (Bonus-GoodHope) which includes for the first time summer delta Si-30 signatures of suspended biogenic silica (i) for the whole water column at three stations and (ii) in the mixed layer at seven stations from the subtropical zone up to the Weddell Gyre. In general, the isotopic composition of biogenic opal exported to depth was comparable to the opal leaving the mixed layer and did not seem to be affected by any diagenetic processes during settling, even if an effect of biogenic silica dissolution cannot be ruled out in the northern part of the Weddell Gyre. We develop a mechanistic understanding of the processes involved in the modern Si-isotopic balance, by implementing a mixed layer model. We observe that the accumulated biogenic silica (sensu Rayleigh distillation) should satisfactorily describe the delta Si-30 composition of biogenic silica exported out of the mixed layer, within the limit of the current analytical precision on the delta Si-30. The failures of previous models (Rayleigh and steady state) become apparent especially at the end of the productive period in the mixed layer, when biogenic silica production and export are low. This results from (1) a higher biogenic silica dissolution:production ratio imposing a lower net fractionation factor and (2) a higher Si-supply:Si-uptake ratio supplying light Si-isotopes into the mixed layer. The latter effect is especially expressed when the summer mixed layer becomes strongly Si-depleted, together with a large vertical silicic acid gradient, e.g. in the Polar Front Zone and at the Polar Front.
PY 2012
SO Biogeosciences
SN 1726-4170
PU Copernicus Gesellschaft Mbh
VL 9
IS 7
UT 000306976100007
BP 2443
EP 2457
DI 10.5194/bg-9-2443-2012
ID 33769
ER

EF