Y. Ternois et al., HYDROCARBONS, STEROLS AND ALKENONES IN SINKING PARTICLES IN THE INDIAN-OCEAN SECTOR OF THE SOUTHERN-OCEAN, Organic geochemistry, 28(7-8), 1998, pp. 489-501
Hydrocarbons, sterols and alkenones were analyzed in samples collected
from a 10 month sediment trap time series deployed in the Indian Ocea
n sector of the Southern Ocean. Fluxes and within-class distributions
varied seasonally. During higher mass and organic carbon (OC) flux per
iods, which occurred in austral summer and fall, fresh marine inputs w
ere predominant. Vertical fluxes were most intense in January, but lim
ited to one week in duration. They were, however, low compared with ot
her oceanic regions. In contrast, low mass and OC Bur periods were cha
racterized by a strong unresolved complex mixture (UCM) in the hydroca
rbon fraction and a high proportion of stanols as a result of zooplank
tonic grazing. Terrigenous inputs were not detectable. The alkenone co
mpositions were consistent with previous data on suspended particles f
rom Antarctic waters. However, U-37(K') values diverged from the linea
r and exponential fits established by Sikes, E. L, and Volkman, J. K.
Calibration of alkenone unsaturation ratios (U-37(K')) for paleotemper
ature estimation in cold polar waters. Geochimica et Cosmochimica Acta
, 1993, 57, 1883-1889], in the low temperature range. The seasonal pat
tern of alkenone production implied that IPT (integrated production te
mperature) is likely to be strongly imprinted by austral summer and fa
ll SST (sea surface temperature). (C) 1998 Elsevier Science Ltd. All r
ights reserved.