Open AccessAnnual cycle of primary production in the Cariaco Basin: Response to upwelling and implications for vertical export
Author(s) -
MullerKarger Frank,
Varela Ramon,
Thunell Robert,
Scranton Mary,
Bohrer Richard,
Taylor Gordon,
Capelo Juan,
Astor Yrene,
Tappa Eric,
Ho TungYuan,
Walsh John J.
Publication year - 2001
Publication title -
journal of geophysical research: oceans
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/1999jc000291
Subject(s) - upwelling , oceanography , hydrography , carbon cycle , ocean gyre , geology , flux (metallurgy) , sediment , total organic carbon , environmental science , annual cycle , settling , structural basin , subtropics , climatology , geomorphology , ecology , materials science , ecosystem , environmental engineering , fishery , metallurgy , biology
Monthly hydrographic, primary production, bacterial production, and settling particulate carbon flux observations were collected between November 1995 and December 1997 at 10.5°N, 64.67°W within the Cariaco Basin, off Venezuela. Upwelling of Subtropical Underwater (SUW) started around October and lasted through approximately May of the following year. Wind speeds >7 m s −1 were observed between January and June, with weaker winds (<5 m s −1 ) between July and December. The upwelling cycle was therefore out of phase with that of the trade winds by 2–3 months. A seasonal cycle punctuated by transient extremes associated with subsurface ventilation events was observed in primary production. High bacterial activity and organic carbon recycling rates were observed near the oxic‐anoxic interface. Integrated primary production was 690 gC m −2 yr −1 in 1996 and 540 gC m −2 yr −1 in 1997. Settling carbon flux measured with sediment traps was about 5.6% of integrated primary production at 275 m and about 1.7% at 1225 m, with no seasonality in the proportion of vertical flux to primary production. In total, between 10 and 11 gC m −2 yr −1 were delivered to the bottom sediment of Cariaco, which suggests that between 4×10 5 and 1×10 6 t of C yr −1 were delivered to sediments within the upwelling area of the Cariaco Basin. This represents permanent sequestration of carbon previously entrained in the North Atlantic gyre in the area of formation of SUW. Results suggests that upwelled inorganic nitrogen, rather than nitrogen fixation, is responsible for the large productivity and particulate carbon settling flux in the Cariaco Basin.