Abstract We evaluate how the concentrations of inorganic nutrients and chlorophyll a vary in a heterogeneous area (Equatorial SW Atlantic), covering a gradient from stations closer to the coast to others more distant associated or not with turbid-zone reefs. Vertical temperature (27.9 ± 0.10 °C; mean ± standard deviation) and salinity (36.2 ± 0.14) profles showed that the water column is well mixed (0-30 m depth). The oligotrophic condition was marked by low concentrations of phosphate (0.30 ± 0.22 µM) and dissolved inorganic nitrogen (0.64 ± 0.74 µM). Moreover, dissolved reactive silicon (DSi) was low in most samples (< 2.0 µM), but higher (>10 µM) in nearshore stations, probably related to continental runoff and/or resuspension of the bottom sediments. The pelagic phytoplankton biomass indicated that chlorophyll a (0.25 ± 0.08 µg L-1) was low, positively correlated with light and negatively correlated with nutrients, indicating possible phytoplankton uptake. Chlorophyll a concentrations were lower in stations closer to the coast and higher in some stations near the reefs, indicating that the latter could be more prone to phytoplankton development and depletion of nutrients, especially DSi. Therefore, although oligotrophy is present along this coast, we found some unexpected heterogeneity of nutrient and chlorophyll a distributions, which were probably infuenced by benthic-pelagic coupling due to the presence of extensive reefs, sponge gardens (18-30 m depth), and the proximity to the coast. These results highlight the importance of understanding the heterogeneity of ocean productivity, especially in lesser known low-latitude areas, which showed distinct nutrient and chlorophyll a levels related to the occurrence of tropical reefs that are capable of supporting important fsh stocks and unique biological communities. Equatorial Atlantic, Atlantic , Atlantic) turbidzone turbid zone 27.9 279 27 9 (27. 010 0 10 0.1 °C C deviation 36.2 362 36 2 (36. 0.14 014 14 030 30 (0-3 depth. depth . depth) 0.30 (0.3 022 22 0.2 µM 0.64 064 64 (0.6 074 74 0.7 µM. Moreover DSi (DSi < ( 20 2. µM, >10 (>1 andor sediments 0.25 025 25 (0.2 008 08 0.0 L1 L 1 L-1 uptake Therefore distributions benthicpelagic benthic 1830 18 (18-3 depth, productivity lowlatitude latitude areas communities 27. (27 01 0. 36. 3 (36 03 (0- 0.3 (0. 02 0.6 06 6 07 7 >1 (> 00 L- 183 (18- (2 (3 (0 > (18 (1