SciELO - Scientific Electronic Library Online

 
vol.26 issue1Diversidad de escarabajos coprófagos (Coleoptera: Scarabaeinae) en un remanente ribereño y un fragmento de bosque húmedo tropical en Córdoba, ColombiaFood habits of Geoffroy's cat (Leopardus geoffroyi) in agroecosystem habitats of Buenos Aires, Argentina author indexsubject indexarticles search
Home Pagealphabetic serial listing  

Services on Demand

Journal

Article

Indicators

  • Have no cited articlesCited by SciELO

Related links

Share


Ecología austral

On-line version ISSN 1667-782X

Abstract

PAPARAZZO, Flavio E. et al. Spatial and temporal trends in the distribution of macronutrients in surface waters of the Drake Passage. Ecol. austral [online]. 2016, vol.26, n.1, pp.27-39. ISSN 1667-782X.

The Drake Passage (DP) links the Southern Pacific and Atlantic Oceans, and acts as a physical narrowing for the largest current of the World Ocean, the Antarctic Circumpolar Current (ACC). This result in a constriction of the main circumpolar fronts related to the ACC: the Subantarctic Front, the Polar Front, the Southern Antarctic Circumpolar Current Front and the Continental Water Boundary Front. Previous studies showed that the DP is a high-nutrient low-chlorophyll (HNLC) region, but studies on the interannual and seasonal macronutrients' fluctuations in relation with chlorophyll and frontal areas in the DP are scarce. This study analyzes the spatial and temporal trends of nitrate, phosphate, and silicate on surface samples from 113 oceanographic stations in the DP during summer and early fall of 2001 to 2004, in relation with the different fronts and chlorophyll-a concentration. The results revealed an increase of nutrients towards the south. Nitrate showed values from 3 µM at 55° S to 27 µM at 63° S, whereas values from 0.3 µM at 55° S to 2.6 µM at 63° S were observed for phosphate. Silicate increased considerably south of Polar Front, from 0 µM at 55° S to 74 µM at 62° S. The nutrients concentration was significantly higher in summer than in early fall and showed a trend to decrease over the studied years. A complex sum of biogeochemical processes would generate the main seasonal trends, while atmospheric-oceanic processes such as Southern Annular Mode and El Niño Southern Oscillation, would be responsible of observed nutrients interannual variability.

Keywords : Nitrate; Phosphate; Silicate; Chlorophyll-a; Temperature; Salinity; Antarctic fronts; Antarctic zones; Seasonal variation; Interannual variation.

        · abstract in Spanish     · text in English

 

Creative Commons License All the contents of this journal, except where otherwise noted, is licensed under a Creative Commons Attribution License