Seasonal and spatial dynamics of iron availability in the Scotia Sea
Autor: | Rebecca E. Korb, Daria J. Hinz, Michael J. Whitehouse, C. Mark Moore, Richard Sanders, Maria C. Nielsdóttir, Thomas S. Bibby, Eric P. Achterberg |
---|---|
Rok vydání: | 2012 |
Předmět: |
0106 biological sciences
geography Chlorophyll a geography.geographical_feature_category 010504 meteorology & atmospheric sciences 010604 marine biology & hydrobiology General Chemistry Oceanography 01 natural sciences chemistry.chemical_compound Nutrient Nitrate chemistry Benthic zone Chlorophyll Phytoplankton Spring (hydrology) Sea ice Environmental Chemistry 14. Life underwater 0105 earth and related environmental sciences Water Science and Technology |
Zdroj: | Marine Chemistry. :62-72 |
ISSN: | 0304-4203 |
DOI: | 10.1016/j.marchem.2011.12.004 |
Popis: | The Southern Ocean is the world's largest high nutrient low chlorophyll (HNLC) region. However, satellite images highlight several areas associated with island chains and shallow topographic features which display high phytoplankton biomass. Here we present the first study of seasonal variations in phytoplankton biomass and iron availability in the Scotia Sea over both austral spring and summer seasons. Based on dissolved iron (dFe) and Chlorophyll a (Chl a) concentrations, the study area is be divided into three regions: North of South Georgia, south of South Georgia and the vicinity of South Orkney Islands. The Scotia Sea to the south of South Georgia exhibited low dFe concentrations ( 0.05). Nitrate concentrations were 16 mu M lower in summer compared to spring, whilst Chl a standing stocks remained high. Enhanced dFe (similar to 0.25 nM) and Chl a concentrations were furthermore observed in the vicinity of the South Orkney Islands, located in the southern Scotia Sea. Iron addition experiments showed that in situ phytoplankton were iron replete spring and summer north of South Georgia and in the vicinity of South Orkney Islands during summer. We thus suggest that increased iron supply in high productivity areas including the area north of South Georgia and the South Orkney Islands, was sustained by a continuous benthic supply from their shelf systems, with a potential additional input from seasonally retreating sea ice in the South Orkney system |
Databáze: | OpenAIRE |
Externí odkaz: |