Distribution of dissolved labile and particulate iron and copper in Terra Nova Bay polynya (Ross Sea,Antarctica) surface waters in relation to nutrients and phytoplankton growth |
| |
| Authors: | Paola Rivaro Carmela Ianni Serena Massolo M Luisa Abelmoschi Cinzia De Vittor Roberto Frache |
| |
| Institution: | 1. Department of Earth, Ocean, Atmospheric Science, Florida State University, 117 N. Woodward Avenue, Tallahassee, FL 32306, USA;2. Joint Institute for the Study of the Atmosphere and Ocean, University of Washington, 7600 Sand Point Way NE/Bldg. 3, Bin C 15700, Seattle, WA 98115-0070, USA;3. NOAA/PMEL, 7600 Sand Point Way NE/Bldg. 3, Bin C 15700, Seattle, WA 98115-0070, USA;4. Skidaway Institute of Oceanography, University of Georgia, 10 Ocean Science Circle, Savannah, GA 31411, USA |
| |
| Abstract: | The distribution of the dissolved labile and of the particulate Fe and Cu together with dissolved oxygen, nutrients, chlorophyll a and total particulate matter was investigated in the surface waters of Terra Nova Bay polynya in mid-January 2003. The measurements were conducted within the framework of the Italian Climatic Long-term Interactions of the Mass balance in Antarctica (CLIMA) Project activities. The labile dissolved fraction was operationally defined by employing the chelating resin Chelex-100, which retains free and loosely bound trace metal species. The dissolved labile Fe ranges from below the detection limit (0.15 nM) to 3.71 nM, while the dissolved labile Cu from below the detection limit (0.10 nM) to 0.90 nM. The lowest concentrations for both metals were observed at 20 m depth (the shallowest depth for which metals were measured). The concentration of the particulate Fe was about 5 times higher than the dissolved Fe concentration, ranging from 0.56 to 24.83 nM with an average of 6.45 nM. The concentration of the particulate Cu ranged from 0.01 to 0.71 nM with an average of 0.17 nM. The values are in agreement with the previous data collected in the same area. We evaluated the role of the Fe and Cu as biolimiting metals. The N:dissolved labile Fe ratios (18,900–130,666) would or would not allow a complete nitrate removal, on the basis of the N:Fe requirement ratios that we calculated considering the N:P and the C:P ratios estimated for diatoms. This finding partially agrees with the Si:N ratio that we found (2.29). Moreover we considered a possible influence of the dissolved labile Cu on the Fe uptake process. |
| |
| Keywords: | |
| 本文献已被 ScienceDirect 等数据库收录！ |
|
