Major elements, nutrients, and plankton biomass in the ice edge and an offshore region of the Indian Ocean sector of the Southern Ocean
Bibliographic Data
| ID | 9221503 |
|---|---|
| Authors | P V Shirodkar (National Institute of Oceanography), Joaquim I Goés (0000-0002-9785-6985, National Institute of Oceanography), R Alagarsamy (National Institute of Oceanography), S P Fondekar (National Institute of Oceanography) |
| Year | 1992 |
| Volume | 28 |
| Issue | 165 |
| Pages | 127-136 |
| Publication date | 1992-04-01 |
| Open Access | Yes |
| Type | ARTICLE |
| Venue | Polar Record (JOURNAL) |
| Journal identifiers | ISSN: 0032-2474 • E-ISSN: 1475-3057 |
| Publisher | Cambridge University Press (CUP) (PUBLISHER) |
| DOI | 10.1017/s0032247400013425 |
| OpenAlex | W2002892933 |
| Language | EN |
| References cited | 8 |
Physico-chemical and biological studies during the austral summer of 1986–87 in the ice-edge and a region offshore of Antarctica indicated significant spatial differences in concentrations of nutrients, dissolved oxygen (DO), Ca, Mg, and chlorophyll a , and in the rates of primary production. The waters within the ice-edge region were richer in nutrients and DO and showed a four-fold increase in chlorophyll a (1.98 mg m -3 ) and a 10-fold increase in primary productivity (0.74 mg C m -3 h -1 ) as compared with offshore waters. In the ice-edge region, Mg was high (1319 mg kg -1 ), whereas values of Ca (421.7 mg kg -1 ) were within the normal range. Offshore Ca (423.8 mg kg -1 ) and Mg (1297 mg kg -1 ) were within the expected limits. In the ice-edge region, Ca/Cl varied from 0.0202 to 0.0229, with a mean of 0.0220, and Mg/Cl varied from 0.0637 to 0.0737, with a mean of 0.0687. These figures were slightly higher than those offshore (Ca/Cl: 0.0205 to 0.0224, mean 0.0214; Mg/Cl: 0.0630 to 0.0693, mean 0.0657), indicating the addition of Mg to the waters in the ice-edge region. Nutrients in the ice-edge region showed increasing concentrations at deeper levels irrespective of their relationship with DO, indicating large amounts of preformed nutrients, a characteristic of Antarctic waters attributable to intense upwelling. Chlorophyll a showed a direct relation with primary productivity and an inverse relation with Mg, suggesting the release of Mg from biogenic matter. Offshore, phosphate-phosphorus (PO 4 -P) was significantly correlated with nitrate-nitrogen (NO 3 -N) and inversely correlated with primary productivity and chlorophyll a , indicating the utilization of PO 4 -P during high production. Significantly elevated concentrations of chlorophyll a, primary productivity and Mg, marked by a considerable decrease in nutrients, were observed at a frontal zone between 64° and 62°S
Chlorophyll · Chlorophyll a · Nutrient · Plankton · Submarine pipeline · Upwelling · Arctic and Antarctic ice dynamics · Chemistry · Environmental Science · Geology · Marine and coastal ecosystems · Marine Bivalve and Aquaculture Studies · Oceanography
| Highly cited | No |
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