Ice Station POLarstern (ISPOL) Fe + C incubations

Here, we hypothesize that Fe uptake rates by sea-ice algae and under-ice phytoplankton are higher than the rates reported for open ocean phytoplankton in the SO. We performed 55Fe and carbon (14C) short-term uptake field measurements in, on and under Antarctic sea ice. We collected under ice seawater, melted snow and sea-ice cores. We then spiked them with 14C or 55Fe radiotracers to measure Fe and C uptake rates by sea-ice algae. Samples were then filtered, and residual radioactivity on the filters measured liquid scintillation counter (Packard).

Data and resources

Additional information

Temporal extent2004-11-29 – 2004-12-31
Date (creation)2022-05-13
Statuscompleted
Update frequencynotPlanned
Metadata languageen
LicenseThe data described in this record are the intellectual property of the University of Tasmania through the Institute for Marine and Antarctic Studies.
Source metadataISO 19115 XML
Last updated2026-11-05
Created2026-11-05
APIpackage_show