Untitled Document
Winter-time dissolved iron and nutrient distributions
in the Subantarctic Zone from 40-52S; 155-160E
Michael Ellwood1, Philip W Boyd2 and
Philip Sutton3
1 Research School of Earth Sciences, Australian National University,
Canberra, ACT 0200, Australia
2 National Institute for Water and Atmospheric Research (NIWA), Centre
for Chemical and Physical Oceanography, Department of Chemistry, University
of Otago, Dunedin, New Zealand.
3 National Institute for Water and Atmospheric Research (NIWA), Wellington,
New Zealand.
Figure
1.
In the Southern Ocean, mesoscale iron fertilization experiments have
clearly demonstrated that iron plays a pivotal role in controlling primary
production in polar and subpolar High Nitrate Low Chlorophyll (HNLC)
waters. There
has been considerable debate about the relative magnitude of different
iron sources to surface waters in these regions, such as upwelling, dust
or entrainment from island and continental self sediments. However, despite
the rapidly emerging field of iron biogeochemistry, there are few vertical
profiles of dissolved iron concentration, and almost no winter iron data. During
2006 we generated the first comprehensive winter dataset for dissolved
iron and nitrate distributions (0-1000 m depth) between 40 °S - 52 °S,
which transects the Subantarctic zone (SAZ), west of New Zealand (Figure
1).
Surface iron concentrations (<0.2 nmol Fe kg-1) were conspicuously
low, i.e., probably biologically limiting even at winter-reserve levels,
at frontal zones between 43 °S (Subtropical Front) and ~51 °S (Subantarctic
Front) (Figure 2). A fivefold range in iron:nitrate molar ratios was
observed along the transect, with Subtropical waters, where blooms occur,
having the highest ratios in subsurface waters. The major wintertime
supply of dissolved iron in the SAZ is from Ekman advection of waters
from the south (but calculated source water dissolved iron is ~0.2 nmol
Fe kg-1), suggesting that mixed-layer dissolved iron concentration is
controlled by how long these southern waters remain at the surface (~3
years).
Figure 2