Table 1. Meltwater and suspended sediment Fe concentrations from Leverett Glacier and comparative studies.
Fe source | Mean Fe concentrations | s.d. | Fe range | n | Source |
---|---|---|---|---|---|
Filtered iron source (nM) | |||||
Greenland | |||||
<0.02 μm | 7 | 9 | <d1–37 | 66 | DFe—this study |
0.02–0.45 μm | 699 | 650 | 232–4,701 | 63 | CNFe—this study |
<0.03 μm—GrIS | 22 | 6–59 | 15 | 11 | |
0.03–0.4 μm—GrIS | 30.8 | 2–117 | 15 | 11 | |
<0.2 μm—GrIS | 3,700 | 2,200–9,310 | 13 | 12 | |
Antarctica | |||||
<0.2 μm—Blood Falls, AntIS | 4 × 106 | 1 | 41 | ||
<0.45 μm—Dry Valleys, AntIS | 335 | 82–1,146 | 11 | 58 | |
Ascorbate-extractable sediments (% dw) | |||||
Glacial meltwater—GrIS | 0.15 | 0.02 | 0.11–0.18 | 33 | SSFe—this study |
Icebergs—AntIS | 0.15 | 0.12 | 0.06–0.36 | 10 | 10 |
Icebergs—AntIS | 0.19 | 0.18 | 0.04–0.49 | 4 | 13 |
Aoelian dust—East Med. | 0.03 | 1 | 37 | ||
Aoelian dust—West Med. | 0.08 | 1 | 37 | ||
Aoelian dust—Sahara | 0.02 | 2 | 37 | ||
Aoelian dust—Sahel | 0.02 | 2 | 37 | ||
Aoelian dust—Beijing | 0.06 | 1 | 37 |
AntIS, Antarctic ice sheet; CNFe, colloidal/nanoparticulate Fe; DFe, dissolved Fe; GrIS, Greenland ice sheet.
Filtered concentrations are discharge weighted and presented in nanomolar. Values below the detection limit are indicated by <d1. Ascorbate-extractable concentrations are presented as % dry weight (% dw).