Marco Grotti
Biographic Data
| ID | 9037677 |
|---|---|
| NAME | Marco Grotti |
| GIVEN NAMES | Marco |
| FAMILY NAME | Grotti |
| SIGNATURE | GROTTI M |
| AFFILIATIONS | University of Genoa |
| ORCID | 0000-0001-6956-5761 |
| VERIFIED | No |
| TOTAL WORKS | 2 |
| TOTAL CITATIONS | 0 |
| AUTHOR COUNT | 2 |
| EDITOR COUNT | 0 |
| FIRST PUBLICATION YEAR | 2016 |
| LATEST PUBLICATION YEAR | 2023 |
| H-INDEX | 0 |
A proposed seasonal cycle of dissolved iron-binding ligands in Antarctic sea ice
Iron (Fe) is an essential micronutrient to oceanic microalgae, and its dissolved fraction (DFe) is retained in surface waters by Fe-binding ligands. Previous work has suggested that ligands may also bind Fe within sea ice, although supporting data are limited. This study investigates distribution, concentration, and potential drivers of Fe-binding ligands in Antarctic sea ice, considering the ice type, location and season. Results suggest that th…
Iron in sea ice
The discovery that melting sea ice can fertilize iron (Fe)-depleted polar waters has recently fostered trace metal research efforts in sea ice. The aim of this review is to summarize and synthesize the current understanding of Fe biogeochemistry in sea ice. To do so, we compiled available data on particulate, dissolved, and total dissolvable Fe (PFe, DFe and TDFe, respectively) from sea-ice studies from both polar regions and from sub-Arctic and …
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Iron in sea ice
The discovery that melting sea ice can fertilize iron (Fe)-depleted polar waters has recently fostered trace metal research efforts in sea ice. The aim of this review is to summarize and synthesize the current understanding of Fe biogeochemistry in sea ice. To do so, we compiled available data on particulate, dissolved, and total dissolvable Fe (PFe, DFe and TDFe, respectively) from sea-ice studies from both polar regions and from sub-Arctic and …
A proposed seasonal cycle of dissolved iron-binding ligands in Antarctic sea ice
Iron (Fe) is an essential micronutrient to oceanic microalgae, and its dissolved fraction (DFe) is retained in surface waters by Fe-binding ligands. Previous work has suggested that ligands may also bind Fe within sea ice, although supporting data are limited. This study investigates distribution, concentration, and potential drivers of Fe-binding ligands in Antarctic sea ice, considering the ice type, location and season. Results suggest that th…
Arctic and Antarctic ice dynamics (2 works) · Environmental Science (2 works) · Geology (2 works) · Marine and coastal ecosystems (2 works) · Oceanography (2 works) · Sea ice (2 works) · Antarctic sea ice (1 work) · Arctic ice pack (1 work) · Biogeochemistry (1 work) · Biota (1 work)