Impact from glacial rock flour on phytoplankton growth and the carbonate system
| Autor: | Jørgen Bendtsen, Niels Daugbjerg, Kristina Vallentin Larsen, Rasmus Dyrberg Dahms, Katherine Richardson, Minik Rosing |
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| Rok vydání: | 2023 |
| DOI: | 10.5194/egusphere-egu23-7285 |
| Popis: | Glacial rock flour (GRF) is a felsic, silicate sediment that originates below the Greenland Ice Sheet, where the ice abrades basement rocks to a very fine powder. This is then transported by meltwater rivers or subglacial discharge into fjords and coastal waters. Thus, GRF is a naturally occurring component of the oceans around Greenland. The grain size of GRF typically ranges |
| Databáze: | OpenAIRE |
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