Table1_Trace Element (Fe, Co, Ni and Cu) Dynamics Across the Salinity Gradient in Arctic and Antarctic Glacier Fjords.XLS

• Main Authors: Jana Krause, Mark J. Hopwood, Juan Höfer, Stephan Krisch, Eric P. Achterberg, Emilio Alarcón, Dustin Carroll, Humberto E. González, Thomas Juul-Pedersen, Te Liu, Pablo Lodeiro, Lorenz Meire, Minik T. Rosing
• Format: Dataset
• Language: unknown
• Published: 2021
• Subjects: Solid Earth Sciences; Climate Science; Atmospheric Sciences not elsewhere classified; Exploration Geochemistry; Inorganic Geochemistry; Isotope Geochemistry; Organic Geochemistry; Geochemistry not elsewhere classified; Igneous and Metamorphic Petrology; Ore Deposit Petrology; Palaeontology (incl. Palynology); Structural Geology; Tectonics; Volcanology; Geology not elsewhere classified; Seismology and Seismic Exploration; Glaciology; Hydrogeology; Natural Hazards; Quaternary Environments; Earth Sciences not elsewhere classified; Evolutionary Impacts of Climate Change; iron; copper; nickel; cobalt; glacier; fjord; Arctic; Antarctic; Ameralik; Greenland; Kangaatsiaq; Antarc*; Climate change; greenlandic
• Online Access: https://doi.org/10.3389/feart.2021.725279.s002; https://figshare.com/articles/dataset/Table1_Trace_Element_Fe_Co_Ni_and_Cu_Dynamics_Across_the_Salinity_Gradient_in_Arctic_and_Antarctic_Glacier_Fjords_XLS/16683595

Around the Greenlandic and Antarctic coastlines, sediment plumes associated with glaciers are significant sources of lithogenic material to the ocean. These plumes contain elevated concentrations of a range of trace metals, especially in particle bound phases, but it is not clear how these particles...