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

• Main Authors: Jana Krause (2885033), Mark J. Hopwood (5009726), Juan Höfer (436195), Stephan Krisch (11483203), Eric P. Achterberg (337732), Emilio Alarcón (9040017), Dustin Carroll (424313), Humberto E. González (9149678), Thomas Juul-Pedersen (11483206), Te Liu (8052152), Pablo Lodeiro (4534324), Lorenz Meire (7500623), Minik T. Rosing (11483209)
• 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

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...