Global Ocean Sediment Composition and Burial Flux in the Deep Sea

Quantitative knowledge about the burial of sedimentary components at the seafloor has wide‐ranging implications in ocean science, from global climate to continental weathering. The use of 230Th‐normalized fluxes reduces uncertainties that many prior studies faced by accounting for the effects of sed...

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Veröffentlicht in:	Global biogeochemical cycles 2021-04, Vol.35 (4), p.n/a
Hauptverfasser:	Hayes, Christopher T., Costa, Kassandra M., Anderson, Robert F., Calvo, Eva, Chase, Zanna, Demina, Ludmila L., Dutay, Jean‐Claude, German, Christopher R., Heimbürger‐Boavida, Lars‐Eric, Jaccard, Samuel L., Jacobel, Allison, Kohfeld, Karen E., Kravchishina, Marina D., Lippold, Jörg, Mekik, Figen, Missiaen, Lise, Pavia, Frank J., Paytan, Adina, Pedrosa‐Pamies, Rut, Petrova, Mariia V., Rahman, Shaily, Robinson, Laura F., Roy‐Barman, Matthieu, Sanchez‐Vidal, Anna, Shiller, Alan, Tagliabue, Alessandro, Tessin, Allyson C., van Hulten, Marco, Zhang, Jing
Format:	Artikel
Sprache:	eng
Schlagworte:	Barium Bottom currents Calcium Calcium carbonate Calcium carbonates carbon cycle Carbonates Composition Continental interfaces, environment Deep sea Estimates Fluctuations Fluxes Global climate Iron marine atlas Mercury Mercury (metal) Ocean currents Ocean floor Ocean, Atmosphere Oceans Opal Organic carbon Productivity Sciences of the Universe Sea currents Sediment sediment burial Sediment composition Sediments Silicon Total organic carbon Uncertainty Weathering
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