The potential of 230 Th for detection of ocean acidification impacts on pelagic carbonate production

Concentrations of dissolved 230Th in the ocean water column increase with depth due to scavenging and downward particle flux. Due to the 230Th scavenging process, any change in the calcium carbonate (CaCO3) fraction of the marine particle flux due to changes in biological CaCO3 hard-shell production...

Ausführliche Beschreibung

Gespeichert in:

Bibliographische Detailangaben
Veröffentlicht in:	Biogeosciences 2018-06, Vol.15 (11), p.3521-3539
Hauptverfasser:	Heinze, Christoph, Ilyina, Tatiana, Gehlen, Marion
Format:	Artikel
Sprache:	eng
Schlagworte:	Acidification Alkalinity Biogeochemistry Calcium Calcium carbonate Calcium carbonates Carbonates Clay Computer simulation Detection Exports Fluxes General circulation models Greenhouse effect Greenhouse gases Ocean acidification Oceans Organic carbon Particle settling Particulate organic carbon Reduction Scavenging Scavenging processes Sea surface Temperature (air-sea) Water column Water depth
Online-Zugang:	Volltext
Tags:	Tag hinzufügen Keine Tags, Fügen Sie den ersten Tag hinzu!

Schreiben Sie den ersten Kommentar!