Modern and Cenozoic records of seawater magnesium from foraminiferal Mg isotopes
Magnesium is an element critically involved in the carbon cycle, because weathering of Ca-Mg silicates removes atmospheric CO<sub>2</sub> into rivers, and formation of Ca-Mg carbonates in the oceans removes carbon from the ocean-atmosphere system. Hence the Mg cycle holds the potential t...
Main Authors: | P. A. E. Pogge von Strandmann, J. Forshaw, D. N. Schmidt |
---|---|
Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2014-09-01
|
Series: | Biogeosciences |
Online Access: | http://www.biogeosciences.net/11/5155/2014/bg-11-5155-2014.pdf |
Similar Items
-
Boron and magnesium isotopic composition of seawater
by: Foster, G.L, et al.
Published: (2010) - Lithium Isotope Evolution of Cenozoic Seawater
- The Magnesium Isotopic Composition of Cenozoic Foraminifera
-
Cenozoic global cooling and increased seawater Mg/Ca via reduced reverse weathering
by: Ann G. Dunlea, et al.
Published: (2017-10-01) -
Planktonic Foraminiferal Isotopic Records of Gutingken Formation at Shoushan, Kaohsiung
by: Wen-chien Tseng, et al.
Published: (2004)