Encyclopedia of Geobiology

2011 Edition
| Editors: Joachim Reitner, Volker Thiel

Divalent Earth Alkaline Cations in Seawater

  • Anton Eisenhauer
Reference work entry
DOI: https://doi.org/10.1007/978-1-4020-9212-1_75

Synonyms

Divalent cations in seawater

Definition

The most abundant divalent earth alkaline cations in seawater are Mg2+, Ca2+, and Sr2+ are simply termed the “divalent cations.” These ions and their dynamic change play a major role for the modern oceans. On long geological time scales dynamic changes of divalent cation concentrations in the oceans influenced the evolution of live and the climate evolution in the past.

Divalent cations in modern ocean water

Magnesium

Magnesium is a chemical element with the symbol Mg, the atomic number 12, and an atomic mass of 24.31. Magnesium is the ninth most abundant element in the universe by mass. It constitutes about 2% of the Earth’s crust by mass, and it is the third most abundant element dissolved in seawater and it is the most abundant divalent cation followed by Ca and Sr in seawater (Brown et al., 1992). Mg ions are essential to all living cells, and is the 11th most abundant element by mass in the human body. In seawater (S= 35 psu), Mg...

Keywords

Calcium Carbonate Divalent Cation Pacific Decadal Oscillation Great Barrier Reef Planktonic Foraminifera 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.
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Copyright information

© Springer Science+Business Media B.V. 2011

Authors and Affiliations

  • Anton Eisenhauer
    • 1
  1. 1.IFM-GEOMARLeibniz-Institut für Meereswissenschaften Christian Albrechts Universität zu KielKielGermany