Birth and Growth of Minerals from Aqueous Solutions, February 2025, Vol. 21, No. 1
April 17, 2025
Biomineral Geochemistry: Windows into Past Climates and Calcification, April 2025, Vol. 21, No. 2
$20.00
Marine calcium carbonate biominerals, especially the shells and skeletons produced by molluscs, corals, and the immeasurably numerous calcifying phytoplankton and zooplankton, are of both societal and environmental importance for two key reasons. Firstly, the mineralised remains of these organisms are one of the largest longterm sinks of carbon on Earth’s surface. Secondly, and perhaps more practically, the (trace) element and isotopic composition of these biominerals probably represents the most widely applied tool for quantitatively reconstructing past environmental conditions on timescales from days to millions of years.
Biomineral Geochemistry: Windows into Past Climates and Calcification
April 2025, Vol. 21, No. 2
Marine calcium carbonate biominerals, especially the shells and skeletons produced by molluscs, corals, and the immeasurably numerous calcifying phytoplankton and zooplankton, are of both societal and environmental importance for two key reasons. Firstly, the mineralised remains of these organisms are one of the largest longterm sinks of carbon on Earth’s surface. Secondly, and perhaps more practically, the (trace) element and isotopic composition of these biominerals probably represents the most widely applied tool for quantitatively reconstructing past environmental conditions on timescales from days to millions of years. It has been known for some time that the processes of biomineralisation imprint on these ‘proxy’ systems, shifting their behaviour away from thermodynamic equilibrium, such that they typically require empirical calibration to an environmental variable of interest.
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