Hey all,
I am working with soft tissue decay experiments under different abiotic conditions. One parameter is the temperature, that is shifted to 4 °C. Under 24 °C we saw calcite precipitation and under 4 °C not which is obvious because calcite precipitation is an endothermic reaction. I just wonder why there is also calcite precipitation in arctic lakes or why molluscs e.g. are able to form their calciumcarbonate shelvs in cold water?
Has anyone of you literature recommendations where this topic is discussed? Or where other parameter enabling calcite precipitation at that temperature are named?
That would be quite interesting and you would help me a lot :)
Best,
Kathrin