Foraminiferal tests are a common component of many marine sediments. The oxygen
isotope ratio (δ18O) of test calcite is frequently used to reconstruct aspects of their life …

We reconstruct trends in ice volume and deep ocean temperature for the past 108 Myr,
resolving variations on timescales of∼ 2 Myr and longer. We use a sea level record as a …

Stable isotopes in the calcium carbonate of benthic foraminifera provide important
paleoenvironmental information about seawater/sedimentary porewaters that these …

Partition coefficients of Mg and Sr (K Mg and K Sr) between calcite and fluid were
determined in crystals grown under different rates (V), where V is defined as the crystal …

Until recently, the process of denitrification (conversion of nitrate or nitrite to gaseous
products) was thought to be performed exclusively by prokaryotes and fungi. The finding that …

Insights into past marine carbon cycling and water mass properties can be obtained by
means of geochemical proxies calibrated through controlled laboratory experiments with …

Biological activity introduces variability in element incorporation during calcification and
thereby decreases the precision and accuracy when using foraminifera as geochemical …

Shelf and coastal regions are exceptionally important for many countries as they provide the
main habitat for many economically important fish and shellfish species. With ongoing …

In the context of recent climate change and increased anthropogenic activities in coastal
areas, which both may have a negative impact on dissolved oxygen concentration, there is …

Ocean chemistry is changing as a result of human activities. Atmospheric carbon dioxide
(CO2) concentrations are increasing, causing an increase in oceanic p CO2 that drives a …