2015 GSA Annual Meeting in Baltimore, Maryland, USA (1-4 November 2015)

Paper No. 255-2
Presentation Time: 2:05 PM

FORAM FARMING: CALIBRATING BENTHIC FORAM MG/CA FOR SECULAR VARIATION IN SEAWATER MG/CA THROUGH CULTURE EXPERIMENTS


HASIUK, Franciszek, Geological and Atmospheric Sciences, Iowa State Unversity, 253 Science I, Ames, IA 50011 and JENNINGS, Deserae, Geological and Atmospheric Sciences, Iowa State University, 253 Science I, Ames, IA 50011, franek@iastate.edu

Foraminiferal Mg/Ca has been commonly used as a proxy for Quaternary seawater temperature. However, uncertainty about 1) the secular variation of seawater Mg/Ca and 2) how foraminiferal calcite responds to changing seawater Mg/Ca has precluded its widespread use across deeper time. This proxy has a second allure in that Mg/Ca-based paleotemperatures can be matched with contemporaneous foraminiferal δ18O to estimate paleo-seawater δ18O, which is a proxy for continental ice volume.

Four studies over the last decade has aimed to reduce this uncertainty by culturing foraminifera in waters of varying Mg/Ca and temperature. This study reports on success in establishing a long-term colony of the HMC benthic foraminifer Peneroplis planatus from Abu Dhabi and Qatar in Iowa, USA. Specimens are kept in independent colony reservoirs that are attached to a 650 L recirculating system utilizing artificial seawater. The system has been operational for 19 months.

Peneroplids from this system have been successfully grown under experimental conditions in water Mg/Ca from 1 to 8 at 25°C for 42 days (3-5 chambers of new growth) in sealed glass jars. Attempts to grow P. planatus below 25°C and in Mg/Ca less than 1 were not successful. Peneroplid calcite was analyzed via electron microprobe. Low-resolution, qualitative maps allowed quantitative spots to avoid areas of anomalously high or low Mg/Ca. Quantative analyses were performed with a 5 µm spots on experimentally grown calcite. Mg/Ca in new chambers gradually changed to reflect experimental conditions. Mg/Ca of the third chamber of new growth was taken to represent equilibrium with seawater Mg/Ca. Foram Mg/Ca vs. seawater Mg/Ca was best fit by the function: Foram Mg/Ca = 0.05 (Seawater Mg/Ca) ^ 0.56. This model is very similar to the only other model reported for a HMC benthic foraminifer, Operculina ammonoides.

This calibration can be used to model how the depositonal chemistry of HMC foraminifera changes with response to changing seawater Mg/Ca. For example, a peneroplid growing in the modern ocean (Mg/Ca = 5.2 mol/mol) precipitates a test with Mg/Ca = 132 mmol/mol. Growing in late Cretaceous seawater (Mg/Ca = 1 mol/mol), it would have a test Mg/Ca of 50 mmol/mol. In comparison, a LMC foram would only vary from 3 to 1 mol/mol from the modern ocean’s Mg/Ca to that of the Cretaceous.