Publication Date:
2024-02-02
Description:
Benthic foraminiferal surface porosity (the mean percentage of surface area covered by pores; higher porosity: lower oxygenation) and iodine to calcium ratio (I/Ca, higher I/Ca: higher oxygenation) are both promising paleoceanographic proxies that will advance through testing in down-core studies. Here we report the first down-core comparison (~45 kyr) of these proxies for a core from the southern Brazilian margin (26°40.22′ S, 46°26.46′ W, 475 m water depth). Both proxies are most sensitive to low-O~2~ conditions (〈 50 µmol/kg), and not well-constrained at higher O~2~ concentrations. Porosity values are generally low (〈 15%) and I/Ca ranges between ~4 and ~6 µmol/mol throughout the core. The two proxies are overall consistent, suggesting that bottom-water oxygen concentrations at the site remained above 50 µmol/kg during the last 45 kyr. Several non-O~2~ factors (e.g., iodate reduction rates, water mass mixing, temperature, foraminiferal shell robustness) could influence the proxies and require further investigation.
Keywords:
AGE; Cibicidoides pseudoungerianus; Cibicidoides pseudoungerianus, Iodine/Calcium ratio; Cibicidoides pseudoungerianus, Iodine/Calcium ratio, standard deviation; Cibicidoides pseudoungerianus, porosity; Cibicidoides pseudoungerianus, porosity, standard deviation; Cibicidoides wuellerstorfi; Cibicidoides wuellerstorfi, porosity; Cibicidoides wuellerstorfi, porosity, standard deviation; DEPTH, sediment/rock; GeoB6201-5; Glacial; Gravity corer (Kiel type); M46/2; Meteor (1986); Methane; Oxygen; SL; southern Brazilian margin
Type:
Dataset
Format:
text/tab-separated-values, 336 data points
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