TY - JOUR
T1 - Refining C. wuellerstorfi and H. elegans Mg/Ca temperature calibrations
AU - Lo Giudice Cappelli, Elena
AU - Regenberg, Marcus
AU - Holbourn, Ann
AU - Kuhnt, Wolfgang
AU - Garbe-Schoenberg, Dieter
AU - Andersen, Nils
N1 - Funding for this research was provided by the Marie Curie Action Plan, Seventh Framework Program (Grant no. 237922) and BMBF Grants 03G0217A (MAJA) and 03G0185A (VITAL).
PY - 2015/12
Y1 - 2015/12
N2 - We present core top Mg/Ca, Sr/Ca and δ18O measurements for Cibicidoides wuellerstorfi and Hoeglundina elegans from the Timor Sea and the Makassar Strait, which span a bottom water temperature (BWT) range from 2 to 18 °C. In both species Mg/Ca ratios are positively and significantly correlated with BWT, while δ18O
measurements are significantly anti-correlated with BWT. Comparison of
calcification temperatures derived from Mg/Ca ratios and δ18O
measurements yield comparable results and closely match CTD-measured
temperatures. We integrate our results with previously published data
sets from the Atlantic, Indian and Pacific Oceans and provide
temperature calibration equations over the temperature range from 2 to
12 °C for H. elegans and from 0 to 10 °C for C. wuellerstorfi. We found geographical differences in the relation of benthic Mg/Ca ratios to BWT: C. wuellerstorfi
shows Mg/Ca sensitivity to BWT of 19% increase in Mg/Ca per °C for the
Atlantic Ocean and of 15% per °C for the Indian and Pacific Oceans. H. elegans
shows Mg/Ca sensitivity to BWT of 16% increase in Mg/Ca per °C for the
Atlantic Ocean and of 14% per °C for the Indian and Pacific Oceans. C. wuellerstorfi Sr/Ca variability appears to be mainly driven by carbonate ion saturation, whereas H. elegans Sr/Ca variability is closely linked to BWT in the compiled data sets from the Atlantic, Indian and Pacific Oceans.
AB - We present core top Mg/Ca, Sr/Ca and δ18O measurements for Cibicidoides wuellerstorfi and Hoeglundina elegans from the Timor Sea and the Makassar Strait, which span a bottom water temperature (BWT) range from 2 to 18 °C. In both species Mg/Ca ratios are positively and significantly correlated with BWT, while δ18O
measurements are significantly anti-correlated with BWT. Comparison of
calcification temperatures derived from Mg/Ca ratios and δ18O
measurements yield comparable results and closely match CTD-measured
temperatures. We integrate our results with previously published data
sets from the Atlantic, Indian and Pacific Oceans and provide
temperature calibration equations over the temperature range from 2 to
12 °C for H. elegans and from 0 to 10 °C for C. wuellerstorfi. We found geographical differences in the relation of benthic Mg/Ca ratios to BWT: C. wuellerstorfi
shows Mg/Ca sensitivity to BWT of 19% increase in Mg/Ca per °C for the
Atlantic Ocean and of 15% per °C for the Indian and Pacific Oceans. H. elegans
shows Mg/Ca sensitivity to BWT of 16% increase in Mg/Ca per °C for the
Atlantic Ocean and of 14% per °C for the Indian and Pacific Oceans. C. wuellerstorfi Sr/Ca variability appears to be mainly driven by carbonate ion saturation, whereas H. elegans Sr/Ca variability is closely linked to BWT in the compiled data sets from the Atlantic, Indian and Pacific Oceans.
KW - Hoeglundina elegans
KW - Cibicidoides wullerstorfi
KW - Mg/Ca paleothermometry
KW - Carbonate ion effect
KW - Core top calibration
KW - Timor Sea
KW - Makassar Strait
KW - Indonesia
U2 - 10.1016/j.marmicro.2015.10.001
DO - 10.1016/j.marmicro.2015.10.001
M3 - Article
SN - 0377-8398
VL - 121
SP - 70
EP - 84
JO - Marine Micropaleontology
JF - Marine Micropaleontology
ER -