Moreno, A., Perez, A., Frigola, J., Nieto-Moreno, V., Rodrigo-Gamiz, M., Martrat, B., Gonzalez-Samperiz, P., Morellon, M., Martin-Puertas, C., Corella, J. P., Belmonte, A., Sancho, C., Cacho, I., Herrera, G., Canals, M., Grimalt, J. O., Jimenez-Espejo, F., Martinez-Ruiz, F., Vegas-Vilarrubia, T. and Valero-Garces, B. L.: The Medieval Climate Anomaly in the Iberian Peninsula reconstructed from marine and lake records, Quaternary Science Reviews, 43, 16–32, doi:10.1016/j.quascirev.2012.04.007, 2012.

The Medieval Climate Anomaly in the Iberian Peninsula reconstructed from marine and lake records

The ?18O composition of foraminifera records both the oxygen isotopic composition of seawater (?18Oseawater) and the calcification temperature (through the kinetic fractionation effect) [Emiliani, 1955]. Shell ?18O and Mg/Ca calcification temperature values for G. ruber are substituted into the oxygen isotope paleotemperature equation [Shackleton, 1974] to solve the ?18Oseawater.

CLE2008: Cleroux et al., 2008 North Atlantic core top calibration for G. ruber (white); paleoData_units changed - was originally deg C; climateInterpretation_seasonality changed - was originally JJA; climateInterpretation_seasonality changed - was originally 6 7 2008

CLE2008: Cleroux et al., 2008 North Atlantic core top calibration for G. ruber (white)

d18Osw not estimated yet, also data for P. obliquiloculata, but not on pangaea

year (MATb9a6b77ab3): paleoData_isPrimary: '' has been replaced by 'TRUE'
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