(a) age model Kroon D, Williams T, Pirmez C, Spezzaferri S, Sato T, Wright JD. Coupled Early Pliocene-Middle Miocene bio-cyclostratigrahy of Site 1006 reveals orbitally induced cyclicity patterns of Great Bahama Bank carbonate production. Proc ODP, Scientific Results 166, 155-166 (2000).(b) corrected to Tanaka T, et al. Jndi-1: a neodymium isotopic reference in consistency with LaJolla neodymium. Chemical Geology 168, 279-281 (2000).(c) corrected for ingrowth of 143Nd using Sm/Nd ratio of 0.139 for foraminiferal calcite Osborne AH, Hathorne EC, Schijf J, Plancherel Y, Boning P, Frank M. The potential of sedimentary foraminiferal rare earth element patterns to trace water masses in the past. Geochemistry Geophysics Geosystems 18, 1550-1568 (2017).(d) corrected for ingrowth of 143Nd using Sm/Nd ratio of 0.109 for detrital material, based on the average upper crustal ratio Taylor SR, McLennan SM. The Continental Crust: Its Composition and Evolution. Blackwell Scientific Publications (1985).
; Störling, Tjördis; Frank, Martin