(a) Summary of the main double inversion experiments carried out. The
terminology “R07” refers to configurations tying the Site 401
records to the chronostratigraphy of ref. 25, the notation “FE” refers to the
3He-based age model of ref. 57). Annotation “sm” refers to inversion of analytically
smoothed δ13C and pH data sets, “rw” to usage of
original sample data for double inversions. “HI” and
“LO” represent potentially extreme configurations taking into
account the boron proxy uncertainty at 95% confidence level. “noW”
has silicate (and carbonate) weathering feedbacks disabled. “Corg”
denote model configurations that allow removal of excess organic carbon from the
surface ocean. Grey shading highlights experiments focussed upon in the main
text and plotted in Figure 3
(“R07sm” in Fig. 3a-f and
“R07sm_Corg” in 3i-n.). Note: (1) peak emissions are binned at 2
kyr resolution, (2) both cumulative emissions and Corg burial are
measured from 40 to 190 ka model time, and (3) peak excess weathering reflects
carbon removal due to silicate weathering above pre-PETM weathering rates. (b)
Summary table presenting the results of sensitivity experiments (shown in Extended Data Fig. 5) to quantify the
importance of uncertainties in the age model for the CIE onset. In these
experiments, the CIE onset phase is assumed to occur linearly, with a duration
of the decline in δ13C and pH varying from 100 to 20,000 yr
duration. Reported are: (1) diagnosed peak carbon emissions, (2) cumulative
carbon emissions occurring over the duration of the onset, and mean (flux
weighted) δ13C of these emissions, (3) cumulative carbon
emissions occurring at the 20 kyr time horizon – comparable to the onset
duration in our assumed age model, plus the mean (flux weighted)
δ13C of these emissions, and (4) the cumulative carbon
emissions occurring at the 20 kyr horizon, plus the mean (flux weighted)
δ13C of these emissions. Note that in all experiments,
once the onset is complete, the target pH and δ13C values are
held constant (and low) until the end of the experiment (50,000 yr).