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. Author manuscript; available in PMC: 2018 Feb 28.
Published in final edited form as: Nature. 2017 Aug 30;548(7669):573–577. doi: 10.1038/nature23646

Extended Data Table 1. Key results from individual model runs.

(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).

a
Experiment ID experimental assumptions peak emissions cumulative emissions cumulative Corg burial ΔSST peak excess weathering
age model δ11B envelope smoothed data? weathering? Corg burial? (PgC yr-1) total (PgC) mean δ13C ‰ total (PgC) mean δ13C ‰ (°C) (PgC yr-1)
R07sm_HI R07 high YES YES NO 0.41 5,688 -18.9 --- --- 2.25 0.030
R07sm R07 mean YES YES NO 0.58 10,213 -11.1 --- --- 3.64 0.053
R07sm_LO R07 low YES YES NO 1.16 19,964 -6.6 --- --- 5.99 0.105

FEsm_HI FE high YES YES NO 0.17 6,502 -16.5 --- --- 2.10 0.038
FEsm FE mean YES YES NO 0.36 12,020 -9.8 --- --- 3.09 0.069
FEsm_LO FE low YES YES NO 0.64 24,124 -6.0 --- --- 4.80 0.132

R07rw R07 mean NO YES NO 0.61 10,984 -12.1 --- --- 4.07 0.061
FErw FE mean NO YES NO 0.45 12,749 -10.2 --- --- 3.14 0.072

R07sm_noW R07 mean YES NO NO 0.52 6,407 -16.7 --- --- 3.34 ---
FEsm_noW FE mean YES NO NO 0.30 6,665 -16.4 --- --- 2.72 ---

R07sm_HI_Corg R07 high YES YES YES 0.41 7,670 -18.0 2,607 -30.0 2.25 0.030
R07sm_Corg R07 mean YES YES YES 0.58 12,220 -10.9 2,540 -30.5 3.64 0.053
R07sm_LO_Corg R07 low YES YES YES 1.16 22,593 -7.1 3,333 -30.9 5.99 0.105
b
Duration of onset (yr) peak emissions cumulative emissions over onset cumulative emissions @ 20,000 yr cumulative emissions @ 50,000 yr
(PgC yr-1) total (PgC) mean δ13C (‰) total (PgC) mean δ13C (‰) total (PgC) mean δ13C (‰)
100 20.00 1,897 -19.0 8,695 -17.0 13,256 -13.4
200 15.21 2,355 -18.4 8,688 -17.0 13,252 -13.4
500 6.90 2,588 -21.5 8,664 -17.0 13,239 -13.6
1,000 3.72 2,799 -24.5 8,613 -17.1 13,200 -13.4
2,000 2.08 3,074 -27.6 8,526 -17.2 13,181 -13.4
5,000 1.07 3,751 -29.0 8,202 -17.8 13,007 -13.5
10,000 0.70 4,691 -26.3 7,612 -18.8 12,706 -13.6
20,000 0.48 6,141 -22.0 6,141 -22.0 12,025 -14.0