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. 2018 Sep 3;376(2130):20170072. doi: 10.1098/rsta.2017.0072

Table 1.

Average planktonic foraminiferal B/Ca and δ11B data during the PETM.

average B/Ca µmol mol−1a
core site species below CIE onset CIE core post-CIE ΔB/Cab
1209 M. velascoensis 70.4 44.5 62.7 25.9
1209 A. soldadoensis 71.0 43.9 53.5 27.1
401 M. subbotinae 51.9 51.4 52.6 0.5
689 Acarinina spp. 49.3 29.8 49.2 19.5
690 Acarinina spp. 53.4 37.0 52.7 16.4
Bass River Acarinina spp. 65.0 40.0 48.0 25.0
Bass River Morozovella spp. 42.0 45.0
Ancora Acarinina spp. 38.0 65.0
Ancora Morozovella spp. 51.0 58.0
1209 Subbotina spp. 46.0 31.3 37.5 14.8
689 Subbotina spp. 37.3 24.9 39.2 12.4
690 Subbotina spp. 45.3 33.8 42.6 11.5
Bass River Subbotina spp. 57.0 40.0 42.0 17.0
Ancora Subbotina spp. 51.0 38.0 49.0 13.0
average δ11B (‰)a Δδ11B (‰)b
1209 M. velascoensis 15.5 14.7 15.3 0.9
401 M. subbotinae 14.7 14.0 14.3 0.7
Bass River Subbotina spp. 13.5 12.5 1.1
Millville Subbotina spp. 12.7

aThe onset of the CIE is identified as the initial decrease in δ13C, core CIE is an interval of sustained low δ13C values (less than 70 kyr) and the post-CIE interval represents the recovery of δ13C to values below the CIE onset (70–200 kyr) (figure 2d).

bDifference between average values prior to the CIE onset and the CIE core interval.