"Table 2. Stable Isotope Composition, Calcification Depth, Calcification Temperatures," " Ambient d13Ceq, and Carbon Isotope Disequilibrium determined for N. pachyderma (s.) " Recovered from Surface and Last Glacial Sediments in the South Atlantic Ocean. Surface Sediments Core ID "Latitude,° S" d18O (per mille) d13C (per mille) d18O calc depth (m) Feb Tc (deg C) ambient preind. d13Ceq (per mil) Mackensen d13Ceq (per mille) preind (d13Ceq - d13Csh) PS2080-1** 41.72 3.08 0.59 1000 3.4 1.89 1.49 1.3 PS2106-1** 41.85 2.67 -0.53 700 4.01 2.43 2.03 2.96 RC11-83 41.53 1.4 0.63 200 9.22 2.87 2.47 2.24 RC15-94 43 0.85 0.41 150 11.48 2.96 2.36 2.55 V22-108 43.2 1.01 0.34 0 11.17 3.13 2.73 2.79 PS2082 43.3 1.32 0.3 50 10.45 3.08 2.64 2.78 PS1751-2** 44.49 2.86 0.99 900 2.78 1.93 1.49 0.94 PS2239-1 45.5 1.89 0.58 75 8.22 3.1 2.65 2.52 RC15-93 46.1 1.7 1 0 7.08 3.28 2.88 2.28 PS1754-1 46.1 2.09 0.86 10 7.73 3.25 2.8 2.39 PS2083-1 46.37 2.14 0.82 30 7.67 3.23 2.75 2.41 PS1754-2 46.77 2.32 0.97 87.5 6.5 3.08 2.65 2.11 RC11-80 46.8 1.71 0.89 0 8.34 3.32 2.92 2.43 Site 704 46.88 2.21 0.89 40 7.27 3.21 2.7 2.32 PS2084-2 47.02 2.4 0.9 62.5 6.4 3.15 2.64 2.25 PS2241-1 47.4 1.9 0.81 0 7.4 3.32 2.92 2.51 PS2085-1 47.75 2.24 1.14 40 6.95 3.19 2.67 2.05 V29-105 48.1 2.26 0.79 0 5.13 3.29 2.89 2.5 PS2086-3 48.32 2.47 0.85 0 6.01 3.25 2.83 2.4 RC13-254 48.5 2.5 1.09 62.5 5.93 3.1 2.6 2.01 PS1756-6 48.9 2.88 1.06 62.5 5.81 3.06 2.57 2 PS2087-1 49.13 2.59 1.11 0 5.6 3.19 2.76 2.08 PS2242-1 49.98 2.8 1.04 87.5 4.22 2.95 2.47 1.91 V29-104 50 2.52 1.21 0 4.24 3.04 2.58 1.83 PS1759-1 50.15 2.87 0.85 75 3.9 2.96 2.48 2.11 PS1654-1 50.16 2.84 1.14 70 4.02 2.97 2.48 1.83 RC13-255 50.5 2.65 1.09 0 4.77 2.97 2.5 1.88 RC13-275 50.8 2.87 1.1 0 3.53 2.9 2.42 1.8 PS1768-8 51.93 3.1 0.69 87.5 2.72 2.75 2.25 2.06 RC13-271 52 2.8 0.85 0 4.09 2.8 2.3 1.95 CHN155-36PG 52.4 3.26 1.29 75 1.82 2.68 2.2 1.39 RC13-269 52.6 2.83 0.92 2.95 2.73 2.26 1.81 RC13-256 53.1 2.97 0.99 300 1.52 2.19 1.53 1.2 CHN115-26PG 53.6 3.05 1.04 250 1.26 2.1 1.62 1.06 RC13-262 53.8 2.83 0.77 500 2.01 2.01 1.46 1.24 RC13-263 53.8 2.84 0.78 500 2.01 2.01 1.46 1.23 MD82424 54.1 3.59 0.92 87.5 0.2 2.48 2.11 1.56 CHN115-27PG 54.6 3.28 1.05 200 0.69 1.96 1.62 0.91 AII107 22GGC 54.8 3.38 0.99 175 0.11 2.04 1.77 1.05 IO1578-5 60 4.22 0.27 1.45 1.28 1.18 *M269-965 60.9 3.2 0.8 10 2.24 2.25 2.23 *1.43 *KG3 62.37 3.27 0.35 300 0.04 1.4 1.38 *1.03 *WS-1 62.44 3.42 0.32 150 -0.63 1.79 1.48 *1.16 *WS-3 64.89 3.28 0.53 150 0.02 1.78 1.45 *0.92 *WS-2 64.92 3.35 0.44 137.5 -0.42 1.87 1.54 *1.10 PS1387 68.5 3.9 0.6 0 0.19 1.74 1.64 1.14 PS1506 68.66 3.51 0.91 112.5 -0.83 1.69 1.59 0.78 PS1388 69 3.5 0.2 112.5 -0.83 1.68 1.59 1.48 PS1648 69.5 3.5 0.6 137.5 -0.66 1.62 1.47 1.02 PS1431 69.5 3.5 0.7 137.5 -0.72 1.62 1.47 0.92 PS1394 70 3.4 0.5 175 -0.27 1.52 1.38 1.02 PS1481 71 3.3 0.5 400 -0.07 1.45 1.35 0.95 Glacial values Core ID "Latitude, ° S" d18O d13C RC12-267 38.8 1.92 -0.81 RC11-83 41.6 2.66 -0.67 RC15-94 43 2.51 -0.36 V22-108 43.2 2.86 -0.42 PS2082 43.3 3.37 -0.37 RC15-93 46.1 2.59 0.59 PS1754-1 46.1 3.19 0.44 RC11-80 46.8 2.85 0.36 Site 704 46.88 3.32 0.44 RC13-254 48.5 3.62 0.22 RC13-275 50.8 4.35 0 PS1768-8 51.93 4.56 -0.35 RC13-271 52 4.31 -0.1 RC13-269 52.6 4.25 -0.1 RC13-259 53.88 4.07 -0.25 PS1387 68.5 4.9 -0.2 PS1506 68.66 4.87 0.21 PS1388 69 4.8 0 PS1648 69.5 5 0 PS1431 69.5 4.9 0.2 PS1394 70 4.9 0 PS1481 71 4.6 0 * indicates sediment trap samples. ** indicate values that are not considered in analysis because they are believed not representative of modern sediments due to loss of surface sediments during coring. Blank spaces indicate places where data were not available in the publication. "Tc = calcification temperature, or ambient temperature at the apparent calcification " depth determined from d18Oshell (Section 5.1). Ambient pre-industrial d13Ceq was also estimated at the apparent calcification depth determined from d18Oshell. Pre-industrial values for d13Ceq were estimated as described text. (d13Ceq - d13Csh) = carbon isotope disequilibrium. Disequilibrium values with * were not corrected to pre-industrial d13Ceq.