Table 1. δ13C of atmospheric CO2 (New Zealand to Antarctica, 2004–2005)
[i] aAfter correction for the N2O effect.
[ii] bThese values are only rough evaluations of the CO2 concentrations calculated from the CO2 pressure of each sample in the source of the mass spectrometer.
Fig. 1.
δ13C values of the CO2 from discrete air samples collected between New Zealand and Antarctica during four cruises between 1998–1999 and 2003–2004. These results were already reported by Longinelli et al. (2007).

Fig. 2.
Routes of the M/V Italica between New Zealand and Antarctica along which flask air samples were collected during eight cruises between 1997 and 2010. Atmospheric CO2 concentrations were measured during 1998–1999, 2003–2004, 2005–2006, 2009 and 2010 cruises.

Fig. 3.
(a) δ13C of atmospheric CO2 from flask air samples collected between New Zealand and Antarctica during 2004–2005 cruise. CO2 concentrations could not be measured during this cruise. (b) δ13C of atmospheric CO2 from flask air samples (2004–2005 cruise). CO2 concentrations in each sample were roughly evaluated from CO2 gas pressure of each sample in the mass spectrometer source, after calibration with known CO2 volumes.

Table 2. δ13C of atmospheric CO2 (New Zealand to Antarctica, 2006)
[i] aAfter correction for the N2O effect.
Fig. 4.
δ13C of atmospheric CO2 from flask air samples collected between New Zealand and Antarctica during 2005–2006 cruise.

Table 3. δ13C of atmospheric CO2 (New Zealand to Antarctica, 2009)
[i] aAfter correction for the N2O effect.
Fig. 5.
δ13C of atmospheric CO2 from flask air samples collected between New Zealand and Antarctica during five cruises between 1998–1999 and 2005–2006.

Fig. 6.
δ13C of atmospheric CO2 from flask air samples and CO2 concentrations measured between New Zealand and Antarctica in December 2009.

Fig. 7.
δ13C of atmospheric CO2 from flask air samples and CO2 concentrations measured between New Zealand and Antarctica in January 2010.

Table 4. δ13C of atmospheric CO2 (New Zealand to Antarctica, 2010)
[i] aAfter correction for the N2O effect.
