Fig. 2 | Nature Communications

Fig. 2

From: Coupling of oceanic carbon and nitrogen facilitates spatially resolved quantitative reconstruction of nitrate inventories

Fig. 2

Distribution of NO3- and δ13CDIC in the modern Pacific and [NO3]-δ13CDIC-coupling in the intermediate Pacific - modern and downcore. All data for the modern Pacific have been taken from the GLODAPv2 database34. a Distribution of [NO3] in the modern Pacific34. b Distribution of δ13C of dissolved inorganic carbon (DIC; δ13CDIC) in the modern Pacific34. The Ocean Data View software has been used to compile these plots62. c Correlation between [NO3] and δ13CDIC in intermediate water depths (700–2000 m) of the modern Pacific (red, N = 4779) and between [NO3]BW and δ13CFORAM in the sediment record of M77/2 52-2 (black, N = 44). Both linear regressions neither differ significantly in slope (P = 0.15) nor in intercept (P = 0.13). Due to graphical reasons all δ13C below −1‰ have been cut in this plot, although they were included into the fit. For a complete plot of all data points see Supplementary Figure 4B

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