Data of Figs. 6 and 8 in Legendre (2024, Jigsaw puzzle of the interwoven biologically-driven ocean carbon pumps. Progress in Oceanography)

Figure 6. Depth variations of carbon-pump components considering only gravitational POC export (i.e., Forg calculated using eqs. 10 and 18 and eq 1 of Martin et al., 1987, with b = 0.86): carbon fluxes at different depths z, and cumulative carbon fluxes from zexp to z. Figure 8. Cumulative carbon-pump fluxes from Fig. 6 are added together showing that [Forg(z) + ∑FseqDIC + ∑FupDIC] = [Forg(z) + ∑FwcDIC] = Fexp. The different curves are added together (a) from left to right, and (b) from the centre to the left and the right.图6：仅考虑重力驱动颗粒有机碳（Particulate Organic Carbon, POC）输出时，碳泵各组分的深度变化特征（即Forg通过公式10、公式18以及Martin等1987年的公式1计算得到，其中参数b=0.86）：涵盖不同深度z处的碳通量，以及从zexp至z的累积碳通量。 图8：将图6中的碳泵累积通量求和后可得如下等式：[Forg(z) + ∑FseqDIC + ∑FupDIC] = [Forg(z) + ∑FwcDIC] = Fexp。各曲线的累加方式分别为：(a) 从左至右；(b) 以中心点为起点分别向左、向右累加。