Fig. 4: Plots of the oxygen isotope composition versus the δ56Fe of I-type cosmic spherules.
From: Traces of the oxygen isotope composition of ancient air in fossilized cosmic dust

Displayed are the δ18O (A) and Δ’17O (B) versus δ56Fe of the spherules investigated in this study, together with modern I-type cosmic spherules that are displayed as ref. 11 (gray triangles). The relation between oxygen and iron isotopes of modern I-type cosmic spherules from Fischer et al.11 is represented as gray solid curves. The oxygen isotope composition of modern atmospheric O2 is shown for comparison at a pre-evaporative δ56Fe of 0‰. The vertical offset of sample MDC-A5 in Δ’17O (B) is depicted with a grey dashed arrow. Error bars for oxygen isotopes are 1SD and for δ56Fe they are 2SD.