Fig. 4 | Nature Communications

Fig. 4

From: Asynchrony between Antarctic temperature and CO2 associated with obliquity over the past 720,000 years

Fig. 4

Obliquity components of climate records and orbital parameters. a DF ΔTsite (thin red) and its obliquity component (red). b The obliquity component of ΔTsite (red), AMI at 77° S (yellow) and obliquity (black). c The obliquity component of ΔTsource (blue), AMI at 38–66° S (yellow) and obliquity (black). d The obliquity component of the CO2 composite record32 (green) and obliquity (black). e The obliquity component of benthic δ18O record40 and obliquity (black). f The obliquity component of ΔTgrad (purple), the insolation gradient between 77° S and 38–66° S (yellow) and obliquity (black, axis inverted). g The differences between the normalized obliquity component of ΔTsite and AMI at 77° S (red). h Orbital eccentricity (black) and precession (yellow). The insolation curves are shown behind the obliquity variations. The obliquity components were calculated using a bandpass filter (Methods)

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