Now I can do what I wanted to do which is to plot these different time scale processes on a common x-axis from the same starting point, limiting the cretaceous data to the first 500,000 years. Green is 1880-present, blue is Milankovitch, brown is ocean volcanic forcing during the cretacous. For comparison, I placed a rough slope on the upswing of the Milankovitch cycle, which came out to .00006 °C/year. And I see I made a mistake in typing the Cretaceous slope, which should be .000002 °C/yr. The ratios of the Cretaceous and Milankovitch slopes compared to the slope for the 1880-present data are ~5000 and 165 respectively.
View attachment 168
So in saying that the ∆°C from 1880 on is not outside temp anomoly in the past, that's right. But what grabs attention is the ∆time during which the change has happened. Viewed on a geologic time scale, the impression is of a instantaneous oxidation reaction of fixed carbon back to gas (ie an explosion), accompanied by the expected temperature change. So the planet has mechanisms to buffer temperature, but they typically work on a very different timescale. How that plays out for the current forcing perturbing the system is of course the big question.