The way plankton absorbed
oxygen at a given temperature mattered less than what proportion of each isotope was available in the sea water as ice sheets came and went.
Not exact matches
Dust found in the ice
gives a record of what was in the air thousands of years ago, whether from volcanic eruptions or human activity, and the isotopic composition of the hydrogen and
oxygen molecules in the snow
give a record of the
temperature of the earth
at the time.
The AGWSF has
given that -18 °C figure to its claim that this would be the
temperature only without its «greenhouse gases», but, in real world physics that is the
temperature for the Earth without any atmosphere
at all, that is, without any nitrogen or
oxygen too.
Temperatures aloft can be measured in a number of ways, two of which are useful for climate monitoring: by radiosondes (balloon - borne instrument packages, including thermometers, released daily or twice daily
at a network of observing stations throughout the world), and by satellite measurements of microwave radiation emitted by
oxygen gas in the lower to mid-troposphere, taken with an instrument known as the Microwave Sounding Unit (MSU).5 The balloon measurements are taken
at the same Greenwich mean times each day, whereas the times of day of the satellite measurements for a
given location drift slowly with changes in the satellite orbits.
They measure the hydrogen and
oxygen isotopes to infer air
temperatures at the time the snow fell, and the dust particles
give a nice indication of the dusty periods (much of the dust was kicked up far away, in the Gobi Desert, rather than from sources closer to Greenland).