Sir Nicholas John Shackleton FRS[1] (23 June 1937 – 24 January 2006) was an English geologist and paleoclimatologist who specialised in the Quaternary Period.
Apart from periods abroad as Visiting Professor or Research Associate, Shackleton's entire scientific career was spent at Cambridge.
He became internationally known, in 1976, with the publication of a paper, with James Hays and John Imbrie, in Science entitled "Variations in the Earth's orbit: Pacemaker of the ice ages".
[5] Using ocean sediment cores, Shackleton, Hays and Imbrie demonstrated that oscillations in climate over the past few million years could be correlated with variations in the orbital and positional relationship between the Earth and the Sun (see Milankovitch cycles).
Much of Shackleton's later work focused on constructing precise timescales based on matching the periodic cycles in deep-sea sediment cores to calculations of incoming sunlight at particular latitudes over geological time.
In addition to his reputation in the scientific world, Shackleton was highly respected by many musicians, and a friend to many who studied at Cambridge, including Christopher Hogwood who lodged with him for several years.