
"Nick" Shackleton
'Sir Nicholas John Shackleton'
FRS (
23 June 1937—
24 January 2006) was a
British geologist and
climatologist who specialised in the
Quaternary Period. He was the great-nephew of the explorer
Ernest Shackleton and the son of the noted geologist
Robert Millner Shackleton.
He earned a
bachelor's degree in physics and a
Ph.D. in geochemistry from
Clare College,
University of Cambridge. He spent his entire career there, eventually becoming a Professor in the
Department of Earth Sciences, working in the
Godwin Institute for Quaternary Research.

The Glacial effect describes the change of the oxygen isotope composition of sea water, due to growing ice sheets in high latitudes during glacials.
Shackleton was a key figure in the field of
palaeoceanography, and was a pioneer in the use of
mass spectrometry to determine changes in climate as recorded in the
oxygen isotope composition of calcareous microfossils. He also found evidence that the earth's last magnetic field reversal was 780,000 years ago. He is probably best known for his contribution to the "Hays, Imbrie and Shackleton" paper in
Science in 1976 which, using ocean sediment cores, 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, a method which allows a far greater level of stratigraphic precision than other dating methods, and also helped to clarify the rates and mechanisms of aspects of climate change.
In September 2000 he published an innovative study of the relationship between the oxygen isotope record of the oceans and isotope records obtained from the ice in Antarctica (glacial effect). This helped to pin down the relative contribution of deep water temperature changes and ice volume changes to the marine isotopic record, and also highlighted the close interdependency between carbon dioxide levels and temperature change over the last 400,000 years.
In 1995 became the director of the Godwin Institute of Quaternary Research. In 1998, he was knighted for his contributions to science. From 1999 to 2003 he was president of the
International Union for Quaternary Research (INQUA). He also had a fine collection of early
clarinets and other
woodwind instruments, which he played and studied.
Awards
★ Fellow of the
Royal Society since 1985
★
Crafoord Prize (1995) jointly with
Willi Dansgaard
★
Wollaston Medal (1996)
★ Knighted in 1998
★ Milankovitch Medal (1999)
★ Vetlesen Prize (2004)
★ Blue Planet Prize (2005)
References
★ Brozan, Nadine (February 12, 2006).
Sir Nicholas Shackleton, Geologist, Is Dead at 68. ''
New York Times''
External links
★
A special issue of Quaternary Science Reviews dedicated to Nick Shackleton; includes several articles by and about him, as well as a complete list of his publications.
★
Nicholas Shackleton
★
Tributes