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Inaugural Article

Sea level and global ice volumes from the Last Glacial Maximum to the Holocene

Kurt Lambeck, Hélène Rouby, Anthony Purcell, Yiying Sun, and Malcolm Sambridge
  1. aResearch School of Earth Sciences, The Australian National University, Canberra, ACT 0200, Australia;
  2. bLaboratoire de Géologie de l'École Normale Supérieure, UMR 8538 du CNRS, 75231 Paris, France; and
  3. cDepartment of Earth Sciences, University of Hong Kong, Hong Kong, China

See allHide authors and affiliations

PNAS October 28, 2014 111 (43) 15296-15303; first published October 13, 2014; https://doi.org/10.1073/pnas.1411762111
Kurt Lambeck
aResearch School of Earth Sciences, The Australian National University, Canberra, ACT 0200, Australia;
bLaboratoire de Géologie de l'École Normale Supérieure, UMR 8538 du CNRS, 75231 Paris, France; and
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  • For correspondence: kurt.lambeck@anu.edu.au
Hélène Rouby
aResearch School of Earth Sciences, The Australian National University, Canberra, ACT 0200, Australia;
bLaboratoire de Géologie de l'École Normale Supérieure, UMR 8538 du CNRS, 75231 Paris, France; and
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Anthony Purcell
aResearch School of Earth Sciences, The Australian National University, Canberra, ACT 0200, Australia;
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Yiying Sun
cDepartment of Earth Sciences, University of Hong Kong, Hong Kong, China
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Malcolm Sambridge
aResearch School of Earth Sciences, The Australian National University, Canberra, ACT 0200, Australia;
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  1. Contributed by Kurt Lambeck, September 12, 2014 (sent for review July 1, 2014; reviewed by Edouard Bard, Jerry X. Mitrovica, and Peter U. Clark)

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Significance

Several areas of earth science require knowledge of the fluctuations in sea level and ice volume through glacial cycles. These include understanding past ice sheets and providing boundary conditions for paleoclimate models, calibrating marine-sediment isotopic records, and providing the background signal for evaluating anthropogenic contributions to sea level. From ∼1,000 observations of sea level, allowing for isostatic and tectonic contributions, we have quantified the rise and fall in global ocean and ice volumes for the past 35,000 years. Of particular note is that during the ∼6,000 y up to the start of the recent rise ∼100−150 y ago, there is no evidence for global oscillations in sea level on time scales exceeding ∼200 y duration or 15−20 cm amplitude.

Abstract

The major cause of sea-level change during ice ages is the exchange of water between ice and ocean and the planet’s dynamic response to the changing surface load. Inversion of ∼1,000 observations for the past 35,000 y from localities far from former ice margins has provided new constraints on the fluctuation of ice volume in this interval. Key results are: (i) a rapid final fall in global sea level of ∼40 m in <2,000 y at the onset of the glacial maximum ∼30,000 y before present (30 ka BP); (ii) a slow fall to −134 m from 29 to 21 ka BP with a maximum grounded ice volume of ∼52 × 106 km3 greater than today; (iii) after an initial short duration rapid rise and a short interval of near-constant sea level, the main phase of deglaciation occurred from ∼16.5 ka BP to ∼8.2 ka BP at an average rate of rise of 12 m⋅ka−1 punctuated by periods of greater, particularly at 14.5–14.0 ka BP at ≥40 mm⋅y−1 (MWP-1A), and lesser, from 12.5 to 11.5 ka BP (Younger Dryas), rates; (iv) no evidence for a global MWP-1B event at ∼11.3 ka BP; and (v) a progressive decrease in the rate of rise from 8.2 ka to ∼2.5 ka BP, after which ocean volumes remained nearly constant until the renewed sea-level rise at 100–150 y ago, with no evidence of oscillations exceeding ∼15–20 cm in time intervals ≥200 y from 6 to 0.15 ka BP.

  • sea level
  • ice volumes
  • Last Glacial Maximum
  • Holocene

Footnotes

  • ↵1To whom correspondence should be addressed. Email: kurt.lambeck{at}anu.edu.au.
  • This contribution is part of the special series of Inaugural Articles by members of the National Academy of Sciences elected in 2009.

  • Author contributions: K.L. designed research; K.L., H.R., A.P., Y.S., and M.S. performed research; Y.S. contributed field data; K.L., H.R., A.P., Y.S., and M.S. analyzed data; K.L. and H.R. wrote the paper; and A.P. and M.S. developed software.

  • Reviewers: E.B., CEREGE; J.X.M., Harvard University; and P.U.C., Oregon State University.

  • The authors declare no conflict of interest.

  • This article contains supporting information online at www.pnas.org/lookup/suppl/doi:10.1073/pnas.1411762111/-/DCSupplemental.

Freely available online through the PNAS open access option.

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Sea level and ice volume since the glacial maximum
Kurt Lambeck, Hélène Rouby, Anthony Purcell, Yiying Sun, Malcolm Sambridge
Proceedings of the National Academy of Sciences Oct 2014, 111 (43) 15296-15303; DOI: 10.1073/pnas.1411762111

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Sea level and ice volume since the glacial maximum
Kurt Lambeck, Hélène Rouby, Anthony Purcell, Yiying Sun, Malcolm Sambridge
Proceedings of the National Academy of Sciences Oct 2014, 111 (43) 15296-15303; DOI: 10.1073/pnas.1411762111
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  • Physical Sciences
  • Earth, Atmospheric, and Planetary Sciences

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  • Last Glacial Maximum sea level
    - Nov 03, 2014
Proceedings of the National Academy of Sciences: 111 (43)
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    • Analysis Strategy
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