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

Lambeck, Kurt, Rouby, Hélène, Purcell, Anthony, Sun, Yiying, Sambridge, Malcolm·2014·Proceedings of the National Academy of Sciences
DOI 10.1073/pnas.1411762111
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Abstract

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.

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  • Periods of deposition and nondeposition and changing sedimentation rates at Page-Ladson from ~14,900 to 8500 cal yr B.P. correlate with sea level fluctuations when ocean levels rose from 100 to 20 m below modern sea level.

    “Periods of deposition and nondeposition as well as changing sedimentation rates at Page-Ladson from ~14,900 to 8500 cal yr B.P. appear to correlate with sea level fluctuations when ocean levels rose from 100 to 20 m below modern sea level (15, 16), even though the site was ~250 to 175 km inland during this time.”

    From Pre-Clovis occupation 14,550 years ago at the Page-Ladson site, Florida, and the peopling of the Americas (2016) · cites this paper as [15]

    The Discussion and Conclusions reports substantial global sea-level rise and changes in its rate during the cited interval, supporting the sea-level context. It does not discuss Page-Ladson or establish a correlation between its deposition and sea-level fluctuations; the claimed correlation is therefore not supported by this source. (LLM, conf=0.88)

    Experimental — accuracy not yet measured

  • Global sea levels began to rise gradually after approximately 16 ka, although the Bering Land Bridge (BLB) was not completely flooded until approximately 11 ka.

    “Global sea levels began to rise gradually after approximately 16 ka although the BLB was not completely flooded until approximately 11 ka [91].”

    From Beringia and the peopling of the Western Hemisphere (2023) · cites this paper as [91]

  • The southern margin of the Cordilleran Ice Sheet reached its maximum several thousand years after the peak in global ice volume at around 20-19 ka.

    “The southern margin of the ice sheet reached its maximum several thousand years after the peak in global ice volume at around 20-19 ka (Carlson & Clark, 2012;Clark et al., 2009;Lambeck et al., 2014;Lisiecki & Raymo, 2005).”

    From Retreat of the Western Cordilleran Ice Sheet Margin During the Last Deglaciation (2018) · cites this paper as Lambeck et al., 2014

  • The Cordilleran Ice Sheet contributed 2.5-3.0 m to eustatic sea-level rise during ice sheet thinning by around 14.0 ka.

    “This finding is consistent with a trend of ice sheet thinning by around 14.0 ka, during which the Cordilleran Ice Sheet contributed 2.5-3.0 m to eustatic sea-level rise (Lambeck et al., 2014;Margold et al., 2014;Menounos et al., 2017), potentially contributing to meltwater pulses at this time (Gomez et al., 2015;Gregoire et al., 2016Gregoire et al., , 2012;;Ivanovic et al., 2017).”

    From Retreat of the Western Cordilleran Ice Sheet Margin During the Last Deglaciation (2018) · cites this paper as Lambeck et al., 2014

  • This finding is consistent with a trend of ice sheet thinning by around 14.0 ka, during which the Cordilleran Ice Sheet contributed 2.5-3.0 m to eustatic sea-level rise.

    “This finding is consistent with a trend of ice sheet thinning by around 14.0 ka, during which the Cordilleran Ice Sheet contributed 2.5-3.0 m to eustatic sea-level rise (Lambeck et al., 2014;Margold et al., 2014;Menounos et al., 2017), potentially contributing to meltwater pulses at this time (Gomez et al., 2015;Gregoire et al., 2016Gregoire et al., , 2012;;Ivanovic et al., 2017).”

    From Retreat of the Western Cordilleran Ice Sheet Margin During the Last Deglaciation (2018) · cites this paper as Lambeck et al., 2014

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Metadata

Authors
Lambeck, K., Rouby, H., Purcell, A., Sun, Y., & Sambridge, M.
Affiliations
  • Research School of Earth Sciences, The Australian National University, Canberra, ACT 0200, Australia;
  • Department of Earth Sciences, University of Hong Kong, Hong Kong, China
Venue
Proceedings of the National Academy of Sciences
Publisher
National Academy of Sciences
Published
2014-10-13
Volume
111
Issue
43
Pages
15296-15303
ISSN
  • 0027-8424
  • 1091-6490
DOI
10.1073/pnas.1411762111
Cited by
2,215
References
2
Language
en

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