Earth and Sustainability Science Research Centre, School
of Biological, Earth and Environmental Sciences, University of New South
Wales, Sydney, Australia
ARC Centre of Excellence in Australian Biodiversity and Heritage,
School of Biological, Earth and Environmental Sciences, University of New
South Wales, Sydney, Australia
Richard T. Jones
Department of Geography, Exeter University, Devon, EX4 4RJ, UK
Earth and Sustainability Science Research Centre, School
of Biological, Earth and Environmental Sciences, University of New South
Wales, Sydney, Australia
ARC Centre of Excellence in Australian Biodiversity and Heritage,
School of Biological, Earth and Environmental Sciences, University of New
South Wales, Sydney, Australia
Claus-Dieter Hillenbrand
British Antarctic Survey, High Cross, Madingley Road, Cambridge CB3
0ET, UK
Christopher J. Fogwill
Earth and Sustainability Science Research Centre, School
of Biological, Earth and Environmental Sciences, University of New South
Wales, Sydney, Australia
School of Geography, Geology and the Environment, Keele University,
Keele ST5 5BG, UK
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4,245
1,667
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6,089
375
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246
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Total: 6,089
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EndNote: 246
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Cumulative views and downloads
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Total article views: 4,854 (including HTML, PDF, and XML)
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EndNote
3,658
1,074
122
4,854
208
136
180
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PDF: 1,074
XML: 122
Total: 4,854
Supplement: 208
BibTeX: 136
EndNote: 180
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587
593
55
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Supplement: 167
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The Last Interglacial (129–116 ka) experienced global temperatures and sea levels higher than today. The direct contribution of warmer conditions to global sea level (thermosteric) are uncertain. We report a global network of sea surface temperatures. We find mean global annual temperature anomalies of 0.2 ± 0.1˚C and an early maximum peak of 0.9 ± 0.1˚C. Our reconstruction suggests warmer waters contributed on average 0.08 ± 0.1 m and a peak contribution of 0.39 ± 0.1 m to global sea level.
The Last Interglacial (129–116 ka) experienced global temperatures and sea levels higher than...
