Cenozoic sea-level and cryospheric evolution from deep-sea geochemical and continental margin records

Using Pacific benthic foraminiferal δ(18)O and Mg/Ca records, we derive a Cenozoic (66 Ma) global mean sea level (GMSL) estimate that records evolution from an ice-free Early Eocene to Quaternary bipolar ice sheets. These GMSL estimates are statistically similar to “backstripped” estimates from cont...

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Bibliographic Details
Published in:Science Advances
Main Authors: Miller, Kenneth G., Browning, James V., Schmelz, W. John, Kopp, Robert E., Mountain, Gregory S., Wright, James D.
Format: Text
Language:English
Published: American Association for the Advancement of Science 2020
Subjects:
Reviews
Antarctic
Pacific
Antarc*
Online Access:http://www.ncbi.nlm.nih.gov/pmc/articles/PMC7228749/
https://doi.org/10.1126/sciadv.aaz1346
Description
Summary:Using Pacific benthic foraminiferal δ(18)O and Mg/Ca records, we derive a Cenozoic (66 Ma) global mean sea level (GMSL) estimate that records evolution from an ice-free Early Eocene to Quaternary bipolar ice sheets. These GMSL estimates are statistically similar to “backstripped” estimates from continental margins accounting for compaction, loading, and thermal subsidence. Peak warmth, elevated GMSL, high CO(2), and ice-free “Hothouse” conditions (56 to 48 Ma) were followed by “Cool Greenhouse” (48 to 34 Ma) ice sheets (10 to 30 m changes). Continental-scale ice sheets (“Icehouse”) began ~34 Ma (>50 m changes), permanent East Antarctic ice sheets at 12.8 Ma, and bipolar glaciation at 2.5 Ma. The largest GMSL fall (27 to 20 ka; ~130 m) was followed by a >40 mm/yr rise (19 to 10 ka), a slowing (10 to 2 ka), and a stillstand until ~1900 CE, when rates began to rise. High long-term CO(2) caused warm climates and high sea levels, with sea-level variability dominated by periodic Milankovitch cycles.

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