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Showing 1–5 of 5 results
Advanced filters: Author: Ulysses Ninnemann Clear advanced filters
  • It is thought that during the mid-Pliocene warm period the Atlantic Meridional Overturning Circulation (AMOC) must have been stronger than today. Here, using proxy data compilation and simulation, Zhang et al.show that the two observations used to support stronger AMOC may not necessitate its increased strength.

    • Zhongshi Zhang
    • Kerim H. Nisancioglu
    • Ulysses S. Ninnemann
    ResearchOpen Access
    Nature Communications
    Volume: 4, P: 1-6
  • The relative contributions of the Greenland and Antarctic Ice Sheets to Last Interglacial sea level rise remain debated, as do the timing and magnitude. Here, data show that the Antarctic Ice Sheet dominated particularly high levels of sea-level rise during the early Last Interglacial.

    • Eelco J. Rohling
    • Fiona D. Hibbert
    • Jimin Yu
    ResearchOpen Access
    Nature Communications
    Volume: 10, P: 1-9
  • The Southern Ocean has a fundamental role in millennial-scale global carbon cycling by regulating the amount of CO2 in the atmosphere. This Review explores Southern Ocean–atmosphere interactions during glacial–deglacial cycles, suggesting that these were critical in driving the termination of the Last Glacial Maximum.

    • Elisabeth L. Sikes
    • Natalie E. Umling
    • Thomas J. Williams
    Reviews
    Nature Reviews Earth & Environment
    Volume: 4, P: 454-470
  • The northern Barents Sea contained seasonal sea ice between 11.7 and 9.1 thousand years ago, even during the warmer-than-present Holocene Thermal Maximum and despite warm Atlantic Water inflow, according to biomarker and benthic foraminiferal stable isotope records.

    • Anna J. Pieńkowski
    • Katrine Husum
    • Riko Noormets
    ResearchOpen Access
    Communications Earth & Environment
    Volume: 2, P: 1-10