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Showing 1–6 of 6 results

Advanced filters: Author: Thomas M. Marchitto Clear advanced filters

Author Correction: Relatively warm deep-water formation persisted in the Last Glacial Maximum

Jack H. Wharton
Emilia Kozikowska
David J. R. Thornalley
Amendments and CorrectionsOpen Access27 Jan 2026
Nature

Volume: 650, P: E9
Relatively warm deep-water formation persisted in the Last Glacial Maximum

During the Last Glacial Maximum, the deep Northwest Atlantic was only about 2 °C colder than today, suggesting sustained production of relatively warm North Atlantic Deep Water during the Last Glacial Maximum.

Jack H. Wharton
Emilia Kozikowska
David J. R. Thornalley
ResearchOpen Access21 Jan 2026
Nature

Volume: 650, P: 116-122
Atmosphere and ocean chemistry

Low atmospheric carbon dioxide concentrations during glacial periods must have been accompanied by changes in surface-ocean carbonate chemistry. But it is unclear whether concurrent changes in the deep sea contributed to the glacial carbon dioxide decline.

Richard E. Zeebe
Thomas M. Marchitto Jr
News & Views01 Jun 2010
Nature Geoscience

Volume: 3, P: 386-387
Millennial-scale changes in North Atlantic circulation since the last glaciation

Thomas M. Marchitto Jr
William B. Curry
Delia W. Oppo
Research11 Jun 1998
Nature

Volume: 393, P: 557-561
Deeper and stronger North Atlantic Gyre during the Last Glacial Maximum

Analysis of benthic foraminiferal δ¹⁸O profiles from sediment cores in two depth transects in the Northwest Atlantic suggests that the subtropical gyre was deeper and stronger during the Last Glacial Maximum compared with today.

Jack H. Wharton
Martin Renoult
David J. R. Thornalley
ResearchOpen Access10 Jul 2024
Nature

Volume: 632, P: 95-100
Consistently dated Atlantic sediment cores over the last 40 thousand years

Claire Waelbroeck
Bryan C. Lougheed
Martin Ziegler
ResearchOpen Access02 Sept 2019
Scientific Data

Volume: 6, P: 1-12