Daniel Baggenstos

Evolution of mean ocean temperature in Marine Isotope Stage 4

Global ocean heat content in the Last Interglacial

Old carbon reservoirs were not important in the deglacial methane budget

Earth’s radiative imbalance from the Last Glacial Maximum to the present

Spatial pattern of accumulation at Taylor Dome during Marine Isotope Stage 4: stratigraphic constraints from Taylor Glacier

Mean global ocean temperatures during the last glacial transition

A Horizontal Ice Core From Taylor Glacier, Its Implications for Antarctic Climate History, and an Improved Taylor Dome Ice Core Time Scale

Stellar<mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML" display="inline"><mml:mrow><mml:mrow><mml:mmultiscripts><mml:mrow><mml:mi>Ar</mml:mi></mml:mrow><mml:mprescripts/><mml:none/><mml:mrow><mml:mn>36</mml:mn><mml:mo>,</mml:mo><mml:mn>38</mml:mn></mml:mrow></mml:mmultiscripts></mml:mrow><mml:mo stretchy="false">(</mml:mo><mml:mi>n</mml:mi><mml:mo>,</mml:mo><mml:mi>γ</mml:mi><mml:mo stretchy="false">)</mml:mo><mml:mmultiscripts><mml:mrow><mml:mi>Ar</mml:mi></mml:mrow><mml:mprescripts/><m

Minimal geological methane emissions during the Younger Dryas–Preboreal abrupt warming event

Synchronous volcanic eruptions and abrupt climate change ∼17.7 ka plausibly linked by stratospheric ozone depletion

Carbon isotopes characterize rapid changes in atmospheric carbon dioxide during the last deglaciation

The WAIS Divide deep ice core WD2014 chronology – Part 1: Methane synchronization (68–31 ka BP) and the gas age–ice age difference

Observing and modeling the influence of layering on bubble trapping in polar firn

Radiometric ⁸¹ Kr dating identifies 120,000-year-old ice at Taylor Glacier, Antarctica

Isotopic constraints on marine and terrestrial N2O emissions during the last deglaciation

Nitrogen trifluoride global emissions estimated from updated atmospheric measurements