List of works - Daniel Baggenstos

A horizontal ice core from Taylor Glacier, its implications for Antarctic climate history, and an improved Taylor Dome ice core time scale

article

Atmospheric gas records from Taylor Glacier, Antarctica, reveal ancient ice with ages spanning the entire last glacial cycle

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

scientific article published on 14 March 2016

Controls on Millennial‐Scale Atmospheric CO 2 Variability During the Last Glacial Period

scientific article published in 2018

Does δ18O of O2 record meridional shifts in tropical rainfall?

scholarly article

Does δ18O of O2 record meridional shifts in tropical rainfall?

supplementary material

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

scientific article published on 08 July 2019

Evolution of mean ocean temperature in Marine Isotope Stages 5-4

Global ocean heat content in the Last Interglacial

scholarly article

Is the Noble Gas‐Based Rate of Ocean Warming During the Younger Dryas Overestimated?

scholarly article

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

scientific article

Mean global ocean temperatures during the last glacial transition

scientific article published in January 2018

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

scientific article published on August 2017

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

scientific article

Old carbon reservoirs were not important in the deglacial methane budget

scientific article published on 01 February 2020

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

scientific article

Snapshots of mean ocean temperature over the last 700 000 years using noble gases in the EPICA Dome C ice core

scientific article published in 2021

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

Spatial pattern of accumulation at Taylor Dome during the last glacial inception: stratigraphic constraints from Taylor Glacier

Stellar ^{36,38}Ar(n,γ)^{37,39}Ar Reactions and Their Effect on Light Neutron-Rich Nuclide Synthesis

scientific article published on 01 September 2018

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

scientific article published on 5 September 2017

List of works by Daniel Baggenstos

A horizontal ice core from Taylor Glacier, its implications for Antarctic climate history, and an improved Taylor Dome ice core time scale

Atmospheric gas records from Taylor Glacier, Antarctica, reveal ancient ice with ages spanning the entire last glacial cycle

Atmospheric gas records from Taylor Glacier, Antarctica, reveal ancient ice with ages spanning the entire last glacial cycle

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

Controls on Millennial‐Scale Atmospheric CO 2 Variability During the Last Glacial Period

Does δ18O of O2 record meridional shifts in tropical rainfall?

Does δ18O of O2 record meridional shifts in tropical rainfall?

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

Evolution of mean ocean temperature in Marine Isotope Stages 5-4

Global ocean heat content in the Last Interglacial

Is the Noble Gas‐Based Rate of Ocean Warming During the Younger Dryas Overestimated?

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

Mean global ocean temperatures during the last glacial transition

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

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

Old carbon reservoirs were not important in the deglacial methane budget

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

Snapshots of mean ocean temperature over the last 700 000 years using noble gases in the EPICA Dome C ice core

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

Spatial pattern of accumulation at Taylor Dome during the last glacial inception: stratigraphic constraints from Taylor Glacier

Stellar ^{36,38}Ar(n,γ)^{37,39}Ar Reactions and Their Effect on Light Neutron-Rich Nuclide Synthesis

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

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

The WAIS-Divide deep ice core WD2014 chronology – Part 2: Methane synchronization (68–31 ka BP) and the gas age-ice age difference