Results 91 to 100 of about 17,653 (244)
PaleoMist reconstruction for the last deglaciation.
PaleoMist reconstruction for the last deglaciation.
Gerrit Lohmann (7018322) +4 more
core +1 more source
Late Weichselian deglaciation of Denmark: some general problems
Deglaciation, Denmark, Late Weichselian ...
Humlum, Ole
core +1 more source
Carbon isotope minima were a ubiquitous feature in the mid-depth (1.5–2.5 km) Atlantic during Heinrich Stadial 1 (HS1, 14.5–17.5 kyr BP) and the Younger Dryas (YD, 11.6–12.9 kyr BP), with the most likely driver being collapse of the Atlantic Meridional ...
D Lund, J Hertzberg, M Lacerra
doaj +1 more source
Greenland deglaciation puzzles
Nitrogen isotope data help to resolve puzzling observations during the last deglaciation [Also see Report by Buizert et al. ]
openaire +3 more sources
Best Practices in Open and Reproducible Antarctic Marine Sediment Core Research
Abstract Marine sediment cores from Antarctica are archived by national programs for reuse and resampling by future researchers, creating a resourceful way to conduct Antarctic science. With reduced budgets to conduct Antarctic field work and to collect new sediment cores offshore of the icy continent, the accessibility of these archived cores and ...
L. E. Miller +12 more
wiley +1 more source
An Inconsistent ENSO Response to Northern Hemisphere Stadials Over the Last Deglaciation
The dynamics shaping the El Niño‐Southern Oscillation's (ENSO) response to present and future climate change remain unclear, partly due to limited paleo‐ENSO records spanning past abrupt climate events.
Ryan H. Glaubke +6 more
doaj +1 more source
ABSTRACT The Medical Journal of Australia (MJA)–Lancet Countdown on health and climate change in Oceania was established in 2017 and produced its first regional assessment in 2018 and annual updates from 2019 to 2025. It examines five broad domains: (1) health hazards, exposures and impacts; (2) adaptation, planning and resilience for health; (3 ...
Paul J. Beggs +40 more
wiley +1 more source
Global marine radiocarbon data compilation for the last deglaciation
Compiled marine radiocarbon data from the global ocean, derived from planktonic/benthic foraminifera and corals, spanning the last deglaciation, with associated calendar ages that are independently derived and/or are consistent with the Marine20 ...
Joos, Fortunat +5 more
core +1 more source
Abstract The sequence of events in the global carbon cycle during deglaciations is not entirely understood. Here, we analyze mean ocean δ13 ${\delta }^{13}$C and δ18 ${\delta }^{18}$O in an updated compilation of foraminiferal stable isotope data comprising 902 time series from 381 sediment cores, with individual records covering intervals within the ...
Peter Köhler, Stefan Mulitza
wiley +1 more source
The role of ice stream dynamics in deglaciation
Since the mid-Pleistocene transition, deglaciation has occurred only after ice sheets have grown large while experiencing several precession and obliquity cycles, indicating that large ice sheets are more sensitive to Milankovitch forcing than small ice ...
Robel, Alexander A., Tziperman, Eli
core +1 more source

