ArticleScientific data2019
Consistently dated Atlantic sediment cores over the last 40 thousand years.
Article in Scientific data, 2019. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 11 papers.
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Who cites it
11 citing papers in PubMed.
- Low variability of the Atlantic Meridional Overturning Circulation throughout the Holocene.Nature communications · 2025Article
- Alpine ice core record of large changes in dust, sea-salt, and biogenic aerosol over Europe during deglaciation.PNAS nexus · 2025Article
- Prevalent North Atlantic Deep Water during the Last Glacial Maximum and Heinrich Stadial 1.Nature geoscience · 2025Article
- Variations in deep-sea methane seepage linked to millennial-scale changes in bottom water temperatures ~ 50-6 ka, NW Svalbard margin.Scientific reports · 2024Article
- The PaleoJump database for abrupt transitions in past climates.Scientific reports · 2023Article
- A global synthesis of high-resolution stable isotope data from benthic foraminifera of the last deglaciation.Scientific data · 2023Article
- Emerging biological archives can reveal ecological and climatic change in Antarctica.Global change biology · 2022Review
- Coupled atmosphere-ice-ocean dynamics during Heinrich Stadial 2.Nature communications · 2022Article
- Strong links between Saharan dust fluxes, monsoon strength, and North Atlantic climate during the last 5000 years.Science advances · 2021Article
- The fast-acting "pulse" of Heinrich Stadial 3 in a mid-latitude boreal ecosystem.Scientific reports · 2020Article
- Consistently dated Atlantic sediment cores over the last 40 thousand years.Scientific data · 2019Article
Corrections and comments
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Authors and funding
63 authors.
Funding
Abstract
Rapid changes in ocean circulation and climate have been observed in marine-sediment and ice cores over the last glacial period and deglaciation, highlighting the non-linear character of the climate system and underlining the possibility of rapid climate shifts in response to anthropogenic greenhouse gas forcing. To date, these rapid changes in climate and ocean circulation are still not fully explained. One obstacle hindering progress in our understanding of the interactions between past ocean circulation and climate changes is the difficulty of accurately dating marine cores. Here, we present a set of 92 marine sediment cores from the Atlantic Ocean for which we have established age-depth models that are consistent with the Greenland GICC05 ice core chronology, and computed the associated dating uncertainties, using a new deposition modeling technique. This is the first set of consistently dated marine sediment cores enabling paleoclimate scientists to evaluate leads/lags between circulation and climate changes over vast regions of the Atlantic Ocean. Moreover, this data set is of direct use in paleoclimate modeling studies.
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Registered trials
Read under generation 80e0d062 · epoch 390. Bibliography from PubMed, PubMed Central and OpenAlex; grants from NIH RePORTER; trial links from ClinicalTrials.gov; estimates, votes and beliefs from the OpenQuestion graph.