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View article: Near Steady Late Pleistocene Tropical Denudation Rates in SW Madagascar
Near Steady Late Pleistocene Tropical Denudation Rates in SW Madagascar Open
Denudation is a key parameter controlling the evolution of the Earth's surface, the production of soils, the stability of relief, or the long‐term evolution of climate. Climate fluctuations conversely have a strong impact on denudation, bu…
View article: Changes in deep water circulation dynamics in the South Atlantic Ocean during Marine Isotope Stage
Changes in deep water circulation dynamics in the South Atlantic Ocean during Marine Isotope Stage Open
Persistent deep-water formation in the North Atlantic and Southern Ocean is believed to drive the ventilation of the global deep ocean throughout late Pleistocene interglacial periods. The persistency of interglacial deep-ocean ventilation…
View article: Near steady denudation rates during the late Pleistocene in the tropics
Near steady denudation rates during the late Pleistocene in the tropics Open
Denudation is a key parameter controlling the evolution of the Earth’s surface, the production of soils, the stability of relief or the long-term evolution of climate. Climate fluctuations conversely have a strong impact on denudation, but…
View article: Comment on sp-2023-34
Comment on sp-2023-34 Open
Abstract. The Intergovernmental Panel on Climate Change (IPCC) plays a pivotal role in delivering information and knowledge on sea level rise (SLR), a global threat impacting coastlines worldwide. However, considerable disparities still pe…
View article: Sea Level Rise in Europe: Knowledge gaps identified through a participatory approach
Sea Level Rise in Europe: Knowledge gaps identified through a participatory approach Open
The Intergovernmental Panel on Climate Change (IPCC) plays a pivotal role in delivering information and knowledge on sea level rise (SLR), a global threat impacting coastlines worldwide. However, considerable disparities still persist in E…
View article: Supplementary material to "Sea Level Rise in Europe: Knowledge gaps identified through a participatory approach"
Supplementary material to "Sea Level Rise in Europe: Knowledge gaps identified through a participatory approach" Open
1. Tables S1-S3.Statistics of responses to closed-ended survey questions using a Likert scale 2. KH-SLR survey "Profiling SLR needs & knowledge gaps" 3. Agenda for the KH-SLR scoping workshop for the North Sea -Arctic Seas basins 4. Agenda…
View article: Atlantic circulation changes across a stadial–interstadial transition
Atlantic circulation changes across a stadial–interstadial transition Open
We combine consistently dated benthic carbon isotopic records distributed over the entire Atlantic Ocean with numerical simulations performed by a glacial configuration of the Norwegian Earth System Model with active ocean biogeochemistry …
View article: Comment on cp-2022-83
Comment on cp-2022-83 Open
Abstract. We combine consistently dated benthic carbon isotopic records distributed over the entire Atlantic Ocean with numerical simulations performed by a glacial configuration of the Norwegian Earth System Model with active ocean biogeo…
View article: Atlantic circulation changes across a stadial-interstadial transition
Atlantic circulation changes across a stadial-interstadial transition Open
We combine consistently dated benthic carbon isotopic records distributed over the entire Atlantic Ocean with numerical simulations performed by a glacial configuration of the Norwegian Earth System Model with active ocean biogeochemistry,…
View article: Increased zonal δ13C gradient in the deep South Atlantic after the Mid-Brunhes Transition
Increased zonal δ13C gradient in the deep South Atlantic after the Mid-Brunhes Transition Open
<p>The climate system experienced several periodic oscillations over the last ca. 800 ka known as glacial-interglacial (G-IG) cycles. Disruptions of the global carbon cycle were evident on this time scale, promoting fluctuations in t…
View article: A Simplified Palaeoceanography Archiving System (PARIS) and GUI for Storage and Visualisation of Marine Sediment Core Proxy Data vs Age and Depth
A Simplified Palaeoceanography Archiving System (PARIS) and GUI for Storage and Visualisation of Marine Sediment Core Proxy Data vs Age and Depth Open
Scientific discovery can be aided when data are shared following the principles of findability, accessibility, interoperability, reusability (FAIR) data (Wilkinson et al., 2016). Recent discussions in the palaeoclimate literature have focu…
View article: A simplified palaeoceanography archiving system (PARIS) and GUI for storage and visualisation of marine sediment core proxy data vs age and depth.
A simplified palaeoceanography archiving system (PARIS) and GUI for storage and visualisation of marine sediment core proxy data vs age and depth. Open
Scientific discovery can be aided when data is shared following the principles of findability, accessibility, interoperability, reusability (FAIR) data (Wilkinson et al., 2016). Recent discussions in the palaeoclimate literature have focus…
View article: A simplified palaeoceanography archiving system (PARIS) and GUI for storage and visualisation of marine sediment core proxy data vs age and depth.
A simplified palaeoceanography archiving system (PARIS) and GUI for storage and visualisation of marine sediment core proxy data vs age and depth. Open
Scientific discovery can be aided when data is shared following the principles of findability, accessibility, interoperability, reusability (FAIR) data (Wilkinson et al., 2016). Recent discussions in the palaeoclimate literature have focus…
View article: A simplified palaeoceanography archiving system (PARIS) and GUI for storage and visualisation of marine sediment core proxy data vs age and depth.
A simplified palaeoceanography archiving system (PARIS) and GUI for storage and visualisation of marine sediment core proxy data vs age and depth. Open
Scientific discovery can be aided when data is shared following the principles of findability, accessibility, interoperability, reusability (FAIR) data (Wilkinson et al., 2016). Recent discussions in the palaeoclimate literature have focus…
View article: The North Atlantic Glacial Eastern Boundary Current as a Key Driver for Ice‐Sheet—AMOC Interactions and Climate Instability
The North Atlantic Glacial Eastern Boundary Current as a Key Driver for Ice‐Sheet—AMOC Interactions and Climate Instability Open
The upper branch of the Atlantic meridional overturning circulation (AMOC) plays a critical role in ocean circulation and climate change, yet its variability during the last glacial period is poorly documented. Here, we investigate the nor…
View article: Age versus two relative paleointensity proxies (slopes of NRM/ARM and NRM/IRM) for u-channel samples from Core MD07-3077 recovered during Marion Dufresne cruise VT90/SOUC
Age versus two relative paleointensity proxies (slopes of NRM/ARM and NRM/IRM) for u-channel samples from Core MD07-3077 recovered during Marion Dufresne cruise VT90/SOUC Open
Two relative paleointensity (RPI) proxies (slopes of NRM/ARM and NRM/IRM) from u-channel samples from Core MD07-3077. The RPI proxies were determined from stepwise alternating field demagnetization applied to the natural remanent magnetiza…
View article: Atlantic Ocean Ventilation Changes Across the Last Deglaciation and Their Carbon Cycle Implications
Atlantic Ocean Ventilation Changes Across the Last Deglaciation and Their Carbon Cycle Implications Open
Changes in ocean ventilation, controlled by both overturning rates and air‐sea gas exchange, are thought to have played a central role in atmospheric CO 2 rise across the last deglaciation. Here, we constrain the nature of Atlantic Ocean v…
View article: Carbon 13 Isotopes Reveal Limited Ocean Circulation Changes Between Interglacials of the Last 800 ka
Carbon 13 Isotopes Reveal Limited Ocean Circulation Changes Between Interglacials of the Last 800 ka Open
Ice core data have shown that atmospheric CO 2 concentrations during interglacials were lower before the Mid‐Brunhes Event (MBE, ~430 ka), than after the MBE by around 30 ppm. To explain such a difference, it has been hypothesized that inc…
View article: Ocean circulation during the last nine interglacials inferred from carbon 13 isotopes - model outputs
Ocean circulation during the last nine interglacials inferred from carbon 13 isotopes - model outputs Open
This dataset contains the model output corresponding to the paper entitled "Ocean circulation during the last nine interglacials inferred from carbon 13 isotopes" submitted to Paleoceanography. For the description of the model and simulati…