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View article: Author Correction: Antarctic ice-shelf collapse in Holocene driven by meltwater release feedbacks
Author Correction: Antarctic ice-shelf collapse in Holocene driven by meltwater release feedbacks Open
View article: Antarctic ice-shelf collapse in Holocene driven by meltwater release feedbacks
Antarctic ice-shelf collapse in Holocene driven by meltwater release feedbacks Open
Circumpolar Deep Water inflow onto Antarctica’s continental shelves is a key driver of accelerated Antarctic Ice Sheet mass loss, both presently and during the last deglaciation. However, the mechanisms driving enhanced inflow and the resu…
View article: Supplementary material to "New isoprenoid GDGT index as a water mass and temperature proxy in the Southern Ocean"
Supplementary material to "New isoprenoid GDGT index as a water mass and temperature proxy in the Southern Ocean" Open
View article: New isoprenoid GDGT index as a water mass and temperature proxy in the Southern Ocean
New isoprenoid GDGT index as a water mass and temperature proxy in the Southern Ocean Open
The Southern Ocean plays a crucial role in the global carbon cycle, ocean heat transport, and Antarctic ice dynamics. Investigating past variability in the Southern Ocean, including temperature and water masses distribution, can improve un…
View article: Data report: gas hydrate assessment in Baffin Bay at IODP Expedition 400 drill sites
Data report: gas hydrate assessment in Baffin Bay at IODP Expedition 400 drill sites Open
International audience
View article: Acidity-driven gas-particle partitioning of nitrate regulates its transport to Arctic through the industrial era
Acidity-driven gas-particle partitioning of nitrate regulates its transport to Arctic through the industrial era Open
View article: Site U1608
Site U1608 Open
International audience
View article: Expedition 400 summary
Expedition 400 summary Open
International audience
View article: Site U1603
Site U1603 Open
International audience
View article: Expedition 400 methods
Expedition 400 methods Open
International audience
View article: Site U1607
Site U1607 Open
View article: Site U1605
Site U1605 Open
International audience
View article: Site U1606
Site U1606 Open
International audience
View article: Site U1604
Site U1604 Open
International audience
View article: Seasonal Sea Surface Temperature Variations at the Northern Limit of the Kuroshio Current in Marine Isotope Stage 20–18
Seasonal Sea Surface Temperature Variations at the Northern Limit of the Kuroshio Current in Marine Isotope Stage 20–18 Open
This study presents a high time‐resolution alkenone unsaturation ratios (U K' 37 ) in the Chiba composite section, a marine sedimentary sequence formed in the Kazusa forearc basin in the northwestern Pacific under the influence of the Kuro…
View article: Survival strategies of Antarctic vegetation during extensive glacial expansion across the Oligocene/Miocene Transition
Survival strategies of Antarctic vegetation during extensive glacial expansion across the Oligocene/Miocene Transition Open
Antarctica’s terrestrial ecosystems are at risk from a rapidly changing climate. Investigating how Antarctica’s vascular plants responded to major climatic variations in the geological past, especially under atmospheric CO2 values similar …
View article: Impact of elevated CO2 on the δ13C of n-alkane biomarkers
Impact of elevated CO2 on the δ13C of n-alkane biomarkers Open
View article: Atmospheric particulates over the northwestern Pacific during the late Holocene: Volcanism, dust, and human perturbation
Atmospheric particulates over the northwestern Pacific during the late Holocene: Volcanism, dust, and human perturbation Open
Mineral aerosols form a key component of Earth’s dynamic biogeochemical systems, yet their composition and mass are variable in time. We reconstruct patterns in mineral aerosol flux from East Asia, the second largest global dust source, in…
View article: Spatially variable response of Antarctica's ice sheets to orbital forcing during the Pliocene
Spatially variable response of Antarctica's ice sheets to orbital forcing during the Pliocene Open
Variations in Earth’s orbit pace global ice-volume/sea-level changes, but the variability in the response for different sectors of the Antarctic Ice Sheet (AIS) to orbitally-forced climate change remains unclear. We present geological reco…
View article: Expedition 400 Preliminary Report: NW Greenland Glaciated Margin
Expedition 400 Preliminary Report: NW Greenland Glaciated Margin Open
International audience
View article: Radiolarian assemblages related to the ocean–ice interaction around the East Antarctic coast
Radiolarian assemblages related to the ocean–ice interaction around the East Antarctic coast Open
The Southern Ocean plays a central role in Earth's climate, ecology, and biogeochemical cycles. Therefore, understanding long-term changes in Southern Ocean water masses in the geologic past is essential for assessing the role of the South…
View article: Toward a Cenozoic history of atmospheric CO <sub>2</sub>
Toward a Cenozoic history of atmospheric CO <sub>2</sub> Open
The geological record encodes the relationship between climate and atmospheric carbon dioxide (CO 2 ) over long and short timescales, as well as potential drivers of evolutionary transitions. However, reconstructing CO 2 beyond direct meas…
View article: Amplified surface warming in the south-west Pacific during the mid-Pliocene (3.3–3.0 Ma) and future implications
Amplified surface warming in the south-west Pacific during the mid-Pliocene (3.3–3.0 Ma) and future implications Open
Based on Nationally Determined Contributions concurrent with Shared Socioeconomic Pathways (SSPs) 2-4.5, the IPCC predicts global warming of 2.1–3.5 ∘C (very likely range 10–90th percentile) by 2100 CE. However, global average temperature …
View article: Climate-controlled submarine landslides on the Antarctic continental margin
Climate-controlled submarine landslides on the Antarctic continental margin Open
Antarctica’s continental margins pose an unknown submarine landslide-generated tsunami risk to Southern Hemisphere populations and infrastructure. Understanding the factors driving slope failure is essential to assessing future geohazards.…
View article: Multiple episodes of ice loss from the Wilkes Subglacial Basin during the Last Interglacial
Multiple episodes of ice loss from the Wilkes Subglacial Basin during the Last Interglacial Open
The Last Interglacial (LIG: 130,000–115,000 years ago) was a period of warmer global mean temperatures and higher and more variable sea levels than the Holocene (11,700–0 years ago). Therefore, a better understanding of Antarctic ice-sheet…
View article: Comment on egusphere-2023-108
Comment on egusphere-2023-108 Open
Abstract. Based on Nationally-Determined Contributions concurrent with Shared Socio-economic Pathway (SSP) 2–4.5, the IPCC predicts global warming between 2.1–3.5°C (very likely range 10th–90th percentile) by 2100 AD. Howe…
View article: Influence of Earlier Snowmelt on the Seedling Growth of Six Subboreal Tree Species in the Spring
Influence of Earlier Snowmelt on the Seedling Growth of Six Subboreal Tree Species in the Spring Open
Climate warming is advancing snowmelt timing in the spring at high latitudes. To predict tree growth in subboreal forests under warmer climates based on mechanistic understanding, it is important to assess how advancing snowmelt influences…
View article: Amplified surface warming in the Southwest Pacific during the mid-Pliocene (3.3–3.0 Ma) and future implications
Amplified surface warming in the Southwest Pacific during the mid-Pliocene (3.3–3.0 Ma) and future implications Open
Based on Nationally-Determined Contributions concurrent with Shared Socio-economic Pathway (SSP) 2–4.5, the IPCC predicts global warming between 2.1–3.5°C (very likely range 10th–90th percentile) by 2100 AD. However, global average tempera…
View article: Ancient marine sediment DNA reveals diatom transition in Antarctica
Ancient marine sediment DNA reveals diatom transition in Antarctica Open
View article: Latitudinal Variance in the Drivers and Pacing of Warmth During Mid‐Pleistocene MIS 31 in the Antarctic Zone of the Southern Ocean
Latitudinal Variance in the Drivers and Pacing of Warmth During Mid‐Pleistocene MIS 31 in the Antarctic Zone of the Southern Ocean Open
Early Pleistocene Marine Isotope Stage (MIS)‐31 (1.081–1.062 Ma) is a unique interval of extreme global warming, including evidence of a West Antarctic Ice Sheet (WAIS) collapse. Here we present a new 1,000‐year resolution, spanning 1.110–…