Articles | Volume 22, issue 3
https://doi.org/10.5194/cp-22-585-2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/cp-22-585-2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
New isoprenoid GDGT index as a water mass and temperature proxy in the Southern Ocean
Institute of Low Temperature Science, Hokkaido University, Sapporo, 060-0819, Japan
Faculty of Environmental Earth Science, Hokkaido University, Sapporo, 060-0810, Japan
now at: Antarctic Research Centre, Victoria University of Wellington, Wellington, 6140, New Zealand
Osamu Seki
CORRESPONDING AUTHOR
Institute of Low Temperature Science, Hokkaido University, Sapporo, 060-0819, Japan
Faculty of Environmental Earth Science, Hokkaido University, Sapporo, 060-0810, Japan
Masanobu Yamamoto
Faculty of Environmental Earth Science, Hokkaido University, Sapporo, 060-0810, Japan
Bella Duncan
Earth Science New Zealand, Lower Hutt, 5011, New Zealand
now at: Antarctic Research Centre, Victoria University of Wellington, Wellington, 6140, New Zealand
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Emma M. de Jong, Xavier Crosta, Sebastian Naeher, Bella Duncan, Johan Etourneau, Jae Il Lee, Robert McKay, and V. Holly L. Winton
EGUsphere, https://doi.org/10.5194/egusphere-2025-5553, https://doi.org/10.5194/egusphere-2025-5553, 2025
This preprint is open for discussion and under review for Biogeosciences (BG).
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This study examines chemical and biological traces (biomarkers) of microscopic algae in Antarctic sediments. We show how sea ice conditions and different phytoplankton communities influence the types of biomarkers preserved on the seafloor, and how these records reveal an overall increase in sea ice duration in the Ross Sea over the past 200 years.
Peter K. Bijl, Kasia K. Śliwińska, Bella Duncan, Arnaud Huguet, Sebastian Naeher, Ronnakrit Rattanasriampaipong, Claudia Sosa-Montes de Oca, Alexandra Auderset, Melissa A. Berke, Bum Soo Kim, Nina Davtian, Tom Dunkley Jones, Desmond D. Eefting, Felix J. Elling, Pierrick Fenies, Gordon N. Inglis, Lauren O'Connor, Richard D. Pancost, Francien Peterse, Addison Rice, Appy Sluijs, Devika Varma, Wenjie Xiao, and Yi Ge Zhang
Biogeosciences, 22, 6465–6508, https://doi.org/10.5194/bg-22-6465-2025, https://doi.org/10.5194/bg-22-6465-2025, 2025
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Many academic laboratories worldwide process environmental samples for analysis of membrane lipid molecules of archaea, for the reconstruction of past environmental conditions. However, the sample workup scheme involves many steps, each of which has a risk of contamination or bias, affecting the results. This paper reviews steps involved in sampling, extraction and analysis of lipids, interpretation and archiving of the data. This ensures reproducible, reusable, comparable and consistent data.
Bella J. Duncan, Robert McKay, Richard Levy, Joseph G. Prebble, Timothy Naish, Osamu Seki, Christoph Kraus, Heiko Moossen, G. Todd Ventura, Denise K. Kulhanek, and James Bendle
EGUsphere, https://doi.org/10.5194/egusphere-2024-4021, https://doi.org/10.5194/egusphere-2024-4021, 2025
This preprint is open for discussion and under review for Climate of the Past (CP).
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We use plant wax compound specific stable isotopes to investigate how ancient Antarctic vegetation adapted to glacial conditions 23 million years ago. We find plants became less water efficient to prioritise photosynthesis during short, harsh growing seasons. Ecosystem changes also included enhanced aridity, and a shift to a stunted, low elevation vegetation. This shows the adaptability of ancient Antarctic vegetation under atmospheric CO2 conditions comparable to modern.
Mutsumi Iizuka, Takuya Itaki, Osamu Seki, Ryosuke Makabe, Motoha Ojima, and Shigeru Aoki
J. Micropalaeontol., 43, 37–53, https://doi.org/10.5194/jm-43-37-2024, https://doi.org/10.5194/jm-43-37-2024, 2024
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Radiolarian fossils are valuable tools for understanding water mass distribution. However, they have not been used in the high-latitude Southern Ocean due to unclear radiolarian assemblages. Our study identifies four assemblages related to water masses and ice edge environments in the high-latitude Southern Ocean, offering insights for water mass reconstruction in this region.
Georgia R. Grant, Jonny H. T. Williams, Sebastian Naeher, Osamu Seki, Erin L. McClymont, Molly O. Patterson, Alan M. Haywood, Erik Behrens, Masanobu Yamamoto, and Katelyn Johnson
Clim. Past, 19, 1359–1381, https://doi.org/10.5194/cp-19-1359-2023, https://doi.org/10.5194/cp-19-1359-2023, 2023
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Regional warming will differ from global warming, and climate models perform poorly in the Southern Ocean. We reconstruct sea surface temperatures in the south-west Pacific during the mid-Pliocene, a time 3 million years ago that represents the long-term outcomes of 3 °C warming, which is expected for the future. Comparing these results to climate model simulations, we show that the south-west Pacific region will warm by 1 °C above the global average if atmospheric CO2 remains above 350 ppm.
Frida S. Hoem, Luis Valero, Dimitris Evangelinos, Carlota Escutia, Bella Duncan, Robert M. McKay, Henk Brinkhuis, Francesca Sangiorgi, and Peter K. Bijl
Clim. Past, 17, 1423–1442, https://doi.org/10.5194/cp-17-1423-2021, https://doi.org/10.5194/cp-17-1423-2021, 2021
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We present new offshore palaeoceanographic reconstructions for the Oligocene (33.7–24.4 Ma) in the Ross Sea, Antarctica. Our study of dinoflagellate cysts and lipid biomarkers indicates warm-temperate sea surface conditions. We posit that warm surface-ocean conditions near the continental shelf during the Oligocene promoted increased precipitation and heat delivery towards Antarctica that led to dynamic terrestrial ice sheet volumes in the warmer climate state of the Oligocene.
Osamu Seki and James Bendle
Clim. Past Discuss., https://doi.org/10.5194/cp-2021-62, https://doi.org/10.5194/cp-2021-62, 2021
Manuscript not accepted for further review
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The reconstruction of CO2 levels in the past is a crucial objective in palaeoclimate research. However, estimates of CO2 level markedly differ among the data. We revised reported alkenone δ13C based CO2 records from the Pliocene to Pleistocene based on a refined approach. Our approach significantly reduced the large offsets between reported alkenone δ13C CO2 records, confirming that better constraints on environmental variables are key aspects for improving alkenone δ13C based CO2 estimates.
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Short summary
We explore the utility of the archaeal-derived lipid biomarker as paleoenvironmental proxies in the Southern Ocean. Based on a reanalysis of the Southern Ocean dataset, we propose a new indicator for reconstructing zonal water mass movements in the Southern Ocean and temperatures in the Antarctic Zone. Applying this method to late Pleistocene sediment cores validates its reliability, confirming a valuable new tool for reconstructing the paleoenvironment of the Southern Ocean.
We explore the utility of the archaeal-derived lipid biomarker as paleoenvironmental proxies in...