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Rapid rise in atmospheric CO2 marked the end of the Late Palaeozoic Ice Age
通讯作者Jurikova, Hana(hj43@st-andrews.ac.uk)
Jurikova, Hana1; Garbelli, Claudio2; Whiteford, Ross1; Reeves, Theodore1; Laker, Gemma M.1; Liebetrau, Volker3; Gutjahr, Marcus3; Eisenhauer, Anton3; Savickaite, Kotryna4; Leng, Melanie J.4
2025
发表期刊NATURE GEOSCIENCE (IF:14.391[JCR-2017],14.846[5-Year])
ISSN1752-0894
卷号18期号:1页码:8
摘要Atmospheric CO2 is thought to play a fundamental role in Earth's climate regulation. Yet, for much of Earth's geological past, atmospheric CO2 has been poorly constrained, hindering our understanding of transitions between cool and warm climates. Beginning similar to 370 million years ago in the Late Devonian and ending similar to 260 million years ago in the Permian, the Late Palaeozoic Ice Age was the last major glaciation preceding the current Late Cenozoic Ice Age and possibly the most intense glaciation witnessed by complex lifeforms. From the onset of the main phase of the Late Palaeozoic Ice Age in the mid-Mississippian similar to 330 million years ago, the Earth is thought to have sustained glacial conditions, with continental ice accumulating in high to mid-latitudes. Here we present an 80-million-year-long boron isotope record within a proxy framework for robust quantification of CO2. Our record reveals that the main phase of the Late Palaeozoic Ice Age glaciation was maintained by prolonged low CO2, unprecedented in Earth's history. About 294 million years ago, atmospheric CO2 rose abruptly (4-fold), releasing the Earth from its penultimate ice age and transforming the Early Permian into a warmer world.
DOI10.1038/s41561-024-01610-2
收录类别SCI
语种英语
关键词[WOS]BORON ISOTOPES ; ACIDIFICATION ; TEMPERATURE ; SEAWATER ; KEY
资助项目Leverhulme Trust[ECF-2023-199] ; Leverhulme Trust Early Career Fellowship[805246] ; European Research Council under the European Union[643084] ; European Commission's Marie Sklodowska-Curie Innovative Training Network ('BASELiNE-Earth' ITN) under European Union[2023-27] ; Italian Ministry for Universities and Research (MUR) through the project 'Dipartimenti di Eccellenza[2022WEZR44] ; European Union-Next Generation EU PRIN MUR[APVV22-0523] ; Slovak Agency for Research and Development[42293280] ; NSFC[ARC DP230100323] ; Australian Research Council
WOS研究方向Geology
WOS类目Geosciences, Multidisciplinary
WOS记录号WOS:001391002100001
项目资助者Leverhulme Trust ; Leverhulme Trust Early Career Fellowship ; European Research Council under the European Union ; European Commission's Marie Sklodowska-Curie Innovative Training Network ('BASELiNE-Earth' ITN) under European Union ; Italian Ministry for Universities and Research (MUR) through the project 'Dipartimenti di Eccellenza ; European Union-Next Generation EU PRIN MUR ; Slovak Agency for Research and Development ; NSFC ; Australian Research Council
出版者NATURE PORTFOLIO
文献类型期刊论文
条目标识符http://ir.nigpas.ac.cn/handle/332004/44776
专题中国科学院南京地质古生物研究所
通讯作者Jurikova, Hana
作者单位1.Univ St Andrews, Sch Earth & Environm Sci, St Andrews, Scotland
2.Sapienza Univ Roma, Dept Earth Sci, Rome, Italy
3.GEOMAR Helmholtz Zentrum Ozeanforschung Kiel, Kiel, Germany
4.British Geol Survey, Nottingham, England
5.Univ Milan, Dept Earth Sci Ardito Desio, Milan, Italy
6.Slovak Acad Sci, Earth Sci Inst, Bratislava, Slovakia
7.Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, Nanjing, Peoples R China
8.Nanjing Univ, Sch Earth Sci & Engn, State Key Lab Mineral Deposits Res, Nanjing, Peoples R China
9.Nanjing Univ, Frontiers Sci Ctr Crit Earth Mat Cycling, Nanjing, Peoples R China
10.Univ Wollongong, Sch Earth Atmospher & Life Sci, Wollongong, NSW, Australia
推荐引用方式
GB/T 7714
Jurikova, Hana,Garbelli, Claudio,Whiteford, Ross,et al. Rapid rise in atmospheric CO2 marked the end of the Late Palaeozoic Ice Age[J]. NATURE GEOSCIENCE,2025,18(1):8.
APA Jurikova, Hana.,Garbelli, Claudio.,Whiteford, Ross.,Reeves, Theodore.,Laker, Gemma M..,...&Angiolini, Lucia.(2025).Rapid rise in atmospheric CO2 marked the end of the Late Palaeozoic Ice Age.NATURE GEOSCIENCE,18(1),8.
MLA Jurikova, Hana,et al."Rapid rise in atmospheric CO2 marked the end of the Late Palaeozoic Ice Age".NATURE GEOSCIENCE 18.1(2025):8.
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