Article (Scientific journals)
Antarctic meteorites threatened by climate warming
Tollenaar, Veronica; Zekollari, Harry; Kittel, Christoph et al.
2024In Nature Climate Change
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Keywords :
Social Sciences (miscellaneous); Environmental Science (miscellaneous)
Abstract :
[en] AbstractMore than 60% of meteorite finds on Earth originate from Antarctica. Using a data-driven analysis that identifies meteorite-rich sites in Antarctica, we show climate warming causes many extraterrestrial rocks to be lost from the surface by melting into the ice sheet. At present, approximately 5,000 meteorites become inaccessible per year (versus ~1,000 finds per year) and, independent of the emissions scenario, ~24% will be lost by 2050, potentially rising to ∼76% by 2100 under a high-emissions scenario.
Disciplines :
Earth sciences & physical geography
Author, co-author :
Tollenaar, Veronica 
Zekollari, Harry 
Kittel, Christoph  ;  Université de Liège - ULiège > Département de géographie > Climatologie et Topoclimatologie
Farinotti, Daniel 
Lhermitte, Stef 
Debaille, Vinciane 
Goderis, Steven 
Claeys, Philippe  ;  Université de Liège - ULiège > Département de géologie > Early Life Traces & Evolution-Astrobiology
Joy, Katherine Helen 
Pattyn, Frank 
Language :
English
Title :
Antarctic meteorites threatened by climate warming
Publication date :
08 April 2024
Journal title :
Nature Climate Change
ISSN :
1758-678X
eISSN :
1758-6798
Publisher :
Springer Science and Business Media LLC
Peer reviewed :
Peer Reviewed verified by ORBi
Tags :
CÉCI : Consortium des Équipements de Calcul Intensif
Funders :
F.R.S.-FNRS - Fonds de la Recherche Scientifique [BE]
BELSPO - Belgian Federal Science Policy Office [BE]
EU - European Union [BE]
Funding text :
This study is dedicated in loving memory to Pietro De Bernardini. V.T. is a Research Fellow of the Fonds de la Recherche Scientifique (FRS-FNRS). V.T., H.Z. and F.P. were supported by the Belgian Federal Science Policy Office (BELSPO; FROID project) and an Université libre de Bruxelles (ULB) Action Blanches project (QUOI). H.Z. acknowledges funding received as a postdoctoral fellowship (chargé de recherches) of the FRS-FNRS, from the research foundation Flanders (FWO) through an Odysseus Type II project (grant agreement number G0DCA23N; ‘GlaciersMD’ project) and from the European Research Council (ERC) under the European Union’s Horizon Framework research and innovation programme (grant agreement number 101115565; ‘ICE3’ project). H.Z., S.L. and F.P. were supported by the European Union’s Horizon 2020 research and innovation programme under grant agreement number 869304 (PROTECT). C.K. was supported by the European Union’s Horizon 2020 research and innovation programme under grant agreement number 101003826 via project CRiceS (climate relevant interactions and feedbacks: the key role of sea ice and snow in the polar and global climate system). V.D., S.G. and P.C. thank BELSPO (BELAM, Amundsen and BAMM! projects) for supporting the Antarctic field expeditions. V.D. thanks the ERC StG ISoSyC and FRS-FNRS for funding. S.G., P.C. and V.D. were supported by the Excellence of Science (EoS) project ‘ET-HoME.’ S.G. and P.C. were also supported by the FWO and the VUB strategic programme. K.H.J. is funded by the Royal Society (grant numbers URF\R\201009 and RF\ERE\210158) and STFC (grant number ST/V000675/1). We would like to thank the Lost Meteorites of Antarctica project field team for their work in collecting the samples (supported by Leverhulme Trust grant number RPG-2016–349, The British Antarctic Survey/NERC and UoM internal Faculty of Science and Engineering funding). We also thank the ANSMET programme for collecting and documenting meteorite MIL 07710 shown in Fig. 1.
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