Magnesium in subaqueous speleothems as a potential palaeotemperature proxy
dc.contributor.author | Drysdale, Russell N | |
dc.contributor.author | Couchoud, Isabelle | |
dc.contributor.author | Zanchetta, G | |
dc.contributor.author | Isola, I. | |
dc.contributor.author | Regattieri, Eleonora | |
dc.contributor.author | Hellstrom, John Charles | |
dc.contributor.author | Govin, Aline | |
dc.contributor.author | Tzedakis, C. | |
dc.contributor.author | Ireland, Trevor | |
dc.contributor.author | Corrick, Ellen | |
dc.contributor.author | Greig, Alan | |
dc.contributor.author | Holden, Peter | |
dc.date.accessioned | 2022-06-07T03:58:44Z | |
dc.date.available | 2022-06-07T03:58:44Z | |
dc.date.issued | 2020 | |
dc.date.updated | 2021-01-17T07:18:26Z | |
dc.description.abstract | Few palaeoclimate archives beyond the polar regions preserve continuous and datable palaeotemperature proxy time series over multiple glacial-interglacial cycles. This hampers efforts to develop a more coherent picture of global patterns of past temperatures. Here we show that Mg concentrations in a subaqueous speleothem from an Italian cave track regional sea-surface temperatures over the last 350,000 years. The Mg shows higher values during warm climate intervals and converse patterns during cold climate stages. In contrast to previous studies, this implicates temperature, not rainfall, as the principal driver of Mg variability. The depositional setting of the speleothem gives rise to Mg partition coefficients that are more temperature dependent than other calcites, enabling the effect of temperature change on Mg partitioning to greatly exceed the effects of changes in source-water Mg/Ca. Subaqueous speleothems from similar deep-cave environments should be capable of providing palaeotemperature information over multiple glacial-interglacial cycles. | en_AU |
dc.format.mimetype | application/pdf | en_AU |
dc.identifier.issn | 2041-1723 | en_AU |
dc.identifier.uri | http://hdl.handle.net/1885/267180 | |
dc.language.iso | en_AU | en_AU |
dc.provenance | This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/ licenses/by/4.0/. | en_AU |
dc.publisher | Macmillan Publishers Ltd | en_AU |
dc.relation | http://purl.org/au-research/grants/arc/DP0773700 | en_AU |
dc.relation | http://purl.org/au-research/grants/arc/DP110102185 | en_AU |
dc.relation | http://purl.org/au-research/grants/arc/DP160102969 | en_AU |
dc.rights | © 2020 The authors | en_AU |
dc.rights.license | creative commons | en_AU |
dc.rights.uri | http://creativeco mmons.org/licenses/by/4.0/ | en_AU |
dc.source | Nature Communications | en_AU |
dc.title | Magnesium in subaqueous speleothems as a potential palaeotemperature proxy | en_AU |
dc.type | Journal article | en_AU |
dcterms.accessRights | Open Access | en_AU |
local.bibliographicCitation.issue | 5027 | en_AU |
local.bibliographicCitation.lastpage | 11 | en_AU |
local.bibliographicCitation.startpage | 1 | en_AU |
local.contributor.affiliation | Drysdale, Russell N, University of Melbourne | en_AU |
local.contributor.affiliation | Couchoud, Isabelle, Universite de Savoie-CNRS | en_AU |
local.contributor.affiliation | Zanchetta, G, University of Pisa | en_AU |
local.contributor.affiliation | Isola, I., Instituto Nazionale di Geofisica e Vulcanologia | en_AU |
local.contributor.affiliation | Regattieri, Eleonora, Istituto di Geoscienze e Georisorse | en_AU |
local.contributor.affiliation | Hellstrom, John Charles, University of Melbourne | en_AU |
local.contributor.affiliation | Govin, Aline, Paris-Saclay University | en_AU |
local.contributor.affiliation | Tzedakis, C., University College London | en_AU |
local.contributor.affiliation | Ireland, Trevor, College of Science, ANU | en_AU |
local.contributor.affiliation | Corrick, Ellen, The University of Melbourne | en_AU |
local.contributor.affiliation | Greig, Alan, University of Melbourne | en_AU |
local.contributor.affiliation | Holden, Peter, College of Science, ANU | en_AU |
local.contributor.authoremail | u8205445@anu.edu.au | en_AU |
local.contributor.authoruid | Ireland, Trevor, u8205445 | en_AU |
local.contributor.authoruid | Holden, Peter, u4044970 | en_AU |
local.description.notes | Imported from ARIES | en_AU |
local.identifier.absfor | 040303 - Geochronology | en_AU |
local.identifier.absfor | 040605 - Palaeoclimatology | en_AU |
local.identifier.absseo | 970104 - Expanding Knowledge in the Earth Sciences | en_AU |
local.identifier.ariespublication | a383154xPUB15046 | en_AU |
local.identifier.citationvolume | 11 | en_AU |
local.identifier.doi | 10.1038/s41467-020-18083-7 | en_AU |
local.identifier.uidSubmittedBy | a383154 | en_AU |
local.publisher.url | https://www.nature.com/ | en_AU |
local.type.status | Published Version | en_AU |
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