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Bernasconi SM, Daëron M, Bergmann KD, Bonifacie M, Meckler AN, Affek HP, Anderson N, Bajnai D, Barkan E, Beverly E, Blamart D, Burgener L, Calmels D, Chaduteau C, Clog M, Davidheiser‐Kroll B, Davies A, Dux F, Eiler J, Elliott B, Fetrow AC, Fiebig J, Goldberg S, Hermoso M, Huntington KW, Hyland E, Ingalls M, Jaggi M, John CM, Jost AB, Katz S, Kelson J, Kluge T, Kocken IJ, Laskar A, Leutert TJ, Liang D, Lucarelli J, Mackey TJ, Mangenot X, Meinicke N, Modestou SE, Müller IA, Murray S, Neary A, Packard N, Passey BH, Pelletier E, Petersen S, Piasecki A, Schauer A, Snell KE, Swart PK, Tripati A, Upadhyay D, Vennemann T, Winkelstern I, Yarian D, Yoshida N, Zhang N, Ziegler M. InterCarb: A Community Effort to Improve Interlaboratory Standardization of the Carbonate Clumped Isotope Thermometer Using Carbonate Standards. Geochem Geophys Geosyst 2021; 22:e2020GC009588. [PMID: 34220359 PMCID: PMC8244079 DOI: 10.1029/2020gc009588] [Citation(s) in RCA: 21] [Impact Index Per Article: 7.0] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 12/11/2020] [Revised: 03/18/2021] [Accepted: 03/19/2021] [Indexed: 06/12/2023]
Abstract
Increased use and improved methodology of carbonate clumped isotope thermometry has greatly enhanced our ability to interrogate a suite of Earth-system processes. However, interlaboratory discrepancies in quantifying carbonate clumped isotope (Δ47) measurements persist, and their specific sources remain unclear. To address interlaboratory differences, we first provide consensus values from the clumped isotope community for four carbonate standards relative to heated and equilibrated gases with 1,819 individual analyses from 10 laboratories. Then we analyzed the four carbonate standards along with three additional standards, spanning a broad range of δ47 and Δ47 values, for a total of 5,329 analyses on 25 individual mass spectrometers from 22 different laboratories. Treating three of the materials as known standards and the other four as unknowns, we find that the use of carbonate reference materials is a robust method for standardization that yields interlaboratory discrepancies entirely consistent with intralaboratory analytical uncertainties. Carbonate reference materials, along with measurement and data processing practices described herein, provide the carbonate clumped isotope community with a robust approach to achieve interlaboratory agreement as we continue to use and improve this powerful geochemical tool. We propose that carbonate clumped isotope data normalized to the carbonate reference materials described in this publication should be reported as Δ47 (I-CDES) values for Intercarb-Carbon Dioxide Equilibrium Scale.
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Affiliation(s)
| | - M. Daëron
- Laboratoire des Sciences du Climat et de l’EnvironnementLSCE/IPSLCEA‐CNRS‐UVSQUniversité Paris‐SaclayGif‐sur‐YvetteFrance
| | - K. D. Bergmann
- Department of Earth, Atmospheric and Planetary SciencesMassachusetts Institute of TechnologyCambridgeMAUSA
| | - M. Bonifacie
- Université de ParisInstitut de Physique du Globe de ParisCNRSParisFrance
| | - A. N. Meckler
- Bjerknes Centre for Climate Research and Department of Earth ScienceUniversity of BergenBergenNorway
| | - H. P. Affek
- Institute of Earth SciencesHebrew University of JerusalemJerusalemIsrael
| | - N. Anderson
- Department of Earth, Atmospheric and Planetary SciencesMassachusetts Institute of TechnologyCambridgeMAUSA
| | - D. Bajnai
- Institute of GeosciencesGoethe University FrankfurtFrankfurt am MainGermany
| | - E. Barkan
- Institute of Earth SciencesHebrew University of JerusalemJerusalemIsrael
| | - E. Beverly
- Now at Department of Earth and Atmospheric SciencesUniversity of HoustonHoustonTXUSA
- Department of Earth and Environmental SciencesUniversity of MichiganAnn ArborMIUSA
| | - D. Blamart
- Laboratoire des Sciences du Climat et de l’EnvironnementLSCE/IPSLCEA‐CNRS‐UVSQUniversité Paris‐SaclayGif‐sur‐YvetteFrance
| | - L. Burgener
- Department of Marine, Earth and Atmospheric SciencesNorth Carolina State UniversityRaleighNCUSA
| | - D. Calmels
- Université de ParisInstitut de Physique du Globe de ParisCNRSParisFrance
- Now at Geosciences Paris Sud (GEOPS)Université Paris‐SaclayCNRSOrsayFrance
| | - C. Chaduteau
- Université de ParisInstitut de Physique du Globe de ParisCNRSParisFrance
| | - M. Clog
- Scottish Universities Environmental Research Centre (SUERC)ScotlandUK
| | | | - A. Davies
- Now at Stockholm UniversityStockholmSweden
- Imperial CollegeLondonUK
| | - F. Dux
- Now at School of Earth and Life SciencesUniversity of WollongongWollongongAustralia
- School of GeographyUniversity of MelbourneMelbourneAustralia
| | - J. Eiler
- Geological and Planetary SciencesCalifornia Institute of TechnologyPasadenaCAUSA
| | - B. Elliott
- Department of Earth, Planetary, and Space SciencesUniversity of California Los AngelesLos AngelesCAUSA
| | | | - J. Fiebig
- Institute of GeosciencesGoethe University FrankfurtFrankfurt am MainGermany
| | - S. Goldberg
- Department of Earth, Atmospheric and Planetary SciencesMassachusetts Institute of TechnologyCambridgeMAUSA
| | - M. Hermoso
- Université de ParisInstitut de Physique du Globe de ParisCNRSParisFrance
- Univ. Littoral Côte d’OpaleUniv. LilleCNRSLaboratoire d’Océanologie et de Géosciences (UMR 8187 LOG)WimereuxFrance
| | | | - E. Hyland
- Department of Marine, Earth and Atmospheric SciencesNorth Carolina State UniversityRaleighNCUSA
| | - M. Ingalls
- Geological and Planetary SciencesCalifornia Institute of TechnologyPasadenaCAUSA
- Now at Department of GeosciencesThe Pennsylvania State UniversityUniversity ParkPAUSA
| | - M. Jaggi
- Geological InstituteETH ZürichZürichSwitzerland
| | | | - A. B. Jost
- Department of Earth, Atmospheric and Planetary SciencesMassachusetts Institute of TechnologyCambridgeMAUSA
| | - S. Katz
- Department of Earth and Environmental SciencesUniversity of MichiganAnn ArborMIUSA
| | - J. Kelson
- Department of Earth and Environmental SciencesUniversity of MichiganAnn ArborMIUSA
| | - T. Kluge
- Imperial CollegeLondonUK
- Now at Karlsruher Institut für Technologie KITKarlsruheGermany
| | - I. J. Kocken
- Department of Earth SciencesUniversity of UtrechtUtrechtThe Netherlands
| | - A. Laskar
- Institute of Earth SciencesAcademia SinicaTaipeiTaiwan
| | - T. J. Leutert
- Bjerknes Centre for Climate Research and Department of Earth ScienceUniversity of BergenBergenNorway
- Now at Max Planck Institute for ChemistryMainzGermany
| | - D. Liang
- Institute of Earth SciencesAcademia SinicaTaipeiTaiwan
| | - J. Lucarelli
- Department of Earth, Planetary, and Space SciencesUniversity of California Los AngelesLos AngelesCAUSA
| | - T. J. Mackey
- Department of Earth, Atmospheric and Planetary SciencesMassachusetts Institute of TechnologyCambridgeMAUSA
- Now at Department of Earth and Planetary SciencesUniversity of New MexicoAlbuquerqueNMUSA
| | - X. Mangenot
- Université de ParisInstitut de Physique du Globe de ParisCNRSParisFrance
- Geological and Planetary SciencesCalifornia Institute of TechnologyPasadenaCAUSA
| | - N. Meinicke
- Bjerknes Centre for Climate Research and Department of Earth ScienceUniversity of BergenBergenNorway
| | - S. E. Modestou
- Bjerknes Centre for Climate Research and Department of Earth ScienceUniversity of BergenBergenNorway
| | - I. A. Müller
- Department of Earth SciencesUniversity of UtrechtUtrechtThe Netherlands
| | | | - A. Neary
- Department of Earth and Environmental SciencesUniversity of MichiganAnn ArborMIUSA
| | - N. Packard
- Department of Earth and Environmental SciencesUniversity of MichiganAnn ArborMIUSA
| | - B. H. Passey
- Department of Earth and Environmental SciencesUniversity of MichiganAnn ArborMIUSA
| | - E. Pelletier
- Department of Earth and Environmental SciencesUniversity of MichiganAnn ArborMIUSA
| | - S. Petersen
- Department of Earth and Environmental SciencesUniversity of MichiganAnn ArborMIUSA
| | - A. Piasecki
- Bjerknes Centre for Climate Research and Department of Earth ScienceUniversity of BergenBergenNorway
- Now at Department of Earth SciencesDartmouth CollegeHanoverNHUSA
| | | | | | - P. K. Swart
- Department of Marine GeosciencesRostiel School of Marine and Atmospheric SciencesUniversity of MiamiMiamiFLUSA
| | - A. Tripati
- Department of Earth, Planetary, and Space SciencesUniversity of California Los AngelesLos AngelesCAUSA
| | - D. Upadhyay
- Department of Earth, Planetary, and Space SciencesUniversity of California Los AngelesLos AngelesCAUSA
| | - T. Vennemann
- Institute of Earth Surface DynamicsUniversity of LausanneLausanneSwitzerland
| | - I. Winkelstern
- Department of Earth and Environmental SciencesUniversity of MichiganAnn ArborMIUSA
- Now at Geology DepartmentGrand Valley State UniversityAllendaleMIUSA
| | - D. Yarian
- Department of Earth and Environmental SciencesUniversity of MichiganAnn ArborMIUSA
| | - N. Yoshida
- Earth‐Life Science InstituteTokyo Institute of TechnologyTokyoJapan
- National Institute of Information and Communications TechnologyTokyoJapan
| | - N. Zhang
- Earth‐Life Science InstituteTokyo Institute of TechnologyTokyoJapan
| | - M. Ziegler
- Department of Earth SciencesUniversity of UtrechtUtrechtThe Netherlands
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Daëron M, Drysdale RN, Peral M, Huyghe D, Blamart D, Coplen TB, Lartaud F, Zanchetta G. Most Earth-surface calcites precipitate out of isotopic equilibrium. Nat Commun 2019; 10:429. [PMID: 30683869 PMCID: PMC6347637 DOI: 10.1038/s41467-019-08336-5] [Citation(s) in RCA: 24] [Impact Index Per Article: 4.8] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 07/29/2018] [Accepted: 01/03/2019] [Indexed: 11/25/2022] Open
Abstract
Oxygen-isotope thermometry played a critical role in the rise of modern geochemistry and remains extensively used in (bio-)geoscience. Its theoretical foundations rest on the assumption that 18O/16O partitioning among water and carbonate minerals primarily reflects thermodynamic equilibrium. However, after decades of research, there is no consensus on the true equilibrium 18O/16O fractionation between calcite and water (18αcc/w). Here, we constrain the equilibrium relations linking temperature, 18αcc/w, and clumped isotopes (Δ47) based on the composition of extremely slow-growing calcites from Devils Hole and Laghetto Basso (Corchia Cave). Equilibrium 18αcc/w values are systematically ~1.5‰ greater than those in biogenic and synthetic calcite traditionally considered to approach oxygen-isotope equilibrium. We further demonstrate that subtle disequilibria also affect Δ47 in biogenic calcite. These observations provide evidence that most Earth-surface calcites fail to achieve isotopic equilibrium, highlighting the need to improve our quantitative understanding of non-equilibrium isotope fractionation effects instead of relying on phenomenological calibrations. Isotopic thermometry of carbonate minerals postulates that their composition reflects thermodynamic equilibrium constants. Here the authors constrain equilibrium relationships between temperature, 18O/16O and clumped isotopes and find that most natural calcites form out of isotopic equilibrium.
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Affiliation(s)
- M Daëron
- Laboratoire des Sciences du Climat et de l'Environnement, LSCE/IPSL, CEA-CNRS-UVSQ, Université Paris-Saclay, Orme des Merisiers, F-91191, Gif-sur-Yvette Cedex, France.
| | - R N Drysdale
- School of Geography, The University of Melbourne, 221 Bouverie Street, Carlton, VIC, 3053, Australia.,EDYTEM UMR CNRS 5204, Bâtiment "Pôle Montagne", Université Savoie Mont Blanc, 5 bd de la Mer Caspienne, F-73376, Le Bourget du Lac Cedex, France
| | - M Peral
- Laboratoire des Sciences du Climat et de l'Environnement, LSCE/IPSL, CEA-CNRS-UVSQ, Université Paris-Saclay, Orme des Merisiers, F-91191, Gif-sur-Yvette Cedex, France
| | - D Huyghe
- Laboratoire d'Ecogéochimie des Environnements Benthiques, LECOB, Sorbonne Université, CNRS, F-66650, Banyuls-sur-mer, France.,Géosciences Environnement Toulouse, UMR 5563 CNRS, UR 234 IRD, UM 97 UPS, Observatoire Midi-Pyrénées, CNES, 14 avenue Édouard Belin, 31400, Toulouse, France.,Centre de Géosciences, MINES ParisTech, PSL University, 35 rue St Honoré, 77305, Fontainebleau Cedex, France
| | - D Blamart
- Laboratoire des Sciences du Climat et de l'Environnement, LSCE/IPSL, CEA-CNRS-UVSQ, Université Paris-Saclay, Orme des Merisiers, F-91191, Gif-sur-Yvette Cedex, France
| | - T B Coplen
- U.S. Geological Survey, 12201 Sunrise Valley Drive, Reston, VA, 20192, USA
| | - F Lartaud
- Laboratoire d'Ecogéochimie des Environnements Benthiques, LECOB, Sorbonne Université, CNRS, F-66650, Banyuls-sur-mer, France
| | - G Zanchetta
- Dipartimento di Scienze della Terra, Università di Pisa, Via S. Maria 53, 56126, Pisa, Italy
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Genty D, Blamart D, Ouahdi R, Gilmour M, Baker A, Jouzel J, Van-Exter S. Precise dating of Dansgaard-Oeschger climate oscillations in western Europe from stalagmite data. Nature 2003; 421:833-7. [PMID: 12594510 DOI: 10.1038/nature01391] [Citation(s) in RCA: 43] [Impact Index Per Article: 2.0] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [MESH Headings] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 09/27/2002] [Accepted: 12/23/2002] [Indexed: 11/09/2022]
Abstract
The signature of Dansgaard-Oeschger events--millennial-scale abrupt climate oscillations during the last glacial period--is well established in ice cores and marine records. But the effects of such events in continental settings are not as clear, and their absolute chronology is uncertain beyond the limit of (14)C dating and annual layer counting for marine records and ice cores, respectively. Here we present carbon and oxygen isotope records from a stalagmite collected in southwest France which have been precisely dated using 234U/230Th ratios. We find rapid climate oscillations coincident with the established Dansgaard-Oeschger events between 83,000 and 32,000 years ago in both isotope records. The oxygen isotope signature is similar to a record from Soreq cave, Israel, and deep-sea records, indicating the large spatial scale of the climate oscillations. The signal in the carbon isotopes gives evidence of drastic and rapid vegetation changes in western Europe, an important site in human cultural evolution. We also find evidence for a long phase of extremely cold climate in southwest France between 61.2 +/- 0.6 and 67.4 +/- 0.9 kyr ago.
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Affiliation(s)
- D Genty
- IPSL/Laboratoire des Sciences du Climat et de l'Environnement, UMR CEA/CNRS 1572 Bat. 709, L'Orme des Merisiers CEA Saclay, 91191 Gif sur Yvette cedex, France.
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