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Meckler AN, Sexton PF, Piasecki AM, Leutert TJ, Marquardt J, Ziegler M, Agterhuis T, Lourens LJ, Rae JWB, Barnet J, Tripati A, Bernasconi SM. Cenozoic evolution of deep ocean temperature from clumped isotope thermometry. Science 2022; 377:86-90. [PMID: 35771913 DOI: 10.1126/science.abk0604] [Citation(s) in RCA: 5] [Impact Index Per Article: 2.5] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/02/2022]
Abstract
Characterizing past climate states is crucial for understanding the future consequences of ongoing greenhouse gas emissions. Here, we revisit the benchmark time series for deep ocean temperature across the past 65 million years using clumped isotope thermometry. Our temperature estimates from the deep Atlantic Ocean are overall much warmer compared with oxygen isotope-based reconstructions, highlighting the likely influence of changes in deep ocean pH and/or seawater oxygen isotope composition on classical oxygen isotope records of the Cenozoic. In addition, our data reveal previously unrecognized large swings in deep ocean temperature during early Eocene acute greenhouse warmth. Our results call for a reassessment of the Cenozoic history of ocean temperatures to achieve a more accurate understanding of the nature of climatic responses to tectonic events and variable greenhouse forcing.
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Affiliation(s)
- A N Meckler
- Bjerknes Centre for Climate Research and Department of Earth Science, University of Bergen, Bergen, Norway
| | - P F Sexton
- School of Environment, Earth and Ecosystem Sciences, The Open University, Milton Keynes, UK
| | - A M Piasecki
- Bjerknes Centre for Climate Research and Department of Earth Science, University of Bergen, Bergen, Norway
| | - T J Leutert
- Bjerknes Centre for Climate Research and Department of Earth Science, University of Bergen, Bergen, Norway
| | - J Marquardt
- Bjerknes Centre for Climate Research and Department of Earth Science, University of Bergen, Bergen, Norway
| | - M Ziegler
- Faculty of Geosciences, Utrecht University, Utrecht, Netherlands
| | - T Agterhuis
- Faculty of Geosciences, Utrecht University, Utrecht, Netherlands
| | - L J Lourens
- Faculty of Geosciences, Utrecht University, Utrecht, Netherlands
| | - J W B Rae
- School of Earth and Environmental Sciences, University of St. Andrews, St. Andrews, UK
| | - J Barnet
- School of Earth and Environmental Sciences, University of St. Andrews, St. Andrews, UK
| | - A Tripati
- Department of Earth, Planetary, and Space Science, Department of Atmospheric and Oceanic Science, Institute of the Environment and Sustainability, American Indian Studies Center, Center for Diverse Leadership in Science, University of California, Los Angeles, Los Angeles, USA
| | - S M Bernasconi
- Department of Earth Science, ETH Zürich, Zürich, Switzerland
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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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Caesar KH, Kyle JR, Lyons TW, Tripati A, Loyd SJ. Carbonate formation in salt dome cap rocks by microbial anaerobic oxidation of methane. Nat Commun 2019; 10:808. [PMID: 30778057 PMCID: PMC6379371 DOI: 10.1038/s41467-019-08687-z] [Citation(s) in RCA: 18] [Impact Index Per Article: 3.6] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [MESH Headings] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 10/17/2017] [Accepted: 01/22/2019] [Indexed: 11/20/2022] Open
Abstract
Major hydrocarbon accumulations occur in traps associated with salt domes. Whereas some of these hydrocarbons remain to be extracted for economic use, significant amounts have degraded in the subsurface, yielding mineral precipitates as byproducts. Salt domes of the Gulf of Mexico Basin typically exhibit extensive deposits of carbonate that form as cap rock atop salt structures. Despite previous efforts to model cap rock formation, the details of subsurface reactions (including the role of microorganisms) remain largely unknown. Here we show that cap rock mineral precipitation occurred via closed-system sulfate reduction, as indicated by new sulfur isotope data. 13C-depleted carbonate carbon isotope compositions and low clumped isotope-derived carbonate formation temperatures indicate that microbial, sulfate-dependent, anaerobic oxidation of methane (AOM) contributed to carbonate formation. These findings suggest that AOM serves as an unrecognized methane sink that reduces methane emissions in salt dome settings perhaps associated with an extensive, deep subsurface biosphere.
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Affiliation(s)
- K H Caesar
- Department of Geological Sciences, California State University, Fullerton, 800 North State College Boulevard, Fullerton, CA, 92831, USA
| | - J R Kyle
- Department of Geological Sciences, University of Texas at Austin, 2275 Speedway Stop C9000, Austin, TX, 78712, USA
| | - T W Lyons
- Department of Earth Sciences, University of California, Riverside, 900 University Avenue, Riverside, CA, 92521, USA
| | - A Tripati
- Department of Earth, Space and Planetary Sciences, Department of Atmospheric and Oceanic Sciences, Institute of the Environment and Sustainability, University of California, Los Angeles, 595 Charles Young Drive, Los Angeles, CA, 90095, USA
| | - S J Loyd
- Department of Geological Sciences, California State University, Fullerton, 800 North State College Boulevard, Fullerton, CA, 92831, USA.
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Huntington KW, Eiler JM, Affek HP, Guo W, Bonifacie M, Yeung LY, Thiagarajan N, Passey B, Tripati A, Daëron M, Came R. Methods and limitations of 'clumped' CO2 isotope (Delta47) analysis by gas-source isotope ratio mass spectrometry. J Mass Spectrom 2009; 44:1318-1329. [PMID: 19621330 DOI: 10.1002/jms.1614] [Citation(s) in RCA: 70] [Impact Index Per Article: 4.7] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 05/28/2023]
Abstract
The geochemistry of multiply substituted isotopologues ('clumped-isotope' geochemistry) examines the abundances in natural materials of molecules, formula units or moieties that contain more than one rare isotope (e.g. (13)C(18)O(16)O, (18)O(18)O, (15)N(2), (13)C(18)O(16)O(2) (2-)). Such species form the basis of carbonate clumped-isotope thermometry and undergo distinctive fractionations during a variety of natural processes, but initial reports have provided few details of their analysis. In this study, we present detailed data and arguments regarding the theoretical and practical limits of precision, methods of standardization, instrument linearity and related issues for clumped-isotope analysis by dual-inlet gas-source isotope ratio mass spectrometry (IRMS). We demonstrate long-term stability and subtenth per mil precision in 47/44 ratios for counting systems consisting of a Faraday cup registered through a 10(12) ohm resistor on three Thermo-Finnigan 253 IRMS systems. Based on the analyses of heated CO(2) gases, which have a stochastic distribution of isotopes among possible isotopologues, we document and correct for (1) isotopic exchange among analyte CO(2) molecules and (2) subtle nonlinearity in the relationship between actual and measured 47/44 ratios. External precisions of approximately 0.01 per thousand are routinely achieved for measurements of the mass-47 anomaly (a measure mostly of the abundance anomaly of (13)C-(18)O bonds) and follow counting statistics. The present technical limit to precision intrinsic to our methods and instrumentation is approximately 5 parts per million (ppm), whereas precisions of measurements of heterogeneous natural materials are more typically approximately 10 ppm (both 1 s.e.). These correspond to errors in carbonate clumped-isotope thermometry of +/-1.2 degrees C and +/-2.4 degrees C, respectively.
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Affiliation(s)
- K W Huntington
- Department of Earth and Space Sciences, University of Washington, Seattle, WA 98195, USA.
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