Article
Geochemistry & Geophysics
C. W. Nooitgedacht, H. J. L. van der Lubbe, S. de Graaf, M. Ziegler, P. T. Staudigel, J. J. G. Reijmer
Summary: The distribution of oxygen isotopes between calcite and fluid inclusions is useful for reconstructing near-surface calcite precipitation temperatures, but its resilience to diagenetic oxygen isotope alteration in deep-formed calcite is poorly understood. Clumped isotopes are also vulnerable to diagenetic alteration, with post-entrapment isotope exchange potentially affecting the calcite-fluid oxygen isotope distribution and clumped isotope composition. The sensitivity of the fluid inclusion thermometer to isotopic alteration is higher than that of the clumped isotope thermometer, with the mass balance of oxygen between calcite and fluid inclusions determining their vulnerability to diagenetic overprinting.
GEOCHIMICA ET COSMOCHIMICA ACTA
(2021)
Article
Geochemistry & Geophysics
C. W. Nooitgedacht, H. J. L. van der Lubbe, M. Ziegler, P. T. Staudigel
Summary: The study reveals that biogenic aragonite undergoes significant oxygen isotope exchange with internal water during heating, affecting the reconstruction of paleotemperatures. In contrast, inorganic aragonite does not exhibit oxygen isotope exchange, suggesting a link between internal oxygen isotope exchange and Δ(47) resetting. Water-aragonite exchange occurs at lower temperatures and may have occurred earlier during the burial of biogenic aragonites.
GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS
(2021)
Article
Geochemistry & Geophysics
K. Prasanna, Prosenjit Ghosh, Robert A. Eagle, Aradhna Tripati, Vivesh V. Kapur, Richard F. Feeney, Benjamin R. Fosu, Divya Mishra
Summary: Carbonate clumped isotope thermometry provides a method to estimate water temperature independently of the δO-18 value, and the new calibration technique presented in this study shows promising results in accurately determining environmental conditions in modern and ancient settings. The study suggests that the δO-18 values in fish otoliths reflect kinetic effects and environmental conditions, with potential diagenesis effects also taken into consideration.
GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS
(2021)
Article
Geochemistry & Geophysics
Guilhem Hoareau, Nemo Crognier, Brice Lacroix, Charles Aubourg, Nick M. W. Roberts, Nathan Niemi, Mathieu Branellec, Nicolas Beaudoin, Isabel Suarez Ruiz
Summary: Clumped isotopes thermometry and U-Pb dating were used to study 10 tectonic calcite veins in the South Pyrenean Frontal Thrust, with results suggesting the veins recorded the end of Pyrenean tectonics at a younger age than previously estimated. These methods show potential in deciphering vein formation history in complex tectonic zones with the knowledge of thermal evolution and clumped isotope reordering extent.
EARTH AND PLANETARY SCIENCE LETTERS
(2021)
Article
Multidisciplinary Sciences
Yixiong Wen, Laiming Zhang, Ann E. Holbourn, Chenguang Zhu, Katharine W. Huntington, Tianjie Jin, Yalin Li, Chengshan Wang
Summary: During the Late Miocene, as the oceans cooled significantly, there was enhanced aridification and restructuring of vegetation and animal communities in vast areas of continents. Debate continues over whether global cooling induced by pCO(2) was the primary driver of this climate and ecosystem upheaval on land. This study presents a record of land surface temperatures (LST) in East Asia from 8 to 5 Ma using paleosol carbonate clumped isotopes and climate model simulations, showing a cooling of LST by approximately 7 degrees C between 7.5 and 5.7 Ma, followed by rapid warming across the Miocene-Pliocene transition (5.5 to 5 Ma). These changes occurred simultaneously with variations in sea surface temperatures, hydroclimate, and ecosystem shifts in East Asia, indicating a global climate forcing mechanism. Modeling experiments also demonstrate that pCO(2)-forced cooling would have caused extensive aridification in East Asia by altering moisture transfer and pathways. Thus, the conclusion is that the hydroclimate and ecosystem shift in East Asia during 8 to 5 Ma were primarily controlled by pCO(2)-forced global cooling.
PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA
(2023)
Article
Geochemistry & Geophysics
Jade Z. Zhang, Sierra V. Petersen
Summary: Geochemical signatures preserved in the geological record can be used to reconstruct past mean temperature and seasonality. A study was conducted to assess the ability of multiple isotope techniques in recording temperature variations in the bivalve Lucina pensylvanica. Comparisons were made between different thermometry methods to determine the most accurate approach for fossil shell analysis. The findings suggest that averaging seasonally-targeted Delta(47)-temperatures best match mean annual temperature, while averaging delta O-18(carb)-based temperatures from different seasons accurately represents seasonality.
Article
Geochemistry & Geophysics
Daniel L. Eldridge, Andrew C. Turner, Markus Bill, Mark E. Conrad, Daniel A. Stolper
Summary: Methane clumped isotope compositions are used as a new isotopic tool to trace the sources, sinks, and lifecycles of methane in the environment. Natural thermogenic methane can have clumped isotope compositions consistent with equilibrium or non-equilibrium processes. Isothermal time-series ethane pyrolysis experiments were conducted to explore the controls on the isotopic composition of thermogenic methane.
GEOCHIMICA ET COSMOCHIMICA ACTA
(2023)
Article
Geosciences, Multidisciplinary
Arun K. Ojha, Deepak C. Srivastava, Rajesh Sharma
Summary: This study utilizes veins, striated faults, and fluid inclusions to investigate the tectonic stresses and fluid evolution in the South Almora Thrust Zone. The analysis reveals four different stress states and the presence of multiple seismic events during the Late Oligocene-Early Miocene.
JOURNAL OF STRUCTURAL GEOLOGY
(2022)
Article
Geochemistry & Geophysics
Philip Staudigel, Chelsea Pederson, Jeroen van der Lubbe, Miguel Bernecker, Mattia Tagliavento, Amelia Davies, Adrian Immenhauser, Jens Fiebig
Summary: The study focuses on the geochemical and ultrastructural properties of thermally altered skeletal carbonate, emphasizing the importance of using models to quantitatively describe diagenetic processes and validating them with clumped isotope analysis.
GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS
(2023)
Article
Geochemistry & Geophysics
P. Staudigel, A. J. Davies, M. Bernecker, M. Tagliavento, H. J. L. van der Lubbe, C. Nooitgedacht, N. Looser, S. M. Bernasconi, H. Vonhof, J. Fiebig
Summary: Geochemical analyses of carbonate minerals provide insight into temperature and water composition during formation, while fluid trapped in minerals can be used to reconstruct paleotemperatures and diagenetic processes. The Delta(47)-Delta(48) dual-clumped isotope thermometer is highly sensitive to water/carbonate ratio and behaves differently in rock-buffered and water-dominated systems. Heating experiments and evaluation of sampling methods demonstrate the potential of this approach in understanding kinetic processes in biomineralization and resolving ambiguities in climate records.
GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS
(2023)
Article
Geochemistry & Geophysics
Attila Demeny, Laszlo Rinyu, Zoltan Kern, Istvan G. Hatvani, Gyorgy Czuppon, Gergely Suranyi, Szabolcs Leel-Ossy, Chuan-Chou Shen, Gabriella Koltai
Summary: The combined use of stable isotope compositions of speleothem carbonate and inclusion-hosted water shows great potential in paleotemperature reconstructions. Different approaches were evaluated for hydrogen and oxygen isotope measurements of inclusion-hosted water and host calcite. The results indicated that hydrogen isotope data may yield realistic temperatures under certain conditions.
Editorial Material
Geosciences, Multidisciplinary
Raphael Pietzsch
Summary: The study suggests that sediments in the South Atlantic basins may have been influenced by hydrothermal fluids, but the current evidence is not sufficient to definitively support this hypothesis, therefore further scrutiny is needed.
MARINE AND PETROLEUM GEOLOGY
(2021)
Article
Geosciences, Multidisciplinary
K. Methner, A. Mulch, J. Fiebig, E. Krsnik, N. Loeffler, D. Bajnai, C. P. Chamberlain
Summary: The study suggests that during the Miocene Climatic Optimum (MCO; ca. 17-15 Ma), the climate in the Northern Rocky Mountain (NRM) region was relatively stable and warm, with temperature records indicating a range from 17°C to 24°C. This stability was reflected in the Delta(47) temperature record and the carbon isotope values, suggesting consistent environmental conditions throughout the MCO period.
PALEOCEANOGRAPHY AND PALEOCLIMATOLOGY
(2021)
Article
Energy & Fuels
Yi-Chia Lu, Sheng-Rong Song, Ling-Wen Liu, Tsung-Ren Peng, Bill Bing-Cheng Chen, Remy Kai-Cheng Tu, Li-Hung Lin, Pei-Ling Wang
Summary: The temperature and oxygen isotope composition of fluids in a geothermal system can be determined using carbonate clumped isotope analysis, which is crucial for understanding the thermal structure and hydrothermal fluid characteristics. A study conducted in Taiwan's Tuchang-Jentse geothermal field analyzed the clumped isotope geochemistry of veins and travertines to investigate past tectonic activities and present reservoir conditions. The findings suggest that the high Delta 47-T and low calculated delta O-18(fluid) values of rhombic calcite indicate mixing of magmatic/metamorphic fluids with meteoric water, while the presence of low delta O-18(fluid) and high Delta 47-T in travertines near faults indicates heating or mixing with deep fluid. The application of carbonate clumped isotope thermometry provides accurate temperature estimates during the exploration phase and valuable information for future site selection.
Article
Geochemistry & Geophysics
Philip T. Staudigel, John A. Higgins, Peter K. Swart
Summary: This study utilized a numerical model and various isotope measurement techniques to investigate the changes in fluid advection rates over time, revealing a significant shift in the relative contributions of different mechanisms governing fluid flow around 13 million years ago.
EARTH AND PLANETARY SCIENCE LETTERS
(2021)
Article
Spectroscopy
Lucie Le Van-Jodin, Denis Rouchon, Van-Hoan Le, Isabelle Chevalier, Jean Brun, Christophe Secouard
JOURNAL OF RAMAN SPECTROSCOPY
(2019)
Article
Chemistry, Analytical
Van-Hoan Le, Marie-Camille Caumon, Alexandre Tarantola, Aurelien Randi, Pascal Robert, Josef Mullis
ANALYTICAL CHEMISTRY
(2019)
Article
Geochemistry & Geophysics
Van-Hoan Le, Marie-Camille Caumon, Alexandre Tarantola, Aurelien Randi, Pascal Robert, Josef Mullis
Article
Computer Science, Interdisciplinary Applications
Van-Hoan Le, Marie-Camille Caumon, Alexandre Tarantola
Summary: Numerous calibration data linking Raman spectral parameters with PVX properties of different gases have been published, but discrepancies exist between them. This paper examines the inter-laboratory applicability of existing calibration data and provides universal calibration data and a user-friendly interface for measurements. The FRAnCIs Python interface facilitates the application of these calibrations and estimates measurement uncertainty.
COMPUTERS & GEOSCIENCES
(2021)
Article
Materials Science, Coatings & Films
Petros Abi Younes, Ashok-Kumar Yadav, Medet Zhukush, Van-Hoan Le, Herve Roussel, Marie-Ingrid Richard, Clement Camp, Kai Szeto, Gianluca Ciatto, Nathanaelle Schneider, Elsje Alessandra Quadrelli, Hubert Renevier, Nicolas Gauthier
Summary: Amorphous organic-inorganic hybrid thin films (Ti-thiolate) on thermal SiO2 substrate are converted into textured titanium disulfide (TiS2) ultrathin films through annealing under Ar/H-2 atmosphere. Two annealing strategies were investigated to control the mineralization process. The stoichiometry and crystallinity of the films were characterized by various techniques.
JOURNAL OF VACUUM SCIENCE & TECHNOLOGY A
(2023)
Article
Chemistry, Physical
Van-Hoan Le, Alexandre Tarantola, Marie-Camille Caumon
Summary: This study aims to interpret the physical mechanisms behind the pressure-induced vibrational frequency shifts of CH4 and N-2 in binary mixtures such as CH4-CO2, N-2-CO2, and CH4-N-2, using two theoretical models and providing a predictive model for the frequency shift of the CH4 nu(1) band as a function of pressure, density, and composition.
PHYSICAL CHEMISTRY CHEMICAL PHYSICS
(2021)
Article
Geochemistry & Geophysics
Lingyu Zhang, Kristoffer Szilas
Summary: This study presents new petrological and geochemical data for the Narssaq Ultramafic Body (NUB) in the Itsaq Gneiss Complex of SW Greenland. The results indicate that the ultramafic rocks of NUB are not mantle residues, but instead represent crustal cumulates derived from high-Mg magmas.
EARTH AND PLANETARY SCIENCE LETTERS
(2024)
Article
Geochemistry & Geophysics
Rong Xu, Sarah Lambart, Oliver Nebel, Ming Li, Zhongjie Bai, Junbo Zhang, Ganglan Zhang, Jianfeng Gao, Hong Zhong, Yongsheng Liu
Summary: This study investigated the iron isotope compositions of Cenozoic basalts in Southeast China, finding significant variations related to different types of basalts and their respective sources.
EARTH AND PLANETARY SCIENCE LETTERS
(2024)
Article
Geochemistry & Geophysics
C. J. Ebinger, Miriam C. Reiss, Ian Bastow, Mary M. Karanja
Summary: The East African rift system is formed above mantle upwellings and the formation of rifts is related to lithospheric thinning and magmatic activity. The amount of splitting varies spatially and the fast axes are predominantly parallel to the orientation of the rifts. Thick lithospheric modules have less splitting and different orientations, which may indicate mantle plume flow. Splitting rotates and increases in strength as it enters the rift zones, suggesting that the anisotropy is mainly present at shallow depths.
EARTH AND PLANETARY SCIENCE LETTERS
(2024)
Correction
Geochemistry & Geophysics
Ekaterina Rojas-Kolomiets, Owen Jensen, Michael Bizimis, Gene Yogodzinski, Lukas Ackerman
EARTH AND PLANETARY SCIENCE LETTERS
(2024)
Article
Geochemistry & Geophysics
Robert W. Nicklas, Igor S. Puchtel, Ethan F. Baxter
Summary: Oxygen fugacity is a fundamental parameter for understanding redox processes in igneous systems. This study compares the Fe-XANES oxybarometry method with the V-in-olivine method for evaluating fO(2) in MORB lavas. The results show that the V-in-olivine method is not applicable to samples with low MgO content, and that the majority of Archean komatiite sources have lower fO(2) than modern MORB.
EARTH AND PLANETARY SCIENCE LETTERS
(2024)
Article
Geochemistry & Geophysics
Chunfei Chen, Stephen F. Foley, Sebastian Tappe, Huange Ren, Lanping Feng, Yongsheng Liu
Summary: The volatile components CO2 and H2O play a major role in mantle melting and heterogeneity. In this study, Ca isotopes were used to trace the lithological heterogeneity in alkaline magmatic rocks. The results revealed the presence of K-richterite and carbonate components as the source of alkaline magmas with low delta 44/40Ca values. These findings highlight the importance of Ca isotopes as a robust tracer of lithological variation caused by volatiles in the Earth's upper mantle.
EARTH AND PLANETARY SCIENCE LETTERS
(2024)
Article
Geochemistry & Geophysics
Timothee Jautzy, Gilles Rixhon, Regis Braucher, Romain Delunel, Pierre G. Valla, Laurent Schmitt, Aster Team
Summary: Although the current approach to estimate catchment-wide denudation rates using only 10Be concentrations has made significant progress in geomorphology, this study argues for the inclusion of 26Al measurements and testing of steady-state assumptions in slow eroding, formerly glaciated landscapes. The study conducted measurements of both 10Be and 26Al in stream sediments from the Vosges Massif in France and found that elevation, slope, channel steepness, and precipitation were the primary factors controlling denudation rates. The study also revealed a significant relationship between the extent of past glaciation and the cosmogenic (un-)steadiness in the stream sediments.
EARTH AND PLANETARY SCIENCE LETTERS
(2024)
Article
Geochemistry & Geophysics
Erik van der Wiel, Douwe J. J. van Hinsbergen, Cedric Thieulot, Wim Spakman
Summary: Numerical models of Earth's mantle dynamics can predict the vigour and mixing of mantle flow, and the average slab sinking rates are an unexplored parameter that can provide intrinsic information on these characteristics. Through numerical experiments, it has been found that slab sinking rates are strongly correlated with mantle convection and mixing, and may explain geochemical observations from hotspot volcanoes.
EARTH AND PLANETARY SCIENCE LETTERS
(2024)