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Wei GY, Zhao M, Sperling EA, Gaines RR, Kalderon-Asael B, Shen J, Li C, Zhang F, Li G, Zhou C, Cai C, Chen D, Xiao KQ, Jiang L, Ling HF, Planavsky NJ, Tarhan LG. Lithium isotopic constraints on the evolution of continental clay mineral factory and marine oxygenation in the earliest Paleozoic Era. SCIENCE ADVANCES 2024; 10:eadk2152. [PMID: 38552018 PMCID: PMC10980266 DOI: 10.1126/sciadv.adk2152] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Grants] [Track Full Text] [Download PDF] [Figures] [Subscribe] [Scholar Register] [Received: 08/08/2023] [Accepted: 02/26/2024] [Indexed: 04/01/2024]
Abstract
The evolution of oxygen cycles on Earth's surface has been regulated by the balance between molecular oxygen production and consumption. The Neoproterozoic-Paleozoic transition likely marks the second rise in atmospheric and oceanic oxygen levels, widely attributed to enhanced burial of organic carbon. However, it remains disputed how marine organic carbon production and burial respond to global environmental changes and whether these feedbacks trigger global oxygenation during this interval. Here, we report a large lithium isotopic and elemental dataset from marine mudstones spanning the upper Neoproterozoic to middle Cambrian [~660 million years ago (Ma) to 500 Ma]. These data indicate a dramatic increase in continental clay formation after ~525 Ma, likely linked to secular changes in global climate and compositions of the continental crust. Using a global biogeochemical model, we suggest that intensified continental weathering and clay delivery to the oceans could have notably increased the burial efficiency of organic carbon and facilitated greater oxygen accumulation in the earliest Paleozoic oceans.
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Affiliation(s)
- Guang-Yi Wei
- School of Earth Sciences and Engineering, and Frontiers Science Center for Critical Earth Material Cycling, Nanjing University, Nanjing 210023, China
- Department of Earth and Planetary Sciences, Yale University, New Haven, CT 06520-8109, USA
| | - Mingyu Zhao
- Department of Earth and Planetary Sciences, Yale University, New Haven, CT 06520-8109, USA
- Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, China
| | - Erik A. Sperling
- Department of Earth and Planetary Sciences, Stanford University, Stanford, CA 94305, USA
| | | | - Boriana Kalderon-Asael
- Department of Earth and Planetary Sciences, Yale University, New Haven, CT 06520-8109, USA
| | - Jun Shen
- State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, China
| | - Chao Li
- State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation and Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu 610059, China
- Key Laboratory of Deep-time Geography and Environment Reconstruction and Applications of Ministry of Natural Resources, Chengdu University of Technology, Chengdu 610059, China
- International Center for Sedimentary Geochemistry and Biogeochemistry Research, Chengdu University of Technology, Chengdu 610059, China
| | - Feifei Zhang
- School of Earth Sciences and Engineering, and Frontiers Science Center for Critical Earth Material Cycling, Nanjing University, Nanjing 210023, China
| | - Gaojun Li
- School of Earth Sciences and Engineering, and Frontiers Science Center for Critical Earth Material Cycling, Nanjing University, Nanjing 210023, China
| | - Chuanming Zhou
- State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, and Center for Excellence in Life and Palaeoenvironment, Chinese Academy of Sciences, Nanjing 210008, China
| | - Chunfang Cai
- Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, China
| | - Daizhao Chen
- Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, China
| | - Ke-Qing Xiao
- State Key Lab of Urban and Regional Ecology, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Shuangqing Rd. 18, 10085, Beijing, China
- University of Chinese Academy of Sciences, Beijing, 100049, China
| | - Lei Jiang
- Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, China
| | - Hong-Fei Ling
- School of Earth Sciences and Engineering, and Frontiers Science Center for Critical Earth Material Cycling, Nanjing University, Nanjing 210023, China
| | - Noah J. Planavsky
- Department of Earth and Planetary Sciences, Yale University, New Haven, CT 06520-8109, USA
| | - Lidya G. Tarhan
- Department of Earth and Planetary Sciences, Yale University, New Haven, CT 06520-8109, USA
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Anderson RP, Woltz CR, Tosca NJ, Porter SM, Briggs DEG. Fossilisation processes and our reading of animal antiquity. Trends Ecol Evol 2023; 38:1060-1071. [PMID: 37385847 DOI: 10.1016/j.tree.2023.05.014] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 03/05/2023] [Revised: 05/19/2023] [Accepted: 05/22/2023] [Indexed: 07/01/2023]
Abstract
Estimates for animal antiquity exhibit a significant disconnect between those from molecular clocks, which indicate crown animals evolved ∼800 million years ago (Ma), and those from the fossil record, which extends only ∼574 Ma. Taphonomy is often held culpable: early animals were too small/soft/fragile to fossilise, or the circumstances that preserve them were uncommon in the early Neoproterozoic. We assess this idea by comparing Neoproterozoic fossilisation processes with those of the Cambrian and its abundant animal fossils. Cambrian Burgess Shale-type (BST) preservation captures animals in mudstones showing a narrow range of mineralogies; yet, fossiliferous Neoproterozoic mudstones rarely share the same mineralogy. Animal fossils are absent where BST preservation occurs in deposits ≥789 Ma, suggesting a soft maximum constraint on animal antiquity.
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Affiliation(s)
- Ross P Anderson
- Department of Earth Sciences, University of Oxford, Oxford, OX1 3AN, UK; All Souls College, University of Oxford, Oxford, OX1 4AL, UK.
| | - Christina R Woltz
- Department of Earth Science, University of California at Santa Barbara, Santa Barbara, CA 93106, USA; Department of Earth and Planetary Sciences, Stanford University, Stanford, CA, 94305, USA
| | - Nicholas J Tosca
- Department of Earth Sciences, University of Cambridge, Cambridge, CB2 3EQ, UK
| | - Susannah M Porter
- Department of Earth Science, University of California at Santa Barbara, Santa Barbara, CA 93106, USA
| | - Derek E G Briggs
- Department of Earth and Planetary Sciences, Yale University, New Haven, CT 06511, USA; Yale Peabody Museum, Yale University, New Haven, CT 06520, USA
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Janssen DJ, Rickli J, Wille M, Sepúlveda Steiner O, Vogel H, Dellwig O, Berg JS, Bouffard D, Lever MA, Hassler CS, Jaccard SL. Chromium Cycling in Redox-Stratified Basins Challenges δ 53Cr Paleoredox Proxy Applications. GEOPHYSICAL RESEARCH LETTERS 2022; 49:e2022GL099154. [PMID: 36589775 PMCID: PMC9787902 DOI: 10.1029/2022gl099154] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Figures] [Subscribe] [Scholar Register] [Received: 04/13/2022] [Revised: 09/24/2022] [Accepted: 09/27/2022] [Indexed: 06/17/2023]
Abstract
Chromium stable isotope composition (δ53Cr) is a promising tracer for redox conditions throughout Earth's history; however, the geochemical controls of δ53Cr have not been assessed in modern redox-stratified basins. We present new chromium (Cr) concentration and δ53Cr data in dissolved, sinking particulate, and sediment samples from the redox-stratified Lake Cadagno (Switzerland), a modern Proterozoic ocean analog. These data demonstrate isotope fractionation during incomplete (non-quantitative) reduction and removal of Cr above the chemocline, driving isotopically light Cr accumulation in euxinic deep waters. Sediment authigenic Cr is isotopically distinct from overlying waters but comparable to average continental crust. New and published data from other redox-stratified basins show analogous patterns. This challenges assumptions from δ53Cr paleoredox applications that quantitative Cr reduction and removal limits isotope fractionation. Instead, fractionation from non-quantitative Cr removal leads to sedimentary records offset from overlying waters and not reflecting high δ53Cr from oxidative continental weathering.
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Affiliation(s)
- David J. Janssen
- Institute of Geological SciencesUniversity of BernBernSwitzerland
- Oeschger Centre for Climate Change ResearchUniversity of BernBernSwitzerland
- Department Surface WatersEawag: Swiss Federal Institute of Aquatic Science and TechnologyKastanienbaumSwitzerland
| | - Jörg Rickli
- Institute of Geological SciencesUniversity of BernBernSwitzerland
- Oeschger Centre for Climate Change ResearchUniversity of BernBernSwitzerland
- Institute of Geochemistry and PetrologyDepartment of Earth SciencesETH ZurichZurichSwitzerland
| | - Martin Wille
- Institute of Geological SciencesUniversity of BernBernSwitzerland
| | - Oscar Sepúlveda Steiner
- Department Surface WatersEawag: Swiss Federal Institute of Aquatic Science and TechnologyKastanienbaumSwitzerland
| | - Hendrik Vogel
- Institute of Geological SciencesUniversity of BernBernSwitzerland
- Oeschger Centre for Climate Change ResearchUniversity of BernBernSwitzerland
| | - Olaf Dellwig
- Marine GeologyLeibniz Institute for Baltic Sea ResearchRostockGermany
| | - Jasmine S. Berg
- Institute of Earth Surface DynamicsUniversity of LausanneLausanneSwitzerland
| | - Damien Bouffard
- Department Surface WatersEawag: Swiss Federal Institute of Aquatic Science and TechnologyKastanienbaumSwitzerland
- Institute of Earth Surface DynamicsUniversity of LausanneLausanneSwitzerland
| | - Mark A. Lever
- Department of Environmental Systems ScienceETH‐ZurichZurichSwitzerland
- Now at Marine Science InstituteUniversity of Texas at AustinTXPort AransasUSA
| | - Christel S. Hassler
- Department F.‐A. Forel for Environmental and Aquatic SciencesUniversity of GenevaGenevaSwitzerland
- Institute of Earth SciencesUniversity of LausanneLausanneSwitzerland
| | - Samuel L. Jaccard
- Institute of Geological SciencesUniversity of BernBernSwitzerland
- Oeschger Centre for Climate Change ResearchUniversity of BernBernSwitzerland
- Institute of Earth SciencesUniversity of LausanneLausanneSwitzerland
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Theoretical Principles and Perspectives of Hyperspectral Imaging Applied to Sediment Core Analysis. QUATERNARY 2022. [DOI: 10.3390/quat5020028] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 01/27/2023]
Abstract
Hyperspectral imaging is a recent technology that has been gaining popularity in the geosciences since the 1990s, both in remote sensing and in the field or laboratory. Indeed, it allows the rapid acquisition of a large amount of data that are spatialized on the studied object with a low-cost, compact, and automatable sensor. This practical article aims to present the current state of knowledge on the use of hyperspectral imaging for sediment core analysis (core logging). To use the full potential of this type of sensor, many points must be considered and will be discussed to obtain reliable and quality data to extract many environmental properties of sediment cores. Hyperspectral imaging is used in many fields (e.g., remote sensing, geosciences and artificial intelligence) and offers many possibilities. The applications of the literature will be reviewed under five themes: lake and water body trophic status, source-to-sink approaches, organic matter and mineralogy studies, and sedimentary deposit characterization. Afterward, discussions will be focused on a multisensor core logger, data management, integrated use of these data for the selection of sample areas, and other opportunities. Through this practical article, we emphasize that hyperspectral imaging applied to sediment cores is still an emerging tool and shows many possibilities for refining the understanding of environmental processes.
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Emmings JF, Poulton SW, Walsh J, Leeming KA, Ross I, Peters SE. Pyrite mega-analysis reveals modes of anoxia through geological time. SCIENCE ADVANCES 2022; 8:eabj5687. [PMID: 35294245 PMCID: PMC8926349 DOI: 10.1126/sciadv.abj5687] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Grants] [Track Full Text] [Figures] [Subscribe] [Scholar Register] [Received: 05/20/2021] [Accepted: 01/21/2022] [Indexed: 06/14/2023]
Abstract
The redox structure of the water column in anoxic basins through geological time remains poorly resolved despite its importance to biological evolution/extinction and biogeochemical cycling. Here, we provide a temporal record of bottom and pore water redox conditions by analyzing the temporal distribution and chemistry of sedimentary pyrite. We combine machine-reading techniques, applied over a large library of published literature, with statistical analysis of element concentrations in databases of sedimentary pyrite and bulk sedimentary rocks to generate a scaled analysis spanning the majority of Earth's history. This analysis delineates the prevalent anoxic basin states from the Archaean to present day, which are associated with diagnostic combinations of five types of syngenetic pyrite. The underlying driver(s) for the pyrite types are unresolved but plausibly includes the ambient seawater inventory, precipitation kinetics, and the (co)location of organic matter degradation coupled to sulfate reduction, iron (oxyhydr)oxide dissolution, and pyrite precipitation.
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Affiliation(s)
- Joseph F. Emmings
- British Geological Survey, Keyworth, Nottingham NG12
5GG, UK
- School of Geography, Geology and the Environment,
University of Leicester, Leicester LE1 7RH, UK
| | - Simon W. Poulton
- School of Earth and Environment, University of Leeds,
Leeds LS2 9JT, UK
| | - Joanna Walsh
- Lyell Centre, British Geological Survey, Riccarton,
Edinburgh EH14 4AS, UK
- Ordnance Survey, Explorer House, Adanac Drive,
Southampton SO16 0AS, UK
| | | | - Ian Ross
- Department of Computer Sciences, University of
Wisconsin–Madison, Madison, WI 53706, USA
| | - Shanan E. Peters
- Department of Geoscience, University of
Wisconsin–Madison, Madison, WI 53706, USA
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Decreasing Phanerozoic extinction intensity as a consequence of Earth surface oxygenation and metazoan ecophysiology. Proc Natl Acad Sci U S A 2021; 118:2101900118. [PMID: 34607946 DOI: 10.1073/pnas.2101900118] [Citation(s) in RCA: 6] [Impact Index Per Article: 2.0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Accepted: 08/26/2021] [Indexed: 11/18/2022] Open
Abstract
The decline in background extinction rates of marine animals through geologic time is an established but unexplained feature of the Phanerozoic fossil record. There is also growing consensus that the ocean and atmosphere did not become oxygenated to near-modern levels until the mid-Paleozoic, coinciding with the onset of generally lower extinction rates. Physiological theory provides us with a possible causal link between these two observations-predicting that the synergistic impacts of oxygen and temperature on aerobic respiration would have made marine animals more vulnerable to ocean warming events during periods of limited surface oxygenation. Here, we evaluate the hypothesis that changes in surface oxygenation exerted a first-order control on extinction rates through the Phanerozoic using a combined Earth system and ecophysiological modeling approach. We find that although continental configuration, the efficiency of the biological carbon pump in the ocean, and initial climate state all impact the magnitude of modeled biodiversity loss across simulated warming events, atmospheric oxygen is the dominant predictor of extinction vulnerability, with metabolic habitat viability and global ecophysiotype extinction exhibiting inflection points around 40% of present atmospheric oxygen. Given this is the broad upper limit for estimates of early Paleozoic oxygen levels, our results are consistent with the relative frequency of high-magnitude extinction events (particularly those not included in the canonical big five mass extinctions) early in the Phanerozoic being a direct consequence of limited early Paleozoic oxygenation and temperature-dependent hypoxia responses.
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