1
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Duan X, Shi Z. Sedimentary records of sea level fall during the end-Permian in the upper Yangtze region (southern China): Implications for the mass extinction. Heliyon 2024; 10:e31226. [PMID: 38799747 PMCID: PMC11126861 DOI: 10.1016/j.heliyon.2024.e31226] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 02/05/2024] [Revised: 05/10/2024] [Accepted: 05/13/2024] [Indexed: 05/29/2024] Open
Abstract
Sea level fall is considered one of the significant factors leading to the end-Permian mass extinction (EPME). We studied the relative sea level changes in the Beifengjing and Shangsi sections, and the results indicate that a sea level fall occurred in the Upper Yangtze region during the Permian-Triassic transition. Considering that there is no significant change in fossil abundance in the strata following the two sea level falls observed in the Beifengjing section, we conclude that the reduction in shallow marine habitat for sea level fall solely was insufficient to cause the mass extinction. However, sea level fall did exacerbate the input of terrestrial debris into the ocean, leading to the deterioration of the marine environment. We propose that the combined adverse effects of volcanic eruptions, sea level falls, and other events exceeded the threshold for biological survival, ultimately resulting in the catastrophic EPME.
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Affiliation(s)
- Xiong Duan
- School of Geographical Sciences, Sichuan Provincial Engineering Laboratory of Monitoring and Control for Soil Erosion in Dry Valley, China West Normal University, Nanchong, 637009, China
- State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu, 610059, China
| | - Zhiqiang Shi
- State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu, 610059, China
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2
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Li M, Xu Y, Sun L, Chen J, Zhang K, Li D, Farquhar J, Zhang X, Sun R, Macdonald FA, Grasby SE, Fu Y, Shen Y. Deglacial volcanism and reoxygenation in the aftermath of the Sturtian Snowball Earth. SCIENCE ADVANCES 2023; 9:eadh9502. [PMID: 37672591 PMCID: PMC10482342 DOI: 10.1126/sciadv.adh9502] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 03/24/2023] [Accepted: 08/02/2023] [Indexed: 09/08/2023]
Abstract
The Cryogenian Sturtian and Marinoan Snowball Earth glaciations bracket a nonglacial interval during which Demosponge and green-algal biomarkers first appear. To understand the relationships between environmental perturbations and early animal evolution, we measured sulfur and mercury isotopes from the Datangpo Formation from South China. Hg enrichment with positive Δ199Hg excursion suggests enhanced volcanism, potentially due to depressurization of terrestrial magma chambers during deglaciation. A thick stratigraphic interval of negative Δ33Spy indicates that the nonglacial interlude was characterized by low but rising sulfate levels. Model results reveal a mechanism to produce the Δ33S anomalies down to -0.284‰ through Rayleigh distillation. We propose that extreme temperatures and anoxia contributed to the apparent delay in green algal production in the aftermath of the Sturtian glaciation and the subsequent reoxygenation of the iron-rich and sulfate-depleted ocean paved the way for evolution of animals.
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Affiliation(s)
- Menghan Li
- School of Earth and Space Sciences, University of Science and Technology of China, Hefei 230026, China
| | - Yilun Xu
- School of Earth and Space Sciences, University of Science and Technology of China, Hefei 230026, China
| | - Lilin Sun
- School of Earth and Space Sciences, University of Science and Technology of China, Hefei 230026, China
| | - Jiubin Chen
- Institute of Surface-Earth System Science, School of Earth System Science, Tianjin University, Tianjin 300350, China
| | - Ke Zhang
- Institute of Surface-Earth System Science, School of Earth System Science, Tianjin University, Tianjin 300350, China
| | - Dandan Li
- School of Earth and Space Sciences, University of Science and Technology of China, Hefei 230026, China
| | - James Farquhar
- Department of Geology and ESSIC, University of Maryland, College Park, MD 20742, USA
| | - Xiaolin Zhang
- School of Earth and Space Sciences, University of Science and Technology of China, Hefei 230026, China
| | - Ruoyu Sun
- Institute of Surface-Earth System Science, School of Earth System Science, Tianjin University, Tianjin 300350, China
| | - Francis A. Macdonald
- Department of Earth Science, University of California–Santa Barbara, Santa Barbara, CA 93106, USA
| | - Stephen E. Grasby
- Geological Survey of Canada, Natural Resources Canada, Calgary, Alberta T2L 2A7, Canada
| | - Yong Fu
- College of Resource and Environmental Engineering, Guizhou University, Guiyang 550012, China
| | - Yanan Shen
- School of Earth and Space Sciences, University of Science and Technology of China, Hefei 230026, China
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3
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Zhou Z, Wang H, Li Y. Mercury stable isotopes in the ocean: Analytical methods, cycling, and application as tracers. THE SCIENCE OF THE TOTAL ENVIRONMENT 2023; 874:162485. [PMID: 36858226 DOI: 10.1016/j.scitotenv.2023.162485] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Subscribe] [Scholar Register] [Received: 11/03/2022] [Revised: 02/22/2023] [Accepted: 02/22/2023] [Indexed: 06/18/2023]
Abstract
Mercury (Hg) has seven stable isotopes that can be utilized to trace the sources of Hg and evaluate the importance of transport and transformation processes in the cycling of Hg in the environment. The ocean is an integral part of the Earth and plays an important role in the global mercury cycle. However, there is a lack of a systematic review of Hg stable isotopes in marine environments. This review is divided into four sections: a) advances in Hg stable isotope analysis, b) the isotope ratios of Hg in various marine environmental matrices (seawater, sediment, and organisms), c) processes governing stable Hg isotope ratios in the ocean, and d) application of Hg stable isotopes to understand biotic uptake and migration. Mercury isotopes have provided much useful information on marine Hg cycling that cannot be given by Hg concentrations alone. This includes (i) sources of Hg in coastal or estuarine environments, (ii) transformation pathways and mechanisms of different forms of Hg in marine environments, (iii) trophic levels and feeding guilds of marine fish, and (iv) migration/habitat changes of marine fish. With the improvement of methods for seawater Hg isotope analysis (especially species-specific methods) and the measurement of Hg isotope fractionation during natural biogeochemical processes in the ocean, Hg stable isotopes will advance our understanding of the marine Hg cycle in the future, e.g., mercury exchange at the sea-atmosphere interface and seawater-sediment interface, contributions of different water masses to Hg in the ocean, fractionation mechanisms of Hg and MeHg transformation in seawater.
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Affiliation(s)
- Zhengwen Zhou
- Frontiers Science Center for Deep Ocean Multispheres and Earth System, Key Laboratory of Marine Chemistry Theory and Technology, Ministry of Education and College of Chemistry and Chemical Engineering, Ocean University of China, Qingdao 266100, China
| | - Huiling Wang
- Frontiers Science Center for Deep Ocean Multispheres and Earth System, Key Laboratory of Marine Chemistry Theory and Technology, Ministry of Education and College of Chemistry and Chemical Engineering, Ocean University of China, Qingdao 266100, China
| | - Yanbin Li
- Frontiers Science Center for Deep Ocean Multispheres and Earth System, Key Laboratory of Marine Chemistry Theory and Technology, Ministry of Education and College of Chemistry and Chemical Engineering, Ocean University of China, Qingdao 266100, China.
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4
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Wignall PB. Paleobiology: Anatomy of a mass extinction double whammy. Curr Biol 2023; 33:R233-R235. [PMID: 36977387 DOI: 10.1016/j.cub.2023.02.008] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [MESH Headings] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 03/29/2023]
Abstract
The Permo-Triassic mass extinction has been resolved into two closely spaced crises that both saw enormous extinction losses. However, food web modelling suggests they were not ecologically equivalent, only the second destabilised communities.
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Affiliation(s)
- Paul B Wignall
- School of Earth and Environment, University of Leeds, Leeds LS2 9JT, UK.
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5
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Liu F, Peng H, Marshall JE, Lomax BH, Bomfleur B, Kent MS, Fraser WT, Jardine PE. Dying in the Sun: Direct evidence for elevated UV-B radiation at the end-Permian mass extinction. SCIENCE ADVANCES 2023; 9:eabo6102. [PMID: 36608140 PMCID: PMC9821938 DOI: 10.1126/sciadv.abo6102] [Citation(s) in RCA: 5] [Impact Index Per Article: 5.0] [Reference Citation Analysis] [Abstract] [Grants] [Track Full Text] [Download PDF] [Figures] [Subscribe] [Scholar Register] [Received: 07/26/2022] [Accepted: 12/07/2022] [Indexed: 06/17/2023]
Abstract
Land plants can adjust the concentration of protective ultraviolet B (UV-B)-absorbing compounds (UACs) in the outer wall of their reproductive propagules in response to ambient UV-B flux. To infer changes in UV-B radiation flux at Earth's surface during the end-Permian mass extinction, we analyze UAC abundances in ca. 800 pollen grains from an independently dated Permian-Triassic boundary section in Tibet. Our data reveal an excursion in UACs that coincide with a spike in mercury concentration and a negative carbon-isotope excursion in the latest Permian deposits, suggesting a close temporal link between large-scale volcanic eruptions, global carbon and mercury cycle perturbations, and ozone layer disruption. Because enhanced UV-B radiation can exacerbate the environmental deterioration induced by massive magmatism, ozone depletion is considered a compelling ecological driver for the terrestrial mass extinction.
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Affiliation(s)
- Feng Liu
- Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008, China
- State Key Laboratory of Palaeobiology and Stratigraphy and Center for Excellence in Life and Paleoenvironment, Nanjing 210008, China
| | - Huiping Peng
- Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008, China
| | - John E. A. Marshall
- School of Ocean and Earth Science, University of Southampton, National Oceanography Centre, Southampton, SO14 3ZH, UK
| | - Barry H. Lomax
- Division of Agricultural and Environmental Sciences, The School of Biosciences, The University of Nottingham, Sutton Bonington Campus, Sutton Bonington, Leicestershire, LE12 5RD, UK
| | - Benjamin Bomfleur
- Palaeobotany Group, Institute of Geology and Palaeontology, University of Münster, Münster 48149, Germany
| | - Matthew S. Kent
- Division of Agricultural and Environmental Sciences, The School of Biosciences, The University of Nottingham, Sutton Bonington Campus, Sutton Bonington, Leicestershire, LE12 5RD, UK
| | - Wesley T. Fraser
- Geography, School of Social Sciences, Oxford Brookes University, Oxford OX3 0BP, UK
| | - Phillip E. Jardine
- Palaeobotany Group, Institute of Geology and Palaeontology, University of Münster, Münster 48149, Germany
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6
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Shen J, Chen J, Yu J, Algeo TJ, Smith RMH, Botha J, Frank TD, Fielding CR, Ward PD, Mather TA. Mercury evidence from southern Pangea terrestrial sections for end-Permian global volcanic effects. Nat Commun 2023; 14:6. [PMID: 36596767 PMCID: PMC9810726 DOI: 10.1038/s41467-022-35272-8] [Citation(s) in RCA: 3] [Impact Index Per Article: 3.0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 08/21/2022] [Accepted: 11/25/2022] [Indexed: 01/04/2023] Open
Abstract
The latest Permian mass extinction (LPME) was triggered by magmatism of the Siberian Traps Large Igneous Province (STLIP), which left an extensive record of sedimentary Hg anomalies at Northern Hemisphere and tropical sites. Here, we present Hg records from terrestrial sites in southern Pangea, nearly antipodal to contemporaneous STLIP activity, providing insights into the global distribution of volcanogenic Hg during this event and its environmental processing. These profiles (two from Karoo Basin, South Africa; two from Sydney Basin, Australia) exhibit significant Hg enrichments within the uppermost Permian extinction interval as well as positive Δ199Hg excursions (to ~0.3‰), providing evidence of long-distance atmospheric transfer of volcanogenic Hg. These results demonstrate the far-reaching effects of the Siberian Traps as well as refine stratigraphic placement of the LPME interval in the Karoo Basin at a temporal resolution of ~105 years based on global isochronism of volcanogenic Hg anomalies.
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Affiliation(s)
- Jun Shen
- State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan, Hubei, 430074, People's Republic of China.
| | - Jiubin Chen
- Institute of Surface-Earth System Science, Tianjin University, Tianjin, 300072, People's Republic of China
| | - Jianxin Yu
- State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan, Hubei, 430074, People's Republic of China
| | - Thomas J Algeo
- State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan, Hubei, 430074, People's Republic of China.,State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan, Hubei, 430074, People's Republic of China.,Department of Geosciences, University of Cincinnati, Cincinnati, OH, 45221-0013, USA
| | - Roger M H Smith
- Evolutionary Studies Institute, University of the Witwatersrand, Johannesburg, 2050, South Africa.,Iziko South African Museum, PO Box 61, Cape Town, 8000, South Africa
| | - Jennifer Botha
- Evolutionary Studies Institute, University of the Witwatersrand, Johannesburg, 2050, South Africa.,National Museum, PO Box 266, Bloemfontein, 9300, South Africa
| | - Tracy D Frank
- Department of Earth Sciences, University of Connecticut, Storrs, CT, 06269, USA
| | | | - Peter D Ward
- Department of Biology, University of Washington, Seattle, WA, 98195-1800, USA
| | - Tamsin A Mather
- Department of Earth Sciences, University of Oxford, South Parks Road, Oxford, OX1 3AN, UK
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7
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Ruhl M, Hesselbo SP, Jenkyns HC, Xu W, Silva RL, Matthews KJ, Mather TA, Mac Niocaill C, Riding JB. Reduced plate motion controlled timing of Early Jurassic Karoo-Ferrar large igneous province volcanism. SCIENCE ADVANCES 2022; 8:eabo0866. [PMID: 36083904 PMCID: PMC9462690 DOI: 10.1126/sciadv.abo0866] [Citation(s) in RCA: 2] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [Abstract] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 01/12/2022] [Accepted: 07/12/2022] [Indexed: 05/24/2023]
Abstract
Past large igneous province (LIP) emplacement is commonly associated with mantle plume upwelling and led to major carbon emissions. One of Earth's largest past environmental perturbations, the Toarcian oceanic anoxic event (T-OAE; ~183 Ma), has been linked to Karoo-Ferrar LIP emplacement. However, the role of mantle plumes in controlling the onset and timing of LIP magmatism is poorly understood. Using global plate reconstruction models and Lower Toarcian sedimentary mercury (Hg) concentrations, we demonstrate (i) that the T-OAE occurred coevally with Karoo-Ferrar emplacement and (ii) that timing and duration of LIP emplacement was governed by reduced Pangean plate motion, associated with a reversal in plate movement direction. This new model mechanistically links Earth's interior and surficial processes, and the mechanism is consistent with the timing of several of the largest LIP volcanic events throughout Earth history and, thus, the timing of many of Earth's past global climate change and mass extinction events.
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Affiliation(s)
- Micha Ruhl
- Department of Geology, Earth Surface Research Laboratory (ESRL) and SFI Research Centre in Applied Geosciences (iCRAG), Trinity College Dublin, The University of Dublin, College Green, Dublin 2, Ireland
- Department of Earth Sciences, University of Oxford, South Parks Road, OX1 3AN, Oxford, UK
| | - Stephen P. Hesselbo
- Camborne School of Mines and Environment and Sustainability Institute, University of Exeter, Penryn Campus, Treliever Road, Penryn, Cornwall TR10 9FE, UK
| | - Hugh C. Jenkyns
- Department of Earth Sciences, University of Oxford, South Parks Road, OX1 3AN, Oxford, UK
| | - Weimu Xu
- Department of Earth Sciences, University of Oxford, South Parks Road, OX1 3AN, Oxford, UK
- School of Earth Sciences and SFI Research Centre in Applied Geosciences (iCRAG), University College Dublin, Belfield, Dublin 4, Ireland
| | - Ricardo L. Silva
- Department of Geology, Earth Surface Research Laboratory (ESRL) and SFI Research Centre in Applied Geosciences (iCRAG), Trinity College Dublin, The University of Dublin, College Green, Dublin 2, Ireland
- Department of Earth Sciences, Clayton H. Riddell Faculty of Environment, Earth, and Resources, University of Manitoba, 125 Dysart Road, Winnipeg, R3T 2N2, Canada
| | - Kara J. Matthews
- Department of Earth Sciences, University of Oxford, South Parks Road, OX1 3AN, Oxford, UK
- Arctic Institute of North America, University of Calgary, 2500 University Drive NW, ES-1040, Calgary, AB T2N 1N4, Canada
| | - Tamsin A. Mather
- Department of Earth Sciences, University of Oxford, South Parks Road, OX1 3AN, Oxford, UK
| | - Conall Mac Niocaill
- Department of Earth Sciences, University of Oxford, South Parks Road, OX1 3AN, Oxford, UK
| | - James B. Riding
- British Geological Survey, Keyworth, Nottingham NG12 5GG, UK
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8
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Wang Y, Pei W, Yang J, Fan Y, Zhang R, Li T, Russell J, Zhang F, Yu X, Hu J, Song Y, Liu Z, Guan M, Han Q. The relationship between volcanism and global climate changes in the Tropical Western Pacific over the mid-Pleistocene transition: Evidence from mercury concentration and isotopic composition. THE SCIENCE OF THE TOTAL ENVIRONMENT 2022; 823:153482. [PMID: 35122862 DOI: 10.1016/j.scitotenv.2022.153482] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 10/26/2021] [Revised: 01/24/2022] [Accepted: 01/24/2022] [Indexed: 06/14/2023]
Abstract
Volcanoes are a significant component of the Earth system, influencing the interaction between oceans and the atmosphere over large spatial and temporal scales. Being a volcanically dynamic region, the Tropical Western Pacific (TWP) can significantly impact variations in global climate. However, high-resolution continuous records of volcanic activity in this region are lacking, resulting in significant uncertainties regarding the coupling between the deep earth, climate changes, and atmospheric CO2 in the TWP. To address this issue, mercury (Hg) levels, isotopic compositions, and Hg/total organic carbon (Hg/TOC) ratios were determined at site U1486 to track volcanic activity throughout the mid-Pleistocene transition (MPT) from 1.3 Myr to 0.6 Myr. Our results of anomalously high Hg concentrations and Hg/TOC ratios provide evidence of time-varying volcanism throughout the MPT. Mercury isotopes in the Hg-enriched sediments were characterized by near-zero Δ199Hg values, which is consistent with volcanism acting as the primary source of Hg to the sediments. Spectral analysis of the Hg/TOC ratio showed significant periodicity at ~100 kyr and ~ 23 kyr as well as a weaker signal at ~41 kyr consistent with Milankovitch cycles. A cross spectral analysis of Hg/TOC and the LR04 δ18O stack record suggests that the peak in volcanism lags the temperature minimum by ~6 kyr, and occurs prior to the δ18O minimum known as the glacial termination by ~14 ± 2 kyr. The records of volcanic activity in this site are also consistent with a prominent rise in atmospheric CO2 and negative excursion of benthic carbon isotopes throughout the MPT. This study provides direct sedimentary evidence in the TWP of the feedback between volcanic activity, climate change and atmospheric CO2.
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Affiliation(s)
- Yipeng Wang
- School of Marine Technology and Geomatics, Jiangsu Ocean University, Lianyungang 222005, Jiangsu Province, China
| | - Wenlong Pei
- School of Marine Technology and Geomatics, Jiangsu Ocean University, Lianyungang 222005, Jiangsu Province, China
| | - Jialei Yang
- School of Marine Technology and Geomatics, Jiangsu Ocean University, Lianyungang 222005, Jiangsu Province, China
| | - Yujin Fan
- School of Marine Technology and Geomatics, Jiangsu Ocean University, Lianyungang 222005, Jiangsu Province, China
| | - Rui Zhang
- Co-Innovation Center of Jiangsu Marine Bio-industry Technology, Jiangsu Ocean University, Lianyungang 222005, Jiangsu Province, China; Jiangsu Key Laboratory of Marine Bioresources and Environment, Jiangsu Ocean University, Lianyungang 222005, Jiangsu Province, China; School of Marine Technology and Geomatics, Jiangsu Ocean University, Lianyungang 222005, Jiangsu Province, China; Department of Earth, Environmental, and Planetary Sciences, Brown University, Providence, RI 02912, USA.
| | - Tiegang Li
- First Institute of Oceanography, Ministry of Natural Resources, Qingdao 266061, Shandong Province, China; Laboratory for Marine Geology, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266061, China; University of Chinese Academy of Sciences, Beijing 100049, China.
| | - James Russell
- Department of Earth, Environmental, and Planetary Sciences, Brown University, Providence, RI 02912, USA
| | - Fan Zhang
- Department of Chemical Engineering, Jiangsu Ocean University, 222005, Jiangsu Province, China
| | - Xiaoxiao Yu
- State Key Laboratory of Isotope Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China
| | - Junjie Hu
- School of Marine Technology and Geomatics, Jiangsu Ocean University, Lianyungang 222005, Jiangsu Province, China
| | - Yuehuo Song
- School of Marine Technology and Geomatics, Jiangsu Ocean University, Lianyungang 222005, Jiangsu Province, China
| | - Zhiyong Liu
- School of Radiation Medicine and Protection, Medicine College, Soochow University, Suzhou 215123, Jiangsu Province, China
| | - Minglei Guan
- School of Marine Technology and Geomatics, Jiangsu Ocean University, Lianyungang 222005, Jiangsu Province, China
| | - Qi Han
- School of Ocean Sciences, China University of Geosciences, Beijing 100083, China
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9
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Shen J, Yin R, Algeo TJ, Svensen HH, Schoepfer SD. Mercury evidence for combustion of organic-rich sediments during the end-Triassic crisis. Nat Commun 2022; 13:1307. [PMID: 35264554 PMCID: PMC8907283 DOI: 10.1038/s41467-022-28891-8] [Citation(s) in RCA: 10] [Impact Index Per Article: 5.0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 09/18/2021] [Accepted: 02/15/2022] [Indexed: 11/09/2022] Open
Abstract
The sources of isotopically light carbon released during the end-Triassic mass extinction remain in debate. Here, we use mercury (Hg) concentrations and isotopes from a pelagic Triassic–Jurassic boundary section (Katsuyama, Japan) to track changes in Hg cycling. Because of its location in the central Panthalassa, far from terrigenous runoff, Hg enrichments at Katsuyama record atmospheric Hg deposition. These enrichments are characterized by negative mass independent fractionation (MIF) of odd Hg isotopes, providing evidence of their derivation from terrestrial organic-rich sediments (Δ199Hg < 0‰) rather than from deep-Earth volcanic gases (Δ199Hg ~ 0‰). Our data thus provide evidence that combustion of sedimentary organic matter by igneous intrusions and/or wildfires played a significant role in the environmental perturbations accompanying the event. This process has a modern analog in anthropogenic combustion of fossil fuels from crustal reservoirs. Mercury (Hg) concentrations and isotopes from a deep-ocean Triassic–Jurassic (~201 Ma) boundary section provide evidence of large inputs from terrestrial organic-rich sources through combustion by magmatic sills and wildfires.
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Affiliation(s)
- Jun Shen
- State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan, Hubei, 430074, P.R. China.
| | - Runsheng Yin
- State Key Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang, Guizhou, 550081, P.R. China.
| | - Thomas J Algeo
- State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan, Hubei, 430074, P.R. China.,State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan, Hubei, 430074, P.R. China.,Department of Geology, University of Cincinnati, Cincinnati, OH, 45221-0013, USA
| | - Henrik H Svensen
- Centre for Earth Evolution and Dynamics (CEED), University of Oslo, Oslo, Norway
| | - Shane D Schoepfer
- Department of Geoscience and Natural Resources, Western Carolina University, Cullowhee, NC, 28723, USA
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10
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Intensified continental chemical weathering and carbon-cycle perturbations linked to volcanism during the Triassic-Jurassic transition. Nat Commun 2022; 13:299. [PMID: 35027546 PMCID: PMC8758789 DOI: 10.1038/s41467-022-27965-x] [Citation(s) in RCA: 16] [Impact Index Per Article: 8.0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 01/28/2021] [Accepted: 01/03/2022] [Indexed: 11/08/2022] Open
Abstract
Direct evidence of intense chemical weathering induced by volcanism is rare in sedimentary successions. Here, we undertake a multiproxy analysis (including organic carbon isotopes, mercury (Hg) concentrations and isotopes, chemical index of alteration (CIA), and clay minerals) of two well-dated Triassic-Jurassic (T-J) boundary sections representing high- and low/middle-paleolatitude sites. Both sections show increasing CIA in association with Hg peaks near the T-J boundary. We interpret these results as reflecting volcanism-induced intensification of continental chemical weathering, which is also supported by negative mass-independent fractionation (MIF) of odd Hg isotopes. The interval of enhanced chemical weathering persisted for ~2 million years, which is consistent with carbon-cycle model results of the time needed to drawdown excess atmospheric CO2 following a carbon release event. Lastly, these data also demonstrate that high-latitude continental settings are more sensitive than low/middle-latitude sites to shifts in weathering intensity during climatic warming events.
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11
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Liu Y, Chen J, Liu J, Gai P, Au Yang D, Zheng W, Li Y, Li D, Cai H, Yuan W, Li Y. Coprecipitation of Mercury from Natural Iodine-Containing Seawater for Accurate Isotope Measurement. Anal Chem 2021; 93:15905-15912. [PMID: 34806358 DOI: 10.1021/acs.analchem.1c03060] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/30/2022]
Abstract
Oceans play a key role in the global mercury (Hg) cycle, but studies on Hg isotopes in seawater are rare due to the extremely low Hg concentration and the lack of a good preconcentration method. Here, we introduce a new coprecipitation method for separating and preconcentrating Hg from seawater for accurate isotope measurement. The coprecipitation was achieved by sequential addition of 0.5 mL of 0.5 M CuSO4, 1 mL of 0.5 M Na2S, and 1 mL of 0.5 M CuSO4 reagents, which allowed for quantitatively precipitating Hg from up to 10 L of seawater. The protocol was validated by testing synthetic solutions with varying Hg and iodide (I-) concentrations and by comparing the reaction times of various reagents added. The method resulted in a quantitative recovery of 98 ± 12% (n = 32, two standard deviations, 2 SD) and a relatively low procedure blank (103 pg of Hg, n = 8). The precipitates were filtrated and analyzed for Hg isotopes. Repeated measurements of synthetic seawaters spiked with certificated standard materials (NIST 3133 and 3177) using the entire method gave identical Hg isotope ratios with near-quantitative Hg recovery, indicating no isotope fractionation during preconcentration. A total of six nearshore seawater samples from the Yellow Sea and the Bohai Sea (China) were analyzed using the coprecipitation method. The data showed a large fractionation of Hg isotopes and revealed the possible impact of both atmospheric and anthropogenic inputs to the coastal seawater Hg budget, implying the potential application of this method in studying marine Hg systematics and global Hg cycling.
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Affiliation(s)
- Yulong Liu
- State Key Laboratory of Environmental Geochemistry (SKLEG), Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550081, China.,University of Chinese Academy of Sciences, Beijing 100049, China
| | - Jiubin Chen
- State Key Laboratory of Environmental Geochemistry (SKLEG), Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550081, China.,School of Earth System Science (SESS), Institute of Surface-Earth System Science, Tianjin University, Tianjin 300072, China
| | - Jianfeng Liu
- State Key Laboratory of Environmental Geochemistry (SKLEG), Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550081, China.,School of Earth System Science (SESS), Institute of Surface-Earth System Science, Tianjin University, Tianjin 300072, China
| | - Pengxue Gai
- State Key Laboratory of Environmental Geochemistry (SKLEG), Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550081, China.,School of Earth System Science (SESS), Institute of Surface-Earth System Science, Tianjin University, Tianjin 300072, China
| | - David Au Yang
- State Key Laboratory of Environmental Geochemistry (SKLEG), Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550081, China
| | - Wang Zheng
- School of Earth System Science (SESS), Institute of Surface-Earth System Science, Tianjin University, Tianjin 300072, China
| | - Yanbin Li
- Key Laboratory of Marine Chemistry Theory and Technology (Ocean University of China), Ministry of Education, Qingdao 266100, China
| | - Dan Li
- College of Environmental Science and Engineering, Ocean University of China, Qingdao 266100, China
| | - Hongming Cai
- School of Earth System Science (SESS), Institute of Surface-Earth System Science, Tianjin University, Tianjin 300072, China
| | - Wei Yuan
- School of Earth System Science (SESS), Institute of Surface-Earth System Science, Tianjin University, Tianjin 300072, China
| | - Yuansheng Li
- Polar Research Institute of China, Shanghai 200136, China
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12
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Selective smartphone aided colorimetric detection of Hg(II) in an aqueous solution via metal ion-induced keto-enol tautomerism–Spectroscopic and theoretical studies. J Mol Struct 2021. [DOI: 10.1016/j.molstruc.2021.131134] [Citation(s) in RCA: 2] [Impact Index Per Article: 0.7] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 12/17/2022]
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13
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Zhang H, Zhang F, Chen JB, Erwin DH, Syverson DD, Ni P, Rampino M, Chi Z, Cai YF, Xiang L, Li WQ, Liu SA, Wang RC, Wang XD, Feng Z, Li HM, Zhang T, Cai HM, Zheng W, Cui Y, Zhu XK, Hou ZQ, Wu FY, Xu YG, Planavsky N, Shen SZ. Felsic volcanism as a factor driving the end-Permian mass extinction. SCIENCE ADVANCES 2021; 7:eabh1390. [PMID: 34788084 PMCID: PMC8597993 DOI: 10.1126/sciadv.abh1390] [Citation(s) in RCA: 11] [Impact Index Per Article: 3.7] [Reference Citation Analysis] [Abstract] [Grants] [Track Full Text] [Download PDF] [Figures] [Subscribe] [Scholar Register] [Received: 02/18/2021] [Accepted: 09/28/2021] [Indexed: 06/13/2023]
Abstract
The Siberian Traps large igneous province (STLIP) is commonly invoked as the primary driver of global environmental changes that triggered the end-Permian mass extinction (EPME). Here, we explore the contributions of coeval felsic volcanism to end-Permian environmental changes. We report evidence of extreme Cu enrichment in the EPME interval in South China. The enrichment is associated with an increase in the light Cu isotope, melt inclusions rich in copper and sulfides, and Hg concentration spikes. The Cu and Hg elemental and isotopic signatures can be linked to S-rich vapor produced by felsic volcanism. We use these previously unknown geochemical data to estimate volcanic SO2 injections and argue that this volcanism would have produced several degrees of rapid cooling before or coincident with the more protracted global warming. Large-scale eruptions near the South China block synchronous with the EPME strengthen the case that the STLIP may not have been the sole trigger.
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Affiliation(s)
- Hua Zhang
- LPS, Nanjing Institute of Geology and Palaeontology and Center for Excellence in Life and Paleoenvironment, Chinese Academy of Sciences, Nanjing 210008, China
| | - Feifei Zhang
- State Key Laboratory for Mineral Deposits Research, School of Earth Sciences and Engineering and Environment and Frontiers Science Center for Critical Earth Material Cycling, Nanjing University, Nanjing 210023, China
| | - Jiu-bin Chen
- Institute of Surface-Earth System Science, Tianjin University, 92 Weijin Road, Tianjin 300072, China
| | - Douglas H. Erwin
- Department of Paleobiology, MRC-121 National Museum of Natural History, P.O. Box 37012, Washington, DC 20013-7012, USA
- Santa Fe Institute, 1399 Hyde Park Road, Santa Fe, NM 87501, USA
| | - Drew D. Syverson
- Department of Earth and Planetary Sciences, Yale University, New Haven, CT 06511, USA
| | - Pei Ni
- State Key Laboratory for Mineral Deposits Research, School of Earth Sciences and Engineering and Environment and Frontiers Science Center for Critical Earth Material Cycling, Nanjing University, Nanjing 210023, China
| | - Michael Rampino
- Departments of Biology and Environmental Studies, New York University, New York, NY 10003, USA
| | - Zhe Chi
- State Key Laboratory for Mineral Deposits Research, School of Earth Sciences and Engineering and Environment and Frontiers Science Center for Critical Earth Material Cycling, Nanjing University, Nanjing 210023, China
| | - Yao-feng Cai
- LPS, Nanjing Institute of Geology and Palaeontology and Center for Excellence in Life and Paleoenvironment, Chinese Academy of Sciences, Nanjing 210008, China
| | - Lei Xiang
- LPS, Nanjing Institute of Geology and Palaeontology and Center for Excellence in Life and Paleoenvironment, Chinese Academy of Sciences, Nanjing 210008, China
| | - Wei-qiang Li
- State Key Laboratory for Mineral Deposits Research, School of Earth Sciences and Engineering and Environment and Frontiers Science Center for Critical Earth Material Cycling, Nanjing University, Nanjing 210023, China
| | - Sheng-Ao Liu
- State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing 100083, China
| | - Ru-cheng Wang
- State Key Laboratory for Mineral Deposits Research, School of Earth Sciences and Engineering and Environment and Frontiers Science Center for Critical Earth Material Cycling, Nanjing University, Nanjing 210023, China
| | - Xiang-dong Wang
- State Key Laboratory for Mineral Deposits Research, School of Earth Sciences and Engineering and Environment and Frontiers Science Center for Critical Earth Material Cycling, Nanjing University, Nanjing 210023, China
| | - Zhuo Feng
- Institute of Deep Time Terrestrial Ecology and Institute of Palaeontology, Yunnan University, Kunming 650500, China
| | - Hou-min Li
- Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China
| | - Ting Zhang
- Institute of Surface-Earth System Science, Tianjin University, 92 Weijin Road, Tianjin 300072, China
| | - Hong-ming Cai
- Institute of Surface-Earth System Science, Tianjin University, 92 Weijin Road, Tianjin 300072, China
| | - Wang Zheng
- Institute of Surface-Earth System Science, Tianjin University, 92 Weijin Road, Tianjin 300072, China
| | - Ying Cui
- Department of Earth and Environmental Studies, Montclair State University, Montclair, NJ 07043, USA
| | - Xiang-kun Zhu
- State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China
| | - Zeng-qian Hou
- Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China
| | - Fu-yuan Wu
- State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China
| | - Yi-gang Xu
- State Key Laboratory of Isotope Geochemistry and Center of Excellence in Deep Earth Science, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China
| | - Noah Planavsky
- Department of Earth and Planetary Sciences, Yale University, New Haven, CT 06511, USA
| | - Shu-zhong Shen
- State Key Laboratory for Mineral Deposits Research, School of Earth Sciences and Engineering and Environment and Frontiers Science Center for Critical Earth Material Cycling, Nanjing University, Nanjing 210023, China
- State Key Laboratory of Isotope Geochemistry and Center of Excellence in Deep Earth Science, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China
- Key Laboratory of Continental Collision and Plateau Uplift, Institute of Tibetan Plateau Research and Center for Excellence in Tibetan Plateau Earth Sciences, Chinese Academy of Sciences, Beijing 100101, China
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14
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Li C, Shen J, Zhang J, Lei P, Kong Y, Zhang J, Tang W, Chen T, Xiang X, Wang S, Zhang W, Zhong H. The silver linings of mercury: Reconsideration of its impacts on living organisms from a multi-timescale perspective. ENVIRONMENT INTERNATIONAL 2021; 155:106670. [PMID: 34090260 DOI: 10.1016/j.envint.2021.106670] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 03/16/2021] [Revised: 04/28/2021] [Accepted: 05/24/2021] [Indexed: 06/12/2023]
Abstract
Research on mercury (Hg), a naturally occurring element in Earth's lithosphere, has been extremely hot in the past few decades due to the outbreak of a series of disastrous poisoning incidents. However, such studies might provide us a biased view towards Hg if no thorough review about its long-term effects on living organisms from a multi-timescale perspective was performed. Hg might have played a mysterious role in critical intervals (e.g., mass extinction and oceanic anoxia events) in several geologic periods due to the elevated Hg levels induced by volcanism whereas it has long been used for various purposes in human history. Therefore, it is necessary to go through previous studies and historical records of different timescales (100 to 106 yr). In this work, we conducted a thorough review of Hg knowledge at three different timescales, i.e., geologic periods (106 yr), human history (103 yr), and contemporary history (100 yr), summarizing recent advances and indicated potential research gaps. By doing so, we demonstrated that it is possible to achieve safe and sustainable Hg applications despite the current Hg crisis. However, such silver linings depend on a better understanding of ecosystem dynamics. Besides, considering the possible dire consequences of erupted Hg levels as suggested in geological periods, swift actions to mitigate the impacts of anthropogenic activities on the Hg cycle will be another key point. Overall, this review presented a unique perspective of Hg combining different timescales, shedding light on the importance of a better understanding of the global ecosystem as a whole and maintaining the sustainability of planet Earth in the future.
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Affiliation(s)
- Chengjun Li
- Institute of Environmental Research at Greater Bay Area, Key Laboratory for Water Quality and Conservation of the Pearl River Delta, Ministry of Education, Guangzhou University, Guangzhou 510006, China
| | - Jun Shen
- State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan, Hubei 430074, China
| | - Jin Zhang
- State Key Laboratory of Pollution Control and Resource Reuse, School of the Environment, Nanjing University, Nanjing 210023, China
| | - Pei Lei
- State Key Laboratory of Pollution Control and Resource Reuse, School of the Environment, Nanjing University, Nanjing 210023, China
| | - Yaqi Kong
- State Key Laboratory of Pollution Control and Resource Reuse, School of the Environment, Nanjing University, Nanjing 210023, China
| | - Jichao Zhang
- Institute of Environmental Research at Greater Bay Area, Key Laboratory for Water Quality and Conservation of the Pearl River Delta, Ministry of Education, Guangzhou University, Guangzhou 510006, China
| | - Wenli Tang
- State Key Laboratory of Pollution Control and Resource Reuse, School of the Environment, Nanjing University, Nanjing 210023, China
| | - Tianyu Chen
- School of Earth Sciences and Engineering, Nanjing University, Nanjing 210023, China
| | - Xin Xiang
- School of Information Management, Nanjing University, Nanjing 210023, China
| | - Shuxiao Wang
- State Key Joint Laboratory of Environmental Simulation and Pollution Control, School of Environment, Tsinghua University, Beijing 100084, China
| | - Wei Zhang
- Institute of Environmental Research at Greater Bay Area, Key Laboratory for Water Quality and Conservation of the Pearl River Delta, Ministry of Education, Guangzhou University, Guangzhou 510006, China.
| | - Huan Zhong
- State Key Laboratory of Pollution Control and Resource Reuse, School of the Environment, Nanjing University, Nanjing 210023, China; Environmental and Life Sciences Program (EnLS), Trent University, Peterborough, Ontario, Canada.
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15
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Li L, Lin LM, Deng J, Lin XL, Li YM, Xia BH. The therapeutic effects of Prunella vulgaris against fluoride-induced oxidative damage by using the metabolomics method. ENVIRONMENTAL TOXICOLOGY 2021; 36:1802-1816. [PMID: 34089294 DOI: 10.1002/tox.23301] [Citation(s) in RCA: 12] [Impact Index Per Article: 4.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 06/08/2020] [Revised: 05/18/2021] [Accepted: 05/24/2021] [Indexed: 06/12/2023]
Abstract
Fluoride is considered as one of the most ubiquitous environmental pollutants. Numerous studies have linked reactive oxygen species (ROS)-dependent oxidative damage with fluoride intoxication, which could be prevented by antioxidants. However, the metabolomic changes induced by ROS disruptions in fluoride intoxication are yet unknown. The present study aimed to provide novel mechanistic insights into the fluoride-induced oxidative damage and to investigate the potential protective effects of ethanolic extract of Prunella vulgaris (natural antioxidant, PV) against fluoride-induced oxidative damage. The serum biochemical indicators related to fluoride-induced oxidative damage, such as lipid peroxidation parameter, inflammation and marker enzymes in the liver increased significantly in the fluoride-treated group, while antioxidant enzymes were decreased. However, PV treatment restored the level of these biochemical indicators, indicating satisfactory antioxidant, anti-inflammatory, and hepatoprotective potential of PV. The metabolomics analysis in the serum was performed by liquid chromatography-mass spectroscopy, whereas the fluoride treatment caused severe metabolic disorders in rats, which could be improved by PV. The differential metabolites screened by multivariate analysis after fluoride and PV treatment, were organic acids, fatty acids, and lipids. These differential metabolites represented disorders of glyoxylate and dicarboxylate metabolism and the citrate cycle (TCA) according to metabolic pathway analysis in fluoride treatment rats. Interestingly, the result of metabolic pathway analysis of post-treatment with PV was consistent with that of fluoride treatment, indicating that the energy metabolism plays a major role in the progress of fluoride-induced oxidative damage, as well as the therapeutic effect of PV. These findings provided a theoretical basis for understanding the mechanism underlying metabolic disorders of fluoride toxicity and the effect of PV.
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Affiliation(s)
- Li Li
- Key Laboratory for Quality Evaluation of Bulk Herbs of Hunan Province, Hunan University of Chinese Medicine, Changsha, China
| | - Li-Mei Lin
- Key Laboratory for Quality Evaluation of Bulk Herbs of Hunan Province, Hunan University of Chinese Medicine, Changsha, China
| | - Jing Deng
- Key Laboratory for Quality Evaluation of Bulk Herbs of Hunan Province, Hunan University of Chinese Medicine, Changsha, China
| | - Xiu-Lian Lin
- Key Laboratory for Quality Evaluation of Bulk Herbs of Hunan Province, Hunan University of Chinese Medicine, Changsha, China
| | - Ya-Mei Li
- Key Laboratory for Quality Evaluation of Bulk Herbs of Hunan Province, Hunan University of Chinese Medicine, Changsha, China
| | - Bo-Hou Xia
- Key Laboratory for Quality Evaluation of Bulk Herbs of Hunan Province, Hunan University of Chinese Medicine, Changsha, China
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16
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Laffoley D, Baxter J, Amon D, Claudet J, Hall‐Spencer J, Grorud‐Colvert K, Levin L, Reid P, Rogers A, Taylor M, Woodall L, Andersen N. Evolving the narrative for protecting a rapidly changing ocean, post-COVID-19. AQUATIC CONSERVATION : MARINE AND FRESHWATER ECOSYSTEMS 2021; 31:1512-1534. [PMID: 33362396 PMCID: PMC7753556 DOI: 10.1002/aqc.3512] [Citation(s) in RCA: 4] [Impact Index Per Article: 1.3] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Subscribe] [Scholar Register] [Received: 07/21/2020] [Revised: 10/06/2020] [Accepted: 10/08/2020] [Indexed: 05/02/2023]
Abstract
The ocean is the linchpin supporting life on Earth, but it is in declining health due to an increasing footprint of human use and climate change. Despite notable successes in helping to protect the ocean, the scale of actions is simply not now meeting the overriding scale and nature of the ocean's problems that confront us.Moving into a post-COVID-19 world, new policy decisions will need to be made. Some, especially those developed prior to the pandemic, will require changes to their trajectories; others will emerge as a response to this global event. Reconnecting with nature, and specifically with the ocean, will take more than good intent and wishful thinking. Words, and how we express our connection to the ocean, clearly matter now more than ever before.The evolution of the ocean narrative, aimed at preserving and expanding options and opportunities for future generations and a healthier planet, is articulated around six themes: (1) all life is dependent on the ocean; (2) by harming the ocean, we harm ourselves; (3) by protecting the ocean, we protect ourselves; (4) humans, the ocean, biodiversity, and climate are inextricably linked; (5) ocean and climate action must be undertaken together; and (6) reversing ocean change needs action now.This narrative adopts a 'One Health' approach to protecting the ocean, addressing the whole Earth ocean system for better and more equitable social, cultural, economic, and environmental outcomes at its core. Speaking with one voice through a narrative that captures the latest science, concerns, and linkages to humanity is a precondition to action, by elevating humankind's understanding of our relationship with 'planet Ocean' and why it needs to become a central theme to everyone's lives. We have only one ocean, we must protect it, now. There is no 'Ocean B'.
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Affiliation(s)
- D. Laffoley
- IUCN World Commission on Protected AreasIUCN (International Union for Conservation of Nature)GlandSwitzerland
| | - J.M. Baxter
- Marine Alliance for Science and Technology for Scotland, School of Biology, East SandsUniversity of St AndrewsSt AndrewsUK
| | - D.J. Amon
- Department of Life SciencesNatural History MuseumLondonUK
| | - J. Claudet
- National Centre for Scientific ResearchPSL Université Paris, CRIOBE, USR 3278 CNRS‐EPHE‐UPVDParisFrance
| | - J.M. Hall‐Spencer
- School of Marine and Biological SciencesUniversity of PlymouthPlymouthUK
- Shimoda Marine Research CenterUniversity of TsukubaShimodaJapan
| | - K. Grorud‐Colvert
- Department of Integrative BiologyOregon State UniversityCorvallisUSA
| | - L.A. Levin
- Center for Marine Biodiversity and Conservation, Scripps Institution of OceanographyUniversity of California San DiegoLa JollaUSA
| | - P.C. Reid
- School of Marine and Biological SciencesUniversity of PlymouthPlymouthUK
- The LaboratoryThe Continuous Plankton Recorder Survey, Marine Biological AssociationCitadel HillPlymouthUK
| | - A.D. Rogers
- Somerville CollegeUniversity of OxfordOxfordUK
- REV OceanLysakerNorway
| | | | - L.C. Woodall
- Department of ZoologyUniversity of OxfordOxfordUK
| | - N.F. Andersen
- Department of Environment and GeographyUniversity of YorkYorkUK
- Centre for Ecology and ConservationUniversity of ExeterPenrynUK
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17
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Petti FM, Furrer H, Collo E, Martinetto E, Bernardi M, Delfino M, Romano M, Piazza M. Archosauriform footprints in the Lower Triassic of Western Alps and their role in understanding the effects of the Permian-Triassic hyperthermal. PeerJ 2020; 8:e10522. [PMID: 33384899 PMCID: PMC7751423 DOI: 10.7717/peerj.10522] [Citation(s) in RCA: 5] [Impact Index Per Article: 1.3] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 08/10/2020] [Accepted: 11/17/2020] [Indexed: 11/20/2022] Open
Abstract
The most accepted killing model for the Permian-Triassic mass extinction (PTME) postulates that massive volcanic eruption (i.e., the Siberian Traps Large Igneous Province) led to geologically rapid global warming, acid rain and ocean anoxia. On land, habitable zones were drastically reduced, due to the combined effects of heating, drought and acid rains. This hyperthermal had severe effects also on the paleobiogeography of several groups of organisms. Among those, the tetrapods, whose geographical distribution across the end-Permian mass extinction (EPME) was the subject of controversy in a number of recent papers. We here describe and interpret a new Early Triassic (?Olenekian) archosauriform track assemblage from the Gardetta Plateau (Briançonnais, Western Alps, Italy) which, at the Permian-Triassic boundary, was placed at about 11° North. The tracks, both arranged in trackways and documented by single, well-preserved imprints, are assigned to Isochirotherium gardettensis ichnosp. nov., and are here interpreted as produced by a non-archosaurian archosauriform (erytrosuchid?) trackmaker. This new discovery provides further evidence for the presence of archosauriformes at low latitudes during the Early Triassic epoch, supporting a model in which the PTME did not completely vacate low-latitude lands from tetrapods that therefore would have been able to cope with the extreme hot temperatures of Pangaea mainland.
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Affiliation(s)
| | - Heinz Furrer
- Paläontologisches Institut und Museum, Universität Zürich, Zürich, Switzerland
| | | | - Edoardo Martinetto
- Dipartimento di Scienze della Terra, Università degli Studi di Torino, Turin, Italy
| | | | - Massimo Delfino
- Dipartimento di Scienze della Terra, Università degli Studi di Torino, Turin, Italy.,Institut Català de Paleontologia Miquel Crusafont, Universitat Autónoma de Barcelona. Edifici ICTA-ICP, Barcelona, Spain
| | - Marco Romano
- Dipartimento di Scienze della Terra, Sapienza, University of Rome, Rome, Italy
| | - Michele Piazza
- Dipartimento di Scienze della Terra, dell'Ambiente e della Vita, Università di Genova, Genoa, Italy
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18
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Synthesis and sensing behavior of a new multichannel sensor based on thiazolyl ferrocene-rhodamine for Hg2+ detection. Microchem J 2020. [DOI: 10.1016/j.microc.2020.105257] [Citation(s) in RCA: 7] [Impact Index Per Article: 1.8] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 12/29/2022]
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19
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The struggle to equilibrate outer and inner milieus: Renal evolution revisited. Ann Anat 2020; 233:151610. [PMID: 33065247 DOI: 10.1016/j.aanat.2020.151610] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 02/26/2020] [Revised: 09/14/2020] [Accepted: 09/15/2020] [Indexed: 11/20/2022]
Abstract
The journey of life, from primordial protoplasm to a complex vertebrate form, is a tale of survival against incessant alterations in climate, surface topography, food chain, and chemistry of the external environment. Kidneys present with an ensemble embodiment of the adaptations devised by diverse life-forms to cope with such challenges and maintain a chemical equilibrium of water and solutes, both in and outside the body. This minireview revisits renal evolution utilizing the classic: From Fish to Philosopher; the story of our internal environment, by Prof. Homer W. Smith (1895-1962) as a template. Prof. Smith's views exemplified the invention of glomeruli, or its abolishment, as a mechanism to filter water. Moreover, with the need to preserve water, as in reptiles, the loop of Henle was introduced to concentrate urine. When compared to smaller mammals, the larger ones, albeit having loops of Henle of similar lengths, demonstrated a distinct packing of the nephrons in kidneys. Moreover, the renal portal system degenerated in mammals, while still present in other vertebrates. This account will present with a critique of the current concepts of renal evolution while examining how various other factors, including the ones that we know more about now, such as genetic factors, synchronize to achieve renal development. Finally, it will try to assess the validity of ideas laid by Prof. Smith with the knowledge that we possess now, and understand the complex architecture that evolution has imprinted on the kidneys during its struggle to survive over epochs.
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20
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Khlebodarova TM, Likhoshvai VA. Causes of global extinctions in the history of life: facts and hypotheses. Vavilovskii Zhurnal Genet Selektsii 2020; 24:407-419. [PMID: 33659824 PMCID: PMC7716527 DOI: 10.18699/vj20.633] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/19/2022] Open
Abstract
Paleontologists define global extinctions on Earth as a loss of about three-quarters of plant and animal species over a relatively short period of time. At least five global extinctions are documented in the Phanerozoic fossil record (~500-million-year period): ~65, 200, 260, 380, and 440 million years ago. In addition, there is evidence of global extinctions in earlier periods of life on Earth - during the Late Cambrian (~500 million years ago) and Ediacaran periods (more than 540 million years ago). There is still no common opinion on the causes of their occurrence. The current study is a systematized review of the data on recorded extinctions of complex life forms on Earth from the moment of their occurrence during the Ediacaran period to the modern period. The review discusses possible causes for mass extinctions in the light of the influence of abiogenic factors, planetary or astronomical, and the consequences of their actions. We evaluate the pros and cons of the hypothesis on the presence of periodicity in the extinction of Phanerozoic marine biota. Strong evidence that allows us to hypothesize that additional mechanisms associated with various internal biotic factors are responsible for the emergence of extinctions in the evolution of complex life forms is discussed. Developing the idea of the internal causes of periodicity and discontinuity in evolution, we propose our own original hypothesis, according to which the bistability phenomenon underlies the complex dynamics of the biota development, which is manifested in the form of global extinctions. The bistability phenomenon arises only in ecosystems with predominant sexual reproduction. Our hypothesis suggests that even in the absence of global abiotic catastrophes, extinctions of biota would occur anyway. However, our hypothesis does not exclude the possibility that in different periods of the Earth's history the biota was subjected to powerful external influences that had a significant impact on its further development, which is reflected in the Earth's fossil record.
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Affiliation(s)
- T M Khlebodarova
- Institute of Cytology and Genetics of Siberian Branch of the Russian Academy of Sciences, Novosibirsk, Russia
| | - V A Likhoshvai
- Institute of Cytology and Genetics of Siberian Branch of the Russian Academy of Sciences, Novosibirsk, Russia
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21
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Dal Corso J, Mills BJW, Chu D, Newton RJ, Mather TA, Shu W, Wu Y, Tong J, Wignall PB. Permo-Triassic boundary carbon and mercury cycling linked to terrestrial ecosystem collapse. Nat Commun 2020; 11:2962. [PMID: 32528009 PMCID: PMC7289894 DOI: 10.1038/s41467-020-16725-4] [Citation(s) in RCA: 30] [Impact Index Per Article: 7.5] [Reference Citation Analysis] [Abstract] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 12/23/2019] [Accepted: 05/18/2020] [Indexed: 11/09/2022] Open
Abstract
Records suggest that the Permo-Triassic mass extinction (PTME) involved one of the most severe terrestrial ecosystem collapses of the Phanerozoic. However, it has proved difficult to constrain the extent of the primary productivity loss on land, hindering our understanding of the effects on global biogeochemistry. We build a new biogeochemical model that couples the global Hg and C cycles to evaluate the distinct terrestrial contribution to atmosphere-ocean biogeochemistry separated from coeval volcanic fluxes. We show that the large short-lived Hg spike, and nadirs in δ202Hg and δ13C values at the marine PTME are best explained by a sudden, massive pulse of terrestrial biomass oxidation, while volcanism remains an adequate explanation for the longer-term geochemical changes. Our modelling shows that a massive collapse of terrestrial ecosystems linked to volcanism-driven environmental change triggered significant biogeochemical changes, and cascaded organic matter, nutrients, Hg and other organically-bound species into the marine system.
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Affiliation(s)
- Jacopo Dal Corso
- School of Earth and Environments, University of Leeds, Leeds, LS2 9JT, UK. .,State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan, 430074, China.
| | - Benjamin J W Mills
- School of Earth and Environments, University of Leeds, Leeds, LS2 9JT, UK.
| | - Daoliang Chu
- State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan, 430074, China
| | - Robert J Newton
- School of Earth and Environments, University of Leeds, Leeds, LS2 9JT, UK
| | - Tamsin A Mather
- Department of Earth Sciences, University of Oxford, South Parks Road, Oxford, OX1 3AN, UK
| | - Wenchao Shu
- State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan, 430074, China
| | - Yuyang Wu
- State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan, 430074, China
| | - Jinnan Tong
- State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan, 430074, China
| | - Paul B Wignall
- School of Earth and Environments, University of Leeds, Leeds, LS2 9JT, UK
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22
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Marshall JEA, Lakin J, Troth I, Wallace-Johnson SM. UV-B radiation was the Devonian-Carboniferous boundary terrestrial extinction kill mechanism. SCIENCE ADVANCES 2020; 6:eaba0768. [PMID: 32518822 PMCID: PMC7253167 DOI: 10.1126/sciadv.aba0768] [Citation(s) in RCA: 15] [Impact Index Per Article: 3.8] [Reference Citation Analysis] [Abstract] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 11/02/2019] [Accepted: 03/23/2020] [Indexed: 05/28/2023]
Abstract
There is an unexplained terrestrial mass extinction at the Devonian-Carboniferous boundary (359 million years ago). The discovery in east Greenland of malformed land plant spores demonstrates that the extinction was coincident with elevated UV-B radiation demonstrating ozone layer reduction. Mercury data through the extinction level prove that, unlike other mass extinctions, there were no planetary scale volcanic eruptions. Importantly, the Devonian-Carboniferous boundary terrestrial mass extinction was coincident with a major climatic warming that ended the intense final glacial cycle of the latest Devonian ice age. A mechanism for ozone layer reduction during rapid warming is increased convective transport of ClO. Hence, ozone loss during rapid warming is an inherent Earth system process with the unavoidable conclusion that we should be alert for such an eventuality in the future warming world.
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Affiliation(s)
- John E. A. Marshall
- School of Ocean and Earth Science, University of Southampton, National Oceanography Centre, European Way, Southampton SO14 3ZH, UK
| | - Jon Lakin
- School of Ocean and Earth Science, University of Southampton, National Oceanography Centre, European Way, Southampton SO14 3ZH, UK
| | - Ian Troth
- School of Ocean and Earth Science, University of Southampton, National Oceanography Centre, European Way, Southampton SO14 3ZH, UK
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23
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Zerkle AL, Yin R, Chen C, Li X, Izon GJ, Grasby SE. Anomalous fractionation of mercury isotopes in the Late Archean atmosphere. Nat Commun 2020; 11:1709. [PMID: 32249783 PMCID: PMC7136252 DOI: 10.1038/s41467-020-15495-3] [Citation(s) in RCA: 14] [Impact Index Per Article: 3.5] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 07/16/2019] [Accepted: 03/11/2020] [Indexed: 11/17/2022] Open
Abstract
Earth's surface underwent a dramatic transition ~2.3 billion years ago when atmospheric oxygen first accumulated during the Great Oxidation Event, but the detailed composition of the reducing early atmosphere is not well known. Here we develop mercury (Hg) stable isotopes as a proxy for paleoatmospheric chemistry and use Hg isotope data from 2.5 billion-year-old sedimentary rocks to examine changes in the Late Archean atmosphere immediately prior to the Great Oxidation Event. These sediments preserve evidence of strong photochemical transformations of mercury in the absence of molecular oxygen. In addition, these geochemical records combined with previously published multi-proxy data support a vital role for methane in Earth's early atmosphere.
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Affiliation(s)
- Aubrey L Zerkle
- School of Earth and Environmental Sciences and Centre for Exoplanet Science, University of St Andrews, St Andrews, Fife, KY16 9AL, Scotland, UK.
| | - Runsheng Yin
- State Key Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang, 550081, China.
| | - Chaoyue Chen
- State Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang, 550081, China
| | - Xiangdong Li
- Department of Civil and Environmental Engineering, The Hong Kong Polytechnic University, Hung Hom, Kowloon, Hong Kong
| | - Gareth J Izon
- School of Earth and Environmental Sciences and Centre for Exoplanet Science, University of St Andrews, St Andrews, Fife, KY16 9AL, Scotland, UK
- Department of Earth, Atmospheric & Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA, USA
| | - Stephen E Grasby
- Geological Survey of Canada, Calgary Natural Resources Canada, 3303 33rd Street NW, Calgary, AB, T2L 2A7, Canada
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24
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Altered fluvial patterns in North China indicate rapid climate change linked to the Permian-Triassic mass extinction. Sci Rep 2019; 9:16818. [PMID: 31727990 PMCID: PMC6856103 DOI: 10.1038/s41598-019-53321-z] [Citation(s) in RCA: 22] [Impact Index Per Article: 4.4] [Reference Citation Analysis] [Abstract] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 05/13/2019] [Accepted: 10/21/2019] [Indexed: 11/18/2022] Open
Abstract
The causes of the severest crisis in the history of life around the Permian-Triassic boundary (PTB) remain controversial. Here we report that the latest Permian alluvial plains in Shanxi, North China, went through a rapid transition from meandering rivers to braided rivers and aeolian systems. Soil carbonate carbon isotope (δ13C), oxygen isotope (δ18O), and geochemical signatures of weathering intensity reveal a consistent pattern of deteriorating environments (cool, arid, and anoxic conditions) and climate fluctuations across the PTB. The synchronous ecological collapse is confirmed by a dramatic reduction or disappearance of dominant plants, tetrapods and invertebrates and a bloom of microbially-induced sedimentary structures. A similar rapid switch in fluvial style is seen worldwide (e.g. Karoo Basin, Russia, Australia) in terrestrial boundary sequences, all of which may be considered against a background of global marine regression. The synchronous global expansion of alluvial fans and high-energy braided streams is a response to abrupt climate change associated with aridity, hypoxia, acid rain, and mass wasting. Where neighbouring uplands were not uplifting or basins subsiding, alluvial fans are absent, but in these areas the climate change is evidenced by the disruption of pedogenesis.
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Li W, Gou W, Li W, Zhang T, Yu B, Liu Q, Shi J. Environmental applications of metal stable isotopes: Silver, mercury and zinc. ENVIRONMENTAL POLLUTION (BARKING, ESSEX : 1987) 2019; 252:1344-1356. [PMID: 31254892 DOI: 10.1016/j.envpol.2019.06.037] [Citation(s) in RCA: 3] [Impact Index Per Article: 0.6] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 04/01/2019] [Revised: 06/03/2019] [Accepted: 06/08/2019] [Indexed: 06/09/2023]
Abstract
With developments in multi-collector inductively coupled plasma mass spectrometry (MC-ICP-MS), applications of metal stable isotopes received increasing attentions in the studies of source and fate of heavy metals in the environment. In light of the rapid progresses in this emerging field, we attempted to review the recent findings comprehensively in a way that environmental scientists can easily read. This review started with an introduction of basic terminologies in isotope geochemistry, followed with detailed descriptions of instrumentation and analytical procedures, and finally focused on the cases of three typical metal stable isotopes (Ag, Hg and Zn) to illustrate how they were applied to address environmental issues. Additionally, future perspectives on the applicability, opportunities, and limitations of metal stable isotope techniques as novel approaches in advancing environmental chemistry were discussed.
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Affiliation(s)
- Wei Li
- Key Laboratory of Surficial Geochemistry, Ministry of Education, School of Earth Sciences and Engineering, Nanjing University, Nanjing, 210023, China
| | - Wenxian Gou
- Key Laboratory of Surficial Geochemistry, Ministry of Education, School of Earth Sciences and Engineering, Nanjing University, Nanjing, 210023, China
| | - Weiqiang Li
- State Key Laboratory of Ore Deposit Research, School of Earth Sciences and Engineering, Nanjing University, Nanjing, 210023, China
| | - Tuoya Zhang
- State Key Laboratory of Environmental Chemistry and Ecotoxicology, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing, 100085, China
| | - Ben Yu
- State Key Laboratory of Environmental Chemistry and Ecotoxicology, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing, 100085, China
| | - Qian Liu
- State Key Laboratory of Environmental Chemistry and Ecotoxicology, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing, 100085, China
| | - Jianbo Shi
- State Key Laboratory of Environmental Chemistry and Ecotoxicology, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing, 100085, China.
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