An authigenic response to Ediacaran surface oxidation: Remarkable micron-scale isotopic heterogeneity revealed by SIMS

[1]  D. Feng,et al.  A transient peak in marine sulfate after the 635-Ma snowball Earth , 2022, Proceedings of the National Academy of Sciences of the United States of America.

[2]  F. Macdonald,et al.  Global and local drivers of the Ediacaran Shuram carbon isotope excursion , 2022, Earth and Planetary Science Letters.

[3]  Huaichun Wu,et al.  Astrochronologic calibration of the Shuram carbon isotope excursion with new data from South China , 2022, Global and Planetary Change.

[4]  G. Shields,et al.  A short-lived oxidation event during the early Ediacaran and delayed oxygenation of the Proterozoic ocean , 2022, Earth and Planetary Science Letters.

[5]  Cheng Meng,et al.  Barite in the Ediacaran Doushantuo Formation and its implications for marine carbon cycling during the largest negative carbon isotope excursion in Earth’s history , 2022, Precambrian Research.

[6]  Q. Tang,et al.  Neoproterozoic Earth-life system , 2022, Precambrian Research.

[7]  F. Macdonald,et al.  The tempo of Ediacaran evolution , 2021, Science advances.

[8]  Guanghui Wu,et al.  Carbon isotopic chemostratigraphy of the Ediacaran-Cambrian successions in the northwestern Tarim Craton, NW China: Correlations with Gondwana supercontinent , 2021, Global and Planetary Change.

[9]  N. Planavsky,et al.  A largely invariant marine dissolved organic carbon reservoir across Earth's history , 2021, Proceedings of the National Academy of Sciences.

[10]  E. al.,et al.  Guttulatic calcite: A carbonate microtexture that reveals frigid formation conditions , 2021, Geology.

[11]  S. Xiao,et al.  Dynamic interplay of biogeochemical C, S and Ba cycles in response to the Shuram oxygenation event , 2021, Journal of the Geological Society.

[12]  B. Pokrovsky,et al.  C, O, and Sr Isotope Geochemistry of the Vendian Shuram–Wonoka Anomaly and Associated Metasedimentary Rocks in the Inner Part of the Patom Upland (Central Siberia) , 2021, Lithology and Mineral Resources.

[13]  S. Xiao,et al.  Deposition or diagenesis? Probing the Ediacaran Shuram excursion in South China by SIMS , 2021, Global and Planetary Change.

[14]  Huan Cui.  Inside out: deep carbon linked to deep-time carbon cycle. , 2021, Science bulletin.

[15]  Yanan Shen,et al.  The largest negative carbon isotope excursions in Neoproterozoic carbonates caused by recycled carbonatite volcanic ash. , 2021, Science bulletin.

[16]  K. Kirsimäe,et al.  The grandest of them all: the Lomagundi–Jatuli Event and Earth's oxygenation , 2020, Journal of the Geological Society.

[17]  D. Schrag,et al.  The role of authigenic carbonate in Neoproterozoic carbon isotope excursions , 2020 .

[18]  Mingsong Li,et al.  Astrochronology of the Ediacaran Shuram carbon isotope excursion, Oman , 2020 .

[19]  Yanan Shen,et al.  High primary productivity during the Ediacaran Period revealed by the covariation of paired C-isotopic records from South China , 2020 .

[20]  N. Planavsky,et al.  Simulating meteoric and mixing zone carbonate diagenesis with a two-dimensional reactive transport model , 2020, American Journal of Science.

[21]  K. Kirsimäe,et al.  The Paleoproterozoic Francevillian succession of Gabon and the Lomagundi-Jatuli event , 2020, Geology.

[22]  P. Claeys,et al.  Global or regional? Constraining the origins of the middle Bambuí carbon cycle anomaly in Brazil , 2020 .

[23]  Zhong‐Qiang Chen,et al.  Transient and stepwise ocean oxygenation during the late Ediacaran Shuram Excursion: Insights from carbonate δ238U of northwestern Mexico , 2020 .

[24]  K. Kirsimäe,et al.  Oxygenated conditions in the aftermath of the Lomagundi-Jatuli Event: The carbon isotope and rare earth element signatures of the Paleoproterozoic Zaonega Formation, Russia , 2020 .

[25]  E. Sperling,et al.  Calibrating the coevolution of Ediacaran life and environment , 2020, Proceedings of the National Academy of Sciences.

[26]  A. J. Kaufman,et al.  Using SIMS to decode noisy stratigraphic δ13C variations in Ediacaran carbonates , 2020 .

[27]  T. Lyons,et al.  Massive formation of early diagenetic dolomite in the Ediacaran ocean: Constraints on the “dolomite problem” , 2020, Proceedings of the National Academy of Sciences.

[28]  M. Fantle,et al.  The Role of Diagenesis in Shaping the Geochemistry of the Marine Carbonate Record , 2020, Annual Review of Earth and Planetary Sciences.

[29]  A. Anbar,et al.  Comparison of Ediacaran platform and slope δ238U records in South China: Implications for global-ocean oxygenation and the origin of the Shuram Excursion , 2020 .

[30]  S. Peters,et al.  Large isotopic variability at the micron-scale in ‘Shuram’ excursion carbonates from South Australia , 2020, Earth and Planetary Science Letters.

[31]  A. J. Kaufman,et al.  Primary or secondary? A dichotomy of the strontium isotope anomalies in the Ediacaran carbonates of Saudi Arabia , 2020 .

[32]  A. Knoll,et al.  Carbon isotopes in clastic rocks and the Neoproterozoic carbon cycle , 2020, American Journal of Science.

[33]  David S. Jones,et al.  Sea level, carbonate mineralogy, and early diagenesis controlled δ13C records in Upper Ordovician carbonates , 2020 .

[34]  J. Valley,et al.  Regionally Correlated Oxygen and Carbon Isotope Zonation in Diagenetic Carbonates of the Bakken Formation , 2020 .

[35]  J. Ogg,et al.  Astronomical time scale for the middle-upper Doushantuo Formation of Ediacaran in South China: Implications for the duration of the Shuram/Wonoka negative δ13C excursion , 2019, Palaeogeography, Palaeoclimatology, Palaeoecology.

[36]  P. Claeys,et al.  ICE OR FIRE? CONSTRAINING THE ORIGIN OF ISOTOPICALLY ANOMALOUS CAP CARBONATE CEMENTS BY SIMS , 2019 .

[37]  P. Hoffman,et al.  Seawater-buffered diagenesis, destruction of carbon isotope excursions, and the composition of DIC in Neoproterozoic oceans , 2019, Proceedings of the National Academy of Sciences.

[38]  T. Lenton,et al.  Unique Neoproterozoic carbon isotope excursions sustained by coupled evaporite dissolution and pyrite burial , 2019, Nature Geoscience.

[39]  J. Strauss,et al.  Upper Windermere Supergroup and the transition from rifting to continent-margin sedimentation, Nadaleen River area, northern Canadian Cordillera , 2019, GSA Bulletin.

[40]  A. Anbar,et al.  Global marine redox changes drove the rise and fall of the Ediacara biota , 2019, Geobiology.

[41]  K. Kirsimäe,et al.  Hydrothermal dedolomitisation of carbonate rocks of the Paleoproterozoic Zaonega Formation, NW Russia — Implications for the preservation of primary C isotope signals , 2019, Chemical Geology.

[42]  S. Finnegan,et al.  Records of carbon and sulfur cycling during the Silurian Ireviken Event in Gotland, Sweden , 2019, Geochimica et Cosmochimica Acta.

[43]  K. Shirai,et al.  An integrated chemostratigraphic (δ13C-δ18O-87Sr/86Sr-δ15N) study of the Doushantuo Formation in western Hubei Province, South China , 2019, Precambrian Research.

[44]  Xi Chen,et al.  Oxygenation variations in the atmosphere and shallow seawaters of the Yangtze Platform during the Ediacaran Period: Clues from Cr-isotope and Ce-anomaly in carbonates , 2018, Precambrian Research.

[45]  A. J. Kaufman,et al.  The Neoproterozoic Hüttenberg δ13C anomaly: Genesis and global implications , 2018, Precambrian Research.

[46]  Yanan Shen,et al.  Ediacaran negative C-isotopic excursions associated with phosphogenic events: Evidence from South China , 2018 .

[47]  Cheng Meng,et al.  Sulfur isotope evidence for transient marine-shelf oxidation during the Ediacaran Shuram Excursion , 2018 .

[48]  J. Barbarand,et al.  The complex diagenetic history of discontinuities in shallow‐marine carbonate rocks: New insights from high‐resolution ion microprobe investigation of δ18O and δ13C of early cements , 2018 .

[49]  J. Valley,et al.  Isotopically zoned carbonate cements in Early Paleozoic sandstones of the Illinois Basin: δ 18 O and δ 13 C records of burial and fluid flow , 2017 .

[50]  R. Bodnar,et al.  Raman geothermometry of carbonaceous material in the basal Ediacaran Doushantuo cap dolostone: The thermal history of extremely negative δ13C signatures in the aftermath of the terminal Cryogenian snowball Earth glaciation , 2017 .

[51]  X. Chen,et al.  Integrated carbon, sulfur, and nitrogen isotope chemostratigraphy of the Ediacaran Lantian Formation in South China: Spatial gradient, ocean redox oscillation, and fossil distribution , 2017, Geobiology.

[52]  Wei Wang,et al.  Chemostratigraphy of the Ediacaran basinal setting on the Yangtze platform, South China: Oceanographic and diagenetic aspects of the carbon isotopic depth gradient , 2017 .

[53]  K. Kodama,et al.  Rock magnetic chronostratigraphy of the Shuram carbon isotope excursion: Wonoka Formation, Australia , 2017 .

[54]  Cheng Meng,et al.  Uncovering the spatial heterogeneity of Ediacaran carbon cycling , 2017, Geobiology.

[55]  A. J. Kaufman,et al.  Was the Ediacaran Shuram Excursion a globally synchronized early diagenetic event? Insights from methane-derived authigenic carbonates in the uppermost Doushantuo Formation, South China , 2017 .

[56]  J. Valley,et al.  In situ δ13C and δ18O microanalysis by SIMS: A method for characterizing the carbonate components of natural and engineered CO2-reservoirs , 2017 .

[57]  Yongxian Li,et al.  Rock magnetic cyclostratigraphy of the Doushantuo Formation, South China and its implications for the duration of the Shuram carbon isotope excursion , 2017 .

[58]  D. Grazhdankin,et al.  Towards an ediacaran time scale: Problems, protocols, and prospects , 2016 .

[59]  Wei Wang,et al.  Methane-derived authigenic carbonate from the lower Doushantuo Formation of South China: Implications for seawater sulfate concentration and global carbon cycle in the early Ediacaran ocean , 2016 .

[60]  F. Macdonald,et al.  Dodging snowballs: Geochronology of the Gaskiers glaciation and the first appearance of the Ediacaran biota , 2016 .

[61]  E. Bellefroid,et al.  Integrated geochemical-petrographic insights from component-selective δ238U of Cryogenian marine carbonates , 2016 .

[62]  A. J. Kaufman,et al.  Phosphogenesis associated with the Shuram Excursion: Petrographic and geochemical observations from the Ediacaran Doushantuo Formation of South China , 2016 .

[63]  J. Valley,et al.  Secondary Ion Mass Spectrometry Bias on Isotope Ratios in Dolomite–Ankerite, Part II: δ13C Matrix Effects , 2016 .

[64]  J. Valley,et al.  Microanalysis of carbonate cement δ18O in a CO2-storage system seal: Insights into the diagenetic history of the Eau Claire Formation (Upper Cambrian), Illinois Basin , 2016 .

[65]  Wei Wang,et al.  Diagenetic overprint to a negative carbon isotope anomaly associated with the Gaskiers glaciation of the Ediacaran Doushantuo Formation in South China , 2016 .

[66]  A. Ravelo,et al.  Mineralogical, geochemical and isotopic characterization of authigenic carbonates from the methane-bearing sediments of the Bering Sea continental margin (IODP Expedition 323, Sites U1343–U1345) , 2016 .

[67]  Xiaoying Shi,et al.  Paired carbonate and organic carbon isotope variations of the Ediacaran Doushantuo Formation from an upper slope section at Siduping, South China , 2016 .

[68]  D. Schrag,et al.  Neoproterozoic stratigraphy of the Zavkhan terrane of Mongolia: The backbone for Cryogenian and early Ediacaran chemostratigraphic records , 2016, American Journal of Science.

[69]  Y. Peng,et al.  Sulfate-driven anaerobic oxidation of methane as the origin of extremely 13 C-depleted calcite in the Doushantuo cap carbonates in South China , 2015 .

[70]  Qin Ye,et al.  Stratigraphic position of the Ediacaran Miaohe biota and its constrains on the age of the upper Doushantuo δ13C anomaly in the Yangtze Gorges area, South China , 2015 .

[71]  N. Butterfield.  The Neoproterozoic , 2015, Current Biology.

[72]  Christopher P. Reed,et al.  Enigmatic carbonates of the Ombombo Subgroup, Otavi Fold Belt, Namibia: A prelude to extreme Cryogenian anoxia? , 2015 .

[73]  A. J. Kaufman,et al.  Redox architecture of an Ediacaran ocean margin: Integrated chemostratigraphic (δ13C–δ34S–87Sr/86Sr–Ce/Ce*) correlation of the Doushantuo Formation, South China , 2015 .

[74]  F. Macdonald,et al.  A Cryogenian chronology: Two long-lasting synchronous Neoproterozoic glaciations , 2015 .

[75]  K. Hoffmann,et al.  Dynamic redox conditions control late Ediacaran metazoan ecosystems in the Nama Group, Namibia , 2015 .

[76]  T. Bontognali,et al.  Methanogenesis produces strong 13C enrichment in stromatolites of Lagoa Salgada, Brazil: a modern analogue for Palaeo‐/Neoproterozoic stromatolites? , 2015, Geobiology.

[77]  B. Pokrovsky,et al.  Geochemistry of C, O, and Sr isotopes in the Neoproterozoic carbonates from the southwestern Patom paleobasin, southern Middle Siberia , 2015, Lithology and Mineral Resources.

[78]  A. Maloof,et al.  Stratigraphic expression of Earth's deepest δ13C excursion in the Wonoka Formation of South Australia , 2015, American Journal of Science.

[79]  L. Hinnov,et al.  Rock Magnetic Cyclostratigraphy , 2014 .

[80]  Xiaoying Shi,et al.  Organic carbon isotope gradient and ocean stratification across the late Ediacaran-Early Cambrian Yangtze Platform , 2014, Science China Earth Sciences.

[81]  D. Schrag,et al.  The stratigraphic relationship between the Shuram carbon isotope excursion, the oxygenation of Neoproterozoic oceans, and the first appearance of the Ediacara biota and bilaterian trace fossils in northwestern Canada , 2013 .

[82]  J. Grotzinger,et al.  Carbon isotopes and lipid biomarkers from organic‐rich facies of the Shuram Formation, Sultanate of Oman , 2013, Geobiology.

[83]  Maoyan Zhu,et al.  The DOUNCE event at the top of the Ediacaran Doushantuo Formation, South China: Broad stratigraphic occurrence and non-diagenetic origin , 2013 .

[84]  Xi Chen,et al.  Cerium anomaly variations in Ediacaran–earliest Cambrian carbonates from the Yangtze Gorges area, South China: Implications for oxygenation of coeval shallow seawater , 2013 .

[85]  D. Schrag,et al.  Authigenic Carbonate and the History of the Global Carbon Cycle , 2013, Science.

[86]  Maoyan Zhu,et al.  Carbon isotope chemostratigraphy and sedimentary facies evolution of the Ediacaran Doushantuo Formation in western Hubei, South China , 2013 .

[87]  V. Barbin.  Application of cathodoluminescence microscopy to recent and past biological materials: a decade of progress , 2013, Mineralogy and Petrology.

[88]  J. Götze.  Application of Cathodoluminescence Microscopy and Spectroscopy in Geosciences , 2012, Microscopy and Microanalysis.

[89]  Wei Wang,et al.  A pronounced negative δ13C excursion in an Ediacaran succession of western Yangtze Platform: A possible equivalent to the Shuram event and its implication for chemostratigraphic correlation in South China , 2012 .

[90]  Z. Yang,et al.  Deciphering the impact of diagenesis overprint on negative δ13C excursions using rock magnetism: Case study of Ediacaran carbonates, Yangjiaping section, South China , 2012 .

[91]  A. Maloof,et al.  A syn‐depositional age for Earth’s deepest δ13C excursion required by isotope conglomerate tests , 2012 .

[92]  A. J. Kaufman,et al.  Sustained low marine sulfate concentrations from the Neoproterozoic to the Cambrian: Insights from carbonates of northwestern Mexico and eastern California , 2012 .

[93]  Johannes E. Schindelin,et al.  Fiji: an open-source platform for biological-image analysis , 2012, Nature Methods.

[94]  G. Shields,et al.  The Ediacaran Period , 2012, Geologic Time Scale 2020.

[95]  M. Wallace,et al.  Synsedimentary diagenesis in a Cryogenian reef complex: Ubiquitous marine dolomite precipitation , 2012 .

[96]  K. Wallmann,et al.  The Global Carbon Cycle: Geological Processes , 2012 .

[97]  S. Xiao,et al.  Rare earth elements and carbon isotope geochemistry of the Doushantuo Formation in South China: Implication for middle Ediacaran shallow marine redox conditions , 2012 .

[98]  D. Schrag,et al.  Uncovering the Neoproterozoic carbon cycle , 2012, Nature.

[99]  L. Kump,et al.  Isotopic Evidence for Massive Oxidation of Organic Matter Following the Great Oxidation Event , 2011, Science.

[100]  D. Feng,et al.  Post-depositional origin of highly 13C-depleted carbonate in the Doushantuo cap dolostone in South China: Insights from petrography and stable carbon isotopes , 2011 .

[101]  Wei Wang,et al.  Ediacaran chemostratigraphy and paleoceanography at a shallow marine setting in northwestern Hunan Province, South China , 2011 .

[102]  W. Fischer,et al.  The stratigraphic expression of a large negative carbon isotope excursion from the Ediacaran Johnnie Formation, Death Valley , 2011 .

[103]  A. Derkowski,et al.  A hydrothermal origin for isotopically anomalous cap dolostone cements from south China , 2011, Nature.

[104]  Xiaoying Shi,et al.  Stratigraphy and paleogeography of the Ediacaran Doushantuo Formation (ca. 635-551Ma) in South China , 2011 .

[105]  J. Grotzinger,et al.  Enigmatic origin of the largest-known carbon isotope excursion in Earth's history , 2011 .

[106]  J. Götze,et al.  MANGANESE-ACTIVATED CATHODOLUMINESCENCE OF SELECTED CARBONATE MINERALS. , 2011 .

[107]  D. Canfield,et al.  Towards a quantitative understanding of the late Neoproterozoic carbon cycle , 2011, Proceedings of the National Academy of Sciences.

[108]  Xiaoying Shi,et al.  Organic carbon isotope constraints on the dissolved organic carbon (DOC) reservoir at the Cryogenian-Ediacaran transition , 2010 .

[109]  R. Neuser,et al.  From tabular to rhombohedral dolomite crystals in Zechstein 2 dolostones from Scharzfeld (SW Harz/Germany): A case study with combined CL and EBSD investigations , 2010 .

[110]  L. Derry.  A burial diagenesis origin for the Ediacaran Shuram–Wonoka carbon isotope anomaly , 2010 .

[111]  A. Sessions,et al.  A Stratified Redox Model for the Ediacaran Ocean , 2010, Science.

[112]  J. Besse,et al.  A multilayered water column in the Ediacaran Yangtze platform? Insights from carbonate and organic matter paired δ13C , 2009 .

[113]  M. Kennedy,et al.  The late Precambrian greening of the Earth , 2009, Nature.

[114]  J. Valley,et al.  Intratest oxygen isotope variability in the planktonic foraminifer N. pachyderma: Real vs. apparent vital effects by ion microprobe , 2009 .

[115]  M. Wallace,et al.  Facies-dependent δ13C variation from a Cryogenian platform margin, South Australia: Evidence for stratified Neoproterozoic oceans? , 2009 .

[116]  B. Pokrovsky,et al.  Constraints on 87Sr/86Sr of Late Ediacaran seawater: insight from Siberian high-Sr limestones , 2009, Journal of the Geological Society.

[117]  M. Kennedy,et al.  Carbon isotope excursions and the oxidant budget of the Ediacaran atmosphere and ocean , 2008 .

[118]  Xiaoying Shi,et al.  Chemocline instability and isotope variations of the Ediacaran Doushantuo basin in South China , 2008 .

[119]  S. Xiao,et al.  Carbon isotope evidence for widespread methane seeps in the ca. 635 Ma Doushantuo cap carbonate in south China , 2008 .

[120]  A. J. Kaufman,et al.  Pulsed oxidation and biological evolution in the Ediacaran Doushantuo Formation , 2008, Proceedings of the National Academy of Sciences.

[121]  H. Strauss,et al.  From snowball earth to the Cambrian bioradiation: Calibration of Ediacaran-Cambrian earth history in South China , 2007 .

[122]  Maoyan Zhu,et al.  Integrated Ediacaran (Sinian) chronostratigraphy of South China , 2007 .

[123]  D. Schrag,et al.  Dolomite formation in the dynamic deep biosphere: results from the Peru Margin , 2007 .

[124]  A. J. Kaufman,et al.  Carbon Isotope Variability across the Ediacaran Yangtze Platform in South China: Implications for a Large Surface-to-Deep Ocean δ13C Gradient , 2007 .

[125]  S. Xiao,et al.  Ediacaran δ13C chemostratigraphy of South China , 2007 .

[126]  A. J. Kaufman,et al.  The effect of rising atmospheric oxygen on carbon and sulfur isotope anomalies in the Neoproterozoic Johnnie Formation, Death Valley, USA , 2007 .

[127]  J. Grotzinger,et al.  Oxidation of the Ediacaran Ocean , 2006, Nature.

[128]  V. Melezhik,et al.  Carbon, oxygen, strontium, and sulfur isotopic compositions in late Precambrian rocks of the Patom Complex, central Siberia: Communication 1. results, isotope stratigraphy, and dating problems , 2006 .

[129]  N. Christie‐Blick,et al.  Stratigraphy, Sedimentary Structures, and Textures of the Late Neoproterozoic Doushantuo Cap Carbonate in South China , 2006 .

[130]  A. J. Kaufman,et al.  Stable isotope record of the terminal Neoproterozoic Krol platform in the Lesser Himalayas of northern India , 2006 .

[131]  P. Allen,et al.  Parasequence development in the Ediacaran Shuram Formation (Nafun Group, Oman): high‐resolution stratigraphic test for primary origin of negative carbon isotopic ratios , 2006 .

[132]  P. Allen,et al.  Chemostratigraphic and sedimentological framework of the largest negative carbon isotopic excursion in Earth history: The Neoproterozoic Shuram Formation (Nafun Group, Oman) , 2006 .

[133]  E. Guerroué.  Sedimentology and chemostratigraphy of the Ediacaran Shuram formation, Nafun group, Oman , 2006 .

[134]  P. Allen,et al.  50 Myr recovery from the largest negative δ13C excursion in the Ediacaran ocean , 2006 .

[135]  D. Schrag,et al.  Toward a Neoproterozoic composite carbon-isotope record , 2005 .

[136]  A. Fallick,et al.  Enigmatic nature of thick sedimentary carbonates depleted in 13C beyond the canonical mantle value: The challenges to our understanding of the terrestrial carbon cycle , 2005 .

[137]  Wei Wang,et al.  U-Pb Ages from the Neoproterozoic Doushantuo Formation, China , 2005, Science.

[138]  N. Christie‐Blick,et al.  Stable isotopic evidence for methane seeps in Neoproterozoic postglacial cap carbonates , 2003, Nature.

[139]  J. Hayes,et al.  Dynamics of the Neoproterozoic carbon cycle , 2003, Proceedings of the National Academy of Sciences of the United States of America.

[140]  S. Gilder,et al.  Combined paleomagnetic and isotopic data from the Doushantuo carbonates, South China: implications for the “snowball Earth” hypothesis , 2003 .

[141]  G. Eberli,et al.  Questioning carbonate diagenetic paradigms: evidence from the Neogene of the Bahamas , 2002 .

[142]  C. Calver.  Isotope stratigraphy of the Ediacarian (Neoproterozoic III) of the Adelaide Rift Complex, Australia, and the overprint of water column stratification , 2000 .

[143]  D. Habermann,et al.  Cathodoluminescence spectroscopy and micro-PIXE: combined high resolution Mn-analyses in dolomites – First results , 2000 .

[144]  Michael A. Arthur,et al.  Interpreting carbon-isotope excursions: carbonates and organic matter , 1999 .

[145]  A. J. Kaufman,et al.  THE ABUNDANCE OF 13C IN MARINE ORGANIC MATTER AND ISOTOPIC FRACTIONATION IN THE GLOBAL BIOGEOCHEMICAL CYCLE OF CARBON DURING THE PAST 800 MA , 1999 .

[146]  M. Kastner.  Oceanic minerals: their origin, nature of their environment, and significance. , 1999, Proceedings of the National Academy of Sciences of the United States of America.

[147]  G. Shields,et al.  Stratified oceans and oxygenation of the late Precambrian environment: a post glacial geochemical record from the Neoproterozoic of W. Mongolia , 1997 .

[148]  A. J. Kaufman,et al.  Isotopes, ice ages, and terminal Proterozoic earth history. , 1997, Proceedings of the National Academy of Sciences of the United States of America.

[149]  E. Anthony,et al.  A widespread positive δ13C anomaly at around 2.33–2.06 Ga on the Fennoscandian Shield—Comment and Reply , 1997 .

[150]  J. Karhu,et al.  Carbon isotopes and the rise of atmospheric oxygen , 1996 .

[151]  A. Fallick,et al.  A widespread positive ?13Ccarbanomaly at around 2.33?2.06 Ga on the Fennoscandian Shield: a paradox? , 1996 .

[152]  J. Banner.  Application of the trace element and isotope geochemistry of strontium to studies of carbonate diagenesis , 1995 .

[153]  S. Burns,et al.  The strontium isotopic composition of carbonates from the late Precambrian (∼ 560-540 Ma) Huqf Group of Oman , 1994 .

[154]  J. Hayes.  Factors controlling 13C contents of sedimentary organic compounds: Principles and evidence , 1993 .

[155]  B. Cervelle,et al.  Mn2+-activated luminescence in dolomite, calcite and magnesite: quantitative determination of manganese and site distribution by EPR and CL spectroscopy , 1993 .

[156]  H. Strauss,et al.  Carbon isotope evidence for the stepwise oxidation of the Proterozoic environment , 1992, Nature.

[157]  A. J. Kaufman,et al.  Biostratigraphic and chemostratigraphic correlation of Neoproterozoic sedimentary successions: upper Tindir Group, northwestern Canada, as a test case. , 1992, Geology.

[158]  A. J. Kaufman,et al.  Isotopic compositions of carbonates and organic carbon from upper Proterozoic successions in Namibia: stratigraphic variation and the effects of diagenesis and metamorphism. , 1991, Precambrian research.

[159]  J. Rimstidt,et al.  Redox conditions of calcite cementation interpreted from Mn and Fe contents of authigenic calcites , 1989 .

[160]  A. Baker,et al.  Heavy carbon in two-billion-year-old marbles from Lofoten-Vesterȧlen, Norway: Implications for the Precambrian carbon cycle , 1989 .

[161]  R. Mason.  Ion microprobe analysis of trace elements in calcite with an application to the cathodoluminescence zonation of limestone cements from the Lower Carboniferous of South Wales, U.K. , 1987 .

[162]  M. Talbot,et al.  Primary and diagenetic carbonates in the anoxic sediments of Lake Bosumtwi, Ghana , 1986 .

[163]  A. J. Kaufman,et al.  Secular variation in carbon isotope ratios from Upper Proterozoic successions of Svalbard and East Greenland , 1986, Nature.

[164]  A. B. Carpenter,et al.  Cathodoluminescence and Composition of Calcite Cement in the Taum Sauk Limestone (Upper Cambrian), Southeast Missouri , 1982 .

[165]  J. Veizer,et al.  Chemical Diagenesis of a Multicomponent Carbonate System -2: Stable Isotopes , 1981 .

[166]  J. Veizer,et al.  Chemical Diagenesis of a Multicomponent Carbonate System--1: Trace Elements , 1980 .

[167]  Cheryl K. Wilgus,et al.  Correlation of 13C12C and 34S32S secular variations , 1980 .

[168]  W. Broecker.  A boundary condition on the evolution of atmospheric oxygen , 1970 .

[169]  Wei Wang,et al.  Spatial and temporal evolution of Ediacaran carbon and sulfur cycles in the Lower Yangtze Block, South China , 2020 .

[170]  I. Jarvis,et al.  Carbon Isotope Stratigraphy , 2020, Geologic Time Scale 2020.

[171]  M. Wallace,et al.  Neoproterozoic marine carbonates and their paleoceanographic significance , 2018 .

[172]  C. Holmden,et al.  Mineralogy, early marine diagenesis, and the chemistry of shallow-water carbonate sediments , 2018 .

[173]  Wei Wang,et al.  The stratigraphic complexity of the middle Ediacaran carbon isotopic record in the Yangtze Gorges area, South China, and its implications for the age and chemostratigraphic significance of the Shuram excursion , 2017 .

[174]  Zhong Li,et al.  Multiphase Calcite Cementation and Fluids Evolution of a Deeply Buried Carbonate Reservoir in the Upper Ordovician Lianglitag Formation, Tahe Oilfield, Tarim Basin, NW China , 2017 .

[175]  J. Valley,et al.  In situ ! 13 C and ! 18 O microanalysis by SIMS : A method for characterizing the carbonate components of natural and engineered CO 2-reservoirs , 2017 .

[176]  J. Warren.  Interpreting Evaporite Textures , 2016 .

[177]  J. Warren.  Evaporites: A Geological Compendium , 2016 .

[178]  A. Fallick,et al.  Petrography and geochemistry of carbonate rocks of the Paleoproterozoic Zaonega Formation, Russia: Documentation of 13C-depleted non-primary calcite , 2014 .

[179]  N. Yoshida,et al.  Carbon and oxygen isotope chemostratigraphies of the Yangtze platform, South China: Decoding temperature and environmental changes through the Ediacaran , 2013 .

[180]  J. Schiffbauer,et al.  Trace fossil evidence for Ediacaran bilaterian animals with complex behaviors , 2013 .

[181]  A. J. Kaufman,et al.  Local δ34S variability in ̃580Ma carbonates of northwestern Mexico and the Neoproterozoic marine sulfate reservoir , 2013 .

[182]  A. J. Kaufman,et al.  Integrated chemostratigraphy of the Doushantuo Formation at the northern Xiaofenghe section (Yangtze Gorges, South China) and its implication for Ediacaran stratigraphic correlation and ocean redox models , 2012 .

[183]  F. Meyer,et al.  A syn-depositional age for Earth s deepest d 13 C excursion required by isotope conglomerate tests , 2012 .

[184]  B. Windley,et al.  The Ediacaran radiogenic Sr isotope excursion in the Doushantuo Formation in the Three Gorges area, South China , 2010 .

[185]  N. Kita.  SITU OXYGEN ISOTOPE GEOCHEMISTRY BY ION MICROPROBE , 2009 .

[186]  C. Glenn,et al.  Marine Authigenesis: From Global to Microbial , 2000 .

[187]  M. Pagel,et al.  Cathodoluminescence in Geosciences , 2000 .

[188]  S. Burns,et al.  Carbon isotopic record of the Latest Proterozoic from Oman , 1993 .

[189]  J. Peterson,et al.  Stratigraphy and Paleogeography , 1991 .

[190]  M. Tucker.  Precambrian dolomites: Petrographic and isotopic evidence that they differ from Phanerozoic dolomites , 1982 .

[191]  P. Scholle,et al.  Carbon Isotope Fluctuations in Cretaceous Pelagic Limestones: Potential Stratigraphic and Petroleum Exploration Tool , 1980 .

[192]  L. Hardie.  Anhydrite and gypsum , 1978 .

[193]  S. Sommer.  Cathodoluminescence of carbonates, 1. Characterization of cathodoluminescence from carbonate solid solutions , 1972 .