How to Build a High-Resolution Digital Geological Timeline?

References

[1] Aubry M P, Ouda K, Dupuis C, . The Global Standard Stratotype-Section and Point (GSSP) for the Base of the Eocene Series in the Dababiya Section (Egypt). Episodes, 2007, 30(4): 271-286.

[2] Burgess S D, Bowring S A, Shen S Z. High-Precision Timeline for Earth’s most Severe Extinction. Proceedings of the National Academy of Sciences of the United States of America, 2014, 1119: 3316-3321.

[3] Chen J T, Montañez I P, Zhang S, . Marine Anoxia Linked to Abrupt Global Warming during Earth’s Penultimate Icehouse. Proceedings of the National Academy of Sciences of the United States of America, 2022, 119(19): e2115231119

[4] Chlupáč I, Jaeger H, Zikmundova J. The Silurian-Devonian Boundary in the Barrandian. Bulletin of Canadian Petroleum Geology, 1972, 20 1 104-174

[5] Davydov V I. Shift in the Paradigm for GSSP Boundary Definition. Gondwana Research, 2020, 86: 266-286.

[6] Deng Y Y, Fan J X, Zhang S H, . Timing and Patterns of the Great Ordovician Biodiversification Event and Late Ordovician Mass Extinction: Perspectives from South China. Earth-Science Reviews, 2021, 220: 103743

[7] Fan J X, Chen Q, Melchin M J, . Quantitative Stratigraphy of the Wufeng and Lungmachi Black Shales and Graptolite Evolution during and after the Late Ordovician Mass Extinction. Palaeogeography, Palaeoclimatology, Palaeoecology, 2013, 389 96-114.

[8] Fan J X, Shen S Z, Erwin D H, . A High-Resolution Summary of Cambrian to Early Triassic Marine Invertebrate Biodiversity. Science, 2020, 367(6475): 272-277.

[9] Gradstein F M, Ogg J G, Schmitz M D, . Geologic Time Scale 2020, 2020, Amsterdam, Oxford, Cambridge: Elsevier

[10] Gradstein F M, Ogg J G, Schmitz M D, . The Geologic Time Scale, 2012, Amsterdam, Oxford, Cambridge: Elsevier

[11] Guo H D. Big Data Drives the Development of Earth Science. Big Earth Data, 2017, 11/2: 1-3.

[12] Gutjahr M, Ridgwell A, Sexton P F, . Very Large Release of Mostly Volcanic Carbon during the Palaeocene-Eocene Thermal Maximum. Nature, 2017, 5487669: 573-577.

[13] Hou M C, Chen A Q, Ogg J G, . China Paleogeography: Current Status and Future Challenges. Earth-Science Reviews, 2019, 189: 177-193.

[14] Hou Z S, Fan J X, Henderson C M, . Dynamic Palaeogeographic Reconstructions of theWuchiapingian Stage (Lopingian, Late Permian) for the South China Block. Palaeogeography, Palaeoclimatology, Palaeoecology, 2020, 546: 109667

[15] Li M S, Huang C J, Hinnov L, . Obliquity-Forced Climate during the Early Triassic Hothouse in China. Geology, 2016, 44(8): 623-626.

[16] Ma X G, Carranza E J M, Wu C L, . Ontology-Aided Annotation, Visualization, and Generalization of Geological Time-Scale Information from Online Geological Map Services. Computers & Geosciences, 2012, 40 107-119.

[17] Molina E, Alegret L, Arenillas I, . The Global Boundary Stratotype Section and Point for the Base of the Danian Stage (Paleocene, Paleogene, “Tertiary”, Cenozoic) at El Kef, Tunisia—Original Definition and Revision. Episodes, 2006, 29(4): 263-273.

[18] Penn J L, Deutsch C. Avoiding Ocean Mass Extinction from Climate Warming. Science, 2022, 376(6592): 524-526.

[19] Penn J L, Deutsch C, Payne J L, . Temperature-Dependent Hypoxia Explains Biogeography and Severity of End-Permian Marine Mass Extinction. Science, 2018, 362(6419): eaat1327

[20] Sadler P M, Cooper R A, Melchin M. High-Resolution, Early Paleozoic (Ordovician-Silurian) Time Scales. Geological Society of America Bulletin, 2009, 1215/6: 887-906.

[21] Schmitz B, Pujalte V, Molina E, . The Global Stratotype Sections and Points for the Bases of the Selandian (Middle Paleocene) and Thanetian (Upper Paleocene) Stages at Zumaia, Spain. Episodes, 2011, 34(4): 220-243.

[22] Schneer C. Geology, Time and History. Earth Sciences History, 1989, 8(2): 103-105.

[23] Shen S Z, Cao C Q, Zhang H, . High-Resolution δ¹³C_carb Chemostratigraphy from Latest Guadalupian through Earliest Triassic in South China and Iran. Earth and Planetary Science Letters, 2013, 375 156-165.

[24] Suganuma Y, Okada M, Head M J, . Formal Ratification of the Global Boundary Stratotype Section and Point (GSSP) for the Chibanian Stage and Middle Pleistocene Subseries of the Quaternary System: The Chiba Section, Japan. Episodes, 2021, 44(3): 317-347.

[25] Wang C S, Hazen R M, Cheng Q M, . The Deep-Time Digital Earth Program: Data-Driven Discovery in Geosciences. National Science Review, 2021, 8(9): nwab027

[26] Wang T T, Ramezani J, Wang C S, . High-Precision U-Pb Geochronologic Constraints on the Late Cretaceous Terrestrial Cyclostratigraphy and Geomagnetic Polarity from the Songliao Basin, Northeast China. Earth and Planetary Science Letters, 2016, 446 37-44.

[27] Weissert H, Joachimski M, Sarnthein M. Chemostratigraphy. Newsletters on Stratigraphy, 2008, 42(3): 145-179.

[28] Wang P X, Tian J, Huang E Q. Earth Systems and Evolution, 2018, Beijing: Science Press

[29] Wu H C, Zhang S H, Hinnov L A, . Time-Calibrated Milankovitch Cycles for the Late Permian. Nature Communications, 2013, 4 2452

[30] Zhang M, Qin H F, He K, . Magnetostratigraphy across the End-Permian Mass Extinction Event from the Meishan Sections, Southeastern China. Geology, 2021, 49(11): 1289-1294.

[31] Zhong Y T, Huyskens M H, Yin Q Z, . High-Precision Geochronological Constraints on the Duration of ‘Dinosaur Pompeii’ and the Yixian Formation. National Science Review, 2021, 8 6 nwab063

[32] Zhu J, Poulsen C J, Tierney J E. Simulation of Eocene Extreme Warmth and High Climate Sensitivity through Cloud Feedbacks. Science Advances, 2019, 5 9 eaax1874