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Issue: Vol. 1 No. 3: September 2024
Type: Editorial
Published: 2024-09-26
DOI: 10.11646/mesozoic.1.3.1
Page range: 210-220
Abstract views: 440
PDF downloaded: 234

In memory of Dr Juan Li, a young geologist (1987–2023)

Key Laboratory of Palaeobiology and Petroleum Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008, China
State Key Laboratory of Mineral Deposits Research, School of Earth Sciences and Engineering, Nanjing University, Nanjing 210023, China
State Key Laboratory of Mineral Deposits Research, School of Earth Sciences and Engineering, Nanjing University, Nanjing 210023, China
Department of Earth and Environmental Sciences, Università di Milano-Bicocca, Milano 20126, Italy
College of Oceanography, Hohai University, Nanjing 210024, China
Institute of Earth Sciences, China University of Geosciences, Beijing 100083, China
State Key Laboratory for Biogeology and Environmental Geology and Hubei Key Laboratory of Critical Zone Evolution, School of Earth Sciences, China University of Geosciences (Wuhan), Wuhan 430074, China
State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China
Key Laboratory of Mineral Resources, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China
College of Oceanography, Hohai University, Nanjing 210024, China
School of Resources and Environmental Engineering, Hefei University of Technology, Hefei 230009, China
State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation and Key Laboratory of Deep-time Geography and Environment Reconstruction and Applications, MNR, Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu 610059, China
School of Marine Science and Engineering, Nanjing Normal University, Nanjing 210023, Jiangsu, China
College of Oceanography, Hohai University, Nanjing 210024, China
School of Earth Sciences and Engineering, Hohai University, Nanjing 211100, China
Key Laboratory of Palaeobiology and Petroleum Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008, China
Key Laboratory of Palaeobiology and Petroleum Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008, China
State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation and Key Laboratory of Deep-time Geography and Environment Reconstruction and Applications, MNR, Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu 610059, China
State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation and Key Laboratory of Deep-time Geography and Environment Reconstruction and Applications, MNR, Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu 610059, China
College of Tourism, Henan Normal University, Xinxiang 453007, China
State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation and Key Laboratory of Deep-time Geography and Environment Reconstruction and Applications, MNR, Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu 610059, China
School of Geography and Environmental Engineering, Gannan Normal University, Ganzhou 341000, China
Key Laboratory of Palaeobiology and Petroleum Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008, China
State Key Laboratory of Isotope Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences (CAS), Guangzhou 510640, China
State Key Laboratory of Nuclear Resources and Environment, East China University of Technology, Nanchang 330013, China
State Key Laboratory of Mineral Deposits Research, School of Earth Sciences and Engineering, Nanjing University, Nanjing 210023, China
Key Laboratory of Palaeobiology and Petroleum Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008, China
In memory of Dr Juan Li, a young geologist (1987–2023)

Abstract

This special issue of Mesozoic is dedicated to the memory of a great specialist in carbonate sedimentology, Dr Juan Li, who passed away on July 19th, 2023. Juan Li sadly left us while logging the Paleocene-Eocene thermal maximum (PETM) interval in the Tibetan Himalaya. This special issue has collected contributions to Mesozoic–Cenozoic geological studies from the Qinghai-Tibet Plateau from colleagues, friends, and fellow scientists to express our remembrance and regret.

References

  1. Li, J., Hu, X., Garzanti, E., An, W. & Wang, J. (2015) Paleogene carbonate microfacies and sandstone provenance (Gamba area, South Tibet): Stratigraphic response to initial India–Asia continental collision. Journal of Asian Earth Sciences, 104, 39–54. https://doi.org/10.1016/j.jseaes.2015.02.007
  2. Li, J., Hu, X., Garzanti, E., Banerjee, S. & BouDagher-Fadel, M. (2020a) Late Cretaceous topographic doming caused by initial upwelling of Deccan magmas: Stratigraphic and sedimentological evidence. Geological Society of America Bulletin, 132, 835–849. https://doi.org/10.1130/B35222.1
  3. Li, J., Hu, X., Garzanti, E. & BouDagher-Fadel, M. (2017) Shallow-water carbonate responses to the Paleocene–Eocene thermal maximum in the Tethyan Himalaya (southern Tibet): Tectonic and climatic implications. Palaeogeography, Palaeoclimatology, Palaeoecology, 466, 153–165. https://doi.org/10.1016/j.palaeo.2016.08.020
  4. Li, J., Hu, X., Garzanti, E. & BouDagher-Fadel, M. (2021) Climate-driven hydrological change and carbonate platform demise induced by the Paleocene–Eocene Thermal Maximum (southern Pyrenees). Palaeogeography, Palaeoclimatology, Palaeoecology, 567, 110250. https://doi.org/10.1016/j.palaeo.2020.110250
  5. Li, J., Hu, X., Garzanti, E. & BouDagher-Fadel, M. (2022) Spatial heterogeneity in carbonate-platform environments and carbon isotope values across the Paleocene–Eocene thermal maximum (Tethys Himalaya, South Tibet). Global and Planetary Change, 214, 103853. https://doi.org/10.1016/j.gloplacha.2022.103853
  6. Li, J., Hu, X., Zachos, J. C., Garzanti, E. & BouDagher-Fadel, M. (2020b) Sea level, biotic and carbon-isotope response to the Paleocene–Eocene thermal maximum in Tibetan Himalayan platform carbonates. Global and Planetary Change, 194, 103316. https://doi.org/10.1016/j.gloplacha.2020.103316
  7. Li, J., Hu, X., Zhao, K., Cai, Y. & Sun, T. (2016) Paleoceanographic evolution and chronostratigraphy of the Aptian Oceanic Anoxic Event 1a (OAE1a) to oceanic red bed 1 (ORB1) in the Gorgo a Cerbara section (central Italy). Cretaceous Research, 66, 115–128. https://doi.org/10.1016/j.cretres.2016.06.004