Yue Li

University of Chinese Academy of Sciences

Author Statistics

Papers

Citation

H-Index

i-10 index

Research Trends

Author Order

Document Type

Co-Authors

Xiangdong Wang

Nanjing University

Le Yao

Nanjing Institute of Geology and Paleontology

Shenyang Yu

Nanjing Institute of Geology and Paleontology

Wei Lin

Chinese Academy of Sciences

Juwan Jeon

University of Chinese Academy of Sciences

Stephen Kershaw

Brunel University of London

Markus Aretz

Géosciences Environnement Toulouse

Yuandong Zhang

Nanjing Institute of Geology and Paleontology

Wenkun Qie

Nanjing Institute of Geology and Paleontology

Ursula Toom

Tallinn University of Technology

Cooperative Institutions

Nanjing Institute of Geology and Paleontology

Chinese Academy of Sciences

University of Chinese Academy of Sciences

Nanjing University

China University of Geosciences

State Key Laboratory of Palaeobiology and Stratigraphy

Cambrian Innovation (United States)

Brunel University of London

Natural History Museum

University of Liège

Author Statistics

Papers

Citation

H-Index

i-10 index

Research Field

Stromatoporoids of the upper Hirnantian (Upper Ordovician) Shiqian Formation of South China: implications for environmental interpretation and the Ordovician–Silurian stromatoporoid transition

Journal of Systematic Palaeontology (2024)

Juwan Jeon Stephen Kershaw Yue Li Zhongyang Chen Ursula Toom

Baltica

10.1080/14772019.2024.2351930

Cite

Citations (1)

Middle Viséan (Mississippian) coral biostrome in central Guizhou, southwestern China and its palaeoclimatological implications

Palaeogeography Palaeoclimatology Palaeoecology (2015)

Le Yao Xiangdong Wang Wei Lin Yue Li Steve Kershaw

Bioerosion

10.1016/j.palaeo.2015.08.031

Cite

Citations (20)

Gigantoproductid brachiopod storm shell beds in the Mississippian of South China: implications for their palaeoenvironmental and palaeogeographical significances

Geologica Belgica (2016)

Le Yao Markus Aretz Yue Li Xiangdong Wang

1. Introduction Storm beds are distinct facies criteria on shelves and ramps, which are generated by storm winds, such as cyclones and hurricanes in tropical latitudes and blizzards in middle and high latitudes (Tucker & Wright, 1990; Flügel, 2004). Ager (1973) defined storm beds as tempestites that are commonly characterized by sharp and erosional base, internal structures including accumulations of shells, graded and flat bedding and parallel and cross lamination, and ripple bedding and burrowing presented at the top part (Aigner, 1985; Flügel, 2004; Dattilo et al., 2012). Tempestites are abundant and widely distributed in carbonate environments during the Phanerozoic (e.g. Einsele & Seilacher, 1982; Flügel, 2004). The sedimentary patterns and biotic distributions of tempestites could provide important information in aspects of their depositional process, palaeoenvironment, palaeogeographical location and even stratigraphic comparison (Johnson, 1989; Lehman & Pope, 1989; Flügel, 2004; Jin et al., 2013). Storm shell beds, which are one common type of tempestites and featured by accumulation of shells, were documented during the icehouse periods of the late Ordovician (Lehman & Pope, 1989; Davis, 1999; Jin et al., 2013), early Silurian (Johnson, 1989; Li & Rong, 2007; Jin, 2008) and early Carboniferous (Jeffery & Aigner, 1982; Butts, 2005) and during greenhouse climate, as in the middle Ordovician (McFarland et al., 1999), late Permian (Simões & Kowalewski, 1998), early Tria

Bedding

Ooid

Paleoecology

10.20341/gb.2015.021

Cite

Citations (15)