G.R. Shi

ORCID: 0000-0002-5126-4036
Publications
Citations
Views
---
Saved
---
About
Contact & Profiles
Research Areas
  • Paleontology and Stratigraphy of Fossils
  • Geological and Geophysical Studies
  • Paleontology and Evolutionary Biology
  • Geology and Paleoclimatology Research
  • Marine Biology and Ecology Research
  • Geological formations and processes
  • Geological and Geochemical Analysis
  • Geological Studies and Exploration
  • Evolution and Paleontology Studies
  • Geochemistry and Elemental Analysis
  • Hydrocarbon exploration and reservoir analysis
  • Marine and coastal plant biology
  • Marine and environmental studies
  • Plant Diversity and Evolution
  • Geochemistry and Geologic Mapping
  • Law in Society and Culture
  • Discourse Analysis in Language Studies
  • Interpreting and Communication in Healthcare
  • Isotope Analysis in Ecology
  • Global Health Care Issues
  • Jury Decision Making Processes
  • EFL/ESL Teaching and Learning
  • Ichthyology and Marine Biology
  • Methane Hydrates and Related Phenomena
  • Healthcare Systems and Reforms

University of Wollongong
2019-2025

Planetary Science Institute
2023

University of California, Los Angeles
2023

Nanjing Normal University
2014-2022

Peking University
2003-2020

Russian Academy of Sciences
2020

National Computer Network Emergency Response Technical Team/Coordination Center of Chinar
2020

Deakin University
2010-2019

China University of Geosciences
2004-2015

The University of Western Australia
2004-2015

10.1016/0031-0182(93)90084-v article EN Palaeogeography Palaeoclimatology Palaeoecology 1993-11-01

Research Article| September 01, 2001 End-Permian catastrophe by a bolide impact: Evidence of gigantic release sulfur from the mantle Kunio Kaiho; Kaiho 1Institute Geology and Paleontology, Tohoku University, Sendai 980-8578, Japan Search for other works this author on: GSW Google Scholar Yoshimichi Kajiwara; Kajiwara 2Institute Geoscience, University Tsukuba, Ibaraki 305, Takanori Nakano; Nakano Yasunori Miura; Miura 3Department Earth Sciences, Faculty Science, Yamaguchi 753-8512, Hodaka...

10.1130/0091-7613(2001)029<0815:epcbab>2.0.co;2 article EN Geology 2001-01-01

Spatial and temporal variations in biological diversity are critical understanding the role of biogeographical regulation (if any) on mass extinctions. An analysis based a latest database stratigraphic ranges 89 Permian brachiopod families, 422 genera, 2059 species within Boreal, Paleoequatorial, Gondwanan Realms Asian–western Pacific region suggests two discrete extinctions, each possibly with different causes. Using species/family rarefaction analysis, we constructed curves for late...

10.1666/0094-8373(2002)028<0449:pepopb>2.0.co;2 article EN Paleobiology 2002-01-01

10.1016/j.palaeo.2010.07.021 article EN Palaeogeography Palaeoclimatology Palaeoecology 2010-09-24

Abstract Analysis of Permian–Triassic brachiopod diversity and body size changes from different water depths spanning the continental shelf to basinal facies in South China provides insights into process environmental deterioration. Comparison temporal between deepwater shallow‐water demonstrates that brachiopods disappeared earlier than brachiopods. This indicates high stress commenced first settings later extended shallow waters. is attributed major volcanic eruptions, which led formation...

10.1111/gbi.12119 article EN Geobiology 2014-11-21

Atmospheric CO2 is thought to play a fundamental role in Earth&amp;#8217;s climate regulation. Yet, for much of deep geological past, atmospheric has been poorly constrained, hindering our understanding transitions between cool and warm climates. Beginning ~370 million years ago the Late Devonian ending ~260 Permian, Palaeozoic Ice Age was last major glaciation preceding current Cenozoic possibly most intense witnessed by complex lifeforms. From onset main phase mid-Mississippian ~330 ago,...

10.5194/egusphere-egu25-16102 preprint EN 2025-03-15

Abstract. Knowledge of the past location tectonic plates is essential to understanding evolution climate, ocean systems, and mantle flow. Tectonic reconstructions become increasingly uncertain back in geological time. Paleomagnetic data constrain latitude continental blocks, however, their longitude unconstrained. For example, South China Block during Early Permian unknown. Paleobiogeographic data, which have long been used reconstructions, make it possible evaluate faunal similarity between...

10.5194/egusphere-2025-1018 preprint EN cc-by 2025-04-03
Coming Soon ...