A5089394868- Paleontology and Stratigraphy of Fossils
- Geological and Geophysical Studies
- Geology and Paleoclimatology Research
- Paleontology and Evolutionary Biology
- Geological and Geochemical Analysis
- Geochemistry and Elemental Analysis
- Hydrocarbon exploration and reservoir analysis
- Evolution and Paleontology Studies
- Isotope Analysis in Ecology
- Coral and Marine Ecosystems Studies
- Geochemistry and Geologic Mapping
- Geological formations and processes
- Marine Biology and Ecology Research
- Methane Hydrates and Related Phenomena
- Marine and coastal plant biology
- Plant Diversity and Evolution
- Cephalopods and Marine Biology
- Mercury impact and mitigation studies
- Marine Sponges and Natural Products
- Morphological variations and asymmetry
- Geotechnical and Geomechanical Engineering
- Subterranean biodiversity and taxonomy
- Drilling and Well Engineering
- earthquake and tectonic studies
- Spacecraft and Cryogenic Technologies
Nanjing Institute of Geology and Paleontology
2015-2024
Chinese Academy of Sciences
2015-2024
University of Chinese Academy of Sciences
2020-2024
Nanjing University of Chinese Medicine
2024
State Key Laboratory of Palaeobiology and Stratigraphy
2022
Cambrian Innovation (United States)
2022
China University of Geosciences
2010-2014
Abstract The Hangenberg Crisis coincided with a large decline of biodiversity and widespread anoxia in the end‐Devonian ocean. Previous research attributed marine to spread deeply‐rooted plants and/or increased volcanism on continents, but crucial links have not been thoroughly explored. Herein, we propose enhanced weathering as key trigger, evidenced by negative shift (∼8‰) lithium isotopes coupled response carbon carbonates South China. Our findings imply that rapid crustal rocks nutrient...
Abstract The sedimentary successions and four fossil groups, including rugose corals, brachiopods, fusulinaceans conodonts, from the Carboniferous Lower Permian of South China have been studied in order to reveal characteristics evolutionary pattern main biological groups East Tethyan region during Late Palaeozoic Ice Age. lithology is diverse, ranging basinal shelf carbonate rocks coal measures continental clastics, while Upper are composed mostly shallow-marine carbonates. From uppermost...
Carboniferous conodonts from the candidate GSSPs of four stages Serpukhovian, Moscovian, Kasimovian and Gzhelian in Naqing adjacent sections South China have been intensely studied recent decades. The conodont zonation is updated based on material China; 39 zones including 11 Tournaisian zones, 4 Visean 3 Serpukhovian 6 Bashkirian 5 Moscovian are separated discussed detail. Species genera Siphonodella, Polygnathus, Protognathodus Gnathodus dominate for Early Mississippian (Tournaisian)...
Abstract The Borkewehr section near Balve at the southeastern end of Remscheid-Altena Anticline is currently best and most complete Devonian/Carboniferous Boundary (DCB) succession Rhenish Massif, Germany. Based on a multidisciplinary approach, focusing refined conodont ammonoid biostratigraphy, microfacies analyses, sequence stratigraphy, carbon isotopes (C org C carb ), trace element geochemistry, including REE data, cyclostratigraphy, proposed as candidate for new basal Carboniferous...
Abstract To improve regional and intercontinental correlation of the uppermost Devonian–lowermost Carboniferous, we examined conodont faunas carbon isotopic records Tangbagou Formation in Qilinzhai section, southern Guizhou, South China. The is a succession mixed carbonate–siliciclastic rocks that accumulated on shallow‐water platform under normal marine conditions. Seven zones for biofacies China, Cl . gilwernensis–Cl unicornis Zone, Po spicatus Si homosimplex sinensis eurylobata Ps...