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Redox conditions across the G–L boundary in South China: Evidence from pyrite morphology and sulfur isotopic compositions

Chemical geology, 2016-11, Vol.440, p.1-14

2016

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Biological extinction and photic-zone anoxia across the Triassic–Jurassic transition: insights from the Qiangtang Basin, eastern Tethys

Journal of the Geological Society, 2023-09, Vol.180 (5)

2023

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Total organic carbon, organic phosphorus, and biogenic barium fluxes as proxies for paleomarine productivity

Earth-science reviews, 2015-10, Vol.149, p.23-52

2015

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Evolution from an anoxic to oxic deep ocean during the Ediacaran–Cambrian transition and implications for bioradiation

Chemical geology, 2012-05, Vol.306-307, p.129-138

2012

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Different controls on the Hg spikes linked the two pulses of the Late Ordovician mass extinction in South China

Scientific reports, 2022-03, Vol.12 (1), p.5195-5195, Article 5195

2022

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Carbon isotope perturbations and faunal changeovers during the Guadalupian mass extinction in the middle Yangtze Platform, South China

Geological magazine, 2018-11, Vol.155 (8), p.1667-1683

2018

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Euxinia caused the Late Ordovician extinction: Evidence from pyrite morphology and pyritic sulfur isotopic composition in the Yangtze area, South China

Palaeogeography, palaeoclimatology, palaeoecology, 2018-12, Vol.511, p.1-11

2018

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Organic accumulation in the lower Chihsia Formation (Middle Permian) of South China: Constraints from pyrite morphology and multiple geochemical proxies

Palaeogeography, palaeoclimatology, palaeoecology, 2012-10, Vol.353-355, p.73-86

2012

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Marine productivity changes during the end-Permian crisis and Early Triassic recovery

Earth-science reviews, 2015-10, Vol.149, p.136-162

2015

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Sulfur isotopic evidence for global marine anoxia and low seawater sulfate concentration during the Late Triassic

Journal of Asian earth sciences, 2023-08, Vol.251, p.105659, Article 105659

2023

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Millennial-scale ocean redox and δ13C changes across the Permian–Triassic transition at Meishan and implications for the biocrisis

International journal of earth sciences : Geologische Rundschau, 2020, Vol.109 (5), p.1753-1766

2020

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Orbitally-paced climate change during the Carnian Pluvial Episode

Earth and planetary science letters, 2024-01, Vol.626, p.118546, Article 118546

2024

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Guadalupian (Middle Permian) ocean redox evolution in South China and its implications for mass extinction

Chemical geology, 2019-12, Vol.530, p.119318, Article 119318

2019

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A Toarcian Ocean Anoxic Event record from an open-ocean setting in the eastern Tethys: Implications for global climatic change and regional environmental perturbation

Science China. Earth sciences, 2021-11, Vol.64 (11), p.1860-1872

2021

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Multiple carbon isotope excursions during the Carnian (Late Triassic) pluvial event: implications for global and regional perturbation

Journal of the Geological Society, 2023-11, Vol.180 (6)

2023

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Sedimentary environments of middle Eocene sediments in the northern Qiangtang Basin, northern Tibetan Plateau: Implications for paleoclimate and paleoelevation

Journal of Asian earth sciences, 2023-04, Vol.245, p.105551, Article 105551

2023

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Detrital zircons of the Devonian-Permian sandstones in the Qiangtang terrane, Tibet: Implication for Qiangtang rifting from Gondwana and uplift history of the Central Uplift

Journal of Asian earth sciences, 2022-11, Vol.239, p.105392, Article 105392

2022

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Episodic euxinia in the Changhsingian (late Permian) of South China: Evidence from framboidal pyrite and geochemical data

Sedimentary geology, 2015-04, Vol.319, p.78-97

2015

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Diagenetic barite deposits in the Yurtus Formation in Tarim Basin, NW China: Implications for barium and sulfur cycling in the earliest Cambrian

Precambrian research, 2015-07, Vol.263, p.79-87

2015

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Organic matter accumulation mechanism under global/regional warming: Insight from the Late Barremian calcareous shales in the Qiangtang Basin (Tibet)

Journal of Asian earth sciences, 2023-01, Vol.241, p.105456, Article 105456

2023

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Two episodes of evolution of trace fossils during the Early Triassic in the Guiyang area, Guizhou Province, South China

Palaeogeography, palaeoclimatology, palaeoecology, 2015-05, Vol.426, p.275-284

2015

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The Toarcian Oceanic Anoxic Event in a shelf environment (Eastern Tethys): Implications for weathering and redox conditions

Sedimentary geology, 2023-09, Vol.455, p.106476, Article 106476

2023

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LOWER TRIASSIC LIMULID TRACKWAYS (KOUPHICHNIUM) FROM THE SOUTHWESTERN MARGIN OF THE YANGTZE CARBONATE PLATFORM: PALEOENVIRONMENTAL AND PALEOECOLOGICAL IMPLICATIONS

Palaios, 2019-04, Vol.34 (4), p.229-243

2019

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Global oceanic anoxia linked with the Capitanian (Middle Permian) marine mass extinction

Earth and planetary science letters, 2023-05, Vol.610, p.118128, Article 118128

2023

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Provenance of Middle Jurassic clastic rocks from the Bogda area of Eastern Tianshan and its implications

International geology review, 2020-07, Vol.62 (10), p.1319-1342

2020

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Redox conditions across the G–L boundary in South China: Evidence from pyrite morphology and sulfur isotopic compositions

Biological extinction and photic-zone anoxia across the Triassic–Jurassic transition: insights from the Qiangtang Basin, eastern Tethys

Total organic carbon, organic phosphorus, and biogenic barium fluxes as proxies for paleomarine productivity

Evolution from an anoxic to oxic deep ocean during the Ediacaran–Cambrian transition and implications for bioradiation

Different controls on the Hg spikes linked the two pulses of the Late Ordovician mass extinction in South China

Carbon isotope perturbations and faunal changeovers during the Guadalupian mass extinction in the middle Yangtze Platform, South China

Euxinia caused the Late Ordovician extinction: Evidence from pyrite morphology and pyritic sulfur isotopic composition in the Yangtze area, South China

Organic accumulation in the lower Chihsia Formation (Middle Permian) of South China: Constraints from pyrite morphology and multiple geochemical proxies

Marine productivity changes during the end-Permian crisis and Early Triassic recovery

Sulfur isotopic evidence for global marine anoxia and low seawater sulfate concentration during the Late Triassic

Millennial-scale ocean redox and δ13C changes across the Permian–Triassic transition at Meishan and implications for the biocrisis

Orbitally-paced climate change during the Carnian Pluvial Episode

Guadalupian (Middle Permian) ocean redox evolution in South China and its implications for mass extinction

A Toarcian Ocean Anoxic Event record from an open-ocean setting in the eastern Tethys: Implications for global climatic change and regional environmental perturbation

Multiple carbon isotope excursions during the Carnian (Late Triassic) pluvial event: implications for global and regional perturbation

Sedimentary environments of middle Eocene sediments in the northern Qiangtang Basin, northern Tibetan Plateau: Implications for paleoclimate and paleoelevation

Detrital zircons of the Devonian-Permian sandstones in the Qiangtang terrane, Tibet: Implication for Qiangtang rifting from Gondwana and uplift history of the Central Uplift

Episodic euxinia in the Changhsingian (late Permian) of South China: Evidence from framboidal pyrite and geochemical data

Diagenetic barite deposits in the Yurtus Formation in Tarim Basin, NW China: Implications for barium and sulfur cycling in the earliest Cambrian

Organic matter accumulation mechanism under global/regional warming: Insight from the Late Barremian calcareous shales in the Qiangtang Basin (Tibet)

Two episodes of evolution of trace fossils during the Early Triassic in the Guiyang area, Guizhou Province, South China

The Toarcian Oceanic Anoxic Event in a shelf environment (Eastern Tethys): Implications for weathering and redox conditions

LOWER TRIASSIC LIMULID TRACKWAYS (KOUPHICHNIUM) FROM THE SOUTHWESTERN MARGIN OF THE YANGTZE CARBONATE PLATFORM: PALEOENVIRONMENTAL AND PALEOECOLOGICAL IMPLICATIONS

Global oceanic anoxia linked with the Capitanian (Middle Permian) marine mass extinction

Provenance of Middle Jurassic clastic rocks from the Bogda area of Eastern Tianshan and its implications

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