A ∼0.5 Myr perturbation of carbon and mercury cycles during the Middle Triassic biotic radiation

The Anisian Stage (Middle Triassic) marks a pivotal interval for biotic recovery following the Permian-Triassic mass extinction, yet its environmental drivers remain poorly understood. This study presents carbon isotopes, mercury (Hg) concentrations, and Hg isotope data from Anisian (mainly Pelsonian substage) marine and terrestrial sections across the Tethys. Our results reveal a widespread Hg enrichment event that is synchronous with the Pelsonian negative carbon isotope excursion (PENCIE). Hg isotopic compositions support an origin from enhanced regional volcanism, coupled with contemporaneous terrestrial input. New high-precision zircon U-Pb ages (244.200 ± 0.037 Ma and 243.451 ± 0.049 Ma), integrated with chemostratigraphic and biostratigraphic data, constrain the duration of the PENCIE to ∼0.5 Myr. This interval coincided with major biodiversification, revealing that recovery occurred alongside environmental perturbations rather than in stable conditions as traditionally thought. These global disturbances in carbon and mercury cycles, linked to volcanism and terrestrial input, likely accelerated Middle Triassic biotic recovery.

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Publication Details

Journal
Science Advances
Published
2026-06-17
DOI
https://doi.org/10.1126/sciadv.aee2291
Primary Topic
Paleontology and Stratigraphy of Fossils
Type
article
Field-Weighted Citation Impact
0.00

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article

A ∼0.5 Myr perturbation of carbon and mercury cycles during the Middle Triassic biotic radiation

Haijun Song, Daoliang Chu, Piero Gianolla, Michael J. Benton et al.
Science Advances
Paleontology and Stratigraphy of Fossils
article

A ∼0.5 Myr perturbation of carbon and mercury cycles during the Middle Triassic biotic radiation

Haijun Song, Daoliang Chu, Piero Gianolla, Michael J. Benton, Aya Schneider‐Mor, Marcello Caggiati, Guido Roghi, Stephen E. Grasby, Jinnan Tong, Yiran Cao, Runsheng Yin, Dorit Korngreen, Jacopo Dal Corso, Xu Dai, Greta Alverà, Maria Ovtcharova
article en

Abstract

The Anisian Stage (Middle Triassic) marks a pivotal interval for biotic recovery following the Permian-Triassic mass extinction, yet its environmental drivers remain poorly understood. This study presents carbon isotopes, mercury (Hg) concentrations, and Hg isotope data from Anisian (mainly Pelsonian substage) marine and terrestrial sections across the Tethys. Our results reveal a widespread Hg enrichment event that is synchronous with the Pelsonian negative carbon isotope excursion (PENCIE). Hg isotopic compositions support an origin from enhanced regional volcanism, coupled with contemporaneous terrestrial input. New high-precision zircon U-Pb ages (244.200 ± 0.037 Ma and 243.451 ± 0.049 Ma), integrated with chemostratigraphic and biostratigraphic data, constrain the duration of the PENCIE to ∼0.5 Myr. This interval coincided with major biodiversification, revealing that recovery occurred alongside environmental perturbations rather than in stable conditions as traditionally thought. These global disturbances in carbon and mercury cycles, linked to volcanism and terrestrial input, likely accelerated Middle Triassic biotic recovery.

Science AdvancesVol. 12(25)
University of Geneva (CH), Natural Resources Canada (CA), Geological Survey of Canada (CA), University of Padua (IT), Friedrich-Alexander-Universität Erlangen-Nürnberg (DE), University of Ferrara (IT), Chinese Academy of Geological Sciences (CN), China University of Geosciences (CN), University of Bristol (GB), Institute of Geosciences and Earth Resources (IT), Geological Survey of Israel (IL)
Alexander von Humboldt-Stiftung, National Natural Science Foundation of China, China Scholarship Council, China University of Geosciences
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Paleontology and Stratigraphy of Fossils
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