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Showing 1–8 of 8 results

Advanced filters: Author: Hugh C. Jenkyns Clear advanced filters

Climate–carbon-cycle interactions and spatial heterogeneity of the late Triassic Carnian pluvial episode

Understanding past warming events is essential to project the consequences of anthropogenic carbon emissions. Here, carbon and hydrological cycle changes of the Carnian Pluvial Episode are revealed, offering insights into Earth System functioning.

Xiangdong Zhao
Naihua Xue
Bo Wang
ResearchOpen Access30 Jun 2025
Nature Communications

Volume: 16, P: 1-11
Lithium isotope evidence for enhanced weathering during Oceanic Anoxic Event 2

Ocean Anoxic Event 2 was marked by rapid global warming and loss of O₂ from the ocean. Lithium isotope data suggest that the warming was accompanied by enhanced silicate weathering, which stimulated marine productivity and helped stabilize atmospheric CO₂ levels.

Philip A. E. Pogge von Strandmann
Hugh C. Jenkyns
Richard G. Woodfine
Research07 Jul 2013
Nature Geoscience

Volume: 6, P: 668-672
The paradox of drowned carbonate platforms and the origin of Cretaceous Pacific guyots

Paul A. Wilson
Hugh C. Jenkyns
Roger L. Larson
Research30 Apr 1998
Nature

Volume: 392, P: 889-894
Massive dissociation of gas hydrate during a Jurassic oceanic anoxic event

Stephen P. Hesselbo
Darren R. Gröcke
Owen R. Green
Research27 Jul 2000
Nature

Volume: 406, P: 392-395
High temperatures in the Late Cretaceous Arctic Ocean

Hugh C. Jenkyns
Astrid Forster
Jaap S. Sinninghe Damsté
Research16 Dec 2004
Nature

Volume: 432, P: 888-892
Early Jurassic large igneous province carbon emissions constrained by sedimentary mercury

Sedimentary mercury measurements suggest carbon emissions from Early Jurassic large igneous province activity were lower than estimates from carbon-cycle models, implying feedbacks that are unaccounted for.

Isabel M. Fendley
Joost Frieling
Hugh C. Jenkyns
ResearchOpen Access26 Feb 2024
Nature Geoscience

Volume: 17, P: 241-248
Carbon sequestration in an expanded lake system during the Toarcian oceanic anoxic event

The Toarcian anoxic event was linked to a massive release of carbon to the atmosphere. Geochemical data suggest that organic carbon burial in large lacustrine systems was key to the recovery of the carbon cycle.

Weimu Xu
Micha Ruhl
Erdem F. Idiz
Research16 Jan 2017
Nature Geoscience

Volume: 10, P: 129-134
New age constraints on the Lower Jurassic Pliensbachian–Toarcian Boundary at Chacay Melehue (Neuquén Basin, Argentina)

Aisha H. Al-Suwaidi
Micha Ruhl
Stephen P. Hesselbo
ResearchOpen Access23 Mar 2022
Scientific Reports

Volume: 12, P: 1-10