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Nature Geoscience (2)

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Advanced filters: Author: Claudio Garbelli Clear advanced filters

Rapid rise in atmospheric CO₂ marked the end of the Late Palaeozoic Ice Age

A pronounced increase in atmospheric CO₂ coincided with warming at the end of the Late Palaeozoic Ice Age, according to an 80-million-year-long boron isotope CO₂ proxy record.

Hana Jurikova
Claudio Garbelli
Lucia Angiolini
ResearchOpen Access06 Jan 2025
Nature Geoscience

Volume: 18, P: 91-97
Permian–Triassic mass extinction pulses driven by major marine carbon cycle perturbations

The end-Permian mass extinction was linked with ocean acidification due to carbon degassing associated with Siberian Trap emplacement, according to boron isotopes from fossil shells and reconstruction of the carbon cycle.

Hana Jurikova
Marcus Gutjahr
Anton Eisenhauer
Research19 Oct 2020
Nature Geoscience

Volume: 13, P: 745-750

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Rapid rise in atmospheric CO2 marked the end of the Late Palaeozoic Ice Age

Permian–Triassic mass extinction pulses driven by major marine carbon cycle perturbations

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Rapid rise in atmospheric CO₂ marked the end of the Late Palaeozoic Ice Age