[HTML][HTML] Epochs, events and episodes: Marking the geological impact of humans

CN Waters, M Williams, J Zalasiewicz, SD Turner… - Earth-Science …, 2022 - Elsevier
Event stratigraphy is used to help characterise the Anthropocene as a chronostratigraphic
concept, based on analogous deep-time events, for which we provide a novel …

The Paleocene-Eocene Thermal Maximum: A perturbation of carbon cycle, climate, and biosphere with implications for the future

FA McInerney, SL Wing - Annual Review of Earth and Planetary …, 2011 - annualreviews.org
During the Paleocene-Eocene Thermal Maximum (PETM),∼ 56 Mya, thousands of
petagrams of carbon were released into the ocean-atmosphere system with attendant …

Very large release of mostly volcanic carbon during the Palaeocene–Eocene Thermal Maximum

M Gutjahr, A Ridgwell, PF Sexton, E Anagnostou… - Nature, 2017 - nature.com
Abstract The Palaeocene–Eocene Thermal Maximum,(PETM) was a global warming event
that occurred about 56 million years ago, and is commonly thought to have been driven …

Spatial patterns of climate change across the Paleocene–Eocene Thermal Maximum

JE Tierney, J Zhu, M Li, A Ridgwell… - Proceedings of the …, 2022 - National Acad Sciences
The Paleocene–Eocene Thermal Maximum (PETM; 56 Ma) is one of our best geological
analogs for understanding climate dynamics in a “greenhouse” world. However, proxy data …

The DeepMIP contribution to PMIP4: Methodologies for selection, compilation and analysis of latest Paleocene and early Eocene climate proxy data, incorporating …

CJ Hollis, T Dunkley Jones… - Geoscientific Model …, 2019 - gmd.copernicus.org
The early Eocene (56 to 48 million years ago) is inferred to have been the most recent time
that Earth's atmospheric CO2 concentrations exceeded 1000 ppm. Global mean …

Solar System chaos and the Paleocene–Eocene boundary age constrained by geology and astronomy

RE Zeebe, LJ Lourens - Science, 2019 - science.org
Astronomical calculations reveal the Solar System's dynamical evolution, including its
chaoticity, and represent the backbone of cyclostratigraphy and astrochronology. An …

Twenty years of XRF core scanning marine sediments: what do geochemical proxies tell us?

RG Rothwell, I Croudace - Micro-XRF Studies of Sediment Cores …, 2015 - Springer
XRF core scanners, with their rapid and non-destructive analytical capability, have now
been used for two decades in the analysis of marine sediments. Initially they were used to …

Silicate weathering as a feedback and forcing in Earth's climate and carbon cycle

DE Penman, JKC Rugenstein, DE Ibarra… - Earth-Science …, 2020 - Elsevier
Current understanding of the long-term carbon cycle posits that Earth's climate is stabilized
by a negative feedback involving CO 2 consumption by chemical weathering of silicate …

[HTML][HTML] Climate model and proxy data constraints on ocean warming across the Paleocene–Eocene Thermal Maximum

TD Jones, DJ Lunt, DN Schmidt, A Ridgwell… - Earth-Science …, 2013 - Elsevier
Constraining the greenhouse gas forcing, climatic warming and estimates of climate
sensitivity across ancient large transient warming events is a major challenge to the …

Carbon dioxide forcing alone insufficient to explain Palaeocene–Eocene Thermal Maximum warming

RE Zeebe, JC Zachos, GR Dickens - Nature Geoscience, 2009 - nature.com
Abstract The Palaeocene–Eocene Thermal Maximum (about 55 Myr ago) represents a
possible analogue for the future and thus may provide insight into climate system sensitivity …