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 …

[HTML][HTML] Hydrological and associated biogeochemical consequences of rapid global warming during the Paleocene-Eocene Thermal Maximum

MJ Carmichael, GN Inglis, MPS Badger… - Global and Planetary …, 2017 - Elsevier
Abstract The Paleocene-Eocene Thermal Maximum (PETM) hyperthermal,~ 56 million years
ago (Ma), is the most dramatic example of abrupt Cenozoic global warming. During the …

Carbon-isotope record of the Early Jurassic (Toarcian) Oceanic Anoxic Event from fossil wood and marine carbonate (Lusitanian Basin, Portugal)

SP Hesselbo, HC Jenkyns, LV Duarte… - Earth and Planetary …, 2007 - Elsevier
The Toarcian Oceanic Anoxic Event (OAE) in the Early Jurassic (∼ 183 Ma ago) was
characterized by widespread near-synchronous deposition of organic-rich shales in marine …

A revised correlation of Tertiary rocks in the British Isles and adjacent areas of NW Europe

C King - 2016 - books.google.com
This Special Report comprehensively describes the stratigraphy and correlation of the
Tertiary (Paleogene–Neogene) rocks of NW Europe and the adjacent Atlantic Ocean and is …

Hyperpycnal flow variability and slope organization on an Eocene shelf margin, Central Basin, Spitsbergen

AL Petter, RJ Steel - AAPG bulletin, 2006 - archives.datapages.com
Identification of bypass at the shelf margin is critical to deep-water exploration. We examine
the shelf margin of an early Eocene fourth-order sequence with an attached basin-floor fan …

The Late Palaeocene–Early Eocene and Toarcian (Early Jurassic) carbon isotope excursions: a comparison of their time scales, associated environmental changes …

AS Cohen, AL Coe, DB Kemp - Journal of the Geological Society, 2007 - lyellcollection.org
Although the Earth's environment is constantly changing, there have been a few unusual
episodes over the last c. 200 Ma when change was extreme in terms of its rapidity, severity …

Responses of calcareous nannofossil assemblages, mineralogy and geochemistry to the environmental perturbations across the Paleocene/Eocene boundary in the …

C Agnini, E Fornaciari, D Rio, F Tateo, J Backman… - Marine …, 2007 - Elsevier
Calcareous nannofossil, mineralogical and geochemical data are presented from the
expanded Paleocene–Lower Eocene Forada section in the Venetian Pre-Alps. The short …

Mode and tempo of the Paleocene-Eocene thermal maximum in an expanded section from the Venetian pre-Alps

L Giusberti, D Rio, C Agnini… - Geological …, 2007 - pubs.geoscienceworld.org
The central part of the Piave River valley in the Venetian pre-Alps of NE Italy exposes an
expanded and continuous marine sediment succession that encompasses the Paleocene …

Global changes in terrestrial vegetation and continental climate during the Paleocene‐Eocene Thermal Maximum

VA Korasidis, SL Wing, CA Shields… - Paleoceanography and …, 2022 - Wiley Online Library
Most studies of the response of terrestrial vegetation to climate change during the
Paleocene‐Eocene Thermal Maximum (PETM) have focused on individual sites and …

Extinction and recovery of benthic foraminifera across the Paleocene–Eocene Thermal Maximum at the Alamedilla section (Southern Spain)

L Alegret, S Ortiz, E Molina - Palaeogeography, Palaeoclimatology …, 2009 - Elsevier
A complete succession of lower bathyal–upper abyssal sediments was deposited across the
Paleocene–Eocene Thermal Maximum (PETM) at Alamedilla (Betic Cordillera, Southern …