Provincialism associated with the Paleocene/Eocene thermal maximum: temporal constraint

A Kahn, MP Aubry - Marine Micropaleontology, 2004 - Elsevier
Sudden global warming∼ 55 Ma is associated with remarkable biotic events among both
terrestrial and marine organisms. The marine microplankton were especially affected, with a …

Ocean warming, not acidification, controlled coccolithophore response during past greenhouse climate change

SJ Gibbs, PR Bown, A Ridgwell, JR Young… - …, 2016 - pubs.geoscienceworld.org
Current carbon dioxide emissions are an assumed threat to oceanic calcifying plankton
(coccolithophores) not just due to rising sea-surface temperatures, but also because of …

[PDF][PDF] Excess barite accumulation during the Paleocene-Eocene Thermal Maximum: Massive input of dissolved barium from seafloor gas hydrate reservoirs

GR Dickens, T Fewless, E Thomas… - … -Geological Society of …, 2003 - researchgate.net
ABSTRACT A–2‰ to–3‰ excursion characterizes carbon isotope records across the
Paleocene-Eocene Thermal Maximum (PETM), probably signifying transfer of∼ 2000 …

Deep‐sea redox across the Paleocene‐Eocene thermal maximum

C Pälike, ML Delaney, JC Zachos - Geochemistry, Geophysics …, 2014 - Wiley Online Library
Large amounts of 13C‐depleted carbon were released to the oceans and atmosphere
during a period of abrupt global warming at the Paleocene‐Eocene thermal maximum …

Response of Antarctic (ODP Site 690) planktonic foraminifera to the Paleocene–Eocene thermal maximum: faunal evidence for ocean/climate change

DC Kelly - Paleoceanography, 2002 - Wiley Online Library
High‐resolution study of Antarctic planktonic foraminiferal assemblages (Ocean Drilling
Program Site 690, Weddell Sea) shows that these microplankton underwent a stepwise …

Variability in climate and productivity during the Paleocene–Eocene Thermal Maximum in the western Tethys (Forada section)

L Giusberti, F Boscolo Galazzo, E Thomas - Climate of the Past, 2016 - cp.copernicus.org
The Forada section (northeastern Italy) provides a continuous, expanded deep-sea record of
the Paleocene–Eocene Thermal Maximum (PETM) in the central-western Tethys. We …

Environmental dynamics during the Paleocene–Eocene thermal maximum (PETM) in the northeastern Peri-Tethys revealed by high-resolution micropalaeontological …

E Shcherbinina, Y Gavrilov, A Iakovleva… - Palaeogeography …, 2016 - Elsevier
The sedimentary record of the Paleocene–Eocene Thermal Maximum (PETM) in the wide
epeiric sea of the NE Peri-Tethys contains a sapropelitic bed (SBD) characterized by a …

Climatic and environmental changes across the early Eocene climatic optimum at mid-Waipara River, Canterbury Basin, New Zealand

EM Crouch, CL Shepherd, HEG Morgans… - Earth-Science …, 2020 - Elsevier
Abstract The Cretaceous–Paleogene marine sedimentary succession exposed in the banks
of the middle reaches of the Waipara River (referred to as mid-Waipara), north Canterbury …

Anomalous shifts in tropical Pacific planktonic and benthic foraminiferal test size during the Paleocene–Eocene thermal maximum

K Kaiho, K Takeda, MR Petrizzo, JC Zachos - Palaeogeography …, 2006 - Elsevier
Paleocene–Eocene warming and changes in oceanic hydrography should have significantly
impacted the ecology of marine microorganisms, both at the surface and on the seafloor. We …

Response of calcareous nannoplankton to the Paleocene–Eocene Thermal Maximum in the Paratethys Seaway (Tarim Basin, West China)

Y Wang, Y Cui, H Su, J Jiang, Y Wang, Z Yang… - Global and Planetary …, 2022 - Elsevier
Abstract The Paleocene-Eocene Thermal Maximum (PETM) was a rapid global warming
occurred 56 million years ago and has been widely viewed as an ancient analogue to the …