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 …
epeiric sea of the NE Peri-Tethys contains a sapropelitic bed (SBD) characterized by a …
The Paleocene–Eocene Thermal Maximum as recorded by Tethyan planktonic foraminifera in the Forada section (northern Italy)
The Forada section in the Venetian Pre-Alps of northern Italy represents an expanded
record of the Paleocene–Eocene Thermal Maximum (PETM) at a depositional paleodepth of …
record of the Paleocene–Eocene Thermal Maximum (PETM) at a depositional paleodepth of …
[PDF][PDF] 140 million years of tropical biome evolution
C Jaramillo - The Geology of Colombia (ed. Gomez, J.). Colombian …, 2019 - stri-apps.si.edu
The origin and development of Neotropical biomes are central to our understanding of
extant ecosystems and our ability to predict their future. During the Cretaceous, biomass of …
extant ecosystems and our ability to predict their future. During the Cretaceous, biomass of …
A biogenic origin for anomalous fine‐grained magnetic material at the Paleocene‐Eocene boundary at Wilson Lake, New Jersey
PC Lippert, JC Zachos - Paleoceanography, 2007 - Wiley Online Library
The Paleocene‐Eocene Thermal Maximum, which occurred∼ 55.5 Ma, was caused by a
massive release of carbon, as indicated by an∼ 3‰ negative carbon isotope excursion …
massive release of carbon, as indicated by an∼ 3‰ negative carbon isotope excursion …
Geochemical evidence for volcanic activity prior to and enhanced terrestrial weathering during the Paleocene Eocene Thermal Maximum
R Wieczorek, MS Fantle, LR Kump… - … et Cosmochimica Acta, 2013 - Elsevier
Abstract The Re–Os and major element geochemistry of an expanded gray shale sequence
from the Central Basin in Spitsbergen, Svalbard Archipelago (Norway) over the Paleocene …
from the Central Basin in Spitsbergen, Svalbard Archipelago (Norway) over the Paleocene …
Coupled high-resolution marine and terrestrial records of carbon and hydrologic cycles variations during the Paleocene–Eocene Thermal Maximum (PETM)
The Paleocene–Eocene Thermal Maximum is characterized by a massive perturbation of
the global carbon cycle reflected in a large, negative carbon isotope excursion associated …
the global carbon cycle reflected in a large, negative carbon isotope excursion associated …
Constraining multiple controls on planktic foraminifera Mg/Ca
Abstract The Mg/Ca of planktic foraminifera is widely used to determine past surface ocean
temperatures but temperature is not the only factor that controls test Mg/Ca. Here we quantify …
temperatures but temperature is not the only factor that controls test Mg/Ca. Here we quantify …
Modeling the global carbon cycle with a gas hydrate capacitor: significance for the latest Paleocene thermal maximum
GR Dickens - Geophysical Monograph Series, 2001 - ui.adsabs.harvard.edu
Abstract The" Latest Paleocene Thermal Maximum"(or LPTM) ca. 55 Ma was characterized
by a 4 to 6 C rise in deep ocean water temperature and an extraordinary injection of 12 C …
by a 4 to 6 C rise in deep ocean water temperature and an extraordinary injection of 12 C …
Temporal variation in the wavelength of hummocky cross-stratification: Implications for storm intensity through Mesozoic and Cenozoic
M Ito, A Ishigaki, T Nishikawa, T Saito - Geology, 2001 - pubs.geoscienceworld.org
Hummocky cross-stratification is believed to be one of the diagnostic sedimentary structures
of storm-dominated shallow-marine environments. The wavelength of this stratification …
of storm-dominated shallow-marine environments. The wavelength of this stratification …
Stable isotopes of carbon and sulphur as indicators of environmental change: past and present
R Newton, S Bottrell - Journal of the Geological Society, 2007 - lyellcollection.org
Stable isotopes of carbon (12C and 13C) and sulphur (32S and 34S) are fractionated during
some of the transformations between reservoirs in the global carbon and sulphur cycles. The …
some of the transformations between reservoirs in the global carbon and sulphur cycles. The …