The Miocene: The future of the past
Abstract The Miocene epoch (23.03–5.33 Ma) was a time interval of global warmth, relative
to today. Continental configurations and mountain topography transitioned toward modern …
to today. Continental configurations and mountain topography transitioned toward modern …
Paleoecology, ploidy, paleoatmospheric composition, and developmental biology: a review of the multiple uses of fossil stomata
Paleoecology, Ploidy, Paleoatmospheric Composition, and Developmental Biology: A Review
of the Multiple Uses of Fossil Stomata | Plant Physiology | Oxford Academic Skip to Main …
of the Multiple Uses of Fossil Stomata | Plant Physiology | Oxford Academic Skip to Main …
Toward a Cenozoic history of atmospheric CO2
Cenozoic CO2 Proxy Integration Project (CenCO2PIP) … - Science, 2023 - science.org
The geological record encodes the relationship between climate and atmospheric carbon
dioxide (CO2) over long and short timescales, as well as potential drivers of evolutionary …
dioxide (CO2) over long and short timescales, as well as potential drivers of evolutionary …
A high‐Fidelity benthic stable isotope record of late Cretaceous–early Eocene climate change and carbon‐cycling
Abstract The Late Cretaceous–Early Paleogene is the most recent period in Earth history
that experienced sustained global greenhouse warmth on multimillion year timescales. Yet …
that experienced sustained global greenhouse warmth on multimillion year timescales. Yet …
Rapid ocean acidification and protracted Earth system recovery followed the end-Cretaceous Chicxulub impact
Mass extinction at the Cretaceous–Paleogene (K-Pg) boundary coincides with the
Chicxulub bolide impact and also falls within the broader time frame of Deccan trap …
Chicxulub bolide impact and also falls within the broader time frame of Deccan trap …
[HTML][HTML] A new high-resolution chronology for the late Maastrichtian warming event: Establishing robust temporal links with the onset of Deccan volcanism
The late Maastrichtian warming event was defined by a global temperature increase of∼ 2.5–
5 C that occurred∼ 150–300 ky before the Cretaceous-Paleogene (K-Pg) mass extinction …
5 C that occurred∼ 150–300 ky before the Cretaceous-Paleogene (K-Pg) mass extinction …
Rapid recovery of Patagonian plant–insect associations after the end-Cretaceous extinction
Abstract The Southern Hemisphere may have provided biodiversity refugia after the
Cretaceous/Palaeogene (K/Pg) mass extinction. However, few extinction and recovery …
Cretaceous/Palaeogene (K/Pg) mass extinction. However, few extinction and recovery …
Stable isotope constraints on marine productivity across the Cretaceous‐Paleogene mass extinction
The effects of the Cretaceous‐Paleogene (K/Pg) mass extinction (~ 66 Ma) on marine
primary and export productivity remain debated. We studied changes in carbon and nitrogen …
primary and export productivity remain debated. We studied changes in carbon and nitrogen …
Multiproxy analysis of paleoenvironmental, paleoclimatic and paleoceanographic changes during the early Danian in the Caravaca section (Spain)
After the Chicxulub impact and mass extinction at the Cretaceous-Paleogene boundary (K-
PgB), ecosystems haltingly recovered under unstable conditions. An early Danian (65.9 Ma) …
PgB), ecosystems haltingly recovered under unstable conditions. An early Danian (65.9 Ma) …
[HTML][HTML] Significant transient pCO2 perturbation at the New Zealand Oligocene-Miocene transition recorded by fossil plant stomata
The reorganisation of Earth's climate system from the Oligocene to the Miocene was
influenced by complex interactions between Tethyan tectonics, orbital parameters …
influenced by complex interactions between Tethyan tectonics, orbital parameters …