The Latest Danian Event (LDE, ~ 62.2 Ma) is characterized by global changes in the carbon cycle as indicated by two negative δ13C excursions of up to ~ 1‰. These δ13C shifts are accompanied by a 2–3 °C warming of both surface and deep waters based on benthic and planktic foraminiferal δ18O measurements, and the LDE has, thus, been considered as a so-called hyperthermal event. The event lasted for 200 kyr and has been identified in various ocean basins and shallow marine settings. Here, we present a compilation of data from three deep-sea cores covering the Pacific, North and South Atlantic oceans as well as a southern Tethyan shelf section to document the response of planktic foraminifera assemblages to ocean warming. In all studied success...
The Paleocene and early Eocene (~66–40 Ma) is characterised by a number of transient warming events,...
An abrupt global warming of 3-4°C occurred near the end of the Maastrichtian at 65.45-65.10 Ma. The ...
During the Middle Eocene Climatic Optimum (MECO; 40 Ma), one of the major short-term Cenozoic climat...
During the Paleocene the marine ecosystem was disturbed by several transient climate events, e.g. th...
A number of short warming events occurred during Paleocene and Eocene, of which the "Paleocene-Eocen...
The early Paleogene is characterized by numerous hyperthermals, transient (< 200 kyr) ocean warming ...
The Latest Danian Event (LDE, c. 62.1 Ma) is an early Palaeogene hyperthermal or transient (<200 ka)...
Superimposed on the warm greenhouse climate of the early Paleogene, several hyperthermals, warming e...
The Paleogene was punctuated by perturbations of the global carbon cycle, many associated with trans...
The Latest Danian Event (LDE; ca. 62.15 Ma) is a major double-spiked eccentricity-driven transient w...
The Latest Danian Event (LDE, ∼62.15 Ma) represents a transient carbon cycle perturbation on a globa...
<div><p>The marine ecosystem has been severely disturbed by several transient paleoenvironmental eve...
Several transient (<200 kyr) hyperthermal events disturbed the early Paleogene marine ecosystem, of ...
This paper provides a synthesis of the long- and short-term response of various marine ecosystems (d...
Several transient hyperthermal events with a significant impact on global climate and environment ar...
The Paleocene and early Eocene (~66–40 Ma) is characterised by a number of transient warming events,...
An abrupt global warming of 3-4°C occurred near the end of the Maastrichtian at 65.45-65.10 Ma. The ...
During the Middle Eocene Climatic Optimum (MECO; 40 Ma), one of the major short-term Cenozoic climat...
During the Paleocene the marine ecosystem was disturbed by several transient climate events, e.g. th...
A number of short warming events occurred during Paleocene and Eocene, of which the "Paleocene-Eocen...
The early Paleogene is characterized by numerous hyperthermals, transient (< 200 kyr) ocean warming ...
The Latest Danian Event (LDE, c. 62.1 Ma) is an early Palaeogene hyperthermal or transient (<200 ka)...
Superimposed on the warm greenhouse climate of the early Paleogene, several hyperthermals, warming e...
The Paleogene was punctuated by perturbations of the global carbon cycle, many associated with trans...
The Latest Danian Event (LDE; ca. 62.15 Ma) is a major double-spiked eccentricity-driven transient w...
The Latest Danian Event (LDE, ∼62.15 Ma) represents a transient carbon cycle perturbation on a globa...
<div><p>The marine ecosystem has been severely disturbed by several transient paleoenvironmental eve...
Several transient (<200 kyr) hyperthermal events disturbed the early Paleogene marine ecosystem, of ...
This paper provides a synthesis of the long- and short-term response of various marine ecosystems (d...
Several transient hyperthermal events with a significant impact on global climate and environment ar...
The Paleocene and early Eocene (~66–40 Ma) is characterised by a number of transient warming events,...
An abrupt global warming of 3-4°C occurred near the end of the Maastrichtian at 65.45-65.10 Ma. The ...
During the Middle Eocene Climatic Optimum (MECO; 40 Ma), one of the major short-term Cenozoic climat...