Jolley et al. (2002) have proposed that the date of the Paleocene - Eocene thermal maximum is ca. 60 Ma, at least 5 m.y. older than currently estimated and, as a result, argue that the Paleogene time scale of Berggren et al. (1995) is grossly miscalibrated. The implications of this proposal are implausible, and we attribute the discrepancy in age noted by Jolley et al. (2002) to miscorrelation of the Staffa-type palynofloras and ambiguous isotopic dates from the North Atlantic igneous province
A significant discrepancy of up to 0.6 Myr exists between radio-isotopically calibrated and astronom...
New information has become available that requires a revision of Paleogene chronology incorporated i...
The construction of a permanent astronomical time scale for the Paleocene tuned to stable 405-kyr ec...
late Paleocene thermal maximum (LPTM) has an age between 57.5 and 60.54 Ma (vs. 54.98 Ma in the curr...
Igneous activity in the North Atlantic igneous province began with the arrival of the proto-Iceland ...
To explore cause and consequences of past climate change, very accurate age models such as those pro...
Here we present combined radio-isotopic dating (U-Pb zircon) and cyclostratigraphic analysis of the ...
Significant progress has been made over the last decade in the extension of astronomically calibrate...
Integrated research over the past decade has led to the recognition of a short (150-200 k.y.) interv...
International audienceTiming is crucial to understanding the causes and consequences of events in Ea...
An age model (Mark et al., 2017) for ODP 758 and the Matuyama-Brunhes boundary transition and Termin...
Five sections drilled in multiple holes over a depth transect of more than 2200 m at the Walvis Ridg...
The first complete cyclic sedimentary successions for the early Paleogene from drilling multiple hol...
The chronology of the events associated with the late Paleocene thermal maximum (LPTM, Chron C24r) h...
A significant discrepancy of up to 0.6 Myr exists between radio-isotopically calibrated and astronom...
A significant discrepancy of up to 0.6 Myr exists between radio-isotopically calibrated and astronom...
New information has become available that requires a revision of Paleogene chronology incorporated i...
The construction of a permanent astronomical time scale for the Paleocene tuned to stable 405-kyr ec...
late Paleocene thermal maximum (LPTM) has an age between 57.5 and 60.54 Ma (vs. 54.98 Ma in the curr...
Igneous activity in the North Atlantic igneous province began with the arrival of the proto-Iceland ...
To explore cause and consequences of past climate change, very accurate age models such as those pro...
Here we present combined radio-isotopic dating (U-Pb zircon) and cyclostratigraphic analysis of the ...
Significant progress has been made over the last decade in the extension of astronomically calibrate...
Integrated research over the past decade has led to the recognition of a short (150-200 k.y.) interv...
International audienceTiming is crucial to understanding the causes and consequences of events in Ea...
An age model (Mark et al., 2017) for ODP 758 and the Matuyama-Brunhes boundary transition and Termin...
Five sections drilled in multiple holes over a depth transect of more than 2200 m at the Walvis Ridg...
The first complete cyclic sedimentary successions for the early Paleogene from drilling multiple hol...
The chronology of the events associated with the late Paleocene thermal maximum (LPTM, Chron C24r) h...
A significant discrepancy of up to 0.6 Myr exists between radio-isotopically calibrated and astronom...
A significant discrepancy of up to 0.6 Myr exists between radio-isotopically calibrated and astronom...
New information has become available that requires a revision of Paleogene chronology incorporated i...
The construction of a permanent astronomical time scale for the Paleocene tuned to stable 405-kyr ec...