Sune O Rasmussen

Biographic Data

ID	10711551
NAME	Sune O Rasmussen
GIVEN NAMES	Sune O
FAMILY NAME	Rasmussen
SIGNATURE	RASMUSSEN S O
AFFILIATIONS	University of Copenhagen
ORCID	0000-0002-4177-3611
VERIFIED	No
TOTAL WORKS	13
TOTAL CITATIONS	0
AUTHOR COUNT	13
EDITOR COUNT	0
FIRST PUBLICATION YEAR	2006
LATEST PUBLICATION YEAR	2018
H-INDEX	0

Formal ratification of the subdivision of the Holocene Series/Epoch (Quaternary System/Period)
Open AccessMike Walker, Martin J Head et al.ARTICLEEpisodes2018
Mike Walker, Martin J. Head, Max Berkelhammer, Svante Björck, Hai Cheng, Les Cwynar, David Fisher, Vasilios Gkinis, Antony Long, John Lowe, Rewi Newnham, Sune Olander Rasmussen, Harvey Weiss. Episodes 2018;41:213-23. https://doi.org/10.18814/epiiugs/2018/018016
A stratigraphic framework for abrupt climatic changes during the Last Glacial period based on three synchronized Greenland ice-core records
Open AccessSune O Rasmussen, Matthias Bigler et al.ARTICLEQuaternary Science Reviews2014
Due to their outstanding resolution and well-constrained chronologies, Greenland ice-core records provide a master record of past climatic changes throughout the Last Interglacial–Glacial cycle in the North Atlantic region. As part of the INTIMATE (INTegration of Ice-core, MArine and TErrestrial records) project, protocols have been proposed to ensure consistent and robust correlation between different records of past climate. A key element of th…
Synchronisation of palaeoenvironmental records over the last 60,000 years, and an extended Intimate event stratigraphy to 48,000 b2k
Open AccessSimon Blockley, Simon P E Blockley et al.ARTICLEQuaternary Science Reviews2012
Formal subdivision of the Holocene Series/Epoch
Open AccessMike Walker, M J C Walker et al.ARTICLEJournal of Quaternary Science2012
This discussion paper, by a Working Group of INTIMATE (Integration of ice‐core, marine and terrestrial records) and the Subcommision on Quaternary Stratigraphy (SQS) of the International Commission on Stratigraphy (ICS), considers the prospects for a formal subdivision of the Holocene Series/Epoch. Although previous attempts to subdivide the Holocene have proved inconclusive, recent developments in Quaternary stratigraphy, notably the definition …
Formal definition and dating of the GSSP (Global Stratotype Section and Point) for the base of the Holocene using the Greenland NGRIP ice core, and selected auxiliary records
Open AccessMike Walker, Sigfús Johnsen et al.ARTICLEJournal of Quaternary Science2009
The Greenland ice core from NorthGRIP (NGRIP) contains a proxy climate record across the Pleistocene–Holocene boundary of unprecedented clarity and resolution. Analysis of an array of physical and chemical parameters within the ice enables the base of the Holocene, as reflected in the first signs of climatic warming at the end of the Younger Dryas/Greenland Stadial 1 cold phase, to be located with a high degree of precision. This climatic event i…
A 60 000 year Greenland stratigraphic ice core chronology
Open AccessAndreas Svensson, K K Andersen et al.ARTICLEClimate of the Past2008
The Greenland Ice Core Chronology 2005 (GICC05) is a time scale based on annual layer counting of high-resolution records from Greenland ice cores. Whereas the Holocene part of the time scale is based on various records from the DYE-3, the GRIP, and the NorthGRIP ice cores, the glacial part is solely based on NorthGRIP records. Here we present an 18 ka extension of the time scale such that GICC05 continuously covers the past 60 ka. The new sectio…
Synchronisation of palaeoenvironmental events in the North Atlantic region during the Last Termination
Open AccessJ J Lowe, Sune O Rasmussen et al.ARTICLEQuaternary Science Reviews2008
High-Resolution Greenland Ice Core Data Show Abrupt Climate Change Happens in Few Years
Open AccessJørgen Peder Steffensen, K K Andersen et al.ARTICLEScience2008
The last two abrupt warmings at the onset of our present warm interglacial period, interrupted by the Younger Dryas cooling event, were investigated at high temporal resolution from the North Greenland Ice Core Project ice core. The deuterium excess, a proxy of Greenland precipitation moisture source, switched mode within 1 to 3 years over these transitions and initiated a more gradual change (over 50 years) of the Greenland air temperature, as r…
Early Holocene climate oscillations recorded in three Greenland ice cores
Open AccessSune O Rasmussen, Bo Vinther et al.ARTICLEQuaternary Science Reviews2007
A synchronized dating of three Greenland ice cores throughout the Holocene
Open AccessBo Vinther, B M Vinther et al.ARTICLEJournal of Geophysical Research:…2006
As part of the effort to create the new Greenland Ice Core Chronology 2005 (GICC05) a synchronized stratigraphical timescale for the Holocene parts of the DYE‐3, Greenland Ice Core Project (GRIP), and North Greenland Ice Core Project (NGRIP) ice cores is made by using volcanic reference horizons in electrical conductivity measurements to match the cores. The main annual layer counting is carried out on the most suited records only, exploiting tha…
The Greenland Ice Core Chronology 2005, 15–42ka. Part 1
Open AccessK K Andersen, Andreas Svensson et al.ARTICLEQuaternary Science Reviews2006
The Greenland Ice Core Chronology 2005, 15–42ka. Part 2
Open AccessAndreas Svensson, Anders Svensson et al.ARTICLEQuaternary Science Reviews2006
A new Greenland ice core chronology for the last glacial termination
Open AccessSune O Rasmussen, K K Andersen et al.ARTICLEJournal of Geophysical Research:…2006
We present a new common stratigraphic timescale for the North Greenland Ice Core Project (NGRIP) and GRIP ice cores. The timescale covers the period 7.9–14.8 kyr before present and includes the Bølling, Allerød, Younger Dryas, and early Holocene periods. We use a combination of new and previously published data, the most prominent being new high‐resolution Continuous Flow Analysis (CFA) impurity records from the NGRIP ice core. Several investigat…

A synchronized dating of three Greenland ice cores throughout the Holocene
Open AccessBo Vinther, B M Vinther et al.ARTICLEJournal of Geophysical Research:…2006
As part of the effort to create the new Greenland Ice Core Chronology 2005 (GICC05) a synchronized stratigraphical timescale for the Holocene parts of the DYE‐3, Greenland Ice Core Project (GRIP), and North Greenland Ice Core Project (NGRIP) ice cores is made by using volcanic reference horizons in electrical conductivity measurements to match the cores. The main annual layer counting is carried out on the most suited records only, exploiting tha…
The Greenland Ice Core Chronology 2005, 15–42ka. Part 1
Open AccessK K Andersen, Andreas Svensson et al.ARTICLEQuaternary Science Reviews2006
The Greenland Ice Core Chronology 2005, 15–42ka. Part 2
Open AccessAndreas Svensson, Anders Svensson et al.ARTICLEQuaternary Science Reviews2006
A new Greenland ice core chronology for the last glacial termination
Open AccessSune O Rasmussen, K K Andersen et al.ARTICLEJournal of Geophysical Research:…2006
We present a new common stratigraphic timescale for the North Greenland Ice Core Project (NGRIP) and GRIP ice cores. The timescale covers the period 7.9–14.8 kyr before present and includes the Bølling, Allerød, Younger Dryas, and early Holocene periods. We use a combination of new and previously published data, the most prominent being new high‐resolution Continuous Flow Analysis (CFA) impurity records from the NGRIP ice core. Several investigat…
Early Holocene climate oscillations recorded in three Greenland ice cores
Open AccessSune O Rasmussen, Bo Vinther et al.ARTICLEQuaternary Science Reviews2007
A 60 000 year Greenland stratigraphic ice core chronology
Open AccessAndreas Svensson, K K Andersen et al.ARTICLEClimate of the Past2008
The Greenland Ice Core Chronology 2005 (GICC05) is a time scale based on annual layer counting of high-resolution records from Greenland ice cores. Whereas the Holocene part of the time scale is based on various records from the DYE-3, the GRIP, and the NorthGRIP ice cores, the glacial part is solely based on NorthGRIP records. Here we present an 18 ka extension of the time scale such that GICC05 continuously covers the past 60 ka. The new sectio…
Synchronisation of palaeoenvironmental events in the North Atlantic region during the Last Termination
Open AccessJ J Lowe, Sune O Rasmussen et al.ARTICLEQuaternary Science Reviews2008
High-Resolution Greenland Ice Core Data Show Abrupt Climate Change Happens in Few Years
Open AccessJørgen Peder Steffensen, K K Andersen et al.ARTICLEScience2008
The last two abrupt warmings at the onset of our present warm interglacial period, interrupted by the Younger Dryas cooling event, were investigated at high temporal resolution from the North Greenland Ice Core Project ice core. The deuterium excess, a proxy of Greenland precipitation moisture source, switched mode within 1 to 3 years over these transitions and initiated a more gradual change (over 50 years) of the Greenland air temperature, as r…
Formal definition and dating of the GSSP (Global Stratotype Section and Point) for the base of the Holocene using the Greenland NGRIP ice core, and selected auxiliary records
Open AccessMike Walker, Sigfús Johnsen et al.ARTICLEJournal of Quaternary Science2009
The Greenland ice core from NorthGRIP (NGRIP) contains a proxy climate record across the Pleistocene–Holocene boundary of unprecedented clarity and resolution. Analysis of an array of physical and chemical parameters within the ice enables the base of the Holocene, as reflected in the first signs of climatic warming at the end of the Younger Dryas/Greenland Stadial 1 cold phase, to be located with a high degree of precision. This climatic event i…
Synchronisation of palaeoenvironmental records over the last 60,000 years, and an extended Intimate event stratigraphy to 48,000 b2k
Open AccessSimon Blockley, Simon P E Blockley et al.ARTICLEQuaternary Science Reviews2012
Formal subdivision of the Holocene Series/Epoch
Open AccessMike Walker, M J C Walker et al.ARTICLEJournal of Quaternary Science2012
This discussion paper, by a Working Group of INTIMATE (Integration of ice‐core, marine and terrestrial records) and the Subcommision on Quaternary Stratigraphy (SQS) of the International Commission on Stratigraphy (ICS), considers the prospects for a formal subdivision of the Holocene Series/Epoch. Although previous attempts to subdivide the Holocene have proved inconclusive, recent developments in Quaternary stratigraphy, notably the definition …
A stratigraphic framework for abrupt climatic changes during the Last Glacial period based on three synchronized Greenland ice-core records
Open AccessSune O Rasmussen, Matthias Bigler et al.ARTICLEQuaternary Science Reviews2014
Due to their outstanding resolution and well-constrained chronologies, Greenland ice-core records provide a master record of past climatic changes throughout the Last Interglacial–Glacial cycle in the North Atlantic region. As part of the INTIMATE (INTegration of Ice-core, MArine and TErrestrial records) project, protocols have been proposed to ensure consistent and robust correlation between different records of past climate. A key element of th…
Formal ratification of the subdivision of the Holocene Series/Epoch (Quaternary System/Period)
Open AccessMike Walker, Martin J Head et al.ARTICLEEpisodes2018
Mike Walker, Martin J. Head, Max Berkelhammer, Svante Björck, Hai Cheng, Les Cwynar, David Fisher, Vasilios Gkinis, Antony Long, John Lowe, Rewi Newnham, Sune Olander Rasmussen, Harvey Weiss. Episodes 2018;41:213-23. https://doi.org/10.18814/epiiugs/2018/018016