The global stratotype section and point (GSSP) for the base of the holocene series/epoch (Quaternary System/Period) in the NGRIP ice core

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Standard

The global stratotype section and point (GSSP) for the base of the holocene series/epoch (Quaternary System/Period) in the NGRIP ice core. / Walker, Mike; Johnsen, Sigfus Johann; Rasmussen, Sune Olander; Steffensen, Jørgen Peder; Popp, Trevor James; Gibbard, Philip; Hoek, Wim; Lowe, John; Andrews, John; Björck, Svante; Cwynar, Les; Hughen, Konrad; Kershaw, Peter; Kromer, Bernd; Litt, Thomas; Lowe, David J.; Nakagawa, Takeshi; Newnham, Rewi; Schwander, Jakob.

I: Episodes, Bind 31, Nr. 2, 01.06.2008, s. 264-267.

Publikation: Bidrag til tidsskrift › Tidsskriftartikel › Forskning › fagfællebedømt

Harvard

Walker, M, Johnsen, SJ, Rasmussen, SO, Steffensen, JP, Popp, TJ, Gibbard, P, Hoek, W, Lowe, J, Andrews, J, Björck, S, Cwynar, L, Hughen, K, Kershaw, P, Kromer, B, Litt, T, Lowe, DJ, Nakagawa, T, Newnham, R & Schwander, J 2008, 'The global stratotype section and point (GSSP) for the base of the holocene series/epoch (Quaternary System/Period) in the NGRIP ice core', Episodes, bind 31, nr. 2, s. 264-267.

APA

Walker, M., Johnsen, S. J., Rasmussen, S. O., Steffensen, J. P., Popp, T. J., Gibbard, P., Hoek, W., Lowe, J., Andrews, J., Björck, S., Cwynar, L., Hughen, K., Kershaw, P., Kromer, B., Litt, T., Lowe, D. J., Nakagawa, T., Newnham, R., & Schwander, J. (2008). The global stratotype section and point (GSSP) for the base of the holocene series/epoch (Quaternary System/Period) in the NGRIP ice core. Episodes, 31(2), 264-267.

Vancouver

Walker M, Johnsen SJ, Rasmussen SO, Steffensen JP, Popp TJ, Gibbard P o.a. The global stratotype section and point (GSSP) for the base of the holocene series/epoch (Quaternary System/Period) in the NGRIP ice core. Episodes. 2008 jun. 1;31(2):264-267.

Author

Walker, Mike ; Johnsen, Sigfus Johann ; Rasmussen, Sune Olander ; Steffensen, Jørgen Peder ; Popp, Trevor James ; Gibbard, Philip ; Hoek, Wim ; Lowe, John ; Andrews, John ; Björck, Svante ; Cwynar, Les ; Hughen, Konrad ; Kershaw, Peter ; Kromer, Bernd ; Litt, Thomas ; Lowe, David J. ; Nakagawa, Takeshi ; Newnham, Rewi ; Schwander, Jakob. / The global stratotype section and point (GSSP) for the base of the holocene series/epoch (Quaternary System/Period) in the NGRIP ice core. I: Episodes. 2008 ; Bind 31, Nr. 2. s. 264-267.

Bibtex

@article{506ef830626d11dd8d9f000ea68e967b,
title = "The global stratotype section and point (GSSP) for the base of the holocene series/epoch (Quaternary System/Period) in the NGRIP ice core",
abstract = "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 is most clearly reflected in an abrupt shift in deuterium excess values, accompanied by more gradual changes in d18O, dust concentration, a range of chemical species, and annual layer thickness. A timescale based on multi-parameter annual layer counting provides an age of 11,700 yr b2k (before AD2000) for the base of the Holocene, with an estimated 2s uncertainty of 99 yr. It is proposed that an archived core from this unique sequence should constitute the Global Stratotype Section and Point (GSSP) for the base of the Holocene Series/Epoch (Quaternary System/Period).",
author = "Mike Walker and Johnsen, {Sigfus Johann} and Rasmussen, {Sune Olander} and Steffensen, {J{\o}rgen Peder} and Popp, {Trevor James} and Philip Gibbard and Wim Hoek and John Lowe and John Andrews and Svante Bj{\"o}rck and Les Cwynar and Konrad Hughen and Peter Kershaw and Bernd Kromer and Thomas Litt and Lowe, {David J.} and Takeshi Nakagawa and Rewi Newnham and Jakob Schwander",
year = "2008",
month = jun,
day = "1",
language = "English",
volume = "31",
pages = "264--267",
journal = "Episodes",
issn = "0705-3797",
publisher = "Geological Society of India",
number = "2",

}

RIS

TY - JOUR

T1 - The global stratotype section and point (GSSP) for the base of the holocene series/epoch (Quaternary System/Period) in the NGRIP ice core

AU - Walker, Mike

AU - Johnsen, Sigfus Johann

AU - Rasmussen, Sune Olander

AU - Steffensen, Jørgen Peder

AU - Popp, Trevor James

AU - Gibbard, Philip

AU - Hoek, Wim

AU - Lowe, John

AU - Andrews, John

AU - Björck, Svante

AU - Cwynar, Les

AU - Hughen, Konrad

AU - Kershaw, Peter

AU - Kromer, Bernd

AU - Litt, Thomas

AU - Lowe, David J.

AU - Nakagawa, Takeshi

AU - Newnham, Rewi

AU - Schwander, Jakob

PY - 2008/6/1

Y1 - 2008/6/1

N2 - 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 is most clearly reflected in an abrupt shift in deuterium excess values, accompanied by more gradual changes in d18O, dust concentration, a range of chemical species, and annual layer thickness. A timescale based on multi-parameter annual layer counting provides an age of 11,700 yr b2k (before AD2000) for the base of the Holocene, with an estimated 2s uncertainty of 99 yr. It is proposed that an archived core from this unique sequence should constitute the Global Stratotype Section and Point (GSSP) for the base of the Holocene Series/Epoch (Quaternary System/Period).

AB - 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 is most clearly reflected in an abrupt shift in deuterium excess values, accompanied by more gradual changes in d18O, dust concentration, a range of chemical species, and annual layer thickness. A timescale based on multi-parameter annual layer counting provides an age of 11,700 yr b2k (before AD2000) for the base of the Holocene, with an estimated 2s uncertainty of 99 yr. It is proposed that an archived core from this unique sequence should constitute the Global Stratotype Section and Point (GSSP) for the base of the Holocene Series/Epoch (Quaternary System/Period).

M3 - Journal article

VL - 31

SP - 264

EP - 267

JO - Episodes

JF - Episodes

SN - 0705-3797

IS - 2

ER -

ID: 5345747