Dating of the GV7 East Antarctic ice core by high-resolution chemical records and focus on the accumulation rate variability in the last millennium

Ice core dating is the first step for a correct interpretation of climatic and environmental changes. In this work, we release the dating of the uppermost 197 m of the 250 m deep GV7(B) ice core (drill site, 70∘41′ S, 158∘52′ E; 1950 m a.s.l. in Oates Land, East Antarctica) with a sub-annual resolut...

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Published in:Climate of the Past
Main Authors: R. Nardin, M. Severi, A. Amore, S. Becagli, F. Burgay, L. Caiazzo, V. Ciardini, G. Dreossi, M. Frezzotti, S.-B. Hong, I. Khan, B. M. Narcisi, M. Proposito, C. Scarchilli, E. Selmo, A. Spolaor, B. Stenni, R. Traversi
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2021
Subjects:
Online Access:https://doi.org/10.5194/cp-17-2073-2021
https://cp.copernicus.org/articles/17/2073/2021/cp-17-2073-2021.pdf
https://doaj.org/article/16dd67f0bb2f4866b86c8313fb33bf00
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author R. Nardin
M. Severi
A. Amore
S. Becagli
F. Burgay
L. Caiazzo
V. Ciardini
G. Dreossi
M. Frezzotti
S.-B. Hong
I. Khan
B. M. Narcisi
M. Proposito
C. Scarchilli
E. Selmo
A. Spolaor
B. Stenni
R. Traversi
author_facet R. Nardin
M. Severi
A. Amore
S. Becagli
F. Burgay
L. Caiazzo
V. Ciardini
G. Dreossi
M. Frezzotti
S.-B. Hong
I. Khan
B. M. Narcisi
M. Proposito
C. Scarchilli
E. Selmo
A. Spolaor
B. Stenni
R. Traversi
author_sort R. Nardin
collection Unknown
container_issue 5
container_start_page 2073
container_title Climate of the Past
container_volume 17
description Ice core dating is the first step for a correct interpretation of climatic and environmental changes. In this work, we release the dating of the uppermost 197 m of the 250 m deep GV7(B) ice core (drill site, 70∘41′ S, 158∘52′ E; 1950 m a.s.l. in Oates Land, East Antarctica) with a sub-annual resolution. Chemical records of NO3-, MSA (methanesulfonic acid), non-sea-salt SO42- (nssSO42-), sea-salt ions and water stable isotopes (δ18O) were studied as candidates for dating due to their seasonal pattern. Different procedures were tested but the nssSO42- record proved to be the most reliable on the short- and long-term scales, so it was chosen for annual layer counting along the whole ice core. The dating was constrained by using volcanic signatures from historically known events as tie points, thus providing an accurate age–depth relationship for the period 1179–2009 CE. The achievement of the complete age scale allowed us to calculate the annual mean accumulation rate throughout the analyzed 197 m of the core, yielding an annually resolved history of the snow accumulation on site in the last millennium. A small yet consistent rise in accumulation rate (Tr = 1.6, p<0.001) was found for the last 830 years starting around mid-18th century.
format Article in Journal/Newspaper
genre Antarc*
Antarctic
Antarctica
East Antarctica
ice core
Oates Land
genre_facet Antarc*
Antarctic
Antarctica
East Antarctica
ice core
Oates Land
geographic Antarctic
East Antarctica
Oates Land
geographic_facet Antarctic
East Antarctica
Oates Land
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long_lat ENVELOPE(158.000,158.000,-70.000,-70.000)
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op_doi https://doi.org/10.5194/cp-17-2073-2021
op_relation doi:10.5194/cp-17-2073-2021
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https://cp.copernicus.org/articles/17/2073/2021/cp-17-2073-2021.pdf
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op_source Climate of the Past, Vol 17, Pp 2073-2089 (2021)
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spelling fttriple:oai:gotriple.eu:oai:doaj.org/article:16dd67f0bb2f4866b86c8313fb33bf00 2025-01-16T19:02:58+00:00 Dating of the GV7 East Antarctic ice core by high-resolution chemical records and focus on the accumulation rate variability in the last millennium R. Nardin M. Severi A. Amore S. Becagli F. Burgay L. Caiazzo V. Ciardini G. Dreossi M. Frezzotti S.-B. Hong I. Khan B. M. Narcisi M. Proposito C. Scarchilli E. Selmo A. Spolaor B. Stenni R. Traversi 2021-10-01 https://doi.org/10.5194/cp-17-2073-2021 https://cp.copernicus.org/articles/17/2073/2021/cp-17-2073-2021.pdf https://doaj.org/article/16dd67f0bb2f4866b86c8313fb33bf00 en eng Copernicus Publications doi:10.5194/cp-17-2073-2021 1814-9324 1814-9332 https://cp.copernicus.org/articles/17/2073/2021/cp-17-2073-2021.pdf https://doaj.org/article/16dd67f0bb2f4866b86c8313fb33bf00 undefined Climate of the Past, Vol 17, Pp 2073-2089 (2021) geo envir Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2021 fttriple https://doi.org/10.5194/cp-17-2073-2021 2023-01-22T18:19:22Z Ice core dating is the first step for a correct interpretation of climatic and environmental changes. In this work, we release the dating of the uppermost 197 m of the 250 m deep GV7(B) ice core (drill site, 70∘41′ S, 158∘52′ E; 1950 m a.s.l. in Oates Land, East Antarctica) with a sub-annual resolution. Chemical records of NO3-, MSA (methanesulfonic acid), non-sea-salt SO42- (nssSO42-), sea-salt ions and water stable isotopes (δ18O) were studied as candidates for dating due to their seasonal pattern. Different procedures were tested but the nssSO42- record proved to be the most reliable on the short- and long-term scales, so it was chosen for annual layer counting along the whole ice core. The dating was constrained by using volcanic signatures from historically known events as tie points, thus providing an accurate age–depth relationship for the period 1179–2009 CE. The achievement of the complete age scale allowed us to calculate the annual mean accumulation rate throughout the analyzed 197 m of the core, yielding an annually resolved history of the snow accumulation on site in the last millennium. A small yet consistent rise in accumulation rate (Tr = 1.6, p<0.001) was found for the last 830 years starting around mid-18th century. Article in Journal/Newspaper Antarc* Antarctic Antarctica East Antarctica ice core Oates Land Unknown Antarctic East Antarctica Oates Land ENVELOPE(158.000,158.000,-70.000,-70.000) Climate of the Past 17 5 2073 2089
spellingShingle geo
envir
R. Nardin
M. Severi
A. Amore
S. Becagli
F. Burgay
L. Caiazzo
V. Ciardini
G. Dreossi
M. Frezzotti
S.-B. Hong
I. Khan
B. M. Narcisi
M. Proposito
C. Scarchilli
E. Selmo
A. Spolaor
B. Stenni
R. Traversi
Dating of the GV7 East Antarctic ice core by high-resolution chemical records and focus on the accumulation rate variability in the last millennium
title Dating of the GV7 East Antarctic ice core by high-resolution chemical records and focus on the accumulation rate variability in the last millennium
title_full Dating of the GV7 East Antarctic ice core by high-resolution chemical records and focus on the accumulation rate variability in the last millennium
title_fullStr Dating of the GV7 East Antarctic ice core by high-resolution chemical records and focus on the accumulation rate variability in the last millennium
title_full_unstemmed Dating of the GV7 East Antarctic ice core by high-resolution chemical records and focus on the accumulation rate variability in the last millennium
title_short Dating of the GV7 East Antarctic ice core by high-resolution chemical records and focus on the accumulation rate variability in the last millennium
title_sort dating of the gv7 east antarctic ice core by high-resolution chemical records and focus on the accumulation rate variability in the last millennium
topic geo
envir
topic_facet geo
envir
url https://doi.org/10.5194/cp-17-2073-2021
https://cp.copernicus.org/articles/17/2073/2021/cp-17-2073-2021.pdf
https://doaj.org/article/16dd67f0bb2f4866b86c8313fb33bf00