High-resolution, well-preserved tritium record in the ice of Bortig Ice Cave, Bihor Mountains, Romania

Two 2 m long ice cores (BA and BB) were extracted from the floor ice of Borştig Ice Cave in December 2005. Below a co-existing dust horizon (~13 cm underneath the 10 December 2005 ice surface) neither core presented any sign of hiatus, so the ice deposition is considered to be continuous. Tritium co...

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Published in:The Holocene
Main Authors: Kern, Zoltán, Molnár, Mihály, Svingor, Éva, Perşoiu, Aurel, Nagy, Balázs
Format: Article in Journal/Newspaper
Language:English
Published: SAGE Publications 2009
Subjects:
Online Access:http://dx.doi.org/10.1177/0959683609105296
http://journals.sagepub.com/doi/pdf/10.1177/0959683609105296
id crsagepubl:10.1177/0959683609105296
record_format openpolar
spelling crsagepubl:10.1177/0959683609105296 2023-05-15T16:39:21+02:00 High-resolution, well-preserved tritium record in the ice of Bortig Ice Cave, Bihor Mountains, Romania Kern, Zoltán Molnár, Mihály Svingor, Éva Perşoiu, Aurel Nagy, Balázs 2009 http://dx.doi.org/10.1177/0959683609105296 http://journals.sagepub.com/doi/pdf/10.1177/0959683609105296 en eng SAGE Publications http://journals.sagepub.com/page/policies/text-and-data-mining-license The Holocene volume 19, issue 5, page 729-736 ISSN 0959-6836 1477-0911 Paleontology Earth-Surface Processes Ecology Archeology Global and Planetary Change journal-article 2009 crsagepubl https://doi.org/10.1177/0959683609105296 2022-07-03T16:08:48Z Two 2 m long ice cores (BA and BB) were extracted from the floor ice of Borştig Ice Cave in December 2005. Below a co-existing dust horizon (~13 cm underneath the 10 December 2005 ice surface) neither core presented any sign of hiatus, so the ice deposition is considered to be continuous. Tritium concentration of 94 samples from a 1.85 m long ice section were analysed by liquid scintillation counting technique. Samples from the lower 0.33 m of the sequence did not contain tritium above the critical level (7.2 TU). The highest value of tritium content (166.4±4.0 TU) was found at ~96 cm below the surface. This salient value is considered to be synchronous with the climax of tritium concentration in the Northern Hemisphere's atmospheric precipitation (1963). Beside this characteristic global radiochemical marker event, minor events were also detected, and dated (ie, 1954, 1958 and 1975) by corresponding peaks in the tritium concentration record of BB ice core to peaks of an estimation of tritium activity of past precipitation at Borştig Ice Cave location. The estimation was based on a data set from four nearby stations of the Global Network of Isotopes in Precipitation. The highest annual accumulation rate (6.74 cm/yr) was between 1958 and 1963 and gradually decreased to 0.54 cm/yr for the recent decades. The mean ice accumulation rate was 4.34 cm/yr over the 1954—1986 period. The estimated age at the bottom of the 21 m thick ice block assuming constant accumulation is roughly 500 years. Article in Journal/Newspaper ice core SAGE Publications (via Crossref) The Holocene 19 5 729 736
institution Open Polar
collection SAGE Publications (via Crossref)
op_collection_id crsagepubl
language English
topic Paleontology
Earth-Surface Processes
Ecology
Archeology
Global and Planetary Change
spellingShingle Paleontology
Earth-Surface Processes
Ecology
Archeology
Global and Planetary Change
Kern, Zoltán
Molnár, Mihály
Svingor, Éva
Perşoiu, Aurel
Nagy, Balázs
High-resolution, well-preserved tritium record in the ice of Bortig Ice Cave, Bihor Mountains, Romania
topic_facet Paleontology
Earth-Surface Processes
Ecology
Archeology
Global and Planetary Change
description Two 2 m long ice cores (BA and BB) were extracted from the floor ice of Borştig Ice Cave in December 2005. Below a co-existing dust horizon (~13 cm underneath the 10 December 2005 ice surface) neither core presented any sign of hiatus, so the ice deposition is considered to be continuous. Tritium concentration of 94 samples from a 1.85 m long ice section were analysed by liquid scintillation counting technique. Samples from the lower 0.33 m of the sequence did not contain tritium above the critical level (7.2 TU). The highest value of tritium content (166.4±4.0 TU) was found at ~96 cm below the surface. This salient value is considered to be synchronous with the climax of tritium concentration in the Northern Hemisphere's atmospheric precipitation (1963). Beside this characteristic global radiochemical marker event, minor events were also detected, and dated (ie, 1954, 1958 and 1975) by corresponding peaks in the tritium concentration record of BB ice core to peaks of an estimation of tritium activity of past precipitation at Borştig Ice Cave location. The estimation was based on a data set from four nearby stations of the Global Network of Isotopes in Precipitation. The highest annual accumulation rate (6.74 cm/yr) was between 1958 and 1963 and gradually decreased to 0.54 cm/yr for the recent decades. The mean ice accumulation rate was 4.34 cm/yr over the 1954—1986 period. The estimated age at the bottom of the 21 m thick ice block assuming constant accumulation is roughly 500 years.
format Article in Journal/Newspaper
author Kern, Zoltán
Molnár, Mihály
Svingor, Éva
Perşoiu, Aurel
Nagy, Balázs
author_facet Kern, Zoltán
Molnár, Mihály
Svingor, Éva
Perşoiu, Aurel
Nagy, Balázs
author_sort Kern, Zoltán
title High-resolution, well-preserved tritium record in the ice of Bortig Ice Cave, Bihor Mountains, Romania
title_short High-resolution, well-preserved tritium record in the ice of Bortig Ice Cave, Bihor Mountains, Romania
title_full High-resolution, well-preserved tritium record in the ice of Bortig Ice Cave, Bihor Mountains, Romania
title_fullStr High-resolution, well-preserved tritium record in the ice of Bortig Ice Cave, Bihor Mountains, Romania
title_full_unstemmed High-resolution, well-preserved tritium record in the ice of Bortig Ice Cave, Bihor Mountains, Romania
title_sort high-resolution, well-preserved tritium record in the ice of bortig ice cave, bihor mountains, romania
publisher SAGE Publications
publishDate 2009
url http://dx.doi.org/10.1177/0959683609105296
http://journals.sagepub.com/doi/pdf/10.1177/0959683609105296
genre ice core
genre_facet ice core
op_source The Holocene
volume 19, issue 5, page 729-736
ISSN 0959-6836 1477-0911
op_rights http://journals.sagepub.com/page/policies/text-and-data-mining-license
op_doi https://doi.org/10.1177/0959683609105296
container_title The Holocene
container_volume 19
container_issue 5
container_start_page 729
op_container_end_page 736
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