Radiocarbon Dating Organic Detritus: Implications for Studying Ice Sheet Dynamics

We present here a description of the 14 C dating method used at the Institute of Geology, Estonian Academy of Science. We discuss results of geochronological studies of several stratigraphic sections, from which we estimate the age of the Late Weichselian (Late Valdaian) glacial maximum. 14 C and pa...

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Published in:Radiocarbon
Main Authors: Punning, Jaan-Mati, Rajamäe, Raivo
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1993
Subjects:
Online Access:http://dx.doi.org/10.1017/s0033822200060471
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0033822200060471
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spelling crcambridgeupr:10.1017/s0033822200060471 2024-03-03T08:45:25+00:00 Radiocarbon Dating Organic Detritus: Implications for Studying Ice Sheet Dynamics Punning, Jaan-Mati Rajamäe, Raivo 1993 http://dx.doi.org/10.1017/s0033822200060471 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0033822200060471 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Radiocarbon volume 35, issue 3, page 449-455 ISSN 0033-8222 1945-5755 General Earth and Planetary Sciences Archeology journal-article 1993 crcambridgeupr https://doi.org/10.1017/s0033822200060471 2024-02-08T08:35:05Z We present here a description of the 14 C dating method used at the Institute of Geology, Estonian Academy of Science. We discuss results of geochronological studies of several stratigraphic sections, from which we estimate the age of the Late Weichselian (Late Valdaian) glacial maximum. 14 C and paleobotanical data indicate that biodetrital materials comprise organic debris from various sources and suggest only a maximum age of investigated strata (16,000 BP). Article in Journal/Newspaper Ice Sheet Cambridge University Press Radiocarbon 35 3 449 455
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic General Earth and Planetary Sciences
Archeology
spellingShingle General Earth and Planetary Sciences
Archeology
Punning, Jaan-Mati
Rajamäe, Raivo
Radiocarbon Dating Organic Detritus: Implications for Studying Ice Sheet Dynamics
topic_facet General Earth and Planetary Sciences
Archeology
description We present here a description of the 14 C dating method used at the Institute of Geology, Estonian Academy of Science. We discuss results of geochronological studies of several stratigraphic sections, from which we estimate the age of the Late Weichselian (Late Valdaian) glacial maximum. 14 C and paleobotanical data indicate that biodetrital materials comprise organic debris from various sources and suggest only a maximum age of investigated strata (16,000 BP).
format Article in Journal/Newspaper
author Punning, Jaan-Mati
Rajamäe, Raivo
author_facet Punning, Jaan-Mati
Rajamäe, Raivo
author_sort Punning, Jaan-Mati
title Radiocarbon Dating Organic Detritus: Implications for Studying Ice Sheet Dynamics
title_short Radiocarbon Dating Organic Detritus: Implications for Studying Ice Sheet Dynamics
title_full Radiocarbon Dating Organic Detritus: Implications for Studying Ice Sheet Dynamics
title_fullStr Radiocarbon Dating Organic Detritus: Implications for Studying Ice Sheet Dynamics
title_full_unstemmed Radiocarbon Dating Organic Detritus: Implications for Studying Ice Sheet Dynamics
title_sort radiocarbon dating organic detritus: implications for studying ice sheet dynamics
publisher Cambridge University Press (CUP)
publishDate 1993
url http://dx.doi.org/10.1017/s0033822200060471
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0033822200060471
genre Ice Sheet
genre_facet Ice Sheet
op_source Radiocarbon
volume 35, issue 3, page 449-455
ISSN 0033-8222 1945-5755
op_rights https://www.cambridge.org/core/terms
op_doi https://doi.org/10.1017/s0033822200060471
container_title Radiocarbon
container_volume 35
container_issue 3
container_start_page 449
op_container_end_page 455
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