Production-related 14C variations - Can they explain the main changes in the atmospheric 14C concentration during the last 50 kyr?

The elevated D14C levels during the last ice age show a good correlation with the strong climatic changes during the last deglaciation. However, carbon cycle models fail to explain the major part of the increased 14C concentrations in the atmosphere during the last ice age (e.g. Köhler et al., 2006)...

Full description

Bibliographic Details
Main Authors: Muscheler, R., Köhler, Peter, Svensson, A., Beer, J.
Format: Conference Object
Language:unknown
Published: 2006
Subjects:
Online Access:https://epic.awi.de/id/eprint/15593/
https://hdl.handle.net/10013/epic.25709
id ftawi:oai:epic.awi.de:15593
record_format openpolar
spelling ftawi:oai:epic.awi.de:15593 2023-05-15T16:28:27+02:00 Production-related 14C variations - Can they explain the main changes in the atmospheric 14C concentration during the last 50 kyr? Muscheler, R. Köhler, Peter Svensson, A. Beer, J. 2006 https://epic.awi.de/id/eprint/15593/ https://hdl.handle.net/10013/epic.25709 unknown Muscheler, R. , Köhler, P. orcid:0000-0003-0904-8484 , Svensson, A. and Beer, J. (2006) Production-related 14C variations - Can they explain the main changes in the atmospheric 14C concentration during the last 50 kyr? , Eos Trans. AGU, 87(52), Fall Meet. Suppl., Abstract PP43C-04, 2006. 11-15 Dec 2006, San Francisco, USA. . hdl:10013/epic.25709 EPIC3Eos Trans. AGU, 87(52), Fall Meet. Suppl., Abstract PP43C-04, 2006. 11-15 Dec 2006, San Francisco, USA. Conference notRev 2006 ftawi 2021-12-24T15:31:22Z The elevated D14C levels during the last ice age show a good correlation with the strong climatic changes during the last deglaciation. However, carbon cycle models fail to explain the major part of the increased 14C concentrations in the atmosphere during the last ice age (e.g. Köhler et al., 2006).The geomagnetic modulation of the 14C production rate is partly responsible for the elevated 14C level during the last 50 kyr. However, the errors of the geomagnetic field reconstructions are large. In addition, geomagnetic field records that can well explain the elevated D14C during the last ice age don't yield a good explanation for D14C during the climatically stable Holocene period. Alternative estimates of the 14C production rate based on 10Be from polar ice cores can explain D14C during the Holocene very well. However, the differences to D14C during MIS2 and MIS3 seem too large to be explained by carbon cycle changes alone.We will discuss potential causes for the disagreement between measured and modeled D14C during the last 50 kyr. In the view of the new dating of the Greenland ice cores (Svensson et al., QSR2006) we will reassess the reliability of the 10Be record as a proxy for the global changes in the 10Be and 14C production rates and discuss the implications for the Radiocarbon-based reconstructions of past ocean circulation.References:Köhler, P., Muscheler, R., Fischer, H. (2006). A model-based interpretation of low frequency changes in the carbon cycle during the last 120,000 years and its implications for the reconstruction of atmospheric D14C, Geochemistry Geophysics Geosystems, doi:10.1029/2005GC001228, in press.Svensson et al. (2006). The Greenland Ice Core Chronology 2005, 15-42 ka.Part 2: Comparison to other records, Quaternary Science Reviews 2006. in press. Conference Object Greenland Greenland ice core Greenland ice cores ice core Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) Greenland
institution Open Polar
collection Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center)
op_collection_id ftawi
language unknown
description The elevated D14C levels during the last ice age show a good correlation with the strong climatic changes during the last deglaciation. However, carbon cycle models fail to explain the major part of the increased 14C concentrations in the atmosphere during the last ice age (e.g. Köhler et al., 2006).The geomagnetic modulation of the 14C production rate is partly responsible for the elevated 14C level during the last 50 kyr. However, the errors of the geomagnetic field reconstructions are large. In addition, geomagnetic field records that can well explain the elevated D14C during the last ice age don't yield a good explanation for D14C during the climatically stable Holocene period. Alternative estimates of the 14C production rate based on 10Be from polar ice cores can explain D14C during the Holocene very well. However, the differences to D14C during MIS2 and MIS3 seem too large to be explained by carbon cycle changes alone.We will discuss potential causes for the disagreement between measured and modeled D14C during the last 50 kyr. In the view of the new dating of the Greenland ice cores (Svensson et al., QSR2006) we will reassess the reliability of the 10Be record as a proxy for the global changes in the 10Be and 14C production rates and discuss the implications for the Radiocarbon-based reconstructions of past ocean circulation.References:Köhler, P., Muscheler, R., Fischer, H. (2006). A model-based interpretation of low frequency changes in the carbon cycle during the last 120,000 years and its implications for the reconstruction of atmospheric D14C, Geochemistry Geophysics Geosystems, doi:10.1029/2005GC001228, in press.Svensson et al. (2006). The Greenland Ice Core Chronology 2005, 15-42 ka.Part 2: Comparison to other records, Quaternary Science Reviews 2006. in press.
format Conference Object
author Muscheler, R.
Köhler, Peter
Svensson, A.
Beer, J.
spellingShingle Muscheler, R.
Köhler, Peter
Svensson, A.
Beer, J.
Production-related 14C variations - Can they explain the main changes in the atmospheric 14C concentration during the last 50 kyr?
author_facet Muscheler, R.
Köhler, Peter
Svensson, A.
Beer, J.
author_sort Muscheler, R.
title Production-related 14C variations - Can they explain the main changes in the atmospheric 14C concentration during the last 50 kyr?
title_short Production-related 14C variations - Can they explain the main changes in the atmospheric 14C concentration during the last 50 kyr?
title_full Production-related 14C variations - Can they explain the main changes in the atmospheric 14C concentration during the last 50 kyr?
title_fullStr Production-related 14C variations - Can they explain the main changes in the atmospheric 14C concentration during the last 50 kyr?
title_full_unstemmed Production-related 14C variations - Can they explain the main changes in the atmospheric 14C concentration during the last 50 kyr?
title_sort production-related 14c variations - can they explain the main changes in the atmospheric 14c concentration during the last 50 kyr?
publishDate 2006
url https://epic.awi.de/id/eprint/15593/
https://hdl.handle.net/10013/epic.25709
geographic Greenland
geographic_facet Greenland
genre Greenland
Greenland ice core
Greenland ice cores
ice core
genre_facet Greenland
Greenland ice core
Greenland ice cores
ice core
op_source EPIC3Eos Trans. AGU, 87(52), Fall Meet. Suppl., Abstract PP43C-04, 2006. 11-15 Dec 2006, San Francisco, USA.
op_relation Muscheler, R. , Köhler, P. orcid:0000-0003-0904-8484 , Svensson, A. and Beer, J. (2006) Production-related 14C variations - Can they explain the main changes in the atmospheric 14C concentration during the last 50 kyr? , Eos Trans. AGU, 87(52), Fall Meet. Suppl., Abstract PP43C-04, 2006. 11-15 Dec 2006, San Francisco, USA. . hdl:10013/epic.25709
_version_ 1766018110967513088