Exact dating of the Meghalayan lower boundary based on high-latitude tree-ring isotope chronology
Subdivision of the Holocene Series/Epoch into the Greenlandian, Northgrippian and Meghalayan Stages/ Ages has recently been ratified based on stable isotope records from ice-core and speleothem archives. The base of the most recent chronostratigraphic unit, corresponding to the Northgrippian Meghala...
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ftunivhelsihelda:oai:helda.helsinki.fi:10138/330959 2024-01-07T09:43:56+01:00 Exact dating of the Meghalayan lower boundary based on high-latitude tree-ring isotope chronology Helama, Samuli Oinonen, Markku Natural Sciences Unit Finnish Museum of Natural History 2021-06-14T22:10:45Z 7 application/pdf http://hdl.handle.net/10138/330959 eng eng Elsevier Scientific Publ. Co 10.1016/j.quascirev.2019.04.013 Unknown funder Helama , S & Oinonen , M 2019 , ' Exact dating of the Meghalayan lower boundary based on high-latitude tree-ring isotope chronology ' , Quaternary Science Reviews , vol. 214 , pp. 178-184 . https://doi.org/10.1016/j.quascirev.2019.04.013 ORCID: /0000-0002-0881-7643/work/58264534 0d41ef0c-e5b9-4122-9b13-7e1455dea214 http://hdl.handle.net/10138/330959 000471738800011 cc_by_nc_nd openAccess info:eu-repo/semantics/openAccess 1171 Geosciences Article acceptedVersion 2021 ftunivhelsihelda 2023-12-14T00:10:03Z Subdivision of the Holocene Series/Epoch into the Greenlandian, Northgrippian and Meghalayan Stages/ Ages has recently been ratified based on stable isotope records from ice-core and speleothem archives. The base of the most recent chronostratigraphic unit, corresponding to the Northgrippian Meghalayan boundary, coincides with the '4.2 ka event' recognised as a low-latitude drought anomaly. The Global Stratotype Section and Point (GSSP) for the boundary, the oxygen isotope record from the Mawmluh Cave speleothem (India), demonstrates this event with markedly weakened Asian summer monsoon. Here we contribute to the assessments of the geological time scale and the global characteristics of this event by detailing an isotopic excursion in tree-ring carbon isotopes from high-latitude/subarctic Europe. The delta C-13 chronology demonstrates extremely overcast (wet) conditions, especially between 2190 and 2100 BCE, with anomalous conditions sustaining until 1990 BCE. In addition to demonstrating its exact dating and duration, the delta C-13 data also illustrate the two-stage nature of the event and highlight the greater magnitude of the earlier stage. This reinforces the characterisation of this 'Meghalayan anomaly' in the context of other proxy-sites around the world. The North Atlantic forcing, previously associated with weakened Asian summer monsoon, accords with the suggested roles of North Atlantic Oscillation and/or southwards shift of Inter-Tropical Convergence Zone in producing the hydroclimatic anomaly. In fact, it would be clarifying to separate the hydroclimatic 'Meghalayan anomaly' from the broadly cited and potentially longer lasting '4.2 ka event', to analyse their respective forcing mechanisms. We conclude by dating the Meghalayan lower boundary to 2190 BCE. (C) 2019 Elsevier Ltd. All rights reserved. Peer reviewed Article in Journal/Newspaper ice core North Atlantic North Atlantic oscillation Subarctic HELDA – University of Helsinki Open Repository Quaternary Science Reviews 214 178 184 |
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ftunivhelsihelda |
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English |
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1171 Geosciences |
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1171 Geosciences Helama, Samuli Oinonen, Markku Exact dating of the Meghalayan lower boundary based on high-latitude tree-ring isotope chronology |
topic_facet |
1171 Geosciences |
description |
Subdivision of the Holocene Series/Epoch into the Greenlandian, Northgrippian and Meghalayan Stages/ Ages has recently been ratified based on stable isotope records from ice-core and speleothem archives. The base of the most recent chronostratigraphic unit, corresponding to the Northgrippian Meghalayan boundary, coincides with the '4.2 ka event' recognised as a low-latitude drought anomaly. The Global Stratotype Section and Point (GSSP) for the boundary, the oxygen isotope record from the Mawmluh Cave speleothem (India), demonstrates this event with markedly weakened Asian summer monsoon. Here we contribute to the assessments of the geological time scale and the global characteristics of this event by detailing an isotopic excursion in tree-ring carbon isotopes from high-latitude/subarctic Europe. The delta C-13 chronology demonstrates extremely overcast (wet) conditions, especially between 2190 and 2100 BCE, with anomalous conditions sustaining until 1990 BCE. In addition to demonstrating its exact dating and duration, the delta C-13 data also illustrate the two-stage nature of the event and highlight the greater magnitude of the earlier stage. This reinforces the characterisation of this 'Meghalayan anomaly' in the context of other proxy-sites around the world. The North Atlantic forcing, previously associated with weakened Asian summer monsoon, accords with the suggested roles of North Atlantic Oscillation and/or southwards shift of Inter-Tropical Convergence Zone in producing the hydroclimatic anomaly. In fact, it would be clarifying to separate the hydroclimatic 'Meghalayan anomaly' from the broadly cited and potentially longer lasting '4.2 ka event', to analyse their respective forcing mechanisms. We conclude by dating the Meghalayan lower boundary to 2190 BCE. (C) 2019 Elsevier Ltd. All rights reserved. Peer reviewed |
author2 |
Natural Sciences Unit Finnish Museum of Natural History |
format |
Article in Journal/Newspaper |
author |
Helama, Samuli Oinonen, Markku |
author_facet |
Helama, Samuli Oinonen, Markku |
author_sort |
Helama, Samuli |
title |
Exact dating of the Meghalayan lower boundary based on high-latitude tree-ring isotope chronology |
title_short |
Exact dating of the Meghalayan lower boundary based on high-latitude tree-ring isotope chronology |
title_full |
Exact dating of the Meghalayan lower boundary based on high-latitude tree-ring isotope chronology |
title_fullStr |
Exact dating of the Meghalayan lower boundary based on high-latitude tree-ring isotope chronology |
title_full_unstemmed |
Exact dating of the Meghalayan lower boundary based on high-latitude tree-ring isotope chronology |
title_sort |
exact dating of the meghalayan lower boundary based on high-latitude tree-ring isotope chronology |
publisher |
Elsevier Scientific Publ. Co |
publishDate |
2021 |
url |
http://hdl.handle.net/10138/330959 |
genre |
ice core North Atlantic North Atlantic oscillation Subarctic |
genre_facet |
ice core North Atlantic North Atlantic oscillation Subarctic |
op_relation |
10.1016/j.quascirev.2019.04.013 Unknown funder Helama , S & Oinonen , M 2019 , ' Exact dating of the Meghalayan lower boundary based on high-latitude tree-ring isotope chronology ' , Quaternary Science Reviews , vol. 214 , pp. 178-184 . https://doi.org/10.1016/j.quascirev.2019.04.013 ORCID: /0000-0002-0881-7643/work/58264534 0d41ef0c-e5b9-4122-9b13-7e1455dea214 http://hdl.handle.net/10138/330959 000471738800011 |
op_rights |
cc_by_nc_nd openAccess info:eu-repo/semantics/openAccess |
container_title |
Quaternary Science Reviews |
container_volume |
214 |
container_start_page |
178 |
op_container_end_page |
184 |
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1787425224440938496 |