Exact dating of the Meghalayan lower boundary based on high-latitude tree-ring isotope chronology

Research output: Contribution to journalArticleScientificpeer-review

Abstract

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.

Original languageEnglish
JournalQuaternary Science Reviews
Volume214
Pages (from-to)178-184
Number of pages7
ISSN0277-3791
DOIs
Publication statusPublished - 15 Jun 2019
MoE publication typeA1 Journal article-refereed

Fields of Science

  • 1171 Geosciences

Cite this

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title = "Exact dating of the Meghalayan lower boundary based on high-latitude tree-ring isotope chronology",
abstract = "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.",
keywords = "1171 Geosciences",
author = "Samuli Helama and Markku Oinonen",
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Exact dating of the Meghalayan lower boundary based on high-latitude tree-ring isotope chronology. / Helama, Samuli; Oinonen, Markku.

In: Quaternary Science Reviews, Vol. 214, 15.06.2019, p. 178-184.

Research output: Contribution to journalArticleScientificpeer-review

TY - JOUR

T1 - Exact dating of the Meghalayan lower boundary based on high-latitude tree-ring isotope chronology

AU - Helama, Samuli

AU - Oinonen, Markku

PY - 2019/6/15

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N2 - 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.

AB - 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.

KW - 1171 Geosciences

U2 - 10.1016/j.quascirev.2019.04.013

DO - 10.1016/j.quascirev.2019.04.013

M3 - Article

VL - 214

SP - 178

EP - 184

JO - Quaternary Science Reviews

JF - Quaternary Science Reviews

SN - 0277-3791

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