Archaeological implications of a widespread 13th Century tephra marker across the central Indonesian Archipelago

Despite the occurrence of exceptionally large eruptions in the Indonesian Archipelago in recent historic times (i.e. Krakatoa 1883, Tambora 1815), no historic tephra beds have been widely identified in the terrestrial realm that could facilitate the correlation of equivalent aged sequences and/or ar...

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Main Authors: Alloway, Brent V, Andreastuti, Supriyati, Setiawan, Ruly, Miksic, John, Hua, Quan
Format: Article in Journal/Newspaper
Language:unknown
Published: Research Online 2017
Subjects:
Online Access:https://ro.uow.edu.au/smhpapers/4262
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spelling ftunivwollongong:oai:ro.uow.edu.au:smhpapers-5286 2023-05-15T13:58:42+02:00 Archaeological implications of a widespread 13th Century tephra marker across the central Indonesian Archipelago Alloway, Brent V Andreastuti, Supriyati Setiawan, Ruly Miksic, John Hua, Quan 2017-01-01T08:00:00Z https://ro.uow.edu.au/smhpapers/4262 unknown Research Online https://ro.uow.edu.au/smhpapers/4262 Faculty of Science, Medicine and Health - Papers: part A article 2017 ftunivwollongong 2020-02-25T11:33:28Z Despite the occurrence of exceptionally large eruptions in the Indonesian Archipelago in recent historic times (i.e. Krakatoa 1883, Tambora 1815), no historic tephra beds have been widely identified in the terrestrial realm that could facilitate the correlation of equivalent aged sequences and/or archaeological remains. This study has identified one such tephra bed of 13th Century age that can be correlated throughout central-east Java and now can be unequivocally correlated with the Samalas 1257 A.D. tephra recently described from Lombok. The occurrence of this historic tephra marker extending ¿650 km west from its eruptive source provides the first opportunity to effect inter-regional correlation over large swathes of central Indonesia. It remains entirely conceivable that in the aftermath of this exceptionally large eruptive event there was considerable westward disruption to subsistence agriculture and trade, food shortages and famine, dislocation of affected populations and socio-political unrest on a scale that equalled or exceeded the catastrophic effects documented from the more recent Tambora 1815 A.D. eruption. Indeed the effects of this mid-13th Century eruption can be registered globally in a variety of records from Antarctica, Europe, Middle East and the Americas. Unfortunately, archaeological evidence indicating such disruption in mid-13th Century Indonesia is yet to be deciphered from the so-far sparse accounts and inscriptions of that time. However, this paucity of evidence does not diminish the utility of this widespread tephra bed as a unique chronostratigraphic marker for archaeological studies across large areas of central Indonesia. Article in Journal/Newspaper Antarc* Antarctica University of Wollongong, Australia: Research Online
institution Open Polar
collection University of Wollongong, Australia: Research Online
op_collection_id ftunivwollongong
language unknown
description Despite the occurrence of exceptionally large eruptions in the Indonesian Archipelago in recent historic times (i.e. Krakatoa 1883, Tambora 1815), no historic tephra beds have been widely identified in the terrestrial realm that could facilitate the correlation of equivalent aged sequences and/or archaeological remains. This study has identified one such tephra bed of 13th Century age that can be correlated throughout central-east Java and now can be unequivocally correlated with the Samalas 1257 A.D. tephra recently described from Lombok. The occurrence of this historic tephra marker extending ¿650 km west from its eruptive source provides the first opportunity to effect inter-regional correlation over large swathes of central Indonesia. It remains entirely conceivable that in the aftermath of this exceptionally large eruptive event there was considerable westward disruption to subsistence agriculture and trade, food shortages and famine, dislocation of affected populations and socio-political unrest on a scale that equalled or exceeded the catastrophic effects documented from the more recent Tambora 1815 A.D. eruption. Indeed the effects of this mid-13th Century eruption can be registered globally in a variety of records from Antarctica, Europe, Middle East and the Americas. Unfortunately, archaeological evidence indicating such disruption in mid-13th Century Indonesia is yet to be deciphered from the so-far sparse accounts and inscriptions of that time. However, this paucity of evidence does not diminish the utility of this widespread tephra bed as a unique chronostratigraphic marker for archaeological studies across large areas of central Indonesia.
format Article in Journal/Newspaper
author Alloway, Brent V
Andreastuti, Supriyati
Setiawan, Ruly
Miksic, John
Hua, Quan
spellingShingle Alloway, Brent V
Andreastuti, Supriyati
Setiawan, Ruly
Miksic, John
Hua, Quan
Archaeological implications of a widespread 13th Century tephra marker across the central Indonesian Archipelago
author_facet Alloway, Brent V
Andreastuti, Supriyati
Setiawan, Ruly
Miksic, John
Hua, Quan
author_sort Alloway, Brent V
title Archaeological implications of a widespread 13th Century tephra marker across the central Indonesian Archipelago
title_short Archaeological implications of a widespread 13th Century tephra marker across the central Indonesian Archipelago
title_full Archaeological implications of a widespread 13th Century tephra marker across the central Indonesian Archipelago
title_fullStr Archaeological implications of a widespread 13th Century tephra marker across the central Indonesian Archipelago
title_full_unstemmed Archaeological implications of a widespread 13th Century tephra marker across the central Indonesian Archipelago
title_sort archaeological implications of a widespread 13th century tephra marker across the central indonesian archipelago
publisher Research Online
publishDate 2017
url https://ro.uow.edu.au/smhpapers/4262
genre Antarc*
Antarctica
genre_facet Antarc*
Antarctica
op_source Faculty of Science, Medicine and Health - Papers: part A
op_relation https://ro.uow.edu.au/smhpapers/4262
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