Dating Amber: Review and Perspective

Amber is a fossilized tree resin that ranges in age from the Carboniferous to the Cenozoic. It occurs globally from the Arctic to Antarctica. As the resin petrifies and turns into amber, it can enclose and preserve other materials. Amber with inclusions can help reconstruct past biodiversity and eco...

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Published in:Minerals
Main Authors: Su-Chin Chang, Yuling Li, Daran Zheng
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2023
Subjects:
Online Access:https://doi.org/10.3390/min13070948
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spelling ftmdpi:oai:mdpi.com:/2075-163X/13/7/948/ 2023-08-20T04:00:20+02:00 Dating Amber: Review and Perspective Su-Chin Chang Yuling Li Daran Zheng agris 2023-07-15 application/pdf https://doi.org/10.3390/min13070948 EN eng Multidisciplinary Digital Publishing Institute Mineral Geochemistry and Geochronology https://dx.doi.org/10.3390/min13070948 https://creativecommons.org/licenses/by/4.0/ Minerals; Volume 13; Issue 7; Pages: 948 U–Pb geochronology 40 Ar/ 39 Ar dating amber evolution fossils Text 2023 ftmdpi https://doi.org/10.3390/min13070948 2023-08-01T10:53:02Z Amber is a fossilized tree resin that ranges in age from the Carboniferous to the Cenozoic. It occurs globally from the Arctic to Antarctica. As the resin petrifies and turns into amber, it can enclose and preserve other materials. Amber with inclusions can help reconstruct past biodiversity and ecosystems. Some amber contains fossils representing the oldest and most detailed records of critical evolutionary traits or markers. Inclusions can even capture behavioral indicators previously only observed in extant organisms. Evidence of insect pollination of flowering plants and dragonfly mating behavior appears in amber, as does the morphological specialization of insects, indicating sociality and social parasitism. Dating amber deposits can help calibrate evolutionary events and inform reconstructions of past ecosystems. While the direct dating of amber remains impossible, age constraints on most amber deposits are based on correlations or relative dating, methods that come with significant uncertainties. This study discusses two cases using 40Ar/39Ar and U–Pb geochronologic methods to constrain the ages of amber deposits in China and the paleo-ecosystems they record. This paper also summarizes how radio-isotopic dating and other techniques combined with the analysis of inclusions in amber can help elucidate biogeography and the dynamic relationship between life and the physical environment. Text Antarc* Antarctica Arctic MDPI Open Access Publishing Arctic Minerals 13 7 948
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic U–Pb geochronology
40 Ar/ 39 Ar dating
amber
evolution
fossils
spellingShingle U–Pb geochronology
40 Ar/ 39 Ar dating
amber
evolution
fossils
Su-Chin Chang
Yuling Li
Daran Zheng
Dating Amber: Review and Perspective
topic_facet U–Pb geochronology
40 Ar/ 39 Ar dating
amber
evolution
fossils
description Amber is a fossilized tree resin that ranges in age from the Carboniferous to the Cenozoic. It occurs globally from the Arctic to Antarctica. As the resin petrifies and turns into amber, it can enclose and preserve other materials. Amber with inclusions can help reconstruct past biodiversity and ecosystems. Some amber contains fossils representing the oldest and most detailed records of critical evolutionary traits or markers. Inclusions can even capture behavioral indicators previously only observed in extant organisms. Evidence of insect pollination of flowering plants and dragonfly mating behavior appears in amber, as does the morphological specialization of insects, indicating sociality and social parasitism. Dating amber deposits can help calibrate evolutionary events and inform reconstructions of past ecosystems. While the direct dating of amber remains impossible, age constraints on most amber deposits are based on correlations or relative dating, methods that come with significant uncertainties. This study discusses two cases using 40Ar/39Ar and U–Pb geochronologic methods to constrain the ages of amber deposits in China and the paleo-ecosystems they record. This paper also summarizes how radio-isotopic dating and other techniques combined with the analysis of inclusions in amber can help elucidate biogeography and the dynamic relationship between life and the physical environment.
format Text
author Su-Chin Chang
Yuling Li
Daran Zheng
author_facet Su-Chin Chang
Yuling Li
Daran Zheng
author_sort Su-Chin Chang
title Dating Amber: Review and Perspective
title_short Dating Amber: Review and Perspective
title_full Dating Amber: Review and Perspective
title_fullStr Dating Amber: Review and Perspective
title_full_unstemmed Dating Amber: Review and Perspective
title_sort dating amber: review and perspective
publisher Multidisciplinary Digital Publishing Institute
publishDate 2023
url https://doi.org/10.3390/min13070948
op_coverage agris
geographic Arctic
geographic_facet Arctic
genre Antarc*
Antarctica
Arctic
genre_facet Antarc*
Antarctica
Arctic
op_source Minerals; Volume 13; Issue 7; Pages: 948
op_relation Mineral Geochemistry and Geochronology
https://dx.doi.org/10.3390/min13070948
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/min13070948
container_title Minerals
container_volume 13
container_issue 7
container_start_page 948
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