Global glaciations and atmospheric change at ca. 2.3 Ga

This paper compiles lithostratigraphic and geochronological data obtained for the Palaeoproterozoic glacial diamictite-bearing successions, and thereby provides insights into understanding the geological processes causing the Huronian Glaciation Event. The majority of evidence for appearances of thi...

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Main Authors: Haoshu Tang, Yanjing Chen
Format: Article
Language:English
Published: Elsevier 2013-09-01
Series:Geoscience Frontiers
Subjects:
Online Access:http://www.sciencedirect.com/science/article/pii/S1674987113000297
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author Haoshu Tang
Yanjing Chen
author_facet Haoshu Tang
Yanjing Chen
author_sort Haoshu Tang
collection DOAJ
description This paper compiles lithostratigraphic and geochronological data obtained for the Palaeoproterozoic glacial diamictite-bearing successions, and thereby provides insights into understanding the geological processes causing the Huronian Glaciation Event. The majority of evidence for appearances of this glaciation event can be related to the Kenorland supercontinent breakup, allied to significant atmospheric change, as well as blooms of biogeochemical oxygenic photosynthesis. In this paper, the Huronian Glaciation Event is constrained to have occurred synchronously during 2.29–2.25 Ga, accompanied by dramatic environmental changes characteristic of the Great Oxidation Event which includes the pre-2.3 Ga hydrosphere oxidation and the post-2.3 Ga atmosphere oxygenation.
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spelling doaj.art-21bb5ee924844c419a109b72b30608bf2023-08-02T02:20:50ZengElsevierGeoscience Frontiers1674-98712013-09-014558359610.1016/j.gsf.2013.02.003Global glaciations and atmospheric change at ca. 2.3 GaHaoshu Tang0Yanjing Chen1State Key Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, 46 Guanshui Road, Guiyang 550002, ChinaKey Laboratory of Orogen and Crust Evolution, Peking University, Beijing 100871, ChinaThis paper compiles lithostratigraphic and geochronological data obtained for the Palaeoproterozoic glacial diamictite-bearing successions, and thereby provides insights into understanding the geological processes causing the Huronian Glaciation Event. The majority of evidence for appearances of this glaciation event can be related to the Kenorland supercontinent breakup, allied to significant atmospheric change, as well as blooms of biogeochemical oxygenic photosynthesis. In this paper, the Huronian Glaciation Event is constrained to have occurred synchronously during 2.29–2.25 Ga, accompanied by dramatic environmental changes characteristic of the Great Oxidation Event which includes the pre-2.3 Ga hydrosphere oxidation and the post-2.3 Ga atmosphere oxygenation.http://www.sciencedirect.com/science/article/pii/S1674987113000297Global glaciationEarth's environmental changeGreat Oxidation EventLithostratigraphyGeochronology
spellingShingle Haoshu Tang
Yanjing Chen
Global glaciations and atmospheric change at ca. 2.3 Ga
Geoscience Frontiers
Global glaciation
Earth's environmental change
Great Oxidation Event
Lithostratigraphy
Geochronology
title Global glaciations and atmospheric change at ca. 2.3 Ga
title_full Global glaciations and atmospheric change at ca. 2.3 Ga
title_fullStr Global glaciations and atmospheric change at ca. 2.3 Ga
title_full_unstemmed Global glaciations and atmospheric change at ca. 2.3 Ga
title_short Global glaciations and atmospheric change at ca. 2.3 Ga
title_sort global glaciations and atmospheric change at ca 2 3 ga
topic Global glaciation
Earth's environmental change
Great Oxidation Event
Lithostratigraphy
Geochronology
url http://www.sciencedirect.com/science/article/pii/S1674987113000297
work_keys_str_mv AT haoshutang globalglaciationsandatmosphericchangeatca23ga
AT yanjingchen globalglaciationsandatmosphericchangeatca23ga