Palynofacies patterns of the Highveld coal deposits (Karoo Basin, South Africa): Clues to reconstruction of palaeoenvironment and palaeoclimate

The early Permian represents a crucial period of climate change in Gondwana. This climate signature is captured in the palynological record that represents the floral assemblage of the region. Palynofacies analysis of the No. 2 Coal Seam of the Highveld Coalfield provides a high-resolution picture o...

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Main Authors: Wheeler Alexander, Götz Annette E.
Format: Article
Language:English
Published: W. Szafer Institute of Botany, Polish Academy of Sciences 2016-06-01
Series:Acta Palaeobotanica
Subjects:
Online Access:http://www.degruyter.com/view/j/acpa.2016.56.issue-1/acpa-2016-0004/acpa-2016-0004.xml?format=INT
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author Wheeler Alexander
Götz Annette E.
author_facet Wheeler Alexander
Götz Annette E.
author_sort Wheeler Alexander
collection DOAJ
description The early Permian represents a crucial period of climate change in Gondwana. This climate signature is captured in the palynological record that represents the floral assemblage of the region. Palynofacies analysis of the No. 2 Coal Seam of the Highveld Coalfield provides a high-resolution picture of this climatic shift, as well as detailing the vegetation patterns and local environments. Core samples taken from two localities were studied with respect to the characteristics of the plant debris and the palynomorph assemblages to differentiate between regional and local signatures. At both of the sampling localities, the No. 2 Coal Seam is split into a Lower Coal Seam and an Upper Coal Seam by a siltstone and a sandstone intraseam parting, respectively. The uneven palaeotopography and distal depositional environment of the Highveld Coalfield distinguish it from the northern Witbank Coalfield as a river-dominated delta plain, with differences in the palaeoenvironment at each locality. Results from the Lower Coal Seam indicate a fern-dominated lowland and conifer-dominated upland. This gives way to a Glossopteris-dominated lowland and a diverse gymnospermous assemblage in the upland of the Upper Coal Seam. This change in floral composition is also observed in the adjacent Witbank Coalfield and is likely caused by climate amelioration related to the movement of Gondwana away from the South Pole.
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spelling doaj.art-949363ec43a54d3fa9b8d22d72e486812022-12-21T23:40:37ZengW. Szafer Institute of Botany, Polish Academy of SciencesActa Palaeobotanica2082-02592016-06-0156131510.1515/acpa-2016-0004acpa-2016-0004Palynofacies patterns of the Highveld coal deposits (Karoo Basin, South Africa): Clues to reconstruction of palaeoenvironment and palaeoclimateWheeler Alexander0Götz Annette E.1The University of Queensland, School of Earth Sciences, St. Lucia, QLD 4072, AustraliaKeele University, School of Physical and Geographical Sciences, Keele, Staffordshire ST5 5BG, United KingdomThe early Permian represents a crucial period of climate change in Gondwana. This climate signature is captured in the palynological record that represents the floral assemblage of the region. Palynofacies analysis of the No. 2 Coal Seam of the Highveld Coalfield provides a high-resolution picture of this climatic shift, as well as detailing the vegetation patterns and local environments. Core samples taken from two localities were studied with respect to the characteristics of the plant debris and the palynomorph assemblages to differentiate between regional and local signatures. At both of the sampling localities, the No. 2 Coal Seam is split into a Lower Coal Seam and an Upper Coal Seam by a siltstone and a sandstone intraseam parting, respectively. The uneven palaeotopography and distal depositional environment of the Highveld Coalfield distinguish it from the northern Witbank Coalfield as a river-dominated delta plain, with differences in the palaeoenvironment at each locality. Results from the Lower Coal Seam indicate a fern-dominated lowland and conifer-dominated upland. This gives way to a Glossopteris-dominated lowland and a diverse gymnospermous assemblage in the upland of the Upper Coal Seam. This change in floral composition is also observed in the adjacent Witbank Coalfield and is likely caused by climate amelioration related to the movement of Gondwana away from the South Pole.http://www.degruyter.com/view/j/acpa.2016.56.issue-1/acpa-2016-0004/acpa-2016-0004.xml?format=INTpalynofaciespalaeoenvironmentpalaeoclimatePermianHighveld CoalfieldSouth Africa
spellingShingle Wheeler Alexander
Götz Annette E.
Palynofacies patterns of the Highveld coal deposits (Karoo Basin, South Africa): Clues to reconstruction of palaeoenvironment and palaeoclimate
Acta Palaeobotanica
palynofacies
palaeoenvironment
palaeoclimate
Permian
Highveld Coalfield
South Africa
title Palynofacies patterns of the Highveld coal deposits (Karoo Basin, South Africa): Clues to reconstruction of palaeoenvironment and palaeoclimate
title_full Palynofacies patterns of the Highveld coal deposits (Karoo Basin, South Africa): Clues to reconstruction of palaeoenvironment and palaeoclimate
title_fullStr Palynofacies patterns of the Highveld coal deposits (Karoo Basin, South Africa): Clues to reconstruction of palaeoenvironment and palaeoclimate
title_full_unstemmed Palynofacies patterns of the Highveld coal deposits (Karoo Basin, South Africa): Clues to reconstruction of palaeoenvironment and palaeoclimate
title_short Palynofacies patterns of the Highveld coal deposits (Karoo Basin, South Africa): Clues to reconstruction of palaeoenvironment and palaeoclimate
title_sort palynofacies patterns of the highveld coal deposits karoo basin south africa clues to reconstruction of palaeoenvironment and palaeoclimate
topic palynofacies
palaeoenvironment
palaeoclimate
Permian
Highveld Coalfield
South Africa
url http://www.degruyter.com/view/j/acpa.2016.56.issue-1/acpa-2016-0004/acpa-2016-0004.xml?format=INT
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