Reinvestigation of Devonian-Carboniferous palynostratigraphy in Yalai village, Nyalam County, southern Tibet, China
Reinvestigation of Devonian-Carboniferous palynostratigraphy in Yalai village, Nyalam County, southern Tibet, China
Reinvestigation of the Devonian-Carboniferous boundary sequence in Yalai village, Nyalam County, southern Tibet, enabled the recovery of well-preserved palynomorphs and conodonts in the Yali section. Based on quantitative analysis of the relative abundances of various palynomorphs, two palynological assemblages are recognized in the Famennian-Tournaisian boundary beds of the Yali section. In ascending order, they are the Retispora lepidophyta–Verrucosisporites irregularis (LI) assemblage and the Retispora lepidophyta–Vallatisporites vallatus (LV) assemblage. Both assemblages are tentatively correlated with the Famennian LN Biozone of Western Europe because of the appearance of Retispora lepidophyta and other index spores such as Vallatisporites verrucosus, Vallatisporites pusillites, Indotriradites explanatus, and Densosporites spitsbergensis in both palynological assemblages. The lower limestones of the Yali Formation yield biostratigraphic markers for the Devonian-Carboniferous boundary, including the conodont Siphonodella sulcata and Protognathodus kockeli, correlated with the VI Biozone from Western Europe and parts of Gondwana. The upper Lazhabu Member of the Yali Formation yielded Retispora lepidophyta, Vallatisporites vallatus, and Vallatisporites pusillites of the LV Biozone, indicating that some typical palynomorphs elements of the LN Biozone of Western Europe persisted into Tournaisian in southern Tibet.
Famennian, Gondwana, Spore, Tibet, Tournaisian
Peng, Huiping
1112e3ae-26f1-441c-84a5-fa4258e8cbd9
Qie, Wenkun
e5073568-979c-46b5-a42b-da9ff0a55cc0
Marshall, John E.A.
cba178e3-91aa-49a2-b2ce-4b8d9d870b06
Zhu, Huaicheng
5e9a8cf6-b7d0-47eb-b13f-ceb72fe88231
Guo, Wen
50b27951-84a0-41f5-8459-596a8259ce06
Song, Junjun
9723f27a-8042-4a47-a7ad-e5e5d881f833
Liu, Feng
30a0aea2-0008-4d2b-bfb9-28527884967c
9 June 2022
Peng, Huiping
1112e3ae-26f1-441c-84a5-fa4258e8cbd9
Qie, Wenkun
e5073568-979c-46b5-a42b-da9ff0a55cc0
Marshall, John E.A.
cba178e3-91aa-49a2-b2ce-4b8d9d870b06
Zhu, Huaicheng
5e9a8cf6-b7d0-47eb-b13f-ceb72fe88231
Guo, Wen
50b27951-84a0-41f5-8459-596a8259ce06
Song, Junjun
9723f27a-8042-4a47-a7ad-e5e5d881f833
Liu, Feng
30a0aea2-0008-4d2b-bfb9-28527884967c
Peng, Huiping, Qie, Wenkun, Marshall, John E.A., Zhu, Huaicheng, Guo, Wen, Song, Junjun and Liu, Feng
(2022)
Reinvestigation of Devonian-Carboniferous palynostratigraphy in Yalai village, Nyalam County, southern Tibet, China.
Review of Palaeobotany and Palynology, 304 (9), [104702].
(doi:10.1016/j.revpalbo.2022.104702).
Abstract
Reinvestigation of the Devonian-Carboniferous boundary sequence in Yalai village, Nyalam County, southern Tibet, enabled the recovery of well-preserved palynomorphs and conodonts in the Yali section. Based on quantitative analysis of the relative abundances of various palynomorphs, two palynological assemblages are recognized in the Famennian-Tournaisian boundary beds of the Yali section. In ascending order, they are the Retispora lepidophyta–Verrucosisporites irregularis (LI) assemblage and the Retispora lepidophyta–Vallatisporites vallatus (LV) assemblage. Both assemblages are tentatively correlated with the Famennian LN Biozone of Western Europe because of the appearance of Retispora lepidophyta and other index spores such as Vallatisporites verrucosus, Vallatisporites pusillites, Indotriradites explanatus, and Densosporites spitsbergensis in both palynological assemblages. The lower limestones of the Yali Formation yield biostratigraphic markers for the Devonian-Carboniferous boundary, including the conodont Siphonodella sulcata and Protognathodus kockeli, correlated with the VI Biozone from Western Europe and parts of Gondwana. The upper Lazhabu Member of the Yali Formation yielded Retispora lepidophyta, Vallatisporites vallatus, and Vallatisporites pusillites of the LV Biozone, indicating that some typical palynomorphs elements of the LN Biozone of Western Europe persisted into Tournaisian in southern Tibet.
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More information
Accepted/In Press date: 31 May 2022
e-pub ahead of print date: 3 June 2022
Published date: 9 June 2022
Additional Information:
Funding Information:
This work was funded by the Second Tibetan Plateau Scientific Expedition and Research (grant 2019QZKK0706 ), the National Natural Science Foundation of China (grant 42172023 , 91855205 ), and the Strategic Priority Research Program (B) of the CAS (grant XDB26000000 ).
Keywords:
Famennian, Gondwana, Spore, Tibet, Tournaisian
Identifiers
Local EPrints ID: 485256
URI: http://eprints.soton.ac.uk/id/eprint/485256
ISSN: 0034-6667
PURE UUID: ac0e8dcb-236c-4d3b-b18e-98d66705af7a
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Date deposited: 01 Dec 2023 17:49
Last modified: 17 Mar 2024 02:34
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Contributors
Author:
Huiping Peng
Author:
Wenkun Qie
Author:
Huaicheng Zhu
Author:
Wen Guo
Author:
Junjun Song
Author:
Feng Liu
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