Biological Diversity, Crisis and Recovery in the Phong Son Formation (D3-C1 Ps), Thua Thien-Hue Province, North-Central Vietnam

Nguyen Huu Hung; Doan Dinh Hung; Nguyen Ba Hung

doi:doi:10.11648/j.eeb.20210604.12

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Biological Diversity, Crisis and Recovery in the Phong Son Formation (D₃-C₁ Ps), Thua Thien-Hue Province, North-Central Vietnam

Nguyen Huu Hung, Doan Dinh Hung, Nguyen Ba Hung

Published in Ecology and Evolutionary Biology (Volume 6, Issue 4)

Received: 6 July 2021 Accepted: 10 August 2021 Published: 17 November 2021

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Abstract

The present of Upper Devonian and Lower Carboniferous sediments and fossils in Hue City, Van Xa area, Huong Thuy District; Thanh Tan, Hien An villages, Dong Lam Quarry, Phong Dien District, Thua Thien-Hue Province has been noted in recent years depend on explosion of limestone underlying the Quaternary cover for cement technology and building. The Phong Son Formation has been established with two members: the underlying Van Xa Member composed of mainly limestone, 280 m thick, containing abundant Famennian brachiopods, crinoids, gastropods; the overlying Hien An Member composed of limestone intercalated with black shale, 210 m thick, containing abundant brachiopods, crinoids, bryozoans, stromatoporoids, corals, trilobites, foraminiferans, gastropods of Latest Famennian-Tournaisian age. Over 1000 macrofossil examples were collected from both the Van Xa Member and Hien An one for analyzing biological diversity, crisis and recovery of all macrofossil group of stratigraphical level of the Phong Son Formation (D₃-C₁ ps). In the Famennian stage, the diversity is related to representatives of phyla Brachiopoda, Cnidaria, Mollusca; belonging to the Cyrtospirifer-Yunnanella Assemblage. In the Tournaisian stage, the recovery and diversity is related to reprensentatives of phyla Porifera, Cnidaria, Arthropoda, Brachiopoda, Bryozoa, Mollusca, and Echinodermata; belonging to the Leptagonia-Phillipsia Assemblage. The crisis at the DCB of the Phong Son Fm is well displayed in phyla Brachiopoda, Cnidaria and Porifera.

Published in	Ecology and Evolutionary Biology (Volume 6, Issue 4)
DOI	10.11648/j.eeb.20210604.12
Page(s)	103-112
Creative Commons	This is an Open Access article, distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution and reproduction in any medium or format, provided the original work is properly cited.
Copyright	Copyright © The Author(s), 2024. Published by Science Publishing Group

Keywords

Macrofossils, Diversity, Famennian-Tournaisian, Vietnam.

References

[1]	Ausich, W. I. and Kammer, T. W. 2006. Stratigraphical and geographical distribution of Mississippian (Lower Carboniferous) Crinoidea from England and Wales. Procceding of the Yorkshire Geological Society, Vol. 56, Part 2, p. 91-109.
[2]	Baliński, A. 2002. Frasnian-Famennian brachiopod extinction and recovery in southern Poland. Acta Palaeontol. Pol. 47 (2): 289-305.
[3]	Bouman, R. W. & Donovan, S. K. 2015. Biodiversity of Mississippian (Lower Carboniferous) crinoids from Bradford Dale, Derbyshire, UK. Procceding of the Yorkshire Geological Society.
[4]	Chen, Z. Q., Zang, Z. X. & Jin, Y. G. 2008. Late Devonian (Famennian) brachiopod Yunnanella from the Junggar Basin, northern Xinjiang, China. Alcheringa, 26: 3, 451-458.
[5]	Chen, Z. Q. & Shi, G. R. 1999. Latest Devonian (Famennian) to Earliest Carboniferous (Tournaisian) brachiopods from Bachu Formation of the Tarim Basin, Xinjiang Province, Northwest China. Rivista Italiana di Paleontologia e Stratigraphia, Vol. 105, No. 2, p. 231-250.
[6]	Doan Nhat Truong (Ed.) 2012. Atlas of Vietnam paleontology, Volum Foraminfera. Vietnam Publishing House of Natural resources-Environment and Cartography, 222 p. (in Vietnamese). Hanoi.
[7]	Dong, D.-Y. 1964. Stromatoporoids from Early Carboniferous of Kwangxi and Kueichow. Acta Paleontologica Sinica, Vol. 12, No. 2, p. 101-114.
[8]	Fontaine, H. 1962. Les calcaires de la region de Huê. Travaux de Gesologie, 1: 11-17. Huê.
[9]	GŁuchowski, E. and Racki G. 2005. Disarticulated crinoid stems from the Devonian and Carboniferous of north Devon, England. Proceeding of the Yorkshire Geological Society, Vol. 55, Part 3, p. 161-172.
[10]	Kobayashi, T. and Hamada, T. 1980. Carboniferous trilobites of Japan in comparison with Asian, Pacific and other faunas. Palaeontological Society of Japan special papers, number 23, 132 p., 22 pls.
[11]	Kurilenko, A. V. & Kulkov, N. P. 2008. A proposed crinoid zonation of the Devonian deposits of eastern Transbaikal. Bulletin of Geosciences, Vol. 83, 3: 461-472.
[12]	Lane, N. G, Maples C. G. and Waters J. A. 2001. Revision of Late Devonian (Famennian) somme Early Carboniferous (Tournaisian) crinoids and blastoloids from the type Devonian area of North Devon. Paleontology, Vol 44, Part 6, p. 1043-1080, 6 pls.
[13]	Ma, X.-P, Sun, Y. –L, Hao W. –C., and Liao, W, W. –H. 2002. Rugosa coral and brachiopods across the Frasnian-Famennian boundary in central Hunan, South China. Acta Palaeontol. Pol. 47 (2): 373-396.
[14]	Mansuy, H. 1913. Paléontologie de l’Annam et de Tonkin. Mémoires du Service Gesologique de l’Indochina, II/3: 48 p. Hanoi.
[15]	Mottequin, B., Brice, D. & Legrand-Blain, M. 2014. Biostratigraphic significance of brachiopods near the Devonian-Carboniferous boundary. Geol. Mag. 151 (2): 216-228.
[16]	Nguyen Huu Hung, Doan Nhat Truong, Nguyen Duc Khoa 1995. Stratigraphy of Devonian- Lower Carboniferous sediments in North-central Vietnam. Geology and Mineral resources, 4: 17-29 (in Vietnamese with English summary). Hanoi.
[17]	Nguyen Huu Hung 1996. Stratigraphy and Stromatoporoidea of Middle-Upper Devonian (Givetian, Frasnian and Famennian Stages) in the North-central Vietnam. Ph. D. thesis, Institute of Geoscience and Minerals resources, Ministry of Natural Resources of Vietnam: 104 p., 23 pls (in Vietnamese). Hanoi.
[18]	Nguyen Huu Hung, Mistiaen B. 1998. Uppermost Famennian stromatoporoids of North-central Vietnam. Journal of Geology, B/11-12: 57-75. Hanoi.
[19]	Nguyen Huu Hung 2000. Environment characteristics of the Muc Bai and Xom Nha Formations. Geological Mapping, 98: 28-32 (in Vietnamese). Hanoi.
[20]	Nguyen Duc Khoa 1996. The Upper Famennian and Tournaisian Rugoses and stratigraphy of Vietnam. Geologos, 1: 19-27. Warszawa.
[21]	Nguyen Van Trang 1978. Stratigraphic position of limestones at Tan Lam, Cam Lo, Thanh Tan, Long Tho and Nam Dong. Geological Mapping, 36: 32-36 (in Vietnamese). Hanoi.
[22]	Nguyen Van Trang (Ed.) 1984. Main characteristics of geological structure and mineral resources of the Hue-Quang Ngai Area. Geology and Mineral resources of Vietnam, 2: 107-137 (in Vietnamese). Hanoi.
[23]	Nguyen Van Trang (Ed.) 1996. Geological and mineral resources map of Vietnam, scale 1:200.000; Hue-Quang Ngai Sheet with explanatory notes. Department of Geology and Minerals of Vietnam (in Vietnamese and English). Hanoi.
[24]	Nguyen Truong Giang 1999. Groundwater in the Tri Thien plain. Journal of Geological Economy and Mineral resources, 17/1: 32-42 (in Vietnamese). Hanoi.
[25]	Phạm Huy Thong 1995. Some results of research on urban geology of Hue City. Geological mapping: 36-43 (in Vietnamese). Hanoi.
[26]	Pham Huy Thong 1997. Legends of Hue geological map sheet group at 1:50.000 scale. Geological mapping: 34-39 (in Vietnamese). Hanoi.
[27]	Porty, E. & Xu, S. C. 1966. Rugosa from the Devonian-Carboniferous transition in Hunan, China. Mém. Inst. Géol. Univ. Louvain, 36: 89-39.
[28]	Qian, W. L. & Roberts, J. 2008. Brachiopods of the Early Carboniferous Schellwienella burlingtonensis Zone in eastern Australia. Alcheringa 19: 4, 255-289.
[29]	Shen, S. –Z., Zhang, H., Li, W. –Z., Mu, L. and Xie, J. –P. 2006. Brachiopod diversity patterns from Carboniferous to Triassic in South China. Geol. J. 41: 345-361.
[30]	Sun, Y. and Baliński, A. 2008. Silicified Mississippian brachiopods from Muhua, southern China: Lingulids, craniids, strophomenids, productids, orthotetids, and orthids. Acta Palaeontol. Pol. 53 (3): 485-524.
[31]	Tolokonnikova, Z., Ernst, A. an Poty E. 2015. Tournaisian (Lower Missippian) bryozoans from Belgium. N. Jb. Geol. Paläont. Abh. 278/1: 23-45.
[32]	Tong Duy Thanh, Vu Khuc (Eds.) 2006. Stratigraphic units of Vietnam. Vietnam National Univ. Publ. House, 526 p.. Hanoi.
[33]	Tran Van Tri, Vu Khuc (Eds.) 2011. Geology and Earth Resources of Vietnam. Publishing House for Science and Technology, 645 p.. Hanoi.
[34]	Yuan, J. and Xiang, L. 1998. Trilobite fauna at the Devonian-Carboniferous boundary in South China (S-Guizhou and N-Guangxi). NMNS. SPEC. PUBL. No. 8., 281 p.

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APA Style

Nguyen Huu Hung, Doan Dinh Hung, Nguyen Ba Hung. (2021). Biological Diversity, Crisis and Recovery in the Phong Son Formation (D3-C1 Ps), Thua Thien-Hue Province, North-Central Vietnam. Ecology and Evolutionary Biology, 6(4), 103-112. https://doi.org/10.11648/j.eeb.20210604.12

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ACS Style

Nguyen Huu Hung; Doan Dinh Hung; Nguyen Ba Hung. Biological Diversity, Crisis and Recovery in the Phong Son Formation (D3-C1 Ps), Thua Thien-Hue Province, North-Central Vietnam. Ecol. Evol. Biol. 2021, 6(4), 103-112. doi: 10.11648/j.eeb.20210604.12

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AMA Style

Nguyen Huu Hung, Doan Dinh Hung, Nguyen Ba Hung. Biological Diversity, Crisis and Recovery in the Phong Son Formation (D3-C1 Ps), Thua Thien-Hue Province, North-Central Vietnam. Ecol Evol Biol. 2021;6(4):103-112. doi: 10.11648/j.eeb.20210604.12

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@article{10.11648/j.eeb.20210604.12,
  author = {Nguyen Huu Hung and Doan Dinh Hung and Nguyen Ba Hung},
  title = {Biological Diversity, Crisis and Recovery in the Phong Son Formation (D3-C1 Ps), Thua Thien-Hue Province, North-Central Vietnam},
  journal = {Ecology and Evolutionary Biology},
  volume = {6},
  number = {4},
  pages = {103-112},
  doi = {10.11648/j.eeb.20210604.12},
  url = {https://doi.org/10.11648/j.eeb.20210604.12},
  eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.eeb.20210604.12},
  abstract = {The present of Upper Devonian and Lower Carboniferous sediments and fossils in Hue City, Van Xa area, Huong Thuy District; Thanh Tan, Hien An villages, Dong Lam Quarry, Phong Dien District, Thua Thien-Hue Province has been noted in recent years depend on explosion of limestone underlying the Quaternary cover for cement technology and building. The Phong Son Formation has been established with two members: the underlying Van Xa Member composed of mainly limestone, 280 m thick, containing abundant Famennian brachiopods, crinoids, gastropods; the overlying Hien An Member composed of limestone intercalated with black shale, 210 m thick, containing abundant brachiopods, crinoids, bryozoans, stromatoporoids, corals, trilobites, foraminiferans, gastropods of Latest Famennian-Tournaisian age. Over 1000 macrofossil examples were collected from both the Van Xa Member and Hien An one for analyzing biological diversity, crisis and recovery of all macrofossil group of stratigraphical level of the Phong Son Formation (D3-C1 ps). In the Famennian stage, the diversity is related to representatives of phyla Brachiopoda, Cnidaria, Mollusca; belonging to the Cyrtospirifer-Yunnanella Assemblage. In the Tournaisian stage, the recovery and diversity is related to reprensentatives of phyla Porifera, Cnidaria, Arthropoda, Brachiopoda, Bryozoa, Mollusca, and Echinodermata; belonging to the Leptagonia-Phillipsia Assemblage. The crisis at the DCB of the Phong Son Fm is well displayed in phyla Brachiopoda, Cnidaria and Porifera.},
 year = {2021}
}

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TY  - JOUR
T1  - Biological Diversity, Crisis and Recovery in the Phong Son Formation (D3-C1 Ps), Thua Thien-Hue Province, North-Central Vietnam
AU  - Nguyen Huu Hung
AU  - Doan Dinh Hung
AU  - Nguyen Ba Hung
Y1  - 2021/11/17
PY  - 2021
N1  - https://doi.org/10.11648/j.eeb.20210604.12
DO  - 10.11648/j.eeb.20210604.12
T2  - Ecology and Evolutionary Biology
JF  - Ecology and Evolutionary Biology
JO  - Ecology and Evolutionary Biology
SP  - 103
EP  - 112
PB  - Science Publishing Group
SN  - 2575-3762
UR  - https://doi.org/10.11648/j.eeb.20210604.12
AB  - The present of Upper Devonian and Lower Carboniferous sediments and fossils in Hue City, Van Xa area, Huong Thuy District; Thanh Tan, Hien An villages, Dong Lam Quarry, Phong Dien District, Thua Thien-Hue Province has been noted in recent years depend on explosion of limestone underlying the Quaternary cover for cement technology and building. The Phong Son Formation has been established with two members: the underlying Van Xa Member composed of mainly limestone, 280 m thick, containing abundant Famennian brachiopods, crinoids, gastropods; the overlying Hien An Member composed of limestone intercalated with black shale, 210 m thick, containing abundant brachiopods, crinoids, bryozoans, stromatoporoids, corals, trilobites, foraminiferans, gastropods of Latest Famennian-Tournaisian age. Over 1000 macrofossil examples were collected from both the Van Xa Member and Hien An one for analyzing biological diversity, crisis and recovery of all macrofossil group of stratigraphical level of the Phong Son Formation (D3-C1 ps). In the Famennian stage, the diversity is related to representatives of phyla Brachiopoda, Cnidaria, Mollusca; belonging to the Cyrtospirifer-Yunnanella Assemblage. In the Tournaisian stage, the recovery and diversity is related to reprensentatives of phyla Porifera, Cnidaria, Arthropoda, Brachiopoda, Bryozoa, Mollusca, and Echinodermata; belonging to the Leptagonia-Phillipsia Assemblage. The crisis at the DCB of the Phong Son Fm is well displayed in phyla Brachiopoda, Cnidaria and Porifera.
VL  - 6
IS  - 4
ER  -

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Author Information

Nguyen Huu Hung

Paleontological and Stratigraphical Society of Vietnam, Ha Noi City, Vietnam
Doan Dinh Hung

Geological Department of the Vietnam National Museum of Nature, Building A20, Vietnam Academy of Science and Technology, Ha Noi City, Vietnam
Nguyen Ba Hung

Geological Department of the Vietnam National Museum of Nature, Building A20, Vietnam Academy of Science and Technology, Ha Noi City, Vietnam

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Nguyen Huu Hung, Doan Dinh Hung, Nguyen Ba Hung. (2021). Biological Diversity, Crisis and Recovery in the Phong Son Formation (D3-C1 Ps), Thua Thien-Hue Province, North-Central Vietnam. Ecology and Evolutionary Biology, 6(4), 103-112. https://doi.org/10.11648/j.eeb.20210604.12

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ACS Style

Nguyen Huu Hung; Doan Dinh Hung; Nguyen Ba Hung. Biological Diversity, Crisis and Recovery in the Phong Son Formation (D3-C1 Ps), Thua Thien-Hue Province, North-Central Vietnam. Ecol. Evol. Biol. 2021, 6(4), 103-112. doi: 10.11648/j.eeb.20210604.12

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AMA Style

Nguyen Huu Hung, Doan Dinh Hung, Nguyen Ba Hung. Biological Diversity, Crisis and Recovery in the Phong Son Formation (D3-C1 Ps), Thua Thien-Hue Province, North-Central Vietnam. Ecol Evol Biol. 2021;6(4):103-112. doi: 10.11648/j.eeb.20210604.12

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@article{10.11648/j.eeb.20210604.12,
  author = {Nguyen Huu Hung and Doan Dinh Hung and Nguyen Ba Hung},
  title = {Biological Diversity, Crisis and Recovery in the Phong Son Formation (D3-C1 Ps), Thua Thien-Hue Province, North-Central Vietnam},
  journal = {Ecology and Evolutionary Biology},
  volume = {6},
  number = {4},
  pages = {103-112},
  doi = {10.11648/j.eeb.20210604.12},
  url = {https://doi.org/10.11648/j.eeb.20210604.12},
  eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.eeb.20210604.12},
  abstract = {The present of Upper Devonian and Lower Carboniferous sediments and fossils in Hue City, Van Xa area, Huong Thuy District; Thanh Tan, Hien An villages, Dong Lam Quarry, Phong Dien District, Thua Thien-Hue Province has been noted in recent years depend on explosion of limestone underlying the Quaternary cover for cement technology and building. The Phong Son Formation has been established with two members: the underlying Van Xa Member composed of mainly limestone, 280 m thick, containing abundant Famennian brachiopods, crinoids, gastropods; the overlying Hien An Member composed of limestone intercalated with black shale, 210 m thick, containing abundant brachiopods, crinoids, bryozoans, stromatoporoids, corals, trilobites, foraminiferans, gastropods of Latest Famennian-Tournaisian age. Over 1000 macrofossil examples were collected from both the Van Xa Member and Hien An one for analyzing biological diversity, crisis and recovery of all macrofossil group of stratigraphical level of the Phong Son Formation (D3-C1 ps). In the Famennian stage, the diversity is related to representatives of phyla Brachiopoda, Cnidaria, Mollusca; belonging to the Cyrtospirifer-Yunnanella Assemblage. In the Tournaisian stage, the recovery and diversity is related to reprensentatives of phyla Porifera, Cnidaria, Arthropoda, Brachiopoda, Bryozoa, Mollusca, and Echinodermata; belonging to the Leptagonia-Phillipsia Assemblage. The crisis at the DCB of the Phong Son Fm is well displayed in phyla Brachiopoda, Cnidaria and Porifera.},
 year = {2021}
}

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TY  - JOUR
T1  - Biological Diversity, Crisis and Recovery in the Phong Son Formation (D3-C1 Ps), Thua Thien-Hue Province, North-Central Vietnam
AU  - Nguyen Huu Hung
AU  - Doan Dinh Hung
AU  - Nguyen Ba Hung
Y1  - 2021/11/17
PY  - 2021
N1  - https://doi.org/10.11648/j.eeb.20210604.12
DO  - 10.11648/j.eeb.20210604.12
T2  - Ecology and Evolutionary Biology
JF  - Ecology and Evolutionary Biology
JO  - Ecology and Evolutionary Biology
SP  - 103
EP  - 112
PB  - Science Publishing Group
SN  - 2575-3762
UR  - https://doi.org/10.11648/j.eeb.20210604.12
AB  - The present of Upper Devonian and Lower Carboniferous sediments and fossils in Hue City, Van Xa area, Huong Thuy District; Thanh Tan, Hien An villages, Dong Lam Quarry, Phong Dien District, Thua Thien-Hue Province has been noted in recent years depend on explosion of limestone underlying the Quaternary cover for cement technology and building. The Phong Son Formation has been established with two members: the underlying Van Xa Member composed of mainly limestone, 280 m thick, containing abundant Famennian brachiopods, crinoids, gastropods; the overlying Hien An Member composed of limestone intercalated with black shale, 210 m thick, containing abundant brachiopods, crinoids, bryozoans, stromatoporoids, corals, trilobites, foraminiferans, gastropods of Latest Famennian-Tournaisian age. Over 1000 macrofossil examples were collected from both the Van Xa Member and Hien An one for analyzing biological diversity, crisis and recovery of all macrofossil group of stratigraphical level of the Phong Son Formation (D3-C1 ps). In the Famennian stage, the diversity is related to representatives of phyla Brachiopoda, Cnidaria, Mollusca; belonging to the Cyrtospirifer-Yunnanella Assemblage. In the Tournaisian stage, the recovery and diversity is related to reprensentatives of phyla Porifera, Cnidaria, Arthropoda, Brachiopoda, Bryozoa, Mollusca, and Echinodermata; belonging to the Leptagonia-Phillipsia Assemblage. The crisis at the DCB of the Phong Son Fm is well displayed in phyla Brachiopoda, Cnidaria and Porifera.
VL  - 6
IS  - 4
ER  -

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