Calcimicrobes in the Dendrolites of the Changshan Formation in the Zhi Dongyu Section

Huang Huiling

doi:doi:10.11648/j.earth.20231205.16

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Calcimicrobes in the Dendrolites of the Changshan Formation in the Zhi Dongyu Section

Huang Huiling

Published in Earth Sciences (Volume 12, Issue 5)

Received: 28 September 2023 Accepted: 16 October 2023 Published: 30 October 2023

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Abstract

Microbial carbonate rocks are classified into stromatolite, dendrolites, thrombolite, and leiolite based on their mesoscale features. Additionally, there are also oncolite and laminite. Based on field exploration sampling and combined with indoor thin section analysis, dendrolites was observed in the Changshan Formation of the Cambrian period in the Zhi Dongyu section of Shandong. It has a thickness of approximately 75 meters and, together with blocky oolitic grainstone, forms the upper part of a third-order depositional sequence that constitutes a late highstand systems tract (LHST). Macroscopically, obvious branching clots can be observed in dendrolites, while microscopically, the development of various calcifying cyanobacteria such as Girvanella, Epiphyton and Hedstroemla can be seen. In terms of Chronostratigraphy, microbial reefs dominated by dendrolites are relatively rare in the Furong Formation's Changshan Formation. Therefore, this study provides an important example for the subsequent research on dendrolites in the Changshan Formation. Additionally, the discovery of Epiphyton in the Changshan Formation contradicts the claim that they were extinct during the Late Ordovician mass extinction. What is more, the abundance of Hedstroemla also raises doubts about the previous belief that Epiphyton dominate the formation of dendrolites clots, emphasizing the importance of Hedstroemla in the formation of dendrolites clots.

Published in	Earth Sciences (Volume 12, Issue 5)
DOI	10.11648/j.earth.20231205.16
Page(s)	176-180
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

Dendrolites, Hedstroemla, Changshan Formation

References

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[3]	Mei M X, Latif K, Liu L, et al. Clots built by photosynthetic biofilms: Evidences from thrombolite bieherms of the Changshan Formation of Cambrian Furongian in Liaodong Peninsula [J]. Journal of Palaeogeography, 2019, 21(2): 254-277.
[4]	Peng S C, Zhao Y L. The Proposedglobal standard stratotype-section and point (GSSP) for the conterminous base of miaolinging series andwuliuan stage at Balang, Jianhe, Guizhou, China was ratified by IUGS [J]. Journal of Stratigraphy, 2018, 42(3): 325-327.
[5]	WOO J, CHOUGH S K, HAN Z. Chambers of Epiphyton Thalli in Microbial Buildups, Zhangxia Formation (Middle Cambrian), Shandong Province, China [J]. Palaios, 2008, 23(1): 55-64.
[6]	RIDING R. Microbial Carbonates: The Geological Record of Calcified Bacterial-Algal Mats and Biofilms [J]. Sedimentology, 2000, 47(1): 179-214.
[7]	Mei M X. Aparticular photozoan factory of carbonate rock of the Cambrian Miaolingian: a case study of the Zhangxia Formation at the Jiawang section in Xuzhou City of Jiang su Province [J]. Acta Geologica Sinica, 2022, 96(3): 744-768.
[8]	WHITTON B. Ecology of Cyanobacteria Ii: Their Diversity in Space and Time / Edited by Brian A. Whitton [M]. London: Springer, 2012.
[9]	RAMEIL N, IMMENHAUSER A, WARRLICH G, et al. Morphological Patterns of Aptian Lithocodium–Bacinella Geobodies: Relation to Environment and Scale [J]. Sedimentology, 2010, 57(3): 883-911.
[10]	FRANTZ C M, PETRYSHYN V A, CORSETTI F A. Grain Trapping by Filamentous Cyanobacterial and Algal Mats: Implications for Stromatolite Microfabrics through Time [J]. Geobiology, 2015, 13(5): 409-423.
[11]	SUOSAARI E P, AWRAMIK S M, REID R P, et al. Living Dendrolitic Microbial Mats in Hamelin Pool, Shark Bay, Western Australia [J]. Geosciences, 2018, 8(6): 212.
[12]	BRADLEY J A, DAILLE L K, TRIVEDI C B, et al. Carbonate-Rich Dendrolitic Cones: Insights into a Modern Analog for Incipient Microbialite Formation, Little Hot Creek, Long Valley Caldera, California [J]. npj Biofilms and Microbiomes, 2017, 3(1): 32.
[13]	MEI M X, RIAZ M, ZHANG Z W, et al. Diversified Calcimicrobes in Dendrolites of the Zhangxia Formation, Miaolingian Series (Middle Cambrian) of the North China Craton [J]. Journal of Palaeogeography, 2021, 10(2): 157-181.
[14]	McConnaughey T A, Whelan J F. Calcification generatesprotons for nutrient and bicarbonate uptake [J]. Earth Science Reviews, 1997, 42(1): 95-117.
[15]	Dupraz C, Reid R P, Braissant O, et al. Processes of Carbonate Precipitation in Modern Microbial Mats [J]. Earth Science Reviews, 2009, 96(3): 141-162.

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APA Style

Huang Huiling. (2023). Calcimicrobes in the Dendrolites of the Changshan Formation in the Zhi Dongyu Section. Earth Sciences, 12(5), 176-180. https://doi.org/10.11648/j.earth.20231205.16

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ACS Style

Huang Huiling. Calcimicrobes in the Dendrolites of the Changshan Formation in the Zhi Dongyu Section. Earth Sci. 2023, 12(5), 176-180. doi: 10.11648/j.earth.20231205.16

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AMA Style

Huang Huiling. Calcimicrobes in the Dendrolites of the Changshan Formation in the Zhi Dongyu Section. Earth Sci. 2023;12(5):176-180. doi: 10.11648/j.earth.20231205.16

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@article{10.11648/j.earth.20231205.16,
  author = {Huang Huiling},
  title = {Calcimicrobes in the Dendrolites of the Changshan Formation in the Zhi Dongyu Section},
  journal = {Earth Sciences},
  volume = {12},
  number = {5},
  pages = {176-180},
  doi = {10.11648/j.earth.20231205.16},
  url = {https://doi.org/10.11648/j.earth.20231205.16},
  eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.earth.20231205.16},
  abstract = {Microbial carbonate rocks are classified into stromatolite, dendrolites, thrombolite, and leiolite based on their mesoscale features. Additionally, there are also oncolite and laminite. Based on field exploration sampling and combined with indoor thin section analysis, dendrolites was observed in the Changshan Formation of the Cambrian period in the Zhi Dongyu section of Shandong. It has a thickness of approximately 75 meters and, together with blocky oolitic grainstone, forms the upper part of a third-order depositional sequence that constitutes a late highstand systems tract (LHST). Macroscopically, obvious branching clots can be observed in dendrolites, while microscopically, the development of various calcifying cyanobacteria such as Girvanella, Epiphyton and Hedstroemla can be seen. In terms of Chronostratigraphy, microbial reefs dominated by dendrolites are relatively rare in the Furong Formation's Changshan Formation. Therefore, this study provides an important example for the subsequent research on dendrolites in the Changshan Formation. Additionally, the discovery of Epiphyton in the Changshan Formation contradicts the claim that they were extinct during the Late Ordovician mass extinction. What is more, the abundance of Hedstroemla also raises doubts about the previous belief that Epiphyton dominate the formation of dendrolites clots, emphasizing the importance of Hedstroemla in the formation of dendrolites clots.
},
 year = {2023}
}

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TY  - JOUR
T1  - Calcimicrobes in the Dendrolites of the Changshan Formation in the Zhi Dongyu Section
AU  - Huang Huiling
Y1  - 2023/10/30
PY  - 2023
N1  - https://doi.org/10.11648/j.earth.20231205.16
DO  - 10.11648/j.earth.20231205.16
T2  - Earth Sciences
JF  - Earth Sciences
JO  - Earth Sciences
SP  - 176
EP  - 180
PB  - Science Publishing Group
SN  - 2328-5982
UR  - https://doi.org/10.11648/j.earth.20231205.16
AB  - Microbial carbonate rocks are classified into stromatolite, dendrolites, thrombolite, and leiolite based on their mesoscale features. Additionally, there are also oncolite and laminite. Based on field exploration sampling and combined with indoor thin section analysis, dendrolites was observed in the Changshan Formation of the Cambrian period in the Zhi Dongyu section of Shandong. It has a thickness of approximately 75 meters and, together with blocky oolitic grainstone, forms the upper part of a third-order depositional sequence that constitutes a late highstand systems tract (LHST). Macroscopically, obvious branching clots can be observed in dendrolites, while microscopically, the development of various calcifying cyanobacteria such as Girvanella, Epiphyton and Hedstroemla can be seen. In terms of Chronostratigraphy, microbial reefs dominated by dendrolites are relatively rare in the Furong Formation's Changshan Formation. Therefore, this study provides an important example for the subsequent research on dendrolites in the Changshan Formation. Additionally, the discovery of Epiphyton in the Changshan Formation contradicts the claim that they were extinct during the Late Ordovician mass extinction. What is more, the abundance of Hedstroemla also raises doubts about the previous belief that Epiphyton dominate the formation of dendrolites clots, emphasizing the importance of Hedstroemla in the formation of dendrolites clots.

VL  - 12
IS  - 5
ER  -

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Author Information

Huang Huiling

School of Earth Sciences and Resources, China University of Geosciences (Beijing), Beijing, China

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Plain Text BibTeX RIS

APA Style

Huang Huiling. (2023). Calcimicrobes in the Dendrolites of the Changshan Formation in the Zhi Dongyu Section. Earth Sciences, 12(5), 176-180. https://doi.org/10.11648/j.earth.20231205.16

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ACS Style

Huang Huiling. Calcimicrobes in the Dendrolites of the Changshan Formation in the Zhi Dongyu Section. Earth Sci. 2023, 12(5), 176-180. doi: 10.11648/j.earth.20231205.16

Copy | Download

AMA Style

Huang Huiling. Calcimicrobes in the Dendrolites of the Changshan Formation in the Zhi Dongyu Section. Earth Sci. 2023;12(5):176-180. doi: 10.11648/j.earth.20231205.16

Copy | Download

@article{10.11648/j.earth.20231205.16,
  author = {Huang Huiling},
  title = {Calcimicrobes in the Dendrolites of the Changshan Formation in the Zhi Dongyu Section},
  journal = {Earth Sciences},
  volume = {12},
  number = {5},
  pages = {176-180},
  doi = {10.11648/j.earth.20231205.16},
  url = {https://doi.org/10.11648/j.earth.20231205.16},
  eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.earth.20231205.16},
  abstract = {Microbial carbonate rocks are classified into stromatolite, dendrolites, thrombolite, and leiolite based on their mesoscale features. Additionally, there are also oncolite and laminite. Based on field exploration sampling and combined with indoor thin section analysis, dendrolites was observed in the Changshan Formation of the Cambrian period in the Zhi Dongyu section of Shandong. It has a thickness of approximately 75 meters and, together with blocky oolitic grainstone, forms the upper part of a third-order depositional sequence that constitutes a late highstand systems tract (LHST). Macroscopically, obvious branching clots can be observed in dendrolites, while microscopically, the development of various calcifying cyanobacteria such as Girvanella, Epiphyton and Hedstroemla can be seen. In terms of Chronostratigraphy, microbial reefs dominated by dendrolites are relatively rare in the Furong Formation's Changshan Formation. Therefore, this study provides an important example for the subsequent research on dendrolites in the Changshan Formation. Additionally, the discovery of Epiphyton in the Changshan Formation contradicts the claim that they were extinct during the Late Ordovician mass extinction. What is more, the abundance of Hedstroemla also raises doubts about the previous belief that Epiphyton dominate the formation of dendrolites clots, emphasizing the importance of Hedstroemla in the formation of dendrolites clots.
},
 year = {2023}
}

Copy | Download

TY  - JOUR
T1  - Calcimicrobes in the Dendrolites of the Changshan Formation in the Zhi Dongyu Section
AU  - Huang Huiling
Y1  - 2023/10/30
PY  - 2023
N1  - https://doi.org/10.11648/j.earth.20231205.16
DO  - 10.11648/j.earth.20231205.16
T2  - Earth Sciences
JF  - Earth Sciences
JO  - Earth Sciences
SP  - 176
EP  - 180
PB  - Science Publishing Group
SN  - 2328-5982
UR  - https://doi.org/10.11648/j.earth.20231205.16
AB  - Microbial carbonate rocks are classified into stromatolite, dendrolites, thrombolite, and leiolite based on their mesoscale features. Additionally, there are also oncolite and laminite. Based on field exploration sampling and combined with indoor thin section analysis, dendrolites was observed in the Changshan Formation of the Cambrian period in the Zhi Dongyu section of Shandong. It has a thickness of approximately 75 meters and, together with blocky oolitic grainstone, forms the upper part of a third-order depositional sequence that constitutes a late highstand systems tract (LHST). Macroscopically, obvious branching clots can be observed in dendrolites, while microscopically, the development of various calcifying cyanobacteria such as Girvanella, Epiphyton and Hedstroemla can be seen. In terms of Chronostratigraphy, microbial reefs dominated by dendrolites are relatively rare in the Furong Formation's Changshan Formation. Therefore, this study provides an important example for the subsequent research on dendrolites in the Changshan Formation. Additionally, the discovery of Epiphyton in the Changshan Formation contradicts the claim that they were extinct during the Late Ordovician mass extinction. What is more, the abundance of Hedstroemla also raises doubts about the previous belief that Epiphyton dominate the formation of dendrolites clots, emphasizing the importance of Hedstroemla in the formation of dendrolites clots.

VL  - 12
IS  - 5
ER  -

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