Dapingian

Dapingian
	470.0 ± 1.4 – 467.3 ± 1.1 Ma PreꞒ Ꞓ O S D C P T J K Pg N ↓
Chronology
	Epochs in the Ordovician -485 — – -480 — – -475 — – -470 — – -465 — – -460 — – -455 — – -450 — – -445 — – P ; a ; l ; e ; o ; z ; o ; i ; c Ꞓ O; r; d; o; v; i; c; i; a; n S F E; a; r; l; y M; i; d; d; l; e L; a; t; e L Stage 10 Tremadocian Floian Dapingian Darriwilian Sandbian Katian Hirnantian Rhuddanian ← First land plant spores[1] ← Ordovician meteor event[2][3] Epochs of the Ordovician Period. ; Axis scale: millions of years ago.;
Etymology
Name formality	Formal
Usage information
Celestial body	Earth
Regional usage	Global (ICS)
Time scale(s) used	ICS Time Scale
Definition
Chronological unit	Age
Stratigraphic unit	Stage
Time span formality	Formal
Lower boundary definition	FAD of the Conodont Baltoniodus triangularis
Lower boundary GSSP	Huanghuachang section, Huanghuachang, Yichang, China; 30.8605°N 111.3740°E
GSSP ratified	2007[4]
Upper boundary definition	FAD of the Graptolite Undulograptus austrodentatus
Upper boundary GSSP	Huangnitang Section, Huangnitang Village, Changshan, Zhejiang, China; 28.8539°N 118.4897°E
GSSP ratified	1987[5]

The Dapingian is the third stage of the Ordovician and the first stage of the Middle Ordovician. It is preceded by the Floian and succeeded by the Darriwilian. The top of the Floian is defined as the first appearance of the conodont species Baltoniodus triangularis which happened about 470 million years ago. The Dapingian lasted for about 2.7 million years until about 467.3 million years ago.[6]

Naming

The Dapingian is named after a village that lies nearby the Dapingian GSSP (Huanghuachang section, in Huanghuachang) where there is also an outcrop of similar rocks, the "Chenjiahe section" (formerly "Daping section") in Chenjiahe. The name was proposed in 2005.[7]

GSSP

Huanghuachang section

Map of China showing the GSSP location.

The GSSP of the Dapingian is the Huanghuachang section (30.8605°N 111.3740°E / 30.8605; 111.3740), in Huanghuachang, Yichang, China. It is an outcrop of the Dawan Formation. The lower boundary is defined as the first appearance of the conodont species Baltoniodus triangularis in the type section. Radiometric dating has constrained the Floian-Dapingian boundary at 470 million years ago.[6] The exact boundary lies 10.57 m above the base of Dawan Formation.[7][8]

Regional stages

The Dapingian overlaps with the Arenig, a geologic stage used in England.[9]

Palaeontology

Agnathans

Agnathans of the Dapingian
Taxa	Presence	Location	Description	Images
Sacabambaspis	Dapingian-Sandbian	Sacabamba, Cochabamba Department, Bolivia; Horn Creek Siltstone, Australia; Argentina; Oman

Endocerids

Endocerids of the Dapingian
Taxa	Presence	Location	Description	Images
Cameroceras	Dapingian-Homerian
Endoceras	Dapingian-Hirnantian
Meniscoceras	Dapingian-Darriwilian	Chazy Reef Formation, New York, USA
Najaceras	Dapingian-Darriwilian	West Spring Creek, Oil Creek Limestone, Oklahoma
Nanno	Dapingian-Darriwilian
Proterovaginoceras	Tremadocian-Darriwilian

References

Wellman, C.H.; Gray, J. (2000). "The microfossil record of early land plants". Phil. Trans. R. Soc. B. 355 (1398): 717–732. doi:10.1098/rstb.2000.0612. PMC 1692785. PMID 10905606.
Korochantseva, Ekaterina; Trieloff, Mario; Lorenz, Cyrill; Buykin, Alexey; Ivanova, Marina; Schwarz, Winfried; Hopp, Jens; Jessberger, Elmar (2007). "L-chondrite asteroid breakup tied to Ordovician meteorite shower by multiple isochron 40 Ar- 39 Ar dating". Meteoritics & Planetary Science. 42 (1): 113–130. Bibcode:2007M&PS...42..113K. doi:10.1111/j.1945-5100.2007.tb00221.x.
Lindskog, A.; Costa, M. M.; Rasmussen, C.M.Ø.; Connelly, J. N.; Eriksson, M. E. (2017-01-24). "Refined Ordovician timescale reveals no link between asteroid breakup and biodiversification". Nature Communications. 8: 14066. doi:10.1038/ncomms14066. ISSN 2041-1723. PMC 5286199. PMID 28117834. It has been suggested that the Middle Ordovician meteorite bombardment played a crucial role in the Great Ordovician Biodiversification Event, but this study shows that the two phenomena were unrelated
Chen, Xu; Bergström, Stig; Zhang, Yuan-Dong; Fan, Jun-Xuan (2009). "The base of the Middle Ordovician in China with special reference to the succession at Hengtang near Jiangshan, Zhejiang Province, southern China" (PDF). Lethaia. 42: 218–231. doi:10.1111/j.1502-3931.2008.00148.x. Retrieved 13 December 2020.
Mitchell, C.; Xu, Chen; Yuan-dong, Zhang; ZhI-hao, Wang; Webby, B.; Finney, S. (September 1997). "Definition of a global boundary stratotype for the Darriwilian Stage of the Ordovician System". Episodes. 20 (3): 158–166. Retrieved 13 December 2020.
"GSSP Table - Paleozoic Era". Geologic TimeScale Foundation. Retrieved 24 November 2012.Note: there is an apparent typo in the article referenced; they give the coordinates as "a latitude of 30°51’37.8"N and a longitude of 110°22’26.5"E", but their map and location description better corresponds to 30°51’37.8"N 111°22’26.5"E.
Wang, Xiaofeng; Stouge, Svend; Erdtmann, Bernd-D.; Chen, Xiaohong; Li, Zhihong; Wang, Chuanshang; Zeng, Qingluan; Zhou, Zhiqiang; Chen, Huiming (2005). "A proposed GSSP for the base of the Middle Ordovician Series: the Huanghuachang section, Yichang, China" (PDF). Episodes. 28 (2): 105–117. Retrieved 4 June 2013.
Wang, Xiaofeng; Stouge, Svend; Xiaohong, Chen; Zhihong, Li; Chuanshang, Wang; Finney, Stan C.; Qingluan, Zeng; Zhiqiang, Zhou; Huiming, Chen; Erdtmann, Bernd-D. (2009). "The Global Stratotype Section and Point for the base of the Middle Ordovician Series and the Third Stage (Dapingian)" (PDF). Episodes. 32 (2): 96–113. Retrieved 4 June 2013.
Gradstein, F. M., ed. (2012). The Geologic Time Scale 2012. Elsevier Science Ltd. p. 504. ISBN 978-0444594259.

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[1] Wellman, C.H.; Gray, J. (2000). "The microfossil record of early land plants". Phil. Trans. R. Soc. B. 355 (1398): 717–732. doi:10.1098/rstb.2000.0612. PMC 1692785. PMID 10905606.

[2] Korochantseva, Ekaterina; Trieloff, Mario; Lorenz, Cyrill; Buykin, Alexey; Ivanova, Marina; Schwarz, Winfried; Hopp, Jens; Jessberger, Elmar (2007). "L-chondrite asteroid breakup tied to Ordovician meteorite shower by multiple isochron 40 Ar- 39 Ar dating". Meteoritics & Planetary Science. 42 (1): 113–130. Bibcode:2007M&PS...42..113K. doi:10.1111/j.1945-5100.2007.tb00221.x.

[3] Lindskog, A.; Costa, M. M.; Rasmussen, C.M.Ø.; Connelly, J. N.; Eriksson, M. E. (2017-01-24). "Refined Ordovician timescale reveals no link between asteroid breakup and biodiversification". Nature Communications. 8: 14066. doi:10.1038/ncomms14066. ISSN 2041-1723. PMC 5286199. PMID 28117834. It has been suggested that the Middle Ordovician meteorite bombardment played a crucial role in the Great Ordovician Biodiversification Event, but this study shows that the two phenomena were unrelated

[4] Chen, Xu; Bergström, Stig; Zhang, Yuan-Dong; Fan, Jun-Xuan (2009). "The base of the Middle Ordovician in China with special reference to the succession at Hengtang near Jiangshan, Zhejiang Province, southern China" (PDF). Lethaia. 42: 218–231. doi:10.1111/j.1502-3931.2008.00148.x. Retrieved 13 December 2020.

[5] Mitchell, C.; Xu, Chen; Yuan-dong, Zhang; ZhI-hao, Wang; Webby, B.; Finney, S. (September 1997). "Definition of a global boundary stratotype for the Darriwilian Stage of the Ordovician System". Episodes. 20 (3): 158–166. Retrieved 13 December 2020.

[GSSP_Table_-_Paleozoic_Era-6] "GSSP Table - Paleozoic Era". Geologic TimeScale Foundation. Retrieved 24 November 2012.Note: there is an apparent typo in the article referenced; they give the coordinates as "a latitude of 30°51’37.8"N and a longitude of 110°22’26.5"E", but their map and location description better corresponds to 30°51’37.8"N 111°22’26.5"E.

[Wang_2005-7] Wang, Xiaofeng; Stouge, Svend; Erdtmann, Bernd-D.; Chen, Xiaohong; Li, Zhihong; Wang, Chuanshang; Zeng, Qingluan; Zhou, Zhiqiang; Chen, Huiming (2005). "A proposed GSSP for the base of the Middle Ordovician Series: the Huanghuachang section, Yichang, China" (PDF). Episodes. 28 (2): 105–117. Retrieved 4 June 2013.

[Wang_2009-8] Wang, Xiaofeng; Stouge, Svend; Xiaohong, Chen; Zhihong, Li; Chuanshang, Wang; Finney, Stan C.; Qingluan, Zeng; Zhiqiang, Zhou; Huiming, Chen; Erdtmann, Bernd-D. (2009). "The Global Stratotype Section and Point for the base of the Middle Ordovician Series and the Third Stage (Dapingian)" (PDF). Episodes. 32 (2): 96–113. Retrieved 4 June 2013.

[The_Geologic_Time_Scale_2012-9] Gradstein, F. M., ed. (2012). The Geologic Time Scale 2012. Elsevier Science Ltd. p. 504. ISBN 978-0444594259.