View/edit a dataset - stages South China (Jur -> Camb)

This page allows you to view all the information for a dataset, i.e. for a set of events and the intervals that they define, including the definitions of the basal events and the data used to set their age. The columns are also plotted. See the introduction page and the notes on table creation for more information

1. Select dataset

Dataset:

2. Select columns & time interval

Top stage/age: Base stage/age: cm per Ma:
columnsfields
Draw all events column Show added abbreviations in the table
Mode selector: View selected - change to edit mode if you want to edit the metadata
OPTIONS SET Dataset: stages South China (Jur -> Camb) Age window: 0-->500 Ma

Dataset metadata

Name: id:26 sort: 0000000250 Dataset type:
TSC_source_notes:
compilation_notes:
Cenozoic notes &
compilation notes
Cretaceous notes &
compilation notes
Jurassic notes &
compilation notes
Triassic notes &
compilation notes
Permo-Carboniferous notes &
compilation notes
Devonian notes &
compilation notes
Silurian-Ordovician notes &
compilation notes
Cambrian notes &
compilation notes
refs to add:
Linked refs:Henderson & Shen 2020;Henderson 2020;Henderson et al. 2012a;Menning et al. 2006;Ogg et al. 2016b;Peng 2003;Peng et al. 2020c;Shen et al. 2019b;Zhang et al. 2019b;
Interval Colour:
Event Colour:
Added abbreviations:
interval types:
prefix(es):

Missing references:Shuzhong et al. 2019; Zhang & Zhan 2019; Zhang & Zhou 2007; sorry, these are not in the bibliography yet insert new entry

Dataset References ↑

Henderson, C. M. & Shen, S. -Z. (2020). Chapter 24 - The Permian Period. In, Gradstein, F. M. , Ogg, J. G. , Schmitz, M. D. , and Ogg, G. M. (ed.) The Geologic Time Scale 2020. Elsevier, Boston, MA 2: 875-902. gs

Henderson, C. M. (2020). Chapter 3D - Conodonts. In, Gradstein, F. M. , Ogg, J. G. , Schmitz, M. D. , and Ogg, G. M. (ed.) The Geologic Time Scale 2020. Elsevier, Boston, MA 1: 56-60. gs

Henderson, C. M., Davydov, V. I. & Wardlaw, B. R. (2012a). The Permian Period. In, Gradstein, F. , et al. , (ed.) The Geologic Time Scale 2012. Amsterdam: Elsevier Press 653-679. gs

Menning, M., et al. (2006). Global Time Scale and regional stratigraphic reference scales of central and west Europe, east Europe, Tethys, south China, and North America as used in the Devonian-Carboniferous-Permian correlation chart 2003 (DCP 2003). Palaeogeography Palaeoclimatology Palaeoecology. 240: 318-372. gs

Ogg, J. G., Ogg, G. M. & Gradstein, F. M. (2016b). A Concise Geologic Time Scale 2016. Elsevier, Amsterdam. 1-234. gs

Peng, S. C. (2003). Chronostratigraphic subdivision of the Cambrian of China. Geologica Acta. 1(1): 135-144. gs

Peng, S. C., Babcock, L. E. & Ahlberg, P. (2020c). Chapter 19 - The Cambrian Period. In, Gradstein, F. M. , Ogg, J. G. , Schmitz, M. D. , and Ogg, G. M. (ed.) The Geologic Time Scale 2020. Elsevier, Boston, MA 2: 565-630. gs

Shen, S. Z., et al. (2019b). Permian integrative stratigraphy and timescale of China. Science in China. Series D Earth Sciences 62: 154-188. gs

Zhang, Y. -D., et al. (2019b). Ordovician integrative stratigraphy and time scale of China. Science in China. Series D Earth Sciences 62: 61-88. gs

Dataset content

ideventxagenotes_2020
6319FAD Morozovella aragonensis52.4584Defines P7 (=E5) base. Berggren and Pearson (2005), which is same chron-age calibration as Berggren et al. (1995a) -- ’Morozovella argonensis’ FAD is recorded in North Atlantic Hole 550, North Pacific Shatsky Rise Hole 577 and in Chron C23r in South Atlantic (Walvis Ridge) Hole 527. Their 52.3 Ma age is at Chron C23r.1 on their polarity scale. [NOTE: The Wade et al. (2011) table based on Berggren-Pearson (2005) lists the same 52.3 Ma, which suggests they didn’t convert to the chron-ages of the GTS04 magnetic scale.]
6326LAD Morozovella velascoensis55.1484DASH (but Wade requested J.Ogg to remove "dash" via e-mail 18July2011) -- Wade et al. (2011) projects as 54.9 Ma relative to GTS04 polarity chrons, therefore at Chron C24r.61 (used here). Berggren and Pearson (2005), puts this LAD 0.2 myr higher than Berggren et al. (1995a) -- This LAD is recorded in younger part of Chron C24r in Hole 577 and in mid-C24r in Hole 577 (at 81.98 m). However, paleomagnetic data (Bleil, 1985, DSDP Leg 86: 449, Fig. 7b) suggests a hiatus occurs between ~82m & 83 m in Hole 577, which would have the effect of depressing (rendering older) the HO of ’M. velascoensis’. The HO of ’M. velascoensis’ in Hole 577 is in Nannofossil zone CP8 (=NP9) (Monechi, 1985: 310, Table 5) which supports interpretation of hiatus in Hole 577, because the LO of ’M. valascoensis’ is in Nannofossil Zone NP10. Furthermore, Monechi (1985: p.307) indicates absence of extremely condensed sedimentation across the Paleocene/Eocene boundary interval. Essentially, it is not yet possible to position this LAD proportionally within the long Chron C24r.
8917top UT28n.2n200.23
8920base UT28n.1n201.4TJB-N/UT28n.1n
10581base Bashkirian323.4
10580base Serpukhovian GTS04 definition328.96Retained here, because relative scaling of Davydov zones and magnetics used this duration

Column mock-up

This column mock-up plot is a simple plot of the data to allow visual comparison with the output from TimeScale Creator

The data plotted here are the columns from the stages South China (Jur -> Camb) dataset for the interval 0 - 500 Ma

The all events column is an optional extra column showing the interval tops and bases as well as the other events in the dataset. This does not correspond to a TSC column, but is useful for checking data.

finished!