Jiangshanium

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system series step ≈ age ( mya )
higher higher higher younger
Cambrian Furongium 10th stage 485.4

489.5
Jiangshanium 489.5

494
Paibium 494

497
Miaolingium Guzhangium 497

500.5
Drumium 500.5

504.5
Wuliuum 504.5

509
2nd series 4th stage 509

514
3rd stage 514

521
Terreneuvium 2nd stage 521

529
Fortunium 529

541
deeper

The Jiangshanium is the middle chronostratigraphic stage of the Furongian series of the Cambrian in geological history . The Jiangshanium is underlain by the Paibium and overlaid by the as yet unnamed 10th stage of the Cambrian. The Jiangshanium lasted approximately from 494 million years to 489.5 million years (interpolated).

Naming and history

The name of the stage was ratified in September 2011. It is named after the Chinese town of Jiangshan in Zhejiang Province .

Definition and GSSP

The lower limit is due to the first appearance of the globally occurring trilobite species Agnostotes orientalis . It also correlates with the first appearance of the trilobite species Irvingella angustilimbata . The upper limit will presumably be defined by the first appearance of the trilobite species Lotagnostus americanus . The 10th stage of the Cambrian has not yet been named and the lower limit has not yet been formally established.

The GSSP (Global Standard-stratotype Section and Points) is a profile in the village of Duibian (Duibian B Section), north of Jiangshan (western Zhejiang province, China). The GSSP is in profile 108.12 m above the base of the Huayansi Formation.

literature

  • Peng Shanchi, Zhu Xuejian, Zuo Jinxun, Lin Huanling, Chen Yong'an, Wang Longwu: Recently Ratified and Proposed Cambrian Global Standard Stratotype-section and Points. Acta Geologica Sinica, 2011 (2): 296-308 abstract

Web links

Individual evidence

  1. ^ GSSP defining the base of the Jiangshanian Stage of the Furongian Series and Cambrian System ratified by IUGS 2011-09-01. Retrieved September 24, 2011
  2. GSSP Table - Paleozoic Era Global Boundary Stratotype Section and Point (GSSP) of the International Commission of Stratigraphy