Dresbachian

The Dresbachian is a Maentwrogian regional stage of North America, lasting from 501 to 497 million years ago.[1] It is part of the Upper Cambrian and is defined by four trilobite zones. It overlaps with the ICS-stages Guzhangian, Paibian and the lowest Jiangshanian.

Key events in the Cambrian

-540 —

–

-535 —

–

-530 —

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-525 —

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-520 —

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-515 —

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-510 —

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-505 —

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-500 —

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-495 —

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-490 —

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-485 —

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N
P
Z

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Ediacaran

C
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Ordovician

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S
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2

M
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F
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Fortunian

"Stage 2"

"Stage 3"

"Stage 4"

Wuliuan

Drumian

Guzhangian

Paibian

Jiangshanian

"Stage 10"

 

 

 

 

 

 

 

 

 

 

←

Orsten Fauna

←

Burgess Shale

←

Kaili biota

←

Archaeocyatha extinction

←

Emu Bay Shale

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Sirius Passet biota

←

Chengjiang biota

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First Trilobites

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SSF diversification, first brachiopods & archaeocyatha

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First halkieriids, mollusсs, hyoliths SSF

←

Treptichnus pedum trace
Large negative peak δ 13C_carb excursion

←

Baykonurian glaciation

 Major Glacial period

Stratigraphic scale of the ICS subdivisions and Precambrian/Cambrian boundary.

The Dresbachian overlies the Middle Cambrian Albertan series, and is the lowest stage of the Upper Cambrian Croixian series, followed by the Franconian stage. The Dresbachian extinction event, about 502 million years ago, was followed by the Cambrian–Ordovician extinction event about 485.4 million years ago.

Naming

The term is derived from the town of Dresbach which is located in southeastern Minnesota on the Mississippi River.

Definition

The Dresbachian is defined by four trilobite zones: Cedaria-, Crepicephalus-, Aphelaspis- and Dunderbergia trilobite zones.

Intensity of Dresbachian extinction event (right side of graph)

Events

The Dresbachian extinction event during the Late Cambrian was the second of two severe extinctions during the first period of the Paleozoic era; the first being the End-Botomian extinction event during the Middle Cambrian. According to data on extinction intensity (see below), both extinction events slashed approximately 40 percent of marine genera. However, the two are poorly documented due to a paucity of fossil evidence so early in the evolution of life.

References

1. https://engineering.purdue.edu/Stratigraphy/resources/geowhen/stages/Maentwrogian.html

• Chen Jun-yuan & Teichert C, 1983; "Cambrian Cephalopods", Geology Vol 11, pp647–650, Nov 1983
• Flower R.H.1964, The Nautiloid Order Ellesmerocerida (Cephalopoda) Menoir 12, New Mexico Bureau of Mines and Mineral Resources, Socorro, NM
• Harland, W. B. et al. 1990. A Geologic Time Scale 1989. Cambridge University Press, Cambridge . Ref in Paleobiology Database on line.
• Moore, Lalicker, and Fischer 1952; Invertebrate Fossils; McGraw-Hill; fig 1-17.
• Geowhen database.