The Tooth of Time: Lauge Koch's Last Lecture

Hoffman, Paul F.

doi:10.12789/geocanj.2013.40.018

2013

DOI: 10.12789/geocanj.2013.40.018

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The Tooth of Time: Lauge Koch's Last Lecture

Paul F. Hoffman

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2023

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The Ordovician System in Greenland

Stouge

Rasmussen

Harper

2023

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Ordovician strata in Greenland are extensively exposed in North Greenland and northern East Greenland; additional small traces (loose blocks) are recorded from the craton of West Greenland. The western North Greenland succession, is nearly identical to that of the Franklinian basin exposed in Ellesmere Island, Arctic Canada; the eastern North Greenland represents the (present) northeastern corner of Laurentia and provides the connection to the East Greenland Caledonian platform. The northern East Greenland succession is the natural northern extension of the Caledonian platform of northern Europe and the Appalachian platform of eastern North America. During the Ordovician Greenland occupied a palaeogeographical subtropical to tropical position with a faunal assemblage typical of Laurentia. A prominent faunal peak of diversification occurred in the Late Ordovician. The stratigraphical succession of Greenland is summarized and age relationships are discussed with reference to the fossil faunas and breaks in the sequences and correlation between the locations and regions are provided.

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The Ordovician System in Greenland

Stouge

Rasmussen

Harper

2023

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The Tooth of Time: Lauge Koch's Last Lecture

Cited by 1 publication

References 36 publications

The Ordovician System in Greenland

The Ordovician System in Greenland

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