The Ordovician Succession Adjacent to Hinlopenstretet, Ny Friesland, Spitsbergen
The Ordovician sections along the western shore of the Hinlopen Strait, Ny Friesland, Spitsbergen were discovered in the late 1960s and since then prompted numerous paleontological publications; several of these publications are now considered classical in the literature of paleontology of Ordovicia...
Published in: | American Museum Novitates |
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American Museum of Natural History
2017
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Online Access: | https://doi.org/10.1206/3882.1 |
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ftbioone:10.1206/3882.1 2024-06-02T08:07:50+00:00 The Ordovician Succession Adjacent to Hinlopenstretet, Ny Friesland, Spitsbergen Björn Kröger Seth Finnegan Franziska Franeck Melanie J. Hopkins Björn Kröger Seth Finnegan Franziska Franeck Melanie J. Hopkins world 2017-09-05 text/HTML https://doi.org/10.1206/3882.1 en eng American Museum of Natural History doi:10.1206/3882.1 All rights reserved. https://doi.org/10.1206/3882.1 Text 2017 ftbioone https://doi.org/10.1206/3882.1 2024-05-07T01:03:04Z The Ordovician sections along the western shore of the Hinlopen Strait, Ny Friesland, Spitsbergen were discovered in the late 1960s and since then prompted numerous paleontological publications; several of these publications are now considered classical in the literature of paleontology of Ordovician trilobites and of Ordovician paleogeography and stratigraphy. Our 2016 expedition aimed at a major recollection and reappraisal of these classical sites. Here we provide a first high-resolution lithological description of the Kirtonryggen and Valhallfonna formations (Tremadocian—Darriwilian), which together comprise a thickness of 843 m, a revised bio-, and lithostratigraphy, and an interpretation of the depositional sequences. We find that the sedimentary succession is very similar to successions of eastern Laurentia; its Tremadocian and early Floian part is composed of predominantly peritidal dolostones and limestones characterized by ribbon carbonates, intraclastic conglomerates, microbial laminites, and stromatolites, and its late Floian to Darriwilian part is composed of fossil-rich, bioturbated, cherty mud-wackestone, skeletal grainstone and shale, with local siltstone and glauconitic horizons. The succession can be subdivided into five third-order depositional sequences, which are interpreted as representing the Sauk IIIB Supersequence known from elsewhere on the Laurentian platform. Text Hinlopen Strait Ny Friesland Spitsbergen BioOne Online Journals Hinlopenstretet ENVELOPE(20.728,20.728,79.246,79.246) Ny Friesland ENVELOPE(16.847,16.847,79.498,79.498) Valhallfonna ENVELOPE(17.566,17.566,79.743,79.743) American Museum Novitates 3882 3882 1 28 |
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English |
description |
The Ordovician sections along the western shore of the Hinlopen Strait, Ny Friesland, Spitsbergen were discovered in the late 1960s and since then prompted numerous paleontological publications; several of these publications are now considered classical in the literature of paleontology of Ordovician trilobites and of Ordovician paleogeography and stratigraphy. Our 2016 expedition aimed at a major recollection and reappraisal of these classical sites. Here we provide a first high-resolution lithological description of the Kirtonryggen and Valhallfonna formations (Tremadocian—Darriwilian), which together comprise a thickness of 843 m, a revised bio-, and lithostratigraphy, and an interpretation of the depositional sequences. We find that the sedimentary succession is very similar to successions of eastern Laurentia; its Tremadocian and early Floian part is composed of predominantly peritidal dolostones and limestones characterized by ribbon carbonates, intraclastic conglomerates, microbial laminites, and stromatolites, and its late Floian to Darriwilian part is composed of fossil-rich, bioturbated, cherty mud-wackestone, skeletal grainstone and shale, with local siltstone and glauconitic horizons. The succession can be subdivided into five third-order depositional sequences, which are interpreted as representing the Sauk IIIB Supersequence known from elsewhere on the Laurentian platform. |
author2 |
Björn Kröger Seth Finnegan Franziska Franeck Melanie J. Hopkins |
format |
Text |
author |
Björn Kröger Seth Finnegan Franziska Franeck Melanie J. Hopkins |
spellingShingle |
Björn Kröger Seth Finnegan Franziska Franeck Melanie J. Hopkins The Ordovician Succession Adjacent to Hinlopenstretet, Ny Friesland, Spitsbergen |
author_facet |
Björn Kröger Seth Finnegan Franziska Franeck Melanie J. Hopkins |
author_sort |
Björn Kröger |
title |
The Ordovician Succession Adjacent to Hinlopenstretet, Ny Friesland, Spitsbergen |
title_short |
The Ordovician Succession Adjacent to Hinlopenstretet, Ny Friesland, Spitsbergen |
title_full |
The Ordovician Succession Adjacent to Hinlopenstretet, Ny Friesland, Spitsbergen |
title_fullStr |
The Ordovician Succession Adjacent to Hinlopenstretet, Ny Friesland, Spitsbergen |
title_full_unstemmed |
The Ordovician Succession Adjacent to Hinlopenstretet, Ny Friesland, Spitsbergen |
title_sort |
ordovician succession adjacent to hinlopenstretet, ny friesland, spitsbergen |
publisher |
American Museum of Natural History |
publishDate |
2017 |
url |
https://doi.org/10.1206/3882.1 |
op_coverage |
world |
long_lat |
ENVELOPE(20.728,20.728,79.246,79.246) ENVELOPE(16.847,16.847,79.498,79.498) ENVELOPE(17.566,17.566,79.743,79.743) |
geographic |
Hinlopenstretet Ny Friesland Valhallfonna |
geographic_facet |
Hinlopenstretet Ny Friesland Valhallfonna |
genre |
Hinlopen Strait Ny Friesland Spitsbergen |
genre_facet |
Hinlopen Strait Ny Friesland Spitsbergen |
op_source |
https://doi.org/10.1206/3882.1 |
op_relation |
doi:10.1206/3882.1 |
op_rights |
All rights reserved. |
op_doi |
https://doi.org/10.1206/3882.1 |
container_title |
American Museum Novitates |
container_volume |
3882 |
container_issue |
3882 |
container_start_page |
1 |
op_container_end_page |
28 |
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1800752973322649600 |