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Coordinated biotic and abiotic change during the Great Ordovician Biodiversification Event: Darriwilian assembly of early Paleozoic building blocks

Palaeogeography, palaeoclimatology, palaeoecology, 2019-09, Vol.530, p.249-270

2019

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End Ordovician extinctions: A coincidence of causes

Gondwana research, 2014-05, Vol.25 (4), p.1294-1307

2014

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The onset of the ‘Ordovician Plankton Revolution’ in the late Cambrian

Palaeogeography, palaeoclimatology, palaeoecology, 2016-09, Vol.458, p.12-28

2016

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A Gondwanan perspective on the Ordovician Radiation constrains its temporal duration and suggests first wave of speciation, fuelled by Cambrian clades

Lethaia, 2018-04, Vol.51 (2), p.286-295

2018

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Cascading trend of Early Paleozoic marine radiations paused by Late Ordovician extinctions

Proceedings of the National Academy of Sciences - PNAS, 2019-04, Vol.116 (15), p.7207-7213

2019

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Building mountain biodiversity: Geological and evolutionary processes

Science (American Association for the Advancement of Science), 2019-09, Vol.365 (6458), p.1114-1119

2019

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The evolutionary dynamics of the early Palaeozoic marine biodiversity accumulation

Proceedings of the Royal Society. B, Biological sciences, 2019-08, Vol.286 (1909), p.20191634-20191634

2019

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Warm-water Tcherskidium fauna (Brachiopoda) in the Late Ordovician Northern Hemisphere of Laurentia and peri-Laurentia

Journal of paleontology, 2022-11, Vol.96 (6), p.1461-1478

2022

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Was the Late Ordovician mass extinction truly exceptional?

Trends in ecology & evolution (Amsterdam), 2023-09, Vol.38 (9), p.812-821

2023

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Onset of main Phanerozoic marine radiation sparked by emerging Mid Ordovician icehouse

Scientific reports, 2016-01, Vol.6 (1), p.18884-18884, Article 18884

2016

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The Ordovician System in Greenland

Geological Society special publication, 2023-06, Vol.533 (1), p.27-64

2023

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Biogeographic and bathymetric determinants of brachiopod extinction and survival during the Late Ordovician mass extinction

Proceedings of the Royal Society. B, Biological sciences, 2016-04, Vol.283 (1829), p.20160007

2016

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Carbon isotope chemostratigraphy and sea-level history of the Hirnantian Stage (uppermost Ordovician) in the Oslo–Asker district, Norway

Geological magazine, 2021-11, Vol.158 (11), p.1977-2008

2021

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Upper Ordovician carbon isotope chemostratigraphy and a high-resolution assessment of the Hirnantian Stage in the Baltic Sea subsurface

GFF, 2024-05, p.1-31

2024

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A multidisciplinary perspective on the Great Ordovician Biodiversification Event and the development of the early Paleozoic world

Palaeogeography, palaeoclimatology, palaeoecology, 2020-04, Vol.543, p.109521, Article 109521

2020

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Precisely locating the Ordovician equator in Laurentia

Geology (Boulder), 2013-02, Vol.41 (2), p.107-110

2013

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Late Ordovician and early Silurian virgianid and stricklandioid brachiopods from North Greenland: implications for a warm‐water faunal province

Papers in palaeontology, 2024-01, Vol.10 (1), p.n/a

2024

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Identifying the most surprising victims of mass extinction events: an example using Late Ordovician brachiopods

Biology letters (2005), 2017-09, Vol.13 (9), p.20170400-20170400

2017

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Did the amalgamation of continents drive the end Ordovician mass extinctions?

Palaeogeography, palaeoclimatology, palaeoecology, 2011-10, Vol.311 (1), p.48-62

2011

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Middle Ordovician carbonate facies development, conodont biostratigraphy and faunal diversity patterns at the Lynna River, northwestern Russia

Estonian journal of earth sciences, 2020-01, Vol.69 (1), p.37

2020

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Subaerial speleothems and deep karst in central Sweden linked to Hirnantian glaciations

Journal of the Geological Society, 2015-05, Vol.172 (3), p.349-356

2015

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Interrogation of distributional data for the End Ordovician crisis interval: where did disaster strike?

Geological journal (Chichester, England), 2011-09, Vol.46 (5), p.478-500

2011

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Unravelling a Late Ordovician pentameride (Brachiopoda) hotspot from the Boda Limestone, Siljan district, central Sweden

GFF, 2010-09, Vol.132 (3-4), p.133-152

2010

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Ecostratigraphical interpretation of lower Middle Ordovician East Baltic sections based on brachiopods

Geological magazine, 2009-09, Vol.146 (5), p.717-731

2009

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The Late Ordovician extinction conundrum

Estonian journal of earth sciences, 2023-03, Vol.72 (1), p.156-156

Rasmussen, Christian M.O

2023

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Coordinated biotic and abiotic change during the Great Ordovician Biodiversification Event: Darriwilian assembly of early Paleozoic building blocks

End Ordovician extinctions: A coincidence of causes

The onset of the ‘Ordovician Plankton Revolution’ in the late Cambrian

A Gondwanan perspective on the Ordovician Radiation constrains its temporal duration and suggests first wave of speciation, fuelled by Cambrian clades

Cascading trend of Early Paleozoic marine radiations paused by Late Ordovician extinctions

Building mountain biodiversity: Geological and evolutionary processes

The evolutionary dynamics of the early Palaeozoic marine biodiversity accumulation

Warm-water Tcherskidium fauna (Brachiopoda) in the Late Ordovician Northern Hemisphere of Laurentia and peri-Laurentia

Was the Late Ordovician mass extinction truly exceptional?

Onset of main Phanerozoic marine radiation sparked by emerging Mid Ordovician icehouse

The Ordovician System in Greenland

Biogeographic and bathymetric determinants of brachiopod extinction and survival during the Late Ordovician mass extinction

Carbon isotope chemostratigraphy and sea-level history of the Hirnantian Stage (uppermost Ordovician) in the Oslo–Asker district, Norway

Upper Ordovician carbon isotope chemostratigraphy and a high-resolution assessment of the Hirnantian Stage in the Baltic Sea subsurface

A multidisciplinary perspective on the Great Ordovician Biodiversification Event and the development of the early Paleozoic world

Precisely locating the Ordovician equator in Laurentia

Late Ordovician and early Silurian virgianid and stricklandioid brachiopods from North Greenland: implications for a warm‐water faunal province

Identifying the most surprising victims of mass extinction events: an example using Late Ordovician brachiopods

Did the amalgamation of continents drive the end Ordovician mass extinctions?

Middle Ordovician carbonate facies development, conodont biostratigraphy and faunal diversity patterns at the Lynna River, northwestern Russia

Subaerial speleothems and deep karst in central Sweden linked to Hirnantian glaciations

Interrogation of distributional data for the End Ordovician crisis interval: where did disaster strike?

Unravelling a Late Ordovician pentameride (Brachiopoda) hotspot from the Boda Limestone, Siljan district, central Sweden

Ecostratigraphical interpretation of lower Middle Ordovician East Baltic sections based on brachiopods

The Late Ordovician extinction conundrum

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