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Items: 5

1.

The nature of Ordovician limestone-marl alternations in the Oslo-Asker District (Norway): witnesses of primary glacio-eustasy or diagenetic rhythms?

Amberg CE, Collart T, Salenbien W, Egger LM, Munnecke A, Nielsen AT, Monnet C, Hammer Ø, Vandenbroucke TR.

Sci Rep. 2016 Jan 7;6:18787. doi: 10.1038/srep18787.

2.

Metal-induced malformations in early Palaeozoic plankton are harbingers of mass extinction.

Vandenbroucke TRA, Emsbo P, Munnecke A, Nuns N, Duponchel L, Lepot K, Quijada M, Paris F, Servais T, Kiessling W.

Nat Commun. 2015 Aug 25;6:7966. doi: 10.1038/ncomms8966.

3.

A Cenozoic-style scenario for the end-Ordovician glaciation.

Ghienne JF, Desrochers A, Vandenbroucke TR, Achab A, Asselin E, Dabard MP, Farley C, Loi A, Paris F, Wickson S, Veizer J.

Nat Commun. 2014 Sep 1;5:4485. doi: 10.1038/ncomms5485.

4.

Marine ostracod provinciality in the Late Ordovician of palaeocontinental Laurentia and its environmental and geographical expression.

Mohibullah M, Williams M, Vandenbroucke TR, Sabbe K, Zalasiewicz JA.

PLoS One. 2012;7(8):e41682. doi: 10.1371/journal.pone.0041682. Epub 2012 Aug 10.

5.

Polar front shift and atmospheric CO2 during the glacial maximum of the Early Paleozoic Icehouse.

Vandenbroucke TR, Armstrong HA, Williams M, Paris F, Zalasiewicz JA, Sabbe K, Nõlvak J, Challands TJ, Verniers J, Servais T.

Proc Natl Acad Sci U S A. 2010 Aug 24;107(34):14983-6. doi: 10.1073/pnas.1003220107. Epub 2010 Aug 9.

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