Format
Sort by
Items per page

Send to

Choose Destination

Search results

Items: 10

1.

Organism motility in an oxygenated shallow-marine environment 2.1 billion years ago.

El Albani A, Mangano MG, Buatois LA, Bengtson S, Riboulleau A, Bekker A, Konhauser K, Lyons T, Rollion-Bard C, Bankole O, Lekele Baghekema SG, Meunier A, Trentesaux A, Mazurier A, Aubineau J, Laforest C, Fontaine C, Recourt P, Chi Fru E, Macchiarelli R, Reynaud JY, Gauthier-Lafaye F, Canfield DE.

Proc Natl Acad Sci U S A. 2019 Feb 26;116(9):3431-3436. doi: 10.1073/pnas.1815721116. Epub 2019 Feb 11.

2.

Ediacaran biozones identified with network analysis provide evidence for pulsed extinctions of early complex life.

Muscente AD, Bykova N, Boag TH, Buatois LA, Mángano MG, Eleish A, Prabhu A, Pan F, Meyer MB, Schiffbauer JD, Fox P, Hazen RM, Knoll AH.

Nat Commun. 2019 Feb 22;10(1):911. doi: 10.1038/s41467-019-08837-3.

3.

Unusual microbial mat-related structural diversity 2.1 billion years ago and implications for the Francevillian biota.

Aubineau J, El Albani A, Chi Fru E, Gingras M, Batonneau Y, Buatois LA, Geffroy C, Labanowski J, Laforest C, Lemée L, Mángano MG, Meunier A, Pierson-Wickmann AC, Recourt P, Riboulleau A, Trentesaux A, Konhauser KO.

Geobiology. 2018 Sep;16(5):476-497. doi: 10.1111/gbi.12296. Epub 2018 Jun 20.

PMID:
29923673
4.

Early Cambrian origin of the shelf sediment mixed layer.

Gougeon RC, Mángano MG, Buatois LA, Narbonne GM, Laing BA.

Nat Commun. 2018 May 15;9(1):1909. doi: 10.1038/s41467-018-04311-8.

5.

Sediment disturbance by Ediacaran bulldozers and the roots of the Cambrian explosion.

Buatois LA, Almond J, Mángano MG, Jensen S, Germs GJB.

Sci Rep. 2018 Mar 14;8(1):4514. doi: 10.1038/s41598-018-22859-9.

6.

The impact of deep-tier burrow systems in sediment mixing and ecosystem engineering in early Cambrian carbonate settings.

Zhang LJ, Qi YA, Buatois LA, Mángano MG, Meng Y, Li D.

Sci Rep. 2017 Apr 4;7:45773. doi: 10.1038/srep45773.

7.

Decoupled evolution of soft and hard substrate communities during the Cambrian Explosion and Great Ordovician Biodiversification Event.

Buatois LA, Mángano MG, Olea RA, Wilson MA.

Proc Natl Acad Sci U S A. 2016 Jun 21;113(25):6945-8. doi: 10.1073/pnas.1523087113. Epub 2016 May 31.

8.

Ediacaran matground ecology persisted into the earliest Cambrian.

Buatois LA, Narbonne GM, Mángano MG, Carmona NB, Myrow P.

Nat Commun. 2014 Mar 28;5:3544. doi: 10.1038/ncomms4544.

PMID:
24675373
9.

Decoupling of body-plan diversification and ecological structuring during the Ediacaran-Cambrian transition: evolutionary and geobiological feedbacks.

Mángano MG, Buatois LA.

Proc Biol Sci. 2014 Feb 12;281(1780):20140038. doi: 10.1098/rspb.2014.0038. Print 2014 Apr 7.

10.

Global deglaciation and the re-appearance of microbial matground-dominated ecosystems in the late Paleozoic of Gondwana.

Buatois LA, Netto RG, Gabriela Mángano M, Carmona NB.

Geobiology. 2013 Jul;11(4):307-17. doi: 10.1111/gbi.12038. Epub 2013 Apr 29.

PMID:
23621394

Supplemental Content

Loading ...
Support Center