Renewal of planktonic foraminifera diversity after the Cretaceous Paleogene mass extinction by benthic colonizers
Research output: Contribution to journal › Journal article › Research › peer-review
Standard
Renewal of planktonic foraminifera diversity after the Cretaceous Paleogene mass extinction by benthic colonizers. / Morard, Raphaël; Hassenrück, Christiane; Greco, Mattia; Fernandez-Guerra, Antonio; Rigaud, Sylvain; Douady, Christophe J.; Kucera, Michal.
In: Nature Communications, Vol. 13, 7135, 2022.Research output: Contribution to journal › Journal article › Research › peer-review
Harvard
APA
Vancouver
Author
Bibtex
}
RIS
TY - JOUR
T1 - Renewal of planktonic foraminifera diversity after the Cretaceous Paleogene mass extinction by benthic colonizers
AU - Morard, Raphaël
AU - Hassenrück, Christiane
AU - Greco, Mattia
AU - Fernandez-Guerra, Antonio
AU - Rigaud, Sylvain
AU - Douady, Christophe J.
AU - Kucera, Michal
N1 - Publisher Copyright: © 2022, The Author(s).
PY - 2022
Y1 - 2022
N2 - The biotic crisis following the end-Cretaceous asteroid impact resulted in a dramatic renewal of pelagic biodiversity. Considering the severe and immediate effect of the asteroid impact on the pelagic environment, it is remarkable that some of the most affected pelagic groups, like the planktonic foraminifera, survived at all. Here we queried a surface ocean metabarcoding dataset to show that calcareous benthic foraminifera of the clade Globothalamea are able to disperse actively in the plankton, and we show using molecular clock phylogeny that the modern planktonic clades originated from different benthic ancestors that colonized the plankton after the end-Cretaceous crisis. We conclude that the diversity of planktonic foraminifera has been the result of a constant leakage of benthic foraminifera diversity into the plankton, continuously refueling the planktonic niche, and challenge the classical interpretation of the fossil record that suggests that Mesozoic planktonic foraminifera gave rise to the modern communities.
AB - The biotic crisis following the end-Cretaceous asteroid impact resulted in a dramatic renewal of pelagic biodiversity. Considering the severe and immediate effect of the asteroid impact on the pelagic environment, it is remarkable that some of the most affected pelagic groups, like the planktonic foraminifera, survived at all. Here we queried a surface ocean metabarcoding dataset to show that calcareous benthic foraminifera of the clade Globothalamea are able to disperse actively in the plankton, and we show using molecular clock phylogeny that the modern planktonic clades originated from different benthic ancestors that colonized the plankton after the end-Cretaceous crisis. We conclude that the diversity of planktonic foraminifera has been the result of a constant leakage of benthic foraminifera diversity into the plankton, continuously refueling the planktonic niche, and challenge the classical interpretation of the fossil record that suggests that Mesozoic planktonic foraminifera gave rise to the modern communities.
U2 - 10.1038/s41467-022-34794-5
DO - 10.1038/s41467-022-34794-5
M3 - Journal article
C2 - 36414628
AN - SCOPUS:85142239704
VL - 13
JO - Nature Communications
JF - Nature Communications
SN - 2041-1723
M1 - 7135
ER -
ID: 329613054