Author Correction: Early fungi from the Proterozoic era in Arctic Canada

International audience Fungi are crucial components of modern ecosystems. They may have had an important role in the colonization of land by eukaryotes, and in the appearance and success of land plants and metazoans(1-3). Nevertheless, fossils that can unambiguously be identified as fungi are absent...

Full description

Bibliographic Details
Published in:Nature
Main Authors: Loron, Corentin, François, Camille, Rainbird, Robert, Turner, Elizabeth, Borensztajn, Stephan, Javaux, Emmanuelle
Other Authors: Université de Liège, Geological Survey of Canada, Central Canada Division, Ottawa, Ontario K1A0E8, Canada, Harquail School of Earth Sciences, Laurentian University, Sudbury, Ontario, Canada, Institut de Physique du Globe de Paris (IPGP (UMR_7154)), Institut national des sciences de l'Univers (INSU - CNRS)-Université de La Réunion (UR)-Institut de Physique du Globe de Paris (IPG Paris)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité), Pfizer Fonds de la Recherche Scientifique - FNRS30442502ERC Stg ELiTE FP7/308074
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2019
Subjects:
KeyWords Plus:INFRARED FTIR SPECTROSCOPY
RAMAN-SPECTROSCOPY
SHALER SUPERGROUP
CELL-WALLS
DIVERSITY
HISTORY
LIFE
[SDU]Sciences of the Universe [physics]
Arctic
Canada
Online Access:https://hal-insu.archives-ouvertes.fr/insu-02914603
https://doi.org/10.1038/s41586-019-1396-8
Description
Summary:International audience Fungi are crucial components of modern ecosystems. They may have had an important role in the colonization of land by eukaryotes, and in the appearance and success of land plants and metazoans(1-3). Nevertheless, fossils that can unambiguously be identified as fungi are absent from the fossil record until the middle of the Palaeozoic era(4,5). Here we show, using morphological, ultrastructural and spectroscopic analyses, that multicellular organic-walled microfossils preserved in shale of the Grassy Bay Formation (Shaler Supergroup, Arctic Canada), which dates to approximately 1,010-890 million years ago, have a fungal affinity. These microfossils are more than half a billion years older than previously reported unambiguous occurrences of fungi, a date which is consistent with data from molecular clocks for the emergence of this clade(6,7). In extending the fossil record of the fungi, this finding also pushes back the minimum date for the appearance of eukaryotic crown group Opisthokonta, which comprises metazoans, fungi and their protist relatives(8,9).

Similar Items