Poxviruses capture host genes by LINE-1 retrotransposition
- University of Utah, United States
- University of California, Davis, United States
Abstract
Horizontal gene transfer (HGT) provides a major source of genetic variation. Many viruses, including poxviruses, encode genes with crucial functions directly gained by gene transfer from hosts. The mechanism of transfer to poxvirus genomes is unknown. Using genome analysis and experimental screens of infected cells, we discovered a central role for Long Interspersed Nuclear Element-1 (LINE-1) retrotransposition in HGT to virus genomes. The process recapitulates processed pseudogene generation, but with host messenger RNA directed into virus genomes. Intriguingly, hallmark features of retrotransposition appear to favor virus adaption through rapid duplication of captured host genes on arrival. Our study reveals a previously unrecognized conduit of genetic traffic with fundamental implications for the evolution of many virus classes and their hosts.
Data availability
Sequencing data have been deposited in the NCBI SRA database under project code PRJNA614958.All data generated or analyses during this study are included in the manuscript and supplemental files.
Article and author information
Author details
Funding
National Institutes of Health (R35GM134936)
- Nels C Elde
National Institutes of Health (T32GM007464)
- Sarah M Fixsen
- Thomas A Sasani
National Institutes of Health (T32AI055434)
- Kelsey R Cone
Burroughs Wellcome Fund (1015462)
- Nels C Elde
University of Utah (HA and Edna Benning Presidential Endowed Chair)
- Nels C Elde
National Institutes of Health (R01AI146915)
- Stefan Rothenburg
The funders had no role in study design, data collection and interpretation, or the decision to submit the work for publication.
Copyright
© 2022, Fixsen et al.
This article is distributed under the terms of the Creative Commons Attribution License permitting unrestricted use and redistribution provided that the original author and source are credited.
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Poxviruses capture host genes by LINE-1 retrotransposition
eLife 11:e63332.
https://doi.org/10.7554/eLife.63332
Further reading
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- Evolutionary Biology
- Microbiology and Infectious Disease
As long suspected, poxviruses capture host genes through a reverse-transcription process now shown to be mediated by retrotransposons.
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- Evolutionary Biology
Living organisms control the formation of mineral skeletons and other structures through biomineralization. Major phylogenetic groups usually consistently follow a single biomineralization pathway. Foraminifera, which are very efficient marine calcifiers, making a substantial contribution to global carbonate production and global carbon sequestration, are regarded as an exception. This phylum has been commonly thought to follow two contrasting models of either in situ ‘mineralization of extracellular matrix’ attributed to hyaline rotaliid shells, or ‘mineralization within intracellular vesicles’ attributed to porcelaneous miliolid shells. Our previous results on rotaliids along with those on miliolids in this paper question such a wide divergence of biomineralization pathways within the same phylum of Foraminifera. We have found under a high-resolution scanning electron microscopy (SEM) that precipitation of high-Mg calcitic mesocrystals in porcelaneous shells takes place in situ and form a dense, chaotic meshwork of needle-like crystallites. We have not observed calcified needles that already precipitated in the transported vesicles, what challenges the previous model of miliolid mineralization. Hence, Foraminifera probably utilize less divergent calcification pathways, following the recently discovered biomineralization principles. Mesocrystalline chamber walls in both models are therefore most likely created by intravesicular accumulation of pre-formed liquid amorphous mineral phase deposited and crystallized within the extracellular organic matrix enclosed in a biologically controlled privileged space by active pseudopodial structures. Both calcification pathways evolved independently in the Paleozoic and are well conserved in two clades that represent different chamber formation modes.
