|
|
|
|
LEADER |
01798 am a22002173u 4500 |
001 |
61263 |
042 |
|
|
|a dc
|
100 |
1 |
0 |
|a David, Lawrence A.
|e author
|
100 |
1 |
0 |
|a Massachusetts Institute of Technology. Department of Biological Engineering
|e contributor
|
100 |
1 |
0 |
|a Massachusetts Institute of Technology. Department of Civil and Environmental Engineering
|e contributor
|
100 |
1 |
0 |
|a Alm, Eric J.
|e contributor
|
100 |
1 |
0 |
|a Alm, Eric J.
|e contributor
|
100 |
1 |
0 |
|a David, Lawrence A.
|e contributor
|
700 |
1 |
0 |
|a Alm, Eric J.
|e author
|
245 |
0 |
0 |
|a Rapid evolutionary innovation during an Archaean genetic expansion
|
260 |
|
|
|c 2011-02-23T14:38:23Z.
|
856 |
|
|
|z Get fulltext
|u http://hdl.handle.net/1721.1/61263
|
520 |
|
|
|a The natural history of Precambrian life is still unknown because of the rarity of microbial fossils and biomarkers. However, the composition of modern-day genomes may bear imprints of ancient biogeochemical events. Here we use an explicit model of macroevolution including gene birth, transfer, duplication and loss events to map the evolutionary history of 3,983 gene families across the three domains of life onto a geological timeline. Surprisingly, we find that a brief period of genetic innovation during the Archaean eon, which coincides with a rapid diversification of bacterial lineages, gave rise to 27% of major modern gene families. A functional analysis of genes born during this Archaean expansion reveals that they are likely to be involved in electron-transport and respiratory pathways. Genes arising after this expansion show increasing use of molecular oxygen (P = 3.4 × 10[superscript −8]) and redox-sensitive transition metals and compounds, which is consistent with an increasingly oxygenating biosphere.
|
546 |
|
|
|a en_US
|
655 |
7 |
|
|a Article
|
773 |
|
|
|t Nature
|