Thrive with Additional Sets of Genome Widespread Paleopolyploidization Buffers plants Through Eocene Climatic Upheaval


Meeting Abstract

37-1  Saturday, Jan. 5 08:00 – 08:15  Thrive with Additional Sets of Genome: Widespread Paleopolyploidization Buffers plants Through Eocene Climatic Upheaval CAI, L*; XI, Z; AMORIM, AM; SUGUMARAN, M; REST, JS; LIU, L; DAVIS, CC; Harvard Univ., Cambridge; Harvard Univ., Cambridge; Universidade Estadual de Santa Cruz, Brazil; Univ. of Malaya, Malaysia; Stony Brook Univ., Stony Brook; Univ. of Georgia, Athens; Harvard Univ., Cambridge lcai@g.harvard.edu

Ancient whole genome duplications (WGDs) are important in eukaryotic genome evolution, and are especially prominent in plants. Recent genomic studies from large vascular plant clades, including ferns, gymnosperms, and angiosperms suggest that WGDs may represent a crucial mode of speciation. Moreover, numerous WGDs have been dated to events coinciding with major episodes of global and climatic upheaval, including the mass extinction at the KT boundary (~65 Ma) and during more recent intervals of global aridification in the Miocene (~10-5 Ma). These findings have led to the hypothesis that polyploidization may buffer lineages against the negative consequences of such disruptions. This work explores WGDs in the largely tropical flowering plant clade Malpighiales using a combination of newly sequenced transcriptomes and complete genomes from 42 species. We conservatively identify 22 ancient WGDs, widely distributed across Malpighiales subclades. Importantly, these events are clustered around the Eocene-Paleocene Transition (~54 Ma), during which time the planet was warmer and wetter than any period in the Cenozoic. These results establish that the Eocene Climate Optimum represents another, previously unrecognized, period of prolific WGDs in plants, and lends support to the hypothesis that polyploidization promotes adaptation and enhances plant survival during major episodes of global change. Malpighiales, in particular, may have been particularly influenced by these events given their predominance in the tropics where Eocene warming likely had profound impacts owing to the relatively tight thermal tolerances of tropical organisms.

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