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      Thoughts on the evolution and ecological niche of diatoms

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          Photosynthetic rates derived from satellite-based chlorophyll concentration

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            Horizontal gene transfer in eukaryotic evolution.

            Horizontal gene transfer (HGT; also known as lateral gene transfer) has had an important role in eukaryotic genome evolution, but its importance is often overshadowed by the greater prevalence and our more advanced understanding of gene transfer in prokaryotes. Recurrent endosymbioses and the generally poor sampling of most nuclear genes from diverse lineages have also complicated the search for transferred genes. Nevertheless, the number of well-supported cases of transfer from both prokaryotes and eukaryotes, many with significant functional implications, is now expanding rapidly. Major recent trends include the important role of HGT in adaptation to certain specialized niches and the highly variable impact of HGT in different lineages.
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              Estimating the timing of early eukaryotic diversification with multigene molecular clocks.

              Although macroscopic plants, animals, and fungi are the most familiar eukaryotes, the bulk of eukaryotic diversity is microbial. Elucidating the timing of diversification among the more than 70 lineages is key to understanding the evolution of eukaryotes. Here, we use taxon-rich multigene data combined with diverse fossils and a relaxed molecular clock framework to estimate the timing of the last common ancestor of extant eukaryotes and the divergence of major clades. Overall, these analyses suggest that the last common ancestor lived between 1866 and 1679 Ma, consistent with the earliest microfossils interpreted with confidence as eukaryotic. During this interval, the Earth's surface differed markedly from today; for example, the oceans were incompletely ventilated, with ferruginous and, after about 1800 Ma, sulfidic water masses commonly lying beneath moderately oxygenated surface waters. Our time estimates also indicate that the major clades of eukaryotes diverged before 1000 Ma, with most or all probably diverging before 1200 Ma. Fossils, however, suggest that diversity within major extant clades expanded later, beginning about 800 Ma, when the oceans began their transition to a more modern chemical state. In combination, paleontological and molecular approaches indicate that long stems preceded diversification in the major eukaryotic lineages.
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                Author and article information

                Contributors
                (View ORCID Profile)
                Journal
                Ecological Monographs
                Ecol Monogr
                Wiley
                0012-9615
                1557-7015
                August 2021
                May 25 2021
                August 2021
                : 91
                : 3
                Affiliations
                [1 ]Department of Botany and Plant Pathology Oregon State University 4575 SW Research Way Corvallis Oregon 97333 USA
                [2 ]Department of Microbiology Oregon State University Nash Hall 226 Corvallis Oregon 97331 USA
                [3 ]School of Marine Sciences University of Maine 5706 Aubert Hall Orono Maine 04469‐5706 USA
                [4 ]Department of Biology Colorado State University Biology Building, Room 111, 1878 Campus Delivery Fort Collins Colorado 80523‐1878 USA
                Article
                10.1002/ecm.1457
                a97d99cb-8f69-4331-bb1e-5d07bb2e901a
                © 2021

                http://creativecommons.org/licenses/by-nc/4.0/

                http://doi.wiley.com/10.1002/tdm_license_1.1

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