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Eocene scaled chrysophytes with pronounced modern affinities
This is the first documentation of scaled chrysophytes of Tertiary age. Siliceous scales belonging to four genera (Synura,Mallomonas,Chrysosphaerella, andSpiniferomonas) are preserved in middle Eocene (∼47 Ma) lacustrine mudstones deposited in a posteruptive crater associated with kimberlite intrusi...
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Published in: | International journal of plant sciences 2005-05, Vol.166 (3), p.533-536 |
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container_title | International journal of plant sciences |
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creator | Siver, P.A Wolfe, A.P |
description | This is the first documentation of scaled chrysophytes of Tertiary age. Siliceous scales belonging to four genera (Synura,Mallomonas,Chrysosphaerella, andSpiniferomonas) are preserved in middle Eocene (∼47 Ma) lacustrine mudstones deposited in a posteruptive crater associated with kimberlite intrusion near Lac de Gras, Northwest Territories, Canada. Astonishingly, most of these microfossils have remarkable morphological affinities with extant congeneric taxa, indicating that the unique siliceous ornamentation of the scaled chrysophytes, including scales, spines, and bristles, was fully evolved by the middle Eocene. These observations imply that the scaled chrysophytes experienced prolonged intervals of relative evolutionary stasis during Neogene and Quaternary times and thus provide a new evolutionary milepost for this algal group. |
doi_str_mv | 10.1086/428702 |
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Siliceous scales belonging to four genera (Synura,Mallomonas,Chrysosphaerella, andSpiniferomonas) are preserved in middle Eocene (∼47 Ma) lacustrine mudstones deposited in a posteruptive crater associated with kimberlite intrusion near Lac de Gras, Northwest Territories, Canada. Astonishingly, most of these microfossils have remarkable morphological affinities with extant congeneric taxa, indicating that the unique siliceous ornamentation of the scaled chrysophytes, including scales, spines, and bristles, was fully evolved by the middle Eocene. These observations imply that the scaled chrysophytes experienced prolonged intervals of relative evolutionary stasis during Neogene and Quaternary times and thus provide a new evolutionary milepost for this algal group.</description><identifier>ISSN: 1058-5893</identifier><identifier>EISSN: 1537-5315</identifier><identifier>DOI: 10.1086/428702</identifier><language>eng</language><publisher>Chicago: The University of Chicago Press</publisher><subject>Algae ; Chrysophyta ; Chrysosphaerella ; Evolutionary biology ; Fossils ; Giraffes ; Golden brown algae ; Lacustrine sediments ; Mallomonas ; Microfossils ; Paleobotany ; Peridotite ; plant morphology ; Sediments ; Spiniferomonas ; Synura ; Taxa ; ultrastructure</subject><ispartof>International journal of plant sciences, 2005-05, Vol.166 (3), p.533-536</ispartof><rights>2005 by The University of Chicago. 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subjects | Algae Chrysophyta Chrysosphaerella Evolutionary biology Fossils Giraffes Golden brown algae Lacustrine sediments Mallomonas Microfossils Paleobotany Peridotite plant morphology Sediments Spiniferomonas Synura Taxa ultrastructure |
title | Eocene scaled chrysophytes with pronounced modern affinities |
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