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Acid-prepared specimens of the placoderm (Early Devonian of New South Wales, Australia) revealed placoderm endocranial anatomy in unprecedented detail. has become a key taxon in discussions of early gnathostome phylogeny, and the question of placoderm monophyly versus paraphyly. The anterior orientation of the facial nerve and related hyoid arch structures in this taxon resemble fossil osteostracans (jawless vertebrates) rather than other early gnathostomes. New specimens of now reveal the previously unknown anterior region of the skull, including an exceptionally elongate premedian bone forming a long rostrum, supported by a thin extension of the postethmo-occipital unit of the braincase. Lateral overlap surfaces indicate an unusual anterior position for the jaws. Digital rendering of a synchrotron radiation scan reveals a uniquely specialized ethmoid commissure sensory canal, doubled back and fused into a midline canal. The visceral surface of the premedian bone has a plexus of perichondral bone canals. An updated skull roof reconstruction of adds to the highly variable dermal skull patterns of the probably non-monophyletic 'acanthothoracids'. The unusual morphology revealed by the new specimens suggests that the earliest known reef fish fauna contained a diverse range of fishes with specialized ecological roles.
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http://dx.doi.org/10.1098/rsos.180094 | DOI Listing |
R Soc Open Sci
September 2025
Department of Understanding Evolution, Naturalis Biodiversity Center, Leiden, The Netherlands.
The origin of jaws and teeth represents one of the most formative episodes in our own evolutionary history. However, this event is poorly understood because of a lack of detailed knowledge of key lineages, including the 'acanthothoracid' placoderms, which were among the earliest jawed vertebrates. Here, we describe sp.
View Article and Find Full Text PDFProc Natl Acad Sci U S A
September 2025
Department of Earth and Space Sciences, University of Washington, Seattle, WA 98195-1310.
The oxygenation history of Earth's surface environments has had a profound influence on the ecology and evolution of metazoan life. It was traditionally thought that the Neoproterozoic Oxygenation Event enabled the origin of animals in marine environments, followed by their persistence in aerobic marine habitats ever since. However, recent studies of redox proxies (e.
View Article and Find Full Text PDFSci Rep
August 2025
Polish Geological Institute-National Research Institute, 4 Rakowiecka Street, Warsaw, PL-00-975, Poland.
A new trackway produced by crawling fishes, which includes imprints of the trunk, snout, tail, body drag traces, and pectoral fins, was discovered in the Lower Devonian (middle-upper Emsian) marginal marine deposits in the Holy Cross Mountains, Poland. The snout imprints are represented by a low-angle variant of the already described Osculichnus tarnowskae, which has generally been interpreted as a hunting trace of fishes. However, in this case, it is considered an imprint of a fish's snout, used for anchoring in the sediment during the locomotion of at least partially emerged fish.
View Article and Find Full Text PDFProc Biol Sci
June 2025
Department of Geology and Geography, West Virginia University, Morgantown, WV 26506, USA.
Horseshoe crabs are an ancient lineage with an evolutionary history stretching back 450 million years and are generally considered to be examples of 'living fossils' exhibiting slow rates of evolution. Despite this reputation, relatively little is known of the early evolution of the group, with only two species described from the Ordovician and a subsequent 80-million-year gap in their fossil record until xiphosurids appear in the Late Devonian. Furthermore, all described Ordovician species are assigned to a single genus, with their close phylogenetic relatedness rendering it unclear whether their morphology is representative of the horseshoe crab ground pattern or an independently derived condition.
View Article and Find Full Text PDFAnn Bot
June 2025
Department of Biological Sciences, California State Polytechnic University - Humboldt, Arcata, California 95521, USA.
Background And Aims: Rooting structures have been documented in different Early Devonian plants, including rhyniophytes and zosterophylls. However, the basal euphyllophytes - the plexus from which modern ferns, equisetophytes and seed plants evolved - are the only group with no known rooting structures in Early Devonian representatives. We revisit the early euphyllophyte Psilophyton crenulatum whose emergences have implications for rooting structure evolution within the clade.
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